890 resultados para cubic boron nitride
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The pH of the surface ocean is a sensitive function of its alkalinity and total inorganic carbon concentration, properties which also control the partial pressure of atmospheric carbon dioxide (Broecker and Peng, 1982). Thus, an accurate proxy for past ocean pH could yield information about variations in atmospheric CO2. Recently, it has been suggested that the boron isotopic composition of foraminiferal tests depends on the pH of sea water as well as its isotopic composition (Vengosh et al., 1991, doi:10.1016/0016-7037(91)90139-V; Hemming and Hanson, 1992, doi:10.1016/0016-7037(92)90151-8). Here we present boron isotope and elemental data for sedimentary pore fluids and isotope data for bulk foraminiferal samples from a deep-sea sediment core. The composition of the pore waters implies that sea water boron concentrations and isotopic composition have been constant during the past 21 Myr, allowing us to reconstruct past ocean pH directly from the foraminiferal isotope data. We find that 21 Myr ago, surface ocean pH was only 7.4 ±0.2, but it then increased to 8.2 ±0.2 (roughly the present value) about 7.5 Myr ago. This is consistent with suggestions (Popp et al., 1989; Cerling, 1991; Arthur et al., 1991) that atmospheric CO2 concentrations may have been much higher 21 Myr ago than today.
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"January 1959."
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"LADC 60"
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"Work Performed Under Contract No. AC02-77CH00178."
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In this paper our method is critically examined to obtain a better understanding of the complexities of the system.
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"U.S. Atomic Energy Commission Contract AT(29-1)-1106."
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"U.S. Atomic Energy Commission Contract AT(29-1)-1106."
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Work done by the National Bureau of Standards, Washington, D.C.
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Includes bibliographical references.
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"Date Distributed: October 13, 1960."
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On cover: AEC research and development report.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.