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(Table 1) Main calcareous nannofossil biostratigraphic events of ODP Leg 107 ...
For ODP Hole 107-653A see Rio et al. (1990) dataset: doi:10.1594/PANGAEA.746173 -
(Table 2) Huminite/vitrinite reflectance and maceral composition of ODP Leg 1...
in vol % (mineral matter free basis) -
(Table 2) Chemical composition of smectites from ODP Site 168-1027
Depth, sediment = mbsf -
(Figure 3) Changes of IPLs in subsurface sediments from IODP Expedition 311, ...
This dataset has no description
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(Figure 2) Changes of IPLs in subsurface sediments from ODP Leg 204, Hydrate ...
This dataset has no description
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(Table 4) Compositions of quenched glasses from peridotides at 13°N MAR
This dataset has no description
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(Table 6) Relative proportions of IPL- and fossil GDGTs, TEX86 temperature pr...
*Sample was analyzed only once (n = 1) -
(Table 3) Radiocarbon age determinations on sediment cores from the Vietnames...
This dataset has no description
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(Table 2) Radiocarbon ages for the three presented sediment cores
This dataset has no description
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(Appendix) Paleomagnetic of ODP Hole 101-635B
Missing step of demagnetization = NRM -
(Appendix) Paleomagnetic of ODP Hole 101-634A
Missing step of demagnetization = NRM -
(Appendix) Paleomagnetic of ODP Hole 101-633A
Missing step of demagnetization = NRM -
(Appendix) Paleomagnetic of ODP Hole 101-632A
Missing step of demagnetization = NRM -
(Appendix) Paleomagnetic of ODP Hole 101-631A
This dataset has no description
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(Appendix) Paleomagnetic of ODP Hole 101-628A
Missing step of demagnetization = NRM -
(Appendix) Paleomagnetic of ODP Hole 101-627B
Missing step of demagnetization = NRM -
(Appendix) Paleomagnetic of ODP Site 101-626
Missing step of demagnetization = NRM -
(Table 5) Sea surface temperture reconstruction for ODP Site 162-980
Sediment depth is composite depth (mcd). -
(Table 1) Sinking rates of particles in the Atlantic Ocean based on seasonal ...
EAA = Eastern Equatorial Atlantic, WEA =Western Equatorial Atlantic. -
(Table 2) Polarity transitions of ODP Hole 114-700B
Transitions interpolated within coring or sampling gaps can be identified from the associated large range of uncertainty. Boundaries of thin or otherwise poorly defined polarity...
