<i>δ</i><sup>13</sup>C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2
Abrupt millennial-scale climate change events of the last deglaciation (i.e. Heinrich Stadial 1 and the Younger Dryas) were accompanied by marked increases in atmospheric CO<sub>2</sub> (CO<sub>2atm</sub>) and decreases in its stable carbon isotopic ratios (<i>δ</i&g...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2017-04-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/13/345/2017/cp-13-345-2017.pdf |