Geochemical Sources and Availability of Amidophosphates on the Early Earth.

Phosphorylation of (pre)biotically relevant molecules in aqueous medium has recently been demonstrated using water-soluble diamidophosphate (DAP). Questions arise relating to the prebiotic availability of DAP and other amidophosphosphorus species on the early earth. Herein, we demonstrate that DAP and other amino-derivatives of phosphates/phosphite are generated when Fe3 P (proxy for mineral schreibersite), condensed phosphates, and reduced oxidation state phosphorus compounds, which could have been available on early earth, are exposed to aqueous ammonia solutions. DAP is shown to remain in aqueous solution under conditions where phosphate is precipitated out by divalent metals. These results show that nitrogenated analogues of phosphate and reduced phosphite species can be produced and remain in solution, overcoming the thermodynamic barrier for phosphorylation in water, increasing the possibility that abiotic phosphorylation reactions occurred in aqueous environments on early earth.

Archean phosphorus liberation induced by iron redox geochemistry.

The element phosphorus (P) is central to ecosystem growth and is proposed to be a limiting nutrient for life. The Archean ocean may have been strongly phosphorus-limited due to the selective binding of phosphate to iron oxyhydroxide. Here we report a new route to solubilizing phosphorus in the ancient oceans: reduction of phosphate to phosphite by iron(II) at low (<200 °C) diagenetic temperatures. Reduction of phosphate to phosphite was likely widespread in the Archean, as the reaction occurs rapidly and is demonstrated from thermochemical modeling, experimental analogs, and detection of phosphite in early Archean rocks. We further demonstrate that the higher solubility of phosphite compared to phosphate results in the liberation of phosphorus from ferruginous sediments. This phosphite is relatively stable after its formation, allowing its accumulation in the early oceans. As such, phosphorus, not as phosphate but as phosphite, could have been a major nutrient in early pre-oxygenated oceans.

Potential Role of Inorganic Confined Environments in Prebiotic Phosphorylation.

A concise outlook on the potential role of confinement in phosphorylation and phosphate condensation pertaining to prebiotic chemistry is presented. Inorganic confinement is a relatively uncharted domain in studies concerning prebiotic chemistry, and even more so in terms of experimentation. However, molecular crowding within confined dimensions is central to the functioning of contemporary biology. There are numerous advantages to confined environments and an attempt to highlight this fact, within this article, has been undertaken, keeping in context the limitations of aqueous phase chemistry in phosphorylation and, to a certain extent, traditional approaches in prebiotic chemistry.

Chemical Transformations in Proto-Cytoplasmic Media. Phosphorus Coupling in the Silica Hydrogel Phase.

It has been proposed that prebiotic chemical studies on the emergence of primitive life would be most relevant when performed in a hydrogel, rather than an aqueous, environment. In this paper we describe the ambient temperature coupling of phosphorus oxyacids [Pi] mediated by Fe(II) under aerobic conditions within a silica hydrogel (SHG) environment. We have chosen to examine SHGs as they have considerable geological precedence as key phases in silicification en route to rock formation. Following a description of the preparation and characterization studies on our SHG formulations, coupling experiments between Pi species are described across multiple permutations of (i) Pi compound; (ii) gel formulation; (iii) metal salt additive; and (iv) pH-modifying agent. The results suggest that successful Pi coupling, indicated by observation of pyrophosphate [PPi(V)] via 31P-NMR spectroscopy, takes place when the following components are present: (i) a mixture of mixture of Pi(III) and Pi(V) or pure PPi(III-V); (ii) Fe(II); (iii) acetic or formic acid (not hydrochloric acid); (iv) aerobic conditions or the presence of H2O2 as an oxidant; and (v) the presence of a gel system. On the basis of these, and aqueous control reactions, we suggest mechanistic possibilities.

Selective Phosphonylation of 5'-Adenosine Monophosphate (5'-AMP) via Pyrophosphite [PPi(III)].

We describe here experiments which demonstrate the selective phospho-transfer from a plausibly prebiotic condensed phosphorus (P) salt, pyrophosphite [H2P2O52-; PPi(III)], to the phosphate group of 5'-adenosine mono phosphate (5'-AMP). We show further that this P-transfer process is accelerated both by divalent metal ions (M2+) and by organic co-factors such as acetate (AcO-). In this specific case of P-transfer from PPi(III) to 5'-AMP, we show a synergistic enhancement of transfer in the combined presence of M2+ & AcO-. Isotopic labelling studies demonstrate that hydrolysis of the phosphonylated 5'-AMP, [P(III)P(V)-5'-AMP], proceeds via nuceophilic attack of water at the Pi(III) terminus.

