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  • 1
    Electronic Resource
    Electronic Resource
    Multitude and temporal variability of ecological niches as indicated by the diversity of cultivated bacterioplankton (2001)
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology ecology 36 (2001), S. 0 
    Details
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: The diversity of cultured planktonic bacteria was analyzed. Bacterial strains were isolated from a eutrophic lake (Zwischenahner Meer, Niedersachsen, Germany) at three different sampling dates (October 1997, April and May 1998). Phylogenetic diversity was assessed by polymerase chain reaction (PCR), denaturing gradient gel electrophoresis (DGGE), and sequencing of 16S rRNA gene fragments. Enterobacterial repetitive intergenic consensus (ERIC)-PCR revealed a high genomic diversity within the strain collections, which exceeded the diversity of the 16S rRNA gene sequences considerably. The composition of each of the three strain collections was unique since strains isolated at different dates always exhibited different ERIC-PCR fingerprints. Growth tests with 59 different carbon substrates demonstrated that even strains with identical ERIC-PCR fingerprints, isolated on one sampling date, differed in their physiology. The culturable fraction investigated in the present study constituted a relatively small fraction (≤15%) of the whole bacterioplankton assemblage. Nevertheless, the high physiological diversity in this fraction already indicates that a multitude of different ecological niches must exist in the planktonic environment. The majority of strains isolated in April prior to the decay of the phytoplankton bloom were members of the Cytophaga-Flavobacterium group. One month later, not a single strain of this group could be isolated. When a group-specific PCR-DGGE technique was employed, rapid shifts in the diversity of non-cultured Cytophaga-Flavobacteria also became evident. Based on the rapid shifts in the composition of cultivated as well as some non-cultivated bacteria, the ecological niches in the planktonic habitat must undergo rapid temporal changes.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1574-6941.2001.tb00835.x
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    Paper (German National Licenses)
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  • 2
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    Environmental regulation of the anaerobic oxidation of methane: a comparison of ANME-I and ANME-II communities (2005)
    Wiley / Society for Applied Microbiology and Blackwell Publishing Ltd,
    In:  Environmental Microbiology, 7 (1). pp. 98-106.
    Details
    Publication Date: 2017-06-28
    Description: The anaerobic oxidation of methane (AOM) is one of the major sinks for methane on earth and is known to be mediated by at least two phylogenetically different groups of anaerobic methanotrophic Archaea (ANME-I and ANME-II). We present the first comparative in vitro study of the environmental regulation and physiology of these two methane-oxidizing communities, which occur naturally enriched in the anoxic Black Sea (ANME-I) and at Hydrate Ridge (ANME-II). Both types of methanotrophic communities are associated with sulfate-reducing-bacteria (SRB) and oxidize methane anaerobically in a 1:1 ratio to sulfate reduction (SR). They responded sensitively to elevated methane partial pressures with increased substrate turnover. The ANME-II-dominated community showed significantly higher cell-specific AOM rates. Besides sulfate, no other electron acceptor was used for AOM. The processes of AOM and SR could not be uncoupled by feeding the SRB with electron donors such as acetate, formate or molecular hydrogen. AOM was completely inhibited by the addition of bromoethanesulfonate in both communities, indicating the participation of methanogenic enzymes in the process. Temperature influenced the intensity of AOM, with ANME-II being more adapted to cold temperatures than ANME-I. The variation of other environmental parameters, such as sulfate concentration, pH and salinity, did not influence the activity of both communities. In conclusion, the ecological niches of methanotrophic Archaea seem to be mainly defined by the availability of methane and sulfate, but it remains open which additional factors lead to the dominance of ANME-I or -II in the environment.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1111/j.1462-2920.2004.00669.x
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 3
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    Methane dynamics in a microbial community of the Black Sea traced by stable carbon isotopes in vitro (2006)
    Elsevier
    In:  Organic Geochemistry, 37 (10). pp. 1411-1419.
    Details
    Publication Date: 2017-06-27
    Description: There is growing concern about the transfer of methane originating from water bodies to the atmosphere. Methane from sediments can reach the atmosphere directly via bubbles or indirectly via vertical turbulent transport. This work quantifies methane gas bubble dissolution using a combination of bubble modeling and acoustic observations of rising bubbles to determine what fraction of the methane transported by bubbles will reach the atmosphere. The bubble model predicts the evolving bubble size, gas composition, and rise distance and is suitable for almost all aquatic environments. The model was validated using methane and argon bubble dissolution measurements obtained from the literature for deep, oxic, saline water with excellent results. Methane bubbles from within the hydrate stability zone (typically below 500 m water depth in the ocean) are believed to form an outer hydrate rim. To explain the subsequent slow dissolution, a model calibration was performed using bubble dissolution data from the literature measured within the hydrate stability zone. The calibrated model explains the impressively tall flares (〉1300 m) observed in the hydrate stability zone of the Black Sea. This study suggests that only a small amount of methane reaches the surface at active seep sites in the Black Sea, and this only from very shallow water areas (〈100 m). Clearly, the Black Sea and the ocean are rather effective barriers against the transfer of bubble methane to the atmosphere, although substantial amounts of methane may reach the surface in shallow lakes and reservoirs.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/j.orggeochem.2006.03.007
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 4
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    Biosynthesis of hopanoids by sulfate-reducing bacteria (genus Desulfovibrio) (2006)
    Wiley / Society for Applied Microbiology and Blackwell Publishing Ltd,
    In:  Environmental Microbiology, 8 (7). pp. 1220-1227.
    Details
    Publication Date: 2017-06-28
    Description: Sulfate reduction accounts for about a half of the remineralization of organic carbon in anoxic marine shelf regions. Moreover, it was already a major microbial process in the very early ocean at least 2.4 billion years before the present. Here we demonstrate for the first time the capability of sulfate-reducing bacteria (SRB) to biosynthesize hopanoids, compounds that are quantitatively important and widely distributed biomarkers in recent and fossil sediments dating back to the late Archean. We found high concentrations (9.8–12.3 mg per gram of dry cells) of non-extended and extended bacteriohopanoids (bacteriohopanetetrol, aminobacteriohopanetriol, aminobacteriohopanetetrol) in pure cultures of SRB belonging to the widely distributed genus Desulfovibrio. Biohopanoids were found – considered as membrane rigidifiers – in more than 50% of bacterial species analysed so far. However, their biosynthesis appeared to be restricted to aerobes or facultative anaerobes with a very few recently described exceptions. Consequently, findings of sedimentary hopanoids are often used as indication for oxygenated settings. Nevertheless, our findings shed new light on the presence of hopanoids in specific anoxic settings and suggests that SRB are substantial sources of this quantitatively important lipid class in recent but also past anoxic environments.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1111/j.1462-2920.2006.01014.x
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    OceanRep: Article in a Scientific Journal - peer-reviewed
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