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- W2092220989 abstract "Abstract Mass occurrence of benthic cyanobacterial mats in a sequence of L ate D evonian black shales and bituminous limestones of the H oly C ross M ts. (central P oland), enclosing the famous K ellwasser and H angenberg extinction horizons, is reported. The microbiota forming the mats is compared with some modern benthic chroococcalean cyanobacteria. Similarly to their extant counterparts, the D evonian cyanobacteria must had been phototrophic and oxygenic aerobes which could, however, tolerate slightly sulfidic conditions characterizing the near‐bottom waters of the L ate D evonian epicontinental sea. The cyanobacterial mats successfully colonized the oxygen‐deficient and H 2 S‐enriched seabed otherwise unfavorable for most other benthic biota. The redox state of this sluggish L ate D evonian sea, ascribed previously mostly to anoxic or euxinic conditions, is reassessed as probably pulsating between anoxic, dysoxic, and weakly oxic conditions. The redox state was dependent on the rate of oxygen production by the cyanobacterial mats, the intensity of H 2 S emissions from the decaying mat biomass, and the rate of planktonic production." @default.
- W2092220989 created "2016-06-24" @default.
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- W2092220989 date "2012-08-07" @default.
- W2092220989 modified "2023-10-02" @default.
- W2092220989 title "Late Devonian marine anoxia challenged by benthic cyanobacterial mats" @default.
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- W2092220989 doi "https://doi.org/10.1111/j.1472-4669.2012.00339.x" @default.
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