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...
| المؤلفون الرئيسيون: | , , , , , , |
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| مؤلفون آخرون: | |
| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
Copernicus Publications
2009
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| الموضوعات: |