Department of Chemistry and Biochemistry, Institute for Genomics and Proteomics, University of California, Los Angeles, CA, USA.
Adv Microb Physiol. 2012;60:91-210. doi: 10.1016/B978-0-12-398264-3.00002-4.
Microorganisms play a dominant role in the biogeochemical cycling of nutrients. They are rightly praised for their facility for fixing both carbon and nitrogen into organic matter, and microbial driven processes have tangibly altered the chemical composition of the biosphere and its surrounding atmosphere. Despite their prodigious capacity for molecular transformations, microorganisms are powerless in the face of the immutability of the elements. Limitations for specific elements, either fleeting or persisting over eons, have left an indelible trace on microbial genomes, physiology, and their very atomic composition. We here review the impact of elemental limitation on microbes, with a focus on selected genetic model systems and representative microbes from the ocean ecosystem. Evolutionary adaptations that enhance growth in the face of persistent or recurrent elemental limitations are evident from genome and proteome analyses. These range from the extreme (such as dispensing with a requirement for a hard to obtain element) to the extremely subtle (changes in protein amino acid sequences that slightly, but significantly, reduce cellular carbon, nitrogen, or sulfur demand). One near-universal adaptation is the development of sophisticated acclimation programs by which cells adjust their chemical composition in response to a changing environment. When specific elements become limiting, acclimation typically begins with an increased commitment to acquisition and a concomitant mobilization of stored resources. If elemental limitation persists, the cell implements austerity measures including elemental sparing and elemental recycling. Insights into these fundamental cellular properties have emerged from studies at many different levels, including ecology, biological oceanography, biogeochemistry, molecular genetics, genomics, and microbial physiology. Here, we present a synthesis of these diverse studies and attempt to discern some overarching themes.
微生物在营养物质的生物地球化学循环中起着主导作用。它们能够有效地将碳和氮固定为有机物,这一点得到了广泛的赞誉。微生物驱动的过程明显改变了生物圈及其周围大气的化学成分。尽管微生物具有巨大的分子转化能力,但在元素的不变性面前,它们无能为力。特定元素的限制,无论是短暂的还是持续数亿年的,都在微生物基因组、生理学及其原子组成上留下了不可磨灭的痕迹。在这里,我们回顾了元素限制对微生物的影响,重点介绍了海洋生态系统中的一些遗传模式系统和代表性微生物。从基因组和蛋白质组分析中可以明显看出,增强在持续或反复元素限制下生长的进化适应。这些适应范围从极端(例如放弃对难以获得的元素的需求)到极其微妙(蛋白质氨基酸序列的变化,这些变化略微但显著地降低了细胞对碳、氮或硫的需求)。一种近乎普遍的适应是细胞发展出复杂的适应程序,根据环境变化来调整其化学成分。当特定元素变得有限时,适应通常始于增加对获取的承诺,并伴随着存储资源的动员。如果元素限制持续存在,细胞会采取节约措施,包括元素节约和元素再循环。这些基本细胞特性的见解来自于许多不同层次的研究,包括生态学、生物海洋学、生物地球化学、分子遗传学、基因组学和微生物生理学。在这里,我们综合了这些多样化的研究,并试图识别出一些总体主题。