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
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/1763
Ver los metadatos del registro completo
| id |
CONICETDig_bdc608000910d405031ae3a1898b9fd8 |
|---|---|
| oai_identifier_str |
oai:ri.conicet.gov.ar:11336/1763 |
| network_acronym_str |
CONICETDig |
| repository_id_str |
3498 |
| network_name_str |
CONICET Digital (CONICET) |
| 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 |
| _version_ |
1846782637768704000 |
| score |
12.982451 |