Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America

Autores
Fontana, Sonia L.; Bianchi, Maria Martha; Bennett, K. D.
Año de publicación
2012
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The vast diversity of present vegetation and environments that occur throughout South America (12°N to 56°S) is the result of diverse processes that have been operating and interacting at different spatial and temporal scales. Global factors, such as the concentration of CO2 in the atmosphere, may have been significant for high altitude vegetation during times of lower abundance, while lower sea levels of glacial stages potentially opened areas of continental shelf for colonisation during a substantial portion of the Quaternary. Latitudinal variation in orbital forcing has operated on a regional scale. The pace of climate change in the tropics is dominated by precessional oscillations of c. 20 kyr, while the high latitudes of the south are dominated by obliquity oscillations of c. 40 kyr. In particular, seasonal insolation changes forced by precessional oscillations must have had important consequences for the distribution limits of species, with potentially different effects depending on the latitude. The availability of taxa, altitude and human impact, among other events, have locally influenced the environments. Disentangling the different forcing factors of environmental change that operate on different timescales, and understanding the underlying mechanisms leads to considerable challenges for palaeoecologists. The papers in this Special Issue present a selection of palaeoecological studies throughout South America on vegetation changes and other aspects of the environment, providing a window on the possible complexity of the nature of transitions and timings that are potentially available.
Fil: Fontana, Sonia L.. The Queens University of Belfast; Irlanda
Fil: Bianchi, Maria Martha. Secretaría de Cultura de la Nación. Dirección Nacional de Cultura y Museos. Instituto Nacional de Antropología y Pensamiento Latinoamericano; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Bennett, K. D.. The Queens University of Belfast; Irlanda
Materia
CLIMATE CHANGE
HOLOCENE
PALAEOECOLOGY
QUATERNARY
SOUTH AMERICA
VEGETATION
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:11336/194784

id CONICETDig_8926f66c14faa04e87b1a4da1f841312
oai_identifier_str oai:ri.conicet.gov.ar:11336/194784
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South AmericaFontana, Sonia L.Bianchi, Maria MarthaBennett, K. D.CLIMATE CHANGEHOLOCENEPALAEOECOLOGYQUATERNARYSOUTH AMERICAVEGETATIONhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The vast diversity of present vegetation and environments that occur throughout South America (12°N to 56°S) is the result of diverse processes that have been operating and interacting at different spatial and temporal scales. Global factors, such as the concentration of CO2 in the atmosphere, may have been significant for high altitude vegetation during times of lower abundance, while lower sea levels of glacial stages potentially opened areas of continental shelf for colonisation during a substantial portion of the Quaternary. Latitudinal variation in orbital forcing has operated on a regional scale. The pace of climate change in the tropics is dominated by precessional oscillations of c. 20 kyr, while the high latitudes of the south are dominated by obliquity oscillations of c. 40 kyr. In particular, seasonal insolation changes forced by precessional oscillations must have had important consequences for the distribution limits of species, with potentially different effects depending on the latitude. The availability of taxa, altitude and human impact, among other events, have locally influenced the environments. Disentangling the different forcing factors of environmental change that operate on different timescales, and understanding the underlying mechanisms leads to considerable challenges for palaeoecologists. The papers in this Special Issue present a selection of palaeoecological studies throughout South America on vegetation changes and other aspects of the environment, providing a window on the possible complexity of the nature of transitions and timings that are potentially available.Fil: Fontana, Sonia L.. The Queens University of Belfast; IrlandaFil: Bianchi, Maria Martha. Secretaría de Cultura de la Nación. Dirección Nacional de Cultura y Museos. Instituto Nacional de Antropología y Pensamiento Latinoamericano; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Bennett, K. D.. The Queens University of Belfast; IrlandaSage Publications Ltd2012-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/194784Fontana, Sonia L.; Bianchi, Maria Martha; Bennett, K. D.; Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America; Sage Publications Ltd; Holocene (Seven Oaks); 22; 11; 11-2012; 1203-12060959-6836CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://journals.sagepub.com/doi/10.1177/0959683612451184info:eu-repo/semantics/altIdentifier/doi/10.1177/0959683612451184info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:27:15Zoai:ri.conicet.gov.ar:11336/194784instacron: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 10:27:15.448CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
title Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
spellingShingle Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
Fontana, Sonia L.
CLIMATE CHANGE
HOLOCENE
PALAEOECOLOGY
QUATERNARY
SOUTH AMERICA
VEGETATION
title_short Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
title_full Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
title_fullStr Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
title_full_unstemmed Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
title_sort Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America
dc.creator.none.fl_str_mv Fontana, Sonia L.
