Occurrence and isotopic composition (δ¹⁸O, δ¹³C) of benthic foraminifera in sediments from DSDP Leg 72
Changes in the vertical water mass structure of the Vema Channel during the Pliocene have been inferred from benthic foraminiferal assemblages and stable isotopic analyses from three sites of DSDP Leg 72 (South Atlantic). Faunal and isotopic results from Sites 516A and 518 suggest that a major chang...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1985
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.718261 https://doi.org/10.1594/PANGAEA.718261 |