The
age of Earth is about 4.54 billion years;[33][34][35] the earliest undisputed evidence of life on Earth dates from at least 3.5 billion years ago according to the stromatolite record.[36] Some computer models suggest life began as early as 4.5 billion years ago.[37][38] The oldest evidence of life is indirect in the form of
isotopic fractionation. Microorganisms will preferentially use the lighter isotope of an atom to build biomass, as it takes less energy to break the bonds for metabolic processes.[39] Biologic material will often have a composition that is enriched in lighter isotopes compared to the surrounding rock it's found in.
Carbon isotopes, expressed scientifically in parts per thousand difference from a standard as
δ13C, are frequently used to detect
carbon fixation by organisms and assess if purported early life evidence has biological origins. Typically, life will preferentially metabolize the isotopically light 12C isotope instead of the heavier 13C isotope. Biologic material can record this fractionation of carbon.
The oldest disputed geochemical evidence of life is isotopically light
graphite inside a single
zircon grain from the
Jack Hills in Western Australia.[40][41] The graphite showed a δ13C signature consistent with biogenic carbon on Earth. Other early evidence of life is found in rocks both from the
Akilia Sequence[42] and the
Isua Supracrustal Belt (ISB) in Greenland.[43][44] These 3.7 Ga
metasedimentary rocks also contain graphite or graphite inclusions with carbon isotope signatures that suggest biological fractionation.
The primary issue with isotopic evidence of life is that
abiotic processes can fractionate isotopes and produce similar signatures to biotic processes.[45] Reassessment of the Akilia graphite show that metamorphism,
Fischer-Tropsch mechanisms in hydrothermal environments, and volcanic processes may be responsible for enrichment lighter carbon isotopes.[46][47][48] The ISB rocks that contain the graphite may have experienced a change in composition from hot fluids, i.e.
metasomatism, thus the graphite may have been formed by abiotic chemical reactions.[45] However, the ISB's graphite is generally more accepted as biologic in origin after further
spectral analysis.[43][44]
Metasedimentary rocks from the 3.5 Ga Dresser Formation, which experienced less metamorphism than the sequences in Greenland, contain better preserved geochemical evidence.[49] Carbon isotopes as well as sulfur isotopes found in
barite, which are fractionated by microbial metabolisms during sulfate reduction,[50] are consistent with biological processes.[51][52] However, the Dresser formation was deposited in an active volcanic and hydrothermal environment,[49] and abiotic processes could still be responsible for these fractionations.[53] Many of these findings are supplemented by direct evidence, typically by the presence of
microfossils, however.
Fossil evidence
Fossils are direct evidence of life. In the search for the earliest life, fossils are often supplemented by geochemical evidence. The fossil record does not extend as far back as the geochemical record due to metamorphic processes that erase fossils from geologic units.
Stromatolites are laminated sedimentary structures created by
photosynthetic organisms as they establish a
microbial mat on a sediment surface. An important distinction for biogenicity is their convex-up structures and wavy laminations, which are typical of microbial communities who build preferentially toward the sun.[54] A disputed report of stromatolites is from the 3.7 Ga Isua metasediments that show convex-up, conical, and domical morphologies.[55][56][57] Further mineralogical analysis disagrees with the initial findings of internal convex-up laminae, a critical criteria for stromatolite identification, suggesting that the structures may be deformation features (i.e.
