Bioestratigrafía con foraminíferos planctónicos y microfacies en rocas de Albiano medio a Maastrichtiano del núcleo A, Valle Medio del Magdalena, Colombia : un enfoque taxonómico y paleoambiental

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dc.contributor.advisorSánchez Quiñónez, Carlos Albertospa
dc.contributor.authorDíaz-Suárez, Camila M.M.spa
dc.contributor.orcidDíaz-Suárez, Camila M.M. [0009000880932735]spa
dc.coverage.countryColombiaspa
dc.coverage.regionMagdalenaspa
dc.date.accessioned2025-07-16T17:18:33Z
dc.date.available2025-07-16T17:18:33Z
dc.date.issued2024-10
dc.descriptionilustraciones a color, diagramas, fotografíasspa
dc.description.abstractLos foraminíferos planctónicos son útiles en investigaciones bioestratigráficas debido a su gran distribución espacial, altas tasas evolutivas y un buen potencial para ser preservados en la roca. Este estudio comprobó la utilidad de los foraminíferos como herramienta para el entendimiento de la depositación de las rocas marinas en la sucesión cretácica en Colombia. Por eso, se centra en la clasificación de foraminíferos planctónicos y la litología en rocas del Albiano tardío al Maastrichtiano tardío en el núcleo del Pozo A (Valle Medio del Magdalena, Colombia). Para lograrlo se observó el Núcleo A con sus variaciones litológicas, se estudiaron 109 secciones delgadas del mismo lugar en su contenido composicional, textural y fósil (vista en 2D) y se reconoció el contenido de foraminíferos planctónicos en 20 muestras de roca del pozo preparadas con nitrógeno líquido y/o peróxido y acetona (vista en 3D). A partir de allí se delimitaron 17 intervalos litológicos, se reconocieron litofacies, límites de unidades, procesos diagenéticos, 49 microfacies y 20 biozonas (formales e informales) con énfasis en foraminíferos planctónicos en sección delgada, definiendo edades. Posteriormente se interpretaron las condiciones paleoambientales bajo las cuales estas rocas se depositaron y se calcularon tasas de sedimentación en roca compactada. En orden ascendente, se encontró que la Formación Simití contiene las biozonas Ticinella praeticinensis (?) de edad Albiano medio (?) y Thalmanninella appenninica de edad Albiano tardío y se depositó en zonas intermareales a lagunares. La Formación Calizas del Salto abarca las biozonas Thalmanninella globotruncanoides (?), Thalmanninella reicheli (?), Rotalipora cushmani y la parte inferior de la biozona Whiteinella archaeocretacea, indicando una edad Cenomaniano y ambientes de rampa media proximal. Las rocas del Miembro Salada en la Formación La Luna posiblemente inician su depositación en la parte superior de la biozona Whiteinella archaeocretacea, seguida por la biozona Helvetoglobotruncana helvetica, Marginotruncana sigali, la subzona informal Marginotruncana coronata y la parte inferior de la biozona Dicarinella concavata indicando el Turoniano y ambientes entre la rampa media distal y la rampa externa distal. El Miembro Pujamana comprende la parte superior de la biozona Dicarinella concavata y la parte basal de la biozona Dicarinella asymetrica, indicando una edad Coniaciano hasta Santoniano (~Santoniano temprano), y ambientes intermareales a lagunares. El Miembro Galembo contiene la parte superior de la biozona Dicarinella asymetrica, correspondiente a Santoniano (~Santoniano tardío) y se depositó en ambientes de rampa media proximal, ocasionalmente en la rampa interna restringida. Finalmente, las rocas del Campaniano al Maastrichtiano abarcan las biozonas Contusotruncana plummerae, Radotruncana calcarata, Globotruncanella havanensis, Globotruncana aegyptiaca, Gansserina gansseri, Trinitella scotti (informal), Pseudoguembelina palpebra, Racemiguembelina fructicosa y Abathomphalus mayaroensis, todas indicando edades de Campaniano a Maastrichtiano. Estas rocas se depositaron en ambientes que oscilan generalmente entre la retrorampa y la rampa interna, con algunas variaciones hacia la rampa media. Por tal motivo los resultados de este estudio aportan nueva información en la comprensión de la edad y ambientes de depósito en rocas del Cretácico superior, usando foraminíferos planctónicos en sección delgada e información litológica detallada. Esta información se ilustra de manera concisa en el resumen gráfico del Núcleo A (Texto tomado de la fuente).spa
dc.description.abstractPlanktonic foraminifera are useful in biostratigraphic investigations due to their large spatial distribution, high evolutionary rates, and good potential to be conserved in rocks. This study proved the usefulness of foraminifera as a tool for understanding the deposition of marine rocks in the Cretaceous succession in Colombia. Therefore, it focuses on the planktonic foraminifera classification and lithology in late Albian to late Maastrichtian rocks observed in the A Well (Middle Magdalena Valley, Colombia). To achieve this, rocks with its lithological variations were observed in the core, from the same place 109 thin sections were studied in their compositional, textural and fossil content (2D view) and the content of planktonic foraminifera was recognized in 20 samples prepared with liquid nitrogen and/or peroxide and acetone (3D view). This way the content and variations of planktonic foraminifera, lithology and diagenetic alterations in the rocks were identified. From there, 17 lithological intervals were marked off and lithofacies, unit limits, 49 microfacies and 20 biozones (formal and informal) based on planktonic foraminifera in thin section were recognized, defining ages. Subsequently, the paleoenvironmental conditions under which these rocks were deposited were interpreted and the sedimentation rates in compacted rock were calculated. In ascending order, the Simití Formation was found to contain the Middle Albian (?) Ticinella praeticinensis biozone (?), the Late Albian Thalmanninella appenninica biozone and was deposited in intertidal to lagoonal areas. The Calizas del Salto Formation encompasses the Thalmanninella globotruncanoides (?), Thalmanninella reicheli (?) and Rotalipora cushmani biozones and the lower part of the Whiteinella archaeocretacea biozone, indicating a Cenomanian age and proximal middle ramp environments. The Salada Member rocks in the La Luna Formation possibly started their deposition in the upper part of the Whiteinella archaeocretacea biozone, followed by the Helvetoglobotruncana helvetica biozone, Marginotruncana sigali biozone, the informal Marginotruncana coronata subzone and the lower part of Dicarinella concavata biozone indicating the Turonian and environments between the distal middle ramp and distal outer ramp. The Pujamana Member comprises the upper part of the Dicarinella concavata biozone and the lower part of Dicarinella asymmetrica biozone indicating a Coniacian to Santonian (~early Santonian) age and intertidal to lagoonal environments. The Galembo Member contains the upper part of Dicarinella asymmetrica biozone, corresponding to a Santonian age (~Late Santonian) and was deposited in proximal middle ramp environments, occasionally in the restricted inner ramp. Finally, the Campanian to Maastrichtian rocks encompass the biozones Contusotruncana plummerae, Radotruncana calcarata, Globotruncanella havanensis, Glotruncanella aegyptiaca, Gansserina gansseri, Trinitella scotti (informal), Pseudoguembelina palpebra, Racemiguembelina fructicosa, and Abathomphalus mayaroensis, all of them indicating Campanian to Maastrichtian ages. These rocks were deposited in environments that generally oscillate between the back ramp and the inner ramp, with some variations towards the middle ramp. Therefore, this studies results provides new information for understanding the age and depositional environments in Upper Cretaceous rocks, using planktonic foraminifera in thin section and detailed lithological information. This information is concisely illustrated in the graphical summary of Well A.eng
dc.description.degreelevelMaestríaspa
dc.description.degreenameMagíster en Ciencias - Geologíaspa
dc.description.researchareaMicropaleontología con foraminíferos Sedimentología de rocas calcáreasspa
dc.format.extent250 páginas + anexosspa
dc.format.mimetypeapplication/pdfspa
dc.identifier.instnameUniversidad Nacional de Colombiaspa
dc.identifier.reponameRepositorio Institucional Universidad Nacional de Colombiaspa
dc.identifier.repourlhttps://repositorio.unal.edu.co/spa
dc.identifier.urihttps://repositorio.unal.edu.co/handle/unal/88347
dc.language.isospaspa
dc.publisherUniversidad Nacional de Colombiaspa
dc.publisher.branchUniversidad Nacional de Colombia - Sede Bogotáspa
dc.publisher.facultyFacultad de Cienciasspa
dc.publisher.placeBogotá, Colombiaspa
dc.publisher.programBogotá - Ciencias - Maestría en Ciencias - Geologíaspa
dc.relation.referencesAbdolreza, M., Hossein, V. y Ali. S. (2020). The Maastrichtian‐Danian in the SW Zagros Fold‐Thrust Belt (S. Iran): An Integration of Planktonic Foraminiferal Biostratigraphy and Gamma‐Ray Spectrometry. Acta Geologica Sinica‐English Edition, 94(5), 1339-1363.spa
dc.relation.referencesAhr, W. (1998). Carbonate ramps, 1973–1996: a historical review. Geological Society, London, Special Publications, 149(1), 7–14. https://doi.org/10.1144/GSL.SP.1999.149.01.02spa
dc.relation.referencesAhr, W. M. (1973). Carbonate Ramp—Alternative to Shelf Model. AAPG Bulletin, 57(9), 1826. https://doi.org/10.1306/83D910BF-16C7-11D7-8645000102C1865Dspa
dc.relation.referencesAl-Awwad, S. F., y Pomar, L. (2015). Origin of the rudstone–floatstone beds in the Upper Jurassic Arab-D reservoir, Khurais Complex, Saudi Arabia. Marine and Petroleum Geology, 67, 743–768. https://doi.org/10.1016/j.marpetgeo.2015.05.014spa
dc.relation.referencesANH. (2012). Cuenca valle medio del Magdalena: Integración geológica de la digitalización y análisis de núcleos, pozo: infantas-1613. https://www.anh.gov.co/documents/2671/6._Informe_Final_VMM.pdfspa
dc.relation.referencesArenillas, I., Arz, J. A., Molina, E., y Dupuis, C. (2000a). The Cretaceous/Paleogene (K/P) Boundary at Aïn Settara, Tunisia: Sudden Catastrophic Mass Extinction in Planktic Foraminifera. Journal of Foraminiferal Research, 30(3), 202–218. https://doi.org/10.2113/0300202spa
dc.relation.referencesArenillas, I., Alegret, L., Sola, J. A. A., y Molina, E. (2000b). Uso didáctico de los foraminíferos en la Enseñanza de Ciencias de la Tierra: su distribución Paleoceanográfica en el tránsito Cretácico-Terciario. Enseñanza de las Ciencias de la Tierra, 8(2), 108-118.spa
dc.relation.referencesArmenteros, I., Bustillo, M., y Huerta, P. (2015). Dolomitización y calcitización en facies lacustres calcáreas y yesíferas (Eoceno superior, Formación Deza, cuenca de Almazán, España). Geogaceta, 57, 11–14. https://sge.usal.es/archivos/geogacetas/geo57/G57art3.pdfspa
