Carbonate microfacies of the San Juan Formation (Ordovician: Oepikodus evae and Oepikodus intermedius conodont zones), Niquivil, Central Precordillera, Province of San Juan (Argentina)
DOI:
https://doi.org/10.21701/bolgeomin.128.1.007Keywords:
carbonate, Floian, microfacies, Niquivil, PrecordilleraAbstract
This contribution presents the description and interpretation of carbonate microfacies of the San Juan Formation (Ordovician) at the Niquivil section, considering the stratigraphical interval between the Oepikodus evae and Oepikodus intermedius conodont zones. The distribution of the microfacies and the conodonts assemblages allow us to identify different sub-environments within the late Floian carbonate ramp of the Central Precordillera. Five microfacies were recognized from the base to the top: M1 Bioclastic mudstone-wackestone; M2 Bioclastic-peloidal wackestone; M3 Intra-bioclastic wackestone; M4 Intra-bioclastic packstone; M5 Peloidal grainstone. The vertical distribution of these microfacies indicates a shallowing trend of the carbonate ramp in the Niquivil section for this temporal interval, which suggests a middle ramp environment with low energy, without wave action, and that evolved towards the middle-inner ramp environment with more energy by wave action and development of tempestites.
Downloads
References
Albanesi, G. 1998. Taxonomía de conodontes de las secuencias ordovícicas del Cerro Potrerillo, Precordillera Central de San Juan, República Argentina. Academia Nacional de Ciencias, Córdoba, 12, 99-253.
Albanesi, G. y Carrera, M. 2001. Niquivil Section of Central Precordillera, Argentina. Proposed as the Global Stratotype for the base of the Middle Ordovician Series. Geological Society of America Annual Meeting, Boston. Abstracts, A446.
Albanesi, G., Carrera, M., Cañas, F. y Saltzman, M. 2003. The Niquivil Section, Precordillera of San Juan, Argentina. Proposed GSSP for the Lower/Middle Ordovician boundary. In G. Albanesi, M. Beresi and S. Peralta (eds). Ordovician from the Andes. Proceedings of the 9th International Symposium on the Ordovician System, San Juan, Argentina. Serie de Correlación Geológica, 17, 33-40.
Albanesi, G., Carrera, M., Cañas, F. y Saltzman, M. 2006. A proposed Global Boundary Stratotype Section and Point for the base of the Middle Ordovician Series: The Niquivil section, Precordillera of San Juan, Argentina. Episodes, Beijing, 29 (1), 1-15. https://doi.org/10.18814/epiiugs/2006/v29i1/001
Bagnoli, G. y Stouge, S. 1997. Lower Ordovician (Billingenian-Kunda) conodont zonation and provinces based on sections from Horns Udde, NothÖland, Sweden. Bollettino de lla Società Paleontologica Italiana, 35 (2), 109-163.
Baldis, B. y Chebli, G. 1969. Estructura profunda del área central de la Precordillera sanjuanina. IV Jornadas Geológicas Argentinas, Actas, 47-66.
Baldis, B. y Beresi, M. 1981. Biofacies de culminación del ciclo deposicional calcáreo del Arenigiano en el Oeste de Argentina. Anais do II Congreso Latinoamericano de Paleontología, Porto Alegre, Brazil, 2, 11-16.
Baldis, B., Beresi, M., Bordonaro, O. y Vaca, A. 1982. Síntesis evolutiva de la Precordillera Argentina. V Congreso Latinoamericano de Geología, 4, 399-445.
Benedetto, J. 1998. Early Paleozoic brachiopods and associated shelly faunas from western Gondwana: their bearing on the geodynamic history of the pre-Andean margin. In: Pankhurst, R.J. and Rapela, C.W. (eds.), The Proto-Andean Margin of Gondwana. Geological Society of London, Special Publication, 142, 57-83. https://doi.org/10.1144/GSL.SP.1998.142.01.04
Benedetto, J. 2002. The Ordovician brachiopod faunas of Argentina: Chronology and biostratigraphic succession. In: Aceñolaza, G. (ed.), Aspects on the Ordovician System of Argentina. Instituto Superior de Correlación Geológica, Universidad Nacional de Tucumán. Serie Correlación Geológica, 16, 87-106.
Beresi, M.S., Cabaleri, N.G., Buitrón Sánchez, B.E., Rodríguez, M.C., Heredia, S.E. y Tortello, M.F. 2012. Microfacies, biota y paleoambientes sedimentarios del Ordovícico temprano-medio del Cerro Salazar, Sonora Central, México. Revista Mexicana de Ciencias Geológicas, 29, 330-345.
