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doi:10.2204/iodp.proc.342.205.2017

Summary

In the present study we analyzed three organic geochemical proxies: the BIT, MI, and %GDGT-0 indexes. The results imply that most of the isoGDGTs preserved in the Oligocene deposits on the Newfoundland sediment drifts are derived from Thaumarchaeota. Furthermore, a moderate to high amount of brGDGTs were observed, suggesting a continental source of lipids in the marine sediment of the two studied sites (U1406 and U1411).