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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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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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 |
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Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
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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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1811632800962445312 |