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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... -
Shelf ecosystems along the U.S. Atlantic Coastal Plain prior to and during th...
The Paleocene-Eocene Thermal Maximum (PETM) is the most pronounced climate event of the early Paleogene. It is characterized by negative δ18O and δ13C excursions recorded in... -
Size-fraction-specific stable isotope variations in early Eocene bulk sedimen...
Here we present changes in abundances and δ13C and δ18O composition of five size fractions of bulk sediments from ODP Site 1209 in Shatsky Rise, north-central Pacific, deposited... -
Paleogene sample-based total organic carbon and Rock-eval pyrolysis measureme...
Deposition of the Paleocene-Eocene Wilcox Group (Gp) in the northern Gulf of Mexico (GoM) occurred during dramatic global climate and regional tectonic change. Key drivers... -
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... -
Palynology and biomarker temperature reconstructions of the Paleocene-Eocene ...
Palynology data and analysis for branched glycerol dialkyl glycerol tetraethers (brGDGTs) from Point Margaret (Southern Australia), respectively, were used to estimate the mean... -
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... -
Photosymbiosis in planktonic foraminifera across the Palaeocene-Eocene Therma...
Under stress, corals and foraminifera may eject algal symbionts ('bleach'), which can increase mortality. How bleaching relates to species viability over warming events is of... -
Lower to middle Eocene astronomically-tuned Ca/Fe-ratios and bulk stable isot...
The geologic time scale for the Cenozoic Era has been notably improved over the last decades by virtue of integrated stratigraphy, combining high-resolution astrochronologies,... -
Stable isotope ratios, and trace elements from Pacific and S. Atlantic mid-la...
Eocene Thermal Maximum 2 (ETM‐2; 54.1 Ma) was the second largest Eocene hyperthermal. Like the Paleocene‐Eocene Thermal Maximum (PETM), ETM‐2 was characterized by massive carbon... -
Calcareous nannofossil abundance of IODP Site 378-U1553
999 means cf: taxonomic note: 'cf.' (= 'confer', in Latin: compare) -
Hyperthermals and the bulk sediment δ13C tie points from IODP Site U1553 corr...
Age model. Hyperthermals (Hyp) and the bulk sediment δ13C records from ODP Site1258 and 1262 were correlated to our record. This table provides the tie points in order to... -
Calcareous nannofossil biostratigraphy of IODP Site 378-U1553
*shipboard data, Röhl, U., Thomas, D.J., Childress, L.B., Anagnostou, E., Ausín, B., Borba Dias, B., Boscolo-Galazzo, F., Brzelinski, S., Dunlea, A.G., George, S.C., Haynes,... -
d13C and d18O stable isotope records of IODP Site 378-U1553
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Temperature estimates based on Mg/Ca and δ18O for the South Dover Bridge core
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Benthic foraminifera stable isotope ratios in the South Dover Bridge core
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Bulk carbonate stable isotope ratios in the South Dover Bridge core
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Planktic to benthic foraminifera ratio in the South Dover Bridge core
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Kaolinite content in the South Dover Bridge core
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Grain size distribution in the South Dover Bridge core
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