Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds

ABSTRACT:The forest–savanna transition is the most widespread ecotone in the tropics, with important eco- logical, climatic, and biogeochemical implications at local to global scales. However, the factors and mechanisms that control this transition vary among continents and regions. Here, we analyze...

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Autores:
Valencia Cárdenas, Santiago
Salazar Villegas, Juan Fernando
Hoyos, Natalia
Armenteras, Dolors
Villegas Palacio, Juan Camilo
Tipo de recurso:
Article of investigation
Fecha de publicación:
2023
Institución:
Universidad de Antioquia
Repositorio:
Repositorio UdeA
Idioma:
eng
OAI Identifier:
oai:bibliotecadigital.udea.edu.co:10495/36572
Acceso en línea:
https://hdl.handle.net/10495/36572
Palabra clave:
Selva lluviosa
Rain forests
Bosques
Forest
Frecuencia de incendios
Fire frequency
Ecorregión de los Llanos
Humid tropical forest
Llanos ecoregion
Intra-seasonal precipitation
Precipitación intraestacional
http://aims.fao.org/aos/agrovoc/c_3062
http://aims.fao.org/aos/agrovoc/c_e750a3e5
Rights
openAccess
License
https://creativecommons.org/licenses/by/4.0/
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oai_identifier_str oai:bibliotecadigital.udea.edu.co:10495/36572
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repository_id_str
dc.title.spa.fl_str_mv Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
title Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
spellingShingle Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
Selva lluviosa
Rain forests
Bosques
Forest
Frecuencia de incendios
Fire frequency
Ecorregión de los Llanos
Humid tropical forest
Llanos ecoregion
Intra-seasonal precipitation
Precipitación intraestacional
http://aims.fao.org/aos/agrovoc/c_3062
http://aims.fao.org/aos/agrovoc/c_e750a3e5
title_short Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
title_full Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
title_fullStr Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
title_full_unstemmed Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
title_sort Current forest–savanna transition in Northern South America departs from Typical Climatic Thresholds
dc.creator.fl_str_mv Valencia Cárdenas, Santiago
Salazar Villegas, Juan Fernando
Hoyos, Natalia
Armenteras, Dolors
Villegas Palacio, Juan Camilo
dc.contributor.author.none.fl_str_mv Valencia Cárdenas, Santiago
Salazar Villegas, Juan Fernando
Hoyos, Natalia
Armenteras, Dolors
Villegas Palacio, Juan Camilo
dc.contributor.researchgroup.spa.fl_str_mv Grupo de Ingeniería y Gestión Ambiental (GIGA)
dc.subject.lemb.none.fl_str_mv Selva lluviosa
Rain forests
topic Selva lluviosa
Rain forests
Bosques
Forest
Frecuencia de incendios
Fire frequency
Ecorregión de los Llanos
Humid tropical forest
Llanos ecoregion
Intra-seasonal precipitation
Precipitación intraestacional
http://aims.fao.org/aos/agrovoc/c_3062
http://aims.fao.org/aos/agrovoc/c_e750a3e5
dc.subject.agrovoc.none.fl_str_mv Bosques
Forest
Frecuencia de incendios
Fire frequency
dc.subject.proposal.spa.fl_str_mv Ecorregión de los Llanos
Humid tropical forest
Llanos ecoregion
Intra-seasonal precipitation
Precipitación intraestacional
dc.subject.agrovocuri.none.fl_str_mv http://aims.fao.org/aos/agrovoc/c_3062
http://aims.fao.org/aos/agrovoc/c_e750a3e5
description ABSTRACT:The forest–savanna transition is the most widespread ecotone in the tropics, with important eco- logical, climatic, and biogeochemical implications at local to global scales. However, the factors and mechanisms that control this transition vary among continents and regions. Here, we analyzed which factors best explain the transition in northern South America (Llanos ecoregion and north- western Amazon), where common thresholds on typical environmental factors (for example, mean annual precipitation (MAP), wet season precipitation) fail to predict it. For instance, savannas in the Llanos occur at MAP levels (> 1500 mm) which are typical of forests in other tropical regions. We examined the transition’s climate features, soils, and disturbance (fire frequency) spaces using re- motely sensed data. We used logistic generalized linear models to assess the effect of seasonal (sea- son length) and intra-seasonal (daily precipitation frequency and intensity) precipitation metrics during the dry season, soil silt content, and fire frequency, on the transition using canopy cover, tree cover, and the maximum Plant Area Volume Density as vegetation structure descriptor variables. Fire frequency and precipitation frequency were the most important variables explaining the transition. Although most fires occur in savannas, we found that a significant percentage of savanna pixels (46%) had no fires. This study indicates that the transition should be characterized regionally in response to biogeographic differences (for example, climatic space) among regions and continents. Our results highlight the importance of fire frequency and intra-seasonal precipitation in determining the transition in northern South America. Further- more, future studies should consider regional differences in the climatic space of forest and savanna to improve projections of global change impacts on these highly diverse ecosystems.
