Reimer, Andreas

[["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","83"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Geomicrobiology Journal"],["dc.bibliographiccitation.lastpage","94"],["dc.bibliographiccitation.volume","25"],["dc.contributor.author","Shiraishi, Fumito"],["dc.contributor.author","Bissett, Andrew"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Arp, Gernot"],["dc.date.accessioned","2018-11-07T11:19:58Z"],["dc.date.available","2018-11-07T11:19:58Z"],["dc.date.issued","2008"],["dc.description.abstract","The impact of microbial activity on biofilm calcification in aquatic environments is still a matter of debate, especially in settings where ambient water has high CaCO3 mineral supersaturation. In this study, biofilms of two CO(2-)degassing karst-water creeks in Germany, which attain high calcite supersaturation during their course downstream, were investigated with regard to water chemistry of the biofilm microenvironment. The biofilms mainly consisted of filamentous cyanobacteria (Phormidium morphotype) and heterotrophic bacteria (including sulfate-reducing bacteria), which affect the microenvironment and produce acidic exopolymers. In situ and ex situ microelectrode measurements showed that a strong pH increase, coupled with Ca2+ consumption, occurred in light conditions at the biofilm surface, while the opposite occurred in the dark. Calcite supersaturation at the biofilm surface, calculated from ex situ Ca2+ and CO32- microelectrode measurements, showed that photosynthesis resulted in high omega values during illumination, while respiration slightly lowered supersaturation values in the dark, compared to values in the water column. Dissociation calculation demonstrated that the potential amount of Ca2+ binding by exopolymers would be insufficient to explain the Ca2+ loss observed, although Ca2+ complexation to exopolymers might be crucial for calcite nucleation. No spontaneous precipitation occurred on biofilm-free limestone substrates under the same condition, regardless of high supersaturation. These facts indicate that photosynthesis is a crucial mechanism to overcome the kinetic barrier for CaCO3 precipitation, even in highly supersaturated settings."],["dc.identifier.doi","10.1080/01490450801934888"],["dc.identifier.isi","000254214400002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/55419"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1521-0529"],["dc.relation.issn","0149-0451"],["dc.title","Photosynthesis, respiration and exopolymer calcium-binding in biofilm calcification (Westerhfer and deinschwanger creek, germany)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1159"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Limnology and Oceanography"],["dc.bibliographiccitation.lastpage","1168"],["dc.bibliographiccitation.volume","53"],["dc.contributor.author","Bissett, Andrew"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Schoon, Raphaela"],["dc.contributor.author","Shiraishi, Fumito"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Arp, Gernot"],["dc.date.accessioned","2018-11-07T11:15:41Z"],["dc.date.available","2018-11-07T11:15:41Z"],["dc.date.issued","2008"],["dc.description.abstract","Epilithic and endolithic biofilms were found to control the formation of stromatolites in karst-water creeks. We used microsensors to determine the influence of biological processes on chemical conditions within the microenvironment of crystal nucleation sites: the stromatolite surface. Phototrophic members of the biofilms consisted of mainly cyanobacteria and diatoms. Oxygen, pH, calcium, and carbonate concentration microprofiles at the stromatolite surface and boundary layer showed a strong diurnal rhythm of calcium carbonate precipitation. During illumination, photosynthesis caused oxygen production, a marked increase in pH and CO32- concentrations, and a decrease in Ca2+ concentration at the stromatolite surface due to calcium carbonate precipitation. The opposite occurred in the dark, indicating decalcification. Calcite was approximately 16 times oversaturated in the bulk water, photosynthesis induced an increase of the supersaturation to > 27 at the stromatolite surface under illumination, and respiration induced a decrease of the supersaturation to < 10 in the dark. Photosynthetically stimulated calcium carbonate precipitation was confirmed by radioactive isotope ( Ca-45(2+)) uptake studies. Over a 24 h light : dark cycle, biofilms showed net calcification. Biotic activity within the stromatolite has a large effect on conditions at its surface and, therefore, contributes considerably to the stromatolite precipitation process."],["dc.identifier.doi","10.4319/lo.2008.53.3.1159"],["dc.identifier.isi","000256498900024"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/54423"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1939-5590"],["dc.relation.issn","0024-3590"],["dc.title","Microbial mediation of stromatolite formation in karst-water creeks"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","6306"],["dc.bibliographiccitation.issue","20"],["dc.bibliographiccitation.journal","Applied