Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos

Ilustraciones, gráficas, mapas

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Fecha de publicación:: 2021

Institución:: Universidad de Caldas

Repositorio:: Repositorio Institucional U. Caldas

Idioma:: eng
spa

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network_acronym_str	REPOUCALDA
network_name_str	Repositorio Institucional U. Caldas
repository_id_str
dc.title.none.fl_str_mv	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
title	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
spellingShingle	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos Oceanografía Geomorfología Cayo Serrana, Atolón Foraminíferos bentónicos Granulometría Eventos Extremos Paleoecología
title_short	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
title_full	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
title_fullStr	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
title_full_unstemmed	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
title_sort	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremos
dc.contributor.none.fl_str_mv	Puerres Torres, Lizeth Trejos Tamayo, Raúl -GIEV-(CUMANDAY) Grupo de Investigación en Estratigrafía y Vulcanología (Categoría A1)
dc.subject.none.fl_str_mv	Oceanografía Geomorfología Cayo Serrana, Atolón Foraminíferos bentónicos Granulometría Eventos Extremos Paleoecología
topic	Oceanografía Geomorfología Cayo Serrana, Atolón Foraminíferos bentónicos Granulometría Eventos Extremos Paleoecología
description	Ilustraciones, gráficas, mapas
publishDate	2021
dc.date.none.fl_str_mv	2021-09-15T20:54:19Z 2021-09-15T20:54:19Z 2021-09-15
dc.type.none.fl_str_mv	Trabajo de grado - Pregrado http://purl.org/coar/resource_type/c_7a1f Text info:eu-repo/semantics/bachelorThesis https://purl.org/redcol/resource_type/TP
dc.type.coarversion.fl_str_mv	http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.identifier.none.fl_str_mv	https://repositorio.ucaldas.edu.co/handle/ucaldas/17122 Universidad de Caldas Repositorio institucional Universidad de Caldas https://repositorio.ucaldas.edu.co/
url	https://repositorio.ucaldas.edu.co/handle/ucaldas/17122 https://repositorio.ucaldas.edu.co/
identifier_str_mv	Universidad de Caldas Repositorio institucional Universidad de Caldas
dc.language.none.fl_str_mv	eng spa
language	eng spa
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F., Yu, X., & Mellor, G. L. (2002). Analyses and simulations of the upper ocean’s response to Hurricane Felix at the Bermuda Testbed Mooring site: 13-23 August 1995. Journal of Geophysical Research: Oceans, 107(C12), 25-1-25–29. https://doi.org/10.1029/2001JC000969 Zeppilli, D., Sarrazin, J., Leduc, D., Arbizu, P. M., Fontaneto, D., Fontanier, C., Gooday, A. J., Kristensen, R. M., Ivanenko, V. N., Sørensen, M. V., Vanreusel, A., Thébault, J., Mea, M., Allio, N., Andro, T., Arvigo, A., Castrec, J., Danielo, M., Foulon, V., … Fernandes, D. (2015). Is the meiofauna a good indicator for climate change and anthropogenic impacts? Marine Biodiversity, 45(3), 505–535. https://doi.org/10.1007/s12526-015-0359-z Zhu, Y., & Toth, Z. (2013). Extreme Weather Events and their Probabilistic Prediction by the NCEP Ensemble Forecast System. www.emc.ncep.noaa.gov/gmb/ens/target/ens/albapr/albapr.html
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spelling	Caracterización de foraminíferos bentónicos del núcleo NCS1, en el Atolón Cayo Serrana: Distribución, variabilidad y respuesta de estos ante eventos oceánicos extremosOceanografíaGeomorfologíaCayo Serrana, AtolónForaminíferos bentónicosGranulometríaEventos ExtremosPaleoecologíaIlustraciones, gráficas, mapasspa: 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.eng: 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.1. 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.UniversitarioGeólogo(a)Micropaleontología y su respuesta a eventos oceánicos extremosFacultad de Ciencias Exactas y NaturalesManizalesGeologíaPuerres Torres, LizethTrejos Tamayo, Raúl-GIEV-(CUMANDAY) Grupo de Investigación en Estratigrafía y Vulcanología (Categoría A1)Hernández Marín, Jessica PaolaBarragán Jacksson, Camila María2021-09-15T20:54:19Z2021-09-15T20:54:19Z2021-09-15Trabajo de grado - Pregradohttp://purl.org/coar/resource_type/c_7a1fTextinfo:eu-repo/semantics/bachelorThesishttps://purl.org/redcol/resource_type/TPhttp://purl.org/coar/version/c_970fb48d4fbd8a85application/pdfapplication/pdfapplication/pdfapplication/pdfhttps://repositorio.ucaldas.edu.co/handle/ucaldas/17122Universidad de CaldasRepositorio institucional Universidad de Caldashttps://repositorio.ucaldas.edu.co/engspaAccary, F., & Roger, J. (2010). Tsunami catalog and vulnerability of martinique (Lesser Antilles, France). Journal of Tsunami Society International, 29(3), 148–170.Acosta Herrera, N. (2004a). 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