Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)

Autores
Nanavati, William; Whitlock, Cathy; Outes, Ana Valeria; Villarosa, Gustavo; Iglesias, Virginia; de Porras, Maria Eugenia
Año de publicación
2019
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
Disentangling anthropogenic and natural drivers of vegetation and fire history at different spatiotemporal scales is a fundamental challenge in Earth Systems science. In the forest-steppe ecotone of southern South America, fire and climate have shaped the position of lower treeline, but the influence of pre-European peoples at the ecotone is less clear. A new 10,800-year history of climate, vegetation, fire, and land use from Laguna Portezuelo (38°S, 71°W, 1730 m elev.), east of the Andes, provides information on pre-European anthropogenic fires in Araucaria forest. Araucaria was an important resource for pre-Europeans and is ingrained into Mapuche-Pehuenche cultural identity. The pollen record shows that Araucaria expanded in the late Holocene with rising human populations and strengthened ENSO. Prior to that, the forest-steppe region supported scattered Nothofagus (mostly N. dombeyi-type pollen) and moderate-to-high fire activity. Beginning at 6800 cal yr BP, changes in ecotone composition and fire are attributed to increased climate variability and human presence. Increased Nothofagus and Araucaria pollen and null-to-low fire activity occurred at 1800, 1200, and 800 cal yr BP, in association with increased strength and frequency of wet El Niño events. After 500 cal yr BP, increased abundance of Plantago, Rumex, and other disturbance taxa (e.g., Apiaceae and Caryophyllaceae) and high fire activity mark Euro-American land use. Non-native Pinus pollen in the 20th century indicate the establishment of Pinus plantations near Laguna Portezuelo.Although archaeological investigations suggest that people lived in southern South America east of the Andes since ca. 12,000 cal yr BP, the vegetation and fire history for most of the postglacial period was governed by the strength and position of the SWW storm tracks. From the late-glacial to early Holocene, region-wide increases in fire were associated with aridity while the SWW were weakened and south of their present position. Between 7000-4000 cal yr BP, increased arboreal taxa and decreased fire throughout Patagonia suggest effectively wet conditions, as the SWW moved northward to their present position. After 4000 cal yr BP, a combination of rising human population and greater climate variability, led to spatially heterogeneous but generally rising fire activity along the forest-steppe ecotone. Throughout Patagonia, wet El Niño and/or negative Southern Annual Mode (SAM) events increased biomass, but made the landscape less flammable and reduced anthropogenic burning. Transitions from wet El Niño and/or negative SAM to dry La Niña and/or positive SAM events increased burnable biomass, amplifying anthropogenic burning. During the last 100 years, increased Euro-American settlement and land clearance led to forest loss, more disturbance, and the spread of introduced taxa along the eastern flanks of the Andes. The ecological changes in recent decades far outweigh thousands of years of pre-European human influence on fire and vegetation history.
Fil: Nanavati, William. State University Of Montana. Department Of Earth Sciences; Estados Unidos
Fil: Whitlock, Cathy. State University Of Montana. Department Of Earth Sciences; Estados Unidos
Fil: Outes, Ana Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina
Fil: Villarosa, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina
Fil: Iglesias, Virginia. State University of Colorado at Boulder; Estados Unidos
Fil: de Porras, Maria Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
20th Congress of the International Union for Quaternary Research
Dublin
Irlanda
International Union for Quaternary Research
Materia
PATAGONIA
FOREST-STEPPE ECOTONE
ANTRHOPIC DRIVERS
PALEOCLIMATE
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/271960

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network_name_str CONICET Digital (CONICET)
spelling Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)Nanavati, WilliamWhitlock, CathyOutes, Ana ValeriaVillarosa, GustavoIglesias, Virginiade Porras, Maria EugeniaPATAGONIAFOREST-STEPPE ECOTONEANTRHOPIC DRIVERSPALEOCLIMATEhttps://purl.org/becyt/ford/1.7https://purl.org/becyt/ford/1Disentangling anthropogenic and natural drivers of vegetation and fire history at different spatiotemporal scales is a fundamental challenge in Earth Systems science. In the forest-steppe ecotone of southern South America, fire and climate have shaped the position of lower treeline, but the influence of pre-European peoples at the ecotone is less clear. A new 10,800-year history of climate, vegetation, fire, and land use from Laguna Portezuelo (38°S, 71°W, 1730 m elev.), east of the Andes, provides information on pre-European anthropogenic fires in Araucaria forest. Araucaria was an important resource for pre-Europeans and is ingrained into Mapuche-Pehuenche cultural identity. The pollen record shows that Araucaria expanded in the late Holocene with rising human populations and strengthened ENSO. Prior to that, the forest-steppe region supported scattered Nothofagus (mostly N. dombeyi-type pollen) and moderate-to-high fire activity. Beginning at 6800 cal yr BP, changes in ecotone composition and fire are attributed to increased climate variability and human presence. Increased Nothofagus and Araucaria pollen and null-to-low fire activity occurred at 1800, 1200, and 800 cal yr BP, in association with increased strength and frequency of wet El Niño events. After 500 cal yr BP, increased abundance of Plantago, Rumex, and other disturbance taxa (e.g., Apiaceae and Caryophyllaceae) and high fire activity mark Euro-American land use. Non-native Pinus pollen in the 20th century indicate the establishment of Pinus plantations near Laguna Portezuelo.Although archaeological investigations suggest that people lived in southern South America east of the Andes since ca. 12,000 cal yr BP, the vegetation and fire history for most of the postglacial period was governed by the strength and position of the SWW storm tracks. From the late-glacial to early Holocene, region-wide increases in fire were associated with aridity while the SWW were weakened and south of their present position. Between 7000-4000 cal yr BP, increased arboreal taxa and decreased