A Low Temperature Limit for Life on Earth

被引:87
作者
Clarke, Andrew [1 ,2 ]
Morris, G. John [3 ]
Fonseca, Fernanda [4 ]
Murray, Benjamin J. [5 ]
Acton, Elizabeth [3 ]
Price, Hannah C. [5 ]
机构
[1] British Antarctic Survey, Cambridge CB3 0ET, England
[2] Univ E Anglia, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England
[3] Asymptote Ltd, St Johns Innovat Ctr, Cambridge, England
[4] INRA, F-78850 Thiverval Grignon, France
[5] Univ Leeds, Sch Earth & Environm, Leeds, W Yorkshire, England
基金
欧洲研究理事会; 英国自然环境研究理事会;
关键词
CELLULAR DESICCATION TOLERANCE; BIOLOGICAL ICE NUCLEATORS; ANTARCTIC NEMATODE; GLASS-FORMATION; COOLING RATE; DEGREES-C; SURVIVAL; FROZEN; VITRIFICATION; DROPLETS;
D O I
10.1371/journal.pone.0066207
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
There is no generally accepted value for the lower temperature limit for life on Earth. We present empirical evidence that free-living microbial cells cooling in the presence of external ice will undergo freeze-induced desiccation and a glass transition (vitrification) at a temperature between -10 degrees C and -26 degrees C. In contrast to intracellular freezing, vitrification does not result in death and cells may survive very low temperatures once vitrified. The high internal viscosity following vitrification means that diffusion of oxygen and metabolites is slowed to such an extent that cellular metabolism ceases. The temperature range for intracellular vitrification makes this a process of fundamental ecological significance for free-living microbes. It is only where extracellular ice is not present that cells can continue to metabolise below these temperatures, and water droplets in clouds provide an important example of such a habitat. In multicellular organisms the cells are isolated from ice in the environment, and the major factor dictating how they respond to low temperature is the physical state of the extracellular fluid. Where this fluid freezes, then the cells will dehydrate and vitrify in a manner analogous to free-living microbes. Where the extracellular fluid undercools then cells can continue to metabolise, albeit slowly, to temperatures below the vitrification temperature of free-living microbes. Evidence suggests that these cells do also eventually vitrify, but at lower temperatures that may be below -50 degrees C. Since cells must return to a fluid state to resume metabolism and complete their life cycle, and ice is almost universally present in environments at sub-zero temperatures, we propose that the vitrification temperature represents a general lower thermal limit to life on Earth, though its precise value differs between unicellular (typically above -20 degrees C) and multicellular organisms (typically below -20 degrees C). Few multicellular organisms can, however, complete their life cycle at temperatures below similar to-2 degrees C.
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页数:11
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