TY - JOUR A1 - Klaver, Martijn A1 - Steenstra, Edgar S. A1 - Borchert, Manuela A1 - Welter, Edmund A1 - Wilke, Max A1 - Berndt, Jasper A1 - Klemme, Stephan T1 - The effect of alkalinity on Ni-O bond length in silicate glasses BT - implications for Ni isotope geochemistry JF - Chemical geology : official journal of the European Association for Geochemistry N2 - Equilibrium mass-dependent ("stable") isotopic fractionation of an element during magmatic processes is driven by a contrast in bonding environment between minerals and silicate melt, which is expressed as an isotopic fractionation factor. A quantitative understanding of such isotopic fractionation factors is vital to interpret observed isotopic variations in magmatic rocks. It is well known that the local environment and the bond strength of an element dictate the sign and magnitude of isotopic fractionation between minerals, but it is uncertain how the structure and chemical composition of a silicate melt can affect mineral-melt isotopic fractionation factors. To explore this, we studied the coordination environment of nickel (Ni) in different silicate glasses using extended X-ray absorption fine structure (EXAFS) measurements at the German synchrotron X-ray source (DESY). We determined -Ni-O bond lengths in a suite of synthetic but near-natural silicate glasses using EXAFS and found that the former vary systematically with melt alkalinity, which is best described by the parameter ln[1 + (Na + K)/Ca]. With increasing melt alkalinity, Ni occupies more IV-fold coordinated sites, which are associated with a shorter -Ni-O bond length. Next, we use the ionic model, which allows to predict isotopic fractionation factors based on the difference in bond length between two phases. We find that more alkaline melts have a stronger preference for the heavier isotopes of Ni than less alkaline melts. This implies that the magnitude of mineral-melt Ni isotope fractionation factors, for instance between olivine and melt, will depend on the alkalinity of the melt. At magmatic temperatures, however, the variation in fractionation factors caused by melt alkalinity will rarely exceed 0.05 parts per thousand and is thus mostly negligible, in particular in the realm of basaltic melt compositions. Nevertheless, the relationship between melt alkalinity and fractionation factor reported here can be used to extrapolate empirical data for mineral-melt Ni isotope fractionation factors, once such data become available, to the full range of magma compositions on Earth and other Solar System bodies. KW - EXAFS KW - Ni-O bond length KW - silicate glasses KW - Ni isotopes KW - isotopic fractionation factors Y1 - 2022 U6 - https://doi.org/10.1016/j.chemgeo.2022.121070 SN - 0009-2541 SN - 1872-6836 VL - 610 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Regenspurg, Simona A1 - Virchow, Lioba A1 - Wilke, Franziska D. H. A1 - Zimmer, Martin A1 - Jolie, Egbert A1 - Hachenberger, Annika A1 - Yirgu, Gezahegn A1 - Gebru, Ermias Filfilu A1 - Vieth-Hillebrand, Andrea A1 - Gizaw, Berhanu T1 - Origin and migration of fluoride in the area of the Aluto Volcanic Complex (Main Ethiopian Rift) JF - Applied geochemistry : journal of the International Association of Geochemistry and Cosmochemistry N2 - Fluoride-enriched ground and surface waters represent a major health risk for the local population in many areas along the East African Rift. The present study investigates the origin of fluoride and the reason for its accumulation in the rift waters, following two hypotheses: (i) fluid-rock-interactions release fluoride from minerals into the water and (ii) magmatic-derived fluoride-containing liquids and gases migrate along permeable fault zones until they dissolve in ground-and surface water or be released to the atmosphere. Rock-, gas, water-, soil-, and plant samples were collected from the area within and close by the Aluto Volcanic Complex, which is part of the Main Ethiopian Rift. Most analyzed waters showed fluoride concentrations above the drinking water limit (> 1.5 mg/L) with the highest values in hot springs (up to 70 mg/L) and the geothermal well (76 mg/L). In the solid phase, a high fluoride content was found in acid volcanic rocks (ignimbrite: 4391 ppm; rhyolite: 3248 ppm) as well as in pumice (up to 1955 ppm). The fluoride content of soil samples collected within the volcanic complex varied between 82 and 1036 ppm, whereas former lake sediments from outside the Aluto Volcanic Complex showed higher fluoride contents ranging from 674 to 8171 ppm. Identified fluoride-rich minerals are various amphiboles (about 3 wt.-% F-), fluor-apatite (about 3 wt % F-), minerals of the fluorcaphite group (about 5 wt.-% F-), parisite (up to 9 wt.-% F-), and fluorite (CaF2). Elevated fluoride concentrations were also measured in some gas samples from fumaroles (up to 50 ppm) and in plant samples collected next to the fumaroles (up to 65 ppm). Leaching experiments of solid samples with deionized water demonstrated that fluoride can easily be mobilized from pumice and sediments but hardly from consolidated rocks. This fluoride release increased with temperature (up to 150 C) and correlated roughly with dis-solved silica indicating the binding of some fluoride to the amorphous or weakly crystalline silica fraction. Based on these results it was concluded that fluoride migrates via different pathways through the environment: At the depth of the magma chamber during magmatic differentiation fluoride enriches initially in the magmatic melt and accumulates in some late-crystallizing minerals of igneous rocks such as fluorite or mica. Upon volcanic eruption fluoride is predominantly incorporated in the glass (ignimbrite) and ash phase (pumice). On the surface, these rocks are exposed to weathering and fluoride leaches partly out into the aqueous phase. Soft and porous rocks such as pumice release fluoride first whereas hard extrusive/igneous rocks are less prone to weathering and retain the fluoride. Pumice and (lake) sediments might act both, as source and as sink for fluoride in the area. Although some fluoride might drain from the surface into the deeper subsoil, we conclude that magmatic fluids (liquid and gas) contribute more substantially to the overall fluoride ground water content because (i) of the much higher fluoride content in deep geothermal waters and hot springs as compared to surface-near waters; (ii) active geothermal surface manifestations located along fault zones indicate that fluids migrate from deep magmatic intrusions (as gas and liquid) towards the surface, where fluoride dissolves in groundwater; (iii) and the good correlation between bicarbonate (deriving from dissolution of magmatic CO2) and fluoride content in all analyzed water samples. KW - fluoride KW - environmental contaminant main Ethiopian rift KW - volcanic area KW - Aluto volcanic complex KW - volcanic gases KW - pumice Y1 - 2022 U6 - https://doi.org/10.1016/j.apgeochem.2022.105403 SN - 0883-2927 SN - 1872-9134 VL - 146 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Van der Looven, Thomas A1 - Winterleitner, Gerd A1 - Betzler, Christian A1 - Mutti, Maria T1 - A biotic perspective on the Oligo-Miocene evolution of the Maldives carbonate platform from forward stratigraphic modelling (Indian Ocean) JF - Marine and petroleum geology N2 - Forward stratigraphic modelling is a fast-developing modelling approach, used to test conceptual models, and predict stratigraphic architecture and depositional facies from basin to reservoir scales. Published subsurface applications demonstrate its added value by integrating multidisciplinary data as well as geological concepts into its constraints. When applied to carbonate depositional systems, composed of multiple sediment factories, the cooperating and interdependent production mechanisms remain poorly studied. By applying the technique to a well-studied section of the Maldives carbonate platform, a specific model design-adapted to the geological age and setting, and constrained by available data-sheds light on the interaction of its carbonate producers. The results yield a naturalistic depositional facies distribution and offer insight in the changing relationship between biotic communities during the platform evolution. After calibration, the reference model unequivocally links the formerly proposed genetic model to the seismostratigraphic architecture. Furthermore, the results show how environmental changes (seemingly of secondary impact compared to changes in physical accommodation in the stratigraphic record) can induce substantial fluctuations in carbonate production rates of biotic communities, affect the ecological accommodation, and thus impact the platform architecture. Therefore, it is crucial to treat carbonate production rates during periods of environmental change as variables with associated uncertainties in a forward stratigraphic model setup. KW - neogene KW - Maldives carbonate platform KW - forward stratigraphic modelling KW - sequence stratigraphy KW - carbonate production Y1 - 2022 U6 - https://doi.org/10.1016/j.marpetgeo.2022.105907 SN - 0264-8172 SN - 1873-4073 VL - 145 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Singh, Manudeo A1 - Sinha, Rajiv T1 - Integrating hydrological connectivity in a process-response framework for restoration and monitoring prioritisation of floodplain wetlands in the Ramganga Basin, India JF - Water N2 - Floodplain wetlands are critical for sustaining various ecological and hydrological functions in a riverine environment. Severe anthropogenic alterations and human occupation of floodplains have threatened these wetlands in several parts of the world. A major handicap in designing sustainable restoration and monitoring strategies for these wetlands is the lack of scientific process-based understanding and information on the basin-scale controls of their degradation. Here, we offer a novel approach to integrate the connectivity of the wetlands with the surrounding landscape along with other attributes such as stream density, hydrometeorological parameters, and groundwater dynamics to explain their degradation and then to prioritise them for restoration and monitoring. We hypothesise that the best possible connectivity scenario for the existence of a wetland would be if (a) the wetland has a high connectivity with its upslope area, and (b) the wetland has a low connectivity with its downslope region. The first condition ensures the flow of water into the wetland and the second condition allows longer water residence time in the wetland. Accordingly, we define four connectivity-based wetland health scenarios-good, no impact, bad, and worst. We have implemented the proposed method in 3226 wetlands in the Ramganga Basin in north India. Further, we have applied specific selection criteria, such as distance from the nearest stream and stream density, to prioritise the wetlands for restoration and monitoring. We conclude that the connectivity analysis offers a quick process-based assessment of wetlands' health status and serves as an important criterion to prioritise the wetlands for developing appropriate management strategies. KW - floodplain protection KW - ganga plains KW - hydrological connectivity KW - wetland health KW - wetland management Y1 - 2022 U6 - https://doi.org/10.3390/w14213520 SN - 2073-4441 VL - 14 IS - 21 PB - MDPI CY - Basel ER - TY - JOUR A1 - Loh, Yvonne Sena Akosua A1 - Fynn, Obed Fiifi A1 - Manu, Evans A1 - Afrifa, George Yamoah A1 - Addai, Millicent Obeng A1 - Akurugu, Bismark Awinbire A1 - Yidana, Sandow Mark T1 - Groundwater-surface water interactions BT - application of hydrochemical and stable isotope tracers to the lake bosumtwi area in Ghana JF - Environmental earth sciences N2 - This research demonstrated the application of hydrochemical data and stable water isotopes of delta O-18 and delta D (or delta 2H) for evaluating the relationship between surface water in Lake Bosumtwi and the underlying groundwater system. It aimed at determining the presence or absence of a hydraulic relationship and for evaluating the possible direction of flow at the interface between the two reservoirs. The study also estimated evaporative losses of infiltrating rainwater as it transits the unsaturated zone and provided important information on the hydrological processes prevailing in the area. The results of Q-Mode hierarchical cluster analysis (HCA) clearly differentiate the lake water from the groundwater based on their spatial relationship. These results indicated that groundwater recharge occurs on the hilltops of the crater, where it is slightly acidic with low levels of dissolved ions, characterised by short residence time and rapid unrestricted vertical infiltration and recharge. The groundwater becomes more mineralized with longer contact times and deeper circulation with the host rock, while it flows from the recharge areas towards the lake at lower elevations. Analyses of delta O-18 and delta D showed a high evaporation rate on the lake surface (90%) with a significant evaporative enrichment, whereas groundwater showed no significant isotopic variations. Thus suggesting that the aquifers have been recharged by recent meteoric water that has undergone some evaporative enrichment since the study established an evaporation rate of water infiltrating the unsaturated zone ranging from 54 to 60%. Both reservoirs do not appear to be hydraulically connected, and where such a connection exists, it is expected to favour the lake. KW - Lake Bosumtwi KW - stable isotopes KW - kinetic fractionation KW - surface water KW - groundwater KW - Ghana Y1 - 2022 U6 - https://doi.org/10.1007/s12665-022-10644-x SN - 1866-6280 SN - 1866-6299 VL - 81 IS - 22 PB - Springer CY - New York ER - TY - JOUR A1 - Lipus, Daniel A1 - Jia, Zeyu A1 - Bartholomäus, Alexander A1 - Burckhardt, Oliver A1 - Sondermann, Megan A1 - Wagner, Dirk A1 - Kallmeyer, Jens T1 - Circular metagenome-assembled genome of Methanobacterium sp. strain ERen5, a putative methanogenic, H2-utilizing terrestrial subsurface archaeon