dc.contributorPuerres Torres, Lizeth
dc.contributorTrejos Tamayo, Raúl
dc.contributor-GIEV-(CUMANDAY) Grupo de Investigación en Estratigrafía y Vulcanología (Categoría A1)
dc.creatorHernández Marín, Jessica Paola
dc.creatorBarragán Jacksson, Camila María
dc.date2021-09-15T20:54:19Z
dc.date2021-09-15T20:54:19Z
dc.date2021-09-15
dc.date.accessioned2023-09-06T18:29:33Z
dc.date.available2023-09-06T18:29:33Z
dc.identifierhttps://repositorio.ucaldas.edu.co/handle/ucaldas/17122
dc.identifierUniversidad de Caldas
dc.identifierRepositorio institucional Universidad de Caldas
dc.identifierhttps://repositorio.ucaldas.edu.co/
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8698195
dc.descriptionIlustraciones, gráficas, mapas
dc.descriptionspa: El núcleo NCS1 localizado en la laguna del atolón de Cayo Serrana en el Archipiélago de San Andrés y Providencia en el Mar Caribe, fue objeto de estudio para evaluar la respuesta de la microfauna bentónica de foraminíferos a la incidencia de eventos oceánicos extremos como huracanes, dada la alta vulnerabilidad de la zona al paso de estos eventos. Se identificaron 10 especies dominantes de las cuales se obtuvo la asociación Archaias angulatus, Asterigerina carinata, Cyclorbiculina compressa, y Acervulina inhaerens indicadora de condiciones de alta energía y transporte. Adicionalmente la proliferación de otras especies como Asterigerina carinata, Rosalina floridana y Quinqueloculina poeyana explican las dinámicas ecológicas subsecuentes al paso de eventos extremos que de igual forma ocasionan anomalías ecofenotípicas en los géneros Archaias, Cyclorbiculina y Laevipeneroplis. Estas evidencias junto con variaciones en la abundancia, diversidad, fragmentación y análisis de parámetros granulométricos indicadores de energía (media y desviación estándar), permitieron proporcionar indicios de cambios en el transporte y energía del medio que fueron soportados por análisis de datos en Modelos Aditivos Generalizados, concluyendo que los principales cambios a nivel ecológico y sedimentarios fueron ocasionados por eventos extremos que afectaron la zona de Cayo Serrana.
dc.descriptioneng: The NCS1 core located in the lagoon of the Cayo Serrana atoll in the Archipelago of San Andres and Providencia in the Colombian Caribbean Sea, was studied to evaluate the response of the benthic foraminifera assemblage to the incidence of oceanic extreme events such as hurricanes, due to the high vulnerability of the area to the passage of these events. Ten dominant species were identified, mainly assemblage made of Archaias angulatus, Asterigerina carinata, Cyclorbiculina compressa Rotorbinella rosea, and Acervulina inhaerens were proxies of high energy and transport conditions. Additionally, the spread of other species such as Asterigerina carinata, Rosalina floridana, and Quinqueloculina poeyana explain the ecological dynamics related to the passage of extreme events that may have caused ecophenotypic anomalies in the genera Archaias, Cyclorbiculina and Laevipeneroplis. These evidences together with variations in their abundance, diversity, fragmentation and granulometric parameters indicators of energy (mean and standard deviation) allowed us to provide clues on the changes of transport and energy of the environment that were supported by data analysis in Generalized Additive Models (GAM). We conclude that the main ecological and sedimentary changes were caused by extreme events that affect the area of Cayo Serrana.
dc.description1. Introducción / 1.1. Planteamiento del problema/ 1.2. Objetivos/ 2. Marco Teórico/ 2.1. Formación Atolones/ 2.2. Eventos Extremos/ 2.3. Eventos Extremos en el Caribe / 2.4. Eventos Extremos en Atolones e Impactos en su Morfología / 2.5. Foraminíferos/2.6. Foraminíferos en Atolones/ 2.7. Los Foraminíferos como Bioindicadores de Eventos Extremos en Atolones/ 2.8. Deformación en Foraminíferos/ 3. Zona de Estudio/ 3.1. Marco Geológico/ 3.2 Oceanografía y Climatología regional/ 4. Metodología / 4.1. Base de datos sobre eventos extremos en la zona de estudio / 4.2. Extracción y muestreo núcleo NSC1 / 4.3. Granulometría / 4.4. Selección y clasificación de foraminíferos/ 4.5. Diagrama ternario de ambiente según a la estructura de la pared/ 4.6. Determinación del índice de diversidad de Shannon-Weaver (H’) / 4.7. Deformación en foraminíferos/ 4.8. Análisis de datos/ 5. Resultados/5.1. Eventos extremos en el área de estudio. / 5.2. Granulometría del núcleo NCS1/ 5.3. Análisis de foraminíferos/ 5.4. Ambiente según la estructura de la pared / 5.5. Índice de diversidad de Shannon – Wiener (H’)./ 5.6. Deformación en Foraminíferos/ 5.7. Foraminíferos y variables indicadoras de energía / 6. Discusión/6.1. Influencia de eventos oceánicos extremos en el Atolón Cayo Serrana / 6.2. Respuesta de foraminíferos bentónicos ante eventos oceánicos extremos. / 7. Conclusiones y recomendaciones/ 8. Referencias/9. Anexos.
dc.descriptionUniversitario
dc.descriptionGeólogo(a)
dc.descriptionMicropaleontología y su respuesta a eventos oceánicos extremos
dc.formatapplication/pdf
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dc.languageeng
dc.languagespa
dc.publisherFacultad de Ciencias Exactas y Naturales
dc.publisherManizales
dc.publisherGeología
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dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectOceanografía
dc.subjectGeomorfología
dc.subjectCayo Serrana, Atolón
dc.subjectForaminíferos bentónicos
dc.subjectGranulometría
dc.subjectEventos Extremos
dc.subjectPaleoecología
dc.titleCaracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
dc.typeTrabajo de grado - Pregrado
dc.typehttp://purl.org/coar/resource_type/c_7a1f
dc.typeText
dc.typeinfo:eu-repo/semantics/bachelorThesis
dc.typehttps://purl.org/redcol/resource_type/TP
dc.typeinfo:eu-repo/semantics/publishedVersion


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