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Carbon concentration of sediment core LV76-21
The total carbon and inorganic carbon (CaCO3) contents were measured in sediment slices of 1 cm thickness with 2 cm resolution using an AN-7529 coulometer (Gorbarenko et al.,... -
Benthic foraminifera abundances of sediment core LV76-21
Benthic foraminifera were studied in the core LV76-21 sediments sampled in 1 cm-thick slices. All the samples were dried, weighted, and wet sieved using a 63 μm sieve. The... -
Size fraction >63 µm determination of sediment core LV76-21
Sediment for IRD determination was sampled from 1 cm-thick slices with steps of 2–4 cm through the core. Samples with a dry weight of approximately 10 g were wet sieved using a... -
Size fraction >150 µm determination of sediment core LV76-21
Sediment for IRD determination was sampled from 1 cm-thick slices with steps of 2–4 cm through the core. Samples with a dry weight of approximately 10 g were wet sieved using a... -
Age determination of sediment core LV76-21
Eight samples of monospecific planktic foraminifera of Neogloboquadrina pachyderma (sin.) with a weight of 4–6 mg were picked from the >125‐μm size fraction and measured in... -
PIP25 indexes and Spring/Summer sea ice concentration (Sp/SuSIC) (Estuarine s...
The PIP25 indexes calculated by IP25 and phytoplankton biomarkers (Brassicasterol, Dinosterol, HBI-III) in the East Siberian Sea. The calculation methods based on Mueller et... -
PIP25 indexes and Spring/Summer sea ice concentration (Sp/SuSIC) (Estuarine s...
The PIP25 indexes calculated by IP25 and phytoplankton biomarkers (Brassicasterol, Dinosterol, HBI-III) in the East Siberian Sea. To better understand the riverine influence, we... -
Bulk parameters and biomarker data from surface sediment across the East Sibe...
A dataset of 42 collected surface sediment samples from the East Siberian Sea by analysis of Arctic sea ice (IP25) and open water phytoplankton biomarkers (Brassicasterol,... -
(Table 4) Chemical composition of bottom sediments from the Sea of Okhotsk
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(Table 3) Mineral composition of clay fraction from bottom sediments of the S...
0 = traces; + = kaolinite is inferred from resolution of reflection doublets of chlorite (004) and kaolinite (002) in diffractograms; empty digital cells = questionable data. -
(Table 2) Physical properties of Holocene and Upper Pleistocene bottom sedime...
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(Table 1) Sedimentation rates and accumulation rates of Upper Pleistocene and...
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(Table 1) Mineral compositions of volcanic glass interlayers in sediment core...
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(Table 2) Average sedimentation and accumulation rates of Sea of Okhotsk bott...
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(Table 1) Manganese contents in sediment cores and in the upper reduced sedim...
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(Table 2) Isotopic composition of authigenic carbonates from the area of the ...
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(Table 1) Chemical composition of authigenic carbonates from the area of the ...
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(Table 2) Contents and accumulation rates of Hg in cores of Upper Quaternary ...
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(Table 1) Core subdivisions, sedimentation rates, and bulk mass accumulation ...
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Results of analysis of sediment core LV76-21 from Detroit Seamount
The sediment core LV76-21 was recovered from northwest of the Detroit Seamount (51°34’N, 167°15.7’E; water depth 2,769 m) using a gravity corer on the R/V “Akademik M.A....