Sulphate reduction rates of Håkon Mosby mud volcano sediments measured at station MSM16/2_823-1 (Z3-S3, old flow surface)


Autoria(s): Felden, Janine; Boetius, Antje
Cobertura

LATITUDE: 72.002700 * LONGITUDE: 14.732467 * DATE/TIME START: 2010-09-28T09:54:00 * DATE/TIME END: 2010-09-28T09:54:00 * MINIMUM DEPTH, sediment/rock: 0.005 m * MAXIMUM DEPTH, sediment/rock: 0.095 m

Data(s)

26/04/2013

Formato

text/tab-separated-values, 19 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.810732

Idioma(s)

en

Publicador

PANGAEA

Relação

doi:10.1594/PANGAEA.861266

Ruff, S Emil; Felden, Janine; Gruber-Vodicka, Harald R; Marcon, Yann; Knittel, Katrin; Ramette, Alban; Boetius, Antje (2016): Disturbance and recovery of deep-sea methanotrophic communities.

Direitos

Access constraints: access rights needed

Fonte

Max-Planck-Institut für Marine Mikrobiologie

Palavras-Chave #DEPTH, sediment/rock; ESONET; European Seafloor Observatory Network; Håkon Mosby Mud Volcano; HERMIONE; Hotspot Ecosystem Research and Mans Impact On European Seas; LOOME; Maria S. Merian; MSM16/2; MSM16/2_823-1; MUC; MultiCorer; Radioactive tracer injection; Sulfate reduction rate
Tipo

Dataset

Resumo

Turnover rates were determined for surface sediment cores obtained in 2009 and 2010. Sulfate reduction (SR) were measured ex situ by the whole core injection method (doi:10.1080/01490457809377722). We incubated the samples at in situ temperature (1.0°C) for 12 hours with carrier-free 35**SO4 (dissolved in water, 50 kBq). Sediment was fixed in 20 ml 20% ZnAc solution for AOM or SR, respectively. Turnover rates were measured as previously described (doi:10.4319/lom.2004.2.171).