Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, CO 80523, USA. Department of Ecology, Evolution and Marine Biology, University of California, Santa Barbara, CA 93117, USA.
Environ Microbiol Rep. 2009 Apr;1(2):162-6. doi: 10.1111/j.1758-2229.2009.00025.x. Epub 2009 Mar 6.
There is some evidence that microbes inhabiting permanently frozen environments are capable of cell maintenance and growth under in situ conditions. In contrast, Arctic tundra surface soils that are only frozen during the winter have exhibited CO2 respiration under frozen conditions. This could result from maintenance metabolism fuelled by recycling cell material, but does necessarily indicate growth, which requires the synthesis of new cell material. We used (13) C-glucose to trace C into membrane lipids and 5-bromo-3-deoxyuridine to monitor DNA synthesis in a laboratory microcosm study on Arctic tundra soils. Organisms were not equally active: fungi incorporated more C than any other group. Although some bacteria were growing, Gram(+) bacteria were almost completely inactive. Shrub tundra microbes were more active in early winter than tussock microbes, incorporating more C and synthesizing more DNA. In late winter, the C incorporation pattern reversed, although DNA production was similar. We demonstrated for the first time that microbes in frozen tundra soils synthesized new cell membranes and DNA, processes fundamentally associated with growth. That microbes can grow during Arctic winters may have important implications for C cycle modelling under a changing climate.
有一些证据表明,栖息在永久冻结环境中的微生物能够在原位条件下维持细胞并生长。相比之下,仅在冬季冻结的北极冻原生态系统表面土壤在冻结条件下表现出 CO2 呼吸作用。这可能是由于回收细胞物质提供的维持代谢,但并不一定表明生长,生长需要合成新的细胞物质。我们使用 (13)C-葡萄糖追踪 C 进入膜脂质,并用 5-溴-2′-脱氧尿苷监测北极冻原生态系统土壤的实验室微宇宙研究中的 DNA 合成。生物的活性并不相同:真菌比任何其他群体都更多地吸收 C。虽然有些细菌在生长,但革兰氏阳性菌几乎完全不活跃。灌木冻原生态系统的微生物在初冬比草丛微生物更活跃,吸收更多的 C 并合成更多的 DNA。在隆冬,尽管 DNA 产量相似,但 C 的掺入模式发生了逆转。我们首次证明,冻结的冻原生态系统土壤中的微生物合成了新的细胞膜和 DNA,这些过程与生长密切相关。微生物能够在北极冬季生长,这可能对气候变化下的 C 循环模型产生重要影响。