Paleoenvironmental interpretation and palynology of outcrop and subsurface sections of the Tarija Formation (Upper Carboniferous), northwestern Argentina
The Tarija Formation of the Macharetí Group has been studied sedimentologically and palynologically at Zanja Honda Creek and the Zanja Honda x-1 well to assess the paleoenviromental and paleoclimatic evolution of the southern portion of the Tarija Basin. In addition, new palynological data and their...
Guardado en:
| Autor principal: | |
|---|---|
| Otros Autores: | |
| Formato: | Capítulo de libro |
| Lenguaje: | Inglés |
| Publicado: |
2007
|
| Materias: | |
| Acceso en línea: | Registro en Scopus DOI Handle Registro en la Biblioteca Digital |
| Aporte de: | Registro referencial: Solicitar el recurso aquí |
| LEADER | 13008caa a22010337a 4500 | ||
|---|---|---|---|
| 001 | PAPER-22740 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205420.0 | ||
| 008 | 190411s2007 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-33847197545 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Papa, C.d. | |
| 245 | 1 | 0 | |a Paleoenvironmental interpretation and palynology of outcrop and subsurface sections of the Tarija Formation (Upper Carboniferous), northwestern Argentina |
| 260 | |c 2007 | ||
| 270 | 1 | 0 | |m Papa, C.d.; National Research Council, Argentina (CONICET) - Natural Sciences Faculty, University of Salta, Buenos Aires 177, 4400 Salta, Argentina; email: delpapac@unsa.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
| 504 | |a Arigós, L.E., Vilela, C.R., Consideraciones geológicas sobre las Sierras Subandinas (1949) Revista de la Asociación Geológica Argentina, tomo IV, (2), pp. 7-132 | ||
| 504 | |a Azcuy, C.L., di Pasquo, M., Palynology of the Late Carboniferous from the Tarija Basin, Argentina: a systematic review of monosaccate pollen genera (2000) Palaentographica Abt. B, 253, pp. 107-137 | ||
| 504 | |a Buatois, L., del Papa, C., Trazas fósiles de la Formación Tarija, Carbonífero Superior del norte argentino: Aspectos icnológicos de la glaciación gondwánica (2003) Ameghiniana, Publicación especial, 9, pp. 119-130 | ||
| 504 | |a Césari, S.N., Gutiérrez, P.R., Palynostratigraphy of Upper Paleozoic sequences in central-western Argentina (2001) Palynology, 24, pp. 113-146 | ||
| 504 | |a Cope, M.J., Chaloner, W.G., Wildfire: an interaction of biological and physical processes (1985) Geological Factors and the Evolution of Plants, pp. 257-277. , Tiffney B.H. (Ed), Yale University Press, New Haven, CT | ||
| 504 | |a del Papa, C.E., Martínez, L., Sedimentación lacustre glaci-dominada en la Formación Tarija (Carbonífero), sierra de Aguaragüe, noroeste argentino (2001) Revista de la Asociación Argentina de Sedimentología, 8 (1), pp. 61-76 | ||
| 504 | |a di Pasquo, M., The Crassispora kosankei-Cystoptychus azcuyi Palynozone from the Upper Carboniferous Tupambi Formation, Tarija basin, northern Argentine (2002) Review of Palaeobotany and Palynology, 118, pp. 47-76 | ||
| 504 | |a di Pasquo, M., Avances sobre palinología, bioestratigrafía y correlación de las asociaciones presentes en los Grupos Macharetí y Mandiyutí, Neopaleozzoico de la Cuenca Tarija, provincia de Salta, Argentina (2003) Ameghiniana, 40, pp. 3-32 | ||
| 504 | |a di Pasquo, M., Azcuy, C.L., Palinología del Grupo Mandiyutí, Carbonífero Superior, Cuenca Tarija, Argentina (1997) 10° Congreso Geológico Chileno (Antofagasta), Actas, 1, pp. 475-479 | ||
