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author Pape, Thomas
Malnati, Janice
Tseng, Yiting
Bohrmann, Gerhard
author_facet Pape, Thomas
Malnati, Janice
Tseng, Yiting
Bohrmann, Gerhard
collection Datos científicos de ciencias marinas y ambientales
contents Shallow sediment cores were collected with a gravity corer and a multi corer from several sites at the Sartori Mud Volcano in the Calabrian accretionary prism during cruise SO278 with R/V SONNE. In order to determine ex-situ concentrations and stable C and H isotopic compositions of methane dissolved in pore water, sediment samples were taken from the sediment cores with cut-off syringes and transferred into glass vials. Methane concentrations in the headspace gas were determined by use of gas chromatography (GC) and used to calculate concentrations of methane dissolved in pore water (uncorrected for sediment porosity and Bunsen coefficient). Stable C and H isotopic compositions of methane were determined by use of GC-isotope ratio mass spectrometry.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_953903
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Concentrations of methane in sediment core GeoB24365-1 from the Calabrian accretionary wedge, RV Sonne cruise SO278
Pape, Thomas
Malnati, Janice
Tseng, Yiting
Bohrmann, Gerhard
Calabrian accretionary prism; Center for Marine Environmental Sciences; DEPTH, sediment/rock; Device type; Gas chromatography; GeoB24365-1; GPF 19-2-007H; Headspace Gas; Ionian Sea; MARUM; Mediterranean Ridge accretionary complex; Mediterranean Sea; Methane; Methane concentration; MUC; MultiCorer; Optional event label; pore water dissolved methane; R/V SONNE; Sample type; Sartori mud volcano; SO278; SO278_65-1; Sonne_2; stable carbon isotope; stable hydrogen isotope (0)
Shallow sediment cores were collected with a gravity corer and a multi corer from several sites at the Sartori Mud Volcano in the Calabrian accretionary prism during cruise SO278 with R/V SONNE. In order to determine ex-situ concentrations and stable C and H isotopic compositions of methane dissolved in pore water, sediment samples were taken from the sediment cores with cut-off syringes and transferred into glass vials. Methane concentrations in the headspace gas were determined by use of gas chromatography (GC) and used to calculate concentrations of methane dissolved in pore water (uncorrected for sediment porosity and Bunsen coefficient). Stable C and H isotopic compositions of methane were determined by use of GC-isotope ratio mass spectrometry.
title Concentrations of methane in sediment core GeoB24365-1 from the Calabrian accretionary wedge, RV Sonne cruise SO278
topic Calabrian accretionary prism; Center for Marine Environmental Sciences; DEPTH, sediment/rock; Device type; Gas chromatography; GeoB24365-1; GPF 19-2-007H; Headspace Gas; Ionian Sea; MARUM; Mediterranean Ridge accretionary complex; Mediterranean Sea; Methane; Methane concentration; MUC; MultiCorer; Optional event label; pore water dissolved methane; R/V SONNE; Sample type; Sartori mud volcano; SO278; SO278_65-1; Sonne_2; stable carbon isotope; stable hydrogen isotope (0)
url https://doi.org/10.1594/PANGAEA.953903