Olson JB, Steppe TF, Litaker RW, Paerl HW
Institute of Marine Sciences, UNC-CH, Morehead City, NC 28557, USA
Microb Ecol. 1998 Nov;36(3):231-238. doi: 10.1007/s002489900110.
Abstract Nitrogen (N) availability is a key nutritional factor controlling microbial production in Antarctic freshwater and soil habitats. Since there are no significant sources of biologically available N entering these ecosystems, nitrogen fixation may be a major source of "new" N supporting primary and secondary production. The role of N2 fixation was examined in cyanobacteria-dominated microbial aggregates embedded in the permanent ice cover of Lake Bonney, McMurdo Dry Valley (Victoria Land) lakes area, and in cyanobacterial mats found in soils adjacent to the ice edge. Nitrogenase activity was extremely low compared to temperate and tropical systems, but N2 fixation was found at all study sites. N2 fixation occurred under both dark and light conditions, indicating the potential involvement of both phototrophic and heterotrophic diazotrophs. Nitrogenase activity measurements (acetylene reduction assay) and molecular characterization (PCR amplification of nifH fragments) demonstrated a diverse and periodically active (when liquid water is present) diazotrophic community in this arid, nutrient-limited environment. As a result of the close proximity to other microorganisms and the nutritional constraints of this environment, these diazotrophs may be involved in mutually beneficial consortial relationships that enhance their growth when water is available.
摘要 氮(N)的可利用性是控制南极淡水和土壤栖息地微生物生产的关键营养因素。由于没有大量生物可利用氮进入这些生态系统,固氮作用可能是支持初级和次级生产的“新”氮的主要来源。在麦克默多干谷(维多利亚地)湖区博尼湖永久冰盖中嵌入的以蓝细菌为主的微生物聚集体,以及在冰缘附近土壤中发现的蓝细菌垫中,研究了固氮作用。与温带和热带系统相比,固氮酶活性极低,但在所有研究地点均发现了固氮作用。固氮作用在黑暗和光照条件下均会发生,这表明光养和异养固氮菌都可能参与其中。固氮酶活性测量(乙炔还原测定)和分子特征分析(nifH片段的PCR扩增)表明,在这个干旱、营养有限的环境中,存在一个多样且具有周期性活性(当液态水存在时)的固氮群落。由于与其他微生物的紧密相邻以及该环境的营养限制,这些固氮菌可能参与了互利共生关系,在有水时促进它们的生长。