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Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
Downcore Florisphaera profunda
This dataset has no description
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A summary of consistently dated Atlantic sediment cores over the last 40 thou...
Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear... -
Correlations between the proxy SST anomalies (annual, boreal summer and borea...
This dataset has no description
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(Table 1) AMS 14C measurements in sediment core MD03-2698
For the resulting age model see doi:10.1594/PANGAEA.733440. (a) Age at 29.087 m depth is from Hughen et al. (2004) and Voelker et al. 2000. -
(Figure 5) Stable isotope ratios on Cibicidoides sp. from sediment core MD03-...
This dataset has no description
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Global marine radiocarbon data compilation for the last deglaciation, spline ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, global ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Carbon 13 isotopes reveal limited ocean circulation changes between interglac...
We present a compilation of δ13C data to characterize the ocean circulation during the interglacials of the last 800 000 years. We selected 9 interglacials for which we have... -
(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... -
Marine fossil radiocarbon (14C) compilation up to 2021, version 2024
Using a new global compilation of deep-sea 14C/C, we estimated (in Rafter et al. 2022) the average D14C (units of per mil) and 14C ventilation age (units of years) over the last... -
Global marine radiocarbon data compilation for the last deglaciation, zonal a...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Marine fossil radiocarbon (14C) compilation up to 2021
This dataset includes a global compilation of new and published 14C measurements of benthic foraminifera and deep-sea corals (from 0-to 49872 years BP). We synthesized this new... -
Last Glacial Maximum (LGM) paleo-dust record
This dataset has no description
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Pre-industrial Holocene (pi-HOL) paleo-dust record
This dataset has no description
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Sea surface temperature reconstruction from biomarker in sediments off Portugal
High resolution reconstructions of sea surface temperature (Uk'37-SST), coccolithophore associations and continental input (total organic carbon, higher plant n-alkanes,... -
Stable isotope record and lithic fragments distribution in sediments of MIS9-...
Stable isotope and ice-rafted debris records from three core sites in the mid-latitude North Atlantic (IODP Site U1313, MD01-2446, MD03-2699) are combined with records of ODP... -
Stable isotope record, and abundances of ice rafted debris and Neogloboquadri...
This paper documents the migration of the Polar Front (PF) over the Iberian margin during some of the cold climatic extremes of the last 45 ka. It is based on a compilation of... -
Analytical results from sediment core MD03-2698
It is well established that orbital scale sea-level changes generated larger transport of sediments into the deep-sea during the last glacial maximum than the Holocene. However,...
