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Paleotemperature calclulated for the 120 k time slice
This dataset has no description
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Clay mineraology and grain size composition of surface sediments from South P...
The reconstruction of low-latitude ocean-atmosphere interactions is one of the major issues of (paleo-)environmental studies. The trade winds, extending over 20° to 30° of... -
Global data compilation of benthic data sets II
In this study we present a global distribution pattern and budget of the minimum flux of particulate organic carbon to the sea floor (J POC alpha). The estimations are based on... -
Stable carbon and oxygen isotope ratios of benthic and planktic foraminifera ...
Benthonic foraminifera in late Pleistocene deep-sea cores show significant variation in delta 13C with depth in sediment. This, and the report by Sommer et al., (in prep) of... -
Last Glacial Maximum (LGM) paleo-dust record
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Pre-industrial Holocene (pi-HOL) paleo-dust record
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Core top coccolithophore productivity compared to modern observations in the ...
This dataset has no description
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Core top chlorophyll concentration compared to modern observations in the eas...
This dataset has no description
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Core top alkenone (C37) data compared to modern observations in the eastern e...
This dataset has no description
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Core top sea surface temperature data compared to modern observations in the ...
This dataset has no description
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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... -
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 ...
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. -
(Table S1) Modern calibration environmental variables and coretop diatom spec...
This dataset has no description
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Database of previously published eastern equatorial Pacific δ¹⁸O and δ¹³C of ...
This dataset has no description
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Eastern Equatorial Pacific Holocene and Last Glacial Maximum stable isotopes ...
This dataset has no description
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(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...