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2
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85040879110
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K. Hsu, Ed (American Geophysical Union, Washington DC)
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S. O. Schlanger, in Mesozoic and Cenozoic Oceans, K. Hsu, Ed (American Geophysical Union, Washington DC, 1986), pp. 61-74.
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(1986)
Mesozoic and Cenozoic Oceans
, pp. 61-74
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Schlanger, S.O.1
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5
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0002741735
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A. Lerman and M. Meybeck, Eds. Kluwer, Boston, MA
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S. O. Schlanger, in Physical and Chemical Weathering in Geochemical Cycles, A. Lerman and M. Meybeck, Eds. (Kluwer, Boston, MA, 1988), pp. 323-340.
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(1988)
Physical and Chemical Weathering in Geochemical Cycles
, pp. 323-340
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Schlanger, S.O.1
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7
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0002638475
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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).
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(1968)
Science
, vol.160
, pp. 77
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-
Harris, W.H.1
Matthews, R.K.2
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9
-
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15844377916
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-
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
-
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15744406186
-
-
note
-
13C.
-
-
-
-
12
-
-
15844401443
-
-
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
-
-
H. M. Stoll and D P Schrag, data not shown
-
H. M. Stoll and D P Schrag, data not shown.
-
-
-
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15
-
-
15844373582
-
-
note
-
The smoothed records reduce the maximum amplitude of the Sr increases from 120 to 80%.
-
-
-
-
16
-
-
15844412477
-
-
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).
-
-
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17
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15844418143
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P. Baker, J. M Gieskes, H. Elderfield, J. Sediment Petrol 52, 52 (1982); F. M Richter and D. J. DePaolo, Earth Planet. Sci. Lett. 83, 27 (1987)
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(1982)
J. Sediment Petrol
, vol.52
, pp. 52
-
-
Baker, P.1
Gieskes, J.M.2
Elderfield, H.3
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18
-
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0023525096
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P. Baker, J. M Gieskes, H. Elderfield, J. Sediment Petrol 52, 52 (1982); F. M Richter and D. J. DePaolo, Earth Planet. Sci. Lett. 83, 27 (1987)
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(1987)
Earth Planet. Sci. Lett.
, vol.83
, pp. 27
-
-
Richter, F.M.1
DePaolo, D.J.2
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20
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15844418523
-
-
note
-
18O. These detrended oxygen isotope data are expressed as per mil increases over the minimum value
-
-
-
-
24
-
-
15844376918
-
-
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.
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-
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25
-
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0028181964
-
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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
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Archer, D.1
Maier-Reimer, E.2
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26
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84874964971
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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
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Opdyke, B.N.1
Walker, J.C.G.2
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27
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0023486332
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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
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Matthews, R.K.1
Frohlich, C.2
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28
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15844432039
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note
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18O records, inverting the result, and normalizing to a specified magnitude of sea level change.
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29
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0003756597
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E. J. Barron, W. W. Hay, E G. Kauffman, Geology 12, 377 (1984); E J. Barron, ibid., p. 595.
-
(1984)
Geology
, vol.12
, pp. 377
-
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Barron, E.J.1
Hay, W.W.2
Kauffman, E.G.3
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30
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0003756597
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E. J. Barron, W. W. Hay, E G. Kauffman, Geology 12, 377 (1984); E J. Barron, ibid., p. 595.
-
Geology
, pp. 595
-
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Barron, E.J.1
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35
-
-
15844392213
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note
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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.
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