TY - JOUR A1 - Schulte, Luise A1 - Li, Chenzhi A1 - Lisovski, Simeon A1 - Herzschuh, Ulrike T1 - Forest-permafrost feedbacks and glacial refugia help explain the unequal distribution of larch across continents JF - Journal of biogeography N2 - Aim: The continental-scale distribution of plant functional types, such as evergreen and summergreen needle-leaf forest, is assumed to be determined by contemporary climate. However, the distribution of summergreen needle-leaf forest of larch (Larix Mill.) differs markedly between the continents, despite relatively similar climatic conditions. The reasons for these differences are little understood. Our aim is to identify potential triggers and drivers of the current distribution patterns by comparing species' bioclimatic niches, glacial refugia and postglacial recolonization patterns. Location: Northern hemisphere. Taxon: Species of the genus Larix (Mill.). Methods: We compare species distribution and dominance using species ranges and sites of dominance, as well as their occurrence on modelled permafrost extent, and active layer thickness (ALT). We compare the bioclimatic niches and calculate the niche overlap between species, using the same data in addition to modern climate data. We synthesize pollen, macrofossil and ancient DNA palaeo-evidence of past Larix occurrences of the last 60,000 years and track differences in distribution patterns through time. Results: Bioclimatic niches show large overlaps between Asian larch species and American Larix laricina. The distribution across various degrees of permafrost extent is distinctly different for Asian L. gmelinii and L. cajanderi compared to the other species, whereas the distribution on different depths of ALT is more similar among Asian and American species. Northern glacial refugia for Larix are only present in eastern Asia and Alaska. Main Conclusion: The dominance of summergreen larches in Asia, where evergreen conifers dominate most of the rest of the boreal forests, is dependent on the interaction of several factors which allows Asian L. gmelinii and L. cajanderi to dominate where these factors coincide. These factors include the early postglacial spread out of northern glacial refugia in the absence of competitors as well as a positive feedback mechanism between frozen ground and forest. KW - bioclimatic niche KW - glacial refugia KW - larch KW - Larix KW - permafrost KW - phylogeography KW - postglacial recolonization Y1 - 2022 U6 - https://doi.org/10.1111/jbi.14456 SN - 0305-0270 SN - 1365-2699 VL - 49 IS - 10 SP - 1825 EP - 1838 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Radosavljevic, Boris A1 - Lantuit, Hugues A1 - Knoblauch, Christian A1 - Couture, Nicole A1 - Herzschuh, Ulrike A1 - Fritz, Michael T1 - Arctic nearshore sediment dynamics - an example from Herschel Island - Qikiqtaruk, Canada JF - Journal of marine science and engineering N2 - Increasing arctic coastal erosion rates imply a greater release of sediments and organic matter into the coastal zone. With 213 sediment samples taken around Herschel Island-Qikiqtaruk, Canadian Beaufort Sea, we aimed to gain new insights on sediment dynamics and geochemical properties of a shallow arctic nearshore zone. Spatial characteristics of nearshore sediment texture (moderately to poorly sorted silt) are dictated by hydrodynamic processes, but ice-related processes also play a role. We determined organic matter (OM) distribution and inferred the origin and quality of organic carbon by C/N ratios and stable carbon isotopes delta C-13. The carbon content was higher offshore and in sheltered areas (mean: 1.0 wt.%., S.D.: 0.9) and the C/N ratios also showed a similar spatial pattern (mean: 11.1, S.D.: 3.1), while the delta C-13 (mean: -26.4 parts per thousand VPDB, S.D.: 0.4) distribution was more complex. We compared the geochemical parameters of our study with terrestrial and marine samples from other studies using a bootstrap approach. Sediments of the current study contained 6.5 times and 1.8 times less total organic carbon than undisturbed and disturbed terrestrial sediments, respectively. Therefore, degradation of OM and separation of carbon pools take place on land and continue in the nearshore zone, where OM is leached, mineralized, or