Salt- corrected chemical compounds, elemental concentrations and Ni isotope data of the solid phase for sediment cores collected during ALKOR cruise AL543

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Main Authors: Fleischmann, Sarah, Scholz, Florian, Du, Jianghui, Scholten, Jan Christoph
Format: Dataset Open Access
Language:en
Published: PANGAEA 2024
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author Fleischmann, Sarah
Scholz, Florian
Du, Jianghui
Scholten, Jan Christoph
author_facet Fleischmann, Sarah
Scholz, Florian
Du, Jianghui
Scholten, Jan Christoph
collection Datos científicos de ciencias marinas y ambientales
contents The reactivity and isotope fractionation of Ni is strongly influenced by biological and redox-related processes in the ocean, giving the isotope system (expressed as δ60 Ni) some potential for studying past ocean environments. This requires, however, a profound understanding of its modern elemental and isotopic oceanic mass balance. In order to better understand mechanisms determining fluxes of Ni and its isotopes from the sediment-porewater system in reducing ocean settings, we present trace metal concentrations and Ni isotope data from sediments, porewaters and the water column of the shallow-water Kiel Bight, in the southwestern Baltic Sea. The samples were collected during RV Alkor cruise AL543. Trace metal concentrations in porewater, bottom water and BTP bottom water samples were measured on a Thermo Scientific Element XR and Nickel isotope compositions were measured using a Thermo Scientific Neptune Plus MC-ICP-MS. Digestion solutions of sediments and suspended particulate matter were measured by ICP-OES.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_974021
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle Salt- corrected chemical compounds, elemental concentrations and Ni isotope data of the solid phase for sediment cores collected during ALKOR cruise AL543
Fleischmann, Sarah
Scholz, Florian
Du, Jianghui
Scholten, Jan Christoph
AL543; AL543_10-2; AL543_11-2; AL543_12-5; AL543_13-2; AL543_3-2; AL543_4-3; AL543_5-3; AL543_7-3; AL543_8-4; AL543_9-2; Alkor (1990); Aluminium; Baltic Sea; Carbon, organic, total; Depth, bottom/max; Depth, top/min; Depth comment; Event label; Factor; Iron; isotope data; LATITUDE; LONGITUDE; Manganese; MIC; MiniCorer; nickel; Nickel; Nickel, error; Nitrogen, total; organic-rich sediments; porewater; Sulfur, total; The Little Belt; δ60Ni
The reactivity and isotope fractionation of Ni is strongly influenced by biological and redox-related processes in the ocean, giving the isotope system (expressed as δ60 Ni) some potential for studying past ocean environments. This requires, however, a profound understanding of its modern elemental and isotopic oceanic mass balance. In order to better understand mechanisms determining fluxes of Ni and its isotopes from the sediment-porewater system in reducing ocean settings, we present trace metal concentrations and Ni isotope data from sediments, porewaters and the water column of the shallow-water Kiel Bight, in the southwestern Baltic Sea. The samples were collected during RV Alkor cruise AL543. Trace metal concentrations in porewater, bottom water and BTP bottom water samples were measured on a Thermo Scientific Element XR and Nickel isotope compositions were measured using a Thermo Scientific Neptune Plus MC-ICP-MS. Digestion solutions of sediments and suspended particulate matter were measured by ICP-OES.
title Salt- corrected chemical compounds, elemental concentrations and Ni isotope data of the solid phase for sediment cores collected during ALKOR cruise AL543
topic AL543; AL543_10-2; AL543_11-2; AL543_12-5; AL543_13-2; AL543_3-2; AL543_4-3; AL543_5-3; AL543_7-3; AL543_8-4; AL543_9-2; Alkor (1990); Aluminium; Baltic Sea; Carbon, organic, total; Depth, bottom/max; Depth, top/min; Depth comment; Event label; Factor; Iron; isotope data; LATITUDE; LONGITUDE; Manganese; MIC; MiniCorer; nickel; Nickel; Nickel, error; Nitrogen, total; organic-rich sediments; porewater; Sulfur, total; The Little Belt; δ60Ni
url https://doi.org/10.1594/PANGAEA.974021