Dataset - B2FIND

(Table 2) Stable isotope ratios of Uvigerina sp. from DSDP Site 68-502

lab: WHOI (Woods Hole Oceanographic Institute)

Leaf-wax-based carbon isotopes of n-alkanoic acids from IODP Site 361-U1478

This dataset contains the leaf-wax-based carbon isotopes (d13C, ‰) from n-alkanoic acids of marine sediments from IODP Site 361-U1478, Mozambique Channel. The Site was drilled...

Stable isotope record of Cibicidoides wuellerstorfi and Uvigerina perigrina o...

The dataset show stable isotope data of d13C and d18O measured on benthic foraminifers, C. wuellerstorfi and U. perigrina. The samples were collected in the Bounty Trough off...

Pliocene planktonic and benthic foraminiferal oxygen and carbon isotope ratio...

Here we present Pliocene planktonic (three species) and benthic foraminiferal oxygen and carbon isotope ratios from IODP Site U1313 (hole A), recovered from the North Atlantic...

Hydrogen isotopic composition of alkenones and oxygen isotopes of benthic for...

Hydrogen isotopic compositions of C37 long chain alkenones (δ2HC37) have been proposed as a proxy for past seawater salinity and applied in several regions. However, previous...

Stable isotopes of Uvigerina spp. from sediment core M78/1_235-1

Stable carbon (δ13C) and oxygen isotope (δ18O) were performed on the benthic foraminiferal species Uvigerina spp. The foraminiferal specimens were selected from piston core...

(Table 3) Oxygen and carbon isotopic record of living (Rose Bengal Stained) b...

Variation of the d13C of living (Rose Bengal stained) deep-sea benthic foraminifera is documented from two deep-water sites (~2430 and ~3010 m) from a northwest Atlantic Ocean...

Stable carbon and oxygen isotopic composition of benthic foraminifera of IODP...

Old Version, please see new version doi:10.1594/PANGAEA.871350

Paleorecords from MD02-2575 (Figure 2)

Palaeoclimate records and numerical model simulations indicate that changes in tropical and subtropical sea surface temperatures and in the annual average position of the...

(Table T1) Stable carbon and oxygen isotope ratios of benthic foraminifera in...

Stable isotope records were generated for a late Pliocene-early Pleistocene interval from Ocean Drilling Program (ODP) Site 1123 in the southwest Pacific (41°47 S, 171°30 W;...

(Table AT1) Grain size distribution and stable isotope record of benthic fora...

The Walvis Paradox states that opal accumulation fluctuates in counterphase to general productivity on Walvis Ridge, off northern Namibia. Sediments of early Quaternary age from...