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(Table S2) The reconstructed sea surface temperature (SST) over the eastern e...
Abundant hydroclimatic evidence from western Amazonia and the adjacent Andes documents wet conditions during Heinrich Stadial 1 (HS1, 18-15 ka), a cold period in the high... -
(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... -
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... -
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... -
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. -
Database of previously published eastern equatorial Pacific δ¹⁸O and δ¹³C of ...
This dataset has no description
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Eastern Equatorial Pacific Holocene and Last Glacial Maximum stable isotopes ...
This dataset has no description
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Alkenone-derived Holocene Sea Surface Temperature database
see dating methoda: Correlation with GISP2 oxygen isotope record (Grootes and Stuiver, 1997).b: The age model of the core AD91-17 is based on AMS 14C, planktonic isotopic record... -
Summary of sea surface temperature trends reconstructed from alkenones for th...
Trend >0 means a warming over the time period, trend <0 means a cooling over the time period. -
World Ocean 14C plateau tuning
On the basis of minor time scale adjustments including the synchronization on IntCal20 the Suigetsu-based atmospheric 14C plateau structures are shown to be authentic. Their... -
Water temperature reconstructions based on paired Uk'37 and Tex86 records, an...
This dataset contains the collection of available published paired Uk'37 and Tex86 records spanning multi-millennial to multi-million year time scales, as well as a collection... -
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... -
Downcore Florisphaera profunda
This dataset has no description
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(Table S2) Diatom species of sediment core MD02-2499
This dataset has no description
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(Table 3) Definition of 14C plateaus for sediment core MD02-2503
This dataset has no description
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(Table 2k) Planktic and benthic 14C and 14C reservoir ages of sediment core M...
All 14C dates are rounded to decades. Planktic plateau boundaries were either defined at or in between single 14C ages of the records. For reasons of specimen availability... -
Mg/Ca values for planktonic foraminifera N. pachyderma from ocean sediment co...
Depth is corrected. -
Mg/Ca values for planktonic foraminifera G. bulloides from ocean sediment cor...
Depth is corrected. -
(Table 1) Age determination of sediment core MD02-2503
Measured on mixed planktonic foraminifera.