Reimer, Andreas

[["dc.bibliographiccitation.firstpage","159"],["dc.bibliographiccitation.issue","1-4"],["dc.bibliographiccitation.journal","Sedimentary Geology"],["dc.bibliographiccitation.lastpage","176"],["dc.bibliographiccitation.volume","126"],["dc.contributor.author","Arp, Gernot"],["dc.contributor.author","Thiel, Volker"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Michaelis, Walter"],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2019-11-06T10:58:31Z"],["dc.date.available","2019-11-06T10:58:31Z"],["dc.date.issued","1999"],["dc.description.abstract","Calcium carbonate precipitation and microbialite formation at highly supersaturated mixing zones of thermal spring waters and alkaline lake water have been investigated at Pyramid Lake, Nevada. Without precipitation, pure mixing should lead to a nearly 100-fold supersaturation at 40°C. Physicochemical precipitation is modified or even inhibited by the properties of biofilms, dependent on the extent of biofilm development and the current precipitation rate. Mucus substances (extracellular polymeric substances, EPS, e.g., of cyanobacteria) serve as effective Ca2+-buffers, thus preventing seed crystal nucleation even in a highly supersaturated macroenvironment. Carbonate is then preferentially precipitated in mucus-free areas such as empty diatom tests or voids. After the buffer capacity of the EPS is surpassed, precipitation is observed at the margins of mucus areas. Hydrocarbon biomarkers extracted from (1) a calcifying Phormidium-biofilm, (2) the stromatolitic carbonate below, and (3) a fossil 'tufa' of the Pleistocene pinnacles, indicate that the cyanobacterial primary producers have been subject to significant temporal changes in their species distribution. Accordingly, the species composition of cyanobacterial biofilms does not appear to be relevant for the formation of microbial carbonates in Pyramid Lake. The results demonstrate the crucial influence of mucus substances on carbonate precipitation in highly supersaturated natural environments."],["dc.identifier.doi","10.1016/S0037-0738(99)00038-X"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/62576"],["dc.language.iso","en"],["dc.relation.issn","0037-0738"],["dc.title","Biofilm exopolymers control microbialite formation at thermal springs discharging into the alkaline Pyramid Lake, Nevada, USA"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","206"],["dc.contributor.author","Kempe, Stefan"],["dc.contributor.author","Landmann, Günter"],["dc.contributor.author","Reimer, Andreas"],["dc.date.accessioned","2020-05-05T14:25:17Z"],["dc.date.available","2020-05-05T14:25:17Z"],["dc.date.issued","1992"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/64842"],["dc.language.iso","en"],["dc.relation.conference","Union San Francisco 1992 Fall Meeting"],["dc.relation.eventend","1992-10"],["dc.relation.eventlocation","San Francisco 1992"],["dc.relation.eventstart","1992-10"],["dc.relation.ispartof","Supplement to EOS"],["dc.title","Sediments of Lake Van, Eastern Anatolia"],["dc.type","conference_paper"],["dc.type.internalPublication","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","66"],["dc.bibliographiccitation.issue","1-4"],["dc.bibliographiccitation.journal","Facies"],["dc.bibliographiccitation.lastpage","79"],["dc.bibliographiccitation.volume","51"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Peckmann, Jörn"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Schumann, G."],["dc.contributor.author","Thiel, Volker"],["dc.date.accessioned","2018-11-07T10:54:36Z"],["dc.date.available","2018-11-07T10:54:36Z"],["dc.date.issued","2005"],["dc.description.abstract","In the euxinic waters of the NW' Black Sea shelf, tower-like carbonate build-ups up to several metres in height grow at sites of cold methane seepage. These structures are part of an unique microbial ecosystem that shows a considerable biodiversity and a remarkable degree of organization. The accretion of the build-ups is promoted by the growth of centimetre-sized, methane-filled spheres constructed by calcifying microbial mats. Progressive mineralization of these spheres involves the early precipitation of strongly luminescent high-Mg-calcite rich in iron sulphides, and closely interfingered aragonite phases that finally create the stable (mega-) thrombolithic fabric of the towers. Within the microbial mats, microorganisms occur in distinctive spatial arrangements. Major players among the microbial consortia are the archaea groups ANME-1 and ANME-2, Crenarchaeota, and sulphate-reducing bacteria (SRB) of the Desulfosaricina/Desulfobacterium group. The intracellular precipitation of iron sulphides (greigite) by some of these bacteria, growing in close association with ANME-2, suggests iron cycling as an additional