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- W1973900445 abstract "Tests of phaeodarian radiolarians are composed largely of organic matter, containing only a small percentage of opaline silica in their matrix. Because of their highly organic nature, these tests are generally dissolved prior to deposition at the sediment-water interfaces of oxic environments. Anoxic environments, however, offer settings of little bioturbation and low oxygenation and may enhance phaeodarian preservation in the sediment records of anoxic locations. Recent southern California continental borderland surface sediment samples are studied in this research to provide a quantitative index of anoxia using phaeodarian surface area as a criterion. Californian Miocene and Pliocene samples have been compared to verify the index in the fossil record." @default.
- W1973900445 created "2016-06-24" @default.
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- W1973900445 date "1986-01-01" @default.
- W1973900445 modified "2023-09-26" @default.
- W1973900445 title "Phaeodarian Radiolarians as Indicators of Recent and Past (Monterey) Anoxic Environments: ABSTRACT" @default.
- W1973900445 doi "https://doi.org/10.1306/948857d2-1704-11d7-8645000102c1865d" @default.
- W1973900445 hasPublicationYear "1986" @default.
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