and Environmental Microbiology"],["dc.bibliographiccitation.lastpage","6312"],["dc.bibliographiccitation.volume","74"],["dc.contributor.author","Bissett, Andrew"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Shiraishi, Fumito"],["dc.contributor.author","Arp, Gernot"],["dc.date.accessioned","2018-11-07T11:10:16Z"],["dc.date.available","2018-11-07T11:10:16Z"],["dc.date.issued","2008"],["dc.description.abstract","Ex situ microelectrode experiments, using cyanobacterial biofilms from karst water creeks, were conducted under various pH, temperature, and constant-alkalinity conditions to investigate the effects of changing environmental parameters on cyanobacterial photosynthesis-induced calcification. Microenvironmental chemical conditions around calcifying sites were controlled by metabolic activity over a wide range of photosynthesis and respiration rates, with little influence from overlying water conditions. Regardless of overlying water pH levels (from 7.8 to 8.9), pH at the biofilm surface was approximately 9.4 in the light and 7.8 in the dark. The same trend was observed at various temperatures (4 C and 17 C). Biological processes control the calcium carbonate saturation state (Omega) in these and similar systems and are able to maintain Omega at approximately constant levels over relatively wide environmental fluctuations. Temperature did, however, have an effect on calcification rate. Calcium flux in this system is limited by its diffusion coefficient, resulting in a higher calcium flux (calcification and dissolution) at higher temperatures, despite the constant, biologically mediated pH. The ability of biological systems to mitigate the effects of environmental perturbation is an important factor that must be considered when attempting to predict the effects of increased atmospheric partial CO2 pressure on processes such as calcification and in interpreting microfossils in the fossil record."],["dc.description.sponsorship","German Research Foundation [DFGFOR 571]"],["dc.identifier.doi","10.1128/AEM.00877-08"],["dc.identifier.isi","000259985300017"],["dc.identifier.pmid","18689512"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53177"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0099-2240"],["dc.title","Metabolic microenvironmental control by photosynthetic biofilms under changing macroenvironmental temperature and pH conditions"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","91"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Palaeogeography, Palaeoclimatology, Palaeoecology"],["dc.bibliographiccitation.lastpage","106"],["dc.bibliographiccitation.volume","262"],["dc.contributor.author","Shiraishi, Fumito"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Bissett, Andrew"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Arp, Gernot"],["dc.date.accessioned","2018-11-07T11:15:00Z"],["dc.date.available","2018-11-07T11:15:00Z"],["dc.date.issued","2008"],["dc.description.abstract","Cyanobacteria-dominated biofilms in a CO(2)-degassing karst-water creek (Westerhofer Bach, Germany) were investigated with regard to the effects of microbial activity on CaCO(3) precipitation, water chemistry of micro- and macroenvironments, stable isotopic records, and tufa fabric formation. Ex situ microelectrode measurements of pH, O(2), and Ca(2+) and CO(3)(2-) revealed that annually laminated calcified biofilms composed mainly of filamentous cyanobacteria (tufa stromatolites) strongly induced CaCO(3) precipitation by photosynthesis under illumination, but inhibited precipitation by respiration in the dark. In contrast, endolithic cyanobacterial biofilms and mosses did not cause photosynthesis-induced precipitation under experimental conditions. No spontaneous precipitation occurred on bare limestone substrates, despite high calcite supersaturation of the ambient water. Mass balance calculations suggest that biofilm photosynthesis was responsible for 10-20% of Ca(2+) loss in the creek, while the remaining Ca(2+) loss derived from physicochemical precipitation on branches, leaves and as fine-grained calcite particles. Neither analysis of bulk water chemistry nor oxygen nor carbon stable isotopic records of the tufa stromatolites confirmed photosynthetic effects, despite the evident photosynthesis-induced calcite precipitation. Oxygen stable isotopic values reflected seasonal changes in water temperature, and carbon stable isotope values probably recorded carbon isotopic composition of dissolved inorganic carbon in the creek water. Annual lamination and fabric formation of the tufa stromatolites is suggested to vary with photosynthesis-induced calcite precipitation rates that are affected by temperature dependency of diffusion coefficients. Photosynthesis-induced precipitation resulted in encrusted cyanobacterial sheaths, reflecting syntaxial overgrowth of microcrystalline cyanobacterial tubes by microspar, instead of microcrystalline sheath impregnation, which was previously suggested as an indicator of photosynthesis-induced precipitation. Therefore, sheath impregnation or encrustation by CaCO(3) cannot be used to distinguish