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Organic carbon accumulation, LGM
LGM (Last Glacial Maximum), average value of core section between 19 and 23 kyr BP or nearest sampled core depth -
Organic carbon accumulation, Holocene
Holocene, average value of core section between 4 and 8 kyr BP or nearest sampled core depth -
Globigerina bulloides dissolution index of the Last Glacial Maximum
-9.9999 = depth unknown -
Globigerina bulloides dissolution index of surface sediments
This dataset has no description
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Planktic foraminifera in surface sediments
see satellite data doi:10.1594/PANGAEA.57967 -
(Table S1) Diatom abundance in coastal upwelling systems
Coastal upwelling systems account for approximately half of global ocean primary production and contribute disproportionately to biologically driven carbon sequestration.... -
Sample locations, stratigraphic information and listing of carbon and oxygen ...
We explored the potential to use the stable isotopic compositions of planktonic foraminifera as a proxy for the position of the Brazil-Malvinas Confluence (BMC) in the Argentine... -
Grain-size analysis of surface sediments, continental margin off NW Africa
The terrigenous fraction of seabed sediments recovered along the north-west African continental margin illustrates spatial variability in grain size attributed to different... -
Geochemistry of sediment core GeoB3176-1
This dataset has no description
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Geochemistry of sediment core GeoB3117-1
This dataset has no description
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Delta 13C measured on alkenones of surface sediment samples GeoB1008-6 to Geo...
We have analyzed the stable carbon isotopic composition of the diunsaturated C37 alkenone in 29 surface sediments from the equatorial and South Atlantic Ocean. Our study area... -
LGM, planktic foraminifera (EPILOG version)
[1] We used planktic foraminiferal assemblages in 70 sediment cores from the tropical and subtropical South Atlantic Ocean (10°N–37°S) to estimate annual mean sea surface... -
Assemblage of planktonic foraminifera for the last glacial maximum (LGM) in s...
This dataset has no description
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Sea surface temperatures calculated for the last glacial maximum from plankto...
This dataset has no description
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Multiproxy sedimentation patterns of sediment cores from the continental marg...
Tropical regions have been reported to play a key role in climate dynamics. To date, however, there are uncertainties in the timing and the amplitude of the response of tropical... -
Phytoplanktonic microfossil groups of sediments from the South and Equatorial...
Individual planktonic microfossil species, or assemblage groups of different species, are often used to, qualitatively and/or quantitatively, reconstruct past (sub)surface-water... -
Planktic foraminifera analyses of surface sediments and satellite data in the...
The Canary Islands region occupies a key position with respect to biogeochemical cycles, with the zonal transition from oligotrophic to nutrient-rich waters and the contribution... -
Sea surface temperature and salinity reconstruction of sediment core GeoB3129-1
A sediment core from the western tropical Atlantic covering the last 21,000 yr has been analysed for centennial scale reconstruction of sea surface temperature (SST) and ice... -
Expanded GHOST database
In this study we review a global set of alkenone- and foraminiferal Mg/Ca-derived sea surface temperatures (SST) records from the Holocene and compare them with a suite of... -
Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum...
The modern Atlantic Ocean, dominated by the interactions of North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW), plays a key role in redistributing heat from the...