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Volcanic production of polyphosphates and its relevance to prebiotic evolution
Abstract
Phosphates would probably have been essential compounds for prebiotic evolution on the primitive Earth. In this context, there have been several studies of condensation of water-soluble phosphates to polyphosphates and phosphorylation and condensation or polymerization of biomolecules with polyphosphates. But most of the phosphorus on the early Earth would have been in the form of water-insoluble apatite, and the origin of the water-soluble polyphosphates required for prebiotic evolution has therefore been a mystery. Here we show, both from experiments that simulate magmatic conditions and from analysis of volatile condensates in volcanic gas, that volcanic activity can produce water-soluble polyphosphates through partial hydrolysis of P4O10. This mechanism seems to be the only viable route identified so far for the production of these species on the primitive Earth.
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“Phosphate is more soluble at pH 6 than at pH 8 and was not likely to have been globally abundant in the early oceans [11,30], although there was surely considerable local phosphate input from volcanos [66,67].”
From Early bioenergetic evolution (2013) · cites this paper as [66]
Citations
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Exogenous phosphorus compounds in early chemical evolution
Schwartz, A. W. (1996) · Origins of Life and Evolution of Biospheres · doi:10.1007/bf02459732 · Cited by 1
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BackgroundMajor anastrophic events for the origin of biological energy conversion
Baltscheffsky, H., & Baltscheffsky, M. (1996) · Origins of Life and Evolution of Biospheres · doi:10.1007/bf02459868 · Cited by 1
“A very early anastrophe leading to these events would have been the continuous production of PPi from cooling volcanic magma on the early earth (Yamagata et al., 1991).”
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Tiedemann, H. (1997) · Science · doi:10.1126/science.277.5332.1687 · Cited by 1
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“Estimates of volcanic P flux into the oceans are difficult to directly measure, and thus have been derived from laboratory experiments using both artificial basalt/phosphate powder mixtures, and condensates from fumaroles (Yamagata et al., 1991).”
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“Accordingly, they are found in volcanic condensates as the result of volcanic activity through partial hydrolysis of P4O10 (Yamagata et al. 1991).”
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“If some portion of the rock-derived P was in solution as pyrophosphate or polyphosphate (Yamagata et al., 1991), it would not have been detected with the colorimetric analysis, and led to an apparent excess of Fe.”
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Metadata
- Authors
- Yamagata, Y., Watanabe, H., Saitoh, M., & Namba, T.
- Affiliations
- Kanazawa University (JP)
- ORCID
- Yamagata, Y.
- Venue
- Nature
- Published
- 1991-08
- Volume
- 352
- Issue
- 6335
- Pages
- 516-519
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1984123403
- Cited by
- 371
- References
- 36
- Citations by year
- 2026: 16 · 2025: 13 · 2024: 11 · 2023: 15 · 2022: 13 · 2021: 23 · 2020: 18 · 2019: 18 · 2018: 8 · 2017: 18 · 2016: 2 · 2015: 12 · 2014: 10 · 2013: 10 · 2012: 12
- FWCI
- 5.61
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- PubMed (publishedVersion)
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- polyphosphate, prebiotic evolution, volcanic activity, water-soluble phosphate, apatite, origin of life, early Earth, phosphate chemistry
- MeSH terms
- Calcium Phosphates, Hot Temperature, Minerals, Phosphorus, Polyphosphates, Silicates, Earth, Planet, Volcanic Eruptions, Evolution, Chemical, Evolution, Planetary
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