Palynological assemblages present in Los Monos (Devonian) and Itacua (Early Carboniferous) formations at Balapuca (Tarija basin), southern Bolivia. Part 2. Itacua Formation assemblages and stratigraphical interpretation and chronology of the Los Monos and Itacua formations
The palynological result of three fertile samples of the Itacua Formation is presented. This unit crops out at Balapuca located in the Bolivian margin of the Bermejo river, in the mountain range of San Telmo. The stratigraphic extension of the species determined in this association allowed the ident...
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| Lenguaje: | Español |
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2007
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| LEADER | 35008caa a22019457a 4500 | ||
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| 001 | PAPER-22631 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205413.0 | ||
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| 024 | 7 | |2 scopus |a 2-s2.0-38149118679 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a di Pasquo, M. | |
| 245 | 1 | 0 | |a Palynological assemblages present in Los Monos (Devonian) and Itacua (Early Carboniferous) formations at Balapuca (Tarija basin), southern Bolivia. Part 2. Itacua Formation assemblages and stratigraphical interpretation and chronology of the Los Monos and Itacua formations |
| 246 | 3 | 1 | |a Asociaciones palinológicas en las formaciones Los Monos (Devónico) e Itacua (Carbonífero Inferior) en Balapuca (Cuenca Tarija), sur de Bolivia. Parte 2. Asociaciones de la Formación Itacua e interpretación estratigráfica y cronología de las formaciones Los Monos e Itacua |
| 260 | |c 2007 | ||
| 270 | 1 | 0 | |m di Pasquo, M.; Consejo Nacional de Investigaciones Científicas y Técnicas, Departamento de Geología, Universidad de Buenos Aires, Pabellón 2, 1 Piso, 1428 Capital Federal, Argentina; email: medipa@gl.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Playford, G., Lower Carboniferous spores from the Ducabrook Formation, Drummond Basin, Queensland (1978) Palaeóntographica, Abteilung B, 167, pp. 105-160 | ||
| 504 | |a Playford, G., Palynology of the Australian Lower Carboniferous: A review (1985) International Congress on Stratigraphy and Geology of Carboniferous, No. 10, Comptes Rendus 4: 247-265. Madrid | ||
| 504 | |a Playford, G., Australian Lower Carboniferous miospores relevant to extra-Gondwanic correlations: And evaluation (1991) Courier Forschungs-Institut Senckenberg, 130, pp. 85-125 | ||
| 504 | |a Playford, G. 1993. Miospores and organic walled microphytoplankton characteristic of strata contiguous with the Devonian-Carboniferous boundary. In Congrés International de la Stratigraphie et Géologie du Carboniféreet Permian, No. 12, Comptes Rendus 1: 127-160. Buenos Aires; Playford, G., McGregor, D.C., Miospores and organic-walled microphytoplankton of Devonian-Carboniferous boundary beds (Bakken Formation), Southern Saskatchewan: A systematic and stratigraphic appraisal (1993) Geological Survey of Canada, Bulletin, 445, pp. 1-107 | ||
| 504 | |a Playford, G., Satterthwait, B., Lower Carboniferous (Visean) of the Bonaparte Gulf Basin, northwestern Australia. Part one (1985) Palaeóntographica, Abteilung B, 195, pp. 129-152 | ||
| 504 | |a Playford, G., Satterthwait, B., Lower Carboniferous (Visean) of the Bonaparte Gulf Basin, northwestern Australia. Part two (1986) Palaeóntographica, Abteilung B, 200, pp. 1-32 | ||