publishDate 2023
dc.date.accessioned.none.fl_str_mv 2023-09-06T16:07:21Z
dc.date.available.none.fl_str_mv 2023-09-06T16:07:21Z
dc.date.issued.none.fl_str_mv 2023
dc.type.spa.fl_str_mv Artículo de investigación
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dc.identifier.citation.spa.fl_str_mv Valencia, S., Salazar, J.F., Hoyos, N. et al. Current Forest–Savanna Transition in Northern South America Departs from Typical Climatic Thresholds. Ecosystems (2023). https://doi.org/10.1007/s10021-023-00872-y
dc.identifier.issn.none.fl_str_mv 1432-9840
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/10495/36572
dc.identifier.doi.none.fl_str_mv 10.1007/s10021-023-00872-y
dc.identifier.eissn.none.fl_str_mv 1435-0629
identifier_str_mv Valencia, S., Salazar, J.F., Hoyos, N. et al. Current Forest–Savanna Transition in Northern South America Departs from Typical Climatic Thresholds. Ecosystems (2023). https://doi.org/10.1007/s10021-023-00872-y
1432-9840
10.1007/s10021-023-00872-y
1435-0629
url https://hdl.handle.net/10495/36572
dc.language.iso.spa.fl_str_mv eng
language eng
dc.relation.ispartofjournalabbrev.spa.fl_str_mv Ecosystems
dc.relation.citationendpage.spa.fl_str_mv 16
dc.relation.citationstartpage.spa.fl_str_mv 1
dc.relation.citationvolume.spa.fl_str_mv 2023
dc.relation.ispartofjournal.spa.fl_str_mv Ecosystems
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spelling Valencia Cárdenas, SantiagoSalazar Villegas, Juan FernandoHoyos, NataliaArmenteras, DolorsVillegas Palacio, Juan CamiloGrupo de Ingeniería y Gestión Ambiental (GIGA)2023-09-06T16:07:21Z2023-09-06T16:07:21Z2023Valencia, S., Salazar, J.F., Hoyos, N. et al. Current Forest–Savanna Transition in Northern South America Departs from Typical Climatic Thresholds. Ecosystems (2023). https://doi.org/10.1007/s10021-023-00872-y1432-9840https://hdl.handle.net/10495/3657210.1007/s10021-023-00872-y1435-0629ABSTRACT:The forest–savanna transition is the most widespread ecotone in the tropics, with important eco- logical, climatic, and biogeochemical implications at local to global scales. However, the factors and mechanisms that control this transition vary among continents and regions. Here, we analyzed which factors best explain the transition in northern South America (Llanos ecoregion and north- western Amazon), where common thresholds on typical environmental factors (for example, mean annual precipitation (MAP), wet season precipitation) fail to predict it. For instance, savannas in the Llanos occur at MAP levels (> 1500 mm) which are typical of forests in other tropical regions. We examined the transition’s climate features, soils, and disturbance (fire frequency) spaces using re- motely sensed data. We used logistic generalized linear models to assess the effect of seasonal (sea- son length) and intra-seasonal (daily precipitation frequency and intensity) precipitation metrics during the dry season, soil silt content, and fire frequency, on the transition using canopy cover, tree cover, and the maximum Plant Area Volume Density as vegetation structure descriptor variables. Fire frequency and