Abstract

Aims: To quantify how fine-grain (within-plot) beta diversity differs among biomes and vegetation types. Study area: Palaearctic biogeographic realm. Methods: We extracted 4,654 nested-plot series with at least four different grain sizes between 0.0001 m² and 1,024 m² from the GrassPlot database spanning broad geographic and ecological gradients. Next, we calculated the slope parameter (z-value) of the power-law species–area relationship (SAR) to use as a measure of multiplicative beta diversity. We did this separately for vascular plants, bryophytes and lichens and for the three groups combined (complete vegetation). We then tested whether z-values differed between biomes, ecological-physiognomic vegetation types at coarse and fine levels and phytosociological classes. Results: We found that z-values varied significantly among biomes and vegetation types. The explanatory power of area for species richness was highest for vascular plants, followed by complete vegetation, bryophytes and lichens. Within each species group, the explained variance increased with typological resolution. In vascular plants, adjusted R2 was 0.14 for biomes, but reached 0.50 for phytosociological classes. Among the biomes, mean z-values were particularly high in the Subtropics with winter rain (Mediterranean biome) and the Dry tropics and subtropics. Natural grasslands had higher z-values than secondary grasslands. Alpine and Mediterranean vegetation types had particularly high z-values whereas managed grasslands with benign soil and climate conditions and saline communities were characterised by particularly low z-values. Conclusions: In this study relating fine-grain beta diversity to typological units, we found distinct patterns. As we explain in a conceptual figure, these can be related to ultimate drivers, such as productivity, stress and disturbance, which can influence z-values via multiple pathways. The provided means, medians and quantiles of z-values for a wide range of typological entities provide benchmarks for local to continental studies, while calling for additional data from under-represented units. Syntaxonomic references: Mucina et al. (2016) for classes occurring in Europe; Ermakov (2012) for classes restricted to Asia. Abbreviations: ANOVA = analysis of variance; EDGG = Eurasian Dry Grassland Group; SAR = species-area relationship.

Highlights

  • The Palaearctic biogeographic realm is the largest terrestrial realm on Earth, covering more than 52 million square kilometres or approximately 40% of the ice-free terrestrial surface of the globe

  • Through covering a diverse set of habitat types and providing high-quality data for vascular plants, and for bryophytes and lichens sampled in the same plots, GrassPlot offers a unique framework to analyse plant diversity patterns and their drivers (Biurrun et al 2021)

  • For log S-space we obtained z-values for 4,570 series for vascular plants, 719 for bryophytes, 417 for lichens and 862 for complete vegetation, while for S-space we estimated z-values for 4,554 series for vascular

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Summary

Introduction

The Palaearctic biogeographic realm (sensu Olson et al 2001) is the largest terrestrial realm on Earth, covering more than 52 million square kilometres or approximately 40% of the ice-free terrestrial surface of the globe. Through covering a diverse set of habitat types and providing high-quality data for vascular plants, and for bryophytes and lichens sampled in the same plots, GrassPlot offers a unique framework to analyse plant diversity patterns and their drivers (Biurrun et al 2021). This is readily evident for species richness, since GrassPlot provides thousands of comprehensively sampled plots at eight standard grain sizes from 0.0001 to 1,000 m2, together with extensive environmental and structural in situ measured variables. Even more unique is the fact that GrassPlot contains thousands of nested-plot series (see Biurrun et al 2019), which allow the analysis of small-scale nested species-area relationships (SARs)

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