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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: | Sci Rep |
|---|---|
| Hauptverfasser: | , , , , , , , , , , |
| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Nature Publishing Group UK
2018
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| Schlagworte: | |
| Online Zugang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6063862/ https://ncbi.nlm.nih.gov/pubmed/30054536 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-29718-7 |
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