JF - Microbiology Resource Announcements N2 - A circular, single-contig Methanobacterium sp. metagenome-assembled genome (MAG) was recovered from high-CO2 enrichments inoculated with drill core material from the tectonic Eger Rift terrestrial subsurface. Annotation of the recovered MAG highlighted putative methanogenesis genes, providing valuable information on archaeal activity in the deep biosphere. Y1 - 2022 U6 - https://doi.org/10.1128/mra.00676-22 SN - 2576-098X VL - 11 IS - 10 PB - American Society for Microbiology CY - Washington ER - TY - JOUR A1 - Schifferle, Lukas A1 - Speziale, Sergio A1 - Lobanov, Sergey S. T1 - High-pressure evolution of the refractive index of MgO up to 140 GPa JF - Journal of applied physics N2 - Refractive index provides fundamental insights into the electronic structure of materials. At high pressure, however, the determination of refractive index and its wavelength dispersion is challenging, which limits our understanding of how physical properties of even simple materials, such as MgO, evolve with pressure. Here, we report on the measurement of room-temperature refractive index of MgO up to similar to 140 GPa. The refractive index of MgO at 600 nm decreases by similar to 2.4% from similar to 1.737 at 1 atm to similar to 1.696 (+/- 0.017) at similar to 140 GPa. Despite the index at 600 nm is essentially pressure independent, the absolute wavelength dispersion of the refractive index at 550-870 nm decreases by similar to 28% from similar to 0.015 at 1 atm to similar to 0.011 (+/- 8.04 x 10(-4)) at similar to 103 GPa. Single-effective-oscillator analysis of our refractive index data suggests that the bandgap of MgO increases by similar to 1.1 eV from 7.4 eV at 1 atm to similar to 8.5 (+/- 0.6) eV at similar to 103 GPa. Y1 - 2022 U6 - https://doi.org/10.1063/5.0106626 SN - 0021-8979 SN - 1089-7550 VL - 132 IS - 12 PB - AIP Publishing CY - Melville ER - TY - JOUR A1 - Bartholomäus, Alexander A1 - Mitzscherling, Julia A1 - Lipus, Daniel A1 - MacLean, Joana A1 - Wagner, Dirk T1 - Draft genome sequence of Paenalcaligenes niemegkensis NGK35T, isolated from plastic-polluted soil of an abandoned landfill JF - Microbiology Resource Announcements N2 - The Gram-negative bacterium Paenalcaligenes niemegkensis NGK35(T) was isolated from plastic debris in an abandoned landfill. It has the ability to grow on polyethylene and hexadecane as the sole carbon sources. Here, we report the corresponding draft genome, which contains 3.66 Mbp and is characterized by a G+C content of 52.1%. Y1 - 2022 U6 - https://doi.org/10.1128/mra.00671-22 SN - 2576-098X VL - 11 IS - 10 PB - American Society for Microbiology CY - Washington ER - TY - JOUR A1 - Rikani, Albano A1 - Frieler, Katja A1 - Schewe, Jacob T1 - Climate change and international migration BT - exploring the macroeconomic channel JF - PLoS one N2 - International migration patterns, at the global level, can to a large extent be explained through economic factors in origin and destination countries. On the other hand, it has been shown that global climate change is likely to affect economic development over the coming decades. Here, we demonstrate how these future climate impacts on national income levels could alter the global migration landscape. Using an empirically calibrated global migration model, we investigate two separate mechanisms. The first is through destination-country income, which has been shown consistently to have a positive effect on immigration. As countries' income levels relative to each other are projected to change in the future both due to different rates of economic growth and due to different levels of climate change impacts, the relative distribution of immigration across destination countries also changes as a result, all else being equal. Second, emigration rates have been found to have a complex, inverted U-shaped dependence on origin-country income. Given the available migration flow data, it is unclear whether this dependence-found in spatio-temporal panel data-also pertains to changes in a given migration flow over time. If it does, then climate change will additionally affect migration patterns through origin countries' emigration rates, as the relative and absolute positions of countries on the migration "hump" change. We illustrate these different possibilities, and the corresponding effects of 3 degrees C global warming (above pre-industrial) on global migration patterns, using climate model projections and two different methods for estimating climate change effects on macroeconomic development. Y1 - 2022 U6 - https://doi.org/10.1371/journal.pone.0276764 SN - 1932-6203 VL - 17 IS - 11 PB - PLoS CY - San Fransisco ER - TY - JOUR A1 - Dahm, Torsten A1 - Hainzl, Sebastian T1 - A Coulomb stress response model for time-dependent earthquake forecasts JF - Journal of geophysical research : Solid earth N2 - Seismicity models are probabilistic forecasts of earthquake rates to support seismic hazard assessment. Physics-based models allow extrapolating previously unsampled parameter ranges and enable conclusions on underlying tectonic or human-induced processes. The Coulomb Failure (CF) and the rate-and-state (RS) models are two widely used physics-based seismicity models both assuming pre-existing populations of faults responding to Coulomb stress changes. The CF model depends on the absolute Coulomb stress and assumes instantaneous triggering if stress exceeds a threshold, while the RS model only depends on stress changes. Both models can predict background earthquake rates and time-dependent stress effects, but the RS model with its three independent parameters can additionally explain delayed aftershock triggering. This study introduces a modified CF model where the instantaneous triggering is replaced by a mean time-to-failure depending on the absolute stress value. For the specific choice of an exponential dependence on stress and a stationary initial seismicity rate, we show that the model leads to identical results as the RS model and reproduces the Omori-Utsu relation for aftershock decays as well stress-shadowing effects. Thus, both CF and RS models can be seen as special cases of the new model. However, the new stress response model can also account for subcritical initial stress conditions and alternative functions of the mean time-to-failure depending on the problem and fracture mode. KW - seismicity KW - physics based model KW - earthquake physics Y1 - 2022 U6 - https://doi.org/10.1029/2022JB024443 SN - 2169-9313 SN - 2169-9356 VL - 127 IS - 9 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Sieber, Melanie J. A1 - Wilke, Max A1 - Appelt, Oona A1 - Oelze, Marcus A1 - Koch-Müller, Monika T1 - Melting relations of Ca-Mg carbonates and trace element signature of carbonate melts up to 9 GPa - a proxy for melting of carbonated mantle lithologies JF - European journal of mineralogy N2 - The most profound consequences of the presence of Ca-Mg carbonates (CaCO3-MgCO3) in the Earth's upper mantle may be to lower the melting temperatures of the mantle and control the melt composition. Low-degree partial melting of a carbonate-bearing mantle produces CO2-rich, silica-poor melts compositionally imposed by the melting relations of carbonates. Thus, understanding the melting relations in the CaCO3-MgCO3 system facilitates the interpretation of natural carbonate-bearing silicate systems. We report the melting relations of the CaCO3-MgCO3 system and the partition coefficient of trace elements between carbonates and carbonate melt from experiments at high pressure (6 and 9 GPa) and temperature (1300-1800 degrees C) using a rocking multi-anvil press. In the absence of water, Ca-Mg carbonates are stable along geothermal gradients typical of subducting slabs. Ca-Mg carbonates ( similar to Mg0.1-0.9Ca0.9-0.1CO3) partially melt beneath mid-ocean ridges and in plume settings. Ca-Mg carbonates melt incongruently, forming periclase crystals and carbonate melt between 4 and 9 GPa. Furthermore, we show that the rare earth element (REE) signature of Group-I kimberlites, namely strong REE fractionation and depletion of heavy REE relative to the primitive mantle, is resembled by carbonate melt in equilibrium with Ca-bearing magnesite and periclase at 6 and 9 GPa. This suggests that the dolomite-magnesite join of the CaCO3-MgCO3 system might be useful to approximate the REE signature of carbonate-rich melts parental to kimberlites. Y1 - 2022 U6 - https://doi.org/10.5194/ejm-34-411-2022 SN - 0935-1221 SN - 1617-4011 VL - 34 IS - 5 SP - 411 EP - 424 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Jia, Zeyu A1 - Lipus, Daniel A1 - Bartholomaeus, Alexander A1 - Burckhardt, Oliver A1 - Sondermann, Megan A1 - Wagner, Dirk A1 - Kallmeyer, Jens T1 - Metagenome-assembled genome of a putative methanogenic Methanosarcina sp. strain enriched from terrestrial high-CO2 subsurface sediments JF - Microbiology Resource Announcements N2 - A metagenome-assembled genome (MAG), named Methanosarcina sp. strain ERenArc_MAG2, was obtained from a 3-month-old H-2/CO2 atmosphere enrichment culture, originally inoculated with 60-m deep drill core sediment collected from the tectonic Eger Rift terrestrial subsurface. Annotation of the recovered draft genome revealed putative archaeal methanogenesis genes in the deep biosphere. A metagenome-assembled genome (MAG), named Methanosarcina sp. strain ERenArc_MAG2, was obtained from a 3-month-old H-2/CO2 atmosphere enrichment culture, originally inoculated with 60-m deep drill core sediment collected from the tectonic Eger Rift terrestrial subsurface. Annotation of the recovered draft genome revealed putative archaeal methanogenesis genes in the deep biosphere. Y1 - 2022 U6 - https://doi.org/10.1128/mra.01039-22 SN - 2576-098X VL - 11 IS - 12 PB - American Society for Microbiology CY - Washington ER - TY - JOUR A1 - Lück, Erika A1 - Guillemoteau, Julien A1 - Tronicke, Jens A1 - Rummel, Udo A1 - Hierold, Wilfried T1 - From point to field scale-indirect monitoring of soil moisture variations at the DWD test site in Falkenberg JF - Geoderma : an international journal of soil science N2 - Information regarding the spatial distribution of soil water content is key in many disciplines and applications including soil and atmospheric sciences, hydrology, and agricultural engineering. Thus, within the past decades various experimental methods and strategies have been developed to map spatial variations in soil moisture distribution and to monitor temporal changes. Our study examines the combination of electrical resistivity mapping and point observations of soil moisture to infer the spatial and the temporal variability of soil moisture. Over a period of around two years, we performed field measurements on six days to collect repeated electrical resistivity mapping data for a nine-hectare test site south-east of Berlin, Germany. Permanently installed TDR probes, temporary TDR measurements within permanently installed tubes, and gravimetric measurements using soil samples provided soil moisture data at various selected points. In addition, soil analysis and classification results are available for 132 regularly distributed positions up to depths of 1.2 m. We compare and link three-dimensional resistivity models obtained via data inversion to soil composition and soil moisture as provided by our point data. Both the soil samples and the resistivity models indicate a two-layer medium characterized by a sandy top layer with varying thickness and a loamy bottom soil. For all six field campaigns, we observe similar resistivity patterns reflecting the temporally stable influence of soil texture. While the overall patterns are stable, the range of resistivity values changes with soil moisture. Finally, to estimate spatial models of soil moisture, we link our soil moisture and resistivity data using empirical petrophysical models relying on a second order polynomial function. We observe a mean prediction error for soil moisture of +/-0.034 m3 & BULL; m? 3 using all observation points while we notice that point-specific models further reduce the error. Thus, we conclude that our experimental and data analysis strategies represent a reliable approach to establish site-specific models and to estimate three-dimensional moisture distribution including temporal variations. KW - earth boundary layer KW - electrical conductivity KW - electrical resistivity KW - near-surface geophysics KW - soil moisture at field scale Y1 - 2022 U6 - https://doi.org/10.1016/j.geoderma.2022.116134 SN - 0016-7061 SN - 1872-6259 VL - 427 PB - Elsevier CY - Amsterdam ER - TY - THES A1 - Heckenbach, Esther Lina T1 - Geodynamic modeling of process interactions at continental plate boundaries N2 - Plate tectonic boundaries constitute the suture zones between tectonic plates. They are shaped by a variety of distinct and interrelated processes and play a key role in geohazards and georesource formation. Many of these processes have been previously studied, while many others remain unaddressed or undiscovered. In this work, the geodynamic numerical modeling software ASPECT is applied to shed light on further process interactions at continental plate boundaries. In contrast to natural data, geodynamic modeling has the advantage that processes can be directly quantified and that all parameters can be analyzed over the entire evolution of a structure. Furthermore, processes and interactions can be singled out from complex settings because the modeler has full control over all of the parameters involved. To account for the simplifying character of models in general, I have chosen to study generic geological settings with a focus on the processes and interactions rather than precisely reconstructing a specific region of the Earth. In Chapter 2, 2D models of continental rifts with different crustal thicknesses between 20 and 50 km and extension velocities in the range of 0.5-10 mm/yr are used to obtain a speed limit for the thermal steady-state assumption, commonly employed to address the temperature fields of continental rifts