Matches in SemOpenAlex for { <https://semopenalex.org/work/W3021795146> ?p ?o ?g. }
- W3021795146 abstract "Occupying more than 70% of the Earth’s surface, the oceans are a very important source of paleoclimatic information. Between 6 and 11 billion metric tons of sediment accumulate in the ocean basins annually, and this provides an archive of climatic conditions near the ocean surface or on the adjacent continents. Sediments are composed of both biogenic and terrigenous materials. The biogenic component includes the remains of planktic (near surface-dwelling) and benthic (bottom-dwelling) organisms, which provide a record of past climate and oceanic circulation, in terms of surface water temperature and salinity, dissolved oxygen in deep water, nutrient or trace element concentrations, etc. By contrast, the nature and abundance of terrigenous material mainly provide a record of humidity-aridity variations on the continents, or the intensity and direction of winds blowing from land areas to the oceans, and other modes of sediment transport to, and within, the oceans (fluvial erosion, ice-rafting, turbidity currents, etc.). Marine sediments also contain biomarkers (organic molecules derived from terrestrial or marine organisms), which can be useful proxies of paleoceanographic conditions or of paleoenvironmental conditions on the adjacent continents." @default.
- W3021795146 created "2020-05-13" @default.
- W3021795146 creator A5049614402 @default.
- W3021795146 date "2015-01-01" @default.
- W3021795146 modified "2023-09-23" @default.
- W3021795146 title "Marine Sediments" @default.
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