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Kohlenstoffkreislauf

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Umweltmikrobiologie

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Zusammenfassung

Die Zusammensetzung der heutigen Erdatmosphäre geht auf biologische Prozesse im Verlauf der Erdgeschichte zurück. Die Uratmosphäre enthielt vor vier Milliarden Jahren vor allem Wasser, CO2 und reduzierte Verbindungen. Wahrscheinlich wurden CH4, H2 und H2S durch die Vorfahren der Archaea, deren Entstehung vor etwa 3,8 Mrd. Jahren angenommen wird, assimiliert.

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  1. Bergische Universität Wuppertal, Wuppertal, Deutschland

    Walter Reineke

  2. TU Bergakademie Freiberg, Freiberg, Deutschland

    Michael Schlömann

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  1. Walter Reineke
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Correspondence to Walter Reineke .

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Reineke, W., Schlömann, M. (2020). Kohlenstoffkreislauf. In: Umweltmikrobiologie. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-59655-5_4

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