Bianchi, Maria Martha
Bennett, K. D.
author Fontana, Sonia L.
author_facet Fontana, Sonia L.
Bianchi, Maria Martha
Bennett, K. D.
author_role author
author2 Bianchi, Maria Martha
Bennett, K. D.
author2_role author
author
dc.subject.none.fl_str_mv CLIMATE CHANGE
HOLOCENE
PALAEOECOLOGY
QUATERNARY
SOUTH AMERICA
VEGETATION
topic CLIMATE CHANGE
HOLOCENE
PALAEOECOLOGY
QUATERNARY
SOUTH AMERICA
VEGETATION
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The vast diversity of present vegetation and environments that occur throughout South America (12°N to 56°S) is the result of diverse processes that have been operating and interacting at different spatial and temporal scales. Global factors, such as the concentration of CO2 in the atmosphere, may have been significant for high altitude vegetation during times of lower abundance, while lower sea levels of glacial stages potentially opened areas of continental shelf for colonisation during a substantial portion of the Quaternary. Latitudinal variation in orbital forcing has operated on a regional scale. The pace of climate change in the tropics is dominated by precessional oscillations of c. 20 kyr, while the high latitudes of the south are dominated by obliquity oscillations of c. 40 kyr. In particular, seasonal insolation changes forced by precessional oscillations must have had important consequences for the distribution limits of species, with potentially different effects depending on the latitude. The availability of taxa, altitude and human impact, among other events, have locally influenced the environments. Disentangling the different forcing factors of environmental change that operate on different timescales, and understanding the underlying mechanisms leads to considerable challenges for palaeoecologists. The papers in this Special Issue present a selection of palaeoecological studies throughout South America on vegetation changes and other aspects of the environment, providing a window on the possible complexity of the nature of transitions and timings that are potentially available.
Fil: Fontana, Sonia L.. The Queens University of Belfast; Irlanda
Fil: Bianchi, Maria Martha. Secretaría de Cultura de la Nación. Dirección Nacional de Cultura y Museos. Instituto Nacional de Antropología y Pensamiento Latinoamericano; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Bennett, K. D.. The Queens University of Belfast; Irlanda
description The vast diversity of present vegetation and environments that occur throughout South America (12°N to 56°S) is the result of diverse processes that have been operating and interacting at different spatial and temporal scales. Global factors, such as the concentration of CO2 in the atmosphere, may have been significant for high altitude vegetation during times of lower abundance, while lower sea levels of glacial stages potentially opened areas of continental shelf for colonisation during a substantial portion of the Quaternary. Latitudinal variation in orbital forcing has operated on a regional scale. The pace of climate change in the tropics is dominated by precessional oscillations of c. 20 kyr, while the high latitudes of the south are dominated by obliquity oscillations of c. 40 kyr. In particular, seasonal insolation changes forced by precessional oscillations must have had important consequences for the distribution limits of species, with potentially different effects depending on the latitude. The availability of taxa, altitude and human impact, among other events, have locally influenced the environments. Disentangling the different forcing factors of environmental change that operate on different timescales, and understanding the underlying mechanisms leads to considerable challenges for palaeoecologists. The papers in this Special Issue present a selection of palaeoecological studies throughout South America on vegetation changes and other aspects of the environment, providing a window on the possible complexity of the nature of transitions and timings that are potentially available.
publishDate 2012
dc.date.none.fl_str_mv 2012-11
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/194784
Fontana, Sonia L.; Bianchi, Maria Martha; Bennett, K. D.; Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America; Sage Publications Ltd; Holocene (Seven Oaks); 22; 11; 11-2012; 1203-1206
0959-6836
CONICET Digital
CONICET
url http://hdl.handle.net/11336/194784
identifier_str_mv Fontana, Sonia L.; Bianchi, Maria Martha; Bennett, K. D.; Palaeoenvironmental changes since the Last Glacial Maximum: patterns, timing and dynamics throughout South America; Sage Publications Ltd; Holocene (Seven Oaks); 22; 11; 11-2012; 1203-1206
0959-6836
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://journals.sagepub.com/doi/10.1177/0959683612451184
info:eu-repo/semantics/altIdentifier/doi/10.1177/0959683612451184
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Sage Publications Ltd
publisher.none.fl_str_mv Sage Publications Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1844614274927820800
score 13.070432