dc.relation.referencesBallesteros, C., y Parra, J. (2012). Estudio estratigráfico secuencial para la Formación La Luna en el costado oriental de la cuenca del Valle Medio del Magdalena: una visión exploratoria de hidrocarburos no convencionales. Tésis de pregrado. Universidad Industrial de Santander.spa
dc.relation.referencesBallesteros, C., Galvis, H., Higuera, I., Marfisi, N., de la Parra, F., Céspedes, S., Cantisano, M., Forero, S., Barrera, P., Rodríguez, C., Zamora, W., Restrepo, D., Cerón, J., y Castillo, R. (2013). Anotaciones acerca de la estratigrafía del intervalo Cenomaniano-Campaniano atravesado por el pozo La Luna-1, cuenca del Valle Medio del Magdalena. XVI Congreso Colombiano de Geología.spa
dc.relation.referencesBanner, F. T., y Desai, D. (1988). A review and revision of the Jurassic-Early Cretaceous Globigerinina, with especial reference to the Aptian assemblages of Speeton (North Yorkshire, England). Journal of Micropalaeontolgy, 7(2), 143-185. https://doi.org/10.1144/jm.7.2.143spa
dc.relation.referencesBarr, F. T. (1962). Upper Cretaceous Planktonic Foraminifera from the Isle of Wight, England. Palaeontology, 4(4), 552-580. https://www.palass.org/sites/default/files/media/publications/palaeontology/volume_4/vol4_part4_pp552-580.pdfspa
dc.relation.referencesBarrero, D., Pardo, A., Vargas, C., Martínez, J. (2007). Colombian sedimentary basins: Nomenclature, boundaries and petroleum geology, a new proposal. ANH. https://www.anh.gov.co/documents/12/colombian_sedimentary_basins.pdfspa
dc.relation.referencesBernal, L. (2009). Caracterización estratigráfica y petrográfica de la Formación La Luna en el sector de El Tablazo, Valle Medio del Magdalena. X Simposio Bolivariano Exploración Petrolera En Cuencas Subandinas, 1–6.spa
dc.relation.referencesBernal L. E. (2006). Cartografía Geológica de 9600 KM2 de la Serrania de san Lucas: Planchas 55 (El Banco), 64 (Barranco de Loba), 85 (Simiti) y 96 (Bocas del Rosario): Aporte al conocimiento de su Evolucion Geologica. Memoria explicativa. Plancha 85 Simiti. Sur de los Departamentos de Bolivar y Cesar. Universidad industrial de santander-Servicio geologico colombiano. Informe técnico.spa
dc.relation.referencesBertle, R. J., y Suttner, T. J. (2005). New biostratigraphic data for the Chikkim Formation (Cretaceous, Tethyan Himalaya, India). Cretaceous Research, 26(6), 882–894. https://doi.org/10.1016/j.cretres.2005.06.001spa
dc.relation.referencesBolli, H. (1945). Zur Stratigraphie der Oberen Kreide in den höheren helvetischen Decken. Eclogae Geologic Helvetiae, 37, 217–331. http://doi.org/10.5169/seals-160503spa
dc.relation.referencesBolli, H. (1951). The Genus Globotruncana in Trinidad, B. W. I.: Notes on Occurrence, Nomenclature and Relationships between Species. Journal of Paleontology, 25(2), 187–199. http://www.jstor.org/stable/1299798spa
dc.relation.referencesBolli, H. (1957). The genera Praeglobotruncana, Rotalipora, Globotruncana and Abathomphalus in the upper Cretaceous of Trinidad, B.W.I. Bulletin of American Paleontology, 215, 51–60. https://www.biodiversitylibrary.org/part/70795spa
dc.relation.referencesBolli, H. (1959). Planktonic Foraminifera from the Cretaceous of Trinidad, B.W.I. Bulletin of American Paleontology, 39, pp. 257-277. https://www.biodiversitylibrary.org/page/10645985spa
dc.relation.referencesBolli, H. M., Loeblich, A. R., y Tappan, H. (1957). Planktonic foraminiferal families Hantkeninidae, Orbulinidae, Globorotaliidae and Globotruncanidae. Bulletin of the United States National Museum, 215(1), 3-50. https://biostor.org/reference/106006spa
dc.relation.referencesBolli, H., Saunders, J., y Perch-Nielsen, K. (1989). Plankton Stratigraphy, Volume 1, Planktic foraminifera, calcareous nannofossils and calpionellids. Cambridge University Press.spa
dc.relation.referencesBorrego, J., Monterde, J., Morales, J., Carro, B., y Lopez, N. (2003). Morfologia de la pirita diagenetica en sedimentos recientes de estuario del rio odiel (SO de España). Geogaceta, 33, 99–101. https://sge.usal.es/archivos/geogacetas/Geo33/Art25.pdfspa
dc.relation.referencesBosence, D. (2005). A genetic classification of carbonate platforms based on their basinal and tectonic settings in the Cenozoic. Sedimentary Geology, 175(1), 49–72. https://doi.org/https://doi.org/10.1016/j.sedgeo.2004.12.030spa
dc.relation.referencesBouDagher-Fadel, M. (2013). Biostratigraphic and geological significance of planktonic foraminifera. UCL Press. Second edition.spa
dc.relation.referencesBouDagher-Fadel, M. (2015). Biostratigraphic and geological significance of planktonic foraminifera. UCL Press. Updated second edition.spa
dc.relation.referencesBouDagher-Fadel, M. K., Banner, F. T., Whittaker, J. E., y Simmons, M. D. (1997). The early evolutionary history of planktonic foraminifera. London: Chapman y Hall.spa
dc.relation.referencesBralower, T. J., y Lorente, M. A.. (2003). Paleogeography and Stratigraphy of the La Luna Formation and Related Cretaceous Anoxic Depositional Systems. Palaios, 18(4–5), 301–304. http://dx.doi.org/10.1669/0883-1351(2003)018<0301:pasotl>2.0.co;2spa
dc.relation.referencesBrönnimann, P. (1952). Globigerinidae from the Upper Cretaceous (Cenomanian-Maestrichtian of Trinidad, BWI. Paleontological Research Institution.spa
dc.relation.referencesBronnimann, P., y Brown Jr, N. (1953). Observations on some Planktonic Heterohelicidae from the Upper Cretaceous of Cuba. Contributions from the Cushman Foundation for Foraminiferal Research, 4, 150–155.spa
dc.relation.referencesBrotzen, F. (1934). Foraminiferen aus dem Senon Palästinas. Zeitschrift Des Deutschen Palästina-Vereins (1878-1945), 57(1), 28–72. https://www.jstor.org/stable/27930052spa
dc.relation.referencesBürgl, H., y Tobón, Y. D. (1954). El Cretáceo Superior en la región de Girardot. Boletin Geologico, 2(1), 23-48.spa
dc.relation.referencesCaballero, V., Parra, M., y Mora Bohorquez, A. R. (2010). Levantamiento de la Cordillera Oriental de Colombia durante el Eoceno tardío-Oligoceno temprano: proveniencia sedimentaria en el Sinclinal de Nuevo Mundo, cuenca Valle Medio del Magdalena. Boletín de geología, 32(1), 45-77. https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/1008spa
dc.relation.referencesCaballero, V., Parra, M., Mora, A., López, C., Rojas, L. E., y Quintero, I. (2013). Factors controlling selective abandonment and reactivation in thick-skin orogens: A case study in the Magdalena Valley, Colombia. Geological Society, London, Special Publications, 377(1), 343-367. https://doi.org/10.1144/SP377.4spa
dc.relation.referencesCampbell, C. (1967). Lamina, Laminset, Bed and Bedset. Sedimentology, 8(1), 7–26. https://doi.org/10.1111/j.1365-3091.1967.tb01301.xspa
dc.relation.referencesCanacol Energy Ltd. (2013). Canacol Energy Ltd. Anuncia descubrimiento de petróleo en el pozo Mono Araña 1 en Colombia. http://www.canacolenergy.co/i/pdf/nr-esp/enero-24.pdfspa
dc.relation.referencesCarman, K. (1929). Some foraminifera from the Niobrara and Benton Formations of Wyoming. Journal of Paleontology, 3(3), 309-315. http://www.jstor.org/stable/1298039spa
dc.relation.referencesCaron, M. (1978). Cretaceous Planktonic Foraminifers from DSDP Leg 40, Southeastern Atlantic Ocean. Initial Reports of the Deep Sea Drilling Project, 40, 651-678. https://doi.org/10.2973/dsdp.proc.40.114.1978spa
dc.relation.referencesCaron, M. (1985) Cretaceous Planktic Foraminifera. In: Bolli, H.M., Saunders, J.B. and Perch Nielsen, K., Eds., Plankton Stratigraphy, Cambridge University Press, Cambridge, 17-86.spa
dc.relation.referencesCaron, M. y Spezzaferri, S. (2006). Scanning Electron Microscope Documentation of the Lost Holotypes ff Mornod, 1949: Thalmanninella Reicheli and Rotalipora Montsalvensis. Journal of Foraminiferal Research, 36(4), 374–378. https://doi.org/10.2113/gsjfr.36.4.374spa
dc.relation.referencesCaron, M., Dall’Agnolo, S., Accarie, H., Barrera, E., Kauffman, E. G., Amédro, F., y Robaszynski, F. (2006). High-resolution stratigraphy of the Cenomanian–Turonian boundary interval at Pueblo (USA) and wadi Bahloul (Tunisia): stable isotope and bio-events correlation. Geobios, 39(2), 171–200. https://doi.org/https://doi.org/10.1016/j.geobios.2004.11.004.spa
dc.relation.referencesCarrivick, J. L. (2007). Modelling coupled hydraulics and sediment transport of a high-magnitude flood and associated landscape change. Annals of Glaciology, 45, 143-154.spa
dc.relation.referencesCediel, F., Shaw, R.P., y Cáceres, C. (2003). Tectonic assembly of the Northern Andean Block. In: Bartolini, C., Buffer, R.T., Blickwede, J. (Eds.), The Circum-gulf of Mexico and the Caribbean: Hydrocarbon Habitats, Basin Formation, and Plate Tectonics. AAPG memoir, 79, 815-848.spa
dc.relation.referencesChacón, B., Martı́n-Chivelet, J., y Gräfe, K. U. (2004). Latest Santonian to latest Maastrichtian planktic foraminifera and biostratigraphy of the hemipelagic successions of the Prebetic Zone (Murcia and Alicante provinces, south-east Spain). Cretaceous Research, 25(4), 585-601. https://doi.org/10.1016/j.cretres.2004.05.003spa
dc.relation.referencesChoquette, P. W., y Pray, L. C. (1970). Geologic Nomenclature and Classification of Porosity in Sedimentary Carbonates1. AAPG Bulletin, 54(2), 207–250. https://doi.org/10.1306/5D25C98B-16C1-11D7-8645000102C1865Dspa
dc.relation.referencesCobianchi, M., Luciani, V., y Bosellini, A. (1997). Early Cretaceous nannofossils and planktonic foraminifera from northern Gargano (Apulia, southern Italy). Cretaceous Research, 18(2), 249-293. https://doi.org/10.1006/cres.1996.0058spa
dc.relation.referencesCoccioni, R., y Premoli Silva, I. (2015). Revised Upper Albian–Maastrichtian planktonic foraminiferal biostratigraphy and magnetostratigraphy of the classical Tethyan Gubbio section (Italy). Newsletters on Stratigraphy, 48(1), 47-90. https://doi.org/10.1127/NOS/2015/0055spa
dc.relation.referencesCoccioni, R., Luciani, V., y Marsili, A. (2006). Cretaceous oceanic anoxic events and radially elongated chambered planktonic foraminifera: Paleoecological and paleoceanographic implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 235(1-3), 66-92. https://doi.org/10.1016/j.palaeo.2005.09.024spa
dc.relation.referencesCooper, M. A., Addison, F. T., Alvarez, R., Coral, M., Graham, R. H., Hayward, A. B., ... y Taborda, A. (1995). Basin development and tectonic history of the Llanos Basin, Eastern Cordillera, and middle Magdalena Valley, Colombia. AAPG Bulletin, 79(10), 1421-1442. https://doi.org/10.1306/7834D9F4-1721-11D7-8645000102C1865Dspa
