Table 4.
The Known Limits of Life on Earth
| Factor | Extremophile | Earth environments | Limit | References |
|---|---|---|---|---|
| High temperature | Thermophile or hyperthermophile | Submarine hydrothermal vents, terrestrial hot springs, deep subterranean environments | 121–122°C | 1–3 |
| Low temperature | Psychrophile | Ice, permafrost, Antarctic dry valleys | −20°C | 4–5 |
| High pressure | Barophile or piezophile | Subseafloor, deep subterranean environments such as the Mariana Trench | >1300 atm | 6–8 |
| High pH | Alkaliphile | Soda lakes | 11.3–11.4 | 9–11 |
| Low pH | Acidophile | Acid mine drainage, hot springs | −0.06 | 12–14 |
| High salinity | Halophile | Brines, evaporite deposits | NaCl ∼5 M | 15–17 |
| Desiccation | Xerophile | Antarctic dry valleys, deserts | <10% relative humidity | 18–20 |
| Ionizing radiation | Radioresistant | High-radiation environments (from radioactive waste, nuclear reactors, cosmic rays, gamma rays, X-rays) | >6000 Gy | 21–23 |
| UV radiation | Radioresistant | High deserts, upper atmosphere | 5000 J/m2 | 21, 24 |
| Toxic element concentrations | — | Acid mine drainage, hot springs | Depends on element | 25–26 |
Blochl et al., 1997; 2Bryer et al., 2000; 3Takai et al., 2008; 4Carpenter et al., 2000; 5Joyce et al., 2004; 6Horikoshi, 1998; 7Sharma et al., 2002; 8Margosch et al., 2006; 9Sturr et al., 1994; 10Jones et al., 1998; 11Sorokin et al., 2001; 12Schleper et al., 1995; 13Johnson, 1998; 14Edwards et al., 2000; 15Antón et al., 2008; 16Oren, 2010; 17Bowers and Wiegel, 2011; 18Potts, 1994; 19Alpert, 2005; 20García, 2011; 21Battista, 1997; 22Ferreira et al., 1999; 23DeVeaux et al., 2007; 24Altiero et al., 2011; 25Nies, 2000; 26Robbins et al., 2000.