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δ¹¹B, Mg/Ca, and input variables for calculated pH and CO₂ during the late Pl...
This dataset has no description
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Mg/Ca and different methods to calculate SST at ODP Sites 165-999 and 144-871
This dataset has no description
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Isotopes measured on Cibicidoides wuellerstorfi from ODP Site 165-999
This dataset has no description
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δ¹¹B-derived pCO₂ calculated with different treatments of Mg/Ca-derived SST a...
pCO₂ (in parts per million) calculated from δ¹¹B as the maximum probability of 10,000 realisations of the Monte Carlo simulation, and calculated with different Mg/Ca-temperature... -
(Table 3b) Strontium isotopic results for ODP Site 165-1000
(a) age model Kameo K, Bralower TJ. Neogene calcareous nannofossil biostratigraphy of Sites 998, 999, and 1000, Caribbean Sea. Proc ODP, Scientific Results 165, (2000).(b)... -
(Table 2b) Neodymium isotopic results for ODP Site 165-1000
(a) age model Kameo K, Bralower TJ. Neogene calcareous nannofossil biostratigraphy of Sites 998, 999, and 1000, Caribbean Sea. Proc ODP, Scientific Results 165, (2000).(b)... -
Age-depth model of sediment core 165-1002 and associated dating uncertainty
Undatable run on 2019-01-09 15:42:36. nsim=10000 bootpc=90 xfactor=0.1 combine=Yes -
A summary of consistently dated Atlantic sediment cores over the last 40 thou...
Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear... -
(Table 3) Definition of 14C plateaus for sediment core 165-1002
This dataset has no description
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(Table 2d) Planktic 14C and 14C reservoir ages of sediment core 165-1002
All 14C dates are rounded to decades. Planktic plateau boundaries were either defined at or in between single 14C ages of the records. Many planktic 14C dates of the ODP 1002... -
(Supplement 1) Relative abundance of planktic foraminifera in sediments of th...
This dataset has no description
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World Ocean 14C plateau tuning
On the basis of minor time scale adjustments including the synchronization on IntCal20 the Suigetsu-based atmospheric 14C plateau structures are shown to be authentic. Their... -
Sea surface temperature anomalies for Pliocene interglacial KM5c (PlioVAR)
We examine a single interglacial during the late Pliocene (KM5c, ca. 3.205 +/- 0.01 Ma) when atmospheric CO2 concentrations were higher than pre-industrial, but similar to today... -
Downcore Florisphaera profunda
This dataset has no description
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Carbonate scenarios analysis from different sources of Fluid inclusions, CCD ...
Carbonate scenario analysis from Horita et al (2002) Fluid inclusions, Palike et al. (2012) CCD reconstruction and various boron isotopic seawater reconstructions. -
Carbonate scenarios analysis from different sources of Fluid inclusions, CCD ...
Carbonate scenario analysis from Horita et al (2002) Fluid inclusions, Palike et al. (2012) CCD reconstruction and various boron isotopic seawater reconstructions. -
Carbonate scenarios analysis from different sources of Fluid inclusions, CCD ...
Carbonate scenario analysis from Horita et al (2002) Fluid inclusions, Palike et al. (2012) CCD reconstruction and various boron isotopic seawater reconstructions. -
Late Pleistocene isotopes analysis from ODP Site 165-999
This dataset has no description
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(Supplement S3) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
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(Table S1) Globigerinoides sacculifer Boron isotope ratios of ODP Hole 165-999A
everal hypotheses have been put forward to explain the onset of intensive glaciations on Greenland, Scandinavia, and North America during the Pliocene epoch between 3.6 and 2.7...