Absence of canonical trophic levels in a microbial mat

IF 2.7 2区 地球科学 Q2 BIOLOGY Geobiology Pub Date : 2022-07-13 DOI:10.1111/gbi.12511
Ana C. Gonzalez-Nayeck, Wiebke Mohr, Tiantian Tang, Sarah Sattin, M. Niki Parenteau, Linda L. Jahnke, Ann Pearson
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引用次数: 2

Abstract

In modern ecosystems, the carbon stable isotope (δ13C) ratios of consumers generally conform to the principle “you are what you eat, +1‰.” However, this metric may not apply to microbial mat systems where diverse communities, using a variety of carbon substrates via multiple assimilation pathways, live in close physical association and phagocytosis is minimal or absent. To interpret the δ13C record of the Proterozoic and early Paleozoic, when mat-based productivity likely was widespread, it is necessary to understand how a microbially driven producer–consumer structure affects the δ13C compositions of biomass and preservable lipids. Protein Stable Isotope Fingerprinting (P-SIF) is a recently developed method that allows measurement of the δ13C values of whole proteins, separated from environmental samples and identified taxonomically via proteomics. Here, we use P-SIF to determine the trophic relationships in a microbial mat sample from Chocolate Pots Hot Springs, Yellowstone National Park (YNP), USA. In this mat, proteins from heterotrophic bacteria are indistinguishable from cyanobacterial proteins, indicating that “you are what you eat, +1‰” is not applicable. To explain this finding, we hypothesize that sugar production and consumption dominate the net ecosystem metabolism, yielding a community in which producers and consumers share primary photosynthate as a common resource. This idea was validated by confirming that glucose moieties in exopolysaccharide were equal in δ13C composition to both cyanobacterial and heterotrophic proteins, and by confirming that highly 13C-depleted fatty acids (FAs) of Cyanobacteria dominate the lipid pool, consistent with flux-balance expectations for systems that overproduce primary photosynthate. Overall, the results confirm that the δ13C composition of microbial biomass and lipids is tied to specific metabolites, rather than to autotrophy versus heterotrophy or to individual trophic levels. Therefore, we suggest that aerobic microbial heterotrophy is simply a case of “you are what you eat.”

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缺乏典型的营养水平的微生物垫
在现代生态系统中,消费者的碳稳定同位素(δ13C)比值一般符合“人如其食,+1‰”的原则。然而,这一指标可能不适用于微生物垫系统,在这些系统中,不同的群落通过多种同化途径使用各种碳基质,生活在密切的物理关联中,吞噬作用最小或不存在。为了解释元古代和早古生代的δ13C记录,有必要了解微生物驱动的生产者-消费者结构如何影响生物量和可保存脂质的δ13C组成。蛋白质稳定同位素指纹图谱(P-SIF)是最近发展起来的一种方法,可以测量从环境样品中分离出来的整个蛋白质的δ13C值,并通过蛋白质组学进行分类鉴定。在这里,我们使用P-SIF来确定来自美国黄石国家公园(YNP)巧克力壶温泉的微生物垫样品的营养关系。在这个垫中,来自异养菌的蛋白质与蓝藻的蛋白质无法区分,说明“吃什么就是什么,+1‰”不适用。为了解释这一发现,我们假设糖的生产和消费主导了净生态系统代谢,从而产生了一个生产者和消费者共享初级光合作用作为共同资源的社区。这一观点得到了验证,证实了胞外多糖中的葡萄糖部分与蓝藻和异养蛋白的δ13C组成相同,并证实了蓝藻的高度13c耗尽脂肪酸(FAs)主导了脂质池,这与过量产生初级光合作用的系统的通量平衡预期一致。总体而言,结果证实微生物生物量和脂质的δ13C组成与特定的代谢物有关,而不是与自养与异养或个体营养水平有关。因此,我们认为需氧微生物异养只是一个“你吃什么就是什么”的例子。
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来源期刊
Geobiology
Geobiology 生物-地球科学综合
CiteScore
6.80
自引率
5.40%
发文量
56
审稿时长
3 months
期刊介绍: The field of geobiology explores the relationship between life and the Earth''s physical and chemical environment. Geobiology, launched in 2003, aims to provide a natural home for geobiological research, allowing the cross-fertilization of critical ideas, and promoting cooperation and advancement in this emerging field. We also aim to provide you with a forum for the rapid publication of your results in an international journal of high standing. We are particularly interested in papers crossing disciplines and containing both geological and biological elements, emphasizing the co-evolutionary interactions between life and its physical environment over geological time. Geobiology invites submission of high-quality articles in the following areas: Origins and evolution of life Co-evolution of the atmosphere, hydrosphere and biosphere The sedimentary rock record and geobiology of critical intervals Paleobiology and evolutionary ecology Biogeochemistry and global elemental cycles Microbe-mineral interactions Biomarkers Molecular ecology and phylogenetics.
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