-
Mediterranean sapropel bulk organic matter and biomarker concentrations and c...
This dataset contains bulk organic matter and biomarker data for two Mediterranean Sea sites: ODP Leg 160 site 964 (including sapropels S5, S7, and i-282) and ODP Leg 160 site... -
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
This dataset has no description
-
New age model for ODP Site162-982
This dataset has no description
-
Oxygen and carbon stable isotopes ratios from benthic foraminifera from Mioce...
Stable oxygen and carbon isotope ratios measured on benthic foraminifera (Cibicidoides mundulus, Cibicidoides wuellerstorfi and Oridorsalis umbonatus) from the Miocene time... -
Modelled carbon and nitrogen zooplankton stable isotope data in the North Atl...
Calanus (copepod) sampled by the Continuous Plankton Recorder (CPR) survey (https://www.cprsurvey.org/) in the North Atlantic from 2009-2018 were analysed for stable carbon... -
Single-shell stable isotopes, weights, ages, Marine Isotope Stages (MIS), and...
This dataset contains single-shell stable isotope data (d18O and d13C), shell weights, ages, and preservation states of Cibicidoides shells spanning MIS 1-2 from ODP Site 929,... -
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... -
U/Th ages of stalagmite PIM5
This dataset has no description
-
U/Th ages of stalagmite PIM4
This dataset has no description
-
d18O composite records of of stalagmites PIM4 and PIM5
This dataset has no description
-
Stable isotope records (d18O and d13C) of speleothems from Amazonian lowlands...
The stable isotope records are based on two stalagmites, PIM4 and PIM5, collected in Cuíca cave (11°40°S, 60°38°W, ~310 m a.s.l.) located in Pimenta Bueno city, Rondônia State,... -
Geochemistry of sediment core EN21103 from Lake Ulu, eastern Siberia
Here are the bundled geochemical data of an 11-m-long sediment core EN21103 collected from Lake Ulu (63.34°N, 141.05°E) in the Oymyakon region (eastern Siberia) during the... -
U/Th, age model and stable isotope data from the Last Glacial Maximum to the ...
Paleoclimate records from the Middle East are sparse in comparison to other regions. The records as such could be useful to improve our understanding of natural variability in... -
Monthly interpolated geochemical data and linear extension rates from IODP Ex...
During the last deglacial transition, orbitally forced changes in the Northern Hemisphere temperature seasonality resulted in the change of global mean climate conditions.... -
Monthly interpolated geochemical data and linear extension rates from modern ...
Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ¹⁸O, δ¹³C) extracted along the growth axes of modern Porites corals recovered at Tahiti that grew between... -
Stable oxygen and carbon isotope data for the Mid-Pleistocene Transition (MPT)
To investigate potential changes in the North Atlantic intermediate water-mass configuration across the Mid-Pleistocene Transition (MPT; approx. 550-1200 ka) we utilize d18O and... -
Mulu Borneo stalagmite SC02 U/Th dating and oxygen and carbon stable isotopes...
Here are presented Mulu, Borneo (4°6'N, 114°53'E) Secret Cave stalagmite SC02 d18O and d13C values over Termination 1, published in Buckingham et al. (2022). U-Th ages were...