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Benthic stable isotopes of IODP sites 342-U1408 and 342-U1410
This dataset has no description
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BFAR for Eocene hyperthermals: PETM, ETM2, ETM3, ODP Site 208-1263
This dataset has no description
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Benthic foraminiferal data for Eocene hyperthermals: PETM, ETM2, ETM3, ODP Si...
This dataset has no description
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Boron isotope, Mg/Ca, Al/Ca data and reconstructed pH and CO2 concentrations ...
This dataset includes measurements on mixed layer planktonic foraminifera from IODP/ODP sites for boron isotopes and trace elements. Boron isotopes were measured after column... -
Palynology of ODP Hole 159-959D spanning the Middle Eocene climatic optimum
This dataset has no description
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Elemental composition of ODP Hole 159-959D spanning the Middle Eocene climati...
This dataset has no description
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(Table 4) Stratigraphic ranges of planktonic foraminifers in ODP Hole 144-872C
Sediment depth is given in mbsf. Species abundance: A = abundant, C = common, F = frequent, R = rare, - = absent. -
Estimated adjusted depth of CO2 of FB2001 drill core from Messel
This table contains atmospheric CO2-estimates based on stomata retrieved in the Messel fossil pit and published by Grein (2010) and Grein et al. (2011). The data is based on... -
Mean Annual Air Temperatures of FB2001 drill core from Messel
This table contains Mean Annual Temperatures (MAT) reconstructed using branched GDGTs obtained on core FB2001 from Messel (earliest Middle Eocene; 47.66 to 47.22 Ma), relative... -
Recurrence times of siderite layers of FB2001 drill core from Messel
To investigate variability and drivers of extreme precipitation events under high greenhouse gas concentrations prevalent during the Eocene we computed recurrence times of Fe/Ti... -
XRF Fe/TI and K/Ti ratios of FB2001 drill core from Messel
The data contains Fe/Ti and K/Ti ratios obtained via XRF core scanning of drill core FB2001 from the Messel fossil pit (earliest Middle Eocene; 47.66 to 47.22 Ma) versus core... -
BrGDGT-based temperature evolution through an Eocene hyperthermal event
Branched glycerol dialkyl glycerol tetraethers (brGDGTs) from maar sediments were analyzed in order to reconstruct continental air temperatures across a middle Eocene (47.2 Ma)... -
Palynological and geochemical results of middle Eocene sediments of ODP Hole ...
New palynological, sedimentological, and geochemical records spanning the Middle Eocene climatic optimum (MECO; ca. 40 Ma) in the equatorial Atlantic Ocean indicate that peak... -
Late Paleocene to early Eocene stable isotope records and calcareous nannofos...
In this study, we create a new age model for the high-latitude South Pacific during the late Paleocene to early Eocene (50.5 to 57.5 Ma). We present a bulk sediment δ13C and... -
Benthic stable isotopes and XRF element counts of IODP Sites 342-U1408 and 34...
Contourite drift deposits characterise the middle Eocene sequences of International Ocean Discovery Program (IODP) Site U1408 and Site U1410 (Newfoundland Ridge, North Atlantic,... -
Boron isotope, Mg/Ca, Al/Ca data from planktonic foraminifera and reconstruct...
This dataset collection includes boron isotope, Mg/Ca, and Al/Ca data from planktonic foraminifera, reconstructed sea surface temperature, seawater pH and atmospheric CO2... -
Middle to late Eocene carbonate accumulation rates in the Pacific, Atlantic, ...
Sedimentary records from the equatorial Pacific show that the deepening of the carbonate compensation depth (depth below which the calcium carbonate flux to the seafloor is... -
ODP Site 208-1263 PETM, ETM2, ETM3: barite accumulation rates, benthic forami...
Data from Ocean Drilling Program Site 1263 on Walvis Ridge in SE Atlantic include barite accumulation rates, benthic foraminiferal data, and carbon and oxygen isotopes for... -
GDGT and GMGT data
These data represent: Raw data presented in Sluijs et al., 2020 (Climate of the Past)- Peak areas of GDGTs and GMGTs peaks across the late Paleocene - early Eocene of Hole 4 of... -
Reconstruction of continental temperatures and oxygen isotope compositions of...
Earth's climate sensitivity – defined as the temperature increase for a doubling of pCO2 – and the mechanisms responsible for amplification of high latitude warming remain...
