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Sea-surface temperature reconstruction of the South China Sea
The tropical ocean plays a major role in global climate. It is therefore crucial to establish the precise phase between tropical and high-latitude climate variability during... -
Sea-surface temperature reconstruction for sediment core GIK18287-3 in the tr...
The timing and magnitude of sea-surface temperature (SST) changes in the tropical southern South China Sea (SCS) during the last 16,500 years have been reconstructed on a... -
Tab. 10, AMS datings of sediment cores, Sunda Shelf
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(Table 12) Element analysis of surface sediments off Vietnam and from Sunda S...
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(Table 11) Carbon analysis of surface sediments off Vietnam and from Sunda shelf
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Stable carbon and oxygen isotope ratios of foraminifera in surface sediments ...
The relationship between planktonic and benthic foraminiferal stable-isotope values and oceanographic conditions and factors controlling isotopic variations are discussed on the... -
(Appendix XIIc) Coarse grain analysis of sediment core GIK18298-2
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(Appendix XIIb) Carbonate chemistry of sediment core GIK18300-2
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(Appendix XIIa) Stable isotope ratios of planktonic foraminifera of sediment ...
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(Appendix XI) Coarse grain analysis of sediment core GIK18312-2
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(Appendix Xb) Coarse grain analysis of sediment core GIK18314-2
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(Appendix Xa) Coarse grain analysis of sediment core GIK18302-2
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(Appendix IX) Coarse grain analysis of sediment core GIK18302-2
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(Appendix VIII) Coarse grain analysis of sediment core GIK18300-2
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(Appendix VII) Coarse grain analysis of sediment core GIK18299-1
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(Appendix VIc) Pollen content of sediment cores from the Sunda Shelf
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(Appendix VIa) N and C content of sediment core GIK18302-2
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(Appendix V) Stable isotope ratios of foraminifera of sediment core GIK18311-2
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(Appendix IV) Stable isotope ratios of Asterorotalia pulchella of sediment co...
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(Appendix III) Ash content of plant material in sediment cores from the Sunda...
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