Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions
Over the past 34 Million years, the Antarctic continental shelf has gradually deepened due to ice sheet loading, thermal subsidence, and erosion from repeated glaciations. The deepening that is recorded in the sedimentary deposits around the Antarctic margin indicates that after the mid-Miocene Clim...
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| Veröffentlicht in: | Scientific reports Jg. 8; H. 1; S. 11323 |
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| Sprache: | Englisch |
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27.07.2018
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| ISSN: | 2045-2322, 2045-2322 |
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| Abstract | Over the past 34 Million years, the Antarctic continental shelf has gradually deepened due to ice sheet loading, thermal subsidence, and erosion from repeated glaciations. The deepening that is recorded in the sedimentary deposits around the Antarctic margin indicates that after the mid-Miocene Climate Optimum (≈15 Ma), Antarctic Ice Sheet (AIS) dynamical response to climate conditions changed. We explore end-members for maximum AIS extent, based on ice-sheet simulations of a late-Pleistocene and a mid-Miocene glaciation. Fundamental dynamical differences emerge as a consequence of atmospheric forcing, eustatic sea level and continental shelf evolution. We show that the AIS contributed to the amplification of its own sensitivity to ocean forcing by gradually expanding and eroding the continental shelf, that probably changed its tipping points through time. The lack of past topographic and bathymetric reconstructions implies that so far, we still have an incomplete understanding of AIS fast response to past warm climate conditions, which is crucial to constrain its future evolution. |
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| AbstractList | Over the past 34 Million years, the Antarctic continental shelf has gradually deepened due to ice sheet loading, thermal subsidence, and erosion from repeated glaciations. The deepening that is recorded in the sedimentary deposits around the Antarctic margin indicates that after the mid-Miocene Climate Optimum (≈15 Ma), Antarctic Ice Sheet (AIS) dynamical response to climate conditions changed. We explore end-members for maximum AIS extent, based on ice-sheet simulations of a late-Pleistocene and a mid-Miocene glaciation. Fundamental dynamical differences emerge as a consequence of atmospheric forcing, eustatic sea level and continental shelf evolution. We show that the AIS contributed to the amplification of its own sensitivity to ocean forcing by gradually expanding and eroding the continental shelf, that probably changed its tipping points through time. The lack of past topographic and bathymetric reconstructions implies that so far, we still have an incomplete understanding of AIS fast response to past warm climate conditions, which is crucial to constrain its future evolution. Over the past 34 Million years, the Antarctic continental shelf has gradually deepened due to ice sheet loading, thermal subsidence, and erosion from repeated glaciations. The deepening that is recorded in the sedimentary deposits around the Antarctic margin indicates that after the mid-Miocene Climate Optimum (≈15 Ma), Antarctic Ice Sheet (AIS) dynamical response to climate conditions changed. We explore end-members for maximum AIS extent, based on ice-sheet simulations of a late-Pleistocene and a mid-Miocene glaciation. Fundamental dynamical differences emerge as a consequence of atmospheric forcing, eustatic sea level and continental shelf evolution. We show that the AIS contributed to the amplification of its own sensitivity to ocean forcing by gradually expanding and eroding the continental shelf, that probably changed its tipping points through time. The lack of past topographic and bathymetric reconstructions implies that so far, we still have an incomplete understanding of AIS fast response to past warm climate conditions, which is crucial to constrain its future evolution.Over the past 34 Million years, the Antarctic continental shelf has gradually deepened due to ice sheet loading, thermal subsidence, and erosion from repeated glaciations. The deepening that is recorded in the sedimentary deposits around the Antarctic margin indicates that after the mid-Miocene Climate Optimum (≈15 Ma), Antarctic Ice Sheet (AIS) dynamical response to climate conditions changed. We explore end-members for maximum AIS extent, based on ice-sheet simulations of a late-Pleistocene and a mid-Miocene glaciation. Fundamental dynamical differences emerge as a consequence of atmospheric forcing, eustatic sea level and continental shelf evolution. We show that the AIS contributed to the amplification of its own sensitivity to ocean forcing by gradually expanding and eroding the continental shelf, that probably changed its tipping points through time. The lack of past topographic and bathymetric reconstructions implies that so far, we still have an incomplete understanding of AIS fast response to past warm climate conditions, which is crucial to constrain its future evolution. |
| ArticleNumber | 11323 |
| Author | Wardell, Nigel Montoli, Enea Colleoni, Florence De Santis, Laura Sorlien, Christopher C. Bart, Philip J. Sauli, Chiara Olivo, Elisabetta Prato, Stefano Gasson, Edward G. W. Bergamasco, Andrea |
| Author_xml | – sequence: 1 givenname: Florence orcidid: 0000-0003-4582-812X surname: Colleoni fullname: Colleoni, Florence email: flocolleoni@gmail.com organization: Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Istituto Nazionale di Oceanografia Sperimentale – sequence: 2 givenname: Laura surname: De Santis fullname: De Santis, Laura organization: Istituto Nazionale di Oceanografia Sperimentale – sequence: 3 givenname: Enea surname: Montoli fullname: Montoli, Enea organization: Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici – sequence: 4 givenname: Elisabetta surname: Olivo fullname: Olivo, Elisabetta organization: Istituto Nazionale di Oceanografia Sperimentale, Dipartimento Scienze Fisiche, della Terra e dell’Ambiente, Universita di Siena – sequence: 5 givenname: Christopher C. surname: Sorlien fullname: Sorlien, Christopher C. organization: Earth Research Institute, University of California – sequence: 6 givenname: Philip J. surname: Bart fullname: Bart, Philip J. organization: Louisiana State University, Department of Geology and Geophysics – sequence: 7 givenname: Edward G. W. surname: Gasson fullname: Gasson, Edward G. W. organization: Department of Geography, University of Sheffield – sequence: 8 givenname: Andrea surname: Bergamasco fullname: Bergamasco, Andrea organization: CNR-ISMAR – sequence: 9 givenname: Chiara surname: Sauli fullname: Sauli, Chiara organization: Istituto Nazionale di Oceanografia Sperimentale – sequence: 10 givenname: Nigel surname: Wardell fullname: Wardell, Nigel organization: Istituto Nazionale di Oceanografia Sperimentale – sequence: 11 givenname: Stefano surname: Prato fullname: Prato, Stefano organization: A.P.E. Research srl |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/30054536$$D View this record in MEDLINE/PubMed |
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| SubjectTerms | 639/705/1042 704/106/413 Atmospheric forcing Climatic conditions Continental shelves Evolution Glaciation Humanities and Social Sciences Ice Miocene multidisciplinary Pleistocene Science Science (multidisciplinary) Sea level |
| Title | Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions |
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