2017
DOI: 10.1093/femsec/fix054
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Physiological characterization of a halotolerant anoxygenic phototrophic Fe(II)-oxidizing green-sulfur bacterium isolated from a marine sediment

Abstract: Anoxygenic photoautotrophic bacteria which use light energy and electrons from Fe(II) for growth, so-called photoferrotrophs, are suggested to have been amongst the first phototrophic microorganisms on Earth and to have contributed to the deposition of sedimentary iron mineral deposits, i.e. banded iron formations. To date only two isolates of marine photoferrotrophic bacteria exist, both of which are closely related purple non-sulfur bacteria. Here we present a novel green-sulfur photoautotrophic Fe(II) oxidi… Show more

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Cited by 28 publications
(37 citation statements)
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“…These include Chlorobium ferrooxidans strain KoFox (Heising et al ., ) and two recently isolated species: Chlorobium phaeoferrooxidans (Crowe et al ., ; Thompson et al ., ) and Chlorobium sp. strain N1 which is closely related to Chlorobium luteolum (Laufer et al ., ). These organisms typically oxidize aqueous Fe(II) completely under normal culture conditions, similarly to Culture KS and in contrast to most other NRFeOx bacteria.…”
Section: Anoxygenic Phototrophic Fe(ii)‐oxidizersmentioning
confidence: 99%
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“…These include Chlorobium ferrooxidans strain KoFox (Heising et al ., ) and two recently isolated species: Chlorobium phaeoferrooxidans (Crowe et al ., ; Thompson et al ., ) and Chlorobium sp. strain N1 which is closely related to Chlorobium luteolum (Laufer et al ., ). These organisms typically oxidize aqueous Fe(II) completely under normal culture conditions, similarly to Culture KS and in contrast to most other NRFeOx bacteria.…”
Section: Anoxygenic Phototrophic Fe(ii)‐oxidizersmentioning
confidence: 99%
“…Green sulfur bacteria such as Chlorobium sp. strain N1, however, utilize higher light intensities (saturation at 400 lux) thus they are not limited to very low light environments (Laufer et al, 2017). All isolated anoxygenic phototrophic Fe(II)oxidizers are metabolically flexible and have the ability to utilize multiple electron donors for CO 2 fixation instead of Fe(II), such as H 2 and H 2 S (Croal et al, 2009).…”
Section: Physiology Existing Isolates/cultures and Ecologymentioning
confidence: 99%
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“…Ϫ ϩ 4Fe 2ϩ ϩ 10H 2 O ϩ hv → (CH 2 O) ϩ 4Fe(OH) 3 ϩ 7H ϩ (1) This process is thought to have fueled the Earth's biosphere prior to the evolution of oxygenic photosynthesis and is likely to have been a key contributor in the deposition of vast formations of layered Fe(II)-Fe(III) and Si-rich rock during Earth's early history (1)(2)(3). Organisms capable of this metabolism are still found in many modern environments, including Fe(II)-rich (4)(5)(6)(7) and Fe(II)-poor (8) stratified lakes, as well as both freshwater (9,10) and marine sediments (11)(12)(13)(14). These microorganisms belong to the purple sulfur bacteria (Gammaproteobacteria), purple nonsulfur bacteria (Alphaproteobacteria), and green sulfur bacteria (Chlorobi).…”
Section: Hcomentioning
confidence: 99%
“…Anoxygenic phototrophs show remarkable versatility with regard to their metabolism. They can fix CO 2 using Fe(II), H 2 , or H 2 S as an electron donor (photoautotrophy), or they can use organic compounds as a carbon source (photoheterotrophy) (9,10,12,14,15). Some isolates can also grow chemoheterotrophically with dioxygen without any light at all, e.g., Rhodopseudomonas palustris TIE-1 (Jiao et al [9]).…”
Section: Hcomentioning
confidence: 99%