Wang Pinxian (2003): Prediction of the next glaciation; a controversial issue

Leg/Site/Hole:
ODP 184
ODP 184 1143
Identifier:
2009-026934
georefid

Creator:
Wang Pinxian
Tongji University, Laboratory of Marine Geology, Shanghai, China
author

Identification:
Prediction of the next glaciation; a controversial issue
2003
Haiyang Dizhi yu Disiji Dizhi = Marine Geology & Quaternary Geology
Science Press, Beijing, China
23
1
1-6
This paper briefly reviews how the prediction of the next glaciation has been evolving in the scientific community and why the viewpoints are so divergent. The key to the scientific prediction of the next glaciation lies in the understanding of specific features of the present and future orbital forcing, and of the mechanisms of carbon cycling. The recent discovery of periodic occurrences of delta (super 13) Cmax over the last 5 Ma in the deep-sea sequence at ODP Site 1143 in the southern South China Sea indicates that long-term changes in carbon reservoirs on Earth have their own periodicity and their own history, and do not simply follow ice cap variations. Because disturbances in carbon reservoirs lead to major growth in the size of ice sheets, and because the Earth is now passing through a delta (super 13) Cmax episode, it is crucial to understand the causal relationship between successive delta (super 13) C changes and ice sheet growth events.
Chinese
Serial
Coverage:Geographic coordinates:
North:9.2143
West:113.1707East: 113.1707
South:9.2143

Quaternary geology; C-13/C-12; carbon; carbon cycle; Cenozoic; Foraminifera; geochemical cycle; geochemical indicators; glacial geology; glaciation; ice caps; ice sheets; Invertebrata; isotope ratios; isotopes; Leg 184; microfossils; Milankovitch theory; North Pacific; Northwest Pacific; Ocean Drilling Program; ODP Site 1143; Pacific Ocean; prediction; Protista; Quaternary; South China Sea; stable isotopes; upper Quaternary; West Pacific;

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