Abstract

Earth’s climate is warming, and there is evidence that increased temperature alters soil C cycling, which may result in a self-reinforcing (positive), microbial mediated feedback to the climate system. Though soil microbes are major drivers of soil C cycling, we lack an understanding of how temperature affects SOM decomposition. Numerous studies have explored, to differing degrees, the extent to which climate change may affect biodiversity. While there is ample evidence that community diversity begets ecosystem stability and resilience, we know of keystone species that perform functions whose effects far outweigh their relative abundance. In this paper, we first review the meaning of microbial diversity and how it relates to ecosystem function, then conduct a literature review of field-based climate warming studies that have made some measure of microbial diversity. Finally, we explore how measures of diversity may yield a larger, more complete picture of climate warming effects on microbial communities, and how this may translate to altered carbon cycling and greenhouse gas emissions. While warming effects seem to be ecosystem-specific, the lack of observable consistency between measures is due in some part to the diversity in measures of microbial diversity.

Highlights

  • Soil is one of the most diverse habitats on Earth, and one of the least characterized in terms of the identification and ecological roles of the microbiota

  • It is likely that soil organic matter (SOM) decay will change under future climate, and of the approximately 3100 Pg of carbon stored in soils, an estimated 5% will be lost in the decade due to warming [1,2]

  • This paper focuses on understanding how climate warming affects soil microbial community diversity, and its impacts on ecosystem function

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Summary

Introduction

Soil is one of the most diverse habitats on Earth, and one of the least characterized in terms of the identification and ecological roles of the microbiota. It is likely that soil organic matter (SOM) decay will change under future climate, and of the approximately 3100 Pg of carbon stored in soils, an estimated 5% will be lost in the decade due to warming [1,2]. These estimates illustrate the vulnerability of this stored C, though the mechanisms of how the C will be lost are not well understood. We explore the support for each hypothesis, and evaluate the literature for evidence of diversity or keystone functions in previously published climate warming studies

Functional Implications of Diversity
Warming Effects on Diversity
Mechanisms and Consequences of Warming Effects on Microbial Diversity
Future Directions
Findings
Conflict of Interest
Full Text
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