Dataset - B2FIND

Pollen-corrected hydrogen isotope fractionation factors, IODP Hole 318-U1356A

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Raw counts of sporomorphs in the Eocene interval of IODP Hole 318-U1356A

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(Table S1) Pollen and spores of IODP Hole 318-U1356A

Sediment depth is given in mbsf. All samples are from the work half of the sediment core.

Dinoflagellate cyst counts from IODP Hole 318-U1356A

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(Table S2) Major and trace element data for fossil fish tooth samples of IODP...

Analytical precision = 2% for elements heavier than Rb; 4% for elements lighter than Rb.

(Table S3) Diatom species counts of IODP Hole 318-U1361A

DEPTH, sediment/rock [m] is given in mbsf.

Dinoflagellate cysts in the Oligocene to Miocene sediments of IODP Site 318-U...

There is growing interest in the scientific community in reconstructing the paleoceanography of the Southern Ocean during the Oligocene-Miocene because these time intervals...

A refined age model for the U1361A marine sediment core

This data set displays a refined age scale for the U1361A marine sediment core (64.41°S, 143.89°E, 3,454 m water depth), recovered from the continental rise offshore of the...

Palynological counts from the Oligocene-Miocene of IODP Site 318-U1356, Wilke...

Palynological counts from IODP Leg 318 Hole U1356A, Cores 95R-11R, and the lithological facies as observed in Salabarnada et al., CP 2018. Reworked dinocysts (as by Bijl et al.,...

Major, trace element and XRF data for sediments and fish tooth samples, from ...

Fossil fish teeth from pelagic open ocean settings are considered a robust archive for preserving the neodymium (Nd) isotopic composition of ancient seawater. However, using...

Sporomorphs and quantitative analysis of the Eocene record from IODP Hole 318...

The early Eocene epoch was characterized by extreme global warmth, which in terrestrial settings was characterized by an expansion of near-tropical vegetation belts into the...

Pollen and spores, calculated temperature and precipitation of IODP Hole 318-...

The warmest global climates of the past 65 million years occurred during the early Eocene epoch (about 55 to 48 million years ago), when the Equator-to-pole temperature...