TY  - JOUR
A1  - De Angelis, A.
A1  - Tatischeff, V.
A1  - Grenier, I. A.
A1  - McEnery, J.
A1  - Mallamaci, Manuela
A1  - Tavani, M.
A1  - Oberlack, U.
A1  - Hanlon, L.
A1  - Walter, R.
A1  - Argan, A.
A1  - Von Ballmoos, P.
A1  - Bulgarelli, A.
A1  - Bykov, A.
A1  - Hernanz, M.
A1  - Kanbach, G.
A1  - Kuvvetli, I.
A1  - Pearce, M.
A1  - Zdziarski, A.
A1  - Conrad, J.
A1  - Ghisellini, G.
A1  - Harding, A.
A1  - Isern, J.
A1  - Leising, M.
A1  - Longo, F.
A1  - Madejski, G.
A1  - Martinez, M.
A1  - Mazziotta, Mario Nicola
A1  - Paredes, J. M.
A1  - Pohl, Martin
A1  - Rando, R.
A1  - Razzano, M.
A1  - Aboudan, A.
A1  - Ackermann, M.
A1  - Addazi, A.
A1  - Ajello, M.
A1  - Albertus, C.
A1  - Alvarez, J. M.
A1  - Ambrosi, G.
A1  - Anton, S.
A1  - Antonelli, L. A.
A1  - Babic, A.
A1  - Baibussinov, B.
A1  - Balbom, M.
A1  - Baldini, L.
A1  - Balman, S.
A1  - Bambi, C.
A1  - Barres de Almeida, U.
A1  - Barrio, J. A.
A1  - Bartels, R.
A1  - Bastieri, D.
A1  - Bednarek, W.
A1  - Bernard, D.
A1  - Bernardini, E.
A1  - Bernasconi, T.
A1  - Bertucci, B.
A1  - Biland, A.
A1  - Bissaldi, E.
A1  - Boettcher, M.
A1  - Bonvicini, V.
A1  - Bosch-Ramon, V.
A1  - Bottacini, E.
A1  - Bozhilov, V.
A1  - Bretz, T.
A1  - Branchesi, M.
A1  - Brdar, V.
A1  - Bringmann, T.
A1  - Brogna, A.
A1  - Jorgensen, C. Budtz
A1  - Busetto, G.
A1  - Buson, S.
A1  - Busso, M.
A1  - Caccianiga, A.
A1  - Camera, S.
A1  - Campana, R.
A1  - Caraveo, P.
A1  - Cardillo, M.
A1  - Carlson, P.
A1  - Celestin, S.
A1  - Cermeno, M.
A1  - Chen, A.
A1  - Cheung, C. C.
A1  - Churazov, E.
A1  - Ciprini, S.
A1  - Coc, A.
A1  - Colafrancesco, S.
A1  - Coleiro, A.
A1  - Collmar, W.
A1  - Coppi, P.
A1  - Curado da Silva, R.
A1  - Cutini, S.
A1  - De Lotto, B.
A1  - de Martino, D.
A1  - De Rosa, A.
A1  - Del Santo, M.
A1  - Delgado, L.
A1  - Diehl, R.
A1  - Dietrich, S.
A1  - Dolgov, A. D.
A1  - Dominguez, A.
A1  - Prester, D. Dominis
A1  - Donnarumma, I.
A1  - Dorner, D.
A1  - Doro, M.
A1  - Dutra, M.
A1  - Elsaesser, D.
A1  - Fabrizio, M.
A1  - Fernandez-Barral, A.
A1  - Fioretti, V.
A1  - Foffano, L.
A1  - Formato, V.
A1  - Fornengo, N.
A1  - Foschini, L.
A1  - Franceschini, A.
A1  - Franckowiak, A.
A1  - Funk, S.
A1  - Fuschino, F.
A1  - Gaggero, D.
A1  - Galanti, G.
A1  - Gargano, F.
A1  - Gasparrini, D.
A1  - Gehrz, R.
A1  - Giammaria, P.
A1  - Giglietto, N.
A1  - Giommi, P.
A1  - Giordano, F.
A1  - Giroletti, M.
A1  - Ghirlanda, G.
A1  - Godinovic, N.
A1  - Gouiffes, C.
A1  - Grove, J. E.
A1  - Hamadache, C.
A1  - Hartmann, D. H.
A1  - Hayashida, M.
A1  - Hryczuk, A.
A1  - Jean, P.
A1  - Johnson, T.
A1  - Jose, J.
A1  - Kaufmann, S.
A1  - Khelifi, B.
A1  - Kiener, J.
A1  - Knodlseder, J.
A1  - Kolem, M.
A1  - Kopp, J.