dc.relation.referencesCushman, J. A. (1926). Some foraminifera from the Mendez Shale of eastern Mexico. Contributions from the Cushman Laboratory for Foraminiferal Research, 2(1), 16-26.spa
dc.relation.referencesCushman, J. A. (1927). An outline of a re-classification of the foraminifera. Contributions from Cushman Laboratory for Foraminiferal Research, 3, 1-105.spa
dc.relation.referencesCushman, J. A. (1927). New and interesting Foraminifera from Mexico and Texas. Contributions from the Cushman Laboratory for Foraminiferal Research, 3, pls-22.spa
dc.relation.referencesCushman, J. A. (1931). Hastigerinella and other interesting foraminifera from the Upper Cretaceous of Texas. Contributions from the Cushman Laboratory for Foraminiferal Research, 7(4), 83-90.spa
dc.relation.referencesCushman, J. A. (1938). Cretaceous species of Gümbelina and related genera. Contributions from the Cushman Laboratory for Foraminiferal Research, 14(1), 2-28.spa
dc.relation.referencesCushman, J. A. y Hedberg, H. D. (1941). Upper cretaceous foraminifera from santander del norte, Colombia, SA. Contributions from the Cushman Laboratory for Foraminiferal Research, 17(4), 79-100.spa
dc.relation.referencesDe Porta, J. (1966). Geología del extremo S del Valle Medio del magdalena entre Honda y Guataquí (Colombia). Boletín de Geología, 22-23, 5-341. https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6552spa
dc.relation.referencesDe Souza, F. L., Krahl, G., y Fauth, G. (2018). Late Cretaceous (Cenomanian-Maastrichtian) planktic foraminifera from Goban Spur (DSDP sites 549 and 550): Biostratigraphic inferences. Cretaceous Research, 86, 238-250. https://doi.org/10.1016/j.cretres.2018.02.012spa
dc.relation.referencesDeford, R., Folk, R., Sander, N., y Cunningham, W. (1972). Carbonate Rocks: Classifications, dolomite, dolomitization. American Association of Petroleum Geologists.spa
dc.relation.referencesDenne, R. A., Hinote, R. E., Breyer, J. A., Kosanke, T. H., Lees, J. A., Engelhardt-Moore, N., ... y Tur, N. (2014). The Cenomanian–Turonian Eagle Ford Group of South Texas: Insights on timing and paleoceanographic conditions from geochemistry and micropaleontologic analyses. Palaeogeography, Palaeoclimatology, Palaeoecology, 413, 2-28. https://doi.org/10.1016/j.palaeo.2014.05.029spa
dc.relation.referencesDíaz, C., Iturralde, M., y García, D. (2001). Evidencias del coctel paleontológico del límite Cretácico–Terciario en Cuba Occidental. In IV Congreso Cubano de Geología (pp. 125-128).spa
dc.relation.referencesDickson, J. (1965). A Modified Staining Technique for Carbonates in Thin Section. Nature, 205(4971), 587. https://doi.org/10.1038/205587a0spa
dc.relation.referencesDieni, I., Massari, F., y Radulovic, V. (2012). Clasts of uppermost Albian (Vraconian) limestone in the Eocene Cuccuru'e Flores Conglomerate of the M. Albo massif (eastern Sardinia). Rivista Italiana di Paleontologia e Stratigrafia, 118(1). https://doi.org/10.13130/2039-4942/5997spa
dc.relation.referencesDouglas, R., y Sliter, W. V. (1966). Regional Distribution of Some Cretaceous Rotaliporidae and Globotrucanidae (Foraminiferida) within North America. Tulane Studies in Geology and Paleontology, 4(3). https://journals.tulane.edu/tsgp/article/view/423/319spa
dc.relation.referencesDunham, R. J. (1962). Classification of Carbonate Rocks According to Depositional Texture. In Classification of Carbonate Rocks—A Symposium. American Association of Petroleum Geologists. https://doi.org/10.1306/M1357spa
dc.relation.referencesDuque-Caro, H. (1965). Zonas bioestratigráficas de foraminíferos del Cretácico de Colombia. Ministerio de Minas y Petroleos, Servicio Geológico Nacional.spa
dc.relation.referencesCaro, H. D. (1975). Los foraminíferos planctónicos y el Terciario de Colombia. Revista Española de Micropaleontología, 7(3), 403-427.spa
dc.relation.referencesEcopetrol. (2000). Atlas of sedimentary basins and petroleum geology of Colombia.spa
dc.relation.referencesEgger, H., Mohamed, O., y Roegl, F. (2013). Plankton stratigraphy of the santonian at morzg, salzburg (gosau group, northern calcareous alps, Austria). Austrian Journal of Earth Sciences, 106(2). https://www.zobodat.at/pdf/MittGeolGes_106_2_0089-0114.pdfspa
dc.relation.referencesEgger, J.G. (1899). Foraminiferen und Ostrakoden aus den Kreidemergeln der Oberbayerischen Alpen. Abhhandlungen der Königlich Bayerischen Akademie der Wissenschaften, Mathematisch-physikalische Classe. 21(1), 1902, 1-230.spa
dc.relation.referencesEhrenberg, C.G. (1840) Über die Bildung der Kreidefelsen und des Kreidemergels durch unsichtbare Organismen. Abhandlungen der Königlichen Akademie der Wissenschaften zu Berlin: 59-147spa
dc.relation.referencesEhrenberg, C.G. (1844) Verbreitung und Einfluß des mikroskopischen Lebens in Süd- und Nord-Amerika. Abhandlungen der Königlichen Akademie der Wissenschaften zu Berlin, 4, 291-445.spa
dc.relation.referencesEl-Nakhal, H. A. (2002). Classification of the meridionally costellate Cretaceous planktonic foraminifera. Journal of Micropalaeontology, 21(1), 1-8.spa
dc.relation.referencesErbacher, J., Bornemann, A., Petrizzo, M. R., y Huck, S. (2020). Chemostratigraphy and stratigraphic distribution of keeled planktonic foraminifera in the Cenomanian of the North German Basin. Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 171(2) 149 - 161https://dx.doi.org/10.1127/zdgg/2020/0211spa
dc.relation.referencesErlich, R. N., Macsotay, O., Nederbragt, A. J., y Lorente, M. A. (1999). Palaeoecology, palaeogeography and depositional environments of Upper Cretaceous rocks of western Venezuela. Palaeogeography, Palaeoclimatology, Palaeoecology, 153(1-4), 203-238.spa
dc.relation.referencesErlich, R. N., T. Villamil, and J. Keens-Dumas, 2003, Controls on the deposition of Upper Cretaceous organic carbon–rich rocks from Costa Rica to Suriname, in C. Bartolini, R. T. Buffler, and J. Blickwede, eds., The Circum-Gulf of Mexico and the Caribbean: Hydrocarbon habitats, basin formation, and plate tectonics: AAPG Memoir 79, p. 1–45.spa
dc.relation.referencesEsmaeilbeig, M. R. (2018). Biostratigraphy of the Gurpi Formation (Santonian–Maastrictian) by using Globotruncanidae, Zagros Mountains, Iran. Carbonates and Evaporites, 33, 133-142.spa
dc.relation.referencesEtayo-Serna, F, Montoya, D., Moreno, G., Terraza, R., y Guzmán, G. (2019). Estudios geológicos y paleontológicos sobre el Cretácico en la región del embalse del río Sogamoso, Valle Medio del Magdalena (Fernando Etayo-Serna (ed.)). Libros del Servicio Geológico Colombiano. https://libros.sgc.gov.co/index.php/editorial/catalog/book/24spa
dc.relation.referencesEtayo-Serna, F, Solé De Porta, N., De Porta, J., y Gaona, T. (2003). The Batá Formation of Colombia is truly Cretaceous, not Jurassic. Journal of South American Earth Sciences, 16(3), 113–117. https://doi.org/10.1016/S0895-9811(03)00048-8spa
dc.relation.referencesEtayo-Serna, F. (1964). Posición de las faunas en los depósitos cretácicos colombianos y su valor en la subdivisión cronológica de los mismos. Bucaramanga. Universidad Industrial de Santander. Boletín de Geología, (16-17), 5-142.spa
dc.relation.referencesEtayo-Serna, F., Renzoni, G., Barrero, D. (1969). Contornos sucesivos del mar Cretáceo en Colombia. Memorias 1er. Cong. Col. de Geol, 217-253.spa
dc.relation.referencesEtayo-Serna, Fernando. 2019a. “ʻFormaciónʼ Simití: unidad ambigua en la estratigrafía del Valle Medio del Magdalena”. En Estudios geológicos y paleontológicos sobre el Cretácico en la región del embalse del río Sogamoso, Valle Medio del Magdalena, dirección científica y edición de Fernando Etayo-Serna. Compilación de los Estudios Geológicos Oficiales en Colombia vol. XXIII. Bogotá: Servicio Geológico Colombianospa
dc.relation.referencesEtayo-Serna, Fernando. 2019b. “Basin development and tectonic history of the Middle Magdalena Valley”. En Estudios geológicos y paleontológicos sobre el Cretácico en la región del embalse del río Sogamoso, Valle Medio del Magdalena, dirección científica y edición de Fernando Etayo-Serna. Compilación de los Estudios Geológicos Oficiales en Colombia vol. XXIII. Bogotá: Servicio Geológico Colombiano.spa
dc.relation.referencesFabre, A. (1987). Tectonique et géneration d’hydrocarbures: Un modèle de l’evolution de la Cordillère Orientale de Colombie et du Bassin de Llanos pendant le Crétacé et le Tertiaire. Archives des Sciences Genève, 40(2), 145-190.spa
dc.relation.referencesFalzoni, F., y Petrizzo, M. R. (2011). Taxonomic overview and evolutionary history of globotruncanita insignis. Journal of Foraminiferal Research, 41(4), 371-383.spa
dc.relation.referencesFalzoni, F., Petrizzo, M. R., Jenkyns, H. C., Gale, A. S., y Tsikos, H. (2016). Planktonic foraminiferal biostratigraphy and assemblage composition across the Cenomanian–Turonian boundary interval at Clot Chevalier (Vocontian Basin, SE France). Cretaceous Research, 59, 69-97.spa
dc.relation.referencesFlores-Cadenas, B. E., Monier-Castillo, A., Lopez-Palomino, I., Ferre, B., Palma-Ramirez, A., Romo-Ramírez, J. R., ... y Contreras-Cruz, D. (2019). Turonian microfossil assemblage of the Eagle Ford Formation From The La Bolita locality, Coahuila, northwest Mexico. Revista Brasileira de Paleontologia, 22, 3.spa
dc.relation.referencesFlügel, E. (2004). Microfacies Data: Fabrics. In Microfacies of Carbonate Rocks: Analysis, Interpretation and Application (pp. 177–242). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-662-08726-8_5spa
dc.relation.referencesFlügel, E. (2010). Microfacies of Carbonate Rocks: Analysis, Interpretation and Application (2nd ed.). Springer. https://doi.org/https://doi.org/10.1007/978-3-642-03796-2spa
dc.relation.referencesFolk, R. L. (1954). The Distinction between Grain Size and Mineral Composition in Sedimentary-Rock Nomenclature. The Journal of Geology, 62(4), 344–359. https://doi.org/10.1086/626171spa
dc.relation.referencesFolk, R. L. (1959). Practical Petrographic Classification of Limestones. AAPG Bulletin, 43(1), 1–38. https://doi.org/10.1306/0BDA5C36-16BD-11D7-8645000102C1865Dspa
dc.relation.referencesFolk, R. L. (1962). Spectral Subdivision of Limestone Types. In Classification of Carbonate Rocks—A Symposium. American Association of Petroleum Geologists. https://doi.org/10.1306/M1357spa
dc.relation.referencesFolk, R. L. (2005). Nannobacteria and the formation of framboidal pyrite: Textural evidence. Journal of Earth System Science, 114(3), 369–374. https://doi.org/10.1007/BF02702955spa
dc.relation.referencesFrankel, J. J. (1964). Recent foraminifera filled and encrusted with pyrite from Durban bay, South Africa. South African Journal of Science, 60(10), 299-301.spa
