A synthesis of marine sediment core δ¹³C data over the last 150 000 years

A synthesis of marine sediment core δ¹³C data over the last 150 000 years

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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...

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Xehetasun bibliografikoak
Egile Nagusiak: Oliver, K, Hoogakker, B, Crowhurst, S, Henderson, G, Rickaby, R, Edwards, N, Elderfield, H
Beste egile batzuk: European Geosciences Union
Formatua: Journal article
Hizkuntza:English
Argitaratua: Copernicus Publications 2009
Gaiak:
Earth sciences
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