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: | Oliver, K, Hoogakker, B, Crowhurst, S, Henderson, G, Rickaby, R, Edwards, N, Elderfield, H |
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Muut tekijät: | European Geosciences Union |
Aineistotyyppi: | Journal article |
Kieli: | English |
Julkaistu: |
Copernicus Publications
2009
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Aiheet: |
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