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Stable isotope ratios measured on foraminifera of DSDP Hole 24-237
This dataset has no description
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(Table 1) Isotopic composition of organic compinents of DSDP Hole 24-231
Plant leaf wax hydrogen isotope (dDwax) reconstructions are increasingly being used to reconstruct hydrological change. This approach is based upon the assumption that... -
(Table 1) Geochemistry of volcanic glass shards from tephra layers of the Gul...
The early hominids of East Africa were dated by determining the ages of tuff beds at the sites. Despite much research using palaeomagnetic and K/Ar-dating techniques, some of... -
Distribution of benthic foraminifera in DSDP Hole 24-238 in the Central India...
Deep-sea benthic foraminifera have been quantitatively analyzed in samples (>125 µm size fraction) from Ocean Drilling Program (ODP) Site 238, to understand paleoceanographic... -
Stable isotope ratios of benthic and planktonic foraminifera from Late Miocen...
Tropical Indian Ocean planktonic and benthic foraminifera have 13C/12C ratios which change abruptly within Magnetic Epoch 6 about 6.2 million years ago. All species analyzed in...