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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... -
(Table 2) Northeast Atlantic core top oxygen isotope measurements
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Total organic carbon content in surface sediments, a compilation from differe...
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Distribution of planktic foraminifera in surface sediments of the Atlantic Oc...
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Global core-top calibration of UK37 (update)
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Documentation of sediment core D11958
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Documentation of sediment core D11957
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Physical properties of sediment core D11958#6
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Physical properties of sediment core D11957#5
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Mapping of C4 plant input from North West Africa into North East Atlantic sed...
Mapping the abundance of 13C in leaf-wax components in surface sediments recovered from the seafloor off northwest Africa (0–35°N) reveals a clear pattern of delta13C... -
Mineralogy and age determination of sediment core D11957P
The Tore Seamount is a circular, volcano-like feature 100 km in diameter with its summit at 2200 m water depth and a small, 5000 m deep basin in its interior. It is situated... -
Paleotemperature and productivity reconstruction of sediment core D11957P on ...
Foraminifera counts and climatic assemblages from the Tore Seamount are used to approach the glacial and interglacial changes in temperature and productivity on the Iberian... -
Stable carbon isotope values of higher-plant derived C29 n-alkanes isolated f...
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(Table 2) Comparison between dolomite, calcite and quartz for Heinrich layers...
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(Table 3) Calculated sea surface temperature and paleoproductivity of sedimen...
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(Table 2) Distribution of planktic foraminifers of sediment core D11957P
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(Fig. 3) Age model of sediment core D11957P
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(Table 5) Stable isotopes of planktonic foraminifera from sediment core D11957P
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(Table 4) Calcium carbonate and total organic carbon content of sediment core...
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(Table 1) Sedimentology of core D11957P
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