Winogradsky Institute of Microbiology, Russian Academy of Sciences, Prospect 60-let Octyabrya 7/2, Moscow, 117312, Russia.
Extremophiles. 2012 Nov;16(6):883-94. doi: 10.1007/s00792-012-0484-6. Epub 2012 Sep 25.
Chitin is produced in large amounts in hypersaline habitats with neutral pH due to the high biomass production of brine shrimp Artemia. Recently, a high abundance of Artemia was also noticed in hypersaline soda lakes in the Kulunda Steppe (Altai, Russia), which prompted us to survey the possibility of microbial chitin utilization at extremely haloalkaline conditions in soda brines. Most active chitin utilisation-supporting microbial growth was found at anaerobic conditions at pH 10 and up to 3.5 M total Na(+). At aerobic conditions, the degradation of chitin was slower, mostly incomplete and active at <2 M total Na(+), although very slow partial degradation was possible up to 4 M Na(+). Anaerobic enrichments at pH 10 yielded two different groups of obligately haloalkaliphilic fermentative anaerobes, exclusively specialized to utilise insoluble chitin as the only growth substrate. One group was represented by a single strain growing at moderate salinity, and another comprised multiple isolates growing up to 3.5 M Na(+). These groups represent two novel bacterial phyla not closely related to any other cultured bacteria. Aerobic enrichments from the lake sediments were dominated by several obligately haloalkaliphilic members of the genus Marinimicrobium in the Gammaproteobacteria. They were less specialised than the anaerobes and grew with chitin and its monomer and oligomers at a pH of 10 up to 2.5 M Na(+). Furthermore, several strains of haloalkaliphilic Gram-positive chitinolytics belonging to bacilli and actinobacteria were isolated from soda lake sediments and surrounding soda soils. In general, the results indicate the presence of an active and diverse haloalkaliphilic chitinolytic microbial community in hypersaline soda habitats.
甲壳素在中性 pH 值的高盐环境中大量产生,这是由于卤虫(Artemia)的高生物质产量。最近,在俄罗斯阿尔泰库伦达草原(Kulunda Steppe)的高盐苏打湖中也发现了大量的卤虫,这促使我们调查在苏打卤水中极盐碱性条件下微生物利用甲壳素的可能性。在 pH 值为 10 及以上和高达 3.5 M 总 Na(+)的厌氧条件下,发现了最多支持微生物生长的活性甲壳素利用。在好氧条件下,甲壳素的降解速度较慢,主要在 <2 M 总 Na(+)时不完全,尽管在高达 4 M Na(+)时可能会非常缓慢地进行部分降解。在 pH 值为 10 时进行的厌氧富集得到了两组专性嗜盐碱性发酵厌氧菌,它们专门利用不溶性甲壳素作为唯一的生长基质。一组由在中等盐度下生长的单一菌株组成,另一组由多达 3.5 M Na(+)的多个分离株组成。这两组代表了两个与任何其他培养细菌都没有密切关系的新型细菌门。从湖底沉积物中进行的好氧富集主要由γ变形菌纲的 Marinimicrobium 属中的几个专性嗜盐碱性成员组成。它们不如厌氧菌专业化,并且可以在 pH 值为 10 及高达 2.5 M Na(+)的条件下与甲壳素及其单体和低聚物一起生长。此外,还从苏打湖沉积物和周围苏打土壤中分离出了几种属于芽孢杆菌和放线菌的嗜盐碱性革兰阳性甲壳素降解菌。总的来说,这些结果表明在高盐苏打栖息地中存在一个活跃且多样化的嗜盐碱性甲壳素分解微生物群落。