Dataset - B2FIND

The late Maastrichtian warming event was defined by a global temperature increase of about 2.5-5°C, which occurred ~150-300 kyr before the K/Pg (Cretaceous/Paleogene) mass...

Oxygen isotopic ratio of Globigerinoides ruber (white variety) in the surface...

The application of stable oxygen isotopic ratio of surface dwelling Globigerinoides ruber (white variety) (δ¹⁸Oruber) to reconstruct past hydrological changes requires precise...

Cenozoic clumped isotope temperature record from the deep North Atlantic

This dataset contains clumped isotope (D47), d18O and d13C data from benthic foraminifera from four IODP sites from the Newfoundland margin. The D47 data were used to...

Morphometrics from the shells of Globorotaloides hexagonus from sediment core...

Here we document the morphometric measurements from the shells of planktic foraminifer Globorotaloides hexagonus from Eastern Equatorial Pacific core site TR163-23 (0° 24.6' N,...

Oxygen and carbon isotopes rom the shells of Globorotaloides hexagonus from s...

Here we document the stable isotope (δ18O and δ13C) from the shells of planktic foraminifer Globorotaloides hexagonus from Eastern Equatorial Pacific core site TR163-23 (0°...

(Table 4) Relative abundance of planktonic foraminifera in ODP Site 162-980

Sediment depth is composite depth (mcd).

Late Maastrichtian-early Eocene benthic stable carbon and oxygen isotope reco...

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Planktic foraminifera stable carbon and oxygen isotope records of IODP Hole 3...

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Planktic foraminifera stable carbon and oxygen isotope records of ODP Hole 12...

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