925 resultados para Harding, Warren G. (Warren Gamaliel), 1865-1923


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Variations in the stable isotopic composition of benthic foraminifera from Deep-Sea Drilling Project (DSDP) site 502B in the Caribbean Sea are used to reconstruct Atlantic intermediate water circulation variability over the last 1.2 m.y. Comparison of this record with other North Atlantic benthic isotope records indicates that Atlantic intermediate water circulation was relatively enhanced during glacial maxima when North Atlantic deep water (NADW) production was reduced. However, a simple, compensatory relationship between intermediate and deepwater circulation is not apparent. Geochemical models have shown that such changes in ocean circulation can affect atmospheric CO2 levels by changing vertical nutrient and alkalinity profiles. The Delta delta13C difference between Caribbean site 502B and deep equatorial Pacific site 677 is highly coherent and in phase with ice volume. Like the delta18O record, there is an increase in amplitude (40%) and a large increase in 100 kyr power after 0.7 Ma. The 1.2? Delta delta13C amplitude scales to 70 ppm V in atmospheric CO2 using Boyle's (1986) box model result. The implied increase in CO2 amplitude after 0.7 Ma may suggest a positive feedback role in effecting the higher-amplitude climatic fluctuations which characterize the last 0.7 m.y.

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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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Front Row, Left to Right: Paul A. Attar, Michael G. Reissing, Steven D. Thrasher, captain John H. Dumont, Stanley C. (Pete) Cox, Richard F. Nelson.

Second Row: Warren G. Uhler, Roy D. Burry, John Candler, Thomas Burns, Andrew Paterson, Patrick Faul, Jon W. Lundin.,

Back Row: swimming coach Gus Stager, Stephen Selander, Frederick R. Damm, Dennis J. Fitzgerald, Richard Abineri, Jerry Traver, diving coach Dick Kimball.

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"Monitoring Systems Research and Development Division, Environmental Monitoring and Support Laboratory."

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Mode of access: Internet.

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"Third edition, revized, with additions and in simplified spelling, February, 1919."

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Mode of access: Internet.

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Three preludes and fugues, op. 37 -- Six sonatas, op. 65.

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Federal Highway Administration, Traffic Systems Division, Washington, D.C.

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Federal Highway Administration, Office of Safety and Traffic Operations Research and Development, Washington, D.C.

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Mode of access: Internet.