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(Table A3) 230Th, aluminium, and opal in particle size fractions of surface s...
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(Table A1+A2) 230Th, 231Pa, 9Be, and 10Be in particle size fractions of surfa...
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(Table 2) Opal_230Th, 231Pa, 9Be, and 10Be by each grain size class in percen...
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(Table 4) Characterization of the particle fractions obtained by sieving and ...
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(Table 3) Contribution of Th and U isotopes by each grain size class in perce...
GeoB1028-4 and PS1769-1 indicates the core sites under more slowly accumulating conditions. -
(Table 2) Recovery and loss through the fractionation process
GeoB1028-4 and PS1769-1 indicates the core sites under more slowly accumulating conditions. -
(Table 1) Position and sedimentology of the studied sediment samples
a and b from Müller (2003a, 2003b).c and d unpublished data (personal communication G.Kuhn) averaged over depth intervals 1.60-1.71 m and 0.1-0.2 m, respectively.e TOC analyzed... -
(Table A2) Th and U specific activities in particle fractions of the carbonat...
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(Table A1) Opal content and concentrations of some elements in particle fract...
This dataset has no description
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(Table 1) Abundance (average and standard deviation) and opal input (average ...
The sediments from this core are made of a diatomaceous ooze containing ice rafted debris, low amount of organic matter and of carbonates. -
Susceptibility of sediment core PS1779-2
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Susceptibility of sediment core PS1776-8
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Susceptibility of sediment core PS1775-4
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Susceptibility of sediment core PS1774-5
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Susceptibility of sediment core PS1771-1
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Stable isotopes in opal of sediment core PS1786-1
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Abundance of organic-walled dinoflagellate cysts of sediment core PS1768-8
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Abundance of organic-walled dinoflagellate cysts of sediment core PS1756-5
This dataset has no description
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Standing stocks of benthic foraminifera, total organic carbon and carbonate c...
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Radiosonde PS16/05885 during POLARSTERN cruise ANT-VIII/3 on 1989-11-03 10:36h
Height of tropopause 12189 m, precipitable water content 1.7719 cm