A1  - Kozhuharov, V.
A1  - Labanti, C.
A1  - Lalkovski, S.
A1  - Laurent, P.
A1  - Limousin, O.
A1  - Linares, M.
A1  - Lindfors, E.
A1  - Lindner, M.
A1  - Liu, J.
A1  - Lombardi, S.
A1  - Loparco, F.
A1  - Lopez-Coto, R.
A1  - Lopez Moya, M.
A1  - Lott, B.
A1  - Lubrano, P.
A1  - Malyshev, D.
A1  - Mankuzhiyil, N.
A1  - Mannheim, K.
A1  - Marcha, M. J.
A1  - Marciano, A.
A1  - Marcote, B.
A1  - Mariotti, M.
A1  - Marisaldi, M.
A1  - McBreen, S.
A1  - Mereghetti, S.
A1  - Merle, A.
A1  - Mignani, R.
A1  - Minervini, G.
A1  - Moiseev, A.
A1  - Morselli, A.
A1  - Moura, F.
A1  - Nakazawa, K.
A1  - Nava, L.
A1  - Nieto, D.
A1  - Orienti, M.
A1  - Orio, M.
A1  - Orlando, E.
A1  - Orleanski, P.
A1  - Paiano, S.
A1  - Paoletti, R.
A1  - Papitto, A.
A1  - Pasquato, M.
A1  - Patricelli, B.
A1  - Perez-Garcia, M. A.
A1  - Persic, M.
A1  - Piano, G.
A1  - Pichel, A.
A1  - Pimenta, M.
A1  - Pittori, C.
A1  - Porter, T.
A1  - Poutanen, J.
A1  - Prandini, E.
A1  - Prantzos, N.
A1  - Produit, N.
A1  - Profumo, S.
A1  - Queiroz, F. S.
A1  - Raino, S.
A1  - Raklev, A.
A1  - Regis, M.
A1  - Reichardt, I.
A1  - Rephaeli, Y.
A1  - Rico, J.
A1  - Rodejohann, W.
A1  - Fernandez, G. Rodriguez
A1  - Roncadelli, M.
A1  - Roso, L.
A1  - Rovero, A.
A1  - Ruffini, R.
A1  - Sala, G.
A1  - Sanchez-Conde, M. A.
A1  - Santangelo, Andrea
A1  - Parkinson, P. Saz
A1  - Sbarrato, T.
A1  - Shearer, A.
A1  - Shellard, R.
A1  - Short, K.
A1  - Siegert, T.
A1  - Siqueira, C.
A1  - Spinelli, P.
A1  - Stamerra, A.
A1  - Starrfield, S.
A1  - Strong, A.
A1  - Strumke, I.
A1  - Tavecchio, F.
A1  - Taverna, R.
A1  - Terzic, T.
A1  - Thompson, D. J.
A1  - Tibolla, O.
A1  - Torres, D. F.
A1  - Turolla, R.
A1  - Ulyanov, A.
A1  - Ursi, A.
A1  - Vacchi, A.
A1  - Van den Abeele, J.
A1  - Vankova-Kirilovai, G.
A1  - Venter, C.
A1  - Verrecchia, F.
A1  - Vincent, P.
A1  - Wang, X.
A1  - Weniger, C.
A1  - Wu, X.
A1  - Zaharijas, G.
A1  - Zampieri, L.
A1  - Zane, S.
A1  - Zimmer, S.
A1  - Zoglauer, A.
T1  - Science with e-ASTROGAM A space mission for MeV-GeV gamma-ray astrophysics
JF  - Journal of High Energy Astrophysics
Y1  - 2018
U6  - https://doi.org/10.1016/j.jheap.2018.07.001
SN  - 2214-4048
SN  - 2214-4056
VL  - 19
SP  - 1
EP  - 106
PB  - Elsevier
CY  - Amsterdam
ER  - 
TY  - JOUR
A1  - Pesicek, J. D.
A1  - Engdahl, E. R.
A1  - Thurber, C. H.
A1  - DeShon, H. R.
A1  - Lange, Dietrich
T1  - Mantle subducting slab structure in the region of the 2010 M8.8 Maule earthquake (30-40 degrees S), Chile
JF  - Geophysical journal international
N2  - We present a new tomographic model of the mantle in the area of the 2010 M8.8 Maule earthquake and surrounding regions. Increased ray coverage provided by the aftershock data allows us to image the detailed subducting slab structure in the mantle, from the region of flat slab subduction north of the Maule rupture to the area of overlapping rupture between the 1960 M9.5 and the 2010 M8.8 events to the south. We have combined teleseismic primary and depth phase arrivals with available local arrivals to better constrain the teleseismic earthquake locations in the region, which we use to conduct nested regionalglobal tomography. The new model reveals the detailed structure of the flat slab and its transition to a more moderately dipping slab in the Maule region. South of the Maule region, a steeply dipping relic slab is imaged from similar to 200 to 1000 km depth that is distinct from the moderately dipping slab above it and from the more northerly slab at similar depths. We interpret the images as revealing both horizontal and vertical tearing of the slab at similar to 38 degrees S to explain the imaged pattern of slab anomalies in the southern portion of the model. In contrast, the transition from a horizontal to moderately subducting slab in the northern portion of the model is imaged as a continuous slab bend. We speculate that the tearing was most likely facilitated by a fracture zone in the downgoing plate or alternatively by a continental scale terrane boundary in the overriding plate.
KW  - Seismicity and tectonics
KW  - Seismic tomography
KW  - Subduction zone processes
Y1  - 2012
U6  - https://doi.org/10.1111/j.1365-246X.2012.05624.x
SN  - 0956-540X
VL  - 191
IS  - 1
SP  - 317
EP  - 324
PB  - Wiley-Blackwell
CY  - Hoboken
ER  - 
TY  - JOUR
A1  - Becker, Dirk
A1  - Geiger, D.
A1  - Dunkel, M.
A1  - Roller, A.
A1  - Bertl, Adam
A1  - Latz, A.
A1  - Carpaneto, Armando
A1  - Dietrich, Peter
A1  - Roelfsema, M. R. G.
A1  - Voelker, C.
A1  - Schmidt, D.
A1  - Müller-Röber, Bernd
A1  - Czempinski, Katrin
A1  - Hedrich, R.
T1  - AtTPK4, an Arabidopsis tandem-pore K+ channel, poised to control the pollen membrane voltage in a pH- and Ca2+- dependent manner
N2  - The Arabidopsis tandem-pore K+ (TPK) channels displaying four transmembrane domains and two pore regions share structural homologies with their animal counterparts of the KCNK family. In contrast to the Shaker-like Arabidopsis channels (six transmembrane domains/one pore region), the functional properties and the biological role of plant TPK channels have not been elucidated yet. Here, we show that AtTPK4 (KCO4) localizes to the plasma membrane and is predominantly expressed in pollen. AtTPK4 (KCO4) resembles the electrical properties of a voltage-independent K+ channel after expression in Xenopus oocytes and yeast. Hyperpolarizing as well as depolarizing membrane voltages elicited instantaneous K+ currents, which were blocked by extracellular calcium and cytoplasmic protons. Functional complementation assays using a K+ transport-deficient yeast confirmed the biophysical and pharmacological properties of the AtTPK4 channel. The features of AtTPK4 point toward a role in potassium homeostasis and membrane voltage control of the growing pollen tube. Thus, AtTPK4 represents a member of plant tandem-pore-K+ channels, resembling the characteristics of its animal counterparts as well as plant-specific features with respect to modulation of channel activity by acidosis and calcium
Y1  - 2004
SN  - 0027-8424
ER  - 
TY  - JOUR
A1  - Schenck, Marcia C.
A1  - Harisch, Immanuel R.
A1  - Dietrich, Anne
A1  - Burton, Eric
T1  - Introduction
BT  - Moorings and (Dis)Entanglements between Africa and East Germany during the Cold War
JF  - Navigating Socialist Encounters
Y1  - 2021
SN  - 978-3-11-062354-3
SN  - 978-3-11-062231-7
U6  - https://doi.org/10.1515/9783110623543-001
SP  - 1
EP  - 58
PB  - de Gruyter
CY  - Oldenburg
ER  - 
TY  - JOUR
A1  - Hetenyi, Gyorgy
A1  - Molinari, Irene
A1  - Clinton, John
A1  - Bokelmann, Gotz
A1  - Bondar, Istvan
A1  - Crawford, Wayne C.
A1  - Dessa, Jean-Xavier
A1  - Doubre, Cecile
A1  - Friederich, Wolfgang
A1  - Fuchs, Florian
A1  - Giardini, Domenico
A1  - Graczer, Zoltan
A1  - Handy, Mark R.
