986 resultados para Moreau, William B.
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Radiocarbon ages on CaCO3 from deep-sea cores offer constraints on the nature of the CaCO3 dissolution process. The idea is that the toll taken by dissolution on grains within the core top bioturbation zone should be in proportion to their time of residence in this zone. If so, dissolution would shift the mass distribution in favor of younger grains, thereby reducing the mean radiocarbon age for the grain ensemble. We have searched in vain for evidence supporting the existence of such an age reduction. Instead, we find that for water depths of more than 4 km in the tropical Pacific the radiocarbon age increases with the extent of dissolution. We can find no satisfactory steady state explanation and are forced to conclude that this increase must be the result of chemical erosion. The idea is that during the Holocene the rate of dissolution of CaCO3 has exceeded the rain rate of CaCO3. In this circumstance, bioturbation exhumes CaCO3 from the underlying glacial sediment and mixes it with CaCO3 raining from the sea surface.
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Accelerator mass spectrometer 14C dated stable isotope data from Neogloboquadrina pachyerma in cores raised from the Mendeleyev Ridge and slope provide evidence for significant influx of meltwater to the western Arctic Ocean during the early part of marine oxygen isotope stage 1 (OIS 1) and during several intervals within OIS 3. The strongest OIS 3 meltwater event occurred before ca. 45 ka (conventional radiocarbon age) and was probably related to the deglaciation at the beginning of OIS 3. Major meltwater input to the western Arctic Ocean during the last deglaciation coincides closely with the maximum rate of global sea-level rise as determined from the Barbados sea-level record, demonstrating a strong link between the global record and changes in the central Arctic Ocean. OIS 2, which includes the last glacial maximum, is very condensed or absent in the cores. Abundance and d13C values for N. pachyderma in the middle part of OIS 3 are similar to modern values, indicating high productivity and seasonal ice-free areas along the Arctic margin at that time. These records indicate that the Arctic Ocean was a source of heat and moisture to the northern polar atmosphere during parts of OIS 3.
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Microform.
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"Prepared June 1979."
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Mode of access: Internet.
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Cover title: Introductory address delivered before the Young Men's Association of Albany on the evening of December 4, 1838, by William B. Sprague.
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The historical portion of this work is by W.B. Vickers--Cf. Pref.
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An issue for 1886 appears in their Prices of railroad stocks for thirty-two years, under title: Hand-book of railroad securities.
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Cover title: Pauper abstract for 1848.
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Editors: Sept. 1897-Sept. 1900, Charles Francis Browne; Oct. 1900-May 1907, Frederick W. Morton.
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"The work of preparing this volume was done by Rees H. Davis, of the Cleveland Bar, working under the direction of William B. Woods, director of law of the city, and with the assistance of L. E. Carter, director of the Bureau of municipal research, and J. C. Mansfield, assistant director of law."--Pref., p. [3]
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Includes index.
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Mode of access: Internet.
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"This is the sixth revision of the ordinances of the city of Jackson"--Pref.