History of Anvers-Hugo Trough, western Antarctic Peninsula shelf, since the Last Glacial Maximum. Part II: Palaeo-productivity and palaeoceanographic changes during the Last Glacial Transition
Following the Last Glacial Maximum (LGM; ca. 23-19 calibrated [cal.] kyr before present [BP]), atmospheric and oceanic warming, together with global sea-level rise, drove widespread deglaciation of the Antarctic Ice Sheet, increasing the flux of freshwater to the ocean and leading to substantial cha...
Published in: | Quaternary Science Reviews |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2022
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/57256/ https://doi.org/10.1016/j.quascirev.2022.107503 https://hdl.handle.net/10013/epic.fb06808c-40fb-488d-aaa1-dc0c976b8a67 |