Strong summer monsoon during the cool MIS-13
The δ 18 O record in deep-sea sediments show a significant reduced amplitude of the ice volume variations before Marine Isotope Stage 11, about 400 ka ago, with less warm interglacials and less cold glacials. The deuterium temperature and the greenhouse gases records in the Antarctic ice cores show...
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Language: | English |
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Online Access: | https://www.vliz.be/imisdocs/publications/315241.pdf |
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ftvliz:oai:oma.vliz.be:296166 2023-05-15T13:54:11+02:00 Strong summer monsoon during the cool MIS-13 Yin, Q.Z. Guo, Z.T. 2008 application/pdf https://www.vliz.be/imisdocs/publications/315241.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000253673000004 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.5194/cp-4-29-2008 https://www.vliz.be/imisdocs/publications/315241.pdf info:eu-repo/semantics/openAccess %3Ci%3EClim.+Past+4%281%29%3C%2Fi%3E%3A+29-34.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.5194%2Fcp-4-29-2008%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.5194%2Fcp-4-29-2008%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2008 ftvliz https://doi.org/10.5194/cp-4-29-2008 2022-05-01T11:00:50Z The δ 18 O record in deep-sea sediments show a significant reduced amplitude of the ice volume variations before Marine Isotope Stage 11, about 400 ka ago, with less warm interglacials and less cold glacials. The deuterium temperature and the greenhouse gases records in the Antarctic ice cores show the same feature. As the reduction in the amplitude of climate and greenhouse gases concentration variations before 400 ka BP is present in both deep-sea and ice cores, it is tempting to conclude that this is a worldwide phenomenon. This is not necessarily true, at least as far as some of the records, in particular of China and Europe, are concerned. The loess in northern China, the sedimentary core in the eastern Tibetan Plateau and the palaeosols in southern China all record an unusually warm and wet climate during Marine Isotope Stage 13, indicating an extremely strong East Asian summer monsoon. The pollen record from Europe shows that the climatic conditions during the interglacials previous to Marine Isotope Stage 11 are at least as warm as the younger interglacials. During Marine Isotope Stage 13, unusually strong African and Indian monsoon are recorded in the sediments of the equatorial Indian Ocean and of the Mediterranean Sea. Other extreme climate events are also recorded in sediment cores of the equatorial Atlantic, the Pacific, the subtropical South Atlantic Ocean and in the Lake Baikal of Siberia. Article in Journal/Newspaper Antarc* Antarctic South Atlantic Ocean Siberia Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) Antarctic Indian Pacific The Antarctic Climate of the Past 4 1 29 34 |
institution |
Open Polar |
collection |
Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) |
op_collection_id |
ftvliz |
language |
English |
description |
The δ 18 O record in deep-sea sediments show a significant reduced amplitude of the ice volume variations before Marine Isotope Stage 11, about 400 ka ago, with less warm interglacials and less cold glacials. The deuterium temperature and the greenhouse gases records in the Antarctic ice cores show the same feature. As the reduction in the amplitude of climate and greenhouse gases concentration variations before 400 ka BP is present in both deep-sea and ice cores, it is tempting to conclude that this is a worldwide phenomenon. This is not necessarily true, at least as far as some of the records, in particular of China and Europe, are concerned. The loess in northern China, the sedimentary core in the eastern Tibetan Plateau and the palaeosols in southern China all record an unusually warm and wet climate during Marine Isotope Stage 13, indicating an extremely strong East Asian summer monsoon. The pollen record from Europe shows that the climatic conditions during the interglacials previous to Marine Isotope Stage 11 are at least as warm as the younger interglacials. During Marine Isotope Stage 13, unusually strong African and Indian monsoon are recorded in the sediments of the equatorial Indian Ocean and of the Mediterranean Sea. Other extreme climate events are also recorded in sediment cores of the equatorial Atlantic, the Pacific, the subtropical South Atlantic Ocean and in the Lake Baikal of Siberia. |
format |
Article in Journal/Newspaper |
author |
Yin, Q.Z. Guo, Z.T. |
spellingShingle |
Yin, Q.Z. Guo, Z.T. Strong summer monsoon during the cool MIS-13 |
author_facet |
Yin, Q.Z. Guo, Z.T. |
author_sort |
Yin, Q.Z. |
title |
Strong summer monsoon during the cool MIS-13 |
title_short |
Strong summer monsoon during the cool MIS-13 |
title_full |
Strong summer monsoon during the cool MIS-13 |
title_fullStr |
Strong summer monsoon during the cool MIS-13 |
title_full_unstemmed |
Strong summer monsoon during the cool MIS-13 |
title_sort |
strong summer monsoon during the cool mis-13 |
publishDate |
2008 |
url |
https://www.vliz.be/imisdocs/publications/315241.pdf |
geographic |
Antarctic Indian Pacific The Antarctic |
geographic_facet |
Antarctic Indian Pacific The Antarctic |
genre |
Antarc* Antarctic South Atlantic Ocean Siberia |
genre_facet |
Antarc* Antarctic South Atlantic Ocean Siberia |
op_source |
%3Ci%3EClim.+Past+4%281%29%3C%2Fi%3E%3A+29-34.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.5194%2Fcp-4-29-2008%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.5194%2Fcp-4-29-2008%3C%2Fa%3E |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/000253673000004 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.5194/cp-4-29-2008 https://www.vliz.be/imisdocs/publications/315241.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/cp-4-29-2008 |
container_title |
Climate of the Past |
container_volume |
4 |
container_issue |
1 |
container_start_page |
29 |
op_container_end_page |
34 |
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1766259869426384896 |