A1  - Herak, Marijan
A1  - Jia, Yan
A1  - Kissling, Edi
A1  - Kopp, Heidrun
A1  - Korn, Michael
A1  - Margheriti, Lucia
A1  - Meier, Thomas
A1  - Mucciarelli, Marco
A1  - Paul, Anne
A1  - Pesaresi, Damiano
A1  - Piromallo, Claudia
A1  - Plenefisch, Thomas
A1  - Plomerova, Jaroslava
A1  - Ritter, Joachim
A1  - Rumpker, Georg
A1  - Sipka, Vesna
A1  - Spallarossa, Daniele
A1  - Thomas, Christine
A1  - Tilmann, Frederik
A1  - Wassermann, Joachim
A1  - Weber, Michael
A1  - Weber, Zoltan
A1  - Wesztergom, Viktor
A1  - Zivcic, Mladen
A1  - Abreu, Rafael
A1  - Allegretti, Ivo
A1  - Apoloner, Maria-Theresia
A1  - Aubert, Coralie
A1  - Besancon, Simon
A1  - de Berc, Maxime Bes
A1  - Brunel, Didier
A1  - Capello, Marco
A1  - Carman, Martina
A1  - Cavaliere, Adriano
A1  - Cheze, Jerome
A1  - Chiarabba, Claudio
A1  - Cougoulat, Glenn
A1  - Cristiano, Luigia
A1  - Czifra, Tibor
A1  - Danesi, Stefania
A1  - Daniel, Romuald
A1  - Dannowski, Anke
A1  - Dasovic, Iva
A1  - Deschamps, Anne
A1  - Egdorf, Sven
A1  - Fiket, Tomislav
A1  - Fischer, Kasper
A1  - Funke, Sigward
A1  - Govoni, Aladino
A1  - Groschl, Gidera
A1  - Heimers, Stefan
A1  - Heit, Ben
A1  - Herak, Davorka
A1  - Huber, Johann
A1  - Jaric, Dejan
A1  - Jedlicka, Petr
A1  - Jund, Helene
A1  - Klingen, Stefan
A1  - Klotz, Bernhard
A1  - Kolinsky, Petr
A1  - Kotek, Josef
A1  - Kuhne, Lothar
A1  - Kuk, Kreso
A1  - Lange, Dietrich
A1  - Loos, Jurgen
A1  - Lovati, Sara
A1  - Malengros, Deny
A1  - Maron, Christophe
A1  - Martin, Xavier
A1  - Massa, Marco
A1  - Mazzarini, Francesco
A1  - Metral, Laurent
A1  - Moretti, Milena
A1  - Munzarova, Helena
A1  - Nardi, Anna
A1  - Pahor, Jurij
A1  - Pequegnat, Catherine
A1  - Petersen, Florian
A1  - Piccinini, Davide
A1  - Pondrelli, Silvia
A1  - Prevolnik, Snjezan
A1  - Racine, Roman
A1  - Regnier, Marc
A1  - Reiss, Miriam
A1  - Salimbeni, Simone
A1  - Santulin, Marco
A1  - Scherer, Werner
A1  - Schippkus, Sven
A1  - Schulte-Kortnack, Detlef
A1  - Solarino, Stefano
A1  - Spieker, Kathrin
A1  - Stipcevic, Josip
A1  - Strollo, Angelo
A1  - Sule, Balint
A1  - Szanyi, Gyongyver
A1  - Szucs, Eszter
A1  - Thorwart, Martin
A1  - Ueding, Stefan
A1  - Vallocchia, Massimiliano
A1  - Vecsey, Ludek
A1  - Voigt, Rene
A1  - Weidle, Christian
A1  - Weyland, Gauthier
A1  - Wiemer, Stefan
A1  - Wolf, Felix
A1  - Wolyniec, David
A1  - Zieke, Thomas
T1  - The AlpArray seismic network
BT  - a large-scale european experiment to image the alpine orogen
JF  - Surveys in Geophysics
N2  - The AlpArray programme is a multinational, European consortium to advance our understanding of orogenesis and its relationship to mantle dynamics, plate reorganizations, surface processes and seismic hazard in the Alps-Apennines-Carpathians-Dinarides orogenic system. The AlpArray Seismic Network has been deployed with contributions from 36 institutions from 11 countries to map physical properties of the lithosphere and asthenosphere in 3D and thus to obtain new, high-resolution geophysical images of structures from the surface down to the base of the mantle transition zone. With over 600 broadband stations operated for 2 years, this seismic experiment is one of the largest simultaneously operated seismological networks in the academic domain, employing hexagonal coverage with station spacing at less than 52 km. This dense and regularly spaced experiment is made possible by the coordinated coeval deployment of temporary stations from numerous national pools, including ocean-bottom seismometers, which were funded by different national agencies. They combine with permanent networks, which also required the cooperation of many different operators. Together these stations ultimately fill coverage gaps. Following a short overview of previous large-scale seismological experiments in the Alpine region, we here present the goals, construction, deployment, characteristics and data management of the AlpArray Seismic Network, which will provide data that is expected to be unprecedented in quality to image the complex Alpine mountains at depth.
