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Defaunation impacts on the carbon balance of tropical forests

dc.contributor.authorBrodie, Jedediah F.
dc.contributor.authorBello, Carolina
dc.contributor.authorEmer, Carine
dc.contributor.authorGaletti, Mauro [UNESP]
dc.contributor.authorLuskin, Matthew S.
dc.contributor.authorOsuri, Anand
dc.contributor.authorPeres, Carlos A.
dc.contributor.authorStoll, Annina
dc.contributor.authorVillar, Nacho
dc.contributor.authorLópez, Ana-Benítez
dc.contributor.institutionUniversity of Montana
dc.contributor.institutionUniversiti Malaysia Sarawak
dc.contributor.institutionETH
dc.contributor.institutionRio de Janeiro Botanical Garden Research Institute
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionFlorida International University (FIU)
dc.contributor.institutionUniversity of Queensland
dc.contributor.institutionNature Conservation Foundation
dc.contributor.institutionUniversity of East Anglia
dc.contributor.institutionNetherlands Institute of Ecology NIOO-KNAW
dc.contributor.institutionMuseo Nacional de Ciencias Naturales (MNCN-CSIC)
dc.date.accessioned2025-04-29T20:14:37Z
dc.date.issued2025-02-01
dc.description.abstractThe urgent need to mitigate and adapt to climate change necessitates a comprehensive understanding of carbon cycling dynamics. Traditionally, global carbon cycle models have focused on vegetation, but recent research suggests that animals can play a significant role in carbon dynamics under some circumstances, potentially enhancing the effectiveness of nature-based solutions to mitigate climate change. However, links between animals, plants, and carbon remain unclear. We explored the complex interactions between defaunation and ecosystem carbon in Earth's most biodiverse and carbon-rich biome, tropical rainforests. Defaunation can change patterns of seed dispersal, granivory, and herbivory in ways that alter tree species composition and, therefore, forest carbon above- and belowground. Most studies we reviewed show that defaunation reduces carbon storage 0−26% in the Neo- and Afrotropics, primarily via population declines in large-seeded, animal-dispersed trees. However, Asian forests are not predicted to experience changes because their high-carbon trees are wind dispersed. Extrapolating these local effects to entire ecosystems implies losses of ∼1.6 Pg CO2 equivalent across the Brazilian Atlantic Forest and 4−9.2 Pg across the Amazon over 100 years and of ∼14.7−26.3 Pg across the Congo basin over 250 years. In addition to being hard to quantify with precision, the effects of defaunation on ecosystem carbon are highly context dependent; outcomes varied based on the balance between antagonist and mutualist species interactions, abiotic conditions, human pressure, and numerous other factors. A combination of experiments, large-scale comparative studies, and mechanistic models could help disentangle the effects of defaunation from other anthropogenic forces in the face of the incredible complexity of tropical forest systems. Overall, our synthesis emphasizes the importance of—and inconsistent results when—integrating animal dynamics into carbon cycle models, which is crucial for developing climate change mitigation strategies and effective policies.en
dc.description.affiliationDivision of Biological Sciences and Wildlife Biology Program University of Montana
dc.description.affiliationInstitute for Biodiversity and Environmental Conservation Universiti Malaysia Sarawak
dc.description.affiliationDepartment of Environmental Systems Science ETH
dc.description.affiliationRio de Janeiro Botanical Garden Research Institute
dc.description.affiliationDepartment of Biodiversity Center for Biodiversity Dynamics and Climate Change São Paulo State University (UNESP)
dc.description.affiliationKimberly Green Latin American and Caribbean Center (LACC) Florida International University (FIU)
dc.description.affiliationSchool of the Environment University of Queensland
dc.description.affiliationCentre for Biodiversity and Conservation Science University of Queensland
dc.description.affiliationNature Conservation Foundation
dc.description.affiliationSchool of Environmental Sciences University of East Anglia
dc.description.affiliationNetherlands Institute of Ecology NIOO-KNAW
dc.description.affiliationDepartment of Biogeography and Global Change Museo Nacional de Ciencias Naturales (MNCN-CSIC)
dc.description.affiliationUnespDepartment of Biodiversity Center for Biodiversity Dynamics and Climate Change São Paulo State University (UNESP)
dc.identifierhttp://dx.doi.org/10.1111/cobi.14414
dc.identifier.citationConservation Biology, v. 39, n. 1, 2025.
dc.identifier.doi10.1111/cobi.14414
dc.identifier.issn1523-1739
dc.identifier.issn0888-8892
dc.identifier.scopus2-s2.0-85207951712
dc.identifier.urihttps://hdl.handle.net/11449/309193
dc.language.isoeng
dc.relation.ispartofConservation Biology
dc.sourceScopus
dc.subjectadaptación
dc.subjectadaptation
dc.subjectanimación del ciclo del carbono
dc.subjectanimating the carbon cycle
dc.subjectbiomasa
dc.subjectbiomass
dc.subjectcaza
dc.subjectclimate change mitigation
dc.subjectexploitation
dc.subjectexplotación
dc.subjecthunting
dc.subjectmitigación del cambio climático
dc.subjectsustainability
dc.subjectsustentabilidad
dc.subjectzoogeochemistry
dc.subjectzoogeoquímica
dc.titleDefaunation impacts on the carbon balance of tropical forestsen
dc.typeResenhapt
dspace.entity.typePublication
unesp.author.orcid0000-0002-8298-9021[1]
unesp.author.orcid0000-0001-6351-4998[2]
unesp.author.orcid0000-0002-8187-8696[4]
unesp.author.orcid0000-0002-5236-7096[5]
unesp.author.orcid0000-0003-3609-4080[9]
unesp.author.orcid0000-0002-6432-1837[10]

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