Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas

Ilustraciones, fotos, gráficas

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Fecha de publicación:
2022
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Universidad de Caldas
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Repositorio Institucional U. Caldas
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eng
spa
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https://repositorio.ucaldas.edu.co/
Palabra clave:
Ridge de Beata
Globigerina bulloides
Bioecozona
Complejo menardii
Bioestratigrafía
Ciencias de la tierra
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id REPOUCALDA_6b724e7b72ecf45ef797beb4aeb447af
oai_identifier_str oai:repositorio.ucaldas.edu.co:ucaldas/18195
network_acronym_str REPOUCALDA
network_name_str Repositorio Institucional U. Caldas
repository_id_str
dc.title.none.fl_str_mv Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
title Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
spellingShingle Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
Ridge de Beata
Globigerina bulloides
Bioecozona
Complejo menardii
Bioestratigrafía
Ciencias de la tierra
title_short Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
title_full Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
title_fullStr Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
title_full_unstemmed Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
title_sort Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficas
dc.contributor.none.fl_str_mv Duque Castaño, Monica
Trejos Tamayo, Raúl
Suarez Ibarra, Jaime Yesid
dc.subject.none.fl_str_mv Ridge de Beata
Globigerina bulloides
Bioecozona
Complejo menardii
Bioestratigrafía
Ciencias de la tierra
topic Ridge de Beata
Globigerina bulloides
Bioecozona
Complejo menardii
Bioestratigrafía
Ciencias de la tierra
description Ilustraciones, fotos, gráficas
publishDate 2022
dc.date.none.fl_str_mv 2022-11-29T21:56:48Z
2022-11-29T21:56:48Z
2022-11-29
dc.type.none.fl_str_mv Trabajo de grado - Pregrado
http://purl.org/coar/resource_type/c_7a1f
Text
info:eu-repo/semantics/bachelorThesis
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/18195
Universidad de Caldas
Repositorio Institucional Universidad de Caldas
https://repositorio.ucaldas.edu.co/
url https://repositorio.ucaldas.edu.co/handle/ucaldas/18195
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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spelling Bioecozonamiento del núcleo PC-029 a partir del estudio de foraminíferos planctónicos Cuaternarios del Caribe colombiano: Implicaciones paleoecológicas y paleoceanográficasRidge de BeataGlobigerina bulloidesBioecozonaComplejo menardiiBioestratigrafíaCiencias de la tierraIlustraciones, fotos, gráficasspa:El patrón de distribución de las abundancias relativas de foraminíferos planctónicos del Cuaternario fue utilizado para realizar una zonación estratigráfica (bioecozonas) e identificar los estadios glaciales e interglaciales en el testigo sedimentario PC-029. Este testigo sedimentario de 4,25 m fue perforado en el mar Caribe cerca al Ridge de Beata, al NW del departamento de la Guajira, Colombia, a una profundidad de la columna de agua de ~3500 a 4000 m. En este estudio fue posible identificar las bioecozonas V, W, X, Y2, Y1 y Z a partir de la presencia y ausencia de las especies dentro del complejo menardii (Globorotalia menardii, Globorotalia tumida y Globorotalia flexuosa), Pulleniatina spp., y Globoconella inflata. Además, las especies Globorotalia truncatulinoides (morfotipo de enrollamiento dextral) y Globorotalia crassaformis permitieron corroborar algunos límites bioestratigráficos. Los resultados obtenidos asignaron una edad al núcleo de 184,78-1,63 ka (Pleistoceno Medio al Holoceno Superior). Se identificaron los Estadios Isotópicos Marinos MIS 6 al MIS 1, los cuales corresponden a dos períodos interglaciales (MIS 5 y 1) y dos períodos glaciales (MIS 6 y 2-4). Asimismo, se analizó la respuesta ecológica de las asociaciones de foraminíferos a los cambios de temperatura durante estos períodos. Los resultados muestran un predominio de las especies asociadas a temperaturas cálidas especialmente en el MIS 5 y 1, mientras que durante los MIS 6, 2 y 4, las especies con afinidad por aguas frías muestran un leve incremento en sus abundancias. Los datos obtenidos sugieren que, si bien las especies frías incrementaron su abundancia durante las épocas glaciales, no hay evidencia de un recambio ecológico significativo durante todo el intervalo de estudio. Por otra parte, se sugiere que la tasa de sedimentación registrada durante el Pleistoceno fue influenciada por la cantidad de nutrientes disponibles en el área de estudio. Estas variaciones fueron registradas en las abundancias de la especie Globigerina bulloides, las cuales fueron relativamente altas en las épocas glaciales y bajas en los períodos interglaciales. La proveniencia de los nutrientes pudo estar relacionada con el sistema de surgencia de la Guajira o la influencia de las aguas Subtropicales Subsuperficiales del Atlántico Tropical. Por lo tanto, se interpreta que estos nutrientes pudieron ser redistribuidos en la cuenca por la influencia de vórtices oceánicos. Finalmente, se sugiere que el uso de la técnica de bioecozonas en testigos