KW  - Seismology
KW  - Alps
KW  - Seismic network
KW  - Geodynamics
KW  - Seismic imaging
KW  - Mountain building
Y1  - 2018
U6  - https://doi.org/10.1007/s10712-018-9472-4
SN  - 0169-3298
SN  - 1573-0956
VL  - 39
IS  - 5
SP  - 1009
EP  - 1033
PB  - Springer
CY  - Dordrecht
ER  - 
TY  - JOUR
A1  - Jain, Varun
A1  - Wheeler, Joshua J.
A1  - Ess, Daniel H.
A1  - Noack, Sebastian
A1  - Vacogne, Charlotte D.
A1  - Schlaad, Helmut
A1  - Bahr, Stephan
A1  - Dietrich, Paul
A1  - Meyer, Michael
A1  - Thissen, Andreas
A1  - Linford, Matthew R.
T1  - Poly(gamma-benzyl l-glutamate), by near-ambient pressure XPS
JF  - Surface science spectra : SSS : an international journal & database devoted to archiving spectra from surfaces & interfaces
N2  - Near-ambient pressure x-ray photoelectron spectroscopy (NAP-XPS) is a less traditional form of XPS that allows samples to be analyzed at relatively high pressures, i. e., at greater than 2500 Pa. In this study, poly(.- benzyl L- glutamate) (PBLG) with a molar mass of 11.3 kg/mol was analyzed by NAP-XPS; here, we show the survey, C 1s, N 1s, and O 1s narrow scans of PBLG. The C 1s peak envelope was fitted in three different ways, to five, six, or seven synthetic peaks. In each fit, there was also a shake-up signal. The O 1s narrow scan was well fit with three peaks: CZO and CvO in a 1:2 ratio from the polymer, and a higher energy signal from water vapor. Hartree-Fock orbital energies of a model monomer served as a guide to an additional fit of the C 1s envelope.
KW  - near-ambient pressure x-ray photoelectron spectroscopy
KW  - NAP-XPS
KW  - XPS
KW  - polymer
KW  - poly(gamma-benzyl L-glutamate)
KW  - PBLG
Y1  - 2019
U6  - https://doi.org/10.1116/1.5109121
SN  - 1055-5269
SN  - 1520-8575
VL  - 26
IS  - 2
PB  - American Institute of Physics
CY  - Melville
ER  - 
TY  - JOUR
A1  - Patel, Dhananjay I.
A1  - Noack, Sebastian
A1  - Vacogne, Charlotte D.
A1  - Schlaad, Helmut
A1  - Bahr, Stephan
A1  - Dietrich, Paul
A1  - Meyer, Michael
A1  - Thissen, Andreas
A1  - Linford, Matthew R.
T1  - Poly(L-lactic acid), by near-ambient pressure XPS
JF  - Surface Science Spectra
N2  - Near ambient pressure - x-ray photoelectron spectroscopy (NAP-XPS) is a less traditional form of XPS that allows samples to be analyzed at relatively high pressures, i.e., at 2500Pa or higher. With NAP-XPS, one can analyze moderately volatile liquids, biological samples, porous materials, and/or polymeric materials that outgas significantly. In this submission we show C 1s, O 1s, and survey NAP-XPS spectra from poly(L-lactic acid). The C 1s and O 1s envelopes were fit with three and two Gaussian-Lorentzian sum functions, respectively. Water vapor (800Pa) was used as the residual gas for charge compensation, which was confirmed by the sharp peak at 535.0 eV in the O 1s narrow scan. The uniqueness plot corresponding to the C 1s fit shows that the fit parameters had statistical significance. C 1s and O 1s spectra of PLLA damaged by exposure to x-rays for ca. 1 hour are also included. Published by the AVS.
KW  - near-ambient pressure X-ray photoelectron spectroscopy
KW  - NAP-XPS
KW  - XPS
KW  - Water Vapor
Y1  - 2019
U6  - https://doi.org/10.1116/1.5110309
SN  - 1055-5269
SN  - 1520-8575
VL  - 26
IS  - 2
PB  - American Institute of Physics
CY  - Melville
ER  - 
TY  - JOUR
A1  - Collings, R.
A1  - Rietbrock, Andreas
A1  - Lange, Dietrich
A1  - Tilmann, F.
A1  - Nippress, Stuart
A1  - Natawidjaja, D.