| 504 | |a Playford, G., Satterthwait, B., Lower Carboniferous (Visean) spores of the Bonaparte Gulf Basin, Northwestern Australia: Part three (1988) Palaeóntographica, Abteilung B, 208, pp. 1-26 | ||
| 504 | |a Potonié, R., Synopsis der Gattungen der Sporae Dispersae. I vol (1956) Beiheftezumgeologischen Jahrbuch, 23, pp. 1-103 | ||
| 504 | |a Potonié, R., Synopsis der Gattungen der Sporae dispersae. V. Teil: Nachtrage zu alien Gruppen (Turmae). (1970) Beihefte zum geologischen Jahrbuch, 87, pp. 1-222 | ||
| 504 | |a Potonié, R., Kremp, G.O., Die Sporae dispersae des Ruhrkarbons, ihre Morphographie and Stratigraphie mit Ausblicken auf Arten anderer Gebiete und Zeitabschnitte, 2 (1956) Palaeóntographica, Abteilung, 8 (99), pp. 85-191 | ||
| 504 | |a Quadros, L.P., Silurian-Devonian acritarch assemblages from Paraná Basin: An update and correlation with northern Brazilian basins (1999) Ordovician-Devonian Palynostratigraphy in Western Gondwana: Update, Problems and Perspectives, pp. 105-145. , Rodrigues, M.A.C, Pereira, E, editores, Universidade do Estado do Rio de Janeiro, Facultad de Geología:, Río de Janeiro | ||
| 504 | |a Richardson, J.B., Middle Old Red Sandstone spore assemblages from the Orcadian Basin north-east Scotland (1965) Palaeontology, 7 (4), pp. 559-605 | ||
| 504 | |a Richardson, J.B., McGregor, D.C., Silurian and Devonian spore zones of the Old Red Sandstone continent and adjacent regions (1986) Geological Survey of Canada, Bulletin, 364, pp. 1-79 | ||
| 504 | |a Rodrigues, R., Loboziak, S., Meló, J.H.G., Alves, D.B., Geochemical characterization and miospore biochronostratigraphy of the Frasnian anoxic event in the Parnaíba Basin, northeast Brazil (1995) Bulletin des Centres de Recherches Exploration-Production Elf-Aquitaine, 19, pp. 319-327 | ||
| 504 | |a Rubinstein, C.V., Primer registro palinológico de la Formación Punta Negra (Devónico Medio-Superior), de la Precordillera de San Juan, Argentina (1999) Simposio Argentino de Paleobotánica y Palinología, 10, pp. 13-18. , Asociación Paleontológica Argentina, Publicación Especial 6:, Buenos Aires | ||
| 504 | |a Schopf, J.M., Wilson, L.R., Bentall, R., An annotated synopsis of Palaeozoicfossil spores and the definition of generic groups. Illinois State Geological Survey (1944) Report Investigation, , 91: 1-66 | ||
| 504 | |a Schulz.A.; Santiago, M.; Hernández, R.;Galli,C.;Álvarez, L; del Papa, C. 1999. Modelo estratigráfico del Carbonífero en el sector sur de la cuenca de Tarija. In Congreso de Exploración y Desarrollo de Hidrocarburos, No. 4, Actas 2: 695-711. Mar del Plata; Smith, A.H.V. 1971. Microfossiles organiques du Paleo-zoique. 4. Les spores. 2. Le genre Verrucosisporites par A.H.V. Smith. Commission Internationale de Microflore du Paleozoique, Centre National de la Recherche Scientifique: 35-87. Paris; Smith, A.H.V., Butterworth, M.A., Miospores in the coal sems of the Carboniferous of Great Britain. The Palaeontological Association (1967) Special Paper in Palaeontology, 1, pp. 1-324 | ||
| 504 | |a Staplin, F.L., Upper Mississippian plant spores from the Golata Formation, Alberta, Canada (1960) Palaeóntographica, Abtellung B, 107, pp. 1-40 | ||
| 504 | |a Streel, M., Associations de spores du Devonien inférieur beige et leur signification stratigraphique. (1967) Annales de la Société Géologique de Belgique, 90 (1), pp. 11-54 | ||
