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Core top alkenone (C37) data compared to modern observations in the eastern e...
This dataset has no description
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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, 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... -
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... -
Radiolarian-based SST reconstruction (MAT) from sediment cores in the Pacific...
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. -
Annual SST estimates for the Last Interglacial (129-116 ka BP)
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 S1) Planktonic foraminifera abundances for the 1223 surface sediment s...
Our training set (SH0911C2, available from http://www.ncdc.noaa.gov/paleo/paleo.html) augments that used by Crundwell el al . [2008, Figure 2] with additional data from Mohtadi... -
Core top coccolithophore productivity compared to modern observations in the ...
This dataset has no description
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Core top chlorophyll concentration compared to modern observations in the eas...
This dataset has no description
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Core top sea surface temperature data compared to modern observations in the ...
This dataset has no description
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(Table 1) Sea surface temperature reconstruction for eastern equatorial Pacif...
Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial... -
Pb isotopic ratios and aluminum normalized elemental concentrations from diff...
Pb isotopic ratios and aluminum normalized elemental concentrations for samples from the Eastern Equatorial Pacific. These samples were from the upper 10 cm of the sediment... -
Grain size analysis of surface sediments from the South Pacific Ocean
This dataset has no description
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Granulometry of surface sediments in 0.05 µm classes from the South Pacific O...
This dataset has no description
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Grain size fractions of surface sediments from the South Pacific Ocean
Silt and clay (%) represent the respective terrigenous weight fractions of dried bulk sediment. -
Clay mineralogy of surface sediments from the South Pacific Ocean
The relative clay-mineral contents (rel%) of illite, smectite, chlorite and kaolinite were determined semi-quantitatively by calculating the integrated peak areas of the...
