Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Johann Philipp Klages"'
Autor:
Johann Philipp Klages, Christoph Gaedicke, Reinhard Drews, Astrid Oetting, Boris Dorschel, Frank Wilhelms, Gerhard Kuhn, Ralf Tiedemann, Olaf Eisen, Emma Smith, Christoph Mayer, Astrid Lambrecht, Andreas Läufer, Jan Erik Arndt, Coen Hofstede, Todd A. Ehlers
The Ekström Ice Shelf is one of numerous small ice shelves that fringe the coastline of western Dronning Maud Land, East Antarctica. Reconstructions of past ice-sheet extent in this area are poorly constrained, due to a lack of geomorphological evid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::746bea9b910e9acea3eef46c1706bc6f
https://doi.org/10.5194/tc-2021-305
https://doi.org/10.5194/tc-2021-305
Autor:
Sandra Passchier, Johann Philipp Klages, Johanna Gille-Petzoldt, Claus-Dieter Hillenbrand, Gabriele Uenzelmann-Neben, Karsten Gohl, Julia S. Wellner, German Leitchenkov, S. M. Bohaty, Rachel L. Lamb, Thomas Frederichs
The West Antarctic Ice Sheet (WAIS) is thought to be highly sensitive to climatic and oceanographic changes. Modelling infers that the WAIS likely had a very dynamic history throughout the Neogene to the present. A complete collapse of the WAIS would
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41364a2c0a14bbca7edcb90eeffe2f4d
https://doi.org/10.5194/egusphere-egu21-14232
https://doi.org/10.5194/egusphere-egu21-14232
Autor:
Claus-Dieter Hillenbrand, Jürgen Titschack, Karsten Gohl, Anton Eisenhauer, Ulrich Salzmann, Johann Philipp Klages, Thorsten Bauersachs, Robert D Larter, Katharina Hochmuth, Torsten Bickert, Gerhard Schmiedl, Juliane Müller, Tina van de Flierdt, Werner Ehrmann, Thomas Frederichs, Gerhard Kuhn, Gerrit Lohmann, Steven M Bohaty, Cornelia Spiegel, Francisco J. Rodríguez Tovar
The Eocene-Oligocene Transition (~34.4–33.7 Ma) marks a major step in the long-term evolution from the greenhouse climate of the Early Palaeogene to the icehouse regime of the Late Neogene and Quaternary. However, it remains uncertain which landmas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b1c749cf801ef75ff80a362d69147f90
https://doi.org/10.5194/egusphere-egu21-1538
https://doi.org/10.5194/egusphere-egu21-1538
Autor:
Claus-Dieter Hillenbrand, Sandra Passchier, Adam Klaus, John M. Fegyveresi, Delaney E. Robinson, W. Rahaman, Thorsten Bauersachs, L. Wu, M. Courtillat, M. Iwai, J. Kim, M.L. Penkrot, Christine S. Siddoway, M.A. De Lira Mota, Johann Philipp Klages, Benedict T. I. Reinardy, M.S.R. Esteves, K. Horikawa, J.G. Prebble, R.P. Scherer, T.M. King, Ellen A. Cowan, Julia S. Wellner, A.R. Halberstadt, Johan Renaudie, S. M. Bohaty, Karsten Gohl, L. Gao, Thomas Frederichs, Masako Yamane
Publikováno v:
Volume 379: Amundsen Sea West Antarctic Ice Sheet History
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b957800ce2e74ac0197cac488fbd7ea
https://doi.org/10.14379/iodp.proc.379.101.2021
https://doi.org/10.14379/iodp.proc.379.101.2021
Autor:
Karsten Gohl, Sandra Passchier, A.R. Halberstadt, Christine S. Siddoway, Adam Klaus, T.M. King, W. Rahaman, Johann Philipp Klages, M.S.R. Esteves, Thomas Frederichs, R.P. Scherer, K. Horikawa, J.G. Prebble, Thorsten Bauersachs, Ellen A. Cowan, L. Gao, Benedict T. I. Reinardy, M.L. Penkrot, Julia S. Wellner, S. M. Bohaty, J. Kim, Delaney E. Robinson, John M. Fegyveresi, Claus-Dieter Hillenbrand, L. Wu, M. Courtillat, Johan Renaudie, Masako Yamane, M. Iwai, M.A. De Lira Mota