T1  - Seismic anisotropy in the sumatra subduction zone
JF  - Journal of geophysical research : Solid earth
N2  - An important tool for understanding deformation occurring within a subduction zone is the measurement of seismic anisotropy through observations of shear wave splitting (SWS). In Sumatra, two temporary seismic networks were deployed between December 2007 and February 2009, covering the fore arc between the fore-arc islands to the back arc. We use SKS and local SWS measurements to determine the type, amount, and location of anisotropy. Local SWS measurements from the fore-arc islands exhibit trench-parallel fast directions which can be attributed to shape preferred orientation of cracks/fractures in the overriding sediments. In the Sumatran Fault region, the predominant fast direction is fault/trench parallel, while in the back-arc region it is trench perpendicular. The trench-perpendicular measurements exhibit a positive correlation between delay time and raypath length in the mantle wedge, while the fault-parallel measurements are similar to the fault-parallel fast directions observed for two crustal events at the Sumatran Fault. This suggests that there are two layers of anisotropy: one due to entrained flow within the mantle wedge and a second layer within the overriding crust due to the shear strain caused by the Sumatran Fault. SKS splitting results show a NNW-SSE fast direction with delay times of 0.8-3.0s. The fast directions are approximately parallel to the absolute plate motion of the subducting Indo-Australian Plate. The small delay times exhibited by the local SWS (0.05-0.45s), in combination with the large SKS delay times, suggest that the anisotropy generating the teleseismic SWS is dominated by entrained flow in the asthenosphere below the slab.
KW  - Sumatra
KW  - Anisotropy
KW  - Shear wave splitting
KW  - Subduction zone
KW  - Mantle rheology
Y1  - 2013
U6  - https://doi.org/10.1002/jgrb.50157
SN  - 2169-9313
SN  - 2169-9356
VL  - 118
IS  - 10
SP  - 5372
EP  - 5390
PB  - American Geophysical Union
CY  - Washington
ER  - 
TY  - JOUR
A1  - Mueller, K.
A1  - Raila, Jens
A1  - Altenkamp, Rainer
A1  - Schmidt, D.
A1  - Dietrich, R.
A1  - Hurtienne, Andrea
A1  - Wink, M.
A1  - Krone, O.
A1  - Brunnberg, Leo
A1  - Schweigert, Florian J.
T1  - Concentrations of retinol, 3,4-didehydroretinol, and retinyl esters in plasma of free-ranging birds of prey
JF  - Journal of animal physiology and animal nutrition
N2  - This study investigated vitamin A compounds in the plasma of healthy free-ranging Central European raptors with different feeding strategies. Plasma samples of nestlings of white-tailed sea eagle [white-tailed sea eagle (WTSE), Haliaeetus albicilla) (n = 32), osprey (Pandion haliaetus) (n = 39), northern goshawk (Accipiter gentilis) (n = 25), common buzzard (Buteo buteo) (n = 31), and honey buzzard (Pernis apivorus) (n = 18) and adults of WTSE (n = 10), osprey (n = 31), and northern goshawk (n = 45) were investigated with reversed-phase-high-performance liquid chromatography (RP-HPLC). In WTSE, northern goshawks and common buzzards retinol were the main plasma component of vitamin A, whilst in ospreys and honey buzzards, 3,4-didehydroretinol predominated. The median of the retinol plasma concentration in the nestlings group ranged from 0.12 to 3.80 mu M and in the adult group from 0.15 to 6.13 mu M. Median plasma concentrations of 3,4-didehydroretinol in nestlings ranged from 0.06 to 3.55 mu M. In adults, northern goshawks had the lowest plasma concentration of 3,4-didehydroretinol followed by WTSE and ospreys. The plasma of all investigated species contained retinyl esters (palmitate, oleate, and stearate). The results show considerable species-specific differences in the vitamin A plasma concentrations that might be caused by different nutrition strategies.
KW  - birds of prey
KW  - plasma
KW  - retinol
KW  - 3,4-didehydroretinol
KW  - retinyl esters
Y1  - 2012
U6  - https://doi.org/10.1111/j.1439-0396.2011.01219.x
SN  - 0931-2439
VL  - 96
IS  - 6
SP  - 1044
EP  - 1053
PB  - Wiley-Blackwell
CY  - Hoboken
ER  - 
TY  - JOUR
A1  - Collings, R.
A1  - Lange, Dietrich
A1  - Rietbrock, Andreas
A1  - Tilmann, F.
A1  - Natawidjaja, D.
A1  - Suwargadi, B.
A1  - Miller, M.
