Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile

Autores
Bujalesky, Gustavo Gabriel; Gonzalez Bonorino, Gustavo; Abascal, Liliana
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Holocene coastal environments in the Tierra del Fuego archipelago in southernmost South America evolved in a temperate cold climate characterized by strong and persistent mid-latitude westerly winds, and under stable to falling relative sea level. Southern and western coasts are rocky, microtidal, and generally devoid of Holocene accretionary coastal landforms; they are young, having originated through flooding by the early Holocene. Northern and eastern coasts are lined by receding cliffs that supply abundant sediment to macro/mesotidal embayments lodging accretionary coastal landforms. Spit growth on the Atlantic shore played a major part in modifying the development of other landforms through barring the shoreline from wave attack. Sediment was mainly supplied from Pleistocene glacial deposits exposed at eroding headlands, and, more locally, obtained through cannibalization and from elevated Pleistocene beaches. In places, westerly winds combined with Atlantic swell to foster spit growth under high-energy wave power on both the bay and the ocean flanks, an unique occurrence. In addition, the westerlies caused widespread deflation on supratidal marshes and delivered fine-grained sediment inland and to the sea. Recent acceleration of glacio-eustatic rise is gradually changing the coastal zone to a condition of relative sea-level rise. The generally high and steep coastlines will not be greatly affected. A few gently-dipping lowlands might be flooded and biodiversity will be negatively affected.
Fil: Bujalesky, Gustavo Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Gonzalez Bonorino, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Tecnológica Nacional. Facultad Regional Río Grande; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Abascal, Liliana. Universidad Tecnológica Nacional. Facultad Regional Río Grande; Argentina
Materia
Subantarctic Holocene Coastal Environments
Coastal Processes
Gravel Beaches
Tierra del Fuego
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:11336/1763

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spelling Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-ChileBujalesky, Gustavo GabrielGonzalez Bonorino, GustavoAbascal, LilianaSubantarctic Holocene Coastal EnvironmentsCoastal ProcessesGravel BeachesTierra del Fuegohttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1https://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Holocene coastal environments in the Tierra del Fuego archipelago in southernmost South America evolved in a temperate cold climate characterized by strong and persistent mid-latitude westerly winds, and under stable to falling relative sea level. Southern and western coasts are rocky, microtidal, and generally devoid of Holocene accretionary coastal landforms; they are young, having originated through flooding by the early Holocene. Northern and eastern coasts are lined by receding cliffs that supply abundant sediment to macro/mesotidal embayments lodging accretionary coastal landforms. Spit growth on the Atlantic shore played a major part in modifying the development of other landforms through barring the shoreline from wave attack. Sediment was mainly supplied from Pleistocene glacial deposits exposed at eroding headlands, and, more locally, obtained through cannibalization and from elevated Pleistocene beaches. In places, westerly winds combined with Atlantic swell to foster spit growth under high-energy wave power on both the bay and the ocean flanks, an unique occurrence. In addition, the westerlies caused widespread deflation on supratidal marshes and delivered fine-grained sediment inland and to the sea. Recent acceleration of glacio-eustatic rise is gradually changing the coastal zone to a condition of relative sea-level rise. The generally high and steep coastlines will not be greatly affected. A few gently-dipping lowlands might be flooded and biodiversity will be negatively affected.Fil: Bujalesky, Gustavo Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Gonzalez Bonorino, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Tecnológica Nacional. Facultad Regional Río Grande; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Abascal, Liliana. Universidad Tecnológica Nacional. Facultad Regional Río Grande; ArgentinaGeological Society2013-10-23info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/1763Bujalesky, Gustavo Gabriel; Gonzalez Bonorino, Gustavo; Abascal, Liliana; Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile; Geological Society; Geological Society Special Publications; 388; 23-10-2013; 281-3030305-8719enginfo:eu-repo/semantics/altIdentifier/doi/10.1144/SP388.10info:eu-repo/semantics/altIdentifier/url/http://sp.lyellcollection.org/content/early/2013/10/18/SP388.10.full.pdf?ijkey=ouIaUokzf7KLzEA&keytype=finiteinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T12:19:41Zoai:ri.conicet.gov.ar:11336/1763instacron: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:34982025-10-22 12:19:41.764CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
title Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
spellingShingle Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
Bujalesky, Gustavo Gabriel
Subantarctic Holocene Coastal Environments
Coastal Processes