worldwide. Because the tectonic deformation from ongoing rifting outpaces heat conduction, the temperature field is not in equilibrium, but is characterized by a transient, tectonically-induced heat flow signal. As a result, I find that isotherm depths of the geodynamic evolution models are shallower than a temperature distribution in equilibrium would suggest. This is particularly important for deep isotherms and narrow rifts. In narrow rifts, the magnitude of the transient temperature signal limits a well-founded applicability of the thermal steady-state assumption to extension velocities of 0.5-2 mm/yr. Estimation of the crustal temperature field affects conclusions on all temperature-dependent processes ranging from mineral assemblages to the feasible exploitation of a geothermal reservoir. In Chapter 3, I model the interactions of different rheologies with the kinematics of folding and faulting using the example of fault-propagation folds in the Andean fold-and-thrust belt. The evolution of the velocity fields from geodynamic models are compared with those from trishear models of the same structure. While the latter use only geometric and kinematic constraints of the main fault, the geodynamic models capture viscous, plastic, and elastic deformation in the entire model domain. I find that both models work equally well for early, and thus relatively simple stages of folding and faulting, while results differ for more complex situations where off-fault deformation and secondary faulting are present. As fault-propagation folds can play an important role in the formation of reservoirs, knowledge of fluid pathways, for example via fractures and faults, is crucial for their characterization. Chapter 4 deals with a bending transform fault and the interconnections between tectonics and surface processes. In particular, the tectonic evolution of the Dead Sea Fault is addressed where a releasing bend forms the Dead Sea pull-apart basin, while a restraining bend further to the North resulted in the formation of the Lebanese mountains. I ran 3D coupled geodynamic and surface evolution models that included both types of bends in a single setup. I tested various randomized initial strain distributions, showing that basin asymmetry is a consequence of strain localization. Furthermore, by varying the surface process efficiency, I find that the deposition of sediment in the pull-apart basin not only controls basin depth, but also results in a crustal flow component that increases uplift at the restraining bend. Finally, in Chapter 5, I present the computational basis for adding further complexity to plate boundary models in ASPECT with the implementation of earthquake-like behavior using the rate-and-state friction framework. Despite earthquakes happening on a relatively small time scale, there are many interactions between the seismic cycle and the long time spans of other geodynamic processes. Amongst others, the crustal state of stress as well as the presence of fluids or changes in temperature may alter the frictional behavior of a fault segment. My work provides the basis for a realistic setup of involved structures and processes, which is therefore important to obtain a meaningful estimate for earthquake hazards. While these findings improve our understanding of continental plate boundaries, further development of geodynamic software may help to reveal even more processes and interactions in the future. N2 - Plattentektonische Grenzen bilden die Nahtstellen zwischen tektonischen Platten. Sie werden durch eine Vielzahl von unterschiedlichen und miteinander verknüpften Prozessen geformt und spielen eine Schlüsselrolle im Bereich der Georisiken und der Entstehung von Georessourcen. Viele dieser Prozesse sind bereits erforscht, während viele andere noch unbearbeitet oder unentdeckt sind. In dieser Arbeit wird die geodynamische numerische Modellierungssoftware ASPECT verwendet, um weitere Prozessinteraktionen an kontinentalen Plattengrenzen zu untersuchen. Im Gegensatz zu natürlichen Daten hat die geodynamische Modellierung den Vorteil, dass Prozesse direkt quantifiziert und alle Parameter über die gesamte Entwicklung einer Struktur analysiert werden können. Außerdem können Prozesse und Wechselwirkungen aus komplexen Zusammenhängen herausgefiltert werden, da der Modellierer volle Kontrolle über alle beteiligten Parameter hat. Um dem vereinfachenden Charakter von Modellen im Allgemeinen Rechnung zu tragen, habe ich mich für die Untersuchung allgemeiner geologischer Gegeben-heiten entschieden, wobei der Schwerpunkt auf den Prozessen und Wechselwirkungen liegt, anstatt eine bestimmte Region der Erde genau zu rekonstruieren. In Kapitel 2 werden 2D-Modelle von kontinentalen Rifts mit unterschiedlichen Krustendicken zwischen 20 und 50 km, sowie Extensionsgeschwindigkeiten im Bereich von 0,5-10 mm/Jahr verwendet, um eine Geschwindigkeitsgrenze für die Annahme eines thermischen Gleichgewichtszustandes zu erhalten, welcher üblicherweise verwendet wird, um die Temperaturfelder kontinentaler Rifts weltweit zu beschreiben. Da die Geschwindigkeit der tektonischen Deformation die der Wärmeleitung übersteigt, befindet sich das Temperaturfeld nicht im Gleichgewicht, sondern ist durch ein transientes, tektonisch induziertes Wärmestromsignal gekennzeichnet. Daraus ergibt sich, dass die Tiefen der Isothermen in den geodynamischen Entwicklungsmodellen flacher liegen, als es eine Temperaturverteilung im Gleichgewichtszustand vermuten ließe. Dies macht sich besondersbei tiefen Isothermen und narrow Rifts bemerkbar. In narrow Rifts begrenzt die Magnitude des transienten Temperatursignals eine fundierte Anwendbarkeit der thermischen Gleichgewichtsannahme auf Extensionsgeschwindigkeiten im Bereich von 0,5-2 mm/Jahr. Die Abschätzung des Temperaturfeldes der Erdkruste wirkt sich auf alle temperaturabhängigen Prozesse aus, von der Mineralzusammensetzung bis hin zur möglichen Nutzung eines geothermischen Reservoirs. In Kapitel 3 modelliere ich die Wechselwirkungen verschiedener Rheologien mit der Kinematik von Auffaltungen und Verwerfungen am Beispiel von fault-propagation folds im andinen Falten- und Überschiebungsgürtel. Die Entwicklung der Geschwindigkeitsfelder aus geodynamischen Modellen wird mit denen aus Trishear-Modellen für dieselbe Struktur verglichen. Während letztere nur geometrische und kinematische Charakteristika der Hauptverwerfung verwenden, erfassen die geodynamischen Modelle sowohl viskose, wie auch plastische und elastische Verformung im gesamten Modellbereich. Meine Forschung zeigt, dass beide Modelle für frühe und damit vergleichbar einfache Phasen der Auffaltung und Verwerfung gleichermaßen gut anwendbar sind, während die Ergebnisse für komplexere Situationen, in denen Verfor-mungen außerhalb der Hauptstörung sowie sekundäre Verwerfungen auftreten, auseinander gehen. Da fault-propagation folds eine wichtige Rolle bei der Bildung von Lagerstätten spielen können, ist Kenntnis zu Migrationswegen von Fluiden, zum Beispiel über Klüfte und Verwerfungen, für ihre Charakterisierung von entscheidender Bedeutung. Kapitel 4 befasst sich mit Biegungen von Transformstörungen sowie den Zusammenhängen zwischen Tektonik und Oberflächenprozessen. Insbesondere wird die tektonische Entwicklung der Verwerfung am Toten Meer behandelt, wo eine von Extension geprägte Biegung der Verwerfung das Pull-Apart-Becken des Toten Meeres bildet, während eine weiter nördlich gelegene von Kompression geprägte Biegung zur Bildung eines Gebirgszuges im Libanon führte. Für dieses Kapitel habe ich gekoppelte 3D Modelle der Geodynamik und Oberflächenentwicklung genutzt sowie beide Arten von Biegungen in einem Modell erforscht. Das Testen von verschiedenen, zufälligen Initialspannungsverteilungen zeigte, dass die Asymmetrie des Beckens eine Folge der Spannungslokalisierung ist. Außerdem habe ich durch Variation der Oberflächenprozesseffizienz herausgearbeitet, dass die Sedimentierung im Pull-Apart-Becken nicht nur die Beckentiefe steuert, sondern auch zu einer Strömungskomponente von Erdkrustenmaterial führt, die die Ablift an der von Kompression geprägten Biegung der Transformstörung erhöht. Anschließend stelle ich in Kapitel 5 die Implementierung von erdbebenähnlichem Verhalten unter Verwendung der Rate-and-State Gleichungen vor, welche die Grundlage für die Erweiterung der Komplexität von Plattengrenzenmodellen in ASPECT bildet. Obwohl Erdbeben auf einer relativ kurzen Zeitskala stattfinden, gibt es viele Wechselwirkungen zwischen dem seismischen Zyklus und den langen Zeitspannen anderer geodynamischer Prozesse. Unter anderem können der Spannungszustand der Kruste sowie das Vorhandensein von Fluiden oder Änderungen der Temperatur das Reibungsverhalten eines Störungssegmentes verändern. Meine Arbeit liefert die Grundlage für einen realistischen Aufbau der beteiligten Strukturen und Prozesse, der wichtig ist, um eine aussagekräftige Abschätzung der Erdbebengefährdung zu erhalten. Während diese Ergebnisse unser Verständnis der kontinentalen Plattengrenzen verbessern, kann die Weiterentwicklung geodynamischer Software dazu beitragen, in Zukunft weitere Prozesse und Wechselwirkungen aufzudecken. T2 - Geodynamische Modellierung von Prozessinteraktionen an kontinentalen Plattengrenzen KW - geodynamic modeling KW - plate boundaries KW - continental crust KW - heat flow KW - landscape evolution KW - geodynamische Modellierung KW - Plattengrenzen KW - kontinentale Kruste KW - Wärmediffusion KW - Oberflächenmodellierung Y1 - 2024 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-647500 ER - TY - JOUR A1 - Scherbaum, Frank A1 - Mzhavanadze, Nana A1 - Rosenzweig, Sebastian A1 - Müller, Meinard T1 - Tuning systems of traditional Georgian singing determined from a new corpus of field recordings JF - Musicologist N2 - In this study we examine the tonal organization of the 2016 GVM dataset, a newly-created corpus of high-quality multimedia field recordings of traditional Georgian singing with a focus on Svaneti. For this purpose, we developed a new processing pipeline for the computational analysis of non-western polyphonic music which was subsequently applied to the complete 2016 GVM dataset. To evaluate under what conditions a single tuning system is representative of current Svan performance practice, we examined the stability of the obtained tuning systems from an ensemble-, a song-, and a corpus-related perspective. Furthermore, we compared the resulting Svan tuning systems with the tuning systems obtained for the Erkomaishvili dataset (Rosenzweig et al., 2020) in the study by Scherbaum et al. (2020). In comparison to a 12-TET (12-tone-equal-temperament) system, the Erkomaishvili and the Svan tuning systems are surprisingly similar. Both systems show a strong presence of pure fourths (500 cents) and fifths (700 cents), and 'neutral' thirds (peaking around 350 cents) as well as 'neutral' sixths. In addition, the sizes of the melodic and the harmonic seconds in both tuning systems differ systematically from each other, with the size of the harmonic second being systematically larger than the melodic one. KW - traditional Georgian music KW - tuning KW - computational ethnomusicology Y1 - 2022 U6 - https://doi.org/10.33906/musicologist.1068947 SN - 2618-5652 VL - 6 IS - 2 SP - 142 EP - 168 PB - Trabzon Univ State Conservatory CY - Trabzon ER - TY - JOUR A1 - Bannister, Stephen A1 - Bertrand, Edward A. A1 - Heimann, Sebastian A1 - Bourguignon, Sandra A1 - Asher, Cameron A1 - Shanks, Jackson A1 - Harvison, Adrian T1 - Imaging sub-caldera structure with local seismicity, Okataina Volcanic Centre, Taupo Volcanic Zone, using double-difference seismic tomography JF - Journal of volcanology and geothermal research N2 - We examine sub-caldera structure and seismicity in and around the Okataina Volcanic Centre (OVC), Taupo Volcanic Zone, New Zealand, using seismic data collected over 4+ years with a temporary array of broadband and short-period seismometers, supplementing data from the permanent New Zealand seismometer network. We derive a new 3-D image of P-wave seismic velocity for the upper crust in the region, using double-difference seismic tomography and utilising waveform cross-correlations. We subsequently relocate 6989 earthquakes which occurred in the region over the 2010-2021 time period, using the 3D velocity model. The seismicity distribution shows spatial clusters west of Lake Rotomahana, as well as beneath Haroharo and the Makatiti Dome, inside the Okataina caldera. Beneath Makatiti Dome 90% of the events are shallower than 7.7 +/- 0.5 km. Outside of the Okataina caldera event relocations highlight short (similar to 3-4 km long) streaks of activity in the Ngakuru graben, part of the active Taupo Rift southwest of Okataina caldera. Inside the OVC the relocated seismicity beneath Makatiti appears closely associated with low (similar to 10%) P-wave velocity anomalies, which we resolve in the similar to 5-to-8-km depth range beneath the Okataina caldera, and which are likely related to partial melt and/or fluid-volatile pathways. Moment tensor analyses for two larger-magnitude events (M(L)4.5 and M(L)4.9) near Haroharo indicate normal faulting, with NNE-SSW fault strike, but with positive CLVD and positive isotropic components when allowing for a full moment tensor, consistent with a magmatic environment with degassing and/or fluid migration. KW - Okataina Caldera KW - Taupo Rift KW - seismic tomography KW - sub-caldera structure KW - Volcanic system Y1 - 2022 U6 - https://doi.org/10.1016/j.jvolgeores.2022.107653 SN - 0377-0273 SN - 1872-6097 VL - 431 PB - Elsevier CY - Amsterdam ER - TY - GEN A1 - Schoenfeldt, Elisabeth A1 - Panek, Tomas A1 - Winocur, Diego A1 - Silhan, Karel A1 - Korup, Oliver T1 - Corrigendum to: postglacial Patagonian mass movement BT - from rotational slides and spreads to earthflows T2 - Geomorphology : an international journal on pure and applied geomorphology Y1 - 2020 U6 - https://doi.org/10.1016/j.geomorph.2020.107471 SN - 0169-555X SN - 1872-695X VL - 373 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Kothari, Kritika