Abstract

Trait-based approaches provide a candidate framework for linking soil microbial community to ecosystem processes, yet how the trade-offs in different microbial traits regulate the community-level metabolic efficiency remains unknown. Herein we assessed the roles of the microbial taxa with particular trait strategies in mediating soil microbial metabolic efficiency along an altitude gradient on the Tibetan Plateau. Results showed that soil microbial metabolic efficiency declined with increasing altitude, as indicated by the increasing metabolic quotient (microbial respiration per unit biomass, qCO2) and decreasing carbon use efficiency (CUE). Both qCO2 and CUE were predominantly predicted by microbial physiological and taxonomic attributes after considering key environmental factors including soil pH, substrate quantity and quality. Specifically, the reduced metabolic efficiency was associated with higher investment into nutrient (particularly for phosphorus) acquisitions via enzymes. Furthermore, we identified key microbial assemblies selected by harsh environments (low substrate quality and temperature) as important predictors of metabolic efficiency. These results suggest that particular microbial assemblies adapted to nutrient limited and cold habitats, but at the expense of lower metabolic efficient at higher altitude. Our findings provide a candidate mechanism underlying community-level metabolic efficiency, which has important implications for microbial-mediated processes such as carbon dynamics under global climate changes.

Highlights

  • Soil microorganisms are critical drivers of the global carbon (C) cycle because of their roles in both soil organic C (SOC) decomposition and formation, regulating major C flux between soil and atmosphere [1, 2]

  • We investigated the associations between microbial metabolic efficiency and resource acquisition strategies

  • Microbial metabolic efficiency and resource acquisition traits along the altitude gradient Microbial metabolic quotient at a community level increased (P < 0.01), while C use efficiency (CUE) decreased with increasing altitude (P < 0.05, Fig. 1a)

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Summary

Introduction

Soil microorganisms are critical drivers of the global carbon (C) cycle because of their roles in both soil organic C (SOC) decomposition and formation, regulating major C flux between soil and atmosphere [1, 2]. Recent studies suggest that the inclusion of metabolic efficiency into existing models improves the prediction of soil C cycling under global changes [6, 7]. Previous studies indicated that altered environmental conditions induced changes in microbial community structure and physiological attributes [9, 10], which may contribute to changes in communitylevel metabolic efficiency [11]. Despite the acknowledgment that intrinsic properties of microbial community are critical to ecosystem functions [12, 13], how these multiple physiological traits inherent to complex microbial community regulate their energy efficiency remains unclear

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