Increased microbial growth, biomass, and turnover drive soil organic carbon accumulation at higher plant diversity. (28th August 2019)

• Record Type: Journal Article
• Authors: Prommer, Judith; Walker, Tom W. N.; Wanek, Wolfgang; Braun, Judith; Zezula, David; Hu, Yuntao; Hofhansl, Florian; Richter, Andreas
• Is Part Of: Global change biology. Volume 26:Number 2(2020)
• Page Start: 669
• Page End: 681
• Publication Date: 2019-08-28
• Subjects: microbial activity -- microbial carbon use efficiency -- microbial necromass -- microbial turnover -- plant diversity -- soil organic carbon; Climatic changes -- Environmental aspects -- Periodicals; Troposphere -- Environmental aspects -- Periodicals; Biodiversity conservation -- Periodicals; Eutrophication -- Periodicals; 551.5
• DOI: 10.1111/gcb.14777
• Languages: English
• ISSNs: 1354-1013

Abstract

Abstract: Species‐rich plant communities have been shown to be more productive and to exhibit increased long‐term soil organic carbon (SOC) storage. Soil microorganisms are central to the conversion of plant organic matter into SOC, yet the relationship between plant diversity, soil microbial growth, turnover as well as carbon use efficiency (CUE) and SOC accumulation is unknown. As heterotrophic soil microbes are primarily carbon limited, it is important to understand how they respond to increased plant‐derived carbon inputs at higher plant species richness (PSR). We used the long‐term grassland biodiversity experiment in Jena, Germany, to examine how microbial physiology responds to changes in plant diversity and how this affects SOC content. The Jena Experiment considers different numbers of species (1–60), functional groups (1–4) as well as functional identity (small herbs, tall herbs, grasses, and legumes). We found that PSR accelerated microbial growth and turnover and increased microbial biomass and necromass. PSR also accelerated microbial respiration, but this effect was less strong than for microbial growth. In contrast, PSR did not affect microbial CUE or biomass‐specific respiration. Structural equation models revealed that PSR had direct positive effects on root biomass, and thereby on microbial growth and microbial biomass carbon. Finally, PSR increased SOC content via its positive influence on microbial biomass carbon. We suggest that PSR favors faster rates of microbial growth and turnover, likely due to greater plant productivity, resulting in higher amounts of microbial biomass and necromass that translate into the observed increase in SOC. We thus identify the microbial mechanism linking species‐rich plant communities to a carbon cycle process of importance to Earth's climate system. Abstract : Increased soil carbon storage through species‐rich plant communities is crucial to mitigate global climate change and reinforces the importance of biodiversity for ecosystem functioning and services. In this study, we investigated the mechanisms linking plant diversity and plant productivity with soil organic carbon (SOC) dynamics. Increases in plant diversity promoted soil microbial growth and turnover through higher plant‐derived carbon input into soil. This accelerated growth and turnover of the soil microbial community increased microbial biomass and subsequent microbial necromass pools that ultimately led to higher SOC accumulation in species‐rich plant communities.