| Literature DB >> 34068713 |
Abstract
The assumption that there was a "water problem" at the emergence of life-that the Hadean Ocean was simply too wet and salty for life to have emerged in it-is here subjected to geological and experimental reality checks. The "warm little pond" that would take the place of the submarine alkaline vent theory (AVT), as recently extolled in the journal Nature, flies in the face of decades of geological, microbiological and evolutionary research and reasoning. To the present author, the evidence refuting the warm little pond scheme is overwhelming given the facts that (i) the early Earth was a water world, (ii) its all-enveloping ocean was never less than 4 km deep, (iii) there were no figurative "Icelands" or "Hawaiis", nor even an "Ontong Java" then because (iv) the solidifying magma ocean beneath was still too mushy to support such salient loadings on the oceanic crust. In place of the supposed warm little pond, we offer a well-protected mineral mound precipitated at a submarine alkaline vent as life's womb: in place of lipid membranes, we suggest peptides; we replace poisonous cyanide with ammonium and hydrazine; instead of deleterious radiation we have the appropriate life-giving redox and pH disequilibria; and in place of messy chemistry we offer the potential for life's emergence from the simplest of geochemically available molecules and ions focused at a submarine alkaline vent in the Hadean-specifically within the nano-confined flexible and redox active interlayer walls of the mixed-valent double layer oxyhydroxide mineral, fougerite/green rust comprising much of that mound.Entities:
Keywords: Hadean Ocean; emergence of life; fougerite/green rust; hydrazine; mushy mantle; peptide membrane; submarine alkaline vents
Year: 2021 PMID: 34068713 PMCID: PMC8151828 DOI: 10.3390/life11050429
Source DB: PubMed Journal: Life (Basel) ISSN: 2075-1729
A Hadean Advisory.
| Effects | Descriptions | References |
|---|---|---|
| Solar luminosity post solar wind | 72% of present flux | [ |
| Solar radiation (UV and X-ray) | Intense: ~100 + times present | [ |
| Earth–Moon distance; Earth’s spin and length of day and tides | <10% of present day; Estimates of length of day from 2 to 10 h; ~20 m tidal amplitude | [ |
| Bombardment and tsunamis | Heavy but not totally vaporizing (negative feedback from heightening atmospheric pressure) | [ |
| Maximum height of ocean plateaux above by mantle plumes. | ~1000 km | [ |
| Ocean depth | 4–6 km | [ |
| Redox state | Upper mantle buffered at quartz-fayalite-magnetite | [ |
| Atmosphere post solar wind | CO2, N2, H2O, > SO2 >> CO, NOx | [ |
| Ocean chemistry | Saline, CO2, NO3−, NO2− + metal ions | [ |
| Magma-driven submarine springs | Acidic, ~400 °C | [ |
| Direct contribution of ~400 °C solution to Hadean Ocean | Fe2+, Mg2+, Mn2+, Zn2+, Co2+, Ni2+, H2S, H2, PO4−, CH4 | [ |
| Serpentinization-driven submarine springs | Alkaline, ~120 °C | [ |
| Direct contribution of ~120 °C alkaline spring to the hydrothermal mound | H2, CH4, HS−, HCOO− > [Fe2S2(MoS4)2]2−/4− | [ |
| Ocean T & pH and chemistry | Strongly carbonic and saline 25 to <85 °C? pH 4.5 to 5.5 with minor nitrate, transition metals in solution fed from ~400 °C springs | [ |
| The Earth electronic and protonic ~1 volt battery | Eh of H2 v. H2O at delta pH 4 to 5 | [ |
| Olivine source of pyrophosphate delivered to ocean via vulcanism | Hydrolysis of volcanic P4O10 to produce P3O93− and P4O124− | [ |
| Lightning | Produces NO from CO2 + N2 | [ |
| Wind speed (cf. “Roaring Forties”) | 12 ms–1 estimate | [ |
| Wave height | 10 m estimate | [ |
| Chemical sediments | Banded iron formation, fougerite, chert, greenalite, mackinawite | [ |
Figure 1Depiction of our Hadean planet. The crust was completely submerged with a ~5 km deep ocean as the magma ocean was still too mushy to support significant bulges even at the apices of mantle plumes [98,99,100,101,102,106,233,234,235] EoL: emergence of life.
