Benthic foraminifera and stable isotope composition in Paleocene-Eocene sediments, supplement to: Thomas, Ellen; Shackleton, Nicholas J (1996): The Paleocene-Eocene benthic foraminiferal extinction and stable isotope anomalies. In: Knox, RWO'B; Corfield, RM; Dunay, RE (eds.), Correlation of the Early Paleogene in Northwest Europe, Geological Society Special Publication, 101, 401-441
In the late Paleocene to early Eocene, deep sea benthic foraminifera suffered their only global extinction of the last 75 million years and diversity decreased worldwide by 30-50% in a few thousand years. At Maud Rise (Weddell Sea, Antarctica; Sites 689 and 690, palaeodepths 1100 m and 1900 m) and W...
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Format: | Article in Journal/Newspaper |
Language: | English |
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PANGAEA - Data Publisher for Earth & Environmental Science
1996
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Online Access: | https://dx.doi.org/10.1594/pangaea.770123 https://doi.pangaea.de/10.1594/PANGAEA.770123 |