photosynthesis-induced from physicochemically-induced CaCO(3) precipitation. (C) 2008 Elsevier B.V. All rights reserved."],["dc.identifier.doi","10.1016/j.palaeo.2008.02.011"],["dc.identifier.isi","000257011900007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/54274"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0031-0182"],["dc.title","Microbial effects on biofilm calcification, ambient water chemistry and stable isotope records in a highly supersaturated setting (Westerhofer Bach, Germany)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","6"],["dc.bibliographiccitation.journal","Frontiers in Earth Science"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","Heim, Christine N."],["dc.contributor.author","Simon, Klaus"],["dc.contributor.author","Ionescu, Danny"],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Quéric, Nadia Valérie"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Thiel, Volker"],["dc.date.accessioned","2019-07-09T11:41:14Z"],["dc.date.available","2019-07-09T11:41:14Z"],["dc.date.issued","2015"],["dc.description.abstract","Microbial iron oxyhydroxides are common deposits in natural waters, recent sediments, and mine drainage systems. Along with these minerals, trace and rare earth elements (TREE) are being accumulated within the mineralizing microbial mats. TREE patterns are widely used to characterize minerals and rocks, and to elucidate their evolution and origin. However, whether and which characteristic TREE signatures distinguish between a biological and an abiological origin of iron minerals is still not well-understood. Here we report on long-term flow reactor studies performed in the Tunnel of Äspö (Äspö Hard Rock Laboratory, Sweden). The development of microbial mats dominated by iron-oxidizing bacteria (FeOB), namely Mariprofundus sp. and Gallionella sp were investigated. The feeder fluids of the flow reactors were tapped at 183 and 290 m below sea-level from two brackish, but chemically different aquifers within the surrounding, ~1.8 Ga old, granodioritic rocks. The experiments investigated the accumulation and fractionation of TREE under controlled conditions of the subsurface continental biosphere, and enabled us to assess potential biosignatures evolving within the microbial iron oxyhydroxides. After 2 and 9 months, concentrations of Be, Y, Zn, Zr, Hf, W, Th, Pb, and U in the microbial mats were 103- to 105-fold higher than in the feeder fluids whereas the rare earth elements and Y (REE+Y) contents were 104- and 106-fold enriched. Except for a hydrothermally induced Eu anomaly, the normalized REE+Y patterns of the microbial iron oxyhydroxides were very similar to published REE+Y distributions of Archaean Banded Iron Formations (BIFs). The microbial iron oxyhydroxides from the flow reactors were compared to iron oxyhydroxides that were artificially precipitated from the same feeder fluid. Remarkably, these abiotic and inorganic iron oxyhydroxides show the same REE+Y distribution patterns. Our results indicate that the REE+Y mirror closely the water chemistry, but they do not allow to distinguish microbially mediated from inorganic iron precipitates. Likewise, all TREE studied showed an overall similar fractionation behavior in biogenic, abiotic, and inorganic iron oxyhydroxides. Exceptions are Ni and Tl, which were only accumulated in the microbial iron oxyhydroxides and may point to a potential utility of these elements as microbial biosignatures."],["dc.identifier.doi","10.3389/feart.2015.00006"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11851"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/58377"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.publisher","Frontiers Media S.A."],["dc.relation.eissn","2296-6463"],["dc.relation.issn","2296-6463"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Assessing the utility of trace and rare earth elements as biosignatures in microbial iron oxyhydroxides"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","170"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Geobiology"],["dc.bibliographiccitation.lastpage","180"],["dc.bibliographiccitation.volume","13"],["dc.contributor.author","Ionescu, Danny"],["dc.contributor.author","Spitzer, S."],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Schneider, D."],["dc.contributor.author","Daniel, Roy Thomas"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Arp, Gernot"],["dc.date.accessioned","2018-11-07T10:00:39Z"],["dc.date.available","2018-11-07T10:00:39Z"],["dc.date.issued","2015"],["dc.description.abstract","Microbialite-forming microbial mats in a hypersaline lake on the atoll of Kiritimati were investigated with respect to microgradients, bulk water chemistry, and microbial community composition. O-2, H2S, and pH microgradients show patterns as commonly observed for phototrophic mats with cyanobacteria-dominated primary production in upper layers, an intermediate purple layer with sulfide oxidation, and anaerobic bottom layers with sulfate reduction. Ca2+ profiles, however, measured in daylight showed an increase of Ca2+ with depth in the oxic zone, followed by a sharp decline and low