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微生物席中不存在典型的营养层次。

Absence of canonical trophic levels in a microbial mat.

机构信息

Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts, USA.

Max-Planck-Institute for Marine Microbiology, Bremen, Germany.

出版信息

Geobiology. 2022 Sep;20(5):726-740. doi: 10.1111/gbi.12511. Epub 2022 Jul 13.

Abstract

In modern ecosystems, the carbon stable isotope (δ C) 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 δ C 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 δ C compositions of biomass and preservable lipids. Protein Stable Isotope Fingerprinting (P-SIF) is a recently developed method that allows measurement of the δ C 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 δ C composition to both cyanobacterial and heterotrophic proteins, and by confirming that highly C-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 δ C 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."

摘要

在现代生态系统中,消费者的碳稳定同位素(δ C)比值通常符合“你吃什么就是什么,+1‰”的原则。然而,对于微生物席系统来说,这种方法可能并不适用,因为在这些系统中,不同的群落通过多种同化途径利用多种碳底物,它们生活在紧密的物理联系中,吞噬作用很少或不存在。为了解释元古代和早古生代的 δ C 记录,当时基于席的生产力可能很普遍,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 δ C 组成。蛋白质稳定同位素指纹图谱(P-SIF)是一种最近开发的方法,允许测量从环境样本中分离出来的、通过蛋白质组学鉴定的整个蛋白质的 δ C 值。在这里,我们使用 P-SIF 来确定美国黄石国家公园巧克力锅温泉微生物席样本中的营养关系。在这个席中,异养细菌的蛋白质与蓝细菌的蛋白质无法区分,这表明“你吃什么就是什么,+1‰”并不适用。为了解释这一发现,我们假设糖的产生和消耗主导着净生态系统代谢,导致一个生产者和消费者共享初级光合作用产物作为共同资源的群落。这一想法通过以下方式得到了验证:确认胞外多糖中的葡萄糖部分在 δ C 组成上与蓝细菌和异养蛋白质相同,并且高度 C depleted 脂肪酸(FAs)的蓝细菌在脂质库中占主导地位,这与过度产生初级光合作用产物的系统的通量平衡预期一致。总的来说,结果证实了微生物生物量和脂质的 δ C 组成与特定代谢物有关,而不是与自养与异养或单个营养级有关。因此,我们建议有氧微生物异养只是“你吃什么就是什么”的一个例子。

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