Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)

Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilom...

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Autores:
Geister, Jorn
Tipo de recurso:
Article of journal
Fecha de publicación:
1986
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/41324
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/41324
http://bdigital.unal.edu.co/31421/
Palabra clave:
Geology
Earth Sciences
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
Geología
Ciencias de la tierra
Geociencias
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
Rights
openAccess
License
Atribución-NoComercial 4.0 Internacional
id UNACIONAL2_c81faf653da56e10faa2bc7c0dedd769
oai_identifier_str oai:repositorio.unal.edu.co:unal/41324
network_acronym_str UNACIONAL2
network_name_str Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
title Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
spellingShingle Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
Geology
Earth Sciences
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
Geología
Ciencias de la tierra
Geociencias
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
title_short Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
title_full Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
title_fullStr Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
title_full_unstemmed Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
title_sort Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)
dc.creator.fl_str_mv Geister, Jorn
dc.contributor.author.spa.fl_str_mv Geister, Jorn
dc.subject.proposal.spa.fl_str_mv Geology
Earth Sciences
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
Geología
Ciencias de la tierra
Geociencias
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
topic Geology
Earth Sciences
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
Geología
Ciencias de la tierra
Geociencias
Pre-Miocene
Miocene
volcanic rocks
coral reef
Fore-reef terrace
Barrier reef
Lagoon
Leeward shelf
Submarine terraces
Pleistocene
description Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilometers broad, sloping gently from the reef to a morphological break below 30 m which marks the beginning of the outer slope.b) Barrier reef: more than 100 m broad and totalling some 30 km in length, it rises up to near low-tide level. Coherent in the north and in the south, its middle section is a chain of coral pillars. A profuse growth of MiIIepora,Palythoa and abundant coralline algae covers the reef crest, where locally a true algal ridge is developed.c) Lagoon: includes a broad and shallow lagoonal terrace adjacent to barrier reef and a deeper lagoon basin, both locally connected by steep "sand cliffs".  From the lagoon floor, covered by bare sand and coral rubble, numerouspatch reefs and coral heads to various heights.d) Leeward shelf: rocky flats with scattered coral growth extend from the shore to a steep escarpment at 20 or more meters depth marking the beginning of the western outer slope. Patch reefs and sandy flats are equally abundant.Submarine terraces, escarpments and valleys, as well as an irregular outline of many reefs reflect a complex geomorphological history of the insular shelf duringPleistocene, which is in part concealed by Holocene reef growth and sedimentation.
publishDate 1986
dc.date.issued.spa.fl_str_mv 1986
dc.date.accessioned.spa.fl_str_mv 2019-06-28T09:57:03Z
dc.date.available.spa.fl_str_mv 2019-06-28T09:57:03Z
dc.type.spa.fl_str_mv Artículo de revista
dc.type.coar.fl_str_mv http://purl.org/coar/resource_type/c_2df8fbb1
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/article
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dc.type.content.spa.fl_str_mv Text
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format http://purl.org/coar/resource_type/c_6501
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dc.identifier.uri.none.fl_str_mv https://repositorio.unal.edu.co/handle/unal/41324
dc.identifier.eprints.spa.fl_str_mv http://bdigital.unal.edu.co/31421/
url https://repositorio.unal.edu.co/handle/unal/41324
http://bdigital.unal.edu.co/31421/
dc.language.iso.spa.fl_str_mv spa
language spa
dc.relation.spa.fl_str_mv http://revistas.unal.edu.co/index.php/geocol/article/view/30591
dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Geología Colombiana
Geología Colombiana
dc.relation.ispartofseries.none.fl_str_mv Geología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992
dc.relation.references.spa.fl_str_mv Geister, Jorn (1986) Recent coral reefs and geology history of providencia island (western caribbean sea, colombia). Geología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
dc.rights.uri.spa.fl_str_mv http://creativecommons.org/licenses/by-nc/4.0/
dc.rights.accessrights.spa.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
Derechos reservados - Universidad Nacional de Colombia
http://creativecommons.org/licenses/by-nc/4.0/