transported beyond the study area. KW - permafrost KW - Arctic Ocean KW - stable carbon isotopes KW - nitrogen KW - sediment KW - chemistry KW - sediment dynamics KW - Beaufort Sea KW - grain size Y1 - 2022 U6 - https://doi.org/10.3390/jmse10111589 SN - 2077-1312 VL - 10 IS - 11 PB - MDPI CY - Basel ER - TY - JOUR A1 - Stuenzi, Simone Maria A1 - Kruse, Stefan A1 - Boike, Julia A1 - Herzschuh, Ulrike A1 - Oehme, Alexander A1 - Pestryakova, Luidmila A. A1 - Westermann, Sebastian A1 - Langer, Moritz T1 - Thermohydrological impact of forest disturbances on ecosystem-protected permafrost JF - Journal of geophysical research : Biogeosciences N2 - Boreal forests cover over half of the global permafrost area and protect underlying permafrost. Boreal forest development, therefore, has an impact on permafrost evolution, especially under a warming climate. Forest disturbances and changing climate conditions cause vegetation shifts and potentially destabilize the carbon stored within the vegetation and permafrost. Disturbed permafrost-forest ecosystems can develop into a dry or swampy bush- or grasslands, shift toward broadleaf- or evergreen needleleaf-dominated forests, or recover to the pre-disturbance state. An increase in the number and intensity of fires, as well as intensified logging activities, could lead to a partial or complete ecosystem and permafrost degradation. We study the impact of forest disturbances (logging, surface, and canopy fires) on the thermal and hydrological permafrost conditions and ecosystem resilience. We use a dynamic multilayer canopy-permafrost model to simulate different scenarios at a study site in eastern Siberia. We implement expected mortality, defoliation, and ground surface changes and analyze the interplay between forest recovery and permafrost. We find that forest loss induces soil drying of up to 44%, leading to lower active layer thicknesses and abrupt or steady decline of a larch forest, depending on disturbance intensity. Only after surface fires, the most common disturbances, inducing low mortality rates, forests can recover and overpass pre-disturbance leaf area index values. We find that the trajectory of larch forests after surface fires is dependent on the precipitation conditions in the years after the disturbance. Dryer years can drastically change the direction of the larch forest development within the studied period. KW - permafrost KW - boreal forest KW - periglacial process KW - Siberia KW - larch forest KW - disturbance Y1 - 2022 U6 - https://doi.org/10.1029/2021JG006630 SN - 2169-8953 SN - 2169-8961 VL - 127 IS - 5 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Heslop, J. K. A1 - Winkel, Matthias A1 - Anthony, K. M. Walter A1 - Spencer, R. G. M. A1 - Podgorski, D. C. A1 - Zito, P. A1 - Kholodov, A. A1 - Zhang, M. A1 - Liebner, Susanne T1 - Increasing organic carbon biolability with depth in yedoma permafrost BT - ramifications for future climate change JF - Journal of geophysical research : Biogeosciences N2 - Permafrost thaw subjects previously frozen organic carbon (OC) to microbial decomposition, generating the greenhouse gases (GHG) carbon dioxide (CO2) and methane (CH4) and fueling a positive climate feedback. Over one quarter of permafrost OC is stored in deep, ice-rich Pleistocene-aged yedoma permafrost deposits. We used a combination of anaerobic incubations, microbial sequencing, and ultrahigh-resolution mass spectrometry to show yedoma OC biolability increases with depth along a 12-m yedoma profile. In incubations at 3 degrees C and 13 degrees C, GHG production per unit OC at 12-versus 1.3-m depth was 4.6 and 20.5 times greater, respectively. Bacterial diversity decreased with depth and we detected methanogens at all our sampled depths, suggesting that in situ microbial communities are equipped to metabolize thawed OC into CH4. We concurrently observed an increase in the relative abundance of reduced, saturated OC compounds, which corresponded to high proportions of C mineralization and positively correlated with anaerobic GHG production potentials and higher proportions of OC being mineralized as CH4. Taking into account the higher global warming potential (GWP) of CH4 compared to CO2, thawed yedoma sediments in our study had 2 times higher