A1  - Saul, Joschim
T1  - Structure and seismogenic properties of the Mentawai segment of the Sumatra subduction zone revealed by local earthquake traveltime tomography
JF  - Journal of geophysical research : Solid earth
N2  - On 12 September 2007, an M-w 8.4 earthquake occurred within the southern section of the Mentawai segment of the Sumatra subduction zone, where the subduction thrust had previously ruptured in 1833 and 1797. Traveltime data obtained from a temporary local seismic network, deployed between December 2007 and October 2008 to record the aftershocks of the 2007 event, was used to determine two-dimensional (2-D) and three-dimensional (3-D) velocity models of the Mentawai segment. The seismicity distribution reveals significant activity along the subduction interface and within two clusters in the overriding plate either side of the forearc basin. The downgoing slab is clearly distinguished by a dipping region of high Vp (8.0 km/s), which can be a traced to similar to 50 km depth, with an increased Vp/Vs ratio (1.75 to 1.90) beneath the islands and the western side of the forearc basin, suggesting hydrated oceanic crust. Above the slab, a shallow continental Moho of less than 30 km depth can be inferred, suggesting that the intersection of the continental mantle with the subducting slab is much shallower than the downdip limit of the seismogenic zone despite localized serpentinization being present at the toe of the mantle wedge. The outer arc islands are characterized by low Vp (4.5-5.8 km/s) and high Vp/Vs (greater than 2.0), suggesting that they consist of fluid saturated sediments. The very low rigidity of the outer forearc contributed to the slow rupture of the M-w 7.7 Mentawai tsunami earthquake on 25 October 2010.
Y1  - 2012
U6  - https://doi.org/10.1029/2011JB008469
SN  - 2169-9313
SN  - 2169-9356
VL  - 117
IS  - 3
PB  - American Geophysical Union
CY  - Washington
ER  - 
TY  - JOUR
A1  - Lange, Dietrich
A1  - Bedford, J. R.
A1  - Moreno, M.
A1  - Tilmann, F.
A1  - Báez, Juan Carlos
A1  - Bevis, M.
A1  - Krüger, Frank
T1  - Comparison of postseismic afterslip models with aftershock seismicity for three subduction-zone earthquakes: Nias 2005, Maule 2010 and Tohoku 2011
JF  - Geophysical journal international
N2  - We focus on the relation between seismic and total postseismic afterslip following the Maule M-w 8.8 earthquake on 2010 February 27 in central Chile. First, we calculate the cumulative slip released by aftershock seismicity. We do this by summing up the aftershock regions and slip estimated from scaling relations. Comparing the cumulative seismic slip with afterslip modelswe showthat seismic slip of individual aftershocks exceeds locally the inverted afterslip model from geodetic constraints. As the afterslip model implicitly contains the displacements from the aftershocks, this reflects the tendency of afterslip models to smear out the actual slip pattern. However, it also suggests that locally slip for a number of the larger aftershocks exceeds the aseismic slip in spite of the fact that the total equivalent moment of the afterslip exceeds the cumulative moment of aftershocks by a large factor. This effect, seen weakly for the Maule 2010 and also for the Tohoku 2011 earthquake, can be explained by taking into account the uncertainties of the seismicity and afterslip models. In spite of uncertainties, the hypocentral region of the Nias 2005 earthquake is suggested to release a large fraction of moment almost purely seismically. Therefore, these aftershocks are not driven solely by the afterslip but instead their slip areas have probably been stressed by interseismic loading and the mainshock rupture. In a second step, we divide the megathrust of the Maule 2010 rupture into discrete cells and count the number of aftershocks that occur within 50 km of the centre of each cell as a function of time. We then compare this number to a time-dependent afterslip model by defining the 'afterslip to aftershock ratio' (ASAR) for each cell as the slope of the best fitting line when the afterslip at time t is plotted against aftershock count. Although we find a linear relation between afterslip and aftershocks for most cells, there is significant variability in ASAR in both the downdip and along-strike directions of the megathrust. We compare the spatial distribution of ASAR with the spatial distribution of seismic coupling, coseismic slip and Bouguer gravity anomaly, and in each case we find no significant correlation.
KW  - Creep and deformation
KW  - Earthquake dynamics
KW  - Seismicity and tectonics
KW  - Continental margins: convergent
Y1  - 2014
U6  - https://doi.org/10.1093/gji/ggu292
SN  - 0956-540X
SN  - 1365-246X
VL  - 199
IS  - 2
SP  - 784
EP  - 799
PB  - Oxford Univ. Press
CY  - Oxford
ER  - 
TY  - JOUR
A1  - Brinker, Walter
A1  - Wirges, Werner
A1  - Molzow, Wolf-Dietrich
A1  - Gerhard, Reimund
A1  - Melcher, R.
A1  - Budde, W.
A1  - Fiedler, H.
T1  - Active silicon CMOS addressing matrices for light-valve projection displays
Y1  - 1995
ER  - 
TY  - GEN
A1  - Schrön, Martin
A1  - Köhli, Markus
A1  - Scheiffele, Lena
A1  - Iwema, Joost
A1  - Bogena, Heye R.
