Dataset - B2FIND

(Table 3) Oxygen isotope ratios of benthic foraminifera from DSDP Hole 80-548

Presently, the intermediate depths of the North Atlantic Ocean are occupied by a great lens of warm, saline water whose source is the Mediterranean Sea. This water flows both...

Benthic foraminifer δ¹⁸O and δ¹³C values and planktonic to benthic foraminife...

We present carbon and oxygen isotope values and planktonic/benthic ratios for middle Miocene (11-17.5 Ma) foraminifers deposited at Ocean Drilling Program Hole 744B in the...

Stable carbon and oxygen isotope ratios of planktonic and benthic foraminifer...

Combined data on benthic foraminifers, siliceous fossils, and stable isotopes depict times of enhanced organic carbon oxidation in the sediments and high primary productivity in...

Age models, stable isotope record, and physical properties of ODP Hole 154-926B

We extend existing high-resolution Oligocene–Miocene proxy records from Ocean Drilling Program (ODP) Leg 154. The extended record spans the time interval from ~17.86 to 26.5...

Estimation of sea surface temperatures and salinity of ODP Site 177-1089 (App...

ODP Site 1089 is optimally located in order to monitor the occurrence of maxima in Agulhas heat and salt spillage from the Indian to the Atlantic Ocean. Radiolarian-based...

Stable carbon and oxygen isotope ratios of planktonic and benthic foraminifer...

Changes in the intermediate water structure of the North Atlantic were reconstructed using benthic foraminiferal delta13C at Ocean Drilling Program (ODP) site 982 for the past...

Stable carbon and oxygen isotope ratios of Cibicidoides wuellerstorfi in the ...

Subpolar North Atlantic proxy records document millennial-scale climate variations 500,000 to 340,000 years ago. The cycles have an approximately constant pacing that is similar...