Community composition influences ecosystem resistance and production more than species richness or intraspecific diversity

Precipitation alters the relationship between biodiversity and multifunctionality of grassland ecosystems

Precipitation changes largely influence the relationship between biodiversity and ecosystem multifunctionality (EMF). Our understanding of how biodiversity at multiple trophic levels regulates EMF under different precipitation conditions and how the relative importance of biodiversity at these different trophic levels to EMF changes dynamically along the precipitation gradient still needs to be improved. This study evaluated how the relationship between plant diversity, soil biodiversity, and EMF responds to precipitation changes using information obtained on biomes (including plants and soil organisms) and ecological functional traits. We collected 120 samples at eight representative stations along a 3177 km precipitation gradient (mean annual precipitation from 268.4 to 722.9 mm) in the northeastern Tibetan Plateau. We investigated the relationship between plant diversity, soil bacterial and fungal diversity, soil ciliate diversity, and EMF along the precipitation gradient. The results showed that across the precipitation gradient, the functional richness of plant diversity was the strongest predictor of EMF, effectively driving EMF over a wide threshold interval from 10% to 99%, with a maximum effect size of 0.27. The relative importance of plant diversity and soil biodiversity on EMF changes around a mean annual precipitation (MAP) of 450 mm. Plant diversity has a significant positive effect on EMF when MAP is above 463 mm. Soil biodiversity is more critical for EMF when MAP is below 428 mm. Our study shows that the impact of plant and soil biomes on EMF changes dynamically along a precipitation gradient. We identified a critical precipitation threshold of approximately 450 mm MAP, the dividing line between semi-arid and sub-humid climates. Our study highlights that the loss of plant and soil biodiversity may have severe consequences under low and high precipitation conditions, respectively, calling for developing biodiversity conservation strategies in response to climate change to avoid impacts on grassland ecosystem services.

Aboveground and belowground biodiversity have complementary effects on ecosystem functions across global grasslands

Grasslands are integral to maintaining biodiversity and key ecosystem services and are under threat from climate change. Plant and soil microbial diversity, and their interactions, support the provision of multiple ecosystem functions (multifunctionality). However, it remains virtually unknown whether plant and soil microbial diversity explain a unique portion of total variation or shared contributions to supporting multifunctionality across global grasslands. Here, we combine results from a global survey of 101 grasslands with a novel microcosm study, controlling for both plant and soil microbial diversity to identify their individual and interactive contribution to support multifunctionality under aridity and experimental drought. We found that plant and soil microbial diversity independently predict a unique portion of total variation in above- and belowground functioning, suggesting that both types of biodiversity complement each other. Interactions between plant and soil microbial diversity positively impacted multifunctionality including primary production and nutrient storage. Our findings were also climate context dependent, since soil fungal diversity was positively associated with multifunctionality in less arid regions, while plant diversity was strongly and positively linked to multifunctionality in more arid regions. Our results highlight the need to conserve both above- and belowground diversity to sustain grassland multifunctionality in a drier world and indicate climate change may shift the relative contribution of plant and soil biodiversity to multifunctionality across global grasslands.

Effects of plant diversity and community structure on ecosystem multifunctionality under different grazing potentials in the eastern Eurasian steppe

Grazing potential represents the potential carrying capacity of steppe livestock production. Understanding the impact of changes in plant diversity and community structure on ecosystem multifunctionality (EMF) at different grazing potentials is crucial for the sustainable management of steppe ecosystems. We examined the associations between plant diversity, community structure, above-ground ecosystem multifunctionality (AEMF), and below-ground ecosystem multifunctionality (BEMF) at various grazing potentials. Our assessment employed generalized linear mixed-effects models and structural equation models to determine the impact of these factors on ecosystem multifunctionality. Our study results indicated that ecosystem multifunctionality differed depending on the level of grazing potential and decreased as grazing potential declined. The impact of plant diversity and community structure on above- and below-ground ecosystem multifunctionality varied. Plant diversity and community structure correlated more with AEMF than BEMF. Plant diversity had the most significant effect on EMF under high grazing potential, while community structure had the greatest effect on EMF under moderate and low grazing potential. These improve our understanding of the correlation between steppe plant diversity, community structure, and above- and below-ground ecosystem multifunctionality. This understanding is necessary to develop strategies to increase plant diversity or regulate community structure and the sustainability of steppes.

Soil-atmosphere fluxes of CO2, CH4, and N2O across an experimentally-grown, successional gradient of biocrust community types

Biological soil crusts (biocrusts) are critical components of dryland and other ecosystems worldwide, and are increasingly recognized as novel model ecosystems from which more general principles of ecology can be elucidated. Biocrusts are often diverse communities, comprised of both eukaryotic and prokaryotic organisms with a range of metabolic lifestyles that enable the fixation of atmospheric carbon and nitrogen. However, how the function of these biocrust communities varies with succession is incompletely characterized, especially in comparison to more familiar terrestrial ecosystem types such as forests. We conducted a greenhouse experiment to investigate how community composition and soil-atmosphere trace gas fluxes of CO2, CH4, and N2O varied from early-successional light cyanobacterial biocrusts to mid-successional dark cyanobacteria biocrusts and late-successional moss-lichen biocrusts and as biocrusts of each successional stage matured. Cover type richness increased as biocrusts developed, and richness was generally highest in the late-successional moss-lichen biocrusts. Microbial community composition varied in relation to successional stage, but microbial diversity did not differ significantly among stages. Net photosynthetic uptake of CO2 by each biocrust type also increased as biocrusts developed but tended to be moderately greater (by up to ≈25%) for the mid-successional dark cyanobacteria biocrusts than the light cyanobacterial biocrusts or the moss-lichen biocrusts. Rates of soil C accumulation were highest for the dark cyanobacteria biocrusts and light cyanobacteria biocrusts, and lowest for the moss-lichen biocrusts and bare soil controls. Biocrust CH4 and N2O fluxes were not consistently distinguishable from the same fluxes measured from bare soil controls; the measured rates were also substantially lower than have been reported in previous biocrust studies. Our experiment, which uniquely used greenhouse-grown biocrusts to manipulate community composition and accelerate biocrust development, shows how biocrust function varies along a dynamic gradient of biocrust successional stages.