Holocene--Late Pleistocene Climatic Ice Core Records from Qinghai-Tibetan Plateau

Three ice cores to bedrock from the Dunde ice cap on the north-central Qinghai-Tibetan Plateau of China provide a detailed record of Holocene and Wisconsin-Wurm late glacial stage (LGS) climate changes in the subtropics. The records reveal that LGS conditions were apparently colder, wetter, and dust...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 1989-10, Vol.246 (4929), p.474-477
Hauptverfasser: Thompson, L. G., Mosley-Thompson, E., Davis, M. E., Bolzan, J. F., Dai, J., Yao, T., Gundestrup, N., Wu, X., Klein, L., Xie, Z.
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container_end_page 477
container_issue 4929
container_start_page 474
container_title Science (American Association for the Advancement of Science)
container_volume 246
creator Thompson, L. G.
Mosley-Thompson, E.
Davis, M. E.
Bolzan, J. F.
Dai, J.
Yao, T.
Gundestrup, N.
Wu, X.
Klein, L.
Xie, Z.
description Three ice cores to bedrock from the Dunde ice cap on the north-central Qinghai-Tibetan Plateau of China provide a detailed record of Holocene and Wisconsin-Wurm late glacial stage (LGS) climate changes in the subtropics. The records reveal that LGS conditions were apparently colder, wetter, and dustier than Holocene conditions. The LGS part of the cores is characterized by more negative $\delta ^{18}$O ratios, increased dust content, decreased soluble aerosol concentrations, and reduced ice crystal sizes than the Holocene part. These changes occurred rapidly $\sim $10,000 years ago. In addition, the last 60 years were apparently one of the warmest periods in the entire record, equalling levels of the Holocene maximum between 6000 and 8000 years ago.
doi_str_mv 10.1126/science.246.4929.474
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source Science Magazine; JSTOR Archive Collection A-Z Listing
subjects Bedrock
Cations
Climate models
Crystals
Glaciers
Ice
Ice caps
Ice cores
Paleoclimatology
Subtropics
title Holocene--Late Pleistocene Climatic Ice Core Records from Qinghai-Tibetan Plateau
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