boudins) caused by extensional tectonics in the Isua Supracrustal Belt.[58][59]
The earliest direct evidence of life are stromatolites found in 3.48 billion-year-old
chert in the Dresser formation of the Pilbara Craton in Western Australia.[4] Several features in these fossils are difficult to explain with abiotic processes, for example, the thickening of laminae over flexure crests that is expected from more sunlight.[60] Sulfur isotopes from barite veins in the stromatolites also favor a biologic origin.[61] However, while most scientists accept their biogenicity, abiotic explanations for these fossils cannot be fully discarded due to their hydrothermal depositional environment and debated geochemical evidence.[62]
Most
archean stromatolites older than 3.0 Ga are found in Australia or South Africa. Stratiform stromatolites from the Pilbara Craton have been identified in the 3.47 Ga Mount Ada Basalt.[63]Barberton, South Africa hosts stratiform stromatolites in the 3.46 Hooggenoeg, 3.42 Kromberg and 3.33 Ga Mendon Formations of the
Onverwacht Group.[64][65] The 3.43 Ga
Strelley Pool Formation in Western Australia hosts stromatolites that demonstrate vertical and horizontal changes that may demonstrate microbial communities responding to transient environmental conditions.[66] Thus, it is likely
anoxygenic or oxygenic
photosynthesis has been occurring since at least 3.43 Ga Strelley Pool Formation.[67]
Claims of the earliest life using fossilized microorganisms (
microfossils) are from
hydrothermal ventprecipitates from an ancient sea-bed in the
Nuvvuagittuq Belt of Quebec, Canada. These may be as old as 4.28 billion years, which would make it the oldest evidence of life on Earth, suggesting "an almost instantaneous emergence of life" after
ocean formation 4.41 billion years ago.[68][69] These findings may be better explained by abiotic processes: for example, silica-rich waters,[70] "chemical gardens,"[71] circulating hydrothermal fluids,[72] and volcanic ejecta[73] can produce morphologies similar to those presented in Nuvvuagittuq.
The 3.48 Ga Dresser formation hosts microfossils of
prokaryotic filaments in silica veins, the earliest fossil evidence of life on Earth,[74] but their origins may be volcanic.[75] 3.465-billion-year-old
AustralianApex chert rocks may once have contained
microorganisms,[76][77] although the validity of these findings has been contested.[78][79] "Putative filamentous microfossils," possibly of
methanogens and/or
methanotrophs that lived about 3.42-billion-year-old in "a paleo-subseafloor
hydrothermal vein system of the
Barberton greenstone belt, have been identified in
South Africa."[1] A diverse set of microfossil morphologies have been found in the 3.43 Ga Strelley Pool Formation including spheroid, lenticular, and film-like microstructures.[80] Their biogenicity are strengthened by their observed chemical preservation.[81] The early lithification of these structures allowed important chemical tracers, such as the
carbon-to-nitrogen ratio, to be retained at levels higher than is typical in older, metamorphosed rock units.
Biomarkers are compounds of biologic origin found in the geologic record that can be linked to past life.[82] Although they aren't preserved until the late Archean, they are important indicators of early
photosynthetic life.
Lipids are particularly useful biomarkers because they can survive for long periods of geologic time and reconstruct past environments.[83]
Fossilized lipids were reported from 2.7 Ga laminated
shales from the Pilbara Craton[84] and the 2.67 Ga
Kaapvaal Craton in South Africa.[85] However, the age of these biomarkers and whether their deposition was synchronous with their host rocks were debated,[86] and further work showed that the lipids were contaminants.[87] The oldest "clearly indigenous"[88] biomarkers are from the 1.64 Ga Barney Creek Formation in the
McArthur Basin in Northern Australia,[89][90] but
hydrocarbons from the 1.73 Ga Wollogorang Formation in the same basin have also been detected.[88]
Other indigenous biomarkers can be dated to the
Mesoproterozoic era (1.6-1.0 Ga). The 1.4 Ga Hongshuizhuang Formation in the
North China Craton contains hydrocarbons in shales that were likely sourced from
prokaryotes.[91] Biomarkers were found in
siltstones from the 1.38 Ga Roper Group of the McArthur Basin.[92] Hydrocarbons possibly derived from bacteria and algae were reported in 1.37 Ga Xiamaling Formation of the NCC.[93] The 1.1 Ga Atar/El Mreïti Group in the
Taoudeni Basin, Mauritania show indigenous biomarkers in black shales.[94]
By
comparing the genomes of modern organisms (in the domains
Bacteria and
Archaea), it is evident that there was a
last universal common ancestor (LUCA). LUCA is not thought to be the first life on Earth, but rather the only type of organism of its time to still have living descendants. In 2016, M. C. Weiss and colleagues proposed a minimal set of genes that each occurred in at least two groups of Bacteria and two groups of Archaea. They argued that such a distribution of genes would be unlikely to arise by
horizontal gene transfer, and so any such genes must have derived from the LUCA.[95] A
molecular clock model suggests that the LUCA may have lived 4.477—4.519 billion years ago, within the
Hadean eon.[37][38]
Model Hadean-like
geothermalmicroenvironments were demonstrated to have the potential to support the synthesis and replication of
RNA and thus possibly the evolution of primitive life.[96] Porous rock systems, comprising heated air-water interfaces, were shown to facilitate
ribozymecatalyzed RNA replication of sense and antisense strands and then subsequent strand-dissociation.[96] This enabled combined synthesis, release and folding of active ribozymes.[96]
Further work on early life
Extraterrestrial origin for early life?