biogeochemical pathway involved in the anaerobic oxidation of methane (AOM)."],["dc.identifier.doi","10.1007/s10347-005-0059-4"],["dc.identifier.isi","000235005200010"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/49604"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0172-9179"],["dc.title","Methane-derived carbonate build-ups and associated microbial communities at cold seeps on the lower Crimean shelf (Black Sea)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1119"],["dc.bibliographiccitation.issue","10"],["dc.bibliographiccitation.journal","Organic Geochemistry"],["dc.bibliographiccitation.lastpage","1129"],["dc.bibliographiccitation.volume","41"],["dc.contributor.author","Blumenberg, Martin"],["dc.contributor.author","Mollenhauer, Gesine"],["dc.contributor.author","Zabel, Matthias"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Thiel, Volker"],["dc.date.accessioned","2018-11-07T08:38:53Z"],["dc.date.available","2018-11-07T08:38:53Z"],["dc.date.issued","2010"],["dc.description.abstract","Geohopanoids derive from bacteriohopanepolyol (BHP) precursors. However, knowledge of the specific sources and diagenetic fate of both compound classes in marine sediments is fragmentary. We studied the relationship between BHPs and geohopanoids in a sediment core from the central Benguela Upwelling System (BUS), including deposits over the last 75 ka. The BUS is a (palaeo)oceanographically stable setting, where primary production is largely controlled by variation in upwelling intensity and therefore nutrient supply. Marine production in the BUS was generally higher during glacial than during interglacial times, as reflected in the levels of sedimentary total organic carbon. Geohopanoids at the study site consisted mainly of extractable hopanes and hopanols and occurred in the highest amounts during glacial periods. A minor, but still considerable fraction of geohopanoids was sulfur-linked to geomacromolecular organic matter. Among these S-bound hopane moieties, 17 beta(H),21 beta(H)-trishomohopane (C(33)) was the predominant compound, suggesting a diagenetic overprint of BHPs before linkage. Among the BHPs, a rare bacteriohopanetetrol with likely 22S configuration was observed. This structural feature was lacking in the geohopanoids, which all had the 22R configuration. Different behaviour of BHP and geohopanoid concentrations, as well as delta(13)C discrepancies indicate a decoupling of bio- and geohopanoids. Geohopanoids most likely reflect laterally-transported fossil organic matter, whereas BHPs are indigenous to the upper water column of the study site and may relate to past upwelling intensity/nutrient levels. Hence, care has to be taken using geohopanoids and other biomarkers for palaeoreconstruction in settings where sedimentation processes are not fully understood. (C) 2010 Elsevier Ltd. All rights reserved."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft [BL 971/1-1, BL 971/1-2]"],["dc.identifier.doi","10.1016/j.orggeochem.2010.06.005"],["dc.identifier.isi","000282908400005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/18860"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0146-6380"],["dc.title","Decoupling of bio- and geohopanoids in sediments of the Benguela Upwelling System (BUS)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Kempe, Stefan"],["dc.date.accessioned","2020-05-05T14:24:21Z"],["dc.date.available","2020-05-05T14:24:21Z"],["dc.date.issued","1987"],["dc.description.abstract","In the SW Harz Mountains (F.R.G.) the dome-shaped Devonian Iberg-Winterberg reef limestone emerges from the surrounding Carboniferous graywackes. The small limestone outcrop (km2) consists of two atoll-like structures, the Iberg in the SE and the Winterberg in the NW. The original reef shape is suppressed by boundary faults, separating the limestone from the clastic rocks. Its total extension may have amounted to 12.5 km2, with a thickness of 600 m (FRANKE, 1973). More than 80 cavities are known within the complex descending a few to 50 m belwo the surface. Most of them are closely associated with iron-manganese ore bodies, which gave rise to intensive mining activity during the last centuries. The natural caves served as shafts for bost descending into the mines and hauling the iron ores in the eralier periods of mining. In the middle of the 19th centruy a gallery (Eisensteinstollen) was driven into the IBerg, but already in 1887 the last mine was abondoned. In 1986 the gallery and the system of natural caves and mines was made accessible again exceeding a total length of 5 km (Fig. 1,2)."],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/64834"],["dc.language.iso","en"],["dc.relation.conference","10th International Congress of