A synthesis of marine sediment core δ13C data over the last 150 000 years
The isotopic composition of carbon, δ13C, in seawater is used in reconstructions of ocean circulation, marine productivity, air-sea gas exchange, and biosphere carbon storage. Here, a synthesis of δ13C measurements taken from foraminifera in marine sediment cores over the last 150 000 years is prese...
Päätekijät: | , , , , , , |
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Aineistotyyppi: | Journal article |
Kieli: | English |
Julkaistu: |
2010
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