A1 - Battisti, Rafael A1 - Boote, Kenneth J. A1 - Archontoulis, Sotirios A1 - Confalone, Adriana A1 - Constantin, Julie A1 - Cuadra, Santiago A1 - Debaeke, Philippe A1 - Faye, Babacar A1 - Grant, Brian A1 - Hoogenboom, Gerrit A1 - Jing, Qi A1 - van der Laan, Michael A1 - Macena da Silva, Fernando Antonio A1 - Marin, Fabio R. A1 - Nehbandani, Alireza A1 - Nendel, Claas A1 - Purcell, Larry C. A1 - Qian, Budong A1 - Ruane, Alex C. A1 - Schoving, Celine A1 - Silva, Evandro H. F. M. A1 - Smith, Ward A1 - Soltani, Afshin A1 - Srivastava, Amit A1 - Vieira, Nilson A. A1 - Slone, Stacey A1 - Salmeron, Montserrat T1 - Are soybean models ready for climate change food impact assessments? JF - European journal of agronomy : the official journal of the European Society for Agronomy N2 - An accurate estimation of crop yield under climate change scenarios is essential to quantify our ability to feed a growing population and develop agronomic adaptations to meet future food demand. A coordinated evaluation of yield simulations from process-based eco-physiological models for climate change impact assessment is still missing for soybean, the most widely grown grain legume and the main source of protein in our food chain. In this first soybean multi-model study, we used ten prominent models capable of simulating soybean yield under varying temperature and atmospheric CO2 concentration [CO2] to quantify the uncertainty in soybean yield simulations in response to these factors. Models were first parametrized with high quality measured data from five contrasting environments. We found considerable variability among models in simulated yield responses to increasing temperature and [CO2]. For example, under a + 3 degrees C temperature rise in our coolest location in Argentina, some models simulated that yield would reduce as much as 24%, while others simulated yield increases up to 29%. In our warmest location in Brazil, the models simulated a yield reduction ranging from a 38% decrease under + 3 degrees C temperature rise to no effect on yield. Similarly, when increasing [CO2] from 360 to 540 ppm, the models simulated a yield increase that ranged from 6% to 31%. Model calibration did not reduce variability across models but had an unexpected effect on modifying yield responses to temperature for some of the models. The high uncertainty in model responses indicates the limited applicability of individual models for climate change food projections. However, the ensemble mean of simulations across models was an effective tool to reduce the high uncertainty in soybean yield simulations associated with individual models and their parametrization. Ensemble mean yield responses to temperature and [CO2] were similar to those reported from the literature. Our study is the first demonstration of the benefits achieved from using an ensemble of grain legume models for climate change food projections, and highlights that further soybean model development with experiments under elevated [CO2] and temperature is needed to reduce the uncertainty from the individual models. KW - Agricultural Model Inter-comparison and Improvement Project (AgMIP); KW - Model ensemble KW - Model calibration KW - Temperature KW - Atmospheric CO2 KW - concentration KW - Legume model Y1 - 2022 U6 - https://doi.org/10.1016/j.eja.2022.126482 SN - 1161-0301 SN - 1873-7331 VL - 135 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Rajewar, S. K. A1 - Mohana Lakshmi, Ch. A1 - Mohanty, Aditya A1 - Pandey, Dwijendra N. A1 - Pandey, Anshuman A1 - Chaurasia, Anurag A1 - Pandey, Ananya A1 - Rajeswar Rao, V. A1 - Naidu, M. S. A1 - Kumar, Amit A1 - Mondal, Saroj K. A1 - Yadav, Rajeev K. A1 - Catherine, J. K. A1 - Giri, R. K. A1 - Gahalaut, Vineet Kumar T1 - Constraining plate motion and crustal deformation from GNSS measurements BT - CSIR-NGRI contribution JF - Journal of the Geological Society of India N2 - Geodetic studies of crustal deformation using Global Navigation Satellite System (GNSS, earlier commonly referred to as Global Positioning System, GPS) measurements at CSIR-NGRI started in 1995 with the installation of a permanent GNSS station at CSIR-NGRI Hyderabad which later became an International GNSS Service (IGS) site. The CSIR-NGRI started expanding its GNSS networks after 2003 with more focussed studies through installation in the NE India, Himalayan arc, Andaman subduction zone, stable and failed rift regions of India plate. In each instance, these measurements helped in unravelling the geodynamics of the region and seismic hazard assessment, e.g., the discovery of a plate boundary fault in the Indo-Burmese wedge, rate and mode of strain accumulation and its spatial variation in the Garhwal-Kumaun and Kashmir region of the Himalayan arc, the influence of non-tectonic deformation on tectonic deformation in the Himalayan arc, nature of crustal deformation through earthquake cycle in the Andaman Sumatra subduction zone, and localised deformation in the intraplate region and across the paleo rift regions. Besides these, GNSS measurements initiated in the Antarctica region have helped in understanding the plate motion and influence of seasonal variations on deformation. Another important by-product of the GNSS observations is the capabilities of these observations in understanding the ionospheric variations due to earthquake processes and also due to solar eclipse. We summarize these outcomes in this article. Y1 - 2021 U6 - https://doi.org/10.1007/s12594-021-1850-8 SN - 0974-6889 VL - 97 IS - 10 SP - 1207 EP - 1213 PB - Springer India CY - New Delhi ER - TY - JOUR A1 - Płóciennik, Mateusz A1 - Zawiska, Izabela A1 - Rzodkiewicz, Monika A1 - Noryśkiewicz, Agnieszka M. A1 - Słowiński, Michał A1 - Müller, Daniela A1 - Brauer, Achim A1 - Antczak-Orlewska, Olga A1 - Kramkowski, Mateusz A1 - Peyron, Odile A1 - Nevalainen, Liisa A1 - Luoto, Tomi P. A1 - Kotrys, Bartosz A1 - Seppä, Heikki A1 - Bidaurreta, Jon Camuera A1 - Rudna, Marta A1 - Mielczarek, Małgorzata A1 - Zawisza, Edyta A1 - Janowska, Ewa A1 - Błaszkiewicz, Mirosław T1 - Climatic and hydrological variability as a driver of the Lake Gościąż biota during the Younger Dryas JF - Catena N2 - The Younger Dryas (YD) is a roughly 1,100-year cold period marking the end of the last glaciation. Climate modelling for northern Europe indicates high summer temperatures and strong continentality. In eastern Europe, the scale of temperature variation and its influence on ecosystems is weakly recognised. Here, we present a multi-proxy reconstruction of YD conditions from Lake Gos ' ciaz (central Poland). The decadal-resolution analysis of its annually varved sediments indicates an initial decrease in Chironomidae-inferred mean July air temperature followed by steady warming. The pollen-inferred winter-to-summer temperature amplitude and annual precip-itation is highest at the Allerod/YD transition and the early YD (ca. 12.7-12.4 ky cal BP) and YD/Holocene (11.7-11.4 ka cal BP) transition. Temperature and precipitation were the main reasons for lake level fluctuations as reflected in the planktonic/littoral Cladocera ratio. The lake's diatom-inferred total phosphorus decreased with increasing summer temperature from about mid YD. Windy conditions in the early YD until ~12.3 ka cal BP caused water mixing and a short-lived/temporary increase in nutrient availability for phytoplankton. The Chironomidae-inferred summer temperature and pollen inferred summer temperature, winter temperature and annual precipitation herein are one of only a few in eastern Europe conducted with such high resolution. KW - Late Glacial KW - Varved sediments KW - Climate reconstructions KW - Chironomidae KW - Cladocera KW - Pollen KW - Diatoms Y1 - 2022 U6 - https://doi.org/10.1016/j.catena.2022.106049 SN - 0341-8162 SN - 1872-6887 VL - 212 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Lupien, Rachel L. A1 - Russell, James M. A1 - Pearson, Emma J. A1 - Castaneda, Isla S. A1 - Asrat, Asfawossen A1 - Förster, Verena A1 - Lamb, Henry F. A1 - Roberts, Helen M. A1 - Schäbitz, Frank A1 - Trauth, Martin H. A1 - Beck, Catherine C. A1 - Feibel, Craig S. A1 - Cohen, Andrew S. T1 - Orbital controls on eastern African hydroclimate in the Pleistocene JF - Scientific reports N2 - Understanding eastern African paleoclimate is critical for contextualizing early human evolution, adaptation, and dispersal, yet Pleistocene climate of this region and its governing mechanisms remain poorly understood due to the lack of long, orbitally-resolved, terrestrial paleoclimate records. Here we present leaf wax hydrogen isotope records of rainfall from paleolake sediment cores from key time windows that resolve long-term trends, variations, and high-latitude effects on tropical African precipitation. Eastern African rainfall was dominantly controlled by variations in low-latitude summer insolation during most of the early and middle Pleistocene, with little evidence that glacial-interglacial cycles impacted rainfall until the late Pleistocene. We observe the influence of high-latitude-driven climate processes emerging from the last interglacial (Marine Isotope Stage 5) to the present, an interval when glacial-interglacial cycles were strong and insolation forcing was weak. Our results demonstrate a variable response of eastern African rainfall to low-latitude insolation forcing and high-latitude-driven climate change, likely related to the relative strengths of these forcings through time and a threshold in monsoon sensitivity. We observe little difference in mean rainfall between the early, middle, and late Pleistocene, which suggests that orbitally-driven climate variations likely played a more significant role than gradual change in the relationship between early humans and their environment. Y1 - 2022 U6 - https://doi.org/10.1038/s41598-022-06826-z SN - 2045-2322 VL - 12 IS - 1 PB - Macmillan Publishers Limited CY - London ER - TY - JOUR A1 - DeFelipe, Irene A1 - Alcalde, Juan A1 - Baykiev, Eldar A1 - Bernal, Isabel A1 - Boonma, Kittiphon A1 - Carbonell, Ramon A1 - Flude, Stephanie A1 - Folch, Arnau A1 - Fullea, Javier A1 - García-Castellanos, Daniel A1 - Geyer, Adelina A1 - Giralt, Santiago A1 - Hernández, Armand A1 - Jiménez-Munt, Ivone A1 - Kumar, Ajay A1 - Llorens, Maria-Gema A1 - Martí, Joan A1 - Molina, Cecilia A1 - Olivar-Castaño, Andrés A1 - Parnell, Andrew A1 - Schimmel, Martin A1 - Torné, Montserrat A1 - Ventosa, Sergi T1 - Towards a digital twin of the Earth system: Geo-Soft-CoRe, a geoscientific software & code repository JF - Frontiers in earth science N2 - The immense advances in computer power achieved in the last decades have had a significant impact in Earth science, providing valuable research outputs that allow the simulation of complex natural processes and systems, and generating improved forecasts. The development and implementation of innovative geoscientific software is currently evolving towards a sustainable and efficient development by integrating models of different aspects of the Earth system. This will set the foundation for a future digital twin of the Earth. The codification and update of this software require great effort from research groups and therefore, it needs to be preserved for its reuse by future generations of geoscientists. Here, we report on Geo-Soft-CoRe, a Geoscientific Software & Code Repository, hosted at the archive DIGITAL.CSIC. This is an open source, multidisciplinary and multiscale collection of software and code developed to analyze different aspects of the Earth system, encompassing tools to: 1) analyze climate variability; 2) assess hazards, and 3) characterize the structure and dynamics of the solid Earth. Due to the broad range of applications of these software packages, this collection is useful not only for basic research in Earth science, but also for applied research and educational purposes, reducing the gap between the geosciences and the society. By providing each software and code with a permanent identifier (DOI), we ensure its self-sustainability and accomplish the FAIR (Findable, Accessible, Interoperable and Reusable) principles. Therefore, we aim for a more transparent science, transferring knowledge in an easier way to the geoscience community, and encouraging an integrated use of computational infrastructure. KW - digital twin KW - software KW - code KW - global change KW - hazards KW - solid earth Y1 - 2022 U6 - https://doi.org/10.3389/feart.2022.828005 SN - 2296-6463 VL - 10 PB - Frontiers Media CY - Lausanne ER - TY - JOUR A1 - Rosa, Angelika D. A1 - Dewaele, Agnès A1 - Garbarino, Gaston A1 - Svitlyk, Volodymyr A1 - Morard, Guillaume A1 - De Angelis, Filippo A1 - Krstulovic, Marija A1 - Briggs, Richard A1 - Irifune, Tetsuo A1 - Mathon, Olivier A1 - Bouhifd, Mohamed Ali T1 - Martensitic fcc-hcp transformation pathway in solid krypton and xenon and its effect on their equations of state JF - Physical review / publ. by The American Institute of Physics. B N2 - The martensitic transformation is a fundamental physical phenomenon at the origin of important industrial applications. However, the underlying microscopic mechanism, which is of critical importance to explain the outstanding mechanical properties of martensitic materials, is still not fully understood. This is because for most martensitic materials the transformation is a fast process that makes in situ studies extremely challenging. Noble solids krypton and xenon undergo a progressive pressure-induced face-centered cubic (fcc) to hexagonal close-packed (hcp) martensitic transition with a very wide coexistence domain. Here, we took advantage of this unique feature to study the detailed transformation progress at the atomic level by employing in situ x-ray diffraction and absorption spectroscopy. We evidenced a four-stage pathway and suggest that the lattice mismatch between the fcc and hcp forms plays a key role in the generation of strain. We also determined precisely the effect of the transformation on the compression behavior of these materials. Y1 - 2022 U6 - https://doi.org/10.1103/PhysRevB.105.144103 