Abstract
A continuous deuterium profile along the 160,000-year Vostok ice core (Antarctica) is interpreted in terms of atmospheric temperature changes. This climatic record is the awaited terrestrial complement of the deep-sea records supporting the existence of a relation between the Pleistocene climate and orbital forcing.
| Original language | English |
|---|---|
| Pages (from-to) | 403-408 |
| Number of pages | 6 |
| Journal | Nature |
| Volume | 329 |
| Issue number | 6138 |
| DOIs | |
| Publication status | Published - 1 Jan 1987 |
| Externally published | Yes |