Phosphorus: a case for mineral-organic reactions in prebiotic chemistry.

The ubiquity of phosphorus (P) in modern biochemistry suggests that P may have participated in prebiotic chemistry prior to the emergence of life. Of the major biogenic elements, phosphorus alone lacks a substantial volatile phase and its ultimate source therefore had to have been a mineral. However, as most native P minerals are chemically un-reactive within the temperature-pressure-pH regimes of contemporary life, it begs the question as to whether the most primitive early living systems on earth had access to a more chemically reactive P-mineral inventory. The meteoritic mineral schreibersite has been proposed as an important source of reactive P on the early earth. The chemistry of schreibersite as a P source is summarized and reviewed here. Recent work has also shown that reduced oxidation state P compounds were present on the early earth; these compounds lend credence to the relevance of schreibersite as a prebiotic mineral. Ultimately, schreibersite will oxidize to phosphate, but several high-energy P intermediates may have provided the reactive material necessary for incorporating P into prebiotic molecules.

Multiplication of microbes below 0.690 water activity: implications for terrestrial and extraterrestrial life.

Since a key requirement of known life forms is available water (water activity; aw ), recent searches for signatures of past life in terrestrial and extraterrestrial environments have targeted places known to have contained significant quantities of biologically available water. However, early life on Earth inhabited high-salt environments, suggesting an ability to withstand low water-activity. The lower limit of water activity that enables cell division appears to be ∼ 0.605 which, until now, was only known to be exhibited by a single eukaryote, the sugar-tolerant, fungal xerophile Xeromyces bisporus. The first forms of life on Earth were, though, prokaryotic. Recent evidence now indicates that some halophilic Archaea and Bacteria have water-activity limits more or less equal to those of X. bisporus. We discuss water activity in relation to the limits of Earth's present-day biosphere; the possibility of microbial multiplication by utilizing water from thin, aqueous films or non-liquid sources; whether prokaryotes were the first organisms able to multiply close to the 0.605-aw limit; and whether extraterrestrial aqueous milieux of ≥ 0.605 aw can resemble fertile microbial habitats found on Earth.

The fuel cell model of abiogenesis: a new approach to origin-of-life simulations.

In this paper, we discuss how prebiotic geo-electrochemical systems can be modeled as a fuel cell and how laboratory simulations of the origin of life in general can benefit from this systems-led approach. As a specific example, the components of what we have termed the "prebiotic fuel cell" (PFC) that operates at a putative Hadean hydrothermal vent are detailed, and we used electrochemical analysis techniques and proton exchange membrane (PEM) fuel cell components to test the properties of this PFC and other geo-electrochemical systems, the results of which are reported here. The modular nature of fuel cells makes them ideal for creating geo-electrochemical reactors with which to simulate hydrothermal systems on wet rocky planets and characterize the energetic properties of the seafloor/hydrothermal interface. That electrochemical techniques should be applied to simulating the origin of life follows from the recognition of the fuel cell-like properties of prebiotic chemical systems and the earliest metabolisms. Conducting this type of laboratory simulation of the emergence of bioenergetics will not only be informative in the context of the origin of life on Earth but may help in understanding whether life might emerge in similar environments on other worlds.

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

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.

Asymmetric general base catalysis of the phospho-aldol reaction via dimeric aluminium hydroxides.

Dimeric aluminium hydroxide complexes containing the (R,R)-N,N'-bis(2'-hydroxy-3'-organobenzyl)-trans-1,2-diaminocyclohexane ligand backbone effect catalysis of the phospho-aldol reaction under ambient, aerobic conditions at catalyst loadings of 0.5 mol% to afford enantioselectivities of ca. 65%.

A Raman spectroscopic study of a fulgurite.

A Raman microspectroscopic study of several fulgurites has been undertaken. A fulgurite is an amorphous mineraloid, a superheated glassy solid that is formed when a lightning bolt hits a sandy or rocky ground and thermal energy is transferred. The Raman spectra revealed several forms of crystalline and fused silica and also the presence of polyaromatic hydrocarbons found in an interfacial zone of a glass bubble. This, together with the presence of anatase, a low-temperature polymorph of TiO(2), suggested that some regions of the fulgurite specimen were not subjected to temperatures of 1800 degrees C, which are attained when lightning hits the surface of sand or a rock.

On the prebiotic potential of reduced oxidation state phosphorus: the H-phosphinate-pyruvate system.