fire throughout Patagonia suggest effectively wet conditions, as the SWW moved northward to their present position. After 4000 cal yr BP, a combination of rising human population and greater climate variability, led to spatially heterogeneous but generally rising fire activity along the forest-steppe ecotone. Throughout Patagonia, wet El Niño and/or negative Southern Annual Mode (SAM) events increased biomass, but made the landscape less flammable and reduced anthropogenic burning. Transitions from wet El Niño and/or negative SAM to dry La Niña and/or positive SAM events increased burnable biomass, amplifying anthropogenic burning. During the last 100 years, increased Euro-American settlement and land clearance led to forest loss, more disturbance, and the spread of introduced taxa along the eastern flanks of the Andes. The ecological changes in recent decades far outweigh thousands of years of pre-European human influence on fire and vegetation history.Fil: Nanavati, William. State University Of Montana. Department Of Earth Sciences; Estados UnidosFil: Whitlock, Cathy. State University Of Montana. Department Of Earth Sciences; Estados UnidosFil: Outes, Ana Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; ArgentinaFil: Villarosa, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; ArgentinaFil: Iglesias, Virginia. State University of Colorado at Boulder; Estados UnidosFil: de Porras, Maria Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina20th Congress of the International Union for Quaternary ResearchDublinIrlandaInternational Union for Quaternary ResearchInternational Union for Quaternary Research2019info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/271960Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S); 20th Congress of the International Union for Quaternary Research; Dublin; Irlanda; 2019; 2519-2519CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://iqua.ie/wp-content/uploads/2020/02/INQUA-2019-Abstract-book.pdfInternacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:21:39Zoai:ri.conicet.gov.ar:11336/271960instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:21:39.317CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
title Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
spellingShingle Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
Nanavati, William
PATAGONIA
FOREST-STEPPE ECOTONE
ANTRHOPIC DRIVERS
PALEOCLIMATE
title_short Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
title_full Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
title_fullStr Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
title_full_unstemmed Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
title_sort Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S)
dc.creator.none.fl_str_mv Nanavati, William
Whitlock, Cathy
Outes, Ana Valeria
Villarosa, Gustavo
Iglesias, Virginia
de Porras, Maria Eugenia
author Nanavati, William
author_facet Nanavati, William
Whitlock, Cathy
Outes, Ana Valeria
Villarosa, Gustavo
Iglesias, Virginia
de Porras, Maria Eugenia
author_role author
author2 Whitlock, Cathy
Outes, Ana Valeria
Villarosa, Gustavo
Iglesias, Virginia
de Porras, Maria Eugenia
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv PATAGONIA
FOREST-STEPPE ECOTONE
ANTRHOPIC DRIVERS
PALEOCLIMATE
topic PATAGONIA
FOREST-STEPPE ECOTONE
ANTRHOPIC DRIVERS
PALEOCLIMATE
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.7
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Disentangling anthropogenic and natural drivers of vegetation and fire history at different spatiotemporal scales is a fundamental challenge in Earth Systems science. In the forest-steppe ecotone of southern South America, fire and climate have shaped the position of lower treeline, but the influence of pre-European peoples at the ecotone is less clear. A new 10,800-year history of climate, vegetation, fire, and land use from Laguna Portezuelo (38°S, 71°W, 1730 m elev.), east of the Andes, provides information on pre-European anthropogenic fires in Araucaria forest. Araucaria was an important resource for pre-Europeans and is ingrained into Mapuche-Pehuenche cultural identity. The pollen record shows that Araucaria expanded in the late Holocene with rising human populations and strengthened ENSO. Prior to that, the forest-steppe region supported scattered Nothofagus (mostly N. dombeyi-type pollen) and moderate-to-high fire activity. Beginning at 6800 cal yr BP, changes in ecotone composition and fire are attributed to increased climate variability and human presence. Increased Nothofagus and Araucaria pollen and null-to-low fire activity occurred at 1800, 1200, and 800 cal yr BP, in association with increased strength and frequency of wet El Niño events. After 500 cal yr BP, increased abundance of Plantago, Rumex, and other disturbance taxa (e.g., Apiaceae and Caryophyllaceae) and high fire activity mark Euro-American land use. Non-native Pinus pollen in the 20th century indicate the establishment of Pinus plantations near Laguna Portezuelo.Although archaeological investigations suggest that people lived in southern South America east of the Andes since ca. 12,000 cal yr BP, the vegetation and fire history for most of the postglacial period was governed by the strength and position of the SWW storm tracks. From the late-glacial to early Holocene, region-wide increases in fire were associated with aridity while the SWW were weakened and south of their present position. Between 7000-4000 cal yr BP, increased arboreal taxa and decreased fire throughout Patagonia suggest effectively wet conditions, as the SWW moved northward to their present position. After 4000 cal yr BP, a combination of rising human population and greater climate variability, led to spatially heterogeneous but generally rising fire activity along the forest-steppe ecotone. Throughout Patagonia, wet El Niño and/or negative Southern Annual Mode (SAM) events increased biomass, but made the landscape less flammable and reduced anthropogenic burning. Transitions from wet El Niño and/or negative SAM to dry La Niña and/or positive SAM events increased burnable biomass, amplifying anthropogenic burning. During the last 100 years, increased Euro-American settlement and land clearance led to forest loss, more disturbance, and the spread of introduced taxa along the eastern flanks of the Andes. The ecological changes in recent decades far outweigh thousands of years of pre-European human influence on fire and vegetation history.