Publikováno v:
Volume 379: Amundsen Sea West Antarctic Ice Sheet History
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71fc51abf43258ad24623bcb325a84d6
https://doi.org/10.14379/iodp.proc.379.102.2021
https://doi.org/10.14379/iodp.proc.379.102.2021
Autor:
Simões Pereira Patric, Ehrmann Werner, Igor Niezgodzki, Kuhn Gerhard, Bickert Torsten, Spiegel Cornelia, Salzmann Ulrich, Hillenbrand Claus-Dieter, Frederichs Thomas, Uenzelmann-Neben Gabriele, Larter Robert, Bohaty Steven, Johann Philipp Klages, Titschack Jürgen, Lohmann Gerrit, Zundel Maximilian, van de Flierdt Tina, Gohl Karsten, Bauersachs Thorsten, Müller Juliane
The mid-Cretaceous was one of the warmest intervals of the past 140 million years (Myr) driven by atmospheric CO2 levels around 1000 ppmv. In the near absence of proximal geological records from south of the Antarctic Circle, it remains disputed whet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0782cf4f4af350fbef32d7710bebc5b5
https://doi.org/10.5194/egusphere-egu2020-242
https://doi.org/10.5194/egusphere-egu2020-242
Autor:
Johann Philipp Klages, Karsten Gohl, Gerold Wefer, Tim Freudenthal, Gerhard Bohrmann, Klaus Wallmann, Michael Riedel
Over the last two decades sea bed drilling technology has proven to provide a valuable complement to the services of classical drill ships. Especially for shallow drillings up to 200 mbsf and when working in remote areas difficult to access, sea bed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d97254d9db707be39794897908cfd631
https://doi.org/10.5194/egusphere-egu2020-5089
https://doi.org/10.5194/egusphere-egu2020-5089
Autor:
John B. Anderson, Martin Jakobsson, Karsten Gohl, Alastair G C Graham, Johann Philipp Klages, Adrian Jenkins, Robert D Larter, Claus-Dieter Hillenbrand, Frank O. Nitsche, James Smith
Publikováno v:
EPIC3Geological Society London Memoirs, The Geological Society, London, 46, pp. 493-500, ISSN: 0435-4052
About 30% of ice draining the West Antarctic Ice Sheet discharges through several glacier systems into the Amundsen Sea Embayment (ASE) (Fig. 1a). Two major ice-stream outlets, Pine Island and Thwaites glaciers, have undergone significant twentieth c
Autor:
Karsten Gohl, Johann Philipp Klages, Robert D Larter, Claus-Dieter Hillenbrand, James Smith, Alastair G C Graham, Gerhard Kuhn
Publikováno v:
Geological Society, London, Memoirs. 46:349-352
Large ice streams that drain the West Antarctic Ice Sheet (WAIS) into the Amundsen Sea Embayment (ASE) are currently thinning, accelerating and retreating rapidly (e.g. Rignot et al. 2014). These ice streams are assumed to have reached the continenta
Autor:
Alastair G C Graham, Karsten Gohl, Claus-Dieter Hillenbrand, Thomas Frederichs, Gerhard Kuhn, Patrycja E Jernas, James Smith, Johann Philipp Klages, Lukas Wacker, Frank O. Nitsche
Publikováno v:
PLoS ONE
EPIC3PLoS ONE, PUBLIC LIBRARY SCIENCE, 12(7), pp. 1-16, ISSN: 1932-6203
PLoS ONE, Vol 12, Iss 7, p e0181593 (2017)
PLoS ONE, 12 (7)
EPIC3PLoS ONE, PUBLIC LIBRARY SCIENCE, 12(7), pp. 1-16, ISSN: 1932-6203
PLoS ONE, Vol 12, Iss 7, p e0181593 (2017)
PLoS ONE, 12 (7)
Source at https://doi.org/10.1371/journal.pone.0181593 Precise knowledge about the extent of the West Antarctic Ice Sheet (WAIS) at the Last Glacial Maximum (LGM; c. 26.5–19 cal. ka BP) is important in order to 1) improve paleo-ice sheet reconstruc