dc.relation.referencesFrerichs, W. E. (1979). Planktonic Foraminifera from the sage breaks shale, Centennial Valley, Wyoming. The Journal of Foraminiferal Research, 9(2), 159-184.spa
dc.relation.referencesGale, A. S., Bown, P., Caron, M., Crampton, J., Crowhurst, S. J., Kennedy, W. J., ... y Wray, D. S. (2011). The uppermost Middle and Upper Albian succession at the Col de Palluel, Hautes-Alpes, France: An integrated study (ammonites, inoceramid bivalves, planktonic foraminifera, nannofossils, geochemistry, stable oxygen and carbon isotopes, cyclostratigraphy). Cretaceous Research, 32(2), 59-130.spa
dc.relation.referencesGale, A. S., Kennedy, W. J., y Petrizzo, M. R. (2021). Stratigraphy of the Albian− Cenomanian boundary interval in the Agadir Basin, Morocco: ammonites, microcrinoids, planktonic foraminifera. Acta Geologica Polonica, 71(4), 453-480.spa
dc.relation.referencesGandolfi, R. (1942). Ricerche micropaleontologiche e stratigrafiche sulla scaglia e sul flysch cretacici dei dintorni di Balerna (Canton Ticino). Rivista Italiana di Paleontologia, 48, 1-160.spa
dc.relation.referencesGandolfi, R. (1955). The genus Globotruncana in northeastern Colombia. Bulletins of American Paleontology, XXVI, 1–118.spa
dc.relation.referencesGandolfi, R. (1957). Notes on some species of Globotruncana. Contribution from the Cushman Foundation for foraminiferal research. 8(2): 59-65spa
dc.relation.referencesGeorgescu, A., García Delgado, D., y Gil González, S. (2013). Planktonic foraminifers and nannoconid assem blages from the Late Aptian and Late Albian limestones of the Pons Formation (Sierra de los Organos, west ern Cuba). In V Convención de Ciencias de la Tierra (Geociencias’ 2013), 1 al 5 de abril de 2013. X Congreso Cubano de Geología (Geología’2013), Memorias en CD-Rom, GE02 (Vol. 10).spa
dc.relation.referencesGeorgescu, M. D. (1996). Santonian-Maastrichtian planktonic foraminifers (Globigerinelloididae, Hedbergellidae, Globotruncanidae and Rugoglobigerinidae) in the Romanian black sea offshore. Micropaleontology, 42(4) 305-333.spa
dc.relation.referencesGeorgescu, M. D. (2000). Late Albian-Turonian planktonic foraminifera in the Romanian western black sea offshore. Revista Española de Micropaleontologia, 32(2), 157-174.spa
dc.relation.referencesGeorgescu, M. D. (2017). Upper Cretaceous planktic foraminiferal biostratigraphy. Studia UBB Geologia, 61(1), 5-20.spa
dc.relation.referencesGeorgescu, M. D., y Huber, B. T. (2006). Paracostellagerina nov. gen., a meridionally costellate planktonic foraminiferal genus of the middle Cretaceous (latest Albian-earliest Cenomanian). Journal of Foraminiferal Research, 36(4), 368-373.spa
dc.relation.referencesGeorgescu, M. D., y Huber, B. T. (2009). Early evolution of the Cretaceous serial planktic foraminifera (late Albian–Cenomanian). Journal of Foraminiferal Research, 39(4), 335-360.spa
dc.relation.referencesGilardoni, S. E. (2017). Late Albian-Cenomanian planktonic foraminiferal biostratigraphy, taxonomy and paleoceanographic inferences. Doctoral thesis, Università degli Studi di Milano. http://hdl.handle.net/2434/479427spa
dc.relation.referencesGiraldo-Villegas, C. A., Rodríguez-Tovar, F. J., Celis, S. A., y Pardo-Trujillo, A. (2025). Campanian-Maastrichtian evolution of sedimentary systems during the final stages of an epeiric sea—La Luna Sea—in eastern Colombia: Processes, spatio-temporal variability, and depositional controls. Marine and Petroleum Geology, 177, 107385. https://doi.org/10.1016/j.marpetgeo.2025.107385spa
dc.relation.referencesGómez-Pérez, I., Fernández-Mendiola, P. A., y García-Mondéjar, J. (1998). Constructional dynamics for a Lower Cretaceous carbonate ramp (Gorbea Massif, north Iberia). Geological Society, London, Special Publications, 149(1), 229–252. https://doi.org/10.1144/GSL.SP.1999.149.01.12spa
dc.relation.referencesGradstein, F. M., Ogg, J. G., Schmitz, M. D., y Ogg, G. M. (Eds.). (2020). Geologic time scale 2020. Elsevier.spa
dc.relation.referencesGraham, J. M. (1995). Lithostratigraphy, microfacies and foraminiferal biostratigraphy of the Santonian-lower Campanian strata in the Trans-Pecos region, West Texas. PhD Thesis. The University of Texas at Dallas.spa
dc.relation.referencesGuerrero, J., Sarmiento - Pérez, G., y Navarrete, R. (2000). The Stratigraphy of the W Side of the Cretaceous Colombian Basin in the Upper Magdalena Valley. Reevaluation of Selected Areas and Type Localities Including Aipe, Guaduas, Ortega, and Piedras. Geologia Colombiana, 25, 45–110.spa
dc.relation.referencesGuzmán, G., Torres. A., Ramírez. R., (2013). “Anexo 1 Columna estratigráfica del Pozo PMM 01”. En Descripción Sedimentológica de Núcleos de Perforación para el Programa de Yacimientos No Convencionales Pozo PMM 01. Génesis, Consultoría en Geología. Informe Interno.spa
dc.relation.referencesHagn, H., y Zeil, W. (1954). Globotruncanen aus dem Ober-Cenoman und Unter-Turon der Bayerischen Alpen. Eclogae Geologicae Helvetiae, 47, 1-60.spa
dc.relation.referencesHakyemez, A., y Özkan-Altiner, S. (2010). Upper Maastrichtian–Eocene planktonic foraminiferal zonation in the Beşparmak Range, Northern Cyprus. Micropaleontology, 56(5), 413-438.spa
dc.relation.referencesHaq, B. U. (2014). Cretaceous eustasy revisited. Global and Planetary Change, 113, 44–58. https://doi.org/https://doi.org/10.1016/j.gloplacha.2013.12.007spa
dc.relation.referencesHaq, B. U., y Boersma, A. (Eds.). (1998). Introduction to marine micropaleontology. Elsevier.spa
dc.relation.referencesHart, M. B. (1999). The evolution and biodiversity of Cretaceous planktonic Foraminiferida. Geobios, 32(2), 247-255.spa
dc.relation.referencesHaynes, J. (1981). Foraminifera. John Wiley y Sons, Ltdspa
dc.relation.referencesHaynes, S. J., Huber, B. T., y Macleod, K. G. (2015). Evolution and phylogeny of mid-Cretaceous (Albian–Coniacian) biserial planktic foraminifera. Journal of Foraminiferal Research, 45(1), 42-81.spa
dc.relation.referencesHedberg, H., y Sass, L. (1937). Synopsis of the geologic formations of the western part of the Maracaibo Basin. Venezuela. Boletín de Geología y Minería, 2–4, 73-112.spa
dc.relation.referencesHofker, J. (1956). Die Globotruncanen von Nordwest-Deutschland und Holland. Neues Jahrbuch fur Geologie und Palaontologie, Abhandlungen, 103, 312-340.spa
dc.relation.referencesHuber, B. T. (1992). Upper Cretaceous planktic foraminiferal biozonation for the austra realm. Marine Micropaleontology, 20(2), 107-128.spa
dc.relation.referencesHuber, B. T., y Leckie, R. M. (2011). Planktic foraminiferal species turnover across deep-sea Aptian/Albian boundary sections. The Journal of Foraminiferal Research, 41(1), 53-95.spa
dc.relation.referencesHuber, B. T., Leckie, R. M., Norris, R. D., Bralower, T. J., y CoBabe, E. (1999). Foraminiferal assemblage and stable isotopic change across the Cenomanian-Turonian boundary in the subtropical North Atlantic. The Journal of Foraminiferal Research, 29(4), 392-417.spa
dc.relation.referencesHuber, B. T., Petrizzo, M. R., Watkins, D. K., Haynes, S. J., y MacLeod, K. G. (2017). Correlation of Turonian continental margin and deep-sea sequences in the subtropical Indian Ocean sediments by integrated planktonic foraminiferal and calcareous nannofossil biostratigraphy. Newsletters on Stratigraphy, 50(2), 141-185.spa
dc.relation.referencesHuber, B., y Petrizzo, M. R. (2014). Evolution and taxonomic study of the cretaceous planktic foraminiferal genus Helvetoglobotruncana reiss, 1957. The Journal of Foraminiferal Research, 44, 40–57. https://doi.org/10.2113/gsjfr.44.1.40spa
dc.relation.referencesHuber, B., Petrizzo, M. R., y Falzoni, F. (2022). Taxonomy and phylogeny of Albian-Maastrichtian planispiral planktonic foraminifera traditionally assigned to Globigerinelloides. Micropaleontology, 68, 117–183. https://doi.org/10.47894/mpal.68.2.01spa
dc.relation.referencesJacob, K., y Sastry, M. V. A. (1950). On the occurrence of Globotruncana in Uttattur stage of the Trichinopoly Cretaceous. South India: Science and Culture, Calcutta, 16(6), 267.spa
dc.relation.referencesJaff, R. B. N. (2021). A designed model for identifications of Dicarinella concavata (Brotzen, 1934) and Dicarinella asymetrica (Sigal, 1952) planktic foraminifer species under thin sections: an example from the Kurdistan region, NE Iraq. JJEES, 154.spa
dc.relation.referencesJaff, R. B. N., y Al-Kahtany, K. (2020). Coniacian/Santonian calcareous nannofossil and planktonic foraminifera in the Kurdistan Region, NE Iraq: biostratigraphy and bioevents. Arabian Journal of Geosciences, 13(18), 916. https://doi.org/10.1007/s12517-020-05922-6.spa
dc.relation.referencesJaff, R. B., Wilkinson, I. P., Lee, S., Zalasiewicz, J., Lawa, F., & Williams, M. (2015). Biostratigraphy and palaeoceanography of the early Turonian–early Maastrichtian planktonic foraminifera of NE Iraq. Journal of Micropalaeontolgy, 34(2), 105-138.spa
dc.relation.referencesJaff, R., y Lawa, F. (2020). Biostratigraphy and Systematic Palaeontology of Late Cretaceous Heterohelicidae Foraminifera from Kurdistan Region North-eastern Iraq. Iraqi National Journal of Earth Science, 20(2), 33-63.spa
dc.relation.referencesJaramillo, C., y Rueda, M. (2004). Impact of Biostratigraphy on Oil Exploration. III Convencion Tecnica ACGGP. La inversion en el conocimiento geologico, P4, CDROM, Bogota. https://stri-sites.si.edu/docs/publications/pdfs/Jaramillo_C_2004_zonacion_colombia_ACGGP.pdfspa
dc.relation.referencesJenkyns, H. C. (1980). Cretaceous anoxic events: from continents to oceans. Journal of the Geological Society, 137(2), 171-188.spa
dc.relation.referencesJenkyns, H. C., Gale, A. S., y Corfield, R. M. (1994). Carbon- and oxygen-isotope stratigraphy of the English Chalk and Italian Scaglia and its palaeoclimatic significance. Geological Magazine, 131(1), 1–34. https://doi.org/10.1017/S0016756800010451spa
dc.relation.referencesJones, R. (2013). Foraminifera and their Applications. Cambridge University Press. https://doi.org/10.1017/CBO9781139567619spa
dc.relation.referencesKeller, B. M. (1935). Microfauna of the Upper Cretaceous in the Dnjepr-Donets valley and some other adjoining regions. (in Russian). Byulleten Moskovskogo Obshchestva Ispytateley Prirody Otdel Geologicheskiy, 13, 522-558.spa
dc.relation.referencesKeller, G. (2004). Low-diversity, late Maastrichtian and early Danian planktic foraminiferal assemblages of the eastern Tethys. The Journal of Foraminiferal Research, 34(1), 49-73.spa
dc.relation.referencesKhan, S., Kroon, D., Ahmad, S., Ali, A., Wadood, B., y Rahman, A. (2021). Planktonic foraminiferal biostratigraphy of the Cretaceous strata, Indus Basin, Pakistan, Eastern Tethys: implications for oceanic anoxic events. Australian Journal of Earth Sciences, 68(8), 1162-1178.spa
