In situ microbialites occurring in reef rocks dredged between 80 and 130 m water depth on the modern fore-reef slopes of Tahiti and the Marquesas islands yield ages ranging from 17,100 Β± 2900 to 4410 Β± 2250 years BP, suggesting that they played a prominent role during the last deglacial sea level ri
Increase of carbon dioxide in the atmosphere during deglaciation: the coral reef hypothesis
β Scribed by W. H. Berger
- Publisher
- Springer
- Year
- 1982
- Tongue
- English
- Weight
- 273 KB
- Volume
- 69
- Category
- Article
- ISSN
- 0028-1042
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