A New Greenland Deep Ice Core

The polar ice sheets are rich sources of information on past atmospheric conditions, including paleoclimates. A new deep ice core has been drilled in south Greenland. Comparison of the oxygen isotopic profile with that from Camp Century and with a deep-sea foraminifera record indicates that the new...

Full description

Bibliographic Details
Published in:Science
Main Authors: Dansgaard, W., Clausen, H. B., Gundestrup, N., Hammer, C. U., Johnsen, S. F., Kristinsdottir, P. M., Reeh, N.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1982
Subjects:
Online Access:http://dx.doi.org/10.1126/science.218.4579.1273
https://www.science.org/doi/pdf/10.1126/science.218.4579.1273
id craaas:10.1126/science.218.4579.1273
record_format openpolar
spelling craaas:10.1126/science.218.4579.1273 2024-10-13T14:07:38+00:00 A New Greenland Deep Ice Core Dansgaard, W. Clausen, H. B. Gundestrup, N. Hammer, C. U. Johnsen, S. F. Kristinsdottir, P. M. Reeh, N. 1982 http://dx.doi.org/10.1126/science.218.4579.1273 https://www.science.org/doi/pdf/10.1126/science.218.4579.1273 en eng American Association for the Advancement of Science (AAAS) Science volume 218, issue 4579, page 1273-1277 ISSN 0036-8075 1095-9203 journal-article 1982 craaas https://doi.org/10.1126/science.218.4579.1273 2024-09-27T04:00:46Z The polar ice sheets are rich sources of information on past atmospheric conditions, including paleoclimates. A new deep ice core has been drilled in south Greenland. Comparison of the oxygen isotopic profile with that from Camp Century and with a deep-sea foraminifera record indicates that the new core reaches back to about 90,000 years before present in a continuous sequence. The details in the Wisconsin part of the ice core records seem to be climatically significant, and the general trends reveal all of the relevant Emiliani stages recorded in deep-sea cores. The redated Camp Century record suggests a dramatic termination of the Eem/Sangamon interglacial. Article in Journal/Newspaper Greenland ice core AAAS Resource Center (American Association for the Advancement of Science) Greenland Science 218 4579 1273 1277
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description The polar ice sheets are rich sources of information on past atmospheric conditions, including paleoclimates. A new deep ice core has been drilled in south Greenland. Comparison of the oxygen isotopic profile with that from Camp Century and with a deep-sea foraminifera record indicates that the new core reaches back to about 90,000 years before present in a continuous sequence. The details in the Wisconsin part of the ice core records seem to be climatically significant, and the general trends reveal all of the relevant Emiliani stages recorded in deep-sea cores. The redated Camp Century record suggests a dramatic termination of the Eem/Sangamon interglacial.
format Article in Journal/Newspaper
author Dansgaard, W.
Clausen, H. B.
Gundestrup, N.
Hammer, C. U.
Johnsen, S. F.
Kristinsdottir, P. M.
Reeh, N.
spellingShingle Dansgaard, W.
Clausen, H. B.
Gundestrup, N.
Hammer, C. U.
Johnsen, S. F.
Kristinsdottir, P. M.
Reeh, N.
A New Greenland Deep Ice Core
author_facet Dansgaard, W.
Clausen, H. B.
Gundestrup, N.
Hammer, C. U.
Johnsen, S. F.
Kristinsdottir, P. M.
Reeh, N.
author_sort Dansgaard, W.
title A New Greenland Deep Ice Core
title_short A New Greenland Deep Ice Core
title_full A New Greenland Deep Ice Core
title_fullStr A New Greenland Deep Ice Core
title_full_unstemmed A New Greenland Deep Ice Core
title_sort new greenland deep ice core
publisher American Association for the Advancement of Science (AAAS)
publishDate 1982
url http://dx.doi.org/10.1126/science.218.4579.1273
https://www.science.org/doi/pdf/10.1126/science.218.4579.1273
geographic Greenland
geographic_facet Greenland
genre Greenland
ice core
genre_facet Greenland
ice core
op_source Science
volume 218, issue 4579, page 1273-1277
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.218.4579.1273
container_title Science
container_volume 218
container_issue 4579
container_start_page 1273
op_container_end_page 1277
_version_ 1812814130102403072