Evolution of the Antarctic Ice Sheet since Late Pleistocene

Available data show that the of fossil plants testified that the Antarctica was a rather warm or even hot and humid region covered with forest from Devonian to Cretaceous periods. Furthermore, even Antarctic coasts still kept in a warm and humid condition until early Tertiary of 37, Ma ago. It there...

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Bibliographic Details
Main Author: Qingsong, Zhang
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 1990
Subjects:
Antarctic
The Antarctic
Advances in Polar Science
Antarc*
Antarctica
Ice Sheet
Polar Science
Online Access:http://library.arcticportal.org/2016/
http://library.arcticportal.org/2016/1/A19900101.pdf
id ftarcticportal:oai:generic.eprints.org:2016
record_format openpolar
spelling ftarcticportal:oai:generic.eprints.org:2016 2023-05-15T13:05:24+02:00 Evolution of the Antarctic Ice Sheet since Late Pleistocene Qingsong, Zhang 1990-12 application/pdf http://library.arcticportal.org/2016/ http://library.arcticportal.org/2016/1/A19900101.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2016/1/A19900101.pdf Qingsong, Zhang (1990) Evolution of the Antarctic Ice Sheet since Late Pleistocene. Advances in Polar Science, 1 (1). pp. 1-7. Article PeerReviewed 1990 ftarcticportal 2023-04-05T22:52:04Z Available data show that the of fossil plants testified that the Antarctica was a rather warm or even hot and humid region covered with forest from Devonian to Cretaceous periods. Furthermore, even Antarctic coasts still kept in a warm and humid condition until early Tertiary of 37, Ma ago. It therefore can be considered that the Antarctica was not situated at its present position, but in tropic or temperate zone before the Tertiary. Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctic Antarctica Ice Sheet Polar Science Polar Science Arctic Portal Library Antarctic The Antarctic
institution Open Polar
collection Arctic Portal Library
op_collection_id ftarcticportal
language English
description Available data show that the of fossil plants testified that the Antarctica was a rather warm or even hot and humid region covered with forest from Devonian to Cretaceous periods. Furthermore, even Antarctic coasts still kept in a warm and humid condition until early Tertiary of 37, Ma ago. It therefore can be considered that the Antarctica was not situated at its present position, but in tropic or temperate zone before the Tertiary.
format Article in Journal/Newspaper
author Qingsong, Zhang
spellingShingle Qingsong, Zhang
Evolution of the Antarctic Ice Sheet since Late Pleistocene
author_facet Qingsong, Zhang
author_sort Qingsong, Zhang
title Evolution of the Antarctic Ice Sheet since Late Pleistocene
title_short Evolution of the Antarctic Ice Sheet since Late Pleistocene
title_full Evolution of the Antarctic Ice Sheet since Late Pleistocene
title_fullStr Evolution of the Antarctic Ice Sheet since Late Pleistocene
title_full_unstemmed Evolution of the Antarctic Ice Sheet since Late Pleistocene
title_sort evolution of the antarctic ice sheet since late pleistocene
publisher Polar Research Institute of China - PRIC
publishDate 1990
url http://library.arcticportal.org/2016/
http://library.arcticportal.org/2016/1/A19900101.pdf
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Advances in Polar Science
Antarc*
Antarctic
Antarctica
Ice Sheet
Polar Science
Polar Science
genre_facet Advances in Polar Science
Antarc*
Antarctic
Antarctica
Ice Sheet
Polar Science
Polar Science
op_relation http://library.arcticportal.org/2016/1/A19900101.pdf
Qingsong, Zhang (1990) Evolution of the Antarctic Ice Sheet since Late Pleistocene. Advances in Polar Science, 1 (1). pp. 1-7.
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