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Shared-role of vegetation types, elevation and soil affecting plant diversity in an old-tropical mountain hotspot

dc.contributor.authorLoiola, Priscilla P. [UNESP]
dc.contributor.authorMorellato, Leonor Patrícia Cerdeira [UNESP]
dc.contributor.authorCamargo, Maria Gabriela Gutierrez [UNESP]
dc.contributor.authorKamimura, Vitor A. [UNESP]
dc.contributor.authorMattos, Jacqueline S. [UNESP]
dc.contributor.authorStreher, Annia Susin [UNESP]
dc.contributor.authorLe Stradic, Soizig [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionInstituto Tecnológico Vale (ITV)
dc.contributor.institutionUniversidade Estadual de Campinas (UNICAMP)
dc.contributor.institutionNational Institute for Space Research (INPE)
dc.contributor.institutionUMR 1202 INRAE/Univ Bordeaux–BIOGECO
dc.date.accessioned2025-04-29T20:02:00Z
dc.date.issued2023-07-01
dc.description.abstractDespite the exceptional species richness and endemism, the environmental drivers of plant diversity along old tropical mountains remain under-explored. The respective importance of vegetation types, elevation, slope, and soil to drive diversity across life-forms is poorly addressed. Here, we tested whether environmental variables drove local and regional plant diversity along an old tropical mountain according to the three main life-forms: graminoids, herbaceous and woody species. We sampled all Angiosperm species on 180 plots across five elevations, at the tropical old-mountain region of Serra do Cipó, South-eastern Brazil. We assessed soil, slope, and vegetation types, and calculated richness and beta-diversity, applying generalized least square models, linear mixed-models and partial Mantel tests to test for relationships. Richness of graminoids and herbaceous species increased with greater elevation and more nutrient-impoverished soils, while woody richness showed the inverse pattern. Beta-diversity was primarily driven by species turnover, correlated with elevation and soil and higher in less dominant vegetation types, with unique species. Despite the limited elevational range in these old mountains, it still played an important role in filtering woody species, while fostering graminoid and herbaceous species. Conservation and restoration actions need to foster the high regional diversity supported by the old mountain heterogeneous landscape and the diversity of life-forms, especially the dominant and highly diverse grassy component.en
dc.description.affiliationDepartment of Biodiversity Laboratory of Phenology São Paulo State University (UNESP), Av 24A 1515, São Paulo
dc.description.affiliationInstituto Tecnológico Vale (ITV), R. Boaventura da Silva, 955
dc.description.affiliationLaboratory of Evolutionary Ecology and Plant Genomics Department of Plant Biology Institute of Biology University of Campinas
dc.description.affiliationEarth Observation and Geoinformatics Division National Institute for Space Research (INPE)
dc.description.affiliationFrench National Institute for Agriculture Food and Environment (INRAE) UMR 1202 INRAE/Univ Bordeaux–BIOGECO
dc.description.affiliationUnespDepartment of Biodiversity Laboratory of Phenology São Paulo State University (UNESP), Av 24A 1515, São Paulo
dc.format.extent1842-1853
dc.identifierhttp://dx.doi.org/10.1007/s11629-022-7838-z
dc.identifier.citationJournal of Mountain Science, v. 20, n. 7, p. 1842-1853, 2023.
dc.identifier.doi10.1007/s11629-022-7838-z
dc.identifier.issn1993-0321
dc.identifier.issn1672-6316
dc.identifier.scopus2-s2.0-85165667711
dc.identifier.urihttps://hdl.handle.net/11449/305099
dc.language.isoeng
dc.relation.ispartofJournal of Mountain Science
dc.sourceScopus
dc.subjectBeta-diversity
dc.subjectCampos rupestres
dc.subjectCerrado
dc.subjectGrassland
dc.subjectHerbaceous
dc.subjectSpecies turnover
dc.titleShared-role of vegetation types, elevation and soil affecting plant diversity in an old-tropical mountain hotspoten
dc.typeArtigopt
dspace.entity.typePublication
unesp.author.orcid0000-0001-8760-2618[1]
unesp.author.orcid0000-0001-5265-8988[2]
unesp.author.orcid0000-0002-3536-6542[3]
unesp.author.orcid0000-0002-3276-5812[4]
unesp.author.orcid0000-0003-3104-0884[5]
unesp.author.orcid0000-0002-9276-7289[6]
unesp.author.orcid0000-0003-2643-3544[7]

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