Abstract

BackgroundIdentifying organism-environment interactions at the molecular level is crucial to understanding how organisms adapt to and change the chemical and molecular landscape of their habitats. In this work we investigated whether relative amino acid compositions could be used as a molecular signature of an environment and whether such a signature could also be observed at the level of the cellular amino acid composition of the microorganisms that inhabit that environment.Methodologies/Principal FindingsTo address these questions we collected and analyzed environmental amino acid determinations from the literature, and estimated from complete genomic sequences the global relative amino acid abundances of organisms that are cognate to the different types of environment. Environmental relative amino acid abundances clustered into broad groups (ocean waters, host-associated environments, grass land environments, sandy soils and sediments, and forest soils), indicating the presence of amino acid signatures specific for each environment. These signatures correlate to those found in organisms. Nevertheless, relative amino acid abundance of organisms was more influenced by GC content than habitat or phylogeny.ConclusionsOur results suggest that relative amino acid composition can be used as a signature of an environment. In addition, we observed that the relative amino acid composition of organisms is not highly determined by environment, reinforcing previous studies that find GC content to be the major factor correlating to amino acid composition in living organisms.

Highlights

  • As early and in the 1930s, Alfred Redfield analyzed the oceanic ratios of carbon, nitrogen and phosphorus to find that they were approximately constant at 106C:16N:1P and similar to those observed in the organisms living in those ecosystems [1]

  • Our results suggest that relative amino acid composition can be used as a signature of an environment

  • We observed that the relative amino acid composition of organisms is not highly determined by environment, reinforcing previous studies that find GC content to be the major factor correlating to amino acid composition in living organisms

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Summary

Introduction

As early and in the 1930s, Alfred Redfield analyzed the oceanic ratios of carbon, nitrogen and phosphorus to find that they were approximately constant at 106C:16N:1P and similar to those observed in the organisms living in those ecosystems [1]. Long term deficits of a given environmental chemical nutrient can be a driving force for evolutionary changes in the composition of the enzymes that fix that nutrient Such changes in the enzyme’s composition usually lead to a decrease in the frequency of amino acids that contain large amounts of the limiting environmental nutrient [9]. Environmental relative amino acid abundances clustered into broad groups (ocean waters, host-associated environments, grass land environments, sandy soils and sediments, and forest soils), indicating the presence of amino acid signatures specific for each environment. These signatures correlate to those found in organisms. Relative amino acid abundance of organisms was more influenced by GC content than habitat or phylogeny

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