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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 alkenone (C37) data compared to modern observations in the eastern e...
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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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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(Table 1) Measured B, Li, Sr and Mg concentrations and isotope ratios for aci...
SW, seawater.a: Previously reported by: Tivey et al. (2006), Craddock et al. (2010), Reeves et al. (2011) and Seewald et al. (2015) for fluids collected in 2006.b: Previously... -
(Table 2) Li, B and Sr concentrations and isotope ratios of fresh and altered...
a: Fresh volcanic rocks from the Manus Basin were previously reported by Beier et al. (2015).b: data previously reported by Wilckens et al. (2019). -
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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Multi-sensor global compilation of mid-Holocene (MH) sea surface temperatures...
This dataset has no description
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(Table S3) B/Ca ratios Cibicidoides wuellerstorfi from Holocene sediments
Size fraction of benthic foraminifera = 150-250 µm. -
(Table S1) B/Ca ratios and stable isotope record of Nuttallides umbonifera fr...
Size fraction of benthic foraminifera = 150-250 µm. -
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. -
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... -
Coral Li/Mg records of deep sea temperature during the last deglaciation
Fossil scleractinian corals were collected from the Galápagos platform in the East Equatorial Pacific (0°N, 90°E) on cruises MV1007 and NA064 from water depths between 419 and... -
Chemical composition of Pacific manganese nodules and crusts analyzed at Scri...
Manganese nodules, coatings and crusts from the Pacific Ocean were analyzed at Scripps Institution of Oceanography using X-ray emission spectrometry (XES). Samples were ground... -
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... -
(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...