Solid-phase geochemistry of sediment cores from IODP Hole 370-C0023A

doi:doi:10.1594/PANGAEA.930858

Solid-phase geochemistry of sediment cores from IODP Hole 370-C0023A

The dataset includes solid-phase geochemistry data of sediment cores from Site C0023 (Hole A) that was recovered during International Ocean Discovery Program (IODP) Expedition 370 in the Nankai Trough offshore Japan in the Pacific Ocean (Drilling vessel Chikyu). Site C0023 was established on 17 September 2016. Coring terminated on 3 November 2016. Solid-phase geochemistry data include bulk iron (Fe), sulfur (S) and aluminum (Al) contents, chromium reducible sulfur (CRS) as well as algal lipid biomarker concentrations and stable carbon isotopes of total organic carbon (δ13C-TOC). The bulk element contents were determined by performing total acid digestions (dissolution of dry sediment in a mixture of 65% HNO3 (3 ml), 30% HCl (2 ml), and 40% suprapur® HF (0.5 ml) in a CEM Mars Xpress microwave system). Sequential iron extractions were performed after Poulton and Canfield (2005) and Henkel et al. (2016) to quantify the reactive iron pools (Fe aca, sodium acetate extraction; Fe hyam, hydroxylamine-HCl extraction; Fe di-ct, sodium dithionite/sodium citrate extraction; Fe oxa, oxalate/oxalic acid extraction). We further determined the amounts of Al (Al aca, Al hyam, Al di-ct, Al oxa) and silicon (Si; Si aca, Si hyam, Si di-ct, Si oxa) released by the different extraction steps for a selection of samples. All elemental contents (except for CRS) were measured by inductively coupled plasma – optical emission spectroscopy (ICP-OES; iCAP 7400, Thermo Fisher Scientific Inc.). CRS was extracted using a CrCl2 solution after Canfield et al. (1986) and Zhabina & Volkov (1978). All values are given in wt%. Algal lipid biomarker analysis was performed after Sturt et al. (2004) and HPLC-MS analyses after Becker et al. (2015). Biomarker concentrations are reported as the integrated peak area of the sum of all detected diols normalized to kg extracted sediment (PA/kg). Stable carbon isotopes of total organic carbon measurement occurred on an EA-IRMS system after complete decalcification of homogenized sediment samples with 10% HCl. The δ13C-TOC values are expressed relative to VPDB (Vienna Pee Dee Belemnite).

BibTex:

@dataset{Köster_Male_and_Kars_Myriam_and_Schubotz_Florence_and_Tsang_Man-Yin_and_Maisch_Markus_and_Kappler_Andreas_and_Morono_Yuki_and_Inagaki_Fumio_and_Heuer_Verena_B_and_Kasten_Sabine_and_Henkel_Susann_2021,
    abstract = {The dataset includes solid-phase geochemistry data of sediment cores from Site C0023 (Hole A) that was recovered during International Ocean Discovery Program (IODP) Expedition 370 in the Nankai Trough offshore Japan in the Pacific Ocean (Drilling vessel Chikyu). Site C0023 was established on 17 September 2016. Coring terminated on 3 November 2016.
Solid-phase geochemistry data include bulk iron (Fe), sulfur (S) and aluminum (Al) contents, chromium reducible sulfur (CRS) as well as algal lipid biomarker concentrations and stable carbon isotopes of total organic carbon (δ13C-TOC). The bulk element contents were determined by performing total acid digestions (dissolution of dry sediment in a mixture of 65% HNO3 (3 ml), 30% HCl (2 ml), and 40% suprapur® HF (0.5 ml) in a CEM Mars Xpress microwave system). Sequential iron extractions were performed after Poulton and Canfield (2005) and Henkel et al. (2016) to quantify the reactive iron pools (Fe aca, sodium acetate extraction; Fe hyam, hydroxylamine-HCl extraction; Fe di-ct, sodium dithionite/sodium citrate extraction; Fe oxa, oxalate/oxalic acid extraction). We further determined the amounts of Al (Al aca, Al hyam, Al di-ct, Al oxa) and silicon (Si; Si aca, Si hyam, Si di-ct, Si oxa) released by the different extraction steps for a selection of samples. All elemental contents (except for CRS) were measured by inductively coupled plasma – optical emission spectroscopy (ICP-OES; iCAP 7400, Thermo Fisher Scientific Inc.). CRS was extracted using a CrCl2 solution after Canfield et al. (1986) and Zhabina & Volkov (1978). All values are given in wt%. Algal lipid biomarker analysis was performed after Sturt et al. (2004) and HPLC-MS analyses after Becker et al. (2015). Biomarker concentrations are reported as the integrated peak area of the sum of all detected diols normalized to kg extracted sediment (PA/kg). Stable carbon isotopes of total organic carbon measurement occurred on an EA-IRMS system after complete decalcification of homogenized sediment samples with 10% HCl. The δ13C-TOC values are expressed relative to VPDB (Vienna Pee Dee Belemnite).},
    author = {Köster, Male and Kars, Myriam and Schubotz, Florence and Tsang, Man-Yin and Maisch, Markus and Kappler, Andreas and Morono, Yuki and Inagaki, Fumio and Heuer, Verena B and Kasten, Sabine and Henkel, Susann},
    doi = {10.1594/PANGAEA.930858},
    institution = {PANGAEA (Geophysics)},
    keyword = {'Hole A', 'IODP Expedition 370', 'Nankai Trough', 'Site C0023'},
    title = {Solid-phase geochemistry of sediment cores from IODP Hole 370-C0023A},
    url = {https://service.tib.eu/ldmservice/vdataset/png-doi-10-1594-pangaea-930858},
    year = {2021}
}