SN - 2469-9950 SN - 2469-9969 VL - 105 IS - 14 PB - American Physical Society CY - College Park ER - TY - JOUR A1 - Kutzschbach, Martin A1 - Wunder, Bernd A1 - Wannhoff, Iris A1 - Wilke, Franziska Daniela Helena A1 - Couffignal, Frédéric A1 - Rocholl, Alexander T1 - Raman spectroscopic quantification of tetrahedral boron in synthetic aluminum-rich tourmaline JF - American mineralogist : an international journal of earth and planetary materials N2 - The Raman spectra of five B-[4]-bearing tourmalines of different composition synthesized at 700 degrees C/4.0 GPa (including first-time synthesis of Na-Li-B-[4]-tourmaline, Ca-Li-B-[4]-tourmaline, and Ca-bearing square-B-[4]-tourmaline) reveal a strong correlation between the tetrahedral boron content and the summed relative intensity of all OH-stretching bands between 3300-3430 cm(-1). The band shift to low wavenumbers is explained by strong O3-H center dot center dot center dot O5 hydrogen bridge bonding. Applying the regression equation to natural B-[4]-bearing tourmaline from the Koralpe (Austria) reproduces the EMPA-derived value perfectly [EMPA: 0.67(12) B-[4] pfu vs. Raman: 0.66(13) B-[4] pfu]. This demonstrates that Raman spectroscopy provides a fast and easy-to-use tool for the quantification of tetrahedral boron in tourmaline. The knowledge of the amount of tetrahedral boron in tourmaline has important implications for the better understanding and modeling of B-isotope fractionation between tourmaline and fluid/melt, widely used as a tracer of mass transfer processes. KW - Tourmaline KW - high pressure KW - synthesis KW - tetrahedral boron KW - Raman KW - SIMS KW - Lithium KW - Beryllium and Boron: Quintessentially Crustal Y1 - 2021 U6 - https://doi.org/10.2138/am-2021-7758 SN - 0003-004X SN - 1945-3027 VL - 106 IS - 6 SP - 872 EP - 882 PB - Mineralogical Society of America CY - Washington, DC [u.a.] ER - TY - JOUR A1 - Farkas, Márton Pál A1 - Hofmann, Hannes A1 - Zimmermann, Günter A1 - Zang, Arno A1 - Bethmann, Falko A1 - Meier, Peter A1 - Cottrell, Mark A1 - Josephson, Neal T1 - Hydromechanical analysis of the second hydraulic stimulation in well PX-1 at the Pohang fractured geothermal reservoir, South Korea JF - Geothermics : an international journal of geothermal research and its applications N2 - In this study, we investigate numerically the hydro-mechanical behavior of fractured crystalline rock due to one of the five hydraulic stimulations at the Pohang Enhanced Geothermal site in South Korea. We use the commercial code FracMan (Golder Associates) that enables studying hydro-mechanical coupled processes in fractured media in three dimensions combining the finite element method with a discrete fracture network. The software is used to simulate fluid pressure perturbation at fractures during hydraulic stimulation. Our numerical simulation shows that pressure history matching can be obtained by partitioning the treatment into separate phases. This results in adjusted stress-aperture relationships. The evolution of aperture adjustment implies that the stimulation mechanism could be a combination of hydraulic fracturing and shearing. The simulated extent of the 0.01 MPa overpressure contour at the end of the treatment equals to similar to 180 m around the injection point. KW - Enhanced Geothermal System KW - Pohang geothermal reservoir KW - hydraulic KW - stimulation KW - PX-1 KW - FracMan Y1 - 2021 U6 - https://doi.org/10.1016/j.geothermics.2020.101990 SN - 0375-6505 SN - 1879-3576 VL - 89 PB - Elsevier CY - Amsterdam [u.a.] ER - TY - JOUR A1 - Licht, Alexis A1 - Kelson, Julia A1 - Bergel, Shelly J. A1 - Schauer, Andrew J. A1 - Petersen, Sierra Victoria A1 - Capirala, Ashika A1 - Huntington, Katharine W. A1 - Dupont-Nivet, Guillaume A1 - Win, Zaw A1 - Aung, Day Wa T1 - Dynamics of pedogenic carbonate growth in the tropical domain of Myanmar JF - Geochemistry, geophysics, geosystems N2 - Pedogenic carbonate is widespread at mid latitudes where warm and dry conditions favor soil carbonate growth from spring to fall. The mechanisms and timing of pedogenic carbonate formation are more ambiguous in the tropical domain, where long periods of soil water saturation and high soil respiration enhance calcite dissolution. This paper provides stable carbon, oxygen and clumped isotope values from Quaternary and Miocene pedogenic carbonates in the tropical domain of Myanmar, in areas characterized by warm (>18°C) winters and annual rainfall up to 1,700 mm. We show that carbonate growth in Myanmar is delayed to the driest and coldest months of the year by sustained monsoonal rainfall from mid spring to late fall. The range of isotopic variability in Quaternary pedogenic carbonates can be solely explained by temporal changes of carbonate growth within the dry season, from winter to early spring. We propose that high soil moisture year-round in the tropical domain narrows carbonate growth to the driest months and makes it particularly sensitive to the seasonal distribution of rainfall. This sensitivity is also enabled by high winter temperatures, allowing carbonate growth to occur outside the warmest months of the year. This high sensitivity is expected to be more prominent in the geological record during times with higher temperatures and greater expansion of the tropical realm. Clumped isotope temperatures, δ13C and δ18O values of tropical pedogenic carbonates are impacted by changes of both rainfall seasonality and surface temperatures; this sensitivity can potentially be used to track past tropical rainfall distribution. KW - clumped isotopes KW - pedogenic carbonate KW - monsoon Y1 - 2022 U6 - https://doi.org/10.1029/2021GC009929 SN - 1525-2027 VL - 23 IS - 7 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Sharma, Shubham A1 - Hainzl, Sebastian A1 - Zöller, Gert T1 - Seismicity parameters dependence on main shock-induced co-seismic stress JF - Geophysical journal international N2 - The Gutenberg-Richter (GR) and the Omori-Utsu (OU) law describe the earthquakes' energy release and temporal clustering and are thus of great importance for seismic hazard assessment. Motivated by experimental results, which indicate stress-dependent parameters, we consider a combined global data set of 127 main shock-aftershock sequences and perform a systematic study of the relationship between main shock-induced stress changes and associated seismicity patterns. For this purpose, we calculate space-dependent Coulomb Stress (& UDelta;CFS) and alternative receiver-independent stress metrics in the surrounding of the main shocks. Our results indicate a clear positive correlation between the GR b-value and the induced stress, contrasting expectations from laboratory experiments and suggesting a crucial role of structural heterogeneity and strength variations. Furthermore, we demonstrate that the aftershock productivity increases nonlinearly with stress, while the OU parameters c and p systematically decrease for increasing stress changes. Our partly unexpected findings can have an important impact on future estimations of the aftershock hazard. KW - earthquake hazards KW - earthquake interaction KW - forecasting and prediction KW - statistical seismology KW - b-value Y1 - 2023 U6 - https://doi.org/10.1093/gji/ggad201 SN - 0956-540X SN - 1365-246X VL - 235 IS - 1 SP - 509 EP - 517 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Dutta, Rishabh A1 - Jónsson, Sigurjón A1 - Vasyura-Bathke, Hannes T1 - Simultaneous Bayesian estimation of non-planar fault geometry and spatially-variable slip JF - JGR / AGU, American Geophysical Union : Solid earth N2 - Large earthquakes are usually modeled with simple planar fault surfaces or a combination of several planar fault segments. However, in general, earthquakes occur on faults that are non-planar and exhibit significant geometrical variations in both the along-strike and down-dip directions at all spatial scales. Mapping of surface fault ruptures and high-resolution geodetic observations are increasingly revealing complex fault geometries near the surface and accurate locations of aftershocks often indicate geometrical complexities at depth. With better geodetic data and observations of fault ruptures, more details of complex fault geometries can be estimated resulting in more realistic fault models of large earthquakes. To address this topic, we here parametrize non-planar fault geometries with a set of polynomial parameters that allow for both along-strike and down-dip variations in the fault geometry. Our methodology uses Bayesian inference to estimate the non-planar fault parameters from geodetic data, yielding an ensemble of plausible models that characterize the uncertainties of the non-planar fault geometry and the fault slip. The method is demonstrated using synthetic tests considering slip spatially distributed on a single continuous finite non-planar fault surface with varying dip and strike angles both in the down-dip and along-strike directions. The results show that fault-slip estimations can be biased when a simple planar fault geometry is assumed in presence of significant non-planar geometrical variations. Our method can help to model earthquake fault sources in a more realistic way and may be extended to include multiple non-planar fault segments or other geometrical fault complexities. KW - non-planar fault geometry KW - Bayesian estimation KW - InSAR and GNSS KW - source modeling Y1 - 2021 U6 - https://doi.org/10.1029/2020JB020441 SN - 2169-9313 SN - 2169-9356 VL - 126 IS - 7 PB - Wiley CY - Hoboken, NJ ER - TY - JOUR A1 - Blanke, Aglaja A1 - Kwiatek, Grzegorz A1 - Goebel, Thomas H. W. A1 - Bohnhoff, Marco A1 - Dresen, Georg T1 - Stress drop-magnitude dependence of acoustic emissions during laboratory stick-slip JF - Geophysical journal international / the Royal Astronomical Society, the Deutsche Geophysikalische Gesellschaft and the European Geophysical Society N2 - Earthquake source parameters such as seismic stress drop and corner frequency are observed to vary widely, leading to persistent discussion on potential scaling of stress drop and event size. Physical mechanisms that govern stress drop variations arc difficult to evaluate in nature and are more readily studied in controlled laboratory experiments. We perform two stick-slip experiments on fractured (rough) and cut (smooth) Westerly granite samples to explore fault roughness effects on acoustic emission (AE) source parameters. We separate large stick-slip events that generally saturate the seismic recording system from populations of smaller AE events which are sensitive to fault stresses prior to slip. AE event populations show many similarities to natural seismicity and may be interpreted as laboratory equivalent of natural microseismic events. We then compare the temporal evolution of mechanical data such as measured stress release during slip to temporal changes in stress drops derived from Alis using the spectral ratio technique. We report on two primary observations: (1) In contrast to most case studies for natural earthquakes, we observe a strong increase in seismic stress drop with AE size. (2) The scaling of stress drop with magnitude is governed by fault roughness, whereby the rough fault shows a more rapid increase of the stress drop magnitude relation with progressing large stick-slip events than the smooth fault. The overall range of AE sizes on the rough surface is influenced by both the average grain size and the width of the fault core. The magnitudes of the smallest AE events on smooth faults may also be governed by grain size. However, AEs significantly grow beyond peak roughness and the width of the fault core. Our laboratory tests highlight that source parameters vary substantially in the presence of fault zone heterogeneity (i.e. roughness and narrow grain size distribution), which may affect seismic energy partitioning and static stress drops of small and large AE events. KW - Acoustic properties KW - Body waves KW - Earthquake dynamics KW - Earthquake source observations KW - Dynamics and mechanics of faulting Y1 - 2021 U6 - https://doi.org/10.1093/gji/ggaa524 SN - 0956-540X SN - 1365-246X VL - 224 IS - 2 SP - 1372 EP - 1381 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Najman, Yani A1 - Sobel, Edward A1 - Millar, Ian A1 - Luan, Xiwu A1 - Zapata, Sebastian A1 - Garzanti, Eduardo A1 - Parra, Mauricio A1 - Vezzoli, Giovanni A1 - Zhang, Peng A1 - Wa Aung, Day A1 - Paw, Saw Mu Tha Lay A1 - Lwin, Thae Naung T1 - The timing of collision between Asia and the West Burma Terrane, and the development of the Indo-Burman Ranges JF - Tectonics N2 - The West Burma Terrane (WBT) is a small terrane bounded to the east by the Asian Sibumasu Block and to the west by the Indo-Burman Ranges (IBR), the latter being an exhumed accretionary prism that formed during subduction of Indian oceanic lithosphere beneath Asia. Understanding the geological history of the WBT is important for reconstruction of the closure history of the Tethys Ocean and India-Asia collision. Currently there are major discrepancies in the proposed timings of collision between the WBT with both India and Asia; whether the WBT collided with India or Asia first is debated, and proposed timings of collisions stretch from the Mesozoic to the Cenozoic. We undertook a multi-technique provenance study involving petrography, detrital zircon U-Pb and Hf analyses, rutile U-Pb analyses and Sr-Nd bulk rock analyses on sediments of the Central Myanmar Basins of the WBT. We determined that the first arrival of Asian material into the basin occurred after the earliest late Eocene and by the early Oligocene, thus placing a minimum constraint on the timing of WBT-Asia collision. Our low temperature thermochronological study of the IBR records two periods of exhumation, in the early-middle Eocene, and at the Oligo-Miocene boundary. The Eocene event may be associated with the collision of the WBT with India. The later event at the Oligo-Miocene boundary may be associated with changes in wedge dynamics resulting from increased sediment supply to the system; however a number of other possible causes provide equally plausible explanations for both events. KW - Central Myanmar Basin KW - Indo-Burman Ranges KW - low temperature thermochronology KW - detrital provenance KW - West Burma Terrane Y1 - 2022 U6 - https://doi.org/10.1029/2021TC007057 SN - 0278-7407 SN - 1944-9194 VL - 41 IS - 7 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Toumoulin, Agathe A1 - Tardif-Becquet, Delphine A1 - Donnadieu, Yannick A1 - Licht, Alexis A1 - Ladant, Jean-Baptiste A1 - Kunzmann, Lutz A1 - Dupont-Nivet, Guillaume T1 - Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse BT - a model-data comparison JF - Climate of the past : an interactive open access journal of the European Geosciences Union N2 - At the junction of greenhouse and icehouse climate states, the Eocene-Oligocene Transition (EOT) is a key moment in Cenozoic climate history. While it is associated with severe extinctions and biodiversity turnovers on land, the role of terrestrial climate evolution remains poorly resolved, especially the associated changes in seasonality. Some paleobotanical and geochemical continental records in parts of the Northern Hemisphere suggest the EOT is associated with a marked cooling in winter, leading to the development of more pronounced seasons (i.e., an increase in the mean annual range of temperature, MATR). However, the MATR increase has been barely studied by climate models and large uncertainties remain on its origin, geographical extent and impact. In order to better understand and describe temperature seasonality changes between the middle Eocene and the early Oligocene, we use the Earth system model IPSL-CM5A2 and a set of simulations reconstructing the EOT through three major climate forcings: pCO(2) decrease (1120, 840 and 560 ppm), the Antarctic ice-sheet (AIS) formation and the associated sea-level decrease. Our simulations suggest that pCO(2) lowering alone is not sufficient to explain the seasonality evolution described by the data through the EOT but rather that the combined effects of pCO(2) , AIS formation and increased continentality provide the best data-model agreement.pCO(2) decrease induces a zonal pattern with alternating increasing and decreasing seasonality bands particularly strong in the northern high latitudes (up to 8 degrees C MATR increase) due to sea-ice and surface albedo feedback. Conversely, the onset of the AIS is responsible for a more constant surface albedo yearly, which leads to a strong decrease in seasonality in the southern midlatitudes to high latitudes (> 40 degrees S). Finally, continental areas that emerged due to the sea-level lowering cause the largest increase in seasonality and explain most of the global heterogeneity in MATR changes (1MATR) patterns. The Delta MATR patterns we reconstruct are generally consistent with the variability of the EOT biotic crisis intensity across the Northern Hemisphere and provide insights on their underlying mechanisms. Y1 - 2022 U6 - https://doi.org/10.5194/cp-18-341-2022 SN - 1814-9324 SN - 1814-9332 VL - 18 IS - 2 SP - 341 EP - 362 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Smith, Taylor A1 - Boers, Niklas T1 - Global vegetation resilience linked to water availability and variability JF - Nature Communications N2 - Quantifying the resilience of vegetated ecosystems is key to constraining both present-day and future global impacts of anthropogenic climate change. Here we apply both empirical and theoretical resilience metrics to remotely-sensed vegetation data in order to examine the role of water availability and variability in controlling vegetation resilience at the global scale. We find a concise global relationship where vegetation resilience is greater in regions with higher water availability. We also reveal that resilience is lower in regions with more pronounced inter-annual precipitation variability, but find less concise relationships between vegetation resilience and intra-annual precipitation variability. Our results thus imply that the resilience of vegetation responds differently to water deficits at varying time scales. In view of projected increases in precipitation variability, our findings highlight the risk of ecosystem degradation under ongoing climate change. Vegetation dynamics depend on both the amount of precipitation and its variability over time. Here, the authors show that vegetation resilience is greater where water availability is higher and where precipitation is more stable from year to year. Y1 - 2023 U6 - https://doi.org/10.1038/s41467-023-36207-7 SN - 2041-1723 VL - 14 IS - 1 PB - Springer Nature CY - London ER - TY - JOUR A1 - Repasch, Marisa A1 - Scheingross, Joel S. A1 - Hovius, Niels A1 - Vieth-Hillebrand, Andrea A1 - Mueller, Carsten W. A1 - Höschen, Carmen A1 - Szupiany, Ricardo N. A1 - Sachse, Dirk T1 - River organic carbon fluxes modulated by hydrodynamic sorting of particulate organic matter JF - Geophysical research letters N2 - Rivers regulate the global carbon cycle by transferring particulate organic carbon (POC) from terrestrial landscapes to marine sedimentary basins, but the processes controlling the amount and composition of fluvially exported POC are poorly understood. We propose that hydrodynamic sorting processes modify POC fluxes during fluvial transit. We test this hypothesis by studying POC transported along a similar to 1,200 km reach of the Rio Bermejo, Argentina. Nanoscale secondary ion mass spectrometry revealed that POC was either fine, mineral-associated organic matter, or coarse discrete organic particles. Mineral-associated POC is more resistant to oxidation and has a lower particle settling velocity than discrete POC. Consequently, hydraulic sorting and downstream fining amplify the proportion of fine, mineral-associated POC from similar to 55% to similar to 78% over 1,220 km of downstream transit. This suggests that mineral-associated POC has a greater probability of export and preservation in marine basins than plant detritus, which may be oxidized to CO2 during transit. KW - compound-specific stable isotopes KW - carbon fluxes KW - rivers KW - NanoSIMS; KW - sediment transport KW - hydrodynamic sorting Y1 - 2022 U6 - https://doi.org/10.1029/2021GL096343 SN - 0094-8276 SN - 1944-8007 VL - 49 IS - 3 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Voglimacci-Stephanopoli, Joëlle A1 - Wendleder, Anna A1 - Lantuit, Hugues A1 - Langlois, Alexandre A1 - Stettner, Samuel A1 - Schmitt, Andreas A1 - Dedieu, Jean-Pierre A1 - Roth, Achim A1 - Royer, Alain T1 - Potential of X-band polarimetric synthetic aperture radar co-polar phase difference for arctic snow depth estimation JF - Cryosphere N2 - Changes in snowpack associated with climatic warming has drastic impacts on surface energy balance in the cryosphere. Yet, traditional monitoring techniques, such as punctual measurements in the field, do not cover the full snowpack spatial and temporal variability, which hampers efforts to upscale measurements to the global scale. This variability is one of the primary constraints in model development. In terms of spatial resolution, active microwaves (synthetic aperture radar - SAR) can address the issue and outperform methods based on passive microwaves. Thus, high-spatial-resolution monitoring of snow depth (SD) would allow for better parameterization of local processes that drive the spatial variability of snow. The overall objective of this study is to evaluate the potential of the TerraSAR-X (TSX) SAR sensor and the wave co-polar phase difference (CPD) method for characterizing snow cover at high spatial resolution. Consequently, we first (1) investigate SD and depth hoar fraction (DHF) variability between different vegetation classes in the Ice Creek catchment (Qikiqtaruk/Herschel Island, Yukon, Canada) using in situ measurements collected over the course of a field campaign in 2019; (2) evaluate linkages between snow characteristics and CPD distribution over the 2019 dataset; and (3) determine CPD seasonality considering meteorological data over the 2015-2019 period. SD could be extracted using the CPD when certain conditions are met. A high incidence angle (>30 circle) with a high topographic wetness index (TWI) (>7.0) showed correlation between SD and CPD (R2 up to 0.72). Further, future work should address a threshold of sensitivity to TWI and incidence angle to map snow depth in such environments and assess the potential of using interpolation tools to fill in gaps in SD information on drier vegetation types. Y1 - 2022 U6 - https://doi.org/10.5194/tc-16-2163-2022 SN - 1994-0416 SN - 1994-0424 VL - 16 IS - 6 SP - 2163 EP - 2181 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Haugk, Charlotte A1 - Jongejans, Loeka L. A1 - Mangelsdorf, Kai A1 - Fuchs, Matthias A1 - Ogneva, Olga A1 - Palmtag, Juri A1 - Mollenhauer, Gesine A1 - Mann, Paul J. A1 - Overduin, P. Paul A1 - Grosse, Guido A1 - Sanders, Tina A1 - Tuerena, Robyn E. A1 - Schirrmeister, Lutz A1 - Wetterich, Sebastian A1 - Kizyakov, Alexander A1 - Karger, Cornelia A1 - Strauss, Jens T1 - Organic matter characteristics of a rapidly eroding permafrost cliff in NE Siberia (Lena Delta, Laptev Sea region) JF - Biogeosciences N2 - Organic carbon (OC) stored in Arctic permafrost represents one of Earth's largest and most vulnerable terrestrial carbon pools. Amplified climate warming across the Arctic results in widespread permafrost thaw. Permafrost deposits exposed at river cliffs and coasts are particularly susceptible to thawing processes. Accelerating erosion of terrestrial permafrost along shorelines leads to increased transfer of organic matter (OM) to nearshore waters. However, the amount of terrestrial permafrost carbon and nitrogen as well as the OM quality in these deposits is still poorly quantified. We define the OM quality as the intrinsic potential for further transformation, decomposition and mineralisation. Here, we characterise the sources and the quality of OM supplied to the Lena River at a rapidly eroding permafrost river shoreline cliff in the eastern part of the delta (Sobo-Sise Island). Our multi-proxy approach captures bulk elemental, molecu- lar geochemical and carbon isotopic analyses of Late Pleistocene Yedoma permafrost and Holocene cover deposits, discontinuously spanning the last similar to 52 kyr. We showed that the ancient permafrost exposed in the Sobo-Sise cliff has a high organic carbon content (mean of about 5 wt %). The oldest sediments stem from Marine Isotope Stage (MIS) 3 interstadial deposits (dated to 52 to 28 cal ka BP) and are overlaid by last glacial MIS 2 (dated to 28 to 15 cal ka BP) and Holocene MIS 1 (dated to 7-0 cal ka BP) deposits. The relatively high average chain length (ACL) index of n-alkanes along the cliff profile indicates a predominant contribution of vascular plants to the OM composition. The elevated ratio of isoand anteiso-branched fatty acids (FAs) relative to mid- and long-chain (C >= 20) n-FAs in the interstadial MIS 3 and the interglacial MIS 1 deposits suggests stronger microbial activity and consequently higher input of bacterial biomass during these climatically warmer periods. The overall high carbon preference index (CPI) and higher plant fatty acid (HPFA) values as well as high C/N ratios point to a good quality of the preserved OM and thus to a high potential of the OM for decomposition upon thaw. A decrease in HPFA values downwards along the profile probably indicates stronger OM decomposition in the oldest (MIS 3) deposits of the cliff. The characterisation of OM from eroding permafrost leads to a better assessment of the greenhouse gas potential of the OC released into river and nearshore waters in the future. Y1 - 2022 U6 - https://doi.org/10.5194/bg-19-2079-2022 SN - 1726-4170 SN - 1726-4189 VL - 19 IS - 7 SP - 2079 EP - 2094 PB - Copernicus CY - Göttingen ER - TY - GEN A1 - Cesca, Simone A1 - Stich, Daniel A1 - Grigoli, Francesco A1 - Vuan, Alessandro A1 - López-Comino, José Ángel A1 - Niemz, Peter A1 - Blanch, Estefanía A1 - Dahm, Torsten A1 - Ellsworth, William L. T1 - Reply to: Multiple induced seismicity mechanisms at Castor underground gas storage illustrate the need for thorough monitoring T2 - Nature communications Y1 - 2022 U6 - https://doi.org/10.1038/s41467-022-30904-5 SN - 2041-1723 VL - 13 IS - 1 PB - Nature Research CY - Berlin ER - TY - JOUR A1 - Fuchs, Matthias A1 - Palmtag, Juri A1 - Juhls, Bennet A1 - Overduin, Pier Paul A1 - Grosse, Guido A1 - Abdelwahab, Ahmed A1 - Bedington, Michael A1 - Sanders, Tina A1 - Ogneva, Olga A1 - Fedorova, Irina A1 - Zimov, Nikita S. A1 - Mann, Paul J. A1 - Strauss, Jens T1 - High-resolution bathymetry models for the Lena Delta and Kolyma Gulf coastal zones JF - Earth system science data N2 - Arctic river deltas and deltaic near-shore zones represent important land-ocean transition zones influencing sediment dynamics and nutrient fluxes from permafrost-affected terrestrial ecosystems into the coastal Arctic Ocean. To accurately model fluvial carbon and freshwater export from rapidly changing river catchments as well as assess impacts of future change on the Arctic shelf and coastal ecosystems, we need to understand the sea floor characteristics and topographic variety of the coastal zones. To date, digital bathymetrical data from the poorly accessible, shallow, and large areas of the eastern Siberian Arctic shelves are sparse. We have digitized bathymetrical information for nearly 75 000 locations from large-scale (1 V 25000-1 V 500000) current and historical nautical maps of the Lena Delta and the Kolyma Gulf region in northeastern Siberia. We present the first detailed and seamless digital models of coastal zone bathymetry for both delta and gulf regions in 50 and 200m spatial resolution. We validated the resulting bathymetry layers using a combination of our own water depth measurements and a collection of available depth measurements, which showed a strong correlation (r>0.9). Our bathymetrical models will serve as an input for a high-resolution coupled hydrodynamic-ecosystem model