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C Calvin–Benson Cycle 228 C Calvin–Benson Cycle In 1951, Calvin published one of the first works in Keywords prebiotic chemistry. He reduced carbon dioxide in aqueous Biosynthesis, autotrophy, carboxylation, carbon dioxide solution, by ionizing radiation, to formic acid. In 1953, Harold Urey rejected this result because of the Definition presence of CO2. Urey was in favor of a reductive primitive A carbon dioxide fixation pathway where a molecule of atmosphere without CO2. However, Calvin maintained CO2 condenses with a 5-C compound (ribulose his interest for origins of life during the rest of his career, 1,5-bisphosphate) to yield two molecules of a 3-C com- and published his main book on this topic in 1969 pound (3-phosphoglycerate). These 3-C molecules serve (Molecular Evolution towards the Origin of Living Systems both as precursors for biosynthesis and, through on Earth and Elsewhere). a cyclic series of enzymatic reactions, to regenerate the See also 5-C molecule necessary for the first carboxylating step (Fig. 1). The pathway is present in several bacterial line- ▶ Calvin–Benson Cycle ages (e.g., cyanobacteria) and its acquisition by eukaryotic ▶ Miller, Stanley cells (chloroplast in algae and plants) was through the ▶ Urey’s Conception of Origins of Life endosymbiotic association with ancient cyanobacteria. History Calvin–Benson Cycle Melvin Calvin (1911–1997) and coworkers established this autotrophic path of carbon in phototrophic organisms using 14C labelled carbon dioxide and Chlorella (a green JULI PERETO´ algae) cultures (Benson & Calvin 1950). Calvin was Cavanilles Institute for Biodiversity and Evolutionary awarded with the Nobel Prize in Chemistry in 1961 “for Biology and Department of Biochemistry and Molecular his research on the carbon dioxide assimilation in plants.” Biology, University of Vale`ncia, Vale`ncia, Spain Overview Synonyms The Calvin–Benson cycle allows the synthesis of one Dark reactions; Reductive pentose phosphate cycle triose from three molecules of carbon dioxide (Fig. 1): 3 CO2 6 ATP 3 Ribulose 1,5-BP 6 3-phosphoglycerate 1 2 3 ATP 6 1,3-bisphosphoglycerate 3 Ribulose 5-P 6[H] xylulose 5-P + ribose 5-P 6 (Gd3P) sedoheptulose 7-P Gd3P DHAP sedoheptulose 1,7-BP DHAP biomass xylulose 5-P + erythrose 4-P fructose 1,6-BP fructose 6-P Calvin–Benson Cycle. Figure 1 The Calvin–Benson cycle. The stoichiometry of the cycle allows the net synthesis of one molecule of triose from three molecules of carbon dioxide (gray boxes). Other five trioses (5 C3) are converted into three pentoses (3 C5) necessary to initiate the cycle again. The energetic cost for the synthesis of one triose is nine ATP molecules and six reducing equivalents (NADH or NADPH). These energetic requirements could be satisfied by a photosynthetic apparatus or a chemolithotrophic metabolism. Except for two key enzymatic steps (1 and 2), all the transformations are a combination of enzymes participating in the Embden–Meyerhof–Parnas pathway and the non-oxidative pentosephosphate pathway. Key enzymatic steps: (1) Rubisco; (2) phosphoribulokinase. Abbreviations: Gd3P, glyceraldehyde 3-phosphate; DHAP, dihydroxyacetonephosphate Campbellrand–Malmani Platform, South Africa C 229 12 electrons (provided by redox coenzymes like NADH or NADPH) and 9 ATP equivalents are required for Cambrian Explosion bringing CO2 to the oxidation level of the triose glyceral- dehyde 3-phosphate. These fueling requirements are Synonyms supplied by either a phototrophic or a chemolithotroph Cambrian radiation C metabolism. The cycle can be divided into two stages: a reductive carboxylation of the pentose ribulose 1,5- Definition bisphosphate (RuBP) up to glyceraldehyde 3-phosphate The Cambrian explosion was a major evolutionary radia- and a series of rearrangements of carbon skeletons from tion of organisms, notably multicellular animals (meta- trioses to regenerate RuBP throughout 4-, 6-, and 7-C zoans), that occurred during the Cambrian period sugar intermediates (Fig. 1). The first step is catalyzed by (542–588 Ma). Pre-Cambrian fossils reveal a mainly the key carboxylating enzyme ▶ Rubisco. As other carbox- microbial biota, with complex, large-bodied organisms ylases, Rubisco also shows a preference for lighter only becoming conspicuous during the latest Proterozoic stable isotopes and thus CO2 fixation results in the deple- Eon (the Ediacaran biota). In contrast, Cambrian fossils tion of 13C(d13C) in the biosynthesized organic matter include abundant evidence for macroscopic motile organ- ranging from À20‰ to À30‰. The second stage of the isms, and unambiguous examples of most major animal cycle occurs by the combination of several enzymatic lineages. Exactly what determined the timing of the activities from the ▶ Embden–Meyerhof–Parnas pathway Cambrian explosion is not clear, and current research and the non-oxidative branch of the pentose phosphate aims to disentangle the effects of physical environment, pathway. ecological context, and factors related to development and The Calvin–Benson cycle was originally described in genetics. green plant (i.e., chloroplast) photosynthesis (Benson & Calvin 1950). It is also active in endosymbiotic See also chemolithotrophic proteobacteria of invertebrates living ▶ Burgess Shale Biota in close proximity to hydrothermal vents. In free-living ▶ Chengjiang Biota, China prokaryotes, this pathway has been demonstrated in cyanobacteria (the group to which the ancestors of plas- tids belonged), some aerobic or facultative anaerobic proteobacteria, CO-oxidizing mycobacteria, diverse iron-sulfur-oxidizing firmicutes and in some green sulfur Cambrian Radiation bacteria. Although Rubisco has been isolated from some Archaea, there is no evidence for the operation of ▶ Cambrian Explosion the full cycle in autotrophic species from this domain (Berg et al. 2010). See also ▶ Autotrophy Campbellrand–Malmani Platform, ▶ Embden-Meyerhof-Parnas Pathway South Africa ▶ Isotopic Fractionation (Planetary Process) ▶ Rubisco Definition The Campbellrand–Malmani ▶ carbonate platform was References and Further Reading deposited in the Kaapval craton, South Africa between 2,588 and 2,520 Ma (Neoarchean). This 1.9-km-thick Benson AA, Calvin M (1950) Carbon dioxide fixation by green plants. 2 Annu Rev Plant Physiol 1:25–42 carbonate platform is preserved over at least 190,000 km Berg IA, Kockelkorn D, Ramos-Vera WH, Say RF, Zarzycki J, Hu¨gler M, and probably originally covered the entire remaining Alber BE, Fuchs G (2010) Autotrophic carbon fixation in archaea. extent of the Kaapvaal craton (600,000 km2). The Nat Rev Microbiol 8:447–460 Campbellrand–Malmani is the first extended carbonate Berg JM, Tymoczko JL, Stryer L (2007) Biochemistry, 6th edn. Freeman, deposit in the Neoarchen ocean, prior of the buildup of New York, ch 20 Kim BH, Gadd GM (2008) Bacterial physiology and metabolism. the oxygen in the ocean and atmosphere, 2.35 Ga ago. Cambridge University Press, Cambridge, ch 10 Abundant of aragonite in its deposits suggests a neutral to.
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