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Volumn 304, Issue 5670, 2004, Pages 575-578

Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon

Author keywords

[No Author keywords available]

Indexed keywords

GLACIERS; ISOTOPES; OXYGEN; PRECIPITATION (METEOROLOGY); THORIUM;

EID: 11144355914     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1091220     Document Type: Article
Times cited : (1059)

References (38)
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    • note
    • Oxygen isotope analyses were performed at the Isotope Laboratory, Institute of Karst Geology, Guilin, China, using a VG MM-903 gas mass spectrometer (for Dongge Cave D3 and D4 analyses, except for D4 between 15.81 ky and 9.98 ky); at the State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Xi'an, China, using a Finnigan MAT 252 Kiel Device III (Dongge Cave D4 between 15.81 and 9.98 ky); and on a Finnigan MAT 251 at the Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences (Hulu Cave H82 between 15.34 and 16.30 ky before the present). Other H82 analyses were reported earlier in (3).
  • 10
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    • note
    • 2 value for any of the three stalagmites is 0.27 (table S6). Because the top of D4 was deposited in isotopic equilibrium and because a portion of D4 replicates the Hulu record, D4 is less likely to have been affected by kinetic effects or water/rock interactions than D3.
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    • note
    • VPDB = -4. 5‰ and temperature 4°C. (VPDB, Vienna Pee Dee belemnite standard.)
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    • note
    • We especially thank G. Comer and W. S. Broecker for their tremendous and generous support of our work. We thank H. Wang, Y. Fong, and L. Tu for stable isotope analyses and Y. Xie, S. He, J. Cao, Z. Wang, J. Zhan, and D. Yu for assistance with fieldwork. Supported by NSF grants ESH0214041, ESH9809459, and MR10116395; a Comer Science and Education Foundation Grant (CC8); National Science Foundation of China grants 40328005 and 40231008; and grants from the Ministry of Land and Resources and the Ministry of Science and Technology of China.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.