_version_ 1867170104254398464
author Perner, Mirjam
Seifert, Richard
Weber, Stefan
Koschinsky, Andrea
Schmidt, Katja
Strauss, Harald
Peters, Marc
Haase, Karsten M
Imhoff, Johannes F
author_facet Perner, Mirjam
Seifert, Richard
Weber, Stefan
Koschinsky, Andrea
Schmidt, Katja
Strauss, Harald
Peters, Marc
Haase, Karsten M
Imhoff, Johannes F
collection Datos científicos de ciencias marinas y ambientales
contents Hydrothermal vent fluids were sampled with a pumped flow-through system with PFA sampling bottles (Kiel Pumping System KIPS) by the ROV QUEST. Fuid chemical parameters were determined immediately after sample recovery. Ph was measured at 20°C in unfiltered sample aliquots. Sulfide concentrations were measured colorimetrcally following the methylene blue method. Fe(II) and Fe(III) was measured colorimetrically with the phenantroline assay. Total Fe was measured by reducing all Fe(III) to Fe(II) with ascorbic acid. Fe(III) was calculated from the diffrence between Fe(II) and total Fe. Light dissolved hydrocharbons were analysed on board applying a purge and trap technique. Dissolved hydrogen was mesured onboard by a GC equipped with a PDD. Stable carbon isotope signatures of methane were analysed using coupled gas chromatography-combustion-isotope ration mass spectrometry. The abundance of bacterial and archaeal taxa was investigated by sequencing of the 16S rRNA gene. The diversity of the cbbL, cbbM and aclb was investigated by sequencing of the genes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_927427
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Physico-chemical parameters and accession numbers from the Lilliput hydrothermal field, southern Mid-Atlantic Ridge (9°S)
Perner, Mirjam
Seifert, Richard
Weber, Stefan
Koschinsky, Andrea
Schmidt, Katja
Strauss, Harald
Peters, Marc
Haase, Karsten M
Imhoff, Johannes F
Accession number, genetics; Area/locality; Candidate Divisions; Endmember fluid portion; Epsilonproteobacteria; fish; Gene name; Hydrogen; Hydrogen sulfide; Iron 2+; Iron 3+; low-temperature hydrothermal fluids; M64/1; M64/1_Lilliput-hydrothermal-field; M68/1; M68/1_Lilliput-hydrothermal-field; MARSUED2; MARSUED3; Meteor (1986); Methane; microbial community; Mid-Atlantic Ridge; pH; Remote operated vehicle QUEST; ROVQ; Sampling date; sulfur oxidation; Temperature, water; Thiomicrospira; δ13C, methane
Hydrothermal vent fluids were sampled with a pumped flow-through system with PFA sampling bottles (Kiel Pumping System KIPS) by the ROV QUEST. Fuid chemical parameters were determined immediately after sample recovery. Ph was measured at 20°C in unfiltered sample aliquots. Sulfide concentrations were measured colorimetrcally following the methylene blue method. Fe(II) and Fe(III) was measured colorimetrically with the phenantroline assay. Total Fe was measured by reducing all Fe(III) to Fe(II) with ascorbic acid. Fe(III) was calculated from the diffrence between Fe(II) and total Fe. Light dissolved hydrocharbons were analysed on board applying a purge and trap technique. Dissolved hydrogen was mesured onboard by a GC equipped with a PDD. Stable carbon isotope signatures of methane were analysed using coupled gas chromatography-combustion-isotope ration mass spectrometry. The abundance of bacterial and archaeal taxa was investigated by sequencing of the 16S rRNA gene. The diversity of the cbbL, cbbM and aclb was investigated by sequencing of the genes.
title Physico-chemical parameters and accession numbers from the Lilliput hydrothermal field, southern Mid-Atlantic Ridge (9°S)
topic Accession number, genetics; Area/locality; Candidate Divisions; Endmember fluid portion; Epsilonproteobacteria; fish; Gene name; Hydrogen; Hydrogen sulfide; Iron 2+; Iron 3+; low-temperature hydrothermal fluids; M64/1; M64/1_Lilliput-hydrothermal-field; M68/1; M68/1_Lilliput-hydrothermal-field; MARSUED2; MARSUED3; Meteor (1986); Methane; microbial community; Mid-Atlantic Ridge; pH; Remote operated vehicle QUEST; ROVQ; Sampling date; sulfur oxidation; Temperature, water; Thiomicrospira; δ13C, methane
url https://doi.org/10.1594/PANGAEA.927427