to better quantify fluvial and coastal carbon fluxes to the Arctic Ocean, but they may be useful for a range of other studies related to Arctic delta and near-shore dynamics such as modeling of submarine permafrost, near-shore sea ice, or shelf sediment transport. The new digital high-resolution bathymetry products are available on the PANGAEA data set repository for the Lena Delta (https://doi.org/10.1594/PANGAEA.934045; Fuchs et al., 2021a) and Kolyma Gulf region (https://doi.org/10.1594/PANGAEA.934049; Fuchs et al., 2021b), respectively. Likewise, the depth validation data are available on PANGAEA as well (https://doi.org/10.1594/PANGAEA.933187; Fuchs et al., 2021c). Y1 - 2022 U6 - https://doi.org/10.5194/essd-14-2279-2022 SN - 1866-3508 SN - 1866-3516 VL - 14 IS - 5 SP - 2279 EP - 2301 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Jones, Benjamin M. A1 - Grosse, Guido A1 - Farquharson, Louise M. A1 - Roy-Léveillée, Pascale A1 - Veremeeva, Alexandra A1 - Kanevskiy, Mikhail Z. A1 - Gaglioti, Benjamin A1 - Breen, Amy L. A1 - Parsekian, Andrew D. A1 - Ulrich, Mathias A1 - Hinkel, Kenneth M. T1 - Lake and drained lake basin systems in lowland permafrost regions JF - Nature reviews earth and environment N2 - The formation, growth and drainage of lakes in Arctic and boreal lowland permafrost regions influence landscape and ecosystem processes. These lake and drained lake basin (L-DLB) systems occupy >20% of the circumpolar Northern Hemisphere permafrost region and similar to 50% of the area below 300 m above sea level. Climate change is causing drastic impacts to L-DLB systems, with implications for permafrost dynamics, ecosystem functioning, biogeochemical processes and human livelihoods in lowland permafrost regions. In this Review, we discuss how an increase in the number of lakes as a result of permafrost thaw and an intensifying hydrologic regime are not currently offsetting the land area gained through lake drainage, enhancing the dominance of drained lake basins (DLBs).The contemporary transition from lakes to DLBs decreases hydrologic storage, leads to permafrost aggradation, increases carbon sequestration and diversifies the shifting habitat mosaic in Arctic and boreal regions. However, further warming could inhibit permafrost aggradation in DLBs, disrupting the trajectory of important microtopographic controls on carbon fluxes and ecosystem processes in permafrost-region L-DLB systems. Further research is needed to understand the future dynamics of L-DLB systems to improve Earth system models, permafrost carbon feedback assessments, permafrost hydrology linkages, infrastructure development in permafrost regions and the well-being of northern socio-ecological systems. Y1 - 2022 U6 - https://doi.org/10.1038/s43017-021-00238-9 SN - 2662-138X VL - 3 IS - 1 SP - 85 EP - 98 PB - Springer Nature CY - London ER - TY - JOUR A1 - Sarr, Anta-Clarisse A1 - Donnadieu, Yannick A1 - Bolton, Clara T. A1 - Ladant, Jean-Baptiste A1 - Licht, Alexis A1 - Fluteau, Frédéric A1 - Laugié, Marie A1 - Tardif-Becquet, Delphine A1 - Dupont-Nivet, Guillaume T1 - Neogene South Asian monsoon rainfall and wind histories diverged due to topographic effects JF - Nature geoscience N2 - The drivers of the evolution of the South Asian Monsoon remain widely debated. An intensification of monsoonal rainfall recorded in terrestrial and marine sediment archives from the earliest Miocene (23-20 million years ago (Ma)) is generally attributed to Himalayan uplift. However, Indian Ocean palaeorecords place the onset of a strong monsoon around 13 Ma, linked to strengthening of the southwesterly winds of the Somali Jet that also force Arabian Sea upwelling. Here we reconcile these divergent records using Earth system model simulations to evaluate the interactions between palaeogeography and ocean-atmosphere dynamics. We show that factors forcing the South Asian Monsoon circulation versus rainfall are decoupled and diachronous. Himalayan and Tibetan Plateau topography predominantly controlled early Miocene rainfall patterns, with limited impact on ocean-atmosphere circulation. The uplift of the East African and Middle Eastern topography played a pivotal role in the establishment of the modern Somali Jet structure above the western Indian Ocean, while strong upwelling initiated as a direct consequence of the emergence of the Arabian Peninsula and the onset of modern-like atmospheric circulation. Our results emphasize that although elevated rainfall seasonality was probably a persistent feature since the India-Asia collision in the Paleogene, modern-like monsoonal atmospheric circulation only emerged in the late Neogene. Y1 - 2022 U6 - https://doi.org/10.1038/s41561-022-00919-0 SN - 1752-0894 SN - 1752-0908 VL - 15 IS - 4 SP - 314 EP - 319 PB - Nature Research CY - Berlin ER - TY - JOUR A1 - Flóvenz, Ólafur G. A1 - Wang, Rongjiang A1 - Hersir, Gylfi Páll A1 - Dahm, Torsten A1 - Hainzl, Sebastian A1 - Vassileva, Magdalena A1 - Drouin, Vincent A1 - Heimann, Sebastian A1 - Isken, Marius Paul A1 - Gudnason, Egill Á. A1 - Ágústsson, Kristján A1 - Ágústsdóttir, Thorbjörg A1 - Horálek, Josef A1 - Motagh, Mahdi A1 - Walter, Thomas R. A1 - Rivalta, Eleonora A1 - Jousset, Philippe A1 - Krawczyk, Charlotte M. A1 - Milkereit, Claus T1 - Cyclical geothermal unrest as a precursor to Iceland's 2021 Fagradalsfjall eruption JF - Nature geoscience N2 - Understanding and constraining the source of geodetic deformation in volcanic areas is an important component of hazard assessment. Here, we analyse deformation and seismicity for one year before the March 2021 Fagradalsfjall eruption in Iceland. We generate a high-resolution catalogue of 39,500 earthquakes using optical cable recordings and develop a poroelastic model to describe three pre-eruptional uplift and subsidence cycles at the Svartsengi geothermal field, 8 km west of the eruption site. We find the observed deformation is best explained by cyclic intrusions into a permeable aquifer by a fluid injected at 4 km depth below the geothermal field, with a total volume of 0.11 ± 0.05 km3 and a density of 850 ± 350 kg m–3. We therefore suggest that ingression of magmatic CO2 can explain the geodetic, gravity and seismic data, although some contribution of magma cannot be excluded. Y1 - 2022 U6 - https://doi.org/10.1038/s41561-022-00930-5 SN - 1752-0894 SN - 1752-0908 VL - 15 IS - 5 SP - 397 EP - 404 PB - Nature Research CY - Berlin ER - TY - JOUR A1 - Kaya, Mustafa Yücel A1 - Dupont-Nivet, Guillaume A1 - Frieling, Joost A1 - Fioroni, Chiara A1 - Rohrmann, Alexander A1 - Altıner, Sevinç Özkan A1 - Vardar, Ezgi A1 - Tanyas, Hakan A1 - Mamtimin, Mehmut A1 - Zhaojie, Guo T1 - The Eurasian epicontinental sea was an important carbon sink during the Palaeocene-Eocene thermal maximum JF - Communications earth and environment N2 - The Palaeocene-Eocene Thermal Maximum (ca. 56 million years ago) offers a primary analogue for future global warming and carbon cycle recovery. Yet, where and how massive carbon emissions were mitigated during this climate warming event remains largely unknown. Here we show that organic carbon burial in the vast epicontinental seaways that extended over Eurasia provided a major carbon sink during the Palaeocene-Eocene Thermal Maximum. We coupled new and existing stratigraphic analyses to a detailed paleogeographic framework and using spatiotemporal interpolation calculated ca. 720–1300 Gt organic carbon excess burial, focused in the eastern parts of the Eurasian epicontinental seaways. A much larger amount (2160–3900 Gt C, and when accounting for the increase in inundated shelf area 7400–10300 Gt C) could have been sequestered in similar environments globally. With the disappearance of most epicontinental seas since the Oligocene-Miocene, an effective negative carbon cycle feedback also disappeared making the modern carbon cycle critically dependent on the slower silicate weathering feedback. Y1 - 2022 U6 - https://doi.org/10.1038/s43247-022-00451-4 SN - 2662-4435 VL - 3 IS - 1 PB - Springer Nature CY - London ER - TY - JOUR A1 - Klose, Tim A1 - Guillemoteau, Julien A1 - Vignoli, Giulio A1 - Walter, Judith A1 - Herrmann, Andreas A1 - Tronicke, Jens T1 - Structurally constrained inversion by means of a Minimum Gradient Support regularizer: examples of FD-EMI data inversion constrained by GPR reflection data JF - Geophysical journal international N2 - Many geophysical inverse problems are known to be ill-posed and, thus, requiring some kind of regularization in order to provide a unique and stable solution. A possible approach to overcome the inversion ill-posedness consists in constraining the position of the model interfaces. For a grid-based parameterization, such a structurally constrained inversion can be implemented by adopting the usual smooth regularization scheme in which the local weight of the regularization is reduced where an interface is expected. By doing so, sharp contrasts are promoted at interface locations while standard smoothness constraints keep affecting the other regions of the model. In this work, we present a structurally constrained approach and test it on the inversion of frequency-domain electromagnetic induction (FD-EMI) data using a regularization approach based on the Minimum Gradient Support stabilizer, which is capable to promote sharp transitions everywhere in the model, i.e., also in areas where no structural a prioriinformation is available. Using 1D and 2D synthetic data examples, we compare the proposed approach to a structurally constrained smooth inversion as well as to more standard (i.e., not structurally constrained) smooth and sharp inversions. Our results demonstrate that the proposed approach helps in finding a better and more reliable reconstruction of the subsurface electrical conductivity distribution, including its structural characteristics. Furthermore, we demonstrate that it allows to promote sharp parameter variations in areas where no structural information are available. Lastly, we apply our structurally constrained scheme to FD-EMI field data collected at a field site in Eastern Germany to image the thickness of peat deposits along two selected profiles. In this field example, we use collocated constant offset ground-penetrating radar (GPR) data to derive structural a priori information to constrain the inversion of the FD-EMI data. The results of this case study demonstrate the effectiveness and flexibility of the proposed approach. KW - Controlled source electromagnetics (CSEM) KW - Inverse theory KW - Electrical properties KW - Ground penetrating radar KW - Frequency Domain Electromagnetics KW - Inversion Y1 - 2023 U6 - https://doi.org/10.1093/gji/ggad041 SN - 0956-540X SN - 1365-246X VL - 233 IS - 3 SP - 1938 EP - 1949 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Cesca, Simone A1 - Sugan, Monica A1 - Rudzinski, Lukasz A1 - Vajedian, Sanaz A1 - Niemz, Peter A1 - Plank, Simon A1 - Petersen, Gesa A1 - Deng, Zhiguo A1 - Rivalta, Eleonora A1 - Vuan, Alessandro A1 - Linares, Milton Percy Plasencia A1 - Heimann, Sebastian A1 - Dahm, Torsten T1 - Massive earthquake swarm driven by magmatic intrusion at the Bransfield Strait, Antarctica JF - Communications earth and environment N2 - An earthquake swarm affected the Bransfield Strait, Antarctica, a unique rift basin in transition from intra-arc rifting to ocean spreading. The swarm, counting similar to 85,000 volcano-tectonic earthquakes since August 2020, is located close to the Orca submarine volcano, previously considered inactive. Simultaneously, geodetic data reported up to similar to 11 cm north-westward displacement over King George Island. We use a broad variety of geophysical data and methods to reveal the complex migration of seismicity, accompanying the intrusion of 0.26-0.56 km(3) of magma. Strike-slip earthquakes mark the intrusion at depth, while shallower normal faulting the similar to 20 km long lateral growth of a dike. Seismicity abruptly decreased after a Mw 6.0 earthquake, suggesting the magmatic dike lost pressure with the slipping of a large fault. A seafloor eruption is likely, but not confirmed by sea surface temperature anomalies. The unrest documents episodic magmatic intrusion in the Bransfield Strait, providing unique insights into active continental rifting. Y1 - 2022 U6 - https://doi.org/10.1038/s43247-022-00418-5 SN - 2662-4435 VL - 3 IS - 1 PB - Springer Nature CY - London ER - TY - JOUR A1 - Irrgang, Anna M. A1 - Bendixen, Mette A1 - Farquharson, Louise M. A1 - Baranskaya, Alisa A1 - Erikson, Li H. A1 - Gibbs, Ann E. A1 - Ogorodov, Stanislav A. A1 - Overduin, Pier Paul A1 - Lantuit, Hugues A1 - Grigoriev, Mikhail N. A1 - Jones, Benjamin M. T1 - Drivers, dynamics and impacts of changing Arctic coasts JF - Nature reviews earth and environment N2 - Arctic coasts are vulnerable to the effects of climate change, including rising sea levels and the loss of permafrost, sea ice and glaciers. Assessing the influence of anthropogenic warming on Arctic coastal dynamics, however, is challenged by the limited availability of observational, oceanographic and environmental data. Yet, with the majority of permafrost coasts being erosive, coupled with projected intensification of erosion and flooding, understanding these changes is critical. In this Review, we describe the morphological diversity of Arctic coasts, discuss important drivers of coastal change, explain the specific sensitivity of Arctic coasts to climate change and provide an overview of pan-Arctic shoreline change and its multifaceted impacts. Arctic coastal changes impact the human environment by threatening coastal settlements, infrastructure, cultural sites and archaeological remains. Changing sediment fluxes also impact the natural environment through carbon, nutrient and pollutant release on a magnitude that remains difficult to predict. Increasing transdisciplinary and interdisciplinary collaboration efforts will build the foundation for identifying sustainable solutions and adaptation strategies to reduce future risks for those living on, working at and visiting