Speleology"],["dc.relation.eventend","1989"],["dc.relation.eventlocation","Budapest, Hungary"],["dc.relation.eventstart","1989"],["dc.relation.ispartof","Proceedings of the 10th international congress of speleology, Budapest, 1989"],["dc.title","Recent and paleokarst systems and their relation to ore mineralization in the Iberg-reef-complex, Harz Mountains"],["dc.type","conference_paper"],["dc.type.internalPublication","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","304"],["dc.bibliographiccitation.issue","3-4"],["dc.bibliographiccitation.journal","Geomicrobiology Journal"],["dc.bibliographiccitation.lastpage","315"],["dc.bibliographiccitation.volume","32"],["dc.contributor.author","Spitzer, S."],["dc.contributor.author","Brinkmann, Nicole"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Ionescu, Danny"],["dc.contributor.author","Friedl, Thomas"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Arp, Gernot"],["dc.date.accessioned","2018-11-07T09:59:35Z"],["dc.date.available","2018-11-07T09:59:35Z"],["dc.date.issued","2015"],["dc.description.abstract","Two different cyanobacterial biofilms from German karstwater creeks were investigated with respect to their photosynthetic effect on Ca2+ removal and potential CaCO3 precipitation in artificial creek waters of different CO2 partial pressures at a given, constant calcite supersaturation. CO2 partial pressures were adjusted to 350 ppmV, 2200 ppmV and 8700 ppmV respectively, covering the range of Phanerozoic atmospheric CO2 partial pressures inferred from palaeosoils, stomatal indices and model calculations. Microsensor measurements of calcium, pH and oxygen revealed differences in the potential to precipitate CaCO3 between the two model organisms Tychonema-relative strain SAG 2388 and Synechococcus sp. strain SAG 2387. Whereas a strong removal of Ca2+ from the solution was measured at Tychonema-relative biofilm, the Synechococcus sp. biofilm exercised a much lower Ca2+ removal during photosynthesis. Photosynthesis was enhanced in both organisms with increasing CO2 and HCO3-, as indicated by enhanced O-2 production, but only for the motile filamentous taxon Tychonema-relative a concomitantly increasing calcium removal was measured. However, model calculations indicate that this short-term Ca2+ binding in the Tychonema-relative is due to complexation to exopolymers or oscillin, with no immediate CaCO3 precipitation. In contrast, Ca2+ and pH measurements at Synechococcus sp. biofilm could be consistent with immediate CaCO3 precipitation at the cells. In both biofilms, pH gradients increase with increasing pCO(2) from 350 to 2200 ppmV due to enhanced photosynthesis, but decrease at a pCO(2) of 8700 ppmV despite of further enhanced photosynthesis. This observation, regardless whether CO2 or HCO3- is used by the cyanobacteria, is in accordance with hydrochemical modeling demonstrating an increased DIC buffering at high pCO(2) conditions. These results indicate that the potential of cyanobacteria to form spatially defined calcification pattern via pH gradients at their cell envelopes ('calcified cyanobacteria') increases at elevated pCO(2), while at high pCO(2) conditions Ca2+ binding and lowered pH microgradients lead to spatially diffuse calcification without defined cell envelope precipitates."],["dc.identifier.doi","10.1080/01490451.2014.885617"],["dc.identifier.isi","000352349600010"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/37626"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1521-0529"],["dc.relation.issn","0149-0451"],["dc.title","Effect of Variable pCO(2) on Ca2+ Removal and Potential Calcification of Cyanobacterial Biofilms -An Experimental Microsensor Study"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","851"],["dc.bibliographiccitation.issue","9"],["dc.bibliographiccitation.journal","Geology"],["dc.bibliographiccitation.lastpage","854"],["dc.bibliographiccitation.volume","28"],["dc.contributor.author","Neuweiler, Fritz"],["dc.contributor.author","Rutsch, M."],["dc.contributor.author","Geipel, G."],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Heise, K. H."],["dc.date.accessioned","2018-11-07T10:30:38Z"],["dc.date.available","2018-11-07T10:30:38Z"],["dc.date.issued","2000"],["dc.description.abstract","Albian carbonate mud-mound limestones exposed near Iraneta, northern Spain, show a fabric- and particle-specific fluorescence. Intense fluorescence is restricted to in situ precipitated microcrystalline (automicritic) fabrics, calcified demosponges, and coralline sponges. Intermediate intensity derives from micritized bioclasts, pellets, and a rim of marine bladed cement. Most invertebrate skeletons, late-diagenetic equant cement, and crosscutting zones of dolomitization are weakly to nonfluorescent. Internal microcrystalline sediment (allomicrite) and red algae debris have variable