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

Absence of canonical trophic levels in a microbial mat

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Absence of canonical trophic levels in a microbial mat

Ana C Gonzalez-Nayeck et al. Geobiology. 2022 Sep.

Abstract

In modern ecosystems, the carbon stable isotope (δ13 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 δ13 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 δ13 C compositions of biomass and preservable lipids. Protein Stable Isotope Fingerprinting (P-SIF) is a recently developed method that allows measurement of the δ13 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 δ13 C composition to both cyanobacterial and heterotrophic proteins, and by confirming that highly 13 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 δ13 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."

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References

REFERENCES

    1. Abelson, P. H., & Hoering, T. C. (1961). Carbon isotope fractionation in formation of amino acids by photosynthetic organisms. Proceedings of the National Academy of Sciences of the United States of America, 47, 623-632.
    1. Alldredge, A. L., & Silver, M. W. (1988). Characteristics, dynamics and significance of marine snow. Progress in Oceanography, 20(1), 41-82.
    1. Anderson, K. L., Tayne, T. A., & Ward, D. M. (1987). Formation and fate of fermentation products in hot spring cyanobacterial mats. Applied and Environmental Microbiology, 53, 2343-2352.
    1. Arnosti, C., Steen, A. D., Ziervogel, K., Ghobrial, S., & Jeffrey, W. H. (2011). Latitudinal gradients in degradation of marine dissolved organic carbon. PLoS One, 6, 8-13.
    1. Awramik, S. M. (1992). The oldest records of photosynthesis. Photosynthesis Research, 33, 75-89.

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