concentrations in anaerobic mat layers. In contrast, dark measurements show a constant Ca2+ concentration throughout the entire measured depth. This is explained by an oxygen-dependent heterotrophic decomposition of Ca2+-binding exopolymers. Strikingly, the daylight maximum in Ca2+ and subsequent drop coincides with a major zone of aragonite and gypsum precipitation at the transition from the cyanobacterial layer to the purple sulfur bacterial layer. Therefore, we suggest that Ca2+ binding exopolymers function as Ca2+ shuttle by their passive downward transport through compression, triggering aragonite precipitation in the mats upon their aerobic microbial decomposition and secondary Ca2+ release. This precipitation is mediated by phototrophic sulfide oxidizers whose action additionally leads to the precipitation of part of the available Ca2+ as gypsum."],["dc.description.sponsorship","German research Foundation (DFG) [64]"],["dc.identifier.doi","10.1111/gbi.12120"],["dc.identifier.isi","000350053400006"],["dc.identifier.pmid","25515845"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/37855"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1472-4669"],["dc.relation.issn","1472-4677"],["dc.title","Calcium dynamics in microbialite-forming exopolymer-rich mats on the atoll of Kiritimati, Republic of Kiribati, Central Pacific"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","83"],["dc.bibliographiccitation.lastpage","118"],["dc.contributor.author","Arp, Gernot"],["dc.contributor.author","Bissett, Andrew"],["dc.contributor.author","Brinkmann, Nicole"],["dc.contributor.author","Cousin, Sylvie"],["dc.contributor.author","de Beer, Dirk"],["dc.contributor.author","Friedl, Thomas"],["dc.contributor.author","Mohr, Kathrin I."],["dc.contributor.author","Neu, Thomas R."],["dc.contributor.author","Reimer, Andreas"],["dc.contributor.author","Shiraishi, Fumito"],["dc.contributor.author","Stackebrandt, Erko"],["dc.contributor.author","Zippel, Barbara"],["dc.date.accessioned","2020-05-04T11:31:29Z"],["dc.date.available","2020-05-04T11:31:29Z"],["dc.date.issued","2010"],["dc.description.abstract","To understand mechanisms of tufa biofilm calcification, selected karstwater stream stromatolites in Germany have been investigated with regard to their hydrochemistry, biofilm community, exopolymers, physicochemical microgradients, calcification pattern and lamination. In stream waters, CO2 degassing drives the increase in calcite saturation to maximum values of approximately 10-fold, independent from the initial Ca2+/alkalinity ratio. For the cyanobacteria of tufa biofilms, a culture-independent molecular approach showed that microscopy of resinembedded biofilm thin sections underestimated the actual diversity of cyanobacteria, i.e. the six cyanobacteria morphotypes were opposed to nine different lineages of the 16S rDNA phylogeny. The same morphotype may even represent two genetically distant cyanobacteria and the closest relatives of tufa biofilm cyanobacteria may be from quite different habitats. Diatom diversity was even higher in the biofilm at the studied exemplar site than that of the cyanobacteria, i.e. 13 diatom species opposed to 9 cyanobacterial lineages. The non-phototrophic prokaryotic biofilm community is clearly different from the soil-derived community of the stream waters, and largely composed of flavobacteria, firmicutes, proteobacteria and actinobacteria. The exopolymeric biofilm matrix can be divided into three structural domains by fluorescence lectin-binding analysis. Seasonal and spatial variability of these structural EPS domains is low in the investigated streams. As indicated by microsensor data, biofilm photosynthesis is the driving mechanism in tufa stromatolite formation. However, photosynthesis-induced biofilm calcification accounts for only 10-20% of the total CaCa2+ loss in the streams, and occurs in parallel to inorganic precipitation driven by CO2-degassing within the water column and on biofilm-free surfaces. Annual stromatolite laminae reflect seasonal changes in temperature and light supply. The stable carbon isotope composition of the laminae is not affected by photosynthesis-induced microgradients, but mirrors that of the bulk water body only reflecting climate fluctuations. Tufa stromatolites with their cyanobacterial-photosynthesis-related calcification fabrics form an analogue to porostromate cyanobacterial stromatolites in fossil settings high in CaCO3 mineral supersaturation but comparatively low in dissolved inorganic carbon. Here, the sum-effect of heterotrophic exopolymerdegradation and secondary Ca2+-release rather decreases calcite saturation, contrary to settings high in dissolved inorganic carbon such as soda lakes."],["dc.identifier.doi","10.1144/SP336.6"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/64602"],["dc.language.iso","en"],["dc.relation.ispartof","Tufas and Speleothems: Unravelling the Microbial and Physical Controls"],["dc.title","Tufa-forming biofilms of German karstwater streams: microorganisms, exopolymers, hydrochemistry and calcification"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]