Quantifying molecular oxygen isotope variations during a Heinrich stadial
δ<sup>18</sup>O of atmospheric oxygen (δ<sup>18</sup>O<sub>atm</sub>) undergoes millennial-scale variations during the last glacial period, and systematically increases during Heinrich stadials (HSs). Changes in δ<sup>18</sup>O<sub>atm</sub>...
| Main Authors: | , , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2015-11-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/11/1527/2015/cp-11-1527-2015.pdf |