| 504 | |a di Pasquo, M., Azcuy, C.L., Palinomorfos retrabajados en el Carbonífero Tardío de la Cuenca Tarija (Argentina) y su aplicación a la datación de eventos diastróficos (1997) Revista Universidade Guarulhos, Geociêcias, 2 (Especial), pp. 28-42 | ||
| 504 | |a di Pasquo, M., Azcuy, C.L., Paleontología, paleoclima y correlación de estratos carboníferos en la provincia de Salta sobre la base de palinomorfos (1999) 14° Congreso Geológico Argentino (Salta), Relatorio, 1, pp. 254-260 | ||
| 504 | |a di Pasquo, M., Azcuy, C.L., Interpretación paleoambiental del Grupo Mandiyutí (Carbonífero Superior): Evidencias palinológicas, sedimentológicas y tafonómicas (1999) Ameghiniana, 36, pp. 71-81 | ||
| 504 | |a di Pasquo, M., Azcuy, C.L., Starck, D., Palinología de la Formación San Telmo (Carbonífero Superior), en la Sierra San Antonio, provincia de Salta, Argentina (2001) Ameghiniana, 38, pp. 85-98 | ||
| 504 | |a Eyles, C.H., Eyles, N., Subaqueous mass flow origin for Lower Permian diamictites and associated facies of the Grant Group, Barbwire Terrace, Canning Basin, Western Australia (2000) Sedimentology, 47, pp. 15-84 | ||
| 504 | |a Eyles, N., Eyles, C.H., Miall, A.D., Lithofacies types and vertical profile models; an alternative approach to the description and environmental interpretation of glacial diamict and diamictite sequences (1983) Sedimentology, 30, pp. 393-410 | ||
| 504 | |a Eyles, C.H., Eyles, N., Miall, A.D., Models of glaciomarine sedimentation and their application to the interpretation of ancient glacial sequences (1985) Palaeogeography, Palaeoclimatology, Palaeoecology, 51, pp. 15-84 | ||
| 504 | |a Fernández Garrasino, C.A., Algunos rasgos sedimentarios y estratigráficos de las llamadas "Areniscas del Palmar" (Carbónico de la cuenca Tarija, Chaco Salteño) y esquemas evolutivos paleoambientales del Grupo Macharetí, Argentina (1978) Reunión Nacional "El Paleozoico de Argentina", Acta Geológica Lilloana, 14 (suplemento), pp. 49-52 | ||
| 504 | |a Golonka, J., Ford, D., Pangean (Late Carboniferous-Middle Jurassic) paleoenvironment and lithofacies (2000) Palaeogeography, Palaeoclimatology, Palaeoecology, 161, pp. 1-34 | ||
| 504 | |a Kelts, K., Hsü, J.K., Freshwater carbonate sedimentation (1978) Lakes: Chemistry, Geology and Physics, pp. 295-323. , Lerman A. (Ed), Springer-Verlag, Berlin | ||
| 504 | |a López Gamundi, O.R., Carácter cratónico de las sedimentitas de la Formación Tarija (Carbónico Superior), sierra de Aguaragüe, República Argentina (1984) Revista de la Asociación de Mineralogía, Petrología y Sedimentología, 13, pp. 17-24 | ||
| 504 | |a López Gamundi, O.R., Sedimentología de la Formación Tarija, Carbonífero de la sierra de Aguaragüe, provincia de Salta (1986) Revista de la Asociación Geológica Argentina, 41, pp. 334-355 | ||
| 504 | |a López Gamundi, O.R., Depositional models for the glaciomarine sequences of Andean Late Paleozoic basins of Argentina (1987) Sedimentary Geology, 52, pp. 109-126 | ||
| 504 | |a Milana, J.P., López, S., Solar cycles recorded en Carboniferous glacimarine rhytmites (western Argentina): relationships between climate and sedimentary environment (1998) Palaeogeography, Palaeoclimatology, Palaeoecology, 144, pp. 37-63 | ||