A1  - Lv, Ling
A1  - Martini, Edoardo
A1  - Baroni, Gabriele
A1  - Rosolem, Rafael
A1  - Weimar, Jannis
A1  - Mai, Juliane
A1  - Cuntz, Matthias
A1  - Rebmann, Corinna
A1  - Oswald, Sascha
A1  - Dietrich, Peter
A1  - Schmidt, Ulrich
A1  - Zacharias, Steffen
T1  - Improving calibration and validation of cosmic-ray neutron sensors in the light of spatial sensitivity
T2  - Postprints der Universität Potsdam : Mathematisch Naturwissenschaftliche Reihe
N2  - In the last few years the method of cosmic-ray neutron sensing (CRNS) has gained popularity among hydrologists, physicists, and land-surface modelers. The sensor provides continuous soil moisture data, averaged over several hectares and tens of decimeters in depth. However, the signal still may contain unidentified features of hydrological processes, and many calibration datasets are often required in order to find reliable relations between neutron intensity and water dynamics. Recent insights into environmental neutrons accurately described the spatial sensitivity of the sensor and thus allowed one to quantify the contribution of individual sample locations to the CRNS signal. Consequently, data points of calibration and validation datasets are suggested to be averaged using a more physically based weighting approach. In this work, a revised sensitivity function is used to calculate weighted averages of point data. The function is different from the simple exponential convention by the extraordinary sensitivity to the first few meters around the probe, and by dependencies on air pressure, air humidity, soil moisture, and vegetation. The approach is extensively tested at six distinct monitoring sites: two sites with multiple calibration datasets and four sites with continuous time series datasets. In all cases, the revised averaging method improved the performance of the CRNS products. The revised approach further helped to reveal hidden hydrological processes which otherwise remained unexplained in the data or were lost in the process of overcalibration. The presented weighting approach increases the overall accuracy of CRNS products and will have an impact on all their applications in agriculture, hydrology, and modeling.
T3  - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 636 
KW  - forested headwater catchment
KW  - moisture observing system
KW  - soil-water content
KW  - parameterization methods
KW  - scale
KW  - field
KW  - dynamics
KW  - observatories
KW  - networks
Y1  - 2019
U6  - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-419134
IS  - 636
SP  - 5009
EP  - 5030
ER  - 
TY  - JOUR
A1  - Schrön, Martin
A1  - Köhli, Markus
A1  - Scheiffele, Lena
A1  - Iwema, Joost
A1  - Bogena, Heye R.
A1  - Lv, Ling
A1  - Martini, Edoardo
A1  - Baroni, Gabriele
A1  - Rosolem, Rafael
A1  - Weimar, Jannis
A1  - Mai, Juliane
A1  - Cuntz, Matthias
A1  - Rebmann, Corinna
A1  - Oswald, Sascha
A1  - Dietrich, Peter
A1  - Schmidt, Ulrich
A1  - Zacharias, Steffen
T1  - Improving calibration and validation of cosmic-ray neutron sensors in the light of spatial sensitivity
JF  - Hydrology and earth system sciences : HESS
N2  - In the last few years the method of cosmic-ray neutron sensing (CRNS) has gained popularity among hydrologists, physicists, and land-surface modelers. The sensor provides continuous soil moisture data, averaged over several hectares and tens of decimeters in depth. However, the signal still may contain unidentified features of hydrological processes, and many calibration datasets are often required in order to find reliable relations between neutron intensity and water dynamics. Recent insights into environmental neutrons accurately described the spatial sensitivity of the sensor and thus allowed one to quantify the contribution of individual sample locations to the CRNS signal. Consequently, data points of calibration and validation datasets are suggested to be averaged using a more physically based weighting approach. In this work, a revised sensitivity function is used to calculate weighted averages of point data. The function is different from the simple exponential convention by the extraordinary sensitivity to the first few meters around the probe, and by dependencies on air pressure, air humidity, soil moisture, and vegetation. The approach is extensively tested at six distinct monitoring sites: two sites with multiple calibration datasets and four sites with continuous time series datasets. In all cases, the revised averaging method improved the performance of the CRNS products. The revised approach further helped to reveal hidden hydrological processes which otherwise remained unexplained in the data or were lost in the process of overcalibration. The presented weighting approach increases the overall accuracy of CRNS products and will have an impact on all their applications in agriculture, hydrology, and modeling.
Y1  - 2017
U6  - https://doi.org/10.5194/hess-21-5009-2017
SN  - 1027-5606
SN  - 1607-7938
VL  - 21
SP  - 5009
EP  - 5030
PB  - Copernicus
CY  - Göttingen
ER  -