An AVT status report.
| Prediction/Expectation | References | Tests | References |
|---|---|---|---|
| Hydrothermal circulation during rift tectonics generates metal sulfide mineral deposits. | [ | Successful field test, | [ |
| Seawater-derived | [ | Stratigraphic, structural, tectonic and lithochemical field work; Lead isotope analyses | [ |
| Some hydrothermal minerals precipitate on sea-floor | [ | Delineation of extensive Mn aureole centered on Irish ore deposit led to the first discovery of fossil hydrothermal chimneys formed through mixing with seawater | [ |
| Some sulfur derived from crustal sources | [ | Isotopic analysis reveals crustal source as do hydrothermal experiments | [ |
| Sulfide dissolves in alkaline hydrothermal solution | [ | Lab demonstrations | [ |
| Serpentinization reaction to formate | [ | Lab demonstration | [ |
| Serpentinization reaction produces H2 >>CH4, although CH4 is entrained from oceanic crust | [ | Prompts amendment to the AVT, viz., to the denitrifying methanotrophic acetogenesis | [ |
| Lightning and space weather radiation produces NOx that rapidly dissolve as nitrate/nitrite in Hadean Ocean | [ | Theoretic studies generally support this hypothesis though not those of Ranjan et al. 2019 [ | [ |
| Source of ammonia at vent from nitrate/nitrite reduction | [ | Eight electron reduction of nitrate to ammonia with green rust | [ |
| Further reduction of NOx to hydrazine N2H4 | [ | Awaiting test | |
| Off-ridge submarine vents will be moderate temperature, H2-bearing, alkaline and long-lived (≥105 years) and would have been the site of life’s emergence | [ | Discovery of Lost City moderate temperature alkaline | [ |
| Green rust, mackinawite/greigite, amorphous silica | [ | Successful lab demonstration | [ |
| Eh and pH gradients ~700 mV and 4–5 units pH (~300 mV) to meet electronic and protonic requirements ~1 V | [ | FeS barriers hold a 700 mV and a 5 unit pH disequilibrium in lab test | [ |
| CO2 reduction forced by H2 and delta pH 4 units | [ | Chemical disequilibria as per Nernst equation | [ |
| The immateriality of the “water problem” in nano-confinement | [ | Lab and molecular dynamic simulations | [ |
| Aminations of carboxylic acids | [ | Lab demonstrations. Amination of pyruvate to alanine | [ |
| Green rust as proto- | [ | Pi + Pi → PPi to equilibrium in microfluidic reactor | [ |
| ΔpH as | [ | Undemonstrated | |
| Oxidation of methane in green rust | [ | Undemonstrated, pending | Cf. [ |
| Theoretical polymerization of amino acids in nano-confined water to produce peptide membranes necessarily pre-LUCA | [ | Undemonstrated, waiting experiment | |
| Expansion from the vent via ocean floor to produce the first deep biosphere | [ | Hypothesis |
Pond and AVT chemistry and “free energies” compared.
| Surface Pond | References | Submarine Alkaline Vent | References | |
|---|---|---|---|---|
| “Free energy” | UV, reverse 2 pH unit pmf | [ | Electrochemical gradients, natural 4 pH unit pmf | [ |
| Electron donors | UV radiation, reduced sulfur & organic compounds, Fe2+ | [ | Fe2+, H2, ē, CH4, HCOO- | [ |
| Electron acceptors | Ferricyanide insidevesicle | [ | Ambient Fe3+, NO, NO2−, NO3− (CO2) | [ |
| Initial boundary | Lipids | [ | Green rust, FeS, silica | [ |
| Organic takeover | Lipids | [ | Peptides | [ |
| Primary ingredients | Lipids HCN, CH3N, H2S, H2O2, quinones, ferricyanide | [ | CO2, H2, CH4, H2O, NO3, NO, NH2, NH3, HPO43−, HS−, Fe2+, Ni2+, Co2+, Mo4+/6+ | [ |
| Other suggestions orderivatives | Acrolein, 2-aminooxazol, quinones, ferricyanide, RNA, DNA, NADH, FMN | [ | NH3 + carboxylic acids → amino acids, N2H4 → heterocycles, e.g., pyrazoles, imides, NAD(P), flavins, quinones | [ |
| Disequilibria conversion mechanisms | Wet/dry cycling aggregation | [ | Visco-elastic allosteric conformational changes/binding change mechanism/pumping/gating/ electrostatic effects | [ |
| Condensations | Wet/dry cycling | [ | Nanoconfined water in green rust interlayers, silica, mackinawite | [ |
| Reproduction | RNA world | [ | Amyloid peptide | [ |
| Waste disposal | None considered | --- | In alkaline spring effluent | [ |