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Sedimentation rates of surface sediments, a compilation from different sources
This dataset has no description
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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... -
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... -
Global compilation of benthic data sets I
Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary... -
Last interglacial and penultimate glacial sea surface temperature anomalies f...
Southern Ocean marine sediments provide an important archive of Quaternary glacial-interglacial climate changes. Sea surface temperature (SST) reconstructions in the Southern... -
Lithogenic thorium fluxes into South Atlantic surface sediments
We present the characteristics of the lithogenic components of seafloor surface sediments covering the entire South Atlantic Ocean (from the equator to Antarctica). These... -
End-member composition of South Atlantic surface sediments
We present the characteristics of the lithogenic components of seafloor surface sediments covering the entire South Atlantic Ocean (from the equator to Antarctica). These... -
Grain-size distributions of South Atlantic surface sediments
We present the characteristics of the lithogenic components of seafloor surface sediments covering the entire South Atlantic Ocean (from the equator to Antarctica). These... -
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. -
Apsorption units at wavenumbers of several samples
This dataset has no description
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Mineral content of several samples
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... -
(Table 1) Loadings for PC 1, 2, and 3 and percentage variance explained (v. e...
Table 1 in paper contains wrong core names. PS1034-3 = GeoB1034-3, PS1035-5 = GeoB1035-5, PS1214-1 = GeoB1214-1. Latitude and Longitude are switched. -
Table1: Barium excess and aluminium in porewater of surface sediments from th...
This dataset has no description
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(Table 2) Estimated sea surface temperatures and factor analysis based on rad...
This dataset has no description
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Abundance of planktonic foraminifera in surface sediments of the South Atlantic
This dataset has no description