Gravel Beaches
Tierra del Fuego
title_short Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
title_full Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
title_fullStr Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
title_full_unstemmed Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
title_sort Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile
dc.creator.none.fl_str_mv Bujalesky, Gustavo Gabriel
Gonzalez Bonorino, Gustavo
Abascal, Liliana
author Bujalesky, Gustavo Gabriel
author_facet Bujalesky, Gustavo Gabriel
Gonzalez Bonorino, Gustavo
Abascal, Liliana
author_role author
author2 Gonzalez Bonorino, Gustavo
Abascal, Liliana
author2_role author
author
dc.subject.none.fl_str_mv Subantarctic Holocene Coastal Environments
Coastal Processes
Gravel Beaches
Tierra del Fuego
topic Subantarctic Holocene Coastal Environments
Coastal Processes
Gravel Beaches
Tierra del Fuego
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Holocene coastal environments in the Tierra del Fuego archipelago in southernmost South America evolved in a temperate cold climate characterized by strong and persistent mid-latitude westerly winds, and under stable to falling relative sea level. Southern and western coasts are rocky, microtidal, and generally devoid of Holocene accretionary coastal landforms; they are young, having originated through flooding by the early Holocene. Northern and eastern coasts are lined by receding cliffs that supply abundant sediment to macro/mesotidal embayments lodging accretionary coastal landforms. Spit growth on the Atlantic shore played a major part in modifying the development of other landforms through barring the shoreline from wave attack. Sediment was mainly supplied from Pleistocene glacial deposits exposed at eroding headlands, and, more locally, obtained through cannibalization and from elevated Pleistocene beaches. In places, westerly winds combined with Atlantic swell to foster spit growth under high-energy wave power on both the bay and the ocean flanks, an unique occurrence. In addition, the westerlies caused widespread deflation on supratidal marshes and delivered fine-grained sediment inland and to the sea. Recent acceleration of glacio-eustatic rise is gradually changing the coastal zone to a condition of relative sea-level rise. The generally high and steep coastlines will not be greatly affected. A few gently-dipping lowlands might be flooded and biodiversity will be negatively affected.
Fil: Bujalesky, Gustavo Gabriel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Gonzalez Bonorino, Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Tecnológica Nacional. Facultad Regional Río Grande; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Abascal, Liliana. Universidad Tecnológica Nacional. Facultad Regional Río Grande; Argentina
description Holocene coastal environments in the Tierra del Fuego archipelago in southernmost South America evolved in a temperate cold climate characterized by strong and persistent mid-latitude westerly winds, and under stable to falling relative sea level. Southern and western coasts are rocky, microtidal, and generally devoid of Holocene accretionary coastal landforms; they are young, having originated through flooding by the early Holocene. Northern and eastern coasts are lined by receding cliffs that supply abundant sediment to macro/mesotidal embayments lodging accretionary coastal landforms. Spit growth on the Atlantic shore played a major part in modifying the development of other landforms through barring the shoreline from wave attack. Sediment was mainly supplied from Pleistocene glacial deposits exposed at eroding headlands, and, more locally, obtained through cannibalization and from elevated Pleistocene beaches. In places, westerly winds combined with Atlantic swell to foster spit growth under high-energy wave power on both the bay and the ocean flanks, an unique occurrence. In addition, the westerlies caused widespread deflation on supratidal marshes and delivered fine-grained sediment inland and to the sea. Recent acceleration of glacio-eustatic rise is gradually changing the coastal zone to a condition of relative sea-level rise. The generally high and steep coastlines will not be greatly affected. A few gently-dipping lowlands might be flooded and biodiversity will be negatively affected.
publishDate 2013
dc.date.none.fl_str_mv 2013-10-23
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/11336/1763
Bujalesky, Gustavo Gabriel; Gonzalez Bonorino, Gustavo; Abascal, Liliana; Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile; Geological Society; Geological Society Special Publications; 388; 23-10-2013; 281-303
0305-8719
url http://hdl.handle.net/11336/1763
identifier_str_mv Bujalesky, Gustavo Gabriel; Gonzalez Bonorino, Gustavo; Abascal, Liliana; Holocene coastal environments and processes in subantarctic/temperate cold Tierra del Fuego, Argentina-Chile; Geological Society; Geological Society Special Publications; 388; 23-10-2013; 281-303
0305-8719
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1144/SP388.10
info:eu-repo/semantics/altIdentifier/url/http://sp.lyellcollection.org/content/early/2013/10/18/SP388.10.full.pdf?ijkey=ouIaUokzf7KLzEA&keytype=finite
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 Geological Society
publisher.none.fl_str_mv Geological Society
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
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