[PDF.67xg] Biogeochemical Controls on Palaeoceanographic Environmental Proxies - Special Publication no 303 (Geological Society Special Publication)

Biogeochemical Controls on Palaeoceanographic Environmental Proxies - Special Publication no 303 (Geological Society Special Publication)

[PDF.gl39] Biogeochemical Controls on Palaeoceanographic Environmental Proxies - Special Publication no 303 (Geological Society Special Publication)

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 | #7030350 in Books |  2008-10-15 | Original language:English |  9.75 x6.75 x.75l,1.50 | File type: PDF | 356 pages

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Most of our information about the evolution of Earth's ocean-climate system comes from the analysis of sediments laid down in the past. For example, the microfossil assemblage reflects the temperature, salinity and nutrient abundance of the water in which the organisms lived, while the chemical and isotopic composition of biogenic carbonates may be used to reconstruct past variations in the operation of the carbon cycle, as well as changes in ocean circulation.

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