Mid-Holocene palaeoceanography of the northern South China Sea using coupled fossil-modern coral and atmosphere-ocean GCM model-Reference-Cited by-同舟云学术

Mid-Holocene palaeoceanography of the northern South China Sea using coupled fossil-modern coral and atmosphere-ocean GCM model

Published:2011-01-15 Issue:8 Volume:38 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Yokoyama Yusuke¹²³,Suzuki Atsushi⁴,Siringan Fernando⁵,Maeda Yasuo⁶,Abe-Ouchi Ayako¹⁷,Ohgaito Rumi⁷,Kawahata Hodaka¹,Matsuzaki Hiroyuki⁸

Affiliation:

1. Department of Ocean Floor Geoscience and Center for Earth Surface System Dynamics, Atmosphere and Ocean Research Institute; University of Tokyo; Kashiwa Japan

2. Department of Earth and Planetary Sciences; University of Tokyo; Tokyo Japan

3. Institute of Biogeosciences; Japan Agency for Marine-Earth Science and Technology; Yokosuka Japan

4. Geological Survey of Japan; National Institute of Advanced Industrial Science and Technology; Tsukuba Japan

5. Marine Science Institute; University of Philippines; Quezon City Philippines

6. Institute of Natural and Environmental Sciences; University of Hyogo; Sanda Japan

7. Research Institute for Global Change; Japan Agency for Marine-Earth Science and Technology; Yokohama Japan

8. Department of Nuclear Engineering and Management, School of Engineering; University of Tokyo; Tokyo Japan

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/gl1101/2010GL044231/2010GL044231.pdf

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4. Stable isotopes in a branching coral monitor seasonal temperature variation;Dunbar;Nature,1981

5. Mean oxygen isotope signatures in Porites spp. corals: Inter-colony variability and correction for extension-rate effects;Felis;Coral Reefs,2003

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