Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica

The typical glacial-marine sedimentation has been recorded from core NP93-2 in the Prydz Bay, Antarctica. The sedimentation processes, sedimentary environment and paleoclimate variations since 12937 a B.P. have been discussed, based on grain size, mineral composition and micropaleontological data, e...

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Main Authors: Shiguo, Wu, Youlang, Luo, Youqiang, Wang, Jun, Lu, Fan, Zheng, Shaoxian, Sun
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 1996
Subjects:
Online Access:http://library.arcticportal.org/2119/
http://library.arcticportal.org/2119/1/A602.007.pdf
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spelling ftarcticportal:oai:generic.eprints.org:2119 2023-06-11T04:03:01+02:00 Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica Shiguo, Wu Youlang, Luo Youqiang, Wang Jun, Lu Fan, Zheng Shaoxian, Sun 1996-12 application/pdf http://library.arcticportal.org/2119/ http://library.arcticportal.org/2119/1/A602.007.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2119/1/A602.007.pdf Shiguo, Wu and Youlang, Luo and Youqiang, Wang and Jun, Lu and Fan, Zheng and Shaoxian, Sun (1996) Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica. Advances in Polar Science, 7 (2). pp. 164-172. Article PeerReviewed 1996 ftarcticportal 2023-04-19T22:52:31Z The typical glacial-marine sedimentation has been recorded from core NP93-2 in the Prydz Bay, Antarctica. The sedimentation processes, sedimentary environment and paleoclimate variations since 12937 a B.P. have been discussed, based on grain size, mineral composition and micropaleontological data, etc. The climate variation occurred at 10 ka, which expressed that there were increased inputs of terrigenous clastics. The climate change once again but temporarily took place at late Holocene. Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctica Polar Science Polar Science Prydz Bay Arctic Portal Library Prydz Bay
institution Open Polar
collection Arctic Portal Library
op_collection_id ftarcticportal
language English
description The typical glacial-marine sedimentation has been recorded from core NP93-2 in the Prydz Bay, Antarctica. The sedimentation processes, sedimentary environment and paleoclimate variations since 12937 a B.P. have been discussed, based on grain size, mineral composition and micropaleontological data, etc. The climate variation occurred at 10 ka, which expressed that there were increased inputs of terrigenous clastics. The climate change once again but temporarily took place at late Holocene.
format Article in Journal/Newspaper
author Shiguo, Wu
Youlang, Luo
Youqiang, Wang
Jun, Lu
Fan, Zheng
Shaoxian, Sun
spellingShingle Shiguo, Wu
Youlang, Luo
Youqiang, Wang
Jun, Lu
Fan, Zheng
Shaoxian, Sun
Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica
author_facet Shiguo, Wu
Youlang, Luo
Youqiang, Wang
Jun, Lu
Fan, Zheng
Shaoxian, Sun
author_sort Shiguo, Wu
title Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica
title_short Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica
title_full Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica
title_fullStr Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica
title_full_unstemmed Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica
title_sort holocene glacial-marine sedimentation in the prydz bay, antarctica
publisher Polar Research Institute of China - PRIC
publishDate 1996
url http://library.arcticportal.org/2119/
http://library.arcticportal.org/2119/1/A602.007.pdf
geographic Prydz Bay
geographic_facet Prydz Bay
genre Advances in Polar Science
Antarc*
Antarctica
Polar Science
Polar Science
Prydz Bay
genre_facet Advances in Polar Science
Antarc*
Antarctica
Polar Science
Polar Science
Prydz Bay
op_relation http://library.arcticportal.org/2119/1/A602.007.pdf
Shiguo, Wu and Youlang, Luo and Youqiang, Wang and Jun, Lu and Fan, Zheng and Shaoxian, Sun (1996) Holocene glacial-marine sedimentation in the Prydz Bay, Antarctica. Advances in Polar Science, 7 (2). pp. 164-172.
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