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Mikrobiologie und Biochemie des Kohlenstoffkreislaufes

  • Chapter
Mikrobiologie von Böden

Part of the book series: Springer-Lehrbuch ((SLB))

Zusammenfassung

Der globale CO2-C-Gehalt in der Atmosphäre (Abb. 10.1) wird heute auf etwa 700 bis 800 Pg C (1 Petagramm = 1015 g = 1 Giga-t C) geschätzt, was im Vergleich zum C-Gehalt in den globalen terrestrischen Ökosystemen (ca. 1000 bis 2300 Pg C) und in den weltweiten Ozeanen (ca. 39 000 bis 41 000 Pg C) relativ gering ist. Ursache dieser sehr geringen atmosphärischen CO2-Konzentration von etwa 0,0383 Vol.-% (bei 78,09 Vol.-% N2 und 20,95 Vol.-% O2) ist die sehr effiziente CO2-Fixierung durch die oxygenen Photosyntheseprozesse (Primärproduktion PP) (Gl. 10.1)

6 CO2 + 6 H2O ↔ C6H12O6 + 6 O2 (10.1)

wodurch das globale Fließgleichgewicht eindeutig auf der rechten Seite liegt und CO2 für die pflanzliche Biomasse in den terrestrischen und aquatischen Ökosystemen zum wachstumsbegrenzenden Faktor geworden ist.

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Authors and Affiliations

  1. Institut für Angewandte Mikrobiologie, Justus Liebig-Universität, Heinrich-Buff-Ring 26–32, 35392, Gießen, Deutschland

    Professor em. Dr. sc. agr. habil. Johannes C. G. Ottow

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  1. Professor em. Dr. sc. agr. habil. Johannes C. G. Ottow
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Ottow, J. (2011). Mikrobiologie und Biochemie des Kohlenstoffkreislaufes. In: Mikrobiologie von Böden. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-00824-5_10

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