(Appendix) Ostracodes at DSDP Leg 72 Holes
From the study of the ostracodes of Sites 516, 517, and 518 in comparison with those of Sites 21, 22, and 357, we can show that a time lag (early to late Oliogene) existed between the formation of the deep water masses (mid-bathyal ± 2000 m) and those of intermediate depths (upper bathyal ± 1000 m)....
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1983
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.811745 https://doi.org/10.1594/PANGAEA.811745 |