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Stable isotope ratios of benthic and planktonic foraminifera from Late Miocene sediments of DSDP Hole 24-238 on the Central Indian Ocean Ridge (Appendix 1)
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 the Late Miocene sectio
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Geochemical dataset
Major and trace elemental and isotopic data for Neoproterozoic carbonate samples collected from six sites across the northern Flinders Ranges, South Australia
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(Table 3) Major and trace element composition of lavas from ODP Leg 135 holes
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Carnat_Commsbio-18-0423-T.xlsx
This is the data set attached to a manuscript submitted to Nature Communications Biology (COMMSBIO-18-0423-T) entitled: "Large sulfur isotope variability suggests unique DMSP cycling and metabolism in
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Moisture and density (MAD) from IODP Hole 386-M0087D
Moisture and density (MAD) data from discrete samples from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). During the onshore phase
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