Phosphate Activation via Reduced Oxidation State Phosphorus (P). Mild Routes to Condensed-P Energy Currency Molecules.

Citation data:

Life (Basel, Switzerland), ISSN: 2075-1729, Vol: 3, Issue: 3, Page: 386-402

Publication Year:
2013
Usage 17
Abstract Views 16
Link-outs 1
Captures 14
Readers 14
Citations 15
Citation Indexes 15
Repository URL:
https://scholarcommons.usf.edu/geo_facpub/612
PMID:
25369812
DOI:
10.3390/life3030386
PMCID:
PMC4187178
Author(s):
Kee, Terence P.; Bryant, David E.; Herschy, Barry; Marriott, Katie E.R.; Cosgrove, Nichola E.; Pasek, Matthew A.; Atlas, Zachary D.; Cousins, Claire R.
Publisher(s):
MDPI AG
Tags:
Biochemistry, Genetics and Molecular Biology; Agricultural and Biological Sciences; Earth and Planetary Sciences; phosphorus; prebiotic chemistry; origin of life; meteorites
article description
The emergence of mechanisms for phosphorylating organic and inorganic molecules is a key step en route to the earliest living systems. At the heart of all contemporary biochemical systems reside reactive phosphorus (P) molecules (such as adenosine triphosphate, ATP) as energy currency molecules to drive endergonic metabolic processes and it has been proposed that a predecessor of such molecules could have been pyrophosphate [P2O74-; PPi(V)]. Arguably the most geologically plausible route to PPi(V) is dehydration of orthophosphate, Pi(V), normally a highly endergonic process in the absence of mechanisms for activating Pi(V). One possible solution to this problem recognizes the presence of reactive-P containing mineral phases, such as schreibersite [(Fe,Ni)3P] within meteorites whose abundance on the early Earth would likely have been significant during a putative Hadean-Archean heavy bombardment. Here, we propose that the reduced oxidation state P-oxyacid, H-phosphite [HPO32-; Pi(III)] could have activated Pi(V) towards condensation via the intermediacy of the condensed oxyacid pyrophosphite [H2P2O52-; PPi(III)]. We provide geologically plausible provenance for PPi(III) along with evidence of its ability to activate Pi(V) towards PPi(V) formation under mild conditions (80 °C) in water.