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- W2022982487 abstract "Laminated, diatomaceous sediments of the Gulf of California consist of regularly alternating light-colored (diatom-rich) and dark-colored (clay-rich) laminae, approximately 2 mm. thick. The mean contents of opal (as diatom frustules) and quartz in the laminae, determined by X-ray diffraction methods, are: light-colored laminae, 52.4 per cent opal and 7.0 per cent quartz; dark-colored laminae, 26.5 per cent opal and 10.0 per cent quartz. The laminae cannot be distinguished on the basis of the contained diatom assemblages, only on the total contents of biogenous and terrigenous materials. Rates of deposition, determined by radiocarbon dating of organic and carbonate carbon in selected core sections, demonstrate that one light-colored lamina and one dark-colored lamina are deposited in a year, and a couplet of laminae constitute a varve. Phytoplankton production in the central Gulf of California is reasonably constant throughout the year, but river discharge fluctuates greatly during a year as a result of to..." @default.
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- W2022982487 date "1966-09-01" @default.
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- W2022982487 title "Origin of Diatom-Rich, Varved Sediments from the Gulf of California" @default.
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- W2022982487 doi "https://doi.org/10.1086/627188" @default.
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