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Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
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... -
(Table 4) Mg/Ca of benthic foraminiferal calcite from the Gulf of California,...
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SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
(Table 1) B/Ca ratios in planktonic foraminifera from core top sediments
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Multi-sensor global compilation of mid-Holocene (MH) sea surface temperatures...
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(Appendix 1) Nd and Mn concentration in planktonic foraminifera of sea surfac...
Planktonic foraminifera size fraction >250 µm. -
Distribution of planktic foraminifera in surface sediments of the Atlantic Oc...
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(Appendix A) Relative abundance of Emiliania huxleyi in sediment cores of the...
The coccolithophore species Emiliania huxleyi is characterized by a wide range of sizes, which can be easily distinguished in the light microscope. In this study we have... -
Radiocarbon ages and 230Th data of five sediment cores from the Björn and Gar...
In locations of rapid sediment accumulation receiving substantial amounts of laterally transported material the timescales of transport and accurate quantification of the... -
Planktnoic 14C dates and calculated calendar ages in core NEAP 4K (Supplement...
*: not included in the final age model, although the age would be consistent if a 800-year surface reservoir age is used. -
H. elegans Cd/Ca and reconstructed seawater Cd in core NEAP 4K (Supplementary...
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Deep water reconstructions in core NEAP 4K (Supplementary Table 1)
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Age model control points used for core NEAP 4K (Supplementary Table 5)
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Coiling ratio of N. pachyderma (s) in core NEAP 4K (Supplementary Table 3)
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(Fig. 3d) Paleosalinity reconstruction for sediment core NEAP-18K
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(Fig. 3c) Summer SST reconstruction for sediment core NEAP-18K
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(Fig. 3b) Stable oxygen isotope ratios of planktonic foraminifera of sediment...
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(Fig. 3a) Stable oxygen isotope ratios of benthic foraminifera of sediment co...
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(Table 3) Age models of sediment cores BOFS8K, BOFS17K and NEAP-08K
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