Abstract

1. Introduction The photochemical reaction of the green sulfur photosynthetic bacteria (Chlorobiaceae) is clearly very different from that of the purple sulfur and non-sulfur bacteria (Chromatiaceae and Rhodospiril- laceae). The latter have a quinone-iron complex, with an operating midpoint potential near -175 mV, as the ‘primary acceptor’ [l-3]. These organisms reduce pyridine nucleotides by energy-dependent reversed electron flow [3,4]. In contrast, the midpoint poten- tial of the ‘primary acceptor’ in green bacteria has a substantially lower value, probably near -540 mV [5-71, and these organisms are capable of direct photoreduction of pyridine nucleotides [3,4,8]. However, the chemical identity of the ‘primary acceptor’ in green bacteria, such as

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