Ex situ sulphate reduction and methane oxidation rates of sediment at the rim of a vesicomyd clam colony in the Japan Deep Sea Trench (dive 956)

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Autori principali: Felden, Janine, Wenzhöfer, Frank
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2014
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author Felden, Janine
Wenzhöfer, Frank
author_facet Felden, Janine
Wenzhöfer, Frank
collection Datos científicos de ciencias marinas y ambientales
contents Sediment samples were collected from the rim of a large vesicomyid clam colony in the Japan Deep Sea Trench. Immediately after sample recovery onboard, the sediment core was sub-sampled for ex situ rate measurements. Sulfate reduction and anaerobic oxidation of methane were measured ex situ by the whole core injection method with three replicate measurements for each method. We incubated the samples at in situ temperature (1.5°C) for 48 hours with either 14C-methane (dissolved in water, 2.5 kBq) or carrier-free 35S-sulfate (dissolved in water, 50 kBq). Sediment was fixed in 25 ml sodium hydroxide (NaOH) solution (2.5%, w/v) or 20 ml ZnAc solution (20%, w/v) for AOM or SR, respectively. Turnover rates were measured as previously described (Kallmeyer et al., 2004; Treude et al., 2003).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_827104
institution PANGAEA
language en
publishDate 2014
publisher PANGAEA
record_format pangaea
spellingShingle Ex situ sulphate reduction and methane oxidation rates of sediment at the rim of a vesicomyd clam colony in the Japan Deep Sea Trench (dive 956)
Felden, Janine
Wenzhöfer, Frank
6K-956-CR; 6K-956-CRW; 6K-956-CW; 6K-956-CY; Center for Marine Environmental Sciences; DEPTH, sediment/rock; Event label; MARUM; Methane, oxidation rate, anaerobic; PUC; Push corer; Radioactive tracer injection, Anion exchange chromatography, scintillation count; Radioactive tracer injection, Gas Chromatography and scintillation counting; Sanriku Escarpment in the Japan Trench; Sulfate reduction rate; YK06-05; Yokosuka
Sediment samples were collected from the rim of a large vesicomyid clam colony in the Japan Deep Sea Trench. Immediately after sample recovery onboard, the sediment core was sub-sampled for ex situ rate measurements. Sulfate reduction and anaerobic oxidation of methane were measured ex situ by the whole core injection method with three replicate measurements for each method. We incubated the samples at in situ temperature (1.5°C) for 48 hours with either 14C-methane (dissolved in water, 2.5 kBq) or carrier-free 35S-sulfate (dissolved in water, 50 kBq). Sediment was fixed in 25 ml sodium hydroxide (NaOH) solution (2.5%, w/v) or 20 ml ZnAc solution (20%, w/v) for AOM or SR, respectively. Turnover rates were measured as previously described (Kallmeyer et al., 2004; Treude et al., 2003).
title Ex situ sulphate reduction and methane oxidation rates of sediment at the rim of a vesicomyd clam colony in the Japan Deep Sea Trench (dive 956)
topic 6K-956-CR; 6K-956-CRW; 6K-956-CW; 6K-956-CY; Center for Marine Environmental Sciences; DEPTH, sediment/rock; Event label; MARUM; Methane, oxidation rate, anaerobic; PUC; Push corer; Radioactive tracer injection, Anion exchange chromatography, scintillation count; Radioactive tracer injection, Gas Chromatography and scintillation counting; Sanriku Escarpment in the Japan Trench; Sulfate reduction rate; YK06-05; Yokosuka
url https://doi.org/10.1594/PANGAEA.827104