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(Supplement T1) Clay mineral compositions at the Aleutian Basin of the Bering...
The clay mineral composition at IODP Exp. 323 Site U1343 in the Bering Sea was analyzed so as to unravel their provenance over glacial-interglacial cycles for the last 2.4 Ma.... -
Diatom analysis in subsample smear slides from IODP Hole 323-U1340A
The dataset of diatom analysis in the subsample smear slides obtained from Sections IODP323-U1340A-10H-1W, 134-149cm, 10H-2W, 001-116cm, and 14H-1W, 60-88cm. -
Silicic acid utilisation from IODP Site 323-U1343
This dataset has no description
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Silicic acid supply from IODP Site 323-U1343
This dataset has no description
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δ30Si from IODP Site 323-U1343
This dataset has no description
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Diatom assemblage data from IODP Site 323-U1343
This dataset has no description
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Relative abundance of Amphimelissa setosa in core sediments and the interpola...
BEA: Beaufort Sea; BER: Bering Sea; CHU: Chukchi Sea; ECS: East China Sea; ESS: East Siberian Sea; GOA: Gulf of Alaska; GRE: Greenland Sea; ICE: Iceland Sea; NOR: Norwegian Sea;... -
(Table 1) Age determination of IODP Hole 323-U1340A
DEPTH, sediment/rock [m] is given in mcd. -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
Sea-ice biomarkers, benthic and planktonic foraminiferal geochemistry, and be...
The dataset compiles sea-ice biomarkers (IP25, HBI II, HBI III, Triene E, Brassicasterol, Campesterol, Cholesterol, β- sitosterol) together with benthic and planktonic... -
Diatom oxygen and silicon isotopes data from IODP Hole 323-U1341B in the Beri...
The Bering Sea is one of the most biologically productive regions in the marine system and plays a key role in regulating the flow of waters to the Arctic Ocean and into the... -
Diatom fragment composition in the back-scattered electron images obtained fr...
The dataset of diatom fragment composition in the back-scattered electron images (BSEI) of cross thin section of laminated sediments and lamina thickness for Sections... -
Diatom abundance from IODP Site 323-U1340
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we... -
Isotopes of benthic foraminifera from different holes of IODP Site 323-U1342
This dataset has no description
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Inductively coupled plasma (ICP) analyses of IODP Site 323-U1341B
This dataset has no description
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X-ray fluorescence (XRF) analyses of IODP Hole 323-U1343E
This dataset has no description
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X-ray fluorescence (XRF) analyses of IODP Hole 323-U1343A
This dataset has no description
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(Table 2) Key diatom species of IODP Hole 323-U1340A
DEPTH, sediment/rock [m] is given in mcd. -
(Appendix 7) Stable isotope rates, and sea surface temperature reconstruction...
DEPTH, sediment/rock [m] is given in mcd. -
(Appendix 5) Bulk density of IODP Hole 323-U1340A
DEPTH, sediment/rock [m] is given in mbsf.
