Links
- The Publications Warehouse does not have links to digital versions of this publication at this time
- Download citation as: RIS | Dublin Core
Abstract
The Middle Pliocene (???3 million years ago) has been identified as the last time the Earth was significantly warmer than it was during the Last Interglacial and Holocene. A quantitative micropaleontological paleotemperature transect from equator to high latitudes in the North Atlantic indicates that Middle Pliocene warmth involved increased meridional oceanic heat transport.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Micropaleontological evidence for increased meridional heat transport in the North Atlantic Ocean during the pliocene |
| Series title | Science |
| Volume | 258 |
| Issue | 5085 |
| Year Published | 1992 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Science |
| First page | 1133 |
| Last page | 1135 |
| Google Analytic Metrics | Metrics page |