dc.relation.referencesKhan, S., Wadood, B., Ahmed, S., Khan, A., Ahmed, F., y Khan, H. (2017). Evaluating paleoceanographic and planktonic foraminiferal diversification from the Cretaceous Mughal Kot Formation, Mughal Kot Section, Lower Indus Basin, Pakistan. Journal of Himalayan Earth Sciences, 50(2), 27-43.spa
dc.relation.referencesKietzmann, D., Palma, R. M., y Bressan, G. S. (2008). Facies y microfacies de la rampa tithoniana-berriasiana de la Cuenca Neuquina (Formación Vaca Muerta) en la sección del arroyo Loncoche - Malargüe, provincia de Mendoza. Revista de La Asociación Geológica Argentina, 63(4), 696-713.spa
dc.relation.referencesKorchagin, O. A. (2011). Upper Campanian-lower Maastrichtian planktonic foraminifers and biostratigraphy of the Moni Formation, southern Cyprus. Stratigraphy and Geological Correlation, 19, 526-544.spa
dc.relation.referencesKorchagin, V. I. (1982). Систематика глоботрунканин - Systematics of the Globotruncanids. Byulleten Moskovskogo Obshchestva Ispytateley Prirody Otdel Geologicheskiy. 57(5): 114-121.spa
dc.relation.referencesKuenzi, W. D., Horst, O. H., y McGEHEE, R. V. (1979). Effect of volcanic activity on fluvial-deltaic sedimentation in a modern arc-trench gap, southwestern Guatemala. Geological Society of America Bulletin, 90(9), 827-838.spa
dc.relation.referencesLeckie, R. M. (1984). Mid-Cretaceous planktonic foraminiferal biostratigraphy off central Morocco, Deep Sea Drilling Project Leg 79, Sites 545 and 547. Initial Reports Deep Sea Drilling Project, 79, 579-620.spa
dc.relation.referencesLeckie, R. M. (1987). Paleoecology of mid-Cretaceous planktonic foraminifera: a comparison of open ocean and epicontinental sea assemblages. Micropaleontology, 33(2), 164-176.spa
dc.relation.referencesLeckie, R. M., Yuretich, R. F., West, O. L., Finkelstein, D., y Schmidt, M. (1998). Paleoceanography of the southwestern Western Interior Sea during the time of the Cenomanian-Turonian boundary (Late Cretaceous). En: Dean, W, Arthur M. Stratigraphy and Paleoenvironments of the Cretaceous Western Interior Seaway, USA. https://doi.org/10.2110/csp.98.06.0101spa
dc.relation.referencesLoeblich Alfred R., J. R., y Tappan, H. (1982). Foraminifera. Journal of Foraminiferal Research, 12(4), 377–382. https://doi.org/10.2113/gsjfr.12.4.377spa
dc.relation.referencesLoeblich Jr, A. R., y Tappan, H. (1984). Suprageneric classification of the Foraminiferida (Protozoa). Micropaleontology, 30, 1-70.spa
dc.relation.referencesLoeblich Jr, A. R., y Tappan, H. (2015). Foraminiferal genera and their classification. Springer.spa
dc.relation.referencesLoeblich, A. R. y Tappan, H. (1961). Cretaceous planktonic foraminifera: Part I-Cenomanian. Micropaleontology, 7, 257-304.spa
dc.relation.referencesLoeblich, A. R. y Tappan, H. (1988). Foraminiferal Genera and Their Classification (Volume I-II). Van Nostrand Reinhold Co., New York. 1-1059spa
dc.relation.referencesLoeblich, A. R., y Tappan, H. (1964). Sarcodina, chiefly the amoebians and foraminiferida: Treatise on invertebrate paleontology, Par C, Protista, 2, Vol. 1-2. Geol. Soc. Amer and University of Kansas Press, Newyork, USA.spa
dc.relation.referencesLongoria, J. F. (1974). Stratigraphic, morphologic and taxonomic studies of Aptian planktonic foraminifera. Revista Española de Micropaleontología, Numero Extraordinario, 5-107.spa
dc.relation.referencesLongoria, J. F., y Gamper, M. A. (1977). Albian planktonic foraminifera from the Sabinas Basin of northern Mexico. The Journal of Foraminiferal Research, 7(3), 196-215.spa
dc.relation.referencesLópez, L., Lo Mónaco, S., Escobar, G., Camargo, C., Lugo, P., Rojas, H., y González, C. (2009). Study of pyrite nodules from querecual formation, anzoátegui state (Venezuela) by with electron probe microanálisis. Acta Microscopica, 18, 333–343.spa
dc.relation.referencesLorente, M. A., Duran, I., y Ruiz, M. (1996). Late Cretaceous in western Venezuela, a new biostratigraphical approach. In AAPG/SVG International congress and exhibition, 2,. 1309-1310.spa
dc.relation.referencesMacellari, C. E. (1988). Cretaceous paleogeography and depositional cycles of western South America. Journal of South american earth Sciences, 1(4), 373-418.spa
dc.relation.referencesMacellari, C. E., y De Vries, T. J. (1987). Late Cretaceous upwelling and anoxic sedimentation in northwestern South America. Palaeogeography, Palaeoclimatology, Palaeoecology, 59, 279-292.spa
dc.relation.referencesMacellari, C. E., y De Vries, T. J. (1987). Late Cretaceous upwelling and anoxic sedimentation in northwestern South America. Palaeogeography, Palaeoclimatology, Palaeoecology, 59, 279-292.spa
dc.relation.referencesMackenzie, F. (2005). Sediments, Diagenesis, and Sedimentary Rocks: Treatise on Geochemistry (Second edi). Elsevier.spa
dc.relation.referencesMagne, J. y Sigal, J. (1954). Description des especes nouvelles; 1 - Foraminiferes. In, Cheylan, G., Magne, J., Sigal, J. y Grekoff, N. (eds) Resultats geologiques et micropaleontologiques du sondage d' El Krachem (Hauts Plateaux algerois). Bulletin de la Société Géologique de France . 3(4-6): 471-492.spa
dc.relation.referencesMantilla, F. L., Reyes, G., Montoya, D., y Mojica, J. (2006). Presencia de Cloritoide en Rocas Cretácicas del Cinturón Esmeraldífero Occidental (Cordillera oriental, Colombia): Implicaciones Genéticas. Boletín de Geología, 28(2). https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/849spa
dc.relation.referencesMarianos, A. W., y Zingula, R. P. (1966). Cretaceous planktonic foraminifers from Dry Creek, Tehama County, California. Journal of Paleontology, 40(2), 328-342.spa
dc.relation.referencesMartin, S. E. (1972). Reexamination of the Upper Cretaceous planktonic foraminiferal genera Planoglobulina Cushman and Ventilabrella Cushman. The Journal of Foraminiferal Research, 2(2), 73-92.spa
dc.relation.referencesMartínez I. R. (1989). Foraminiferal biostratigraphy and paleoenvironments of the Maastrichtian Colon mudstones of northern South America. Micropaleontology, 35(2), 97-113.spa
dc.relation.referencesMartínez, C. (2007). Foraminiferos rotálidos del Cretácico superior de la Cuenca pirenaica. Tésis de Doctorado. Universitat Autónoma de Barcelona. https://www.tdx.cat/handle/10803/3442?locale-attribute=es#page=1spa
dc.relation.referencesMaughan, E. K., Zambrano O., F., Mojica G., P., Abozaglo M., J., Pachon P., F., y Duran R., R. (1979). Paleontologic and stratigraphic relations of phosphate beds in Upper Cretaceous rocks of the Cordillera Oriental, Colombia. Instituto Nacional de Investigaciones Geológico-Mineras. USGS Numbered Series, 79-1525. https://doi.org/10.3133/ofr791525spa
dc.relation.referencesMcCourt, W. J., Aspden, J. A., y Brook, M. (1984). New geological and geochronological data from the Colombian Andes: continental growth by multiple accretion. Journal of the Geological Society, 141(5), 831-845.spa
dc.relation.referencesMichael, F. Y. (1973). Planktonic foraminifera from the Comanchean Series (Cretaceous) of Texas. The Journal of Foraminiferal Research, 2(4), 200–220. https://doi.org/10.2113/gsjfr.2.4.200spa
dc.relation.referencesMinter, N. J., Buatois, L. A., y Mángano, M. G. (2016). The Conceptual and Methodological Tools of Ichnology. In M. G. Mángano y L. A. Buatois (Eds.), The Trace-Fossil Record of Major Evolutionary Events: Volume 1: Precambrian and Paleozoic (pp. 1–26). Springer Netherlands. https://doi.org/10.1007/978-94-017-9600-2_1spa
dc.relation.referencesMolina, E. (1990). Ontogenia y tafonomía de los foraminíferos planctónicos: consecuencias en su aplicación geológica. Comunicaciones de la Reunión de Tafonomía y Fosilización, 231-236.spa
dc.relation.referencesMohamed, S. (2005). Biostratigraphie de haute résolution des foraminifères planctoniques du passage Cénomanien-Turonien et impact de l'événement anoxique EAO-2 sur ce groupe dans la marge sud de la Téthys. Exemple des régions de Jerissa et Bargou en Tunisie. Université El Manar ( Tunisie)spa
dc.relation.referencesMojica, J., y Franco, R. (1990). Estructura y Evolución Tectónica del Valle Medio y Superior del Magdalena, Colombia. Geología Colombiana, 17, 41–64. https://revistas.unal.edu.co/index.php/geocol/article/view/30633spa
dc.relation.referencesMontanaro Gallitelli, E. (1957). A revision of the foraminiferal family Heterohelicidae. Bulletin United States National Museum, 215, 133–154spa
dc.relation.referencesMoore, C. (2001). Carbonate Reservoirs: Porosity, Evolution and Diagenesis in a Sequence Stratigraphic Framework. Elsevier Science.spa
dc.relation.referencesMorales, L., CPI (1958). General Geology and Oil Occurrences of Middle Magdalena Valley, Colombia. In Habitat of Oil (pp. 641–695). American Association of Petroleum Geologists. https://doi.org/10.1306/SV18350C25spa
dc.relation.referencesMorgulis, S. (1931). Studies on the Chemical Composition of Bone Ash. Journal of Biological Chemistry, 93(2), 455–466. https://doi.org/https://doi.org/10.1016/S0021-9258(18)76453-3spa
dc.relation.referencesMornod, L. (1950). Les Globorotalides du Cretace superieur du Montsalvens (Prealpes fribourgeoises). Eclogae Geologicae Helvetiae. 42(2): 573-595spa
dc.relation.referencesMorrow, A. L. (1934). Foraminifera and ostracoda from the Upper Cretaceous of Kansas. Journal of Paleontology. 8: 186-205spa
dc.relation.referencesMount, J. (1985). Mixed siliciclastic and carbonate sediments: a proposed first‐order textural and compositional classification. Sedimentology, 32(3), 435-442.spa
dc.relation.referencesMülayim, O. (2020).Cenomanian–turonian platform evolution and records of OAE 2 on the drowned northern arabian carbonate platform (se Turkey): Integration of biostratigraphy, sequence stratigraphy, sedimentology, and stable isotopes. Ph.D. - Doctoral Program. Middle East Technical University. https://hdl.handle.net/11511/69113spa
dc.relation.referencesMülayim, O., Yılmaz, İ. Ö., Özer, S., Sarı, B., y Taslı, K. (2020). A Cenomanian–Santonian rudist–bearing carbonate platform on the northern Arabian Plate, Turkey: facies and sequence stratigraphy. Cretaceous Research, 110, 104414.spa
dc.relation.referencesMweneinda, A. (2014). Mid-Cretaceous stratigraphy and micropalaeontology of the coastal basins of Tanzania. Doctoral dissertation, Cardiff University.spa
dc.relation.referencesNakkady, S. E. (1950). A new foraminiferal fauna from the Esna shales and Upper Cretaceous chalk of Egypt. Journal of Paleontology. 24(6): 675-692.spa
dc.relation.referencesNavarrete-Parra, R.E. et al. (2019). Turonian-Campanian Foraminifera Zonation for the La Luna and Lower Umir Formations, Middle Magdalena Valley Basin, Northern Colombia. In: Cusminsky, G., Bernasconi, E., Concheyro, G. (eds) Advances in South American Micropaleontology. Springer Earth System Sciences. Springer, Cham. https://doi.org/10.1007/978-3-030-02119-1_4spa
