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S8 - Cumulative offset of ODP Hole 208-1267A
This dataset has no description
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S6 - Cumulative offset of ODP Hole 208-1263D
This dataset has no description
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S6 - Cumulative offset of ODP Hole 208-1263C
This dataset has no description
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S6 - Cumulative offset of ODP Hole 208-1263B
This dataset has no description
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S6 - Cumulative offset of ODP Hole 208-1263A
This dataset has no description
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(Appendix 1) Depth model of ODP Hole 171-1052F
This dataset has no description
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(Appendix 1) Depth model of ODP Hole 171-1052D
This dataset has no description
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(Appendix 1) Depth model of ODP Hole 171-1052C
This dataset has no description
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(Appendix 1) Depth model of ODP Hole 171-1052B
This dataset has no description
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(Appendix 1) Depth model of ODP Hole 171-1052A
This dataset has no description
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Final stable oxygen and carbon isotope ratios of benthic foraminifera versus ...
This dataset has no description
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(Appendix A) Stable carbon and oxygen isotope ratios of benthic foraminifera ...
This dataset has no description
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Interpolated stable carbon and oxygen isotope ratios of ODP Site 138-846 in t...
This dataset has no description
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(Appendix A) Stable carbon and oxygen isotope ratios of benthic foraminifera ...
This dataset has no description
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Gaussian interpolated Δδ13C of IODP Site 339-U1385
This dataset has no description
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Continuous data of Globigerinoides ruber calcite delta18O and delta13C versus...
Samples were obtained from either those taken aboard JOIDES Resolution during Leg 160 or in the Bremen Ocean Drilling Program (ODP) Core Repository. On the ship, approximately... -
Middle to late Miocene (13.7-8.6 Ma) stable isotope stratigraphy and paleocea...
International Ocean Discovery Program (IODP) Site U1490 in the Western Pacific Warm Pool (05°48.95ʹN, 142°39.27ʹE, 2341 m water depth) provides the opportunity to directly... -
Barite Accumulation rates across Paleocene-Eocene Thermal Maximum (PETM)
Barite accumulation rates (BAR) have been measured from 12 DSDP/ODP site globally (DSDP site 525, 549 and ODP site 690, 738, 1051, 1209, 1215, 1220, 1221, 1263,1265 and 1266A)... -
Ti/Al ratios of ODP Site 160-967
The evolution of the Solar System has been shown to be chaotic (Laskar, 1990, doi:10.1016/0019-1035(90)90084-M), which limits our ability to retrace the orbital and precessional... -
(Table 1) Age comparison between the GPTS and ODP Site 181-1123 age model for...
Today the deep western boundary current (DWBC) east of New Zealand is the most important route for deep water entering the Pacific Ocean. Large-scale changes in deep water...
