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Par Collection Par Auteur- OLAUSSON, E. (1)
- 1981 (1)
- Up to one fourth of the isotopic change in foraminifera found in deep-sea cores (or some 0.3 /) may be due to a gradual change in the isotopic composition of the Antarctic and Greenland ice sheets. Therefore the peak-to-valley variation of the 0
- 1981