Cabaleri, N., Armella, C., Cagnoni, M., Panarello, H., Ramos, A. y Valencio, S. 2002. Microfacies y condiciones paleoambientales durante la depositación de la sección superior de la Formación San Juan (Llanvirniano temprano) en la región de Huaco, San Juan, Argentina. XV Congreso Geológico Argentino, 776-781.
Cañas, F. 1995. Early Ordovician Carbonate platform facies of the Argentine Precordillera: restricted shelf to open platform evolution. In: Fullerton, Cooper, J.D., Drosser, M.K. and Finney, S.C. (eds.), VII International Symposium on the Ordovician System. Book 77, Society for Sedimentary Geology, Fullerton, California, 221-224.
Cañas, F. 1999. Facies and sequences of late Cambian-early Ordovician carbonates of the Argentina Precordillera: A stratigraphic comparation with Laurentia plataforms. In: Keppie, D. and Ramos, V. (eds.), Laurentia-Gondwana connections before Pangea. Geological Society of America Special paper, 336, 43-62. https://doi.org/10.1130/0-8137-2336-1.43
Cañas, F. 2002. Selected sections of Lower to Middle Ordovician carbonate sedimentation of the Argentine Precordillera: The La Silla and San Juan formations at Cerros La Silla and Niquivil. Miscelánea, 8, 5-20.
Cañas, F. y Carrera, M. 2003. Precordilleran reefs. In: Benedetto, J.L. (ed.), Ordovician Fossils of Argentina. Secretaría de Ciencia y Tecnología, Universidad Nacional de Córdoba, Córdoba, 131-142.
Carlorosi, J., Heredia, S. y Aceñolaza, G. 2013. Middle Ordovician (early Dapingian) conodonts in the Central Andean Basin of NW Argentina. Alcheringa, 37, 1-13. https://doi.org/10.1080/03115518.2013.744240
Carrera, M. 2001. Análisis de la distribución y comparación de las biofacies de la Formación San Juan (Ordovícico temprano), Precordillera Argentina. Ameghiniana, 38, 169-184.
Cech, N. y Carrera, M. 2002. Dinámica de las comunidades arenigianas de la Formación San Juan (Ordovícico), Precordillera argentina. Ameghiniana, 39, 21-40.
Cooper, B. 1981. Early Ordovician conodonts from the Horn Valley Siltstone, central Australia. Palaeontology, 24 (1), 147-183.
Di Paola, E. y Spiegelman, A. 1984. Facies glauconíticas de formaciones terciarias y cretácicas de la Cuenca Malvinas, Argentina. IX Congreso Geológico Argentino, S.C. de Bariloche, 5, 285-298.
Dunham, R.J. 1962. Classification of carbonate rocks according to depositional texture. American Association of Petroleum Geologists, Memoir 1, 108-121.
Embry, A.F. y Klovan, J. E. 1971. Absolute water depth limits of Late Devonian paleoecological zones. Geologische Rundschau, 61, 672-686. https://doi.org/10.1007/BF01896340
Epstein, A.G., Epstein, J.P. y Harris, L. 1977. Conodont Alteration - An Index to Organic Metamorphism. United State Geological Survey Professional Paper, 995, 1-27. https://doi.org/10.3133/pp995
Fernández-Bastero, S., Velo, A., García, T., Gago-Duport, L., Santos, A., García-Gil, S. y Vilas, F. 2000. Las glauconitas de la plataforma continental gallega: Indicadores geoquímicos del grado de evolución. Journal of Iberian Geology, 26, 233-247.
Folk, R. 1962. Spectral subdivision of limestone type. American Association of Petroleum Geologists, Memoir 1, 62-84.
Flügel, E. 2010. Microfacies of Carbonate Rocks. Analysis, Interpretation and Application. 2nd Edition. Springer-Verlag, Berlín-Heidelberg, 984 pp. https://doi.org/10.1007/978-3-642-03796-2
Heredia, S., Beresi, M., Mestre, A. y Rodríguez, C. 2009. El Ordovícico en la Sierra de La Higuera (Mendoza): conodontes y microfacies. Serie Correlación Geológica, 24, 65-76.
Herrera, Z. y Benedetto, J.L. 1991. Early Ordovician brachiopod faunas from the Precordillera basin, Western Argentina: biostratigraphy and paleobiogeographical affinities. In: MacKinnon, D.I., Lee, D.E. and Campbell, J.D. (eds.), Brachiopods through Time. Balkema, Rotterdam, 283-301.
