-
(Supplement 1) Relative abundance of planktic foraminifera in sediments of th...
This dataset has no description
-
δ¹¹B, Mg/Ca, and input variables for calculated pH and CO₂ during the late Pl...
This dataset has no description
-
Mg/Ca and different methods to calculate SST at ODP Sites 165-999 and 144-871
This dataset has no description
-
Isotopes measured on Cibicidoides wuellerstorfi from ODP Site 165-999
This dataset has no description
-
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... -
Dynamic storage of glacial CO2 in the Atlantic Ocean revealed by boron [CO32-...
This dataset has no description
-
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. -
Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
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. -
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. -
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 S1, Figure 2) Sedimentation rates for 108 sediment core sites during t...
The SR errors in Fig.2 are given by the averaged values of 'Error [+, 97.5%]' and 'Error [-, 2.5%]'.The calculation focused on 19-21 ka since the age model did not cover the... -
(Table S4c) Sr-isotope record of ODP Site 165-1000A
Sediment depth is given in mcd. Age after Steph et al. (2010). -
(Table S4b) Sr-isotope record of ODP Hole 165-999A
Sediment depth is given in mcd. Age after Haug and Tiedemann (1998), Steph et al. (2006). -
(Table S3b) Pb-isotope record of ODP Hole 165-999A
Sediment depth is given in mcd. Age after Gaug and Tiedemann (1998), Steph et al. (2006). -
(Table S2d) Nd-isotope record of ODP Site 165-1000
Sediment depth is given in mcd. Age after Steph et al. (2010). -
(Table S2c) Nd-isotope record of ODP Hole 165-998A
Sediment depth is given in mcd. Age after Kameo and Bralower (2000). -
(Table S2b) Nd-isotope record of ODP Hole 165-999A
Sediment depth is given in mcd. Age after Haug and Tiedemann (1998), Steph et al. (2006).