fluorescence. Correlation between rock fluorescence and soluble humic substances was evaluated from 3 g of automicrite, allomicrite, and cement. Time-resolved laser-induced fluorescence spectroscopy (TRLFS) with ultra-short pulses on two extracrystalline fractions (NaOH-soluble) and two intracrystalline fractions (HCl-soluble and NaOH-soluble) showed that most of the soluble humic substances of automicrite are within the crystals; but conversely, are significantly enriched on outer surfaces of allomicrite. Spar cement is close to detection limits. Fluorescence lifetimes are in the range of 0.5-2 ns and 3.5-6 ns. We conclude that precipitation of automicrite took place during oxidative organic matter diagenesis, i.e., during condensation reactions of degradation products of marine biopolymers. By contrast, allomicrite formed by skeletal breakdown followed by ingestion, organic coating, and reingestion during deposit feeding. A humic-substance-based model of marine polymer gels represents a new approach for the understanding of ancient polygenetic carbonate muds, so typical of Phanerozoic mud-mounds in deeper water settings."],["dc.identifier.doi","10.1130/0091-7613(2000)028<0851:SHSFIS>2.3.CO;2"],["dc.identifier.isi","000089269100021"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/43909"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0091-7613"],["dc.title","Soluble humic substances from in situ precipitated microcrystalline calcium carbonate, internal sediment, and spar cement in a Cretaceous carbonate mud-mound"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","313"],["dc.bibliographiccitation.issue","2-3"],["dc.bibliographiccitation.journal","Deutsche hydrographische Zeitschrift"],["dc.bibliographiccitation.lastpage","329"],["dc.bibliographiccitation.volume","51"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Brasse, S."],["dc.contributor.author","Doerffer, R."],["dc.contributor.author","Dürselen, C. -D."],["dc.contributor.author","Kempe, S."],["dc.contributor.author","Michaelis, W."],["dc.contributor.author","Rick, H. -J."],["dc.contributor.author","Seifert, R."],["dc.date.accessioned","2020-05-05T14:27:14Z"],["dc.date.available","2020-05-05T14:27:14Z"],["dc.date.issued","1999"],["dc.description.abstract","Carbon cycling in the shallow, near-coastal environment of the German Bight, south-eastern North Sea was studied during different seasons (spring, summer, winter). Special emphasis was placed on the investigation of processes: biologically induced internal transformation within the water column as well as external influences (rivers, Wadden Sea). Detailed analysis of dissolved inorganic carbon, total alkalinity, particulate organic carbon, dissolved oxygen and calculated CO2 fluxes revealed carbon cycling in the German Bight to be highly variable between seasons, with either dominance of physical processes during winter or pronounced biological control during productive times in spring and summer. During winter, enhanced input of particulate carbon was gained from the Wadden Sea by ice transport while biological processes stayed low. In spring, high primary production decreased the inorganic carbon pool and pronounced CO2 fluxes from the atmosphere into the surface water amounted to 40 mmol m-2 d-1. About sixty per cent of the produced biomass was rapidly remineralised within the surface layer, while in the bottom waters remineralisation stayed low. Degassing of CO2 to the atmosphere could only be observed during times of enhanced river discharge. During summer, high regenerated production accounted for CO2 fluxes of up to 25 mmol m-2 d-1 into the surface water. Replenishment of DIC in the surface layer through vertical mixing was hindered by strong stratification. Ninety-five per cent of the primary produced biomass was remineralised. Our investigations clearly show the German Bight to be a net carbon sink in spring and summer. Apart from degassing of CO2 as a result of late autumn vertical mixing or short term events like enhanced freshwater input, CO2 concentrations close to equilibrium during winter suggest that the German Bight constitutes a net annual sink for atmospheric CO2."],["dc.identifier.doi","10.1007/BF02764179"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/64850"],["dc.language.iso","en"],["dc.relation.eissn","1616-7228"],["dc.relation.issn","0012-0308"],["dc.title","Carbon cycling in the German Bight: An estimate of transformation processes and transport"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","93"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Journal of Sea