Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons

Chilean glaciers at a latitude of 41°S reached a maximum extent about 19,400 carbon-14 years before the present (B. P.), shrank 50 percent by 16,000 years B. P., and readvanced to a smaller maximum after 14,800 years B. P. These fluctuations were closely in step with those of the Laurentide ice shee...

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Published in:Science
Main Author: Mercer, J. H.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1972
Subjects:
Online Access:http://dx.doi.org/10.1126/science.176.4039.1118
https://www.science.org/doi/pdf/10.1126/science.176.4039.1118
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spelling craaas:10.1126/science.176.4039.1118 2024-09-30T14:26:40+00:00 Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons Mercer, J. H. 1972 http://dx.doi.org/10.1126/science.176.4039.1118 https://www.science.org/doi/pdf/10.1126/science.176.4039.1118 en eng American Association for the Advancement of Science (AAAS) Science volume 176, issue 4039, page 1118-1120 ISSN 0036-8075 1095-9203 journal-article 1972 craaas https://doi.org/10.1126/science.176.4039.1118 2024-09-12T04:01:09Z Chilean glaciers at a latitude of 41°S reached a maximum extent about 19,400 carbon-14 years before the present (B. P.), shrank 50 percent by 16,000 years B. P., and readvanced to a smaller maximum after 14,800 years B. P. These fluctuations were closely in step with those of the Laurentide ice sheet east of the Mississippi River but differ somewhat from the accepted sequence in New Zealand. A corresponding pattern is not apparent in the Antarctic paleotemperature curve deduced from changes in oxygen isotope ratios. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet AAAS Resource Center (American Association for the Advancement of Science) Antarctic New Zealand The Antarctic Science 176 4039 1118 1120
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Chilean glaciers at a latitude of 41°S reached a maximum extent about 19,400 carbon-14 years before the present (B. P.), shrank 50 percent by 16,000 years B. P., and readvanced to a smaller maximum after 14,800 years B. P. These fluctuations were closely in step with those of the Laurentide ice sheet east of the Mississippi River but differ somewhat from the accepted sequence in New Zealand. A corresponding pattern is not apparent in the Antarctic paleotemperature curve deduced from changes in oxygen isotope ratios.
format Article in Journal/Newspaper
author Mercer, J. H.
spellingShingle Mercer, J. H.
Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons
author_facet Mercer, J. H.
author_sort Mercer, J. H.
title Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons
title_short Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons
title_full Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons
title_fullStr Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons
title_full_unstemmed Chilean Glacial Chronology 20,000 to 11,000 Carbon-14 Years Ago: Some Global Comparisons
title_sort chilean glacial chronology 20,000 to 11,000 carbon-14 years ago: some global comparisons
publisher American Association for the Advancement of Science (AAAS)
publishDate 1972
url http://dx.doi.org/10.1126/science.176.4039.1118
https://www.science.org/doi/pdf/10.1126/science.176.4039.1118
geographic Antarctic
New Zealand
The Antarctic
geographic_facet Antarctic
New Zealand
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_source Science
volume 176, issue 4039, page 1118-1120
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.176.4039.1118
container_title Science
container_volume 176
container_issue 4039
container_start_page 1118
op_container_end_page 1120
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