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Stable isotope record on revised age model, IODP Site U1338-U1337
This dataset has no description
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Northwestern Australian Margin radiolarian dataset of IODP 363 Site U1483
This dataset has no description
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GTS-12 adjusted age models for ODP Site 198-1209
GTS-12 timescale adjusted age models for ODP site 1209 with biostratigraphic (calcareous nannoplankton and foraminifer), magnetostratigraphic datums and cyclostratigraphic... -
Nannofossil datums refined of ODP Sites 208-1263
This dataset has been carefully reviewed and curated in accordance with PANGAEA's exceptionally high quality standards. However, due to discontinued communication from the... -
Oxygen isotopic ratios of Cibicidoides from IODP Site 303-U1308
This dataset has no description
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(Table S18) Calcareous nannofossil biostratigraphy of ODP Site 208-1264
This dataset has no description
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(Table S17) Size fraction, and stable oxygen and carbon isotope records of be...
This dataset has no description
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(Table S16) Magnetochron boundary positions and their astronomically tuned age
Note: Magnetochron boundary position for Site U1333 are based U-Channel VGP data (Tab.S17-19) plotted on the adjusted rmcd (revised m CCSF-A) (Westerhold et al. 2012).... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...
The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and... -
(Table S7) Magnetostratigraphy of Site 208-1267
This dataset has no description
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Early Eocene-early Oligocene carbon and oxygen stable isotope data of bulk ca...
Here, we present carbon and oxygen stable isotope data measured on bulk carbonates samples from Site U1558. The site was drilled during the International Ocean Discovery Program... -
Table 6-2: Nannofossil datums of ODP Hole 208-1264A
The top and bottom sample intervals of the shipboard nannofossil datums were updated to factor in the composite depth scale revisions in this study. -
Table 6-5: Planktic foraminiferal datums of ODP Site 208-1264
The top and bottom sample intervals of the shipboard planktic foraminiferal datums were updated to factor in the composite depth scale revisions in this study. -
Table 6-4: Nannofossil datums of ODP Hole 208-1264C
The top and bottom sample intervals of the shipboard nannofossil datums were updated to factor in the composite depth scale revisions in this study. -
Table 6-3: Nannofossil datums of ODP Hole 208-1264B
The top and bottom sample intervals of the shipboard nannofossil datums were updated to factor in the composite depth scale revisions in this study. -
Table 6-6: Palaeomagnetic reversals from ODP Sites 208-1265 and 208-1266
These palaeomagnetic reversals from Sites 1265/1266 (Bowles, 2006) were transferred to 1264 by Liebrand et al., 2016. Here, we update the depths to accommodate the changes to...
