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Volumn 274, Issue 5289, 1996, Pages 943-948

Nonstationary phase of the plio-pleistocene Asian monsoon

Author keywords

[No Author keywords available]

Indexed keywords

RAIN;

EID: 0029659190     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.274.5289.943     Document Type: Article
Times cited : (284)

References (62)
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    • 18O over the past 3.5 Ma at Site 722. This result agrees with those previously published for Site 659 over the interval 0.5 to 3.5 Ma (34). Our analysis suggests a zero phase relation at the precession band and a ∼2-ky lead over the obliquity band. Retaining the phase of ice at Late Pleistocene values relative to orbits (40) (6-ky lead for precession, 11.4-ky lead for obliquity), we constructed a tuning target by normalizing tilt and precession (3-4), applying the measured phase relations (11.4 + 2 = 13,4 ky for obliquity and 6 + 0 = 6 ky for precession), and averaging the two records. Site 722 lithogenic % maxima were then correlated directly to maxima in the tuning target.
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    • Our analysis of the eccentricity band yielded no interpretable results with respect to monsoon strength although some Late Pleistocene records indicate significant concentrations of variance at the 100-ky band (26, 56, 57). Our findings regarding regional aridity differ little from previously published results (29, 30, 33-35, 47).
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    • 18O data (G. sacculifer) over the intervals 3.4 to 3.73 Ma and 4.2 to 4.5 Ma indicate in-phase relations.
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    • note
    • Supported by the Ocean Science Division of the NSF and JOI/USSSP. Samples were provided by the international Ocean Drilling Program. Technical assistance was provided by L. Nik, J. Cook, and A. Martin. We thank F. Sirocko and R. Tiedemann for valuable comments and constructive criticisms.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.