| 504 | |a Streel, M., Caputo, M.V., Loboziak, S., Meló, J.H.G., Late Frasnian-Famennian climates based on palynomorph analysis and the question of the Late Devonian glaciations (2000) Earth-Sciences Reviews, 52, pp. 121-173 | ||
| 504 | |a Suárez Soruco, R., Lobo Boneta, J., La fase compresiva Eohercínica en el sector oriental de la Cuenca Cordillerana de Bolivia (1983) Revista Técnica Yacimientos Petrolíferos Fiscales Bolivianos, 9, pp. 189-202 | ||
| 504 | |a Sullivan, H.J., A Tournaisian spore flora from the Cementstone Group of Ayreshire, Scotland (1968) Palaeontology, 11, pp. 116-131 | ||
| 504 | |a Turnau, E., Microflora of the Famennian and Tournaisian deposits from boreholes of northern Poland (1975) Acta Geológica Polonica, 25, pp. 505-528 | ||
| 504 | |a Turnau, E., Spore zonation of Uppermost Devonian and Lower Carboniferous deposits of western Pomerania (1978) Mededelingen rijks geologische dienst, 30, pp. 1-35 | ||
| 504 | |a Turnau, E., Miospore stratigraphy of Middle Devonian deposits from western Pomerania (1986) Review of Palaeobotany and Palynology, 93, pp. 107-125 | ||
| 504 | |a Turnau, E., Miospore stratigraphy of Middle Devonian deposits from Western Pomerania (1996) Review of Palaeobotany and Palynology, 93, pp. 107-125 | ||
| 504 | |a Turnau, E., Racki, G., Givetian palynostratigraphy and palynofecies: New data from the Bodzentyn Syncline (Holy Cross Mountains, central Poland) (1999) Review of Palaeobotany and Palynology, 106, pp. 237-271 | ||
| 504 | |a Utting, J., Palynology of the Lower Carboniferous Windsor Group and Windsor-Canso boundary beds of Nova Scotia, and their equivalents in Quebec, New Brunswick and Newfoundland (1987) Geological Survey of Canada, Bulletin, 374, pp. 1-93 | ||
| 504 | |a Utting, J., Giles, P.S., Biostratigraphical implications of new palynological data from the Mississippian of Newfoundland and Nova Scotia, Canada (2004) Memoirs of the Association of Australasian Palaeontologists, 29, pp. 115-160 | ||
| 504 | |a Utting, J., Wielens, H., Organic petrology, thermal maturity, geology, and petroleum source rock potential of Lower Permian coal, Karoo Supersystem, Zambia (1992) Energy Sources, 14, pp. 337-354 | ||
| 504 | |a Vavrdová, M., Isaacson, P.E., Late Famennian phytogeographycprovincialism: Evidencefora limited separation of Gondwana and Laurentia (1999) Abhandlungen der Geologischen Bundesanstalt, 54, pp. 453-463 | ||
| 504 | |a Vavrdová, M., Bek, J., Dufka, P., Isaacson, P.E., Palynology of the Devonian (Lochkovian to Tournalsian) sequence, Madre de Dios Basin, northern Bolivia (1996) Vestnik Ceskeho geologickeho ustavu, 71 (4), pp. 333-349 | ||
| 504 | |a Vavrdová, M., Isaacson, P.E., Diaz, E., Bek, Devonian-Carboniferous boundary at Lake Titikaka, Bolivia: Preliminary palynological results (1993) Congrés International de la Stratigraphie et Géologie du Carbonifere et Permien, No.12, Comptes Rendus 1: 187-200. Buenos Aires, , 1 | ||
| 504 | |a Veevers, J.J., Powell, C.M., Late Paleozoic glacial episodes in Gondwanaland reflected in transgressive-regressive depositional sequences in Euroamerica (1987) Bulletin of Geological Society of America, 98, pp. 475-487 | ||
| 504 | |a Winslow, M.R., Plant spores and other microfossils from the Upper Devonian and Lower Mississippian rocks of Ohio (1962) United States Geological Survey, Professional Paper, 364, pp. 1-93 | ||
