Planktonic foraminifera and microfossil composition of IODP Hole 302-M0004C ...
Calcareous microfossils are widely used by paleoceanographers to investigate past sea-surface hydrology. Among these microfossils, planktonic foraminifera are probably the most extensively used tool (e.g. [1] for a review), as they are easy to extract from the sediment and can also be used for coupl...
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Format: | Dataset |
Language: | English |
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PANGAEA
2011
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Online Access: | https://dx.doi.org/10.1594/pangaea.788078 https://doi.pangaea.de/10.1594/PANGAEA.788078 |
Summary: | Calcareous microfossils are widely used by paleoceanographers to investigate past sea-surface hydrology. Among these microfossils, planktonic foraminifera are probably the most extensively used tool (e.g. [1] for a review), as they are easy to extract from the sediment and can also be used for coupled geochemical (e.g; d18O, d13C, Mg/Ca) and paleo-ecological investigations. Planktonic foraminifera are marine protists, which build a calcareous shell made of several chambers which reflect in their chemistry the properties of the ambient water-masses. Planktonic foraminifera are known to thrive in various habitats, distributed not only along a latitudinal gradient, but also along different water-depth intervals within surface waters (0-1000 m). Regarding their biogeographical distribution, planktonic foraminifera assemblages therefore mirror different water-masses properties, such as temperature, salinity and nutrient content of the surface water in which they live. The investigation of the specific composition ... : AGE, sediment [m] gives the original top mbsf of a sample. AGE [ka BP] is the oregan age (11-30-06) fichier Shannon. ... |
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