Isoprenoid quinones resolve the stratification of redox processes in a biogeochemical continuum from the photic zone to deep anoxic sediments of the Black Sea.
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dc.contributor.author | Becker, Kevin W | |
dc.contributor.author | Elling, Felix J | |
dc.contributor.author | Schröder, Jan Martin | |
dc.contributor.author | Lipp, Julius S | |
dc.contributor.author | Goldhammer, Tobias | |
dc.contributor.author | Zabel, Matthias | |
dc.contributor.author | Elvert, Marcus | |
dc.contributor.author | Overmann, Jörg | |
dc.contributor.author | Hinrichs, Kai-Uwe | |
dc.coverage.spatial | LATITUDE: 41.528000 * LONGITUDE: 30.885000 * DATE/TIME START: 2011-02-19T21:58:00 * DATE/TIME END: 2011-02-19T21:58:00 * MINIMUM DEPTH, water: 17 m * MAXIMUM DEPTH, water: 1205 m | |
dc.date.accessioned | 2019-11-23T11:27:49Z | |
dc.date.available | 2019-11-23T11:27:49Z | |
dc.date.issued | 2018-10-16 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.895302 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.895302 | |
dc.identifier.citation | Becker, Kevin W; Elling, Felix J; Schröder, Jan Martin; Lipp, Julius S; Goldhammer, Tobias; Zabel, Matthias; Elvert, Marcus; Overmann, Jörg; Hinrichs, Kai-Uwe (2018): Isoprenoid quinones resolve the stratification of redox processes in a biogeochemical continuum from the photic zone to deep anoxic sediments of the Black Sea. Applied and Environmental Microbiology, 84(10), https://doi.org/10.1128/AEM.02736-17 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/7336 | |
dc.format | text/tab-separated-values, 104 data points | |
dc.language.iso | en | |
dc.publisher | PANGAEA | |
dc.relation.isbasedon | Becker, Kevin W; Elling, Felix J; Schröder, Jan Martin; Lipp, Julius S; Goldhammer, Tobias; Zabel, Matthias; Elvert, Marcus; Overmann, Jörg; Hinrichs, Kai-Uwe (2018): Isoprenoid quinones resolve the stratification of redox processes in a biogeochemical continuum from the photic zone to deep anoxic sediments of the Black Sea. Applied and Environmental Microbiology, 84(10), https://doi.org/10.1128/AEM.02736-17 | |
dc.relation.uri | https://doi.org/10.1594/PANGAEA.895911 | |
dc.rights | CC-BY-4.0: Creative Commons Attribution 4.0 International | |
dc.rights | Access constraints: unrestricted | |
dc.subject | Ammonium | |
dc.subject | Center for Marine Environmental Sciences | |
dc.subject | CTD/Rosette | |
dc.subject | CTD-RO | |
dc.subject | DEPTH, water | |
dc.subject | GeoB15105-5 | |
dc.subject | Hydrogen sulfide | |
dc.subject | M84/1 | |
dc.subject | M84/1_130-1 | |
dc.subject | MARUM | |
dc.subject | Meteor (1986) | |
dc.subject | Phosphate | |
dc.subject | Sulfate | |
dc.title | Isoprenoid quinones resolve the stratification of redox processes in a biogeochemical continuum from the photic zone to deep anoxic sediments of the Black Sea. | |
dc.title.alternative | Geochemistry at CTD cast GeoB15105-5 | |
dc.type | Dataset |
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