Paleoenvironmental and paleoclimatic changes based on microfossils in marine sediments –an example since the last interglacial around Japan–
Author:
Affiliation:
1. Atsubetsu-kita 3-5-18-2, Atsubetsu-ku, Sapporo 004-0073, Japan.
Publisher
The Geological Society of Japan
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
Link
https://www.jstage.jst.go.jp/article/geosoc/115/7/115_7_311/_pdf
Reference34 articles.
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2. Barron, J.A., 1998, Late Neogene changes in diatom sedimentation in the North Pacific. Jour. Asian Earth Sci., 16, 85-95.
3. Beaufort, L., de Garidel-Thoron, T., Mix, A.C. and Pisias, N.G., 2001, ENSO-like forcing on oceanic primary production during the late Pleistocene. Science, 293, 2440-2444.
4. Birchfield, G.E. and Gurmbine, R.W., 1985, “Slow” physics of large continental ice sheets, the underlying bedrock and the Pleistocene Ice Ages. Jour. Geophys. Res., 90, 11294-11302.
5. Berggren, W.A., 1998, The Cenozoic Era: Lyellian (chron) stratigraphy and nomenclatural Reform at the millennium. In Blundell, D.J., Scott, A.C., eds., The Past is the Key to the Present, Geol. Soc., London, Special Pub., 143, 111-132.
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