Did Nature use Reduced Oxidation State Phosphorus in Prebiotic Chemistry? Strengthening the Case for a Non-Phosphate World prior to the RNA-World

Lead Research Organisation: University of Bradford
Department Name: Faculty of Life Sciences

Abstract

Phosphate is a key ingredient in all life on Earth. Phosphate is everywhere on Earth, we dig it out of the ground as a calcium salt, we use it to brush our teeth, we consume it in food and drink every day. However, despite it being a rather common chemical, it is by no means certain that Nature chose phosphate for the earliest forms of life on Earth. A large part of the problem is that phosphate chemicals are both extremely insoluble and very unreactive chemically. In 1955, the scientist Addison Gulick proposed that this phosphate problem could have been solved if other forms of phosphorus were available on the early Earth. These chemicals, called phosphonates and phosphinates, are close relatives of phosphate but are both more soluble and chemically reactive in water. The problem is that phosphonates and phosphinates are unknown on Earth today because over the millennia, the chemical environment of Earth has changed to such a degree that only phosphates are now stable. However, we have recently discovered that phosphinates and phosphonates could have been readily available to prebiotic chemistry on the early Earth through chemical reactions of iron-rich meteorites with water in the presence of light. This discovery allows us to explore in detail the potential of phosphonates and phosphinates in the origin-of-life problem for the first time with a degree of confidence that such chemistry could have been available on the early Earth.This project is built in two parts. In Part 1 we will look in detail at how exactly phosphonates and phosphinates were formed from the chemical modification of actual meteorite fragments. In Part 2, we explore potential chemical reactions which could have taken place on an early Earth with these two phosphorus species and which could have an impact in how some key biological molecules, such as prebiotic organic phosphorus polymers, might have emerged.

Publications

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Description The impact of meteorites on the early earth may have had a crucial influence on the emergence of life. Aside from the
potential of extraterrestrial organic species, meteorites infalls are likely to have provided crucial elements in the correct
form for subsequent preparation for molecules of life. Of these, how phosphorus became the primary element of the
backbone of nucleic acids including DNA and RNA, the molecules encoding life, remains a mystery. These studies have
established mechanisms to show meteorites bearing a mineral called Schreibersite, which may have provided phosphorus
in the right form to generate molecules that serve as precursors to nucleic acid systems and provide pre-biotic chemical
reactions to couple amino acids and hence potentially from primitive proteins. The mechanisms involve two key steps: (i)
the corrosion of the Schreibersite bearing meteorite. It appears that this process is driven by the electrochemistry of the
meteorite themselves, with a corrosion process that literally unlocks the Schreibersite from the meteorite body (ii) the
production of phosphorus species from Fe3P like Schreibersite that have been shown to have the ability to couple amino
acids, the first step towards primitive proteins.
Exploitation Route This work
will be of interest not only to members of the scientific community but also to the general public. Much has been published
on the origin and role of prebiotic chemicals but until recently discussion of phosphorus has been limited to orthophosphate
and sources thereof. We envisage this work to provide a step-change in thinking about pre-RNA & prebiotic worlds.
Analytical measurements arising from the projects will contribute fundamentally to the wider understanding of the
interrelationship between minerals and biologically relevant molecular species and how these interactions may leave
'biomarker' degredant traces. Such information is fundamental to exo-biological prospecting and will underpin new areas of
investigation for high-impact projects such as the ESA's ExoMars mission where one of the primary objectives is the
'Search for traces of past and present life' in the Martian environment. In the wider context, progress in in situ analyses
and, particularly the development of oxo-phosphorus quantitative models, will contribute to ongoing developments in rapid
'real-time' process information for chemical and pharmaceutical manufacturing industries.
Sectors Agriculture, Food and Drink,Chemicals,Education,Culture, Heritage, Museums and Collections,Pharmaceuticals and Medical Biotechnology

 
Description This work will be of interest not only to members of the scientific community but also to the general public. Much has been published on the origin and role of prebiotic chemicals but until recently discussion of phosphorus has been limited to orthophosphate and sources thereof. We envisage this work to provide a step-change in thinking about pre-RNA & prebiotic worlds. Analytical measurements arising from the projects will contribute fundamentally to the wider understanding of the interrelationship between minerals and biologically relevant molecular species and how these interactions may leave 'biomarker' degredant traces. Such information is fundamental to exo-biological prospecting and will underpin new areas of investigation for high-impact projects such as the ESA's ExoMars mission where one of the primary objectives is the 'Search for traces of past and present life' in the Martian environment. In the wider context, progress in in situ analyses and, particularly the development of oxo-phosphorus quantitative models, will contribute to ongoing developments in rapid 'real-time' process information for chemical and pharmaceutical manufacturing industries.
First Year Of Impact 2012
Sector Chemicals,Education,Culture, Heritage, Museums and Collections,Pharmaceuticals and Medical Biotechnology
Impact Types Cultural,Societal