Research"],["dc.bibliographiccitation.lastpage","103"],["dc.bibliographiccitation.volume","42"],["dc.contributor.author","Brasse, S."],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Seifert, R."],["dc.contributor.author","Michaelis, W."],["dc.date.accessioned","2020-05-05T14:27:46Z"],["dc.date.available","2020-05-05T14:27:46Z"],["dc.date.issued","1999"],["dc.description.abstract","The distribution of dissolved inorganic carbon (DIC) and total alkalinity (TA) in the German Bight, southeastern North Sea, was investigated during winter (February/March) 1996. Generally, high biological activity and riverine input dominate the carbon chemistry of this area for most of the year and mask impacts of other processes. During the investigation period, the presence of extended ice sheets, low river discharge and minimal primary productivity in the German Bight allowed the recognition of a considerable influence from sediment–water interaction. Water masses in front of the North Frisian Wadden Sea were clearly distinguished from others by considerably higher DIC and TA concentrations and a different DIC : TA ratio. We suggest that remineralisation products of Wadden Sea sediments and the DIC- and TA-enriched porewaters were subsequently released into the water column by enhanced erosion due to ice drift. The DIC : TA ratio of 1 : 1 indicates that either sulphate reduction or a combination of carbonate dissolution and aerobic remineralisation were the main processes generating this DIC. The calculated amount of DIC delivered from the Wadden Sea to the German Bight of about 10,000 t (equivalent to 76 mmol m−2 d−1) was in the same order of magnitude as the riverine input and about ten times higher than by diffusion alone. Apparently, for the carbon cycling in the coastal waters, sediment–water interaction may be a relevant process."],["dc.identifier.doi","10.1016/S1385-1101(99)00020-9"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/64853"],["dc.language.iso","de"],["dc.relation.issn","1385-1101"],["dc.title","The influence of intertidal mudflats on the dissolved inorganic carbon and total alkalinity distribution in the German Bight, southeastern North Sea"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","4883"],["dc.bibliographiccitation.issue","20"],["dc.bibliographiccitation.journal","Biogeosciences"],["dc.bibliographiccitation.lastpage","4902"],["dc.bibliographiccitation.volume","19"],["dc.contributor.author","Arif, Sania"],["dc.contributor.author","Nacke, Heiko"],["dc.contributor.author","Schliekmann, Elias"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Arp, Gernot"],["dc.contributor.author","Hoppert, Michael"],["dc.date.accessioned","2022-11-01T10:17:31Z"],["dc.date.available","2022-11-01T10:17:31Z"],["dc.date.issued","2022"],["dc.description.abstract","Abstract. The Kilianstollen Marsberg (Rhenish Massif, Germany) has\r\nbeen extensively mined for copper ores, dating from early medieval period\r\nuntil 1945. The exposed organic-rich alum shale rocks influenced by the\r\ndiverse mine drainages at an ambient temperature of 10 ∘C could\r\nnaturally enrich biogeochemically distinct heavy metal resistant microbiota.\r\nThis amplicon-sequence-based study evaluates the microbially colonized\r\nsubterranean rocks of the abandoned copper mine Kilianstollen to\r\ncharacterize the colonization patterns and biogeochemical pathways of\r\nindividual microbial groups. Under the selective pressure of the heavy metal\r\ncontaminated environment at illuminated sites, Chloroflexi (Ktedonobacteria) and Cyanobacteria (Oxyphotobacteria) build up\r\nwhitish–greenish biofilms. In contrast, Proteobacteria, Firmicutes and Actinobacteria dominate rocks around the\r\nuncontaminated spring water streams. The additional metagenomic analysis\r\nrevealed that the heavy metal resistant microbiome was evidently involved in\r\nredox cycling of transition metals (Cu, Zn, Co, Ni, Mn, Fe, Cd, Hg). No\r\ndeposition of metals or minerals, though, was observed by transmission\r\nelectron microscopy in Ktedonobacteria biofilms which may be indicative for the presence of\r\ndifferent detoxification pathways. The underlying heavy metal resistance\r\nmechanisms, as revealed by analysis of metagenome-assembled genomes, were\r\nmainly attributed to transition metal efflux pumps, redox enzymes,\r\nvolatilization of Hg, methylated intermediates of As3+, and reactive\r\noxygen species detoxification pathways."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2022"],["dc.identifier.doi","10.5194/bg-19-4883-2022"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/116831"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-605"],["dc.relation.eissn","1726-4189"],["dc.rights","CC BY 4.0"],["dc.title","Composition and niche-specific characteristics of microbial consortia colonizing Marsberg copper mine in the Rhenish Massif"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","unpublished"],["dspace.entity.type","Publication"]]