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...
| 主要な著者: | , , , , , , |
|---|---|
| その他の著者: | |
| フォーマット: | Journal article |
| 言語: | English |
| 出版事項: |
Copernicus Publications
2009
|
| 主題: |
Search Result 1
