ArticleNature communications2024
Landform and lithospheric development contribute to the assembly of mountain floras in China.
Article in Nature communications, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.
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8 citing papers in PubMed.
- Bedrock lithology determines forest demographic responses to drought.Nature communications · 2026Article
- Article
- Plastid and nuclear phylogenomics of Cyphostemma (Vitaceae) provide new insights into genome size evolution across sub-Saharan Africa.Journal of integrative plant biology · 2026Article
- Phylogenetic discordance arises from incomplete lineage sorting and pre-speciation introgression during erosion-mediated radiation of Asian warty newts.Zoological research · 2026Article
- Elevational patterns of multidimensional plant diversity and community structure in a subtropical karst mountain system.Plant diversity · 2026Article
- Survival at the edge: genomic vulnerability and genetic purging of a limestone cliff-endemic sky island shrub under climate change.Forestry research · 2026Article
- Cliff-dwelling plants: rare and precious species in harsh habitats.Frontiers in plant science · 2025Review
- Landform and lithospheric development contribute to the assembly of mountain floras in China.Nature communications · 2024Article
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32 authors.
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Abstract
Although it is well documented that mountains tend to exhibit high biodiversity, how geological processes affect the assemblage of montane floras is a matter of ongoing research. Here, we explore landform-specific differences among montane floras based on a dataset comprising 17,576 angiosperm species representing 140 Chinese mountain floras, which we define as the collection of all angiosperm species growing on a specific mountain. Our results show that igneous bedrock (granitic and karst-granitic landforms) is correlated with higher species richness and phylogenetic overdispersion, while the opposite is true for sedimentary bedrock (karst, Danxia, and desert landforms), which is correlated with phylogenetic clustering. Furthermore, we show that landform type was the primary determinant of the assembly of evolutionarily older species within floras, while climate was a greater determinant for younger species. Our study indicates that landform type not only affects montane species richness, but also contributes to the composition of montane floras. To explain the assembly and differentiation of mountain floras, we propose the 'floristic geo-lithology hypothesis', which highlights the role of bedrock and landform processes in montane floristic assembly and provides insights for future research on speciation, migration, and biodiversity in montane regions.
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