Høeg O. A. 1932. Ordovician algae from the Trondheim area. In: Kiær, J, (ed.), The Hovin Group in the Trondheim area, II, Paleontological part. Skr utgift Nor Vidensk Akad Oslo Matem-Naturv Kl, 1927, 63-96.
Johnston, D. y Barnes, C. 1999. Early and Middle Ordovician (Arenig) conodonts from St. Pauls Inlet and Martin Point, Cow Head Group, western Newfoundland, Canada; 1-2. Biostratigraphy and paleoecology. Geologica et Palaeontologica, 33, 21-70.
Keller, M. 1999. Argentine Precordillera. Sedimentary and Plate Tectonic History of a Laurentian Crustal Fragment in South America. Geological Society of America, Special Paper, 341, 1-131. https://doi.org/10.1130/0-8137-2341-8.1
Landing, E. 1996. Avalon - Insular continent by the latest Precambrian. In: Nance, C. and Thompson, M. (eds.), Avalonian and related peri-Gondwanan terranes of the circum-North Atlantic. Geological Society of America, Special Paper, 304, 27-64 https://doi.org/10.1130/0-8137-2304-3.29
Lehnert, O. 1993. Bioestratigrafía de los conodontes arenigianos de la Formación San Juan en la localidad de Niquivil (Precordillera Sanjuanina, Argentina) y su correlación intercontinental. Revista Española de Paleontología, 8 (2), 153-164. https://doi.org/10.7203/sjp.24558
Li, Z., Stouge, S., Chen, X., Wang, C., Wang, X. y Zen, G. 2010. Precisely compartmentalized and correlated Lower Ordovician Oepikodus evae Zone of the Fuluoian in the Huanghuachang section, Yichang, Hubei Province. Acta Palaeontologica Sinica, 49, 108-124.
Löfgren, A. y Tolmacheva, T. 2008. Morphology, evolution and stratigraphic distribution in the Middle Ordovician conodont genus Microzarkodina. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 99, 27-48. https://doi.org/10.1017/S1755691008007056
Mestre, A. 2010. Estratigrafía y bioestratigrafía de conodontes de la "Transición Cuspidal" de la Formación San Juan al sur del paralelo 30°, Precordillera de San Juan. Tesis Doctoral, Facultad de Ciencias Exactas, Físicas y Naturales de la Universidad Nacional de San Juan, 330 pp.
Mestre, A. 2011. Brechas intraclásticas (tsunamitas?) en el tope de la Formación San Juan (Darriwiliano), Precordillera de San Juan, Argentina. Microfacies y Conodontes. Serie Correlación Geológica, 27 (1), 28-35.
Nielsen, A.T. 2011. A re-calibrated revised sea-level curve for the Ordovician of Baltoscandia. In: Gutiérrez-Marco, J.C., Rábano, I. and García-Bellido, D. (eds.), Ordovician of the World. Serie Cuadernos del Museo Geominero, 14. Instituto Geológico y Minero de España, Madrid, 399-402.
Ortiz, A. y Zambrano, J.J. 1981. La Provincia Geológica Precordillera Oriental. VIII Congreso Geológico Argentino, San Luis, 3, 59-74.
Soria, T., Heredia, S., Mestre, A. y Rodríguez, C. 2013. Conodontes floianos de la Formación San Juan en la quebrada de Talacasto, Precordillera de San Juan. Serie Correlación Geológica, 29 (1), 93-106.
Wang, X., Chen, X., Li, Z. y Wamg, C. 2003. The Conodont succession from the proposed GSSP for the Middle Ordovician base at Huanghuachang Section Yichang, China. In: Albanesi, G., Beresi, M. and Peralta, S. (eds.), Ordovician from the Andes. Instituto Superior de Correlación Geológica, Universidad Nacional de Tucumán. Serie Correlación Geológica, 17, 161-166.
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2024 Consejo Superior de Investigaciones Científicas (CSIC)

This work is licensed under a Creative Commons Attribution 4.0 International License.
© CSIC. Manuscripts published in both the print and online versions of this journal are the property of the Consejo Superior de Investigaciones Científicas, and quoting this source is a requirement for any partial or full reproduction.
All contents of this electronic edition, except where otherwise noted, are distributed under a Creative Commons Attribution 4.0 International (CC BY 4.0) licence. You may read here the basic information and the legal text of the licence. The indication of the CC BY 4.0 licence must be expressly stated in this way when necessary.
Self-archiving in repositories, personal webpages or similar, of any version other than the final version of the work produced by the publisher, is not allowed.