dc.relation.referencesNavidtalab, A., Heimhofer, U., Huck, S., Omidvar, M., Rahimpour-Bonab, H., Aharipour, R., y Shakeri, A. (2019). Biochemostratigraphy of an upper Albian–Turonian succession from the southeastern Neo-Tethys margin, SW Iran. Palaeogeography, Palaeoclimatology, Palaeoecology, 533, 109255. https://doi.org/10.1016/j.palaeo.2019.109255spa
dc.relation.referencesNederbragt, A. J. (1989). Chamber proliferation in the Cretaceous planktonic foraminifera Heterohelicidae. The Journal of Foraminiferal Research, 19(2), 105-114.spa
dc.relation.referencesNederbragt, A. J. (1991). Late Cretaceous Biostratigraphy and Development of Heterohelicidae (Planktic Foraminifera). Micropaleontology, 37(4), 329–372. https://doi.org/10.2307/1485910spa
dc.relation.referencesNichols, G. (2009). Sedimentology and stratigraphy. John Wiley y Sons.spa
dc.relation.referencesNicholson, P. T., y Shaw, I. (Eds.). (2000). Ancient Egyptian materials and technology.spa
dc.relation.referencesNotestein, F., Hubman, C., y Bowler, J. (1944). Geology of the Barco Concession, Republic of Colombia, South America. GSA Bulletin, 55(10), 1165–1216. https://doi.org/10.1130/GSAB-55-1165spa
dc.relation.referencesOdin, G. S., y Fullagar, P. D. (1988). Chapter C4 Geological Significance of the Glaucony Facies. In G. S. Odln (Ed.), Green Marine Clays, 45, 295–332. Elsevier. https://doi.org/10.1016/S0070-4571(08)70069-4spa
dc.relation.referencesOdin, G. S., y Matter, A. (2003). De Glauconiarum Origine. In Sandstone Diagenesis: Recent and Ancient (pp. 121–151). John Wiley y Sons, Ltd. https://doi.org/https://doi.org/10.1002/9781444304459.ch4spa
dc.relation.referencesOdin, G. S., y Lamaurelle, M. A. (2001). The global Campanian-Maastrichtian stage boundary. Episodes Journal of International Geoscience, 24(4), 229-238.spa
dc.relation.referencesOgg, J. G., Ogg, G., y Gradstein, F. M. (2016). A concise geologic time scale: 2016. Elsevier.spa
dc.relation.referencesOkay, A. I., y Altiner, D. (2007). A condensed Mesozoic succession north of Izmir: A fragment of the Anatolide-Tauride platform in the Bornova Flysch Zone. Turkish Journal of Earth Sciences, 16(3), 257-279.spa
dc.relation.referencesOmidvar, M., Safari, A., Vaziri-Moghaddam, H., y Ghalavand, H. (2018). Foraminiferal biostratigraphy of Upper Cretaceous (Campanian–Maastrichtian) sequences in the Peri-Tethys basin; Moghan area, NW Iran. Journal of African Earth Sciences, 140, 94-113.spa
dc.relation.referencesOrabi, O. H., y Khalil, H. (2012). Late Campanian/Maastrichtian boundary at west-central Sinai, Egypt. Al-Azhar Bull. Sci, 8Th L.S.C, 1-28.spa
dc.relation.referencesOrabi, O. H., y Zahran, E. (2014). Paleotemperatures and paleodepths of the upper cretaceous rocks in El Qusaima, northeastern Sinai, Egypt. Journal of African Earth Sciences, 91, 79-88.spa
dc.relation.referencesÖzkan, R., y Altiner, D. (2019). The Cretaceous Mardin Group carbonates in southeast Turkey: Lithostratigraphy, foraminiferal biostratigraphy, microfacies and sequence stratigraphic evolution. Cretaceous Research, 98, 153-178.spa
dc.relation.referencesPacheco Sintura, P. A., Cardona Molina, A., y Cortés, F. B. (2015). Compositional characterization and storage capacity of shale samples from La Luna and Conejo Formations (Middle Magdalena basin and the Eastern Cordillera): Implications for evaluation of cretaceous shale gas in Colombia. Boletín de Ciencias de La Tierra, 37, 45–53. https://doi.org/10.15446/rbct.n37.43685spa
dc.relation.referencesPaez-Reyes, M., Carvajal-Ortiz, H., Sahoo, S. K., Varol, O., Miller, B. V., Hughes, G. W., ... y Copeland, P. (2021). Assessing the contribution of the La Luna Sea to the global sink of organic carbon during the Cenomanian-Turonian Oceanic anoxic event 2 (OAE2), Global and Planetary Change, 199, 103424. https://doi.org/10.1016/j.gloplacha.2021.103424spa
dc.relation.referencesParnaud, F., Gou, Y., Pacual, J. C., Capello, M. A., Truskowski, I., y Passalacqua, H. (1995). Stratigraphic synthesis of western Venezuela. Petroleum Basins of South America. AAPG Memoir, 62, 681-698.spa
dc.relation.referencesPatarroyo, G. D., Ceolin, D., Fauth, G., Torres, G. A., Cárdenas, C. P., y Rincón, D. A. (2019). Lower Cretaceous Benthic Foraminifers and Ostracods of the Middle Magdalena Basin, Colombia: Biostratigraphic and Paleoenvironmental Inferences. In Advances in South American Micropaleontology: Selected Papers of the 11th Argentine Paleontological Congress (pp. 21-45). Springer International Publishing.spa
dc.relation.referencesPatarroyo, G. D., Kochhann, K. G., Ceolin, D., Guerra, R. M., Alegret, L., y Bom, M. H. (2022). Paleoenvironmental changes recorded at a late Maastrichtian marine succession of northern South America. Journal of South American Earth Sciences, 119, 104015.spa
dc.relation.referencesPatarroyo, G. D., Kochhann, K. G., Guerra, R. M., Alegret, L., Ceolin, D., y Torres, J. M. (2023). Maastrichtian Microfossils of the Shallow Marine Umir Formation, Northeastern Colombia. Ameghiniana, 60(4), 297-311. https://doi.org/10.5710/AMGH.02.03.2023.3525spa
dc.relation.referencesPatarroyo, G. D., Torres, G. A., Rincón, D. A., Cárdenas, C. P., y Márquez, R. E. (2017). Bioestratigrafía e inferencias paleoambientales de las asociaciones de foraminíferos en las formaciones cretácicas La Luna-Colón (Cuenca del Catatumbo, Colombia). Boletín de Geología, 39(3), 25-40.spa
dc.relation.referencesPatarroyo, G., Torres, G., Cárdenas, C., y Rincón, D. (2015). Foraminiferal Assemblages and Palaeoenvironmental Inferences of the Lowermost Colon Formation (Late Campanian): Catatumbo Basin, Colombia. AAPG Latin America and Caribbean Región, 20th Caribbean Geological Conference.spa
dc.relation.referencesPerez-Infante, J., Farrimond, P., y Furrer, M. (1996). Global and local controls influencing the deposition of the La Luna Formation (Cenomanian-Campanian), western Venezuela. Chemical Geology, 130(3), 271–288. https://doi.org/https://doi.org/10.1016/0009-2541(96)00019-8spa
dc.relation.referencesPérez-Rodríguez, I. (2013). Biocronoestratigrafía y evolución ambiental del Coniaciense Superior al Maastrichtiense con foraminíferos planctónicos. Tesis doctoral, Univ. de Zaragoza, 350 p. https://dialnet.unirioja.es/servlet/tesis?codigo=84018&orden=1&info=linkspa
dc.relation.referencesPérez-Rodríguez, I., Lees, J. A., Larrasoaña, J. C., Arz, J. A., y Arenillas, I. (2012). Planktonic foraminiferal and calcareous nannofossil biostratigraphy and magnetostratigraphy of the uppermost Campanian and Maastrichtian at Zumaia, northern Spain. Cretaceous Research, 37, 100-126.spa
dc.relation.referencesPessagno, E. A. (1967). Upper Cretaceous planktonic foraminifera from the western Gulf Coastal Plain. Palaeontographica Americana, 5, 245-445.spa
dc.relation.referencesPessagno, E. A., 1960. Stratigraphy and micropaleontology of the Cretaceous and lower Tertiary of Puerto Rico. Micropaleontology, 6, 87–110.spa
dc.relation.referencesPetrizzo, M. R. y Huber, B. T. (2006). Biostratigraphy and taxonomy of late Albian planktonic foraminifera from ODP Leg 171B (western North Atlantic Ocean). Journal of Foraminiferal Research, 36, 166-190.spa
dc.relation.referencesPetrizzo, M. R., y Gilardoni, S. E. (2020). Planktonic foraminiferal biostratigraphy of late Albian-Cenomanian pelagic sequences from the Umbria-Marche basin (central Italy) and the Mazagan Plateau (northeast Atlantic Ocean). Rivista italiana di Paleontologia e Stratigrafia, 126(3), 865-904.spa
dc.relation.referencesPetrizzo, M. R., Jiménez Berrocoso, Á., Falzoni, F., Huber, B. T., y Macleod, K. G. (2017). The Coniacian–Santonian sedimentary record in southern Tanzania (Ruvuma Basin, East Africa): Planktonic foraminiferal evolutionary, geochemical and palaeoceanographic patterns. Sedimentology, 64(1), 252-285.spa
dc.relation.referencesPetrizzo, M. R., Watkins, D. K., MacLeod, K. G., Hasegawa, T., Huber, B. T., Batenburg, S. J., y Kato, T. (2021). Exploring the paleoceanographic changes registered by planktonic foraminifera across the Cenomanian-Turonian boundary interval and Oceanic Anoxic Event 2 at southern high latitudes in the Mentelle Basin (SE Indian Ocean). Global and Planetary Change, 206, 103595.spa
dc.relation.referencesPetters, S. W. (1977). Upper Cretaceous planktonic foraminifera from the subsurface of the Atlantic Coastal Plain of New Jersey. The Journal of Foraminiferal Research, 7(3), 165-187.spa
dc.relation.referencesPetters, S. W. (1983). Gulf of Guinea planktonic foraminiferal biochronology and geological history of the South Atlantic. The Journal of Foraminiferal Research, 13(1), 32-59.spa
dc.relation.referencesPetters, V. (1954a). Tertiary and upper Cretaceous foraminifera from Colombia, South America. Contributions from the Cushman Foundation for Foraminiferal Research, 5(1), 37–41.spa
dc.relation.referencesPetters, V. (1954b). Typical foraminiferal horizons in the Lower Cretaceous of Colombia, SA. Cushman Foundation for Foraminiferal Research Contributions, 5, 128–137.spa
dc.relation.referencesPetters, V. (1955). Development of Upper Cretaceous foraminiferal faunas in Colombia. Journal of Paleontology, 212-225.spa
dc.relation.referencesPettijohn, F. J., y Potter, P. E. (1964). Classification of primary sedimentary structures. In Atlas and Glossary of Primary Sedimentary Structures (pp. 3–9). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-94899-2_3spa
dc.relation.referencesPindell, J., y Dewey, J. F. (1982). Permo‐Triassic reconstruction of western Pangea and the evolution of the Gulf of Mexico/Caribbean region. Tectonics, 1(2), 179-211.spa
dc.relation.referencesPlummer, H. J. (1927). Foraminifera of the Midway Formation in Texas. University of Texas Bulletin, 2644, 1-206spa
dc.relation.referencesPlummer, H. J. (1931). Some Cretaceous foraminifera in Texas. University of Texas Bulletin. 3101, 109-203.spa
dc.relation.referencesPorthault, B. (1978). Foraminifères caractéristiques du Cénomanien à faciès pélagique dans le Sud-Est de la France. Géologie Méditerranéenne, 5(1), 183-194.spa
dc.relation.referencesPostuma, J. A. (1971). Manual of planktonic foraminifera. Elsevier, 1-420.spa
dc.relation.referencesPremoli Silva, I. y Verga, D. (2004). Practical manual of Cretaceous planktonic foraminifera. International School on Planctonic foraminifera, 3º Course: Cretaceous.spa
dc.relation.referencesPremoli Silva, I. y Verga, D. (2011). Practical manual of Cretaceous planktonic foraminifera. International School on Planctonic foraminifera, 3º Course: Cretaceous. New Editing.spa
