Correspondence between the ENSO-like state and glacial-interglacial condition during the past 360 kyr-Reference-Cited by-同舟云学术

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Correspondence between the ENSO-like state and glacial-interglacial condition during the past 360 kyr

Published:2016-10-21 Issue:5 Volume:35 Page:1018-1031
ISSN:0254-4059
Container-title:Chinese Journal of Oceanology and Limnology
language:en
Short-container-title:Chin. J. Ocean. Limnol.

Author:

Zhang Shuai,Li Tiegang,Chang Fengming,Yu Zhoufei,Xiong Zhifang,Wang Haixia

Publisher

Springer Science and Business Media LLC

Subject

Water Science and Technology,Oceanography

Link

http://link.springer.com/article/10.1007/s00343-017-6082-9/fulltext.html

Reference94 articles.

1. An Z S. 2000. The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews, 19 (1-5): 171–187.

2. Anand P, Elderfield H, Conte M H. 2003. Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series. Paleoceanography, 18(2):1050.

3. Andreasen D J, Ravelo A C. 1997. Tropical Pacific ocean thermocline depth reconstructions for the last glacial maximum. Paleoceanography, 12 (3): 395–413.

4. Barker S, Greaves M, Elderfield H. 2003. A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry. Geochemistry, Geophysics, Geosystems, 4(9):8407.

5. Beaufort L, de Garidel-Thoron T, Mix A C, Pisias N G. 2001. ENSO-like forcing on oceanic primary production during the Late Pleistocene. Science, 293(5539):2440–2444.

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