| 504 | |a Padula, E.L., Reyes, F.C., Contribución al léxico estratigráfico de las Sierras Subandinas, Bolivia (1958) Yacimientos Petrolíferos Fiscales Bolivianos Boletín Técnico, 1, pp. 9-70 | ||
| 504 | |a Pozzo, A., Fernández Garrasino, C.O., Sobre la presencia de depósitos de barrera litoral en la Formación Tupambi (Mississippiano) en el subsuelo del Chaco Salteño (provincia de Salta, Argentina) (1979) 7° Congreso Geológico Argentino (Neuquén, 1979), Actas, 1, pp. 551-562 | ||
| 504 | |a Reyes, F.C., On the Carboniferous and Permian of Bolivia and Northwestern Argentina (1972) An. Acad. Brasil. Ciências (Suppl.), 4, pp. 261-277 | ||
| 504 | |a Scott, A.C., The Pre-Quaternary history of fire (2000) Palaeogeography, Palaeoclimatology, Palaeoecology, 164, pp. 281-329 | ||
| 504 | |a Souza, P.A., Petri, S., Dino, R., Late Carboniferous palynology from the Itararé Subgroup (Paraná Basin) at Aracoiaba da Serra, Sâo Paulo State, Brazil (2003) Palynology, 27, pp. 39-74 | ||
| 504 | |a Starck, D., Silurian-Jurassic stratigraphy and basin evolution of nothwestern Argentina (1995) Petroleum Basin of South America, 62, pp. 51-267. , Tankard A.J., Suárez R., and Welsink H.J. (Eds), American Association Petroleum Geologists, Memoir | ||
| 504 | |a Van Wagoner, J.C., Mitchum, R.M., Campion, K.M., Rahmanian, V.D., Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies (1990) American Association of Petroleum Geologist, Methods in Exploration Series, 7, p. 60 | ||
| 504 | |a Wang, X., Van der Kaars, S., Kershaw, P., Bird, M., Jansen, F., A record of fire, vegetation and climate through the last three glacial cycles from Lombok Ridge core G6-4, Eastern Indian Ocean, Indonesia (1999) Palaeogeography, Palaeoclimatology, Palaeoecology, 147, pp. 241-256 | ||
| 520 | 3 | |a The Tarija Formation of the Macharetí Group has been studied sedimentologically and palynologically at Zanja Honda Creek and the Zanja Honda x-1 well to assess the paleoenviromental and paleoclimatic evolution of the southern portion of the Tarija Basin. In addition, new palynological data and their implications are presented. The Tarija Formation consists mainly of thick diamictites interbedded with sandstone and mudstone layers; for the first time, a varves succession is described from the cores of the ZH x-1 well. Fifty-six spore species, 18 monosaccates, 1 praecolpate pollen grain, 4 paleophytoplankton species, and much phytodebris are recorded. The indigenous miospores are assigned to the middle portion of the Dictyotriletes bireticulatus-Cristatisporites chacoparanensis (BC) Biozone di Pasquo of early Late Carboniferous (Westphalian) age. Moreover, abundant reworked palynomorphs occur in both assemblages, recording erosion of Silurian-Early Carboniferous rocks. Some Late Carboniferous species such as Crassispora kosankei (Potonié and Kremp) Bhardwaj emend. Smith and Butterworth, Cristatisporites rollerii Ottone, and Cystoptychus azcuyi di Pasquo, exclusive of the KA Biozone, and Raistrickia radiosa Playford and Helby of the RS Biozone di Pasquo are interpreted as reworked from the lower Tupambi and Itacuamí formations. A fluviolacustrine setting is interpreted for the Tarija Formation on the basis of the presence of glacial varves, continental algae such as Botryococcus braunii Kützing, and overall facies associations. A hiatus between the fluviodeltaic interglacial Tupambi-Itacuamí depositional cycle ("Cycle I") and the fluviolacustrine, glacially influenced Itacuamí-Tarija depositional cycle ("Cycle II") is suggested by the sedimentary and palynologic data. This interpretation is confirmed by short-ranged species with biostratigraphic value, as well as the recognition of useful lithological and palynological differences helpful for characterizing both similar superposed sedimentary cycles. © 2006 Elsevier Ltd. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Princeton Environmental Institute, Princeton University, PIP 2304/00 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: We thank Lic. Gustavo Holfeltz, technician of the Laboratory of Palynology (Geological Department, University of Buenos Aires), and Dra. Nilda Menegatti, technician of the Laboratory of XR diffraction (LANAIS, University of Salta) for their laboratory assistance. We are very grateful to the Secretaría de Recursos Energéticos, Salta province, and Pluspetrol S.A., Tartagal, for providing the cores and information about the wells. We thank the referees S. Césari and E. Ottone for their thoughtful suggestions. This research was supported by CONICET–PEI N°6091 grant (CdP) and CONICET–PIP 2304/00 (MdP). This publication is a contribution to IGCP Project N°471, “Evolution of Western Gondwana During the Late Paleozoic: Tectosedimentary Record, Paleoclimates and Biological Changes.” | ||
| 593 | |a National Research Council, Argentina (CONICET) - Natural Sciences Faculty, University of Salta, Buenos Aires 177, 4400 Salta, Argentina | ||
| 593 | |a Department of Geology, Exact and Natural Sciences Faculty, University of Buenos Aires, Ciudad Universitaria, Pabellon II, 1428 Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a GLACIOTERRESTRIAL |
| 690 | 1 | 0 | |a LATE CARBONIFEROUS |
| 690 | 1 | 0 | |a PALYNOLOGY |
| 690 | 1 | 0 | |a SEDIMENTATION |
| 690 | 1 | 0 | |a TARIJA FORMATION |
| 690 | 1 | 0 | |a CARBONIFEROUS |
| 690 | 1 | 0 | |a DIAMICTITE |
| 690 | 1 | 0 | |a MUDSTONE |
| 690 | 1 | 0 | |a OUTCROP |
| 690 | 1 | 0 | |a PALEOCLIMATE |
| 690 | 1 | 0 | |a PALEOENVIRONMENT |
| 690 | 1 | 0 | |a PALYNOLOGY |
| 690 | 1 | 0 | |a PALYNOMORPH |
| 690 | 1 | 0 | |a SANDSTONE |
| 690 | 1 | 0 | |a SEDIMENTATION |
| 690 | 1 | 0 | |a SILURIAN |
| 690 | 1 | 0 | |a ALGAE |
| 690 | 1 | 0 | |a BOTRYOCOCCUS BRAUNII |
| 690 | 1 | 0 | |a CRASSISPORA KOSANKEI |
| 690 | 1 | 0 | |a CYSTOPTYCHUS AZCUYI |
| 690 | 1 | 0 | |a DICTYOTRILETES BIRETICULATUS |
| 690 | 1 | 0 | |a RAISTRICKIA RADIOSA |
| 651 | 4 | |a NORTHWESTERN ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a SOUTH AMERICA | |
| 651 | 4 | |a CRISTATISPORITES CHACOPARANENSIS | |
| 700 | 1 | |a Pasquo, M.d. | |
| 773 | 0 | |d 2007 |g v. 23 |h pp. 99-119 |k n. 1 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
| 856 | 4 | 1 | |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-33847197545&doi=10.1016%2fj.jsames.2006.09.004&partnerID=40&md5=a0f55cfab3b01c029ed4f4a9bd49ed11 |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.jsames.2006.09.004 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_08959811_v23_n1_p99_Papa |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v23_n1_p99_Papa |y Registro en la Biblioteca Digital |
| 961 | |a paper_08959811_v23_n1_p99_Papa |b paper |c PE | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 963 | |a VARI | ||
| 999 | |c 83693 | ||