dc.relation.referencesPremoli, S. I. y Bolli, H. (1973). Late Cretaceous to Eocene planktonic foraminifera and stratigraphy of Leg 15 sites in the Caribbean Sea. Initial reports of deep sea drilling project, 15, 449-547.spa
dc.relation.referencesPrince, M., Sánchez, C., Rojas, D., Acevedo, R., y Daza, D. (2011). La Formación Umir en el sector norte de la cuenca del Valle Medio del Magdalena: Una nueva frontera exploratoria en una cuenca madura. In Memorias XVI Congreso Latinoamericano de Geología y XIII Congreso Colombiano de Geología. Medellín, Colombia (pp. 117-118).spa
dc.relation.referencesRamírez. R., Guzmán, G., Torres. A. (2013). Descripción Sedimentológica de Núcleos de Perforación para el Programa de Yacimientos No Convencionales Pozo PMM 01. Génesis, Consultoría en Geología. Informe Interno.spa
dc.relation.referencesRangel, A., Parra, P., y Niño, C. (2000). The La Luna formation: chemostratigraphy and organic facies in the Middle Magdalena Basin. Organic Geochemistry, 31(12), 1267–1284. https://doi.org/10.1016/S0146-6380(00)00127-3spa
dc.relation.referencesRead, J. F. (1985). Carbonate Platform Facies Models 1. AAPG Bulletin, 69(1), 1–21. https://doi.org/10.1306/AD461B79-16F7-11D7-8645000102C1865Dspa
dc.relation.referencesRehman, S. U., Ahsan, N., Shah, M. M., Munawar, M. J., Miraj, M. A. F., Rehman, F., y Mahmood, K. (2021). Depositional environments and microfacies of the upper Turonian–Maastrichtian Kawagarh Formation, Kalachitta Range, Lesser Himalayas, Pakistan. Australian Journal of Earth Sciences, 68(7), 1017–1030. https://doi.org/10.1080/08120099.2021.1889662spa
dc.relation.referencesRehman, T. P., y Wright, V. P. (1992). Carbonate ramp depositional systems. Sedimentary Geology, 79(1), 3–57. https://doi.org/10.1016/0037-0738(92)90003-Aspa
dc.relation.referencesReichel, M. (1950). Observations sur les Globotruncana du gisement de la Breggia (Tessin). Eclogae Geologicae Helvetiae, 42, 591-617spa
dc.relation.referencesRemin, Z., Dubicka, Z., Kozłowska, A., y Kuchta, B. (2012). A new method of rock disintegration and foraminiferal extraction with the use of liquid nitrogen [LN2]. Do conventional methods lead to biased paleoecological and paleoenviromental interpretations?. Marine Micropaleontology, 86, 11-14.spa
dc.relation.referencesRenz, O. (1936). Stratigraphische und mikropalaeontologische Untersuchung der Scaglia (Obere Kreide-Tertiar) im zentralen Apennin. Eclogae Geologicae Helvetiae, 29(1), 1-149spa
dc.relation.referencesRenz, O., Luterbacher, H. y Schneider, A. (1963). Stratigraphisch-palaontologische Untersuchungen im Albien und Cenomanien des Neuenburger Jura. Eclogae Geologicae Helvetiae, 56(2), 1073-1116.spa
dc.relation.referencesRestrepo-Pace, P. A., Colmenares, F., Higuera, C., y Mayorga, M. (2004). A Fold-and-thrust belt along the western flank of the Eastern Cordillera of Colombia— Style, kinematics, and timing constraints derived from seismic data and detailed surface mapping. In Thrust Tectonics and Hydrocarbon Systems. American Association of Petroleum Geologists. https://doi.org/10.1306/M82813C31spa
dc.relation.referencesReuss, A. E. (1845). Die Versteinerungen der böhmischen Kreide-formation. E. Schweizebart, Stuttgart. 1-58.spa
dc.relation.referencesRivera, H., Le Roux J. P., Barragán, J.C., Mariño-Martinez, J.E. (2018). Rampa mixta dominada por tormentas: modelo depositacional de la sucesión de black shales cretácico de la cuenca cordillera oriental, Colombia. Revista Norandina, 14(6), 29-30.spa
dc.relation.referencesRobaszynski, F, Caron, M., Gonzalez Donoso J.M., Wonders A. (1984). Atlas of late Cretaceous globotruncanids. Rev. Micropaleont., 26, 145-305.spa
dc.relation.referencesRobaszynski, F., Caron, M., Gonzales Donoso, J. M., Wonders, A. A. H. y the European Working Group on Planktonic Foraminifera (1984). Atlas of Late Cretaceous globotruncanids. Revue de Micropaléontologie, 26(3-4), 145-305spa
dc.relation.referencesRobaszynski, F., Zagrarni, M. F., Caron, M., y Amedro, F. (2010). The global bio-events at the Cenomanian-Turonian transition in the reduced Bahloul Formation of Bou Ghanem (central Tunisia). Cretaceous Research, 31(1), 1-15.spa
dc.relation.referencesRoss, M. I., y Scotese, C. R. (1988). A hierarchical tectonic model of the Gulf of Mexico and Caribbean region. Tectonophysics, 155(1-4), 139-168.spa
dc.relation.referencesSánchez, J., Horton, B. K., Tesón, E., Mora, A., Ketcham, R. A., y Stockli, D. F. (2012). Kinematic evolution of Andean fold-thrust structures along the boundary between the Eastern Cordillera and Middle Magdalena Valley basin, Colombia. Tectonics, 31(3). https://doi.org/10.1029/2011TC003089spa
dc.relation.referencesSari, B. (2006). Upper Cretaceous planktonic foraminiferal biostratigraphy of the Bey Daglari Autochthon in the Korkuteli area, western Taurides, Turkey. Journal of Foraminiferal Research, 36(3).spa
dc.relation.referencesSari, B. (2017). Lithostratigraphy and planktonic foraminifera of the uppermost Cretaceous-Upper Paleocene strata of the Tavas nappe of the Lycian nappes (SW Turkey). Geologia Croatica, 70(3), 163-177.spa
dc.relation.referencesSarmiento - Pérez, G., Puentes, J., y Sierra, C. (2015a). Estratigrafía y Petrofacies de la Formación La Luna en el Sinclinal de Nuevo Mundo, Valle Medio del Magdalena. Geología Norandina, 12(4), 21–40.spa
dc.relation.referencesSarmiento - Pérez, G., Puentes, J., y Sierra, C. (2015b). Evolución Geológica y Estratigrafía del Sector Norte del Valle Medio del Magdalena. Geología Norandina, 12(1), 51-82.spa
dc.relation.referencesSarmiento-Rojas, L. F. (2011). Llanos Basin. In F. Cediel y G. Ojeda (Eds.), Petroleum Geology of Colombia (p. 177). University EAFIT.spa
dc.relation.referencesSarmiento-Rojas, L. F., Van Wess, J. D., y Cloetingh, S. (2006). Mesozoic transtensional basin history of the Eastern Cordillera, Colombian Andes: Inferences from tectonic models. Journal of South American Earth Sciences, 21(4), 383–411. https://doi.org/10.1016/j.jsames.2006.07.003spa
dc.relation.referencesSawlowicz, Z. (1993). Pyrite framboids and their development: a new conceptual mechanism. Geologische Rundschau, 82(1), 148–156. https://doi.org/10.1007/BF00563277spa
dc.relation.referencesSawyer, M. S. (2016). Foraminiferal Biostratigraphy in Proximity to the Albian/Cenomanian Boundary using Six Global Deep Sea Drilling Project Sites. Master's thesis.spa
dc.relation.referencesSchmid, R. (1981). Descriptive nomenclature and classification of pyroclastic deposits and fragments: Recommendations of the IUGS Subcommission on the Systematics of Igneous Rocks. Geologische Rundschau, 70, 794-799.spa
dc.relation.referencesScholle, P. A., Bebout, D. G., & Moore, C. H. (Eds.). (1983). Carbonate depositional environments: AAPG Memoir 33. AAPG.spa
dc.relation.referencesScholle, P. A., y Ulmer-Scholle, D. S. (2003). A Color Guide to the Petrography of Carbonate Rocks: Grains, textures, porosity, diagenesis. American Association of Petroleum Geologists. https://doi.org/10.1306/M77973spa
dc.relation.referencesSeferinov, S. (2017). Family Globigerinidae Carpenter, Parker and Jones, 1862 from the Paleocene and Eocene in Lom Depression. Review of the Bulgarian Geological Society, 78, 73-95.spa
dc.relation.referencesSigal, J. (1948). Notes sur les genres de foraminiferes Rotalipora Brotzen 1942 et Thalmanninella Famille des Globorotaliidae. Revue de l'Institut Francaise du Pétrole, 3(4), 95-103.spa
dc.relation.referencesSigal, J. (1952). Apercu stratigraphique sur la micropaleontologie du Cretace. XIX Congr. géol. internat., Algers, Monographies Regionales. 1(26): 3-43spa
dc.relation.referencesSigal, J. (1956). Notes micropaléontologiques nord-africaines. 4. Biticinella breggiensis (Gandolfi) nouveau morphogenre. Société Géologique De France, C. R. Des Séances, 3, 35–37spa
dc.relation.referencesSigal, J. (1966). Contribution á une monographie des Rosalines. I. Le genre Ticinella Reichel, souche des Rotalipores. Eclogae Geologicae Helvetiae. 59: 185-217.spa
dc.relation.referencesSilva, I. P., Caron, M., Leckie, R. M., Petrizzo, M. R., Soldan, D., y Verga, D. (2009). Paraticinella n. gen. and taxonomic revision of Ticinella bejaouaensis Sigal, 1966. Journal of Foraminiferal Research, 39(2), 126-137.spa
dc.relation.referencesSilva, I. P., Spezzaferri, S., y D'angelantonio, A. (1998). Cretaceous foraminiferal bio-isotope stratigraphy of Hole 967E and Paleogene planktonic foraminiferal biostratigraphy of Hole 966F, eastern Mediterranean. In Proceedings of the Ocean Drilling Program. Scientific results, 160, 377-394).spa
dc.relation.referencesSliter, W. V. (1973). Upper Cretaceous foraminifers from the Vancouver Island area, British Columbia, Canada. The Journal of Foraminiferal Research, 3(4), 167-186.spa
dc.relation.referencesSliter, W. V. (1989). Biostratigraphic zonation for Cretaceous planktonic foraminifers examined in thin section. Journal of Foraminiferal Research, 19(1), 1–19. https://doi.org/10.2113/gsjfr.19.1.1spa
dc.relation.referencesSliter, W. V. (1992). Cretaceous planktonic foraminiferal biostratigraphy and paleoceanographic events in the Pacific Ocean with emphasis on indurated sediment. In Ishizaki, K., Saito, T. (Eds.). Centenary of Japanese Micropaleontology, 281-99. Terra Scientific Publiching Company, Tokyo, 281-299.spa
dc.relation.referencesSliter, W. V. (1999). Cretaceous planktic foraminiferal biostratigraphy of the Calera Limestone, northern California, USA. The Journal of Foraminiferal Research, 29(4), 318-339.spa
dc.relation.referencesSmith, C. C. y Pessagno, E. A. (1973). Planktonic foraminifera and stratigraphy of the Corsicana formation (Maestrichtian) North-central Texas. Cushman Foundation for Foraminiferal Research, Special Publication, 12, 1-67.spa
dc.relation.referencesSorkhabi, R. (2017). Petroleum Industry. In: Sorkhabi, R. (eds) Encyclopedia of Petroleum Geoscience. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-02330-4_19-1spa
dc.relation.referencesSubbotina, N. N. (1949). Микрофауна меловых отложений южного склона Кавказа [Microfauna from the Cretaceous of the southern slope of the Caucasus]. Trudy vnigri Mikrofauna USSR, 34, 5-36spa
dc.relation.referencesSubbotina, N. N. (1959). Planktonic foraminifera. In, Rauzer-Chernousova, D. M. y Fursenko, A. V. (eds) Principles of paleontology, part 1, Protozoa. Akademia Nauk SSSR, Moscow 1-368.spa
dc.relation.referencesTappan, H. (1940). Foraminifera from the Grayson formation of Northern Texas. Journal of Paleontology. 14(2): 93-126.spa
dc.relation.referencesTappan, H. (1943). Foraminifera from the Duck Creek formation of Oklahoma and Texas. Journal of Paleontology, 17(5), 467-517spa
