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Age determination of Northwest Atlantic sediment cores
This dataset contains new and updated age models for sediment cores from depth transects at Blake Outer Ridge and Cape Hatteras. Primarily, this includes new AMS-14C ages... -
Downcore and single benthic foraminiferal δ18O data from Cape Hatteras and Bl...
This dataset contains downcore benthic δ18O data from four cores at Cape Hatteras (for each core there is data from between one and three different benthic foraminifera... -
Monospecific benthic δ18O data from Cape Hatteras and Blake Outer Ridge durin...
This dataset contains monospecific benthic δ18O data from cores that form depth transects at Cape Hatteras and Blake Outer Ridge. Data is from either the Mid-Holocene or LGM and... -
Vertical δ18O profiles from Cape Hatteras and Blake Outer Ridge during the Mi...
This dataset consists of glacial and Mid-Holocene multi-species benthic δ18O mean data from cores that form depth transects at Cape Hatteras and Blake Outer Ridge. The mean δ18O... -
Mean ages calculated by the bayesian age-depth model of sediment core JPC42 f...
Age-depth model of the JPC42 sediment core. The core chronology is based on the radiocarbon ages published in Caniupán et al. (2014, doi:10.1016/j.yqres.2014.07.009). All... -
Predicted mean grain size of the JPC42 sediment core from Wide Channel (Chile...
Mean grain size predicted at a 2 mm resolution using the XRF intensities of Fe, K, Ti, Rb, Zr and Mn following Liu et al. (2019, doi:10.1029/2018GC008154). A set of 112 samples... -
XRF core scanner geochemistry, PC1 scores and detrended PC1 scores of sedimen...
Inorganic geochemical data of the JPC42 and KC41 cores obtained by ITRAX XRF core scanning (Cox Analytical Instruments) at the Woods Hole Oceanographic Institution, PC1 scores,... -
Geochemical and sedimentological data of the JPC42 sediment core from Wide Ch...
Organic geochemical and sedimentological data analyzed at a 10 to 20 cm interval on the JPC42 and KC41 cores including total organic carbon content, stable carbon isotopes,... -
Geochemistry of sediment core TN041-8PG and TN041-8JPC from modern sediments ...
This dataset has no description
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Diatom assemblages excluding Chaetoceros resting spores of sediment core JPC4...
Diatom abundance and assemblage data are presented for JPC43 - a ~12 m marine sediment core recovered from 576 m water depth in Neny Fjord, Marguerite Bay, Antarctic Peninsula... -
Depth, age, diatom concentration and Chaetoceros resting spores of sediment c...
Diatom abundance and assemblage data are presented for JPC43 - a ~12 m marine sediment core recovered from 576 m water depth in Neny Fjord, Marguerite Bay, Antarctic Peninsula... -
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... -
Major and trace elemental concentration from sediment core EW0408-85JC and IO...
Here we report the sediment major and trace element geochemistry at two water depths in the Gulf of Alaska, Northeast Pacific, spanning the last ~50 kyr. These data were used to... -
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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Annual SST estimates from the late Marine Isotope Stage 6 (140-135 kyr) and c...
This dataset has no description
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Maximum annual SST estimates during the early LIG (129-124 ka; 189 sites)
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. -
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. -
SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
Note, that we have assumed a thermal equator of 5 degrees North, where sites above this latitude 'Summer' = JJA, and 'Winter' = DJF. Sites south of this line have 'Summer'...