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Volumn 272, Issue 5269, 1996, Pages 1771-1774

Evidence for glacial control of rapid sea level changes in the early cretaceous

Author keywords

[No Author keywords available]

Indexed keywords

ICE;

EID: 0030056546     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.272.5269.1771     Document Type: Article
Times cited : (144)

References (35)
  • 2
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    • S. O. Schlanger, in Mesozoic and Cenozoic Oceans, K. Hsu, Ed (American Geophysical Union, Washington DC, 1986), pp. 61-74.
    • (1986) Mesozoic and Cenozoic Oceans , pp. 61-74
    • Schlanger, S.O.1
  • 7
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    • E. Gavish and G. Friedman, J. Sediment. Petrol. 39, 980 (1969); W H. Harris and R. K. Matthews, Science 160, 77 (1968).
    • (1968) Science , vol.160 , pp. 77
    • Harris, W.H.1    Matthews, R.K.2
  • 9
    • 15844377916 scopus 로고    scopus 로고
    • note
    • Sites 391C and 534A are located in the Blake-Bahama Basin off the coast of Florida, and site 603B is located approximately 1000 km to the northeast, off the coast of Virginia.
  • 10
    • 15744406186 scopus 로고    scopus 로고
    • note
    • 13C.
  • 12
    • 15844401443 scopus 로고    scopus 로고
    • note
    • 3, measured as acid-insoluble residue or by Ca content. Sr and Ca determinations were made in 1.0 N acetic acid dissolutions by atomic adsorption spectroscopy. Reproducibility is better than 1 % (coefficient of variation)
  • 13
    • 15844421803 scopus 로고    scopus 로고
    • H. M. Stoll and D P Schrag, data not shown
    • H. M. Stoll and D P Schrag, data not shown.
  • 15
    • 15844373582 scopus 로고    scopus 로고
    • note
    • The smoothed records reduce the maximum amplitude of the Sr increases from 120 to 80%.
  • 16
    • 15844412477 scopus 로고    scopus 로고
    • note
    • Bulk carbonate was flushed with 1.0 N ammonium acetate to remove Sr adsorbed on exchange sites. The carbonate residue was then dissolved in 1.0 N acetic acid as in (13).
  • 20
    • 15844418523 scopus 로고    scopus 로고
    • note
    • 18O. These detrended oxygen isotope data are expressed as per mil increases over the minimum value
  • 24
    • 15844376918 scopus 로고    scopus 로고
    • note
    • The effect of Ca variability on Sr partitioning is not included in the model, because the riverine-hydrothermal flux is held constant and Ca is not released during aragonite recrystallizaton. Initial Sr model concentrations are 1650 ppm for aragonite and 500 ppm for calcite.
  • 25
    • 0028181964 scopus 로고
    • D. Archer and E. Maier-Reimer, Nature 367, 260 (1994); B. N. Opdyke and J. C. G. Walker, Geology 20, 733 (1992).
    • (1994) Nature , vol.367 , pp. 260
    • Archer, D.1    Maier-Reimer, E.2
  • 26
    • 84874964971 scopus 로고
    • D. Archer and E. Maier-Reimer, Nature 367, 260 (1994); B. N. Opdyke and J. C. G. Walker, Geology 20, 733 (1992).
    • (1992) Geology , vol.20 , pp. 733
    • Opdyke, B.N.1    Walker, J.C.G.2
  • 27
    • 0023486332 scopus 로고
    • R. K Matthews and C Frohlich, Geology 15, 673 (1987). A smaller amount of total recrystallization scales with the total amount of sea level change implied by the model.
    • (1987) Geology , vol.15 , pp. 673
    • Matthews, R.K.1    Frohlich, C.2
  • 28
    • 15844432039 scopus 로고    scopus 로고
    • note
    • 18O records, inverting the result, and normalizing to a specified magnitude of sea level change.
  • 30
    • 0003756597 scopus 로고    scopus 로고
    • E. J. Barron, W. W. Hay, E G. Kauffman, Geology 12, 377 (1984); E J. Barron, ibid., p. 595.
    • Geology , pp. 595
    • Barron, E.J.1
  • 35
    • 15844392213 scopus 로고    scopus 로고
    • note
    • Supported in part by an Office of Naval Research graduate fellowship to H.M.S. Conversations with F. Richter, M. Monahan, and P. Koch were instrumental in developing this project.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.