While current geochemical evidence dates the origin of life to possibly as early as 4.1 Ga, and fossil evidence shows life at 3.5 Ga, some researchers speculate that life may have started nearly 4.5 billion years ago.[37][38] According to biologist
Stephen Blair Hedges, "If life arose relatively quickly on Earth ... then it could be common in the
universe."[99][100][101] The possibility that terrestrial life forms may have been seeded from outer space has been considered.[102][103] In January 2018, a study found that 4.5 billion-year-old
meteorites found on Earth contained
liquid water along with
prebioticcomplex organic substances that may be ingredients for
life.[104]
^Altermann, Wladyslaw (2009). "From Fossils to Astrobiology – A Roadmap to Fata Morgana?". In Seckbach, Joseph; Walsh, Maud (eds.). From Fossils to Astrobiology: Records of Life on Earth and the Search for Extraterrestrial Biosignatures. Cellular Origin, Life in Extreme Habitats and Astrobiology. Vol. 12. Dordrecht, the Netherlands; London:
Springer Science+Business Media. p. xvii.
ISBN978-1-4020-8836-0.
LCCN2008933212.
^Dose, K.; Bieger-Dose, A.; Dillmann, R.; Gill, M.; Kerz, O.; Klein, A.; Meinert, H.; Nawroth, T.; Risi, S.; Stridde, C. (1995). "ERA-experiment "space biochemistry"". Advances in Space Research. 16 (8): 119–129.
Bibcode:
1995AdSpR..16h.119D.
doi:
10.1016/0273-1177(95)00280-R.
PMID11542696.
^Horneck, G.; Eschweiler, U.; Reitz, G.; Wehner, J.; Willimek, R.; Strauch, K. (1995). "Biological responses to space: results of the experiment "Exobiological Unit" of ERA on EURECA I". Adv. Space Res. 16 (8): 105–118.
Bibcode:
1995AdSpR..16h.105H.
doi:
10.1016/0273-1177(95)00279-N.
PMID11542695.
^Weiss, M. C.; Sousa, F. L.; Mrnjavac, N.; Neukirchen, S.; Roettger, M.; Nelson-Sathi, S.; Martin, W. F. (2016). "The physiology and habitat of the last universal common ancestor". Nature Microbiology. 1 (9): 16116.
doi:
10.1038/nmicrobiol.2016.116.
PMID27562259.
S2CID2997255.
^
abcSalditt A, Karr L, Salibi E, Le Vay K, Braun D, Mutschler H. Ribozyme-mediated RNA synthesis and replication in a model Hadean microenvironment. Nat Commun. 2023 Mar 17;14(1):1495. doi: 10.1038/s41467-023-37206-4. PMID: 36932102; PMCID: PMC10023712