H-Phosphinic acid and pyruvic acid, both plausible prebiotic chemicals, react selectively in water to build structural complexity including amide bond formation under remarkably mild conditions and oxidative coupling of P(1) compounds to condensed pyrophosphorus compounds.

Rapid Raman mapping of a fulgurite.

A fulgurite is a naturally occurring glass formed when lightning hits sand, rock, or soil. The formation of fulgurites is accompanied by mineralogical and sometimes compositional changes, and may record information about the environment in which they were formed. A previous investigation using Raman point spectroscopy discovered the presence of anatase, a low-temperature polymorph of TiO(2), and polyaromatic hydrocarbons within a fulgurite. These findings indicate that there were regions within the sample that were not subjected to temperatures of 2,000 K or more that the matrix is reported to attain when struck by lightning. This paper seeks to expand the previous research by utilizing the capabilities of a new Raman spectroscopic technological development that enables rapid mapping. The entire surface area of a cross-sectioned fulgurite (approximately 40 mm x 23 mm) sample was mapped allowing several regions of polyaromatic hydrocarbons and anatase to be located. Furthermore, shocked quartz was found within the boundary regions of the fulgurite, and is proposed to have resulted from contact with vaporized material during the lightning strike. Shocked quartz is typically indicative of extraterrestrial impact, yet its discovery here suggests that its formation is not exclusive to the impact process.

Interaction of spin-labeled inhibitors of the vacuolar H+-ATPase with the transmembrane Vo-sector.

The osteoclast variant of the vacuolar H(+)-ATPase (V-ATPase) is a potential therapeutic target for combating the excessive bone resorption that is involved in osteoporosis. The most potent in a series of synthetic inhibitors based on 5-(5,6-dichloro-2-indolyl)-2-methoxy-2,4-pentadienamide (INDOL0) has demonstrated specificity for the osteoclast enzyme, over other V-ATPases. Interaction of two nitroxide spin-labeled derivatives (INDOL6 and INDOL5) with the V-ATPase is studied here by using the transport-active 16-kDa proteolipid analog of subunit c from the hepatopancreas of Nephrops norvegicus, in conjunction with electron paramagnetic resonance (EPR) spectroscopy. Analogous experiments are also performed with vacuolar membranes from Saccharomyces cerevisiae, in which subunit c of the V-ATPase is replaced functionally by the Nephrops 16-kDa proteolipid. The INDOL5 derivative is designed to optimize detection of interaction with the V-ATPase by EPR. In membranous preparations of the Nephrops 16-kDa proteolipid, the EPR spectra of INDOL5 contain a motionally restricted component that arises from direct association of the indolyl inhibitor with the transmembrane domain of the proteolipid subunit c. A similar, but considerably smaller, motionally restricted population is detected in the EPR spectra of the INDOL6 derivative in vacuolar membranes, in addition to the larger population from INDOL6 in the fluid bilayer regions of the membrane. The potent classical V-ATPase inhibitor concanamycin A at high concentrations induces motional restriction of INDOL5, which masks the spectral effects of displacement at lower concentrations of concanamycin A. The INDOL6 derivative, which is closest to the parent INDOL0 inhibitor, displays limited subtype specificity for the osteoclast V-ATPase, with an IC(50) in the 10-nanomolar range.

Direct evidence for the availability of reactive, water soluble phosphorus on the early Earth. H-phosphinic acid from the Nantan meteorite.

Anoxic irradiation of a type IIICD iron meteorite known to contain the phosphide mineral schreibersite (Fe,Ni)3P in the presence of ethanol/water affords the reactive oxyacid H-phosphinic acid (H3PO2) as the dominant phosphorus product.

On the origin of the Murchison meteorite phosphonates. Implications for pre-biotic chemistry.

Ab initio calculations, combined with experimental studies on the anaerobic hydrolysis of phosphaalkynes under thermal and photochemical conditions suggest a potential, exogenous source of reduced oxidation state phosphorus for the early Earth.

Concanamycin and indolyl pentadieneamide inhibitors of the vacuolar H+-ATPase bind with high affinity to the purified proteolipid subunit of the membrane domain.

