Abstract
Our planet requires a continual source of fixed carbon because heterotrophic organisms produce energy by oxidizing the organic carbon to CO2, thereby depleting the organic carbon. Reconversion of CO2 to organic carbon occurs by a reductive process called CO2 fixation. Many strict anaerobes perform CO2 fixation by a pathway which is called the reductive acetyl-CoA or the Wood/ Ljungdahl pathway (see Chapter 1). Formation of acetyl-CoA via the Wood/ Ljungdahl pathway occurs in many anaerobic environments including marine and freshwater sediments, in the soil, and in landfills and waste-treatment sites. Autotrophic anaerobes are also common in the rumen of cows, horses, and sheep, and in the hindgut of termites and the large intestine of humans (Breznak and Kane, 1990; Breznak and Switzer, 1986; Lajoie et al., 1988) (see Part IV of this book).
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Ragsdale, S.W. (1994). CO Dehydrogenase and the Central Role of This Enzyme in the Fixation of Carbon Dioxide by Anaerobic Bacteria. In: Drake, H.L. (eds) Acetogenesis. Chapman & Hall Microbiology Series. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-1777-1_3
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