dc.relation.referencesTchegliakova, N. (1993): Los Foraminíferos y Minerales autigénicos de la Formación Umir (Sección Quebrada La Julia, Valle Medio del Magdalena): Registro de una Laguna costera a finales del Cretácico Superior (Maestrichtiano). Geologia Colombiana, 18, 107 – 117.spa
dc.relation.referencesTchegliakova, N. (1995). Los Foraminíferos de la Formación Umir (Sección Quebrada La Julia): Registro del Cretácico Superior cuspidal (Maastrichtiano) en el Valle Medio del Magdalena, Colombia. Geología Colombiana, 19, 109-130.spa
dc.relation.referencesTchegliakova, N. (1996). Registro de las biozonas de foraminíferos planctónicos Gansserina gansseri y Abathomphalus mayaroensis (maastrchtiano medio y superior) en el extremo meridional del Valle Medio del Magdalena (Colombia, Sur América). Geología Colombiana, 20, 67-80.spa
dc.relation.referencesTchegliakova, N., y Mojica, J. (2001). El Senoniano de la barrera de Girardot-Guataquí, Valle Alto del Magdalena, Colombia: Precisiones sobre la estratigrafía y establecimiento de una zonación micropaleontológica. Revista de la Academia Colombiana de Ciencias Exáctas, Físicas y Naturales, 25(94), 37-76.spa
dc.relation.referencesTchegliakova, N., y Pérez, V. (1995). Registro de la Zona bioestratigráfica Dicarinella concavata (Foraminiferida) en el Extremo noroccidental de Suramérica (Colombia). Geología Colombiana, 19, 131-143.spa
dc.relation.referencesTchegliakova, N., Sarmiento, G., y Guerrero, J. (1997). Bioestratigrafía y paleoecología de los foraminíferos bentónicos de la formación chipaque y el grupo guadalupe. turoniano maastrichtiano del piedemonte llanero de los andes colombianos. Geología Colombiana, 22, 103-119.spa
dc.relation.referencesTeichert, C. (1958). Concepts of Facies. AAPG Bulletin, 42(11), 2718–2744. https://doi.org/10.1306/0BDA5C0C-16BD-11D7-8645000102C1865Dspa
dc.relation.referencesTerraza Melo, Roberto. (2019). “ʻFormación La Luna”: expresión espuria en la geología colombiana”. En Estudios geológicos y paleontológicos sobre el Cretácico en la región del embalse del río Sogamoso, Valle Medio del Magdalena, dirección científica y edición de Fernando Etayo-Serna. Compilación de los Estudios Geológicos Oficiales en Colombia vol. XXIII. Bogotá: Servicio Geológico Colombiano.spa
dc.relation.referencesTrujillo, E. F. (1960). Upper Cretaceous foraminifera from near Redding, Shasta County, California. Journal of Paleontology, 34, 290-346.spa
dc.relation.referencesTruskowski, I., Galea-Álvarez, F., y Sliter, W. (1996). Late Cretaceous biostratigraphy of the La Luna Formation, Maracaibo basin. AAPG Bulletin, 80(8).spa
dc.relation.referencesUlmer-Scholle, D. S., Scholle, P. A., Schieber, J., y Raine, R. J. (2015). A Color Guide to the Petrography of Sandstones, Siltstones, Shales and Associated Rocks. American Association of Petroleum Geologists. https://doi.org/10.1306/M1091304spa
dc.relation.referencesUseche, F., Barragán, R., Moreno-Bedmar, J., y Canet, C. (2014). Mexican archives for the major Cretaceous Oceanic Anoxic Events. Boletin de La Sociedad Geologica Mexicana, 66, 491–501. https://doi.org/10.18268/BSGM2014v66n3a7spa
dc.relation.referencesVan Houten, F. B., y Travis, R. B. (1968). Cenozoic deposits, upper Magdalena valley, Colombia. AAPG bulletin, 52(4), 675-702.spa
dc.relation.referencesVélez, L. (2014). Estratigrafía de la Formación La Luna en el Valle Medio del Magdalena. Universidad Nacional de Colombia. (Trabajo de grado).spa
dc.relation.referencesVenkatachalapthy, R., y Harini, L. (2019). Cenomanian planktic foraminiferal biostratigraphy of Southern India and their correlation. Journal of the Palaeontological Society of India, 64(1), 107-114.spa
dc.relation.referencesVillamil, T. (2003). Regional hydrocarbon systems of Colombia and western Venezuela: Their origin, potential, and exploration, in C. Bartolini, R. T. Buffler, and J. Blickwede, eds., The Circum-Gulf of Mexico and the Caribbean: Hydrocarbon habitats, basin formation, and plate tectonics. AAPG Memoir 79, p. 697–734. https://doi.org/10.1306/M79877C32spa
dc.relation.referencesVillamil, T., y Arango, C. (1998). Integrated Stratigraphy of Latest Cenomanian and Early Turonian Facies of Colombia. In Paleogeographic Evolution and Non-Glacial Eustasy, Northern South America. SEPM Society for Sedimentary Geology. 58. https://doi.org/10.2110/pec.98.58.0129spa
dc.relation.referencesVillamil, T., Arango, C., y Hay, W. W. (1999). Plate tectonic paleoceanographic hypothesis for Cretaceous source rocks and cherts of northern South America. In Barrera, E. y Johnson C. Evolution of the Cretaceous Ocean-Climate System. Geological Society of America. p. 191-202. https://doi.org/10.1130/0-8137-2332-9.191spa
dc.relation.referencesVoorwijk, G. H. (1937). Foraminifera from the Upper Cretaceous of Habana, Cuba. Proceedings of the Koninklijke Nederlandse Akademie van Wetenschappen, 40, 190-198.spa
dc.relation.referencesWalaszczyk, I., Čech, S., Crampton, J. S., Dubicka, Z., Ifrim, C., Jarvis, I., ... y Toshimitsu, S. (2022). The global boundary stratotype section and point (GSSP) for the base of the Coniacian Stage (Salzgitter-Salder, Germany) and its auxiliary sections (Słupia Nadbrzeżna, central Poland; Střeleč, Czech Republic; and El Rosario, NE Mexico). IUGS. Episodes, 45(2), 181-220. https://doi.org/10.18814/epiiugs/2021/021022spa
dc.relation.referencesWalaszczyk, I., Kopaevich, L., y Benyamovskiy, V. (2013). Inoceramid and foraminiferal record and biozonation of the Turonian and Coniacian (Upper Cretaceous) of the Mangyshlak Mts., western Kazakhstan. Acta Geologica Polonica, 63. https://doi.org/10.2478/agp-2013-0020spa
dc.relation.referencesWalaszczyk, I., Kopaevich, L., y Olferiev, A. G. (2004). Inoceramid/foraminiferal succession of the Turonian and Coniacian (Upper Cretaceous) of the Briansk region (Central European Russia). Acta Geologica Polonica, 54, 597–609.spa
dc.relation.referencesWalaszczyk, I., Lees, J., Peryt, D., Cobban, W., y Wood, C. (2012). Testing the congruence of the macrofossil versus microfossil record in the Turonian-Coniacian boundary succession of the Wagon Mound-Springer composite section (NE New Mexico, USA). Acta Geologica Polonica, 62, 581–594. https://doi.org/10.2478/v10263-012-0031-xspa
dc.relation.referencesWard, D. E., Goldsmith, R., Cruz B., J., y Restrepo A., H. (1973). Geología de los cuadrángulos H-12 Bucaramanga y H-13 Pamplona, departamento de Santander. Boletín Geológico, 21(1-3), 1–134. https://doi.org/10.32685/0120-1425/bolgeol21.1-3.1973.383spa
dc.relation.referencesWentworth, C. K. (1922). A scale of grade and class terms for clastic sediments. The journal of geology, 30(5), 377-392.spa
dc.relation.referencesWheeler, O. C. (1929). Report on the Palmira Series with notes on stratigraphy of the Umir, Lisama y La Paz Formations near the eastern part of De Mares Concession. Informe Geológico, 37.spa
dc.relation.referencesWhite, C. D., Novakovic, D., Dutton, S. P., y Willis, B. J. (2003). A Geostatistical Model for Calcite Concretions in Sandstone. Mathematical Geology, 35(5), 549–575. https://doi.org/10.1023/A:1026282602013spa
dc.relation.referencesWright, V. P. (1992). A revised classification of limestones. Sedimentary Geology, 76(3), 177–185. https://doi.org/10.1016/0037-0738(92)90082-3spa
dc.relation.referencesYoung, J.R., Wade, B.S., y Huber B.T. (eds) pforams@mikrotax website. 2017. Consultada en 2023. URL: http://www.mikrotax.org/pforamsspa
dc.relation.referencesZambrano, F. (1969). Composición de las fosforitas marinas del área La Azufrada (Santander). Servicio Geológico Colombiano, 20-22.spa
dc.relation.referencesZapata, E., Lorente, M. A., Rey, O., y Padrón, V. (2000). Diagenetic evaluation of La Luna Formation at Tachira and Mérida states, western Venezuela. SEPM Research Conference. Paleogeography and Hydrocarbon Potential of the La Luna Formation and Related Cretaceous Anoxic Systems, 1–7.spa
dc.rights.accessrightsinfo:eu-repo/semantics/openAccessspa
dc.rights.licenseAtribución-NoComercial-CompartirIgual 4.0 Internacionalspa
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/spa
dc.subject.ddc550 - Ciencias de la tierra::551 - Geología, hidrología, meteorologíaspa
dc.subject.lembESTRATIGRAFIAspa
dc.subject.lembGeology, Stratigraphiceng
dc.subject.lembFORAMINIFEROSspa
dc.subject.lembForaminiferaeng
dc.subject.lembFORAMINIFEROS FOSILESspa
dc.subject.lembForaminifera, fossileng
dc.subject.lembROCAS SEDIMENTARIASspa
dc.subject.lembRocks, sedimentaryeng
dc.subject.lembPETROLOGIAspa
dc.subject.lembPetrologyeng
dc.subject.lembCRISTALOGRAFIAspa
dc.subject.lembCrystallographyeng
dc.subject.proposalValle Medio del Magdalenaspa
dc.subject.proposalForaminíferos planctónicosspa
dc.subject.proposalFormación La Lunaspa
dc.subject.proposalMiembro Saladaspa
dc.subject.proposalMiembro Pujamanaspa
dc.subject.proposalMiembro Galembospa
dc.subject.proposalTaxonomíaspa
dc.subject.proposalCenomanianospa
dc.subject.proposalTuronianospa
dc.subject.proposalConiacianospa
dc.subject.proposalSantonianospa
dc.subject.proposalCampanianospa
dc.subject.proposalMaastrichtianospa
dc.subject.proposalColombiaspa
dc.subject.proposalMiddle Magdalena Valleyeng
dc.subject.proposalPlanktonic foraminiferaeng
dc.subject.proposalLa Luna Formationeng
dc.subject.proposalSalada Membereng
dc.subject.proposalPujamana Membereng
dc.subject.proposalTaxonomyeng
dc.subject.proposalCenomanianeng
dc.subject.proposalTuronianeng
dc.subject.proposalSantonianeng
dc.subject.proposalCampanianeng
dc.subject.proposalMaastrichtianeng
dc.titleBioestratigrafía con foraminíferos planctónicos y microfacies en rocas de Albiano medio a Maastrichtiano del núcleo A, Valle Medio del Magdalena, Colombia : un enfoque taxonómico y paleoambientalspa
dc.title.translatedPlanktonic foraminiferal biostratigraphy and microfacies in middle Albian to Maastrichtian rocks of core A, middle Magdalena Valley, Colombia : a taxonomic and paleoenvironmental approacheng
dc.typeTrabajo de grado - Maestríaspa
dc.type.coarhttp://purl.org/coar/resource_type/c_bdccspa
dc.type.coarversionhttp://purl.org/coar/version/c_ab4af688f83e57aaspa
dc.type.contentTextspa
dc.type.driverinfo:eu-repo/semantics/masterThesisspa
dc.type.redcolhttp://purl.org/redcol/resource_type/TMspa
dc.type.versioninfo:eu-repo/semantics/acceptedVersionspa
dcterms.audience.professionaldevelopmentEstudiantesspa
dcterms.audience.professionaldevelopmentInvestigadoresspa
dcterms.audience.professionaldevelopmentMaestrosspa
dcterms.audience.professionaldevelopmentProveedores de ayuda financiera para estudiantesspa
dcterms.audience.professionaldevelopmentPúblico generalspa
oaire.accessrightshttp://purl.org/coar/access_right/c_abf2spa

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