precipitation frequency were the most important variables explaining the transition. Although most fires occur in savannas, we found that a significant percentage of savanna pixels (46%) had no fires. This study indicates that the transition should be characterized regionally in response to biogeographic differences (for example, climatic space) among regions and continents. Our results highlight the importance of fire frequency and intra-seasonal precipitation in determining the transition in northern South America. Further- more, future studies should consider regional differences in the climatic space of forest and savanna to improve projections of global change impacts on these highly diverse ecosystems.COL000861916application/pdfengSpringerNueva York, Estados Unidoshttps://creativecommons.org/licenses/by/4.0/http://creativecommons.org/licenses/by/2.5/co/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Current forest–savanna transition in Northern South America departs from Typical Climatic ThresholdsArtículo de investigaciónhttp://purl.org/coar/resource_type/c_2df8fbb1https://purl.org/redcol/resource_type/ARThttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionSelva lluviosaRain forestsBosquesForestFrecuencia de incendiosFire frequencyEcorregión de los LlanosHumid tropical forestLlanos ecoregionIntra-seasonal precipitationPrecipitación intraestacionalhttp://aims.fao.org/aos/agrovoc/c_3062http://aims.fao.org/aos/agrovoc/c_e750a3e5Ecosystems1612023EcosystemsPublicationORIGINALValenciaSantiago_2023_CurrentForestSavanna.pdfValenciaSantiago_2023_CurrentForestSavanna.pdfArtículo de investigaciónapplication/pdf2342347https://bibliotecadigital.udea.edu.co/bitstreams/640d2d26-2374-4c3d-9332-cc6ff9faa5c7/download725b00f343ec30b66060e7fbb92d4591MD51trueAnonymousREADLICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://bibliotecadigital.udea.edu.co/bitstreams/e9da8eee-10d9-4a44-92fc-3953827a4aad/download8a4605be74aa9ea9d79846c1fba20a33MD53falseAnonymousREADCC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8927https://bibliotecadigital.udea.edu.co/bitstreams/bc1f3a97-fc0c-4622-95b4-36173ed2721b/download1646d1f6b96dbbbc38035efc9239ac9cMD52falseAnonymousREADTEXTValenciaSantiago_2023_CurrentForestSavanna.pdf.txtValenciaSantiago_2023_CurrentForestSavanna.pdf.txtExtracted texttext/plain74334https://bibliotecadigital.udea.edu.co/bitstreams/43a2b2a8-6fd8-4d3b-86b3-feb3d74ad749/download7a7863dd69b8a1692883e8dd075e2553MD54falseAnonymousREADTHUMBNAILValenciaSantiago_2023_CurrentForestSavanna.pdf.jpgValenciaSantiago_2023_CurrentForestSavanna.pdf.jpgGenerated Thumbnailimage/jpeg15260https://bibliotecadigital.udea.edu.co/bitstreams/1c259bf5-15a6-499f-b967-bdeee77fc63d/download98a54e42ed12484d1695651526b020d4MD55falseAnonymousREAD10495/36572oai:bibliotecadigital.udea.edu.co:10495/365722025-03-27 01:35:44.418https://creativecommons.org/licenses/by/4.0/open.accesshttps://bibliotecadigital.udea.edu.coRepositorio Institucional de la Universidad de Antioquiaaplicacionbibliotecadigitalbiblioteca@udea.edu.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