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Автор Rea, David K.
Автор Chambers, Lucy W.
Автор Chuey, John M.
Автор Janecek, Thomas R.
Автор Leinen, Margaret
Автор Pisias, Nicklas G.
Дата выпуска 1986
dc.description Samples from the upper portion of a cyclic pelagic carbonate sediment sequence in Deep‐Sea Drilling Project (DSDP) hole 503B (4.0°N, 95.6°W) are the first group to be analyzed for paleoceanographic and paleoclimatic proxy‐indicators of ice volume, deep ocean and surface water circulation, and atmospheric circulation in order to resolve the complex origin of the cyclicity. Temporal resolution is taken from the δ<sup>18</sup>O time scale, most other parameters are calculated in terms of their mass flux to the seafloor. CaCO<sub>3</sub> percent in the sediments fluctuates in the well‐known Pacific pattern and is higher during glacial times. The fluxes of opal and organic carbon have patterns similar to each other and show a variability of a factor of 2.5 to 4. The longer organic carbon record shows flux maxima during both glacial and interglacial times. The accumulation patterns of both opal and organic carbon suggest that the variability in surface water productivity and/or seafloor preservation of those materials is not simply correlated to glacial or interglacial periods. Eolian dust fluxes are greater during interglacial periods by factors of 2 to 5, indicating that eolian source regions in central and northern South America were more arid during interglacial periods. The record of eolian grain size provides a semiquantitative estimation of the intensity of the transporting winds. The eolian data suggest more intense atmospheric circulation during interglacial periods, opposite to the anticipated results. We interpret this observation as recording the southerly shift of the intertropical convergence zone to the latitude of hole 503B during glaciations.
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Копирайт Copyright 1986 by the American Geophysical Union.
Тема Milankovitch Cycles Through Geologic Time
Тема OCEANOGRAPHY: GENERAL
Тема 4267
Название A 420,000‐year record of cyclicity in oceanic and atmospheric processes from the eastern equatorial Pacific
Тип article
DOI 10.1029/PA001i004p00577
Electronic ISSN 1944-9186
Print ISSN 0883-8305
Журнал Paleoceanography
Том 1
Первая страница 577
Последняя страница 586
Выпуск 4
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