A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions
Antarctic cryosphere has significant impact on the global climate system by influencing the ocean currents, the atmosphere, and the sea level for long term durations. Antarctic Ice Sheet (AIS) has evolved from temporary to permanent ice sheet during Oligocene (~32 Ma). Throughout its evolution, it w...
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ftnipr:oai:nipr.repo.nii.ac.jp:00016861 2023-05-15T13:46:39+02:00 A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions 2021-12 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16861 http://id.nii.ac.jp/1291/00016731/ en eng https://doi.org/10.1016/j.polar.2021.100720 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16861 http://id.nii.ac.jp/1291/00016731/ Polar Science, 30, 100720(2021-12) 18739652 Antarctic ice sheet Cenozoic Paleoclimate Ice sheet fluctuations Journal Article 2021 ftnipr https://doi.org/10.1016/j.polar.2021.100720 2023-02-18T20:11:55Z Antarctic cryosphere has significant impact on the global climate system by influencing the ocean currents, the atmosphere, and the sea level for long term durations. Antarctic Ice Sheet (AIS) has evolved from temporary to permanent ice sheet during Oligocene (~32 Ma). Throughout its evolution, it witnessed severe climatic conditions leading to several phases of retreat and advancements. Major climatic events were directly associated with the evolution of AIS. Paleocene Eocene Thermal Maximum (PETM), Early Eocene Climatic Optimum (EECO, ~44.9 Ma), Eocene Oligocene Boundary (Oi1 event, ~34 Ma), Oligocene-Miocene Boundary (Mi1 event ~25Ma), Mid Miocene Climatic Optimum (MMCO; ~15Ma), Miocene-Pliocene Boundary (~3Ma) and Mid-late Pleistocene Transition (MPT, after ~1.25 Ma) are the major reported global climatic events. This work summarises these events and critically reviews the role of various factors in the advancement and retreat of AIS and its coupled response to the global climate change including future global challenges. Existing knowledge gaps and challenges are outlined for each of the climatic events and priorities for future research are suggested. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Polar Science Polar Science National Institute of Polar Research Repository, Japan Antarctic Polar Science 30 100720 |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
Antarctic ice sheet Cenozoic Paleoclimate Ice sheet fluctuations |
spellingShingle |
Antarctic ice sheet Cenozoic Paleoclimate Ice sheet fluctuations A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions |
topic_facet |
Antarctic ice sheet Cenozoic Paleoclimate Ice sheet fluctuations |
description |
Antarctic cryosphere has significant impact on the global climate system by influencing the ocean currents, the atmosphere, and the sea level for long term durations. Antarctic Ice Sheet (AIS) has evolved from temporary to permanent ice sheet during Oligocene (~32 Ma). Throughout its evolution, it witnessed severe climatic conditions leading to several phases of retreat and advancements. Major climatic events were directly associated with the evolution of AIS. Paleocene Eocene Thermal Maximum (PETM), Early Eocene Climatic Optimum (EECO, ~44.9 Ma), Eocene Oligocene Boundary (Oi1 event, ~34 Ma), Oligocene-Miocene Boundary (Mi1 event ~25Ma), Mid Miocene Climatic Optimum (MMCO; ~15Ma), Miocene-Pliocene Boundary (~3Ma) and Mid-late Pleistocene Transition (MPT, after ~1.25 Ma) are the major reported global climatic events. This work summarises these events and critically reviews the role of various factors in the advancement and retreat of AIS and its coupled response to the global climate change including future global challenges. Existing knowledge gaps and challenges are outlined for each of the climatic events and priorities for future research are suggested. |
format |
Article in Journal/Newspaper |
title |
A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions |
title_short |
A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions |
title_full |
A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions |
title_fullStr |
A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions |
title_full_unstemmed |
A review of Antarctic ice sheet fluctuations records during Cenozoic and its cause and effect relation with the climatic conditions |
title_sort |
review of antarctic ice sheet fluctuations records during cenozoic and its cause and effect relation with the climatic conditions |
publishDate |
2021 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16861 http://id.nii.ac.jp/1291/00016731/ |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Ice Sheet Polar Science Polar Science |
genre_facet |
Antarc* Antarctic Ice Sheet Polar Science Polar Science |
op_relation |
https://doi.org/10.1016/j.polar.2021.100720 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16861 http://id.nii.ac.jp/1291/00016731/ Polar Science, 30, 100720(2021-12) 18739652 |
op_doi |
https://doi.org/10.1016/j.polar.2021.100720 |
container_title |
Polar Science |
container_volume |
30 |
container_start_page |
100720 |
_version_ |
1766244939927126016 |