| 504 | |a Young, G.C. 1996. Devonian. In An Australian Phanerozoic Timescale (Young, G.C; Laurie, J.R.; editors). Oxford University Press 4: 96-109. Melbourne | ||
| 520 | 3 | |a The palynological result of three fertile samples of the Itacua Formation is presented. This unit crops out at Balapuca located in the Bolivian margin of the Bermejo river, in the mountain range of San Telmo. The stratigraphic extension of the species determined in this association allowed the identification of two sets of palynomorphs, one indigenous, composed of 61 species of spores and few colonies of Botryocoocus, and another set of reworked species, composed by spores, acritarchs, prasinophytes, chloroficean algae, cryptospores and chitinozoans, mostly coming from the Devonian layers and subordinated spores of the Tournaisian (Carboniferous) ones. Two indigenous spore species are proposed as new Palinoestratigrafía de la Formación Itacua, Bolivia. Parte 2 combinations. The stratigraphical distribution of indigenous key species allowed assigning this association to the early Visean (Early Carboniferous). This is the first work where indigenous palynomorphs of this age are Illustrated along with a selection of reworked species, and are obtained of an in situ deposit of the Itacua Formation cropping out in the southern Tarija Basin. Based on the age attributed to the Los Monos and Itacua formations in this study, a hiatus is defined between them, characterized by an erosive phase during the Frasnian-Tournaisian and, another non-depostional hiatus identified in the latest Famennian ('Strunian'). This is interpreted from the presence/absence of reworked species with restricted stratigraphical range in the Itacua Formation assemblage. On the other hand, the Machareti Group overlies this unit, and it was dated as early Late Carboniferous based on palynology. Between both units, a new hiatus that spans the late Visean-Serpukhovian partly interpreted as non-depositional is registered. In addition, a discussion about a possible tectonic and glacioeustatic origen for both hiatus is included. |l eng | |
| 593 | |a Consejo Nacional de Investigaciones Científicas y Técnicas, Departamento de Geología, Universidad de Buenos Aires, Pabellón 2, 1 Piso, 1428 Capital Federal, Argentina | ||
| 690 | 1 | 0 | |a DEVONIAN |
| 690 | 1 | 0 | |a EARLY CARBONIFEROUS |
| 690 | 1 | 0 | |a ITACUA FORMATION |
| 690 | 1 | 0 | |a LOS MONOS FORMATION |
| 690 | 1 | 0 | |a PALYNOSTRATIGRAPHY |
| 690 | 1 | 0 | |a SOUTHERN BOLIVIA |
| 690 | 1 | 0 | |a TARIJA BASIN |
| 690 | 1 | 0 | |a ALGAE |
| 690 | 1 | 0 | |a CROPS |
| 690 | 1 | 0 | |a GEOCHRONOLOGY |
| 690 | 1 | 0 | |a MARINE BIOLOGY |
| 690 | 1 | 0 | |a PLANTS (BOTANY) |
| 690 | 1 | 0 | |a STRATIGRAPHY |
| 690 | 1 | 0 | |a BIOSTRATIGRAPHY |
| 690 | 1 | 0 | |a CARBONIFEROUS |
| 690 | 1 | 0 | |a DEVONIAN |
| 690 | 1 | 0 | |a GEOCHRONOLOGY |
| 690 | 1 | 0 | |a PALYNOLOGY |
| 690 | 1 | 0 | |a PALYNOMORPH |
| 690 | 1 | 0 | |a TARIJA BASIN |
| 690 | 1 | 0 | |a ACRITARCHA |
| 690 | 1 | 0 | |a ALGAE |
| 690 | 1 | 0 | |a CHITINOZOA |
| 690 | 1 | 0 | |a PRASINOPHYCEAE |
| 651 | 4 | |a BOLIVIA | |
| 651 | 4 | |a SOUTH AMERICA | |
| 773 | 0 | |d 2007 |g v. 34 |h pp. 163-198 |k n. 2 |p Rev. Geol. Chile |x 07160208 |w (AR-BaUEN)CENRE-104 |t Revista Geologica de Chile | |
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