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Diatoms in surface sediments
Data are accessible on request: Rainer.Gersonde@awi.de -
Meteorological observations during POLARSTERN cruise ANT-VI/2
This dataset has no description
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Age models of west off Antarctic Peninsula sediment cores
This dataset has no description
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Magnetic susceptibility of sediment core PS1565-2
This dataset has no description
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Grain-size and mineral composition, and water content of sediment core PS1565-2
This dataset has no description
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Element analysis of sediment core PS1565-2
This dataset has no description
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IRD counts in sediment core PS1565-2
This dataset has no description
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Multibeam survey (latitude, longitude, depth) from POLARSTERN cruise ANT-VI/2
This dataset has no description
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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 1) Distribution of tephra layers in sediment cores from the Bellingsha...
This dataset has no description
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Clay mineralogy of ODP Leg 178 sites
The clay mineral compositions of upper Miocene to Quaternary sediments recovered at Ocean Drilling Program (ODP) Leg 178, Sites 1095 and 1096, from the continental rise west of... -
Susceptibility of surface sediments from the Southern Ocean
measured on dry samples -
Physical oceanography during POLARSTERN cruise ANT-VI/2
This dataset has no description
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Ice-rafted debris in surface sediments from the Southern Ocean
This dataset has no description
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Magnetic susceptibility and ice-rafted debris in surface sediments of the Atl...
Spatial distribution of magnetic susceptibility and the gravel fraction in surface sediments in the Atlantic sector of the Southern Ocean were investigated to reconstruct source... -
Overview images and shape files from multibeam profiles during POLARSTERN cru...
This dataset has no description
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Station list and links to master tracks in different resolutions of POLARSTER...
This dataset has no description
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Wet chemical surface ozone measurements during POLARSTERN cruise ANT-VI/1-2 (...
The destinations are described in Fütterer (1986). It is possible that the high ozone peak at 22.5°S may be due to both stratospheric intrusion and long-distance transport from... -
Clay mineralogy of sediment core PS1565-2
This dataset has no description
