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- W137304501 abstract "This article outlines the history of marine laminated sediment research and then focuses on the nature of diatom records from Quaternary laminated marine sediments. Laminated marine diatom ooze accumulates under conditions of varying supply of different sedimentary components such as diatom frustules and terrigenous grains, in areas where the dissolved oxygen concentrations in the bottom waters are almost depleted and preclude the active, bioturbating fauna. This facilitates the preservation of the seasonal succession of surface water diatom blooms, as promoted by processes such as coastal upwelling, and water column stratification and subsequent collapse. These seasonally laminated sediments, or marine varves, record information about oceanographic and climatic processes over subannual to millennial timescales, from locations such as semienclosed seas (e.g., Gulf of California, NW Mexico), silled basins (e.g., Santa Barbara Basin, California margin and Iceberg Alley, MacRobertson Shelf, Antarctica), and the open continental margin (e.g., Peru margin). Quaternary laminated diatom ooze also accumulates in the deep sea in well-oxygenated waters but beneath convergent oceanic frontal systems, such as in the South Atlantic associated with the Polar Front Zone. Here, the presence or absence of the laminated diatom mat deposits reflects the movement of major oceanic frontal systems over glacial to interglacial timescales." @default.
- W137304501 created "2016-06-24" @default.
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- W137304501 date "2013-01-01" @default.
- W137304501 modified "2023-10-12" @default.
- W137304501 title "DIATOM RECORDS | Diatom Fossil Records from Marine Laminated Sediments" @default.
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- W137304501 doi "https://doi.org/10.1016/b978-0-444-53643-3.00226-0" @default.
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