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Volumn 274, Issue 5294, 1996, Pages 1867-1870

Forcing of Atlantic equatorial and subpolar millennial cycles by precession

Author keywords

[No Author keywords available]

Indexed keywords

ALGA; ARTICLE; ATLANTIC OCEAN; CLIMATE; GEOGRAPHY; MARINE ENVIRONMENT; PRIORITY JOURNAL; SCIENCE;

EID: 0030303362     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.274.5294.1867     Document Type: Article
Times cited : (190)

References (37)
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    • Test of symmetry of a random variable Y about a point c. If we assume that Y has a frequency function p, then symmetry about c is p(Y + c) = p(Y - c). P. J. Bickel and K. A. Doksum, Mathematical Statistics (Holden-Day, Oakland, CA, 1977).
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    • note
    • Calendric chronology of cores RC2402 and RC2408 yields eight peak-to-peak intervals having a range of 8.1 to 9.0 ky, with a mean of 8.43 ky.
  • 24
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    • note
    • 14C chronology ranges from ±30 to ±420 for dated samples, but for interpolated values we consider that these estimates could be larger as a result of variation in sedimentation rate. However, in RC2408, F. profunda maxima were either directly AMS-dated or have dates closely allied with them. Calendric conversion yields 2σ errors ranging from ±35 to ±450. We found that the extreme case for the oldest peak-to-peak interval for conversion (15), using a minus error for the younger peak and a plus error for the older peak, is 8.75 ky. The estimate of the oldest interval for conversion (76) is 9.3 ky.
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    • S. P. Harrison et al., Quat. Res. 45, 138 (1996); S. O. Dahl and A. Nesje, Holocene 3, 269 (1993). Increased precipitation is inferred from changes in vegetation and lake levels and glacial accretion on the continents adjacent to the subpolar North Atlantic after 5 ka.
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    • S. P. Harrison et al., Quat. Res. 45, 138 (1996); S. O. Dahl and A. Nesje, Holocene 3, 269 (1993). Increased precipitation is inferred from changes in vegetation and lake levels and glacial accretion on the continents adjacent to the subpolar North Atlantic after 5 ka.
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    • note
    • We thank M. Yarusinski for assistance. Supported by NSF [MG&G grant OCE93-13821 (95%)], and NSF OCE801015 AMS/National Ocean Sciences Accelerator Mass Spectrometry Facility. This is Lamont-Doherty Earth Observatory contribution 5579.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.