GWP at 12-versus 9.0-m depth at 3 degrees C and 15 times higher GWP at 13 degrees C. Considering that yedoma is vulnerable to processes that thaw deep OC, our findings imply that it is important to account for this increasing GHG production and GWP with depth to better understand the disproportionate impact of yedoma on the magnitude of the permafrost carbon feedback. KW - permafrost KW - carbon KW - yedoma KW - Alaska KW - FT-ICR MS KW - microbes Y1 - 2019 U6 - https://doi.org/10.1029/2018JG004712 SN - 2169-8953 SN - 2169-8961 VL - 124 IS - 7 SP - 2021 EP - 2038 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Tanski, George A1 - Couture, Nicole A1 - Lantuit, Hugues A1 - Eulenburg, Antje A1 - Fritz, Michael T1 - Eroding permafrost coasts release low amounts of dissolved organic carbon (DOC) from ground ice into the nearshore zone of the Arctic Ocean JF - Global biogeochemical cycles N2 - Ice-rich permafrost coasts in the Arctic are highly sensitive to climate warming and erode at a pace that exceeds the global average. Permafrost coasts deliver vast amounts of organic carbon into the nearshore zone of the Arctic Ocean. Numbers on flux exist for particulate organic carbon (POC) and total or soil organic carbon (TOC, SOC). However, they do not exist for dissolved organic carbon (DOC), which is known to be highly bioavailable. This study aims to estimate DOC stocks in coastal permafrost as well as the annual flux into the ocean. DOC concentrations in ground ice were analyzed along the ice-rich Yukon coast (YC) in the western Canadian Arctic. The annual DOC flux was estimated using available numbers for coast length, cliff height, annual erosion rate, and volumetric ice content in different stratigraphic horizons. Our results showed that DOC concentrations in ground ice range between 0.3 and 347.0mgL(-1) with an estimated stock of 13.63.0gm(-3) along the YC. An annual DOC flux of 54.90.9Mgyr(-1) was computed. These DOC fluxes are low compared to POC and SOC fluxes from coastal erosion or POC and DOC fluxes from Arctic rivers. We conclude that DOC fluxes from permafrost coasts play a secondary role in the Arctic carbon budget. However, this DOC is assumed to be highly bioavailable. We hypothesize that DOC from coastal erosion is important for ecosystems in the Arctic nearshore zones, particularly in summer when river discharge is low, and in areas where rivers are absent. KW - Arctic KW - permafrost KW - coastal erosion KW - biogeochemistry KW - carbon cycle Y1 - 2016 U6 - https://doi.org/10.1002/2015GB005337 SN - 0886-6236 SN - 1944-9224 VL - 30 SP - 1054 EP - 1068 PB - American Geophysical Union CY - Cambridge ER - TY - THES A1 - Feige, Katharina T1 - Molecular ecological analysis of methanogenic communities in terrestrial and submarine permafrost deposits of Siberian Laptev Sea area T1 - Molekular-ökologische Analyse von methanogenen Gemeinschaften im terrestrischen und submarinen Permafrost im Laptevseegebiet N2 - Despite general concern that the massive deposits of methane stored under permafrost underground and undersea could be released into the atmosphere due to rising temperatures attributed to global climate change, little is known about the methanogenic microorganisms in permafrost sediments, their role in methane emissions, and their phylogeny. The aim of this thesis was to increase knowledge of uncultivated methanogenic microorganisms in submarine and terrestrial permafrost deposits, their community composition, the role they play with regard to methane emissions, and their phylogeny. It is assumed that methanogenic communities in warmer submarine permafrost may serve as a model to anticipate the response of methanogenic communities in colder terrestrial permafrost to rising temperatures. The compositions of methanogenic communities were examined in terrestrial and submarine permafrost sediment samples. The submarine permafrost studied in this research was 10°C warmer than the terrestrial permafrost. By polymerase chain reaction (PCR), DNA was extracted from each of the samples and analyzed by molecular microbiological methods such as PCR-DGGE, RT-PCR, and cloning. Furthermore, these samples were used for in vitro experiment and FISH. The submarine permafrost analysis of the isotope composition