sedimentarios del Caribe colombiano es una herramienta útil para datar sedimentos marinos Cuaternarios y permite realizar estimaciones confiables de la tasa de sedimentación. Sin embargo, la estratigrafía isotópica de oxígeno y las dataciones radiométricas son necesarias para refinar las interpretaciones asociadas al modelo de edad.eng:The distribution pattern of the relative abundances of Quaternary planktonic foraminifera was used to make a stratigraphic zonation (bioecozones) and identify the glacial and interglacial stages in the sedimentary core PC-029. This 4.25-meter sedimentary core was drilled in the Caribbean Sea near the Beata Ridge, NW of the department of La Guajira, Colombia, at a water column depth of 3500 to 4000 m. In this study, it was possible to identify the V, W, X, Y2, Y1 and Z bioecozones from the presence and absence of the species within the menardii complex (Globorotalia menardii, Globorotalia tumida and Globorotalia flexuosa), Pulleniatina spp., and Globoconella inflata. Furthermore, the species Globorotalia truncatulinoides (dextral coiling morphotype) and Globorotalia crassaformis allowed to corroborate some biostratigraphy limits. The results obtained assigned an age to the core of 184,78 - 1,63 ka (Middle Pleistocene to Late Holocene). Marine Isotopic Stages, MIS 6 to MIS 1 were identified, which correspond to two interglacial periods (MIS 5 and MIS 1) and two glacial periods (MIS 6 and MIS 2-4). In addition, the ecological response of foraminifera associations to temperature changes during these periods was analyzed. The results show a predominance of species associated with warm temperatures, especially in MIS 5 and 1, while during MIS 6, 2 and 4, species with an affinity for cold waters show a slight increase in their abundances. The data obtained suggest that, although the cold species increased their abundance during the ice ages, there is no evidence of a significant ecological turnover during the entire study interval. On the other hand, it is suggested that the sedimentation rate recorded during the Pleistocene was influenced by the amount of nutrients available in the study area. These variations were recorded in the abundances of the species Globigerina bulloides, which were relatively high in the glacial times and low in the interglacial periods. The provenance of the nutrients could be related to the upwelling system of La Guajira or the influence of the Subtropical Underwater of the tropical Atlantic. Therefore, it is interpreted that these nutrients could be redistributed in the basin by the influence of oceanic vortices. Finally, it is suggested that the use of the bioecozones technique in sedimentary cores from the Colombian Caribbean is a useful tool to date Quaternary marine sediments and allows reliable estimates of the sedimentation rate. However, oxygen isotopic stratigraphy and radiometric dating are necessary to refine the interpretations associated with the age pattern.1. Introducción / 2. Objetivos / 2.1. Objetivo General / 2.2. Objetivos Específicos / 3. Área de Estudio / 3.1. Localización / 3.2. Contexto Geológico / 3.2.1. Formación de la Placa Caribe / 3.2.2. Evolución temporal de la placa Caribe y el mar Caribe / 3.2.3. Geología actual alrededor del mar Caribe / 3.3. Contexto Oceanográfico / 4. Antecedentes / 4.1. Bioestratigrafía del Cuaternario tardío basada en foraminíferos planctónicos para el océano Atlántico y el mar Caribe / 4.2. Estudios realizados en el área del mar Caribe para el Cuaternario / 5. Materiales y métodos / 5.1. Revisión bibliográfica / 5.2. Extracción y muestreo del pozo PC-029 / 5.3. Preparación de muestras / 9 5.4. Selección y clasificación de foraminíferos planctónicos / 5.5. Determinación de bioecozonas y construcción del modelo de edad / 5.6. Análisis paleoecológico de las asociaciones de foraminíferos planctónicos / 6. Resultados / 6.1. Descripción litológica del pozo PC-029 / 6.2. Taxonomía y distribución de los foraminíferos planctónicos a lo largo del pozo / 6.3. Bioecozonamiento (BZ) para el pozo PC-029 / 7. Discusión / 7.1. Bioecozonamiento y su relación con los estadios isotópicos marinos (MIS-Marine Isotope Stages) / 7.2. Comparación de las edades propuestas con la técnica del nanoplancton calcáreo / 7.3. Variaciones en la tasa de sedimentación del pozo PC-029 / 7.4. Análisis paleoecológico de las asociaciones de foraminíferos planctónicos a lo largo del pozo PC-029 / 7.5. Relación de las abundancias del complejo menardii con los estadios isotópicos marinos MIS 6 - MIS 1 / 8. Conclusiones / 9. Referencias / 10. AnexosUniversitarioGeólogo(a)Facultad de Ciencias Exactas y NaturalesManizalesGeologíaDuque Castaño, MonicaTrejos Tamayo, RaúlSuarez Ibarra, Jaime YesidLeal Posada, Laura2022-11-29T21:56:48Z2022-11-29T21:56:48Z2022-11-29Trabajo de grado - Pregradohttp://purl.org/coar/resource_type/c_7a1fTextinfo:eu-repo/semantics/bachelorThesishttp://purl.org/coar/version/c_970fb48d4fbd8a85application/pdfapplication/pdfapplication/pdfapplication/pdfhttps://repositorio.ucaldas.edu.co/handle/ucaldas/18195Universidad de CaldasRepositorio Institucional Universidad de Caldashttps://repositorio.ucaldas.edu.co/engspaAze, T., Ezard, T. H. G., Purvis, A., Coxall, H. K., Stewart, D. R. M., Wade, B. 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