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Compilation of planktonic foraminiferal census counts from the Southern Hemis...
We present an improved database of planktonic foraminiferal census counts from the Southern Hemisphere Oceans (SHO) from 15°S to 64°S. The SHO database combines 3 existing... -
(Table S1) Planktonic foraminifera abundances for the 1223 surface sediment s...
Our training set (SH0911C2, available from http://www.ncdc.noaa.gov/paleo/paleo.html) augments that used by Crundwell el al . [2008, Figure 2] with additional data from Mohtadi... -
(Table 3) Dead benthic foraminifera in surface sediments from the eastern Sou...
This dataset has no description
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(Table 2) Live benthic foraminifera in surface sediments from the eastern Sou...
This dataset has no description
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Foraminifera and stable isotopes of sediment core PS2076-3
This dataset has no description
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Foraminifera and stable isotopes of sediment core PS2076-1
This dataset has no description
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Wet chemical surface ozone measurements during POLARSTERN cruise ANT-IX/3 and...
The destinations are described in Bathmann et al. (1992). Please note, that the positions were taken from the mastertrack of the respective cruise. The mastertrack of PS18/3 is... -
Meteorological observations during POLARSTERN cruise ANT-IX/4
This dataset has no description
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Abundance of organic-walled dinoflagellate cysts of sediment core PS2082-1
This dataset has no description
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δ18O and δ13C of Cibicidoides wuellerstorfi and related species and carbonate...
The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are... -
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean
We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle... -
Compilation of delta 18O data from planktonic foraminifera in surface sediment
Note that the exact depth in sediment is not given in this compilation. -
SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
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. -
Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
Annual SST estimates from the late Marine Isotope Stage 6 (140-135 kyr) and c...
This dataset has no description
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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. -
SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
Note, that we have assumed a thermal equator of 5 degrees North, where sites above this latitude 'Summer' = JJA, and 'Winter' = DJF. Sites south of this line have 'Summer'... -
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. -
Sedimentation rates of surface sediments, a compilation from different sources
This dataset has no description
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Total organic carbon content in surface sediments, a compilation from differe...
This dataset has no description
