Dataset - B2FIND

Foraminiferal faunal estimates of paleotemperature: Circumventing the no-anal...

The sensitivity of the tropics to climate change, particularly the amplitude of glacial-to-interglacial changes in sea surface temperature (SST), is one of the great...

Stable isotope data of the 120 k time slice

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Age determination of sediment core RC10-196

Note that in the NW Pacific, Sarnthein et al. (2007) have no reliable estimate of reservoir age correction at 14270 14C age. They estimate that the reservoir correction is...

Radiocarbon age determinations on sediment core RC10-288

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Radiocarbon age determinations on sediment core RC10-5

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Stable isotopes measured on foraminifera from the 120 kyr time slice reconstr...

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Abundance of microfossils in the 120 kyr time slice reconstruction from sedim...

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(Table 1) Foraminifera weight, size index and CO3 concentrations of core top ...

Down water column traverses of core top weights for three planktonic species confirm Lohmann's (1995) relationship between foraminifera shell weight loss and bottom water...

(Table 2) Composition of Aleutian Trench sediments

Point counting analysis

Stable carbon and oxygen isotope ratios of Neogloboquadrina pachyderma (s) of...

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Sedimentation and accumulation rates of opal, carbonate and organic carbon an...

Note that MARtoc, MARcaco3, and MARopal (mg/cm2/y) are not 230Th fluxes, but are estimated as: MAR = f * LSR * DBD (where DBD = dry bulk density; LSR = linear sedimentation...