the rapidly changing Arctic coast. Y1 - 2022 U6 - https://doi.org/10.1038/s43017-021-00232-1 SN - 2662-138X VL - 3 IS - 1 SP - 39 EP - 54 PB - Nature Research CY - London ER - TY - JOUR A1 - Bereswill, Sarah A1 - Gatz-Miller, Hannah A1 - Su, Danyang A1 - Tötzke, Christian A1 - Kardjilov, Nikolay A1 - Oswald, Sascha A1 - Mayer, Klaus Ulrich T1 - Coupling non-invasive imaging and reactive transport modeling to investigate water and oxygen dynamics in the root zone JF - Vadose zone journal N2 - Oxygen (O-2) availability in soils is vital for plant growth and productivity. The transport and consumption of O-2 in the root zone is closely linked to soil moisture content, the spatial distribution of roots, as well as structure and heterogeneity of the surrounding soil. In this study, we measure three-dimensional root system architecture and the spatiotemporal dynamics of soil moisture (& theta;) and O-2 concentrations in the root zone of maize (Zea mays) via non-invasive imaging, and then construct and parameterize a reactive transport model based on the experimental data. The combination of three non-invasive imaging methods allowed for a direct comparison of simulation results with observations at high spatial and temporal resolution. In three different modeling scenarios, we investigated how the results obtained for different levels of conceptual complexity in the model were able to match measured & theta; and O-2 concentration patterns. We found that the modeling scenario that considers heterogeneous soil structure and spatial variability of hydraulic parameters (permeability, porosity, and van Genuchten & alpha; and n), better reproduced the measured & theta; and O-2 patterns relative to a simple model with a homogenous soil domain. The results from our combined imaging and modeling analysis reveal that experimental O-2 and water dynamics can be reproduced quantitatively in a reactive transport model, and that O-2 and water dynamics are best characterized when conditions unique to the specific system beyond the distribution of roots, such as soil structure and its effect on water saturation and macroscopic gas transport pathways, are considered. Y1 - 2023 U6 - https://doi.org/10.1002/vzj2.20268 SN - 1539-1663 VL - 22 IS - 5 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Stoltnow, Malte A1 - Weis, Philipp A1 - Korges, Maximilian T1 - Hydrological controls on base metal precipitation and zoning at the porphyry-epithermal transition constrained by numerical modeling JF - Scientific reports N2 - Ore precipitation in porphyry copper systems is generally characterized by metal zoning (Cu-Mo to Zn-Pb-Ag), which is suggested to be variably related to solubility decreases during fluid cooling, fluid-rock interactions, partitioning during fluid phase separation and mixing with external fluids. Here, we present new advances of a numerical process model by considering published constraints on the temperature- and salinity-dependent solubility of Cu, Pb and Zn in the ore fluid. We quantitatively investigate the roles of vapor-brine separation, halite saturation, initial metal contents, fluid mixing and remobilization as first-order controls of the physical hydrology on ore formation. The results show that the magmatic vapor and brine phases ascend with different residence times but as miscible fluid mixtures, with salinity increases generating metal-undersaturated bulk fluids. The release rates of magmatic fluids affect the location of the thermohaline fronts, leading to contrasting mechanisms for ore precipitation: higher rates result in halite saturation without significant metal zoning, lower rates produce zoned ore shells due to mixing with meteoric water. Varying metal contents can affect the order of the final metal precipitation sequence. Redissolution of precipitated metals results in zoned ore shell patterns in more peripheral locations and also decouples halite saturation from ore precipitation. Y1 - 2023 U6 - https://doi.org/10.1038/s41598-023-30572-5 SN - 2045-2322 VL - 13 IS - 1 PB - Springer Nature CY - London ER - TY - JOUR A1 - Schmidt, Lena Katharina A1 - Francke, Till A1 - Grosse, Peter Martin A1 - Mayer, Christoph A1 - Bronstert, Axel T1 - Reconstructing five decades of sediment export from two glacierized high-alpine catchments in Tyrol, Austria, using nonparametric regression JF - Hydrology and earth system sciences : HESS N2 - Knowledge on the response of sediment export to recent climate change in glacierized areas in the European Alps is limited, primarily because long-term records of suspended sediment concentrations (SSCs) are scarce. Here we tested the estimation of sediment export of the past five decades using quantile regression forest (QRF), a nonparametric, multivariate regression based on random forest. The regression builds on short-term records of SSCs and long records of the most important hydroclimatic drivers (discharge, precipitation and air temperature - QPT). We trained independent models for two nested and partially glacier-covered catchments, Vent (98 km(2)) and Vernagt (11.4 km(2)), in the upper otztal in Tyrol, Austria (1891 to 3772 m a.s.l.), where available QPT records start in 1967 and 1975. To assess temporal extrapolation ability, we used two 2-year SSC datasets at gauge Vernagt, which are almost 20 years apart, for a validation. For Vent, we performed a five-fold cross-validation on the 15 years of SSC measurements. Further, we quantified the number of days where predictors exceeded the range represented in the training dataset, as the inability to extrapolate beyond this range is a known limitation of QRF. Finally, we compared QRF performance to sediment rating curves (SRCs). We analyzed the modeled sediment export time series, the predictors and glacier mass balance data for trends (Mann-Kendall test and Sen's slope estimator) and step-like changes (using the widely applied Pettitt test and a complementary Bayesian approach).Our validation at gauge Vernagt demonstrated that QRF performs well in estimating past daily sediment export (Nash-Sutcliffe efficiency (NSE) of 0.73) and satisfactorily for SSCs (NSE of 0.51), despite the small training dataset. The temporal extrapolation ability of QRF was superior to SRCs, especially in periods with high-SSC events, which demonstrated the ability of QRF to model threshold effects. Days with high SSCs tended to be underestimated, but the effect on annual yields was small. Days with predictor exceedances were rare, indicating a good representativity of the training dataset. Finally, the QRF reconstruction models outperformed SRCs by about 20 percent points of the explained variance.Significant positive trends in the reconstructed annual suspended sediment yields were found at both gauges, with distinct step-like increases around 1981. This was linked to increased glacier melt, which became apparent through step-like increases in discharge at both gauges as well as change points in mass balances of the two largest glaciers in the Vent catchment. We identified exceptionally high July temperatures in 1982 and 1983 as a likely cause. In contrast, we did not find coinciding change points in precipitation. Opposing trends at the two gauges after 1981 suggest different timings of "peak sediment". We conclude that, given large-enough training datasets, the presented QRF approach is a promising tool with the ability to deepen our understanding of the response of high-alpine areas to decadal climate change. Y1 - 2023 U6 - https://doi.org/10.5194/hess-27-1841-2023 SN - 1027-5606 SN - 1607-7938 VL - 27 IS - 9 SP - 1841 EP - 1863 PB - Copernicus CY - Göttingen ER - TY - JOUR A1 - Cabieces, Roberto A1 - Olivar‐Castaño, Andrés A1 - Junqueira, Thiago C. A1 - Relinque, Jesús A1 - Fernandez-Prieto, Luis M. A1 - Vackár, Jiří A1 - Rösler, Boris A1 - Barco, Jaime A1 - Pazos, Antonio A1 - García‐Martínez, Luz T1 - Integrated Seismic Program (ISP): A new Python GUI-based software for earthquake seismology and seismic signal processing JF - Seismological research letters N2 - Integrated Seismic Program (ISP) is a graphical user interface designed to facilitate and provide a user-friendly framework for performing diverse common and advanced tasks in seismological research. ISP is composed of five main modules for earthquake location, time-frequency analysis and advanced signal processing, implementation of array techniques to estimate the slowness vector, seismic moment tensor inversion, and receiver function computation and analysis. In addition, several support tools are available, allowing the user to create an event database, download data from International Federation of Digital Seismograph Networks services, inspect the background noise, and compute synthetic seismograms. ISP is written in Python3, supported by several open-source and/or publicly available tools. Its modular design allows for new features to be added in a collaborative development environment. Y1 - 2022 U6 - https://doi.org/10.1785/0220210205 SN - 0895-0695 SN - 1938-2057 VL - 93 IS - 3 SP - 1895 EP - 1908 PB - Seismological Society of America CY - Albany ER - TY - JOUR A1 - Blanchard, Ingrid A1 - Petitgirard, Sylvain A1 - Laurenz, Vera A1 - Miyajima, Nobuyoshi A1 - Wilke, Max A1 - Rubie, David C. A1 - Lobanov, Sergey S. A1 - Hennet, Louis A1 - Morgenroth, Wolfgang A1 - Tucoulou, Rémi A1 - Bonino, Valentina A1 - Zhao, Xuchao A1 - Franchi, Ian T1 - Chemical analysis of trace elements at the nanoscale in samples recovered from laser-heated diamond anvil cell experiments JF - Physics and chemistry of minerals N2 - High pressure and high temperature experiments performed with laser-heated diamond anvil cells (LH-DAC) are being extensively used in geosciences to study matter at conditions prevailing in planetary interiors. Due to the size of the apparatus itself, the samples that are produced are extremely small, on the order of few tens of micrometers. There are several ways to analyze the samples and extract physical, chemical or structural information, using either in situ or ex situ methods. In this paper, we compare two nanoprobe techniques, namely nano-XRF and NanoSIMS, that can be used to analyze recovered samples synthetized in a LH-DAC. With these techniques, it is possible to extract the spatial distribution of chemical elements in the samples. We show the results for several standards and discuss the importance of proper calibration for the acquisition of quantifiable results. We used these two nanoprobe techniques to retrieve elemental ratios of dilute species (few tens of ppm) in quenched experimental molten samples relevant for the formation of the iron-rich core of the Earth. We finally discuss the applications of such probes to constrain the partitioning of trace elements between metal and silicate phases, with a focus on moderately siderophile elements, tungsten and molybdenum. KW - NanoSIMS KW - Nano-XRF KW - Diamond anvil cell KW - Focused ion beam Y1 - 2022 U6 - https://doi.org/10.1007/s00269-022-01193-7 SN - 0342-1791 SN - 1432-2021 VL - 49 IS - 6 PB - Springer CY - New York ER - TY - JOUR A1 - Weidle, Christian A1 - Wiesenberg, Lars A1 - El-Sharkawy, Amr A1 - Krüger, Frank A1 - Scharf, Andreas A1 - Agard, Philippe A1 - Meier, Thomas T1 - A 3-D crustal shear wave velocity model and Moho map below the Semail Ophiolite, eastern Arabia JF - Geophysical journal international N2 - The Semail Ophiolite in eastern Arabia is the largest and best-exposed slice of oceanic lithosphere on land. Detailed knowledge of the tectonic evolution of the shallow crust, in particular during and after ophiolite obduction in Late Cretaceous times is contrasted by few constraints on physical and compositional properties of the middle and lower continental crust below the obducted units. The role of inherited, pre-obduction crustal architecture remains therefore unaccounted for in our understanding of crustal evolution and the present-day geology. Based on seismological data acquired during a 27-month campaign in northern Oman, Ambient Seismic Noise Tomography and Receiver Function analysis provide for the first time a 3-D radially anisotropic shear wave velocity (V-S) model and a consistent Moho map below the iconic Semail Ophiolite. The model highlights deep crustal boundaries that segment the eastern Arabian basement in two distinct units. The previously undescribed Western Jabal Akhdar Zone separates Arabian crust with typical continental properties and a thickness of similar to 40-45 km in the northwest from a compositionally different terrane in the southeast that is interpreted as a terrane accreted during the Pan-African orogeny in Neoproterozoic times. East of the Ibra Zone, another deep crustal boundary, crustal thickness decreases to 30-35 km and very high lower crustal V-S suggest large-scale mafic intrusions into, and possible underplating of the Arabian continental crust that occurred most likely during Permian breakup of Pangea. Mafic reworking is sharply bounded by the (upper crustal) Semail Gap Fault Zone, northwest of which no such high velocities are found in the crust. Topography of the Oman Mountains is supported by a mild crustal root and Moho depth below the highest topography, the Jabal Akhdar Dome, is similar to 42 km. Radial anisotropy is robustly resolved in the upper crust and aids in discriminating dipping allochthonous units from autochthonous sedimentary rocks that are indistinguishable by isotropic V-S alone. Lateral thickness variations of the ophiolite highlight the Haylayn Ophiolite Massif on the northern flank of Jabal Akhdar Dome and the Hawasina Window as the deepest reaching unit. Ophiolite thickness is similar to 10 km in the southern and northern massifs, and <= 5 km elsewhere. KW - Composition and structure of the continental crust KW - Asia KW - Body waves KW - Seismic anisotropy KW - Seismic tomography KW - Surface waves and free oscillations Y1 - 2022 U6 - https://doi.org/10.1093/gji/ggac223 SN - 0956-540X SN - 1365-246X VL - 231 IS - 2 SP - 817 EP - 834 PB - Oxford University Press CY - Oxford ER -