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Documentation of sediment core MD03-2621
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(Supplementary Table 2) Tie points of sediment core MD03-2621
DEPTH, sediment/rock = Corrected depth -
Total reflectance of sediment core MD03-2621
DEPTH, sediment/rock = Corrected depth -
Sediment total reflectance measurements from the Cariaco Basin (MD03-2621) an...
During the last glacial period, the North Atlantic region experienced pronounced, millennial-scale alternations between cold, stadial conditions and milder interstadial... -
Opal of sediment core MD97-2142
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Elemental composition of sediment core MD06-3075
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UK'37 index and sea surface temperature reconstruction for sediment core MD06...
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Reconstruction of primary productivity for sediment core MD06-3075
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Stable oxygen isotope record of Globigerinoides ruber from sediment core MD06...
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Stable oxygen isotope record of benthic foraminifera from sediment core MD06-...
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Age model of sediment core MD06-3075
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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... -
Stable oxygen isotope, UK'37, productivity, CaCO3 and XRF records from sedime...
Proxy records of hydrologic variability in the West Pacific Warm Pool (WPWP) have revealed wide-scale changes in past convective activity in response to orbital and sub-orbital... -
(Table 2) Oxygen isotopes measured on water bottle samples during POSEIDON cr...
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Distribution of planktic foraminifera in surface sediments of the Atlantic Oc...
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Time slice 2 of planktic foraminifera of the last glacial maximum
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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 determination and sea-surface reconstruction of sediment cores from the N...
Polycystine radiolarians are used to reconstruct summer sea surface temperatures (SSSTs) for the Late Pleistocene-Holocene (600-13,400 14C years BP) in the Norwegian Sea. At... -
Stable isotope record of planktonic foraminifera from the western Iberian mar...
The surface water hydrography along the western Iberian margin, as part of the North Atlantic's eastern boundary upwelling system, consists of a complex, seasonally variable... -
Glacial North Atlantic: Sea surface conditions reconstructed by GLAMAP 2000
The response of the tropical ocean to global climate change and the extent of sea ice in the glacial nordic seas belong to the great controversies in paleoclimatology. Our new...