of CH4 suggested a relationship between methane content and in situ active methanogenesis. Furthermore, active methanogenesis was proven using 13C-isotope measurements of methane in submarine permafrost sediment with a high TOC value and a high methane concentration. In the molecular-microbiological studies uncultivated lines of Methanosarcina, Methanomicrobiales, Methanobacteriacea and the Groups 1.3 and Marine Benthic from Crenarchaeota were found in all submarine and terrestrial permafrost samples. Methanosarcina was the dominant group of the Archaea in all submarine and terrestrial permafrost samples. The archaeal community composition, in particular, the methanogenic community composition showed diversity with changes in temperatures. Furthermore, cell count of methanogens in submarine permafrost was 10 times higher than in terrestrial permafrost. In vitro experiments showed that methanogens adapt quickly and well to higher temperatures. If temperatures rise due to climate change, an increase in methanogenic activity can be expected as long as organic material is sufficiently available and qualitatively adequate. N2 - Trotz allgemeiner Bedenken, dass auf Grund des Temperaturanstieges im Zusammenhang mit der globalen Klimaerwärmung große Mengen des in terrestrischen und submarinen Permafrostsedimenten gespeicherten Methans freigesetzt werden könnte, ist bisher wenig über die in diesen Böden lebenden methanogenen Mikroorganismen, ihre Phylogenese und sowie ihre Bedeutung hinsichtlich der Methanemissionen bekannt. Das Ziel dieser Doktorarbeit war die Erweiterung der bisherigen Kenntnisse über unkultivierte methanogene Mikroorganismen in submarinen und terrestrischen Sedimentablagerungen, die Zusammensetzung ihrer Lebensgemeinschaft, ihrer Phylogenese und ihrer Bedeutung bei der Emission von Methan. Es wird vermutet, dass methanogene Gemeinschaften submarines Permafrostes zur Erstellung von Modellen genutzt werden können, um Aussagen bezüglich potenzieller Reaktionen methanogener Gemeinschaften des kälteren terrestrischen Permafrostes auf steigende Temperaturen, zu ermöglichen. Die Zusammensetzung der methanogenen Gemeinschaft wurde in terrestrischen und submarinen Permafrostproben untersucht. Der im Rahmen dieser Forschungsarbeit untersuchte submarine Permafrost wies eine im Vergleich zum terrestrischen Permafrost um circa 10°C höhere Temperatur auf. Mittels Polymerasenkettenreaktion (PCR) wurde von jeder der Proben DNA extrahiert und mittels weiterer molekular-mikrobiologischen Methoden wie DGGE, RT-PCR und Klonierung analysiert. Des Weiteren wurden die Proben für in vitro Experimente und Zellzählungen (DAPI und FISH) verwendet. Die Analyse der Isotopenzusammensetzung von CH4 in submarinen Permafrostsedimenten ließ einen Zusammenhang zwischen Methangehalt und aktiver in situ Methanogenese vermuten. Überdies konnte aktive Methanogenese, mittels 13C-Isotopenmessungen von Methan in submarinem Permafrostsediment mit hohem TOC-Wert und hoher Methankonzentration, bewiesen werden. Im Rahmen der molekular-mikrobiologischen Untersuchungen wurden in allen submarinen und terrestrischen Permafrostproben unkultivierte Linien von Methanosarcina, Methanomicrobiales, Methanobacteriacea und den Gruppen 1.3 und Marine Benthic von Crenarchaeota gefunden. Methanosarcina war in allen submarinen und terrestrischen Permafrostproben die dominierende Gruppe der Archaeen. Die Zusammensetzung der archaealen Gemeinschaft, insbesondere die Zusammensetzung der methanogenen Gemeinschaft, variierte zwischen den submarinen und terrestrischen Proben. Des Weiteren fand sich bei der Zellzählung der Methanogenen im submarinen Permafrost eine 10-fach höhere Zellzahl als im terrestrischen Permafrost. Die in vitro Experimente zeigten, dass Methanogene sich schnell und gut an höhere Temperaturen anpassen können. Im Falle weiter steigender Temperaturen auf Grund der Klimaveränderungen, kann – bei ausreichender Verfügbarkeit und Qualität organischen Materials – mit einer Zunahme der methanogenen Aktivität gerechnet werden. KW - methanogene Archaea KW - Permafrost KW - submarin KW - terrestrisch KW - methanogenic archaea KW - permafrost KW - submarine KW - terrestrial Y1 - 2009 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-37998 ER -