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Maximum annual SST estimates during the early LIG (129-124 ka; 189 sites)
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
(Dataset 1) Pliocene alkenone unsaturation index (Uk37) and SST anomalies of ...
Change history in September 2021 it was found, that the ages in all "Dataset 1" datasets were declared here as being in "ka BP" but they were actually in "Ma". To correct this... -
Annual SST estimates for the Last Interglacial (129-116 ka BP)
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
(Supplement S3) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
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Late Miocene carbon isotope and paleoproductivity record of ODP Hole 184-1146A
This dataset has no description
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(Table S3) Mg/Ca seawater estimation for ODP Site 184-1143
Mg/Casw interpolated at 2kyr resolution then smoothed (600 kyr) -
(Table S3) Mg/Ca seawater back-calculated from ODP Site 184-1143 Mg/Ca and TE...
This dataset has no description
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(Table S2) Globigerinoides sacculifer Mg/Ca data and temperature estimates fo...
DEPTH, sediment/rock [m] is given in mcd. -
(Table S1) GDGT abundance, temperature estimates, and BIT indices for ODP Sit...
DEPTH, sediment/rock [m] is given in mcd. -
(Table S1) Comparison of ages for ODP Site 184-1146 biostratigraphic datums
This dataset has no description
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(Appendix 2) Mg/Ca ratios of Globigerinoides ruber from ODP Site 184-1143
Sediment depth (m) is composite depth (mcd) -
(Table 1) Estimated age for the last occurrence of Globoquadrina dehiscens
Ages were transfered to the timscale of Berggren et al. (1995) -
Stable oxygen and carbon isotope ratios measured on benthic foraminifera from...
Measured were epifaunal foraminifera >250 µm, e.g. Planulina wuellerstorfi or Cibicidoides mundulus, except in ~6% samples, where either Cibicidoides barnetti, C. bradyi, C.... -
(Table S3) Age model of ODP Site 184-1146
This dataset has no description
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Stable isotope ratios measured on benthic foraminifera Planulina wuellerstorf...
This dataset has no description
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Benthic foraminifera extinction groups population in Middle Miocene sediments
Fifty-eight species of elongate, cylindrical benthic foraminifera (here referred to as the Extinction Group) belonging to genera that became extinct during the mid-Pleistocene... -
Geochemistry and stable isotope record of benthic foraminifera of Miocene sed...
The processes causing the middle Miocene global cooling, which marked the Earth's final transition into an 'icehouse' climate about 13.9 million years ago (Myr ago) (Flower and... -
Late Miocene development of the western Pacific warm pool: Planktonic foramin...
The disappearance at ~10 Ma of the deep dwelling planktonic foraminifer Globoquadrina dehiscens from the western Pacific including the South China Sea was about 3 Myr earlier... -
Stable isotopes measured on Miocene benthic foraminifera from ODP sites 202-1...
One of the most enigmatic features of Cenozoic long-term climate evolution is the long-lasting positive carbon-isotope excursion or “Monterey Excursion”, which started during a... -
Plio-Pleistocene tropical alkenone SST reconstructions for ODP Site 184-1146
This dataset has no description
