Sediment reveals Early Holocene climate change in China
1996
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Sediment reveals Early Holocene climate change in China
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1996
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EOS (American Geophysical Union)
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Abstract
A major question regarding paleorecords is whether the easy-to-acquire oceanic record can be validated by continental proxy records that are available only from the Arctic and Antarctic ice cores. The ice core records may not provide a complete record of the changes that have occurred in the temperate and tropical regions of the continents. Thick (100–300 m) deposits of wind-borne dust in China are providing new insight into paleoclimate. These deposits vie with the ice cores in providing a record of continuous accumulation over the last 2.6 m.y., but they are poorer in temporal resolution than the ice cores.
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10.1029/95EO00004
Previously Published Citation
Banerjee, S. K. (1996). "Sediment reveals Early Holocene climate change in China." Eos, Transactions of the American Geophysical Union 77: 3, 1-5.
Suggested citation
Banerjee, Subir. (1996). Sediment reveals Early Holocene climate change in China. Retrieved from the University Digital Conservancy, 10.1029/95EO00004.
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