dcsimg

Stylacontarium bispiculum is a species of radiolarians in the family Actinommidae. Dead Stylacontarium bispiculum form siliceous oozes.

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  • URI: http://purl.obolibrary.org/obo/ENVO_02000044
  • Definition: Siliceous ooze is a marine sediment composed of the debris of plankton with silica shells, such as diatoms and radiolaria. This ooze is limited to areas with high biological productivity, such as the polar oceans, and upwelling zones near the equator. The least common type of sediment, it covers only 15% of the ocean floor. It accumulates at a slower rate than calcareous ooze: 0.2-1 cm / 1000 yr.
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EOL has data for 18 attributes, including:

Known occurrences, collected specimens and observations of Stylacontarium bispiculum Popofsky 1912. View this species on GBIF