Stable oxygen and carbon isotope ratios of foraminifera from Oligocene to Miocene sediments of DSDP Hole 39-354 from Ceara Rise, West Altlantic (Table 1)
The oxygen- and carbon-isotope compositions of planktic and benthic foraminifera and calcareous nannofossils from Middle Oligocene-Early Miocene Equatorial Atlantic sediments (DSDP Site 354) indicate two important paleoceanographic changes, in the Late Oligocene (foraminiferal Zone P.21) and in the...
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Format: | Dataset |
Language: | English |
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PANGAEA
1983
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.690399 https://doi.org/10.1594/PANGAEA.690399 |