Fil: Nanavati, William. State University Of Montana. Department Of Earth Sciences; Estados Unidos
Fil: Whitlock, Cathy. State University Of Montana. Department Of Earth Sciences; Estados Unidos
Fil: Outes, Ana Valeria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina
Fil: Villarosa, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Biodiversidad y Medioambiente. Universidad Nacional del Comahue. Centro Regional Universidad Bariloche. Instituto de Investigaciones en Biodiversidad y Medioambiente; Argentina
Fil: Iglesias, Virginia. State University of Colorado at Boulder; Estados Unidos
Fil: de Porras, Maria Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
20th Congress of the International Union for Quaternary Research
Dublin
Irlanda
International Union for Quaternary Research
description Disentangling anthropogenic and natural drivers of vegetation and fire history at different spatiotemporal scales is a fundamental challenge in Earth Systems science. In the forest-steppe ecotone of southern South America, fire and climate have shaped the position of lower treeline, but the influence of pre-European peoples at the ecotone is less clear. A new 10,800-year history of climate, vegetation, fire, and land use from Laguna Portezuelo (38°S, 71°W, 1730 m elev.), east of the Andes, provides information on pre-European anthropogenic fires in Araucaria forest. Araucaria was an important resource for pre-Europeans and is ingrained into Mapuche-Pehuenche cultural identity. The pollen record shows that Araucaria expanded in the late Holocene with rising human populations and strengthened ENSO. Prior to that, the forest-steppe region supported scattered Nothofagus (mostly N. dombeyi-type pollen) and moderate-to-high fire activity. Beginning at 6800 cal yr BP, changes in ecotone composition and fire are attributed to increased climate variability and human presence. Increased Nothofagus and Araucaria pollen and null-to-low fire activity occurred at 1800, 1200, and 800 cal yr BP, in association with increased strength and frequency of wet El Niño events. After 500 cal yr BP, increased abundance of Plantago, Rumex, and other disturbance taxa (e.g., Apiaceae and Caryophyllaceae) and high fire activity mark Euro-American land use. Non-native Pinus pollen in the 20th century indicate the establishment of Pinus plantations near Laguna Portezuelo.Although archaeological investigations suggest that people lived in southern South America east of the Andes since ca. 12,000 cal yr BP, the vegetation and fire history for most of the postglacial period was governed by the strength and position of the SWW storm tracks. From the late-glacial to early Holocene, region-wide increases in fire were associated with aridity while the SWW were weakened and south of their present position. Between 7000-4000 cal yr BP, increased arboreal taxa and decreased fire throughout Patagonia suggest effectively wet conditions, as the SWW moved northward to their present position. After 4000 cal yr BP, a combination of rising human population and greater climate variability, led to spatially heterogeneous but generally rising fire activity along the forest-steppe ecotone. Throughout Patagonia, wet El Niño and/or negative Southern Annual Mode (SAM) events increased biomass, but made the landscape less flammable and reduced anthropogenic burning. Transitions from wet El Niño and/or negative SAM to dry La Niña and/or positive SAM events increased burnable biomass, amplifying anthropogenic burning. During the last 100 years, increased Euro-American settlement and land clearance led to forest loss, more disturbance, and the spread of introduced taxa along the eastern flanks of the Andes. The ecological changes in recent decades far outweigh thousands of years of pre-European human influence on fire and vegetation history.
publishDate 2019
dc.date.none.fl_str_mv 2019
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format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/271960
Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S); 20th Congress of the International Union for Quaternary Research; Dublin; Irlanda; 2019; 2519-2519
CONICET Digital
CONICET
url http://hdl.handle.net/11336/271960
identifier_str_mv Anthropogenic and natural drivers of vegetation and fire history along the forest-steppe border of the eastern Andes (38-50°S); 20th Congress of the International Union for Quaternary Research; Dublin; Irlanda; 2019; 2519-2519
CONICET Digital
CONICET
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