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
dc.format.mimetype.spa.fl_str_mv application/pdf
dc.publisher.spa.fl_str_mv Departamento de Geociencias
institution Universidad Nacional de Colombia
bitstream.url.fl_str_mv https://repositorio.unal.edu.co/bitstream/unal/41324/1/30591-110744-1-PB.pdf
https://repositorio.unal.edu.co/bitstream/unal/41324/2/30591-110744-1-PB.pdf.jpg
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spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Geister, Jorndd68598c-503f-4999-b044-dee1afeff56b3002019-06-28T09:57:03Z2019-06-28T09:57:03Z1986https://repositorio.unal.edu.co/handle/unal/41324http://bdigital.unal.edu.co/31421/Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilometers broad, sloping gently from the reef to a morphological break below 30 m which marks the beginning of the outer slope.b) Barrier reef: more than 100 m broad and totalling some 30 km in length, it rises up to near low-tide level. Coherent in the north and in the south, its middle section is a chain of coral pillars. A profuse growth of MiIIepora,Palythoa and abundant coralline algae covers the reef crest, where locally a true algal ridge is developed.c) Lagoon: includes a broad and shallow lagoonal terrace adjacent to barrier reef and a deeper lagoon basin, both locally connected by steep "sand cliffs".  From the lagoon floor, covered by bare sand and coral rubble, numerouspatch reefs and coral heads to various heights.d) Leeward shelf: rocky flats with scattered coral growth extend from the shore to a steep escarpment at 20 or more meters depth marking the beginning of the western outer slope. Patch reefs and sandy flats are equally abundant.Submarine terraces, escarpments and valleys, as well as an irregular outline of many reefs reflect a complex geomorphological history of the insular shelf duringPleistocene, which is in part concealed by Holocene reef growth and sedimentation.Providencia Island, composed of pre-Miocene and Miocene volcanic rocks, is surrounded by an extensive coral reef complex which, from east to west, can besubdivided morphologically and ecologically into the following subparallel units:a) Fore-reef terrace: a bare rocky flat, from one to several kilometers broad, sloping gently from the reef to a morphological break below 30 m which marks the beginning of the outer slope.b) Barrier reef: more than 100 m broad and totalling some 30 km in length, it rises up to near low-tide level. Coherent in the north and in the south, its middle section is a chain of coral pillars. A profuse growth of MiIIepora,Palythoa and abundant coralline algae covers the reef crest, where locally a true algal ridge is developed.c) Lagoon: includes a broad and shallow lagoonal terrace adjacent to barrier reef and a deeper lagoon basin, both locally connected by steep "sand cliffs".  From the lagoon floor, covered by bare sand and coral rubble, numerouspatch reefs and coral heads to various heights.d) Leeward shelf: rocky flats with scattered coral growth extend from the shore to a steep escarpment at 20 or more meters depth marking the beginning of the western outer slope. Patch reefs and sandy flats are equally abundant.Submarine terraces, escarpments and valleys, as well as an irregular outline of many reefs reflect a complex geomorphological history of the insular shelf duringPleistocene, which is in part concealed by Holocene reef growth and sedimentationapplication/pdfspaDepartamento de Geocienciashttp://revistas.unal.edu.co/index.php/geocol/article/view/30591Universidad Nacional de Colombia Revistas electrónicas UN Geología ColombianaGeología ColombianaGeología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992Geister, Jorn (1986) Recent coral reefs and geology history of providencia island (western caribbean sea, colombia). Geología Colombiana - An International Journal on Geosciences; Vol. 15 (1986); 115-134 Geología Colombiana; Vol. 15 (1986); 115-134 2357-3767 0072-0992 .Recent coral reefs and geology history of providencia island (western caribbean sea, colombia)Artículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTGeologyEarth SciencesPre-MioceneMiocenevolcanic rockscoral reefFore-reef terraceBarrier reefLagoonLeeward shelfSubmarine terracesPleistoceneGeologíaCiencias de la tierraGeocienciasPre-MioceneMiocenevolcanic rockscoral reefFore-reef terraceBarrier reefLagoonLeeward shelfSubmarine terracesPleistoceneORIGINAL30591-110744-1-PB.pdfapplication/pdf15095209https://repositorio.unal.edu.co/bitstream/unal/41324/1/30591-110744-1-PB.pdfa90452f213c46bbc1e443a09cda11613MD51THUMBNAIL30591-110744-1-PB.pdf.jpg30591-110744-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg7276https://repositorio.unal.edu.co/bitstream/unal/41324/2/30591-110744-1-PB.pdf.jpg8f8bf3601e9f1782624a5c8db7eadeb4MD52unal/41324oai:repositorio.unal.edu.co:unal/413242024-01-29 23:07:08.497Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co