High-resolution palaeoclimate records recovered from the Iberian margin in core MD95-2040 exhibit large fluctuations in oceanographic conditions over the last 190 ka. Large-scale cooling of the surface ocean is indicated by the presence of the polar planktonic foraminifer Neogloboquadrina pachyderma
β¦ LIBER β¦
On the timing and mechanism of millennial-scale climate variability during the last glacial cycle
β Scribed by E. Rohling; P. Mayewski; P. Challenor
- Publisher
- Springer-Verlag
- Year
- 2003
- Tongue
- English
- Weight
- 563 KB
- Volume
- 20
- Category
- Article
- ISSN
- 0930-7575
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