The macrolide antibiotic concanamycin is a potent and specific inhibitor of the vacuolar H(+)-ATPase (V-ATPase), binding to the V(0) membrane domain of this eukaryotic acid pump. Although binding is known to involve the 16 kDa proteolipid subunit, contributions from other V(0) subunits are possible that could account for the apparently different inhibitor sensitivities of pump isoforms in vertebrate cells. In this study, we used a fluorescence quenching assay to directly examine the roles of V(0) subunits in inhibitor binding. Pyrene-labeled V(0) domains were affinity purified from Saccharomyces vacuolar membranes, and the 16 kDa proteolipid was subsequently extracted into chloroform and methanol and purified by size exclusion chromatography. Fluorescence from the isolated proteins was strongly quenched by nanomolar concentrations of both concanamycin and an indolyl pentadieneamide compound, indicating high-affinity binding of both natural macrolide and synthetic inhibitors. Competition studies showed that these inhibitors bind to overlapping sites on the proteolipid. Significantly, the 16 kDa proteolipid in isolation was able to bind inhibitors as strongly as V(0) did. In contrast, proteolipids carrying mutations that confer resistance to both inhibitors showed no binding. We conclude that the extracted 16 kDa proteolipid retains sufficient fold to form a high-affinity inhibitor binding site for both natural and synthetic V-ATPase inhibitors and that the proteolipid contains the major proportion of the structural determinants for inhibitor binding. The role of membrane domain subunit a in concanamycin binding and therefore in defining the inhibitor binding properties of tissue-specific V-ATPases is critically re-assessed in light of these data.

Spin-labelled vacuolar-ATPase inhibitors in lipid membranes.

Two spin-labelled derivatives of the 5-(2-indolyl)-2,4-pentadienoyl class of inhibitors of the vacuolar ATPase have been synthesised and their EPR properties characterised in phospholipid membranes. One spin-labelled inhibitor is the amide derivative of pentadienic acid and 4-amino-TEMPO (INDOL6), and the other is the 3-hydroxymethyl-PROXYL ester (INDOL5). The response of the EPR spectra to the chain-melting transition of dimyristoyl phosphatidylcholine (DMPC) bilayers demonstrates that both derivatives incorporate in phospholipid membranes. The axially anisotropic EPR spectra of INDOL6 in fluid DMPC membranes indicate that the indolyl-pentadienoyl inhibitors intercalate between the lipid chains, in the membrane. INDOL5, designed to possess additional internal segmental mobility, exhibits more nearly isotropic motion of the spin-label moiety in fluid membranes than does INDOL6. The EPR characteristics of INDOL5 are therefore well suited to detecting specific ligand-protein interactions. Progressive saturation EPR experiments with polar and hydrophobic relaxation agents (aqueous Ni2+ and oxygen) show that the nitroxide group is buried in the membrane, with the indole moiety providing the anchor at the membrane polar-apolar interface. Rates of spin-label reduction by externally added ascorbate confirm this assignment. These two spin-labelled derivatives provide complementary EPR probes of the lipid environment (INDOL6), and of ligand-protein interactions (INDOL5), for this class of V-ATPase inhibitor.

Interaction of inhibitors of the vacuolar H(+)-ATPase with the transmembrane Vo-sector.

The macrolide antibiotic concanamycin A and a designed derivative of 5-(2-indolyl)-2,4-pentadienamide (INDOL0) are potent inhibitors of vacuolar H(+)-ATPases, with IC(50) values in the low and medium nanomolar range, respectively. Interaction of these V-ATPase inhibitors with spin-labeled subunit c in the transmembrane V(o)-sector of the ATPase was studied by using the transport-active 16-kDa proteolipid analogue of subunit c from the hepatopancreas of Nephrops norvegicus. Analogous experiments were also performed with vacuolar membranes from Saccharomyces cerevisiae. Membranous preparations of the Nephrops 16-kDa proteolipid were spin-labeled either on the unique cysteine C54, with a nitroxyl maleimide, or on the functionally essential glutamate E140, with a nitroxyl analogue of dicyclohexylcarbodiimide (DCCD). These residues were previously demonstrated to be accessible to lipid. Interaction of the inhibitors with these lipid-exposed residues was studied by using both conventional and saturation transfer EPR spectroscopy. Immobilization of the spin-labeled residues by the inhibitors was observed on both the nanosecond and microsecond time scales. The perturbation by INDOL0 was mostly greater than that by concanamycin A. Qualitatively similar but quantitatively greater effects were obtained with the same spin-label reagents and vacuolar membranes in which the Nephrops 16-kDa proteolipid was expressed in place of the native vma3p proteolipid of yeast. The spin-label immobilization corresponds to a direct interaction of the inhibitors with these intramembranous sites on the protein. A mutational analysis on transmembrane segment 4 known to give resistance to concanamycin A also gave partial resistance to INDOL0. The results are consistent with transmembrane segments 2 and 4 of the 16-kDa putative four-helix bundle, and particularly the functionally essential protonation locus, being involved in the inhibitor binding sites. Inhibition of proton transport may also involve immobilization of the overall rotation of the proteolipid subunit assembly.