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(Table S3) Geochemistry of ODP Hole 188-1166A
DEPTH, sediment/rock [m] = Top Depth [mbsf]CaO* refers to CaO in the silicate fraction. -
(Table S2) Geochemistry of IODP Hole 318-U1356A
DEPTH, sediment/rock = Top Depth (mbsf)CaO* refers to CaO in the silicate fraction. -
(Table A2) Age tie points for ODP Hole 188-1166A
Age tie points for Hole 1166A according to Gradstein et al. [2004] -
Sea surface temperature based on TEX86 as well as mean annual air temperature...
This dataset has no description
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Sea surface temperature based on TEX86 as well as mean annual air temperature...
This dataset has no description
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R-code of sporomorph analyses of IODP Hole 318-U1356A
This dataset has no description
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(Table S6) Calculated annual mean air temperature of IODP Hole 318-U1356A
Sediment depth is given in mbsf. All samples are from the work half of the sediment core. -
(Table S5) Taxa defining the upper and lower limits in the application of the...
Temperate rainforest biome, samples with counts >= 90, nearest living relatives (NLR) >= 5. Sediment depth is given in mbsf. -
(Table S4) Taxa defining the upper and lower limits in the application of the...
Paratropical rainforest biome, samples with counts >= 90, nearest living relatives (NLR) >= 5. Sediment depth is given in mbsf. -
(Table S3) Bioclimatic analysis for IODP Hole 318-U1356A based on Mosbrugger ...
Ts not available for some taxa. Sediment depth is given in mbsf. -
(Table S2) Bioclimatic analysis for IODP Hole 318-U1356A based on Greenwood e...
T sum not available for some taxa. Sediment depth is given in mbsf. -
(Tabld S1) Bulk geochemistry, TEX86, SST and BIT reconstruction at ODP Hole 2...
This dataset has no description
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Lower Albian Mazagan Plateau (Niveau Paquier) individuals per gram sediment o...
This dataset has no description
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Leaf-wax-based carbon isotopes of n-alkanoic acids from IODP Site 361-U1478
This dataset contains the leaf-wax-based carbon isotopes (d13C, ‰) from n-alkanoic acids of marine sediments from IODP Site 361-U1478, Mozambique Channel. The Site was drilled... -
(Supplementary Table 1) Iceberg-rafted debris (IBRD) mass accumulation rates ...
The Pliocene and Early Pleistocene, between 5.3 and 0.8 million years ago, span a transition from a global climate state that was 2-3 °C warmer than present with limited ice... -
(Table T1) Cenozoic and Mesozoic biostratigraphic datums of ODP Hole 210-1276A
Sediments recovered from Ocean Drilling Program Leg 210 Hole 1276A range in age from Early Cretaceous (earliest Albian) to Paleogene (earliest Oligocene). In this study, samples... -
Palynological counts from the Oligocene-Miocene of IODP Site 318-U1356, Wilke...
Palynological counts from IODP Leg 318 Hole U1356A, Cores 95R-11R, and the lithological facies as observed in Salabarnada et al., CP 2018. Reworked dinocysts (as by Bijl et al.,... -
Persistent monsoonal forcing of Mediterranean Outflow dynamics during the lat...
The mode and vigor of the global oceanic circulation critically depend on the salinity of (sub)surface water masses advected to the loci of deep-water formation. Within the... -
(Data S1) Palynological analysis of IODP and ODP sediment cores around the An...
The circum-Antarctic Southern Ocean is an important region for global marine food webs and carbon cycling because of sea-ice formation and its unique plankton ecosystem.... -
Age tie points and geochemistry of sediment cores from the Antarctic continen...
Few high-latitude terrestrial records document the timing and nature of the Cenozoic "Greenhouse" to "Icehouse" transition. Here we exploit the bulk geochemistry of marine...
