Table 1.
Transition | Date, Gya | Source | Method |
---|---|---|---|
Abiogenesis | >4.10 ± 0.01 | Bell et al. (2015) | Carbon isotope ratio |
Abiogenesis | 3.9 | Betts et al. (2018) | Molecular clock |
Abiogenesis | >3.86 ± 0.01 | Mojzsis et al. (1996) | Carbon isotope ratio |
Abiogenesis | >3.77–4.28 | Dodd et al. (2017) | Microfossils, isotope ratio |
Abiogenesis | >3.5 | Awramik (1992) | Microfossils, stromatolites |
Cyanobacteria | <10 Ma | Lazcano and Miller (1994) | Molecular evolution model |
Eukaryotes | <1.84 | Betts et al. (2018) | Molecular clock |
Eukaryotes | >1.87–1.68 | Parfrey et al. (2011) | Molecular clock |
Sex | >1.2 | Butterfield (2000) | Fossils of red algae |
Intelligence | ≈0 | Pääbo (2014) | Oldest artwork |
Boundary | Timing | Source | Method |
---|---|---|---|
Oceans form |
4.40 Gya |
Peck et al. (2001) |
Oxygen isotope ratio |
Oceans form |
4.3–4.2 Gya |
Cavosie et al. (2005) |
Oxygen isotope ratio |
Biosphere ends |
0.8–1.2 Ga |
Franck et al. (2006) |
Climate model |
Biosphere ends |
0.9–1.5 Ga |
Caldeira and Kasting (1992) |
Climate model |
Biosphere ends |
≈1.0 Ga |
Kasting (1988) |
Climate model |
Biosphere ends | 1.8–3.3 Ga | Rushby et al. (2013) | Climate model |
Biosphere end dates are given for eukaryotic life. Extremophiles may persist beyond the dates given.