Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica

We describe paleoenvironmental changes related to ice sheet and ice shelf developments in the western Ross Sea in the late Quaternary, based on the three sediment cores collected along ca 167°E We distinguish four lithologic units in their sequences as follows (1) Unit I of diatomaceous mud, (2) Uni...

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Main Authors: Nishimura,Akira, Nakasone,Toru, Hiramatsu,Chikara, Tanahashi,Manabu
Format: Report
Language:English
Published: Geological Survey of Japan/Kawasaki Geological Engineering Co., Ltd./Japan Petroleum Exploration Co. Ltd./Japan National Oil Corporation 1998
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3029
http://id.nii.ac.jp/1291/00003029/
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003029 2023-05-15T13:49:00+02:00 Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica Nishimura,Akira Nakasone,Toru Hiramatsu,Chikara Tanahashi,Manabu 1998-10 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3029 http://id.nii.ac.jp/1291/00003029/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3029&item_no=1&attribute_id=18&file_no=1 en eng Geological Survey of Japan/Kawasaki Geological Engineering Co., Ltd./Japan Petroleum Exploration Co. Ltd./Japan National Oil Corporation National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3029 http://id.nii.ac.jp/1291/00003029/ AA1130866X Polar geoscience, 11, 208-221(1998-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3029&item_no=1&attribute_id=18&file_no=1 Ross Sea late Quaternary sea bottom sediments AMS radiocarbon dating Departmental Bulletin Paper P(論文) 1998 ftnipr 2022-11-26T19:42:23Z We describe paleoenvironmental changes related to ice sheet and ice shelf developments in the western Ross Sea in the late Quaternary, based on the three sediment cores collected along ca 167°E We distinguish four lithologic units in their sequences as follows (1) Unit I of diatomaceous mud, (2) Unit IIA of mud, (3) Unit IIB of alternating clay and thin laminated silt, and (4) Unit III of consolidated sandy silt with pebbly gravel Interpreted sedimentary environments based on the time constraints of fifteen AMS ^<14>C dates and characteristics of sediments and diatom assemblages, are summarized as follows (1) Prior to the ice sheet advance, this area was possibly under a marine environment, (2) the grounded ice sheet is thought to have advanced between 35 and 20 ka BP, (3) shelf ice possibly covered the southern site between 25 and 20 ka BP, (4) an open marine environment with moderate productivity existed from 20 ka BP at the northern site, and (5) an open marine environment with high productivity existed from 9kaBP The length and timing of the ice sheet advance cannot explain radiocarbon dates of all sites Radiocarbon dating of marine sediments in the Antarctic area shows a large reservoir effect and contamination of reworked dead carbon In our estimation of the ages, two thousand years correction is needed in the upper unit at least Age data for lower units are thought to be older than the true sedimentary ages though these need further consideration Report Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Polar geoscience Ross Sea National Institute of Polar Research Repository, Japan Antarctic The Antarctic Ross Sea
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Ross Sea
late Quaternary
sea bottom sediments
AMS radiocarbon dating
spellingShingle Ross Sea
late Quaternary
sea bottom sediments
AMS radiocarbon dating
Nishimura,Akira
Nakasone,Toru
Hiramatsu,Chikara
Tanahashi,Manabu
Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica
topic_facet Ross Sea
late Quaternary
sea bottom sediments
AMS radiocarbon dating
description We describe paleoenvironmental changes related to ice sheet and ice shelf developments in the western Ross Sea in the late Quaternary, based on the three sediment cores collected along ca 167°E We distinguish four lithologic units in their sequences as follows (1) Unit I of diatomaceous mud, (2) Unit IIA of mud, (3) Unit IIB of alternating clay and thin laminated silt, and (4) Unit III of consolidated sandy silt with pebbly gravel Interpreted sedimentary environments based on the time constraints of fifteen AMS ^<14>C dates and characteristics of sediments and diatom assemblages, are summarized as follows (1) Prior to the ice sheet advance, this area was possibly under a marine environment, (2) the grounded ice sheet is thought to have advanced between 35 and 20 ka BP, (3) shelf ice possibly covered the southern site between 25 and 20 ka BP, (4) an open marine environment with moderate productivity existed from 20 ka BP at the northern site, and (5) an open marine environment with high productivity existed from 9kaBP The length and timing of the ice sheet advance cannot explain radiocarbon dates of all sites Radiocarbon dating of marine sediments in the Antarctic area shows a large reservoir effect and contamination of reworked dead carbon In our estimation of the ages, two thousand years correction is needed in the upper unit at least Age data for lower units are thought to be older than the true sedimentary ages though these need further consideration
format Report
author Nishimura,Akira
Nakasone,Toru
Hiramatsu,Chikara
Tanahashi,Manabu
author_facet Nishimura,Akira
Nakasone,Toru
Hiramatsu,Chikara
Tanahashi,Manabu
author_sort Nishimura,Akira
title Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica
title_short Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica
title_full Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica
title_fullStr Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica
title_full_unstemmed Sediment cores and their radiocarbon ages in the Western Ross Sea, Antarctica
title_sort sediment cores and their radiocarbon ages in the western ross sea, antarctica
publisher Geological Survey of Japan/Kawasaki Geological Engineering Co., Ltd./Japan Petroleum Exploration Co. Ltd./Japan National Oil Corporation
publishDate 1998
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3029
http://id.nii.ac.jp/1291/00003029/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3029&item_no=1&attribute_id=18&file_no=1
geographic Antarctic
The Antarctic
Ross Sea
geographic_facet Antarctic
The Antarctic
Ross Sea
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Polar geoscience
Ross Sea
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Polar geoscience
Ross Sea
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3029
http://id.nii.ac.jp/1291/00003029/
AA1130866X
Polar geoscience, 11, 208-221(1998-10)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3029&item_no=1&attribute_id=18&file_no=1
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