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Stable oxygen isotope record of Neogloboquadrina pachyderma s of sediment cor...
Sediments for the δ18O of planktic and benthic foraminifera analysis from core LV76-21 were sampled from 1 cm-thick slices with step of 2–5 cm along the core length.... -
Element concentrations of sediment core LV76-21
Nearly 30 mg of sediment was sampled with steps of 1 cm through the core depth for element content analyses. The sediment was compressed into tablets of 5 mm in diameter and... -
Color b* value of sediment core LV76-21
The color b values are widely used as a paleoproductivity proxy for the NW Pacific and its marginal seas (Nürnberg and Tiedemann, 2004; Riethdorf et al., 2013). The color b... -
Stable oxygen isotope record of Cibicidoides spp. of sediment core LV76-21
Sediments for the δ18O of planktic and benthic foraminifera analysis from core LV76-21 were sampled from 1 cm-thick slices with step of 2–5 cm along the core length.... -
Chlorin concentration of sediment core LV76-21
The sediment for chlorin determination was sampled in slices of 1 cm thick with a resolution of 1 cm. Chlorin content is the product of chlorophyll-a transformation in sediments... -
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... -
Sedimentological data sets from the prehistoric site of Ajor Pazi (northern I...
During a rescue excavation in 2018, 136 sedimentary bulk samples were collected from sediment cross-sections at the prehistoric site of Ajor Pazi (northern Iran). This study... -
Rock magnetic properties of IODP Holes 375-U1518E and 375-U1518F
Hemipelagic sediments contained in 7 cc plastic cubes were analyzed for paleomagnetic and rock magnetic properties. Samples were collected from Holes U1518E and U1518F drilled... -
The magnetostratigraphy and cyclostratigraphy age data, and MS and NGR data u...
The IODP Expedition 368 began drilling in the South China Sea in 2017. The initial chronology of Site 368-U1505, including magnetostratigraphy and biostratigraphy, was completed... -
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.... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1i
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole VB1
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1a
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1d
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied... -
Intercorrelation of down-core variations of the high-resolution magnetic susc...
Down-core variations of the high-resolution magnetic susceptibility (0.1 cm steps)have been obtained for kasten and pilot cores from sites CON01-603 and CON01-605. This allowed... -
Magnetic Susceptibility of Cuttings of the KTB Pilot Hole HB1g (special samples)
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied...