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Sea surface temperatures reconstructed from sediment core CHN82-24
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(Table 2) Trace metal ratios of various benthic foraminifera shells
Benthic foraminiferal d13C and Cd/Ca studies suggest that deep Atlantic circulation during the Last Glacial Maximum was very different from today, with high-nutrient (low d13C,... -
Stable carbon and oxygen isotope ratios of benthic foraminifera
Carbon isotopic measurements on the benthic foraminiferal genus Cibicidoides document that mean deep ocean delta13C values were 0.46 per mil lower during the last glacial... -
(Appendix 1) Stable carbon and oxygen isotope ratios of Cibicidoides spp. fro...
C. wuellerstorfi and C. kullenbergi -
Atlantic sea surface temperatures during the last glacial maximum (LGM) time ...
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Planktic foraminiferal assemblage for the 10kyr time slice from different sed...
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Sea surface temperatures of the last glacial maximum, GLAMAP
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Time slice 2 of planktic foraminifera of the last glacial maximum
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Sea surface temperatures calculated for 10 ka BP from planktic foraminifera
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Sea surface temperatures calculated for today from planktic foraminifera
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Database of the GLAMAP project
A uniform chronology for foraminifera-based sea surface temperature records has been established in more than 120 sediment cores obtained from the equatorial and eastern... -
Age model and Cadmium/Calcium ratio of sediment core CH82-24 (specmap2.039)
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Stable isotopes of sediment core CH82-24 (specmap2.017)
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Age model of sediment core CH82-24 (specmap2.026)
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Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean
We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle...
