Palaeontology and biostratigraphy of the late Palaeozoic Copacabana Group at the Angosto del Beu, Bolivia
The Copacabana Group at the Angosto del Beu, northwestern Bolivia, yielded abundant invertebrates together with fusulinids and palynomorphs that suggest an early Late Carboniferous-Early Permian age for the unit. The lower section f the group contains the fusulinid Millerella extensa Marshall, and i...
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1998
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| LEADER | 18337caa a22012377a 4500 | ||
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| 001 | PAPER-3033 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518203230.0 | ||
| 008 | 190411s1998 xx ||||fo|||| 00| 0 eng|d | ||
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| 100 | 1 | |a Ottone, E.G. | |
| 245 | 1 | 0 | |a Palaeontology and biostratigraphy of the late Palaeozoic Copacabana Group at the Angosto del Beu, Bolivia |
| 260 | |c 1998 | ||
| 270 | 1 | 0 | |m Depto. de Ciencias Geológicas, Fac. de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón n, 1428, Buenos Aires, Argentina |
| 506 | |2 openaire |e Política editorial | ||
| 504 | |a Aliaga López, E., Palinoestratigrafía del Paleozoico de la sección del Pongo de Coñec, Cuenca Madre de Dios, suroeste del Perú (1985) 4° Reunión RANE-ARPEL, pp. 1-11. , Quito | ||
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| 504 | |a Veevers, J.J., Powell, C.M.A., Late Paleozoic glacial episodes in Gondwanaland reflected in transgressive-regressive depositional sequences in Euroamerica (1987) Geological Society of America Bulletin, 98, pp. 475-487. , Boulder | ||
| 504 | |a Vergel, M.M., Contenido palinológico de la Formación Melo (Paleozoico Superior) de Melo, Uruguay (1987) 10° Congreso Geológico Argentino, Actas, 3, pp. 117-120. , Tucumán | ||
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| 520 | 3 | |a The Copacabana Group at the Angosto del Beu, northwestern Bolivia, yielded abundant invertebrates together with fusulinids and palynomorphs that suggest an early Late Carboniferous-Early Permian age for the unit. The lower section f the group contains the fusulinid Millerella extensa Marshall, and is regarded as early Late Carboniferous in age. The upper section of the unit includes a palynological assemblage mainly dominated by taeniate disaccate pollen grains and monosaccates. The presence of Hamiapollenites insolitus (Bharadwaj and Salujha) Balme, and Pakkapites fusus (Bose and Kar) Menendez together with several biostratigraphically useful brachiopod species such as Kochiproductus peruvianus (d'Orbigny), Neospirifer condor (d'Orbigny), and Linoproductus cora (d;Orbigny), dates the upper section of the group as Early Permian. Comparison with the lake Titikaka and the Altiplano outcrops, and the Madre de Didos subsurface sections, provides a better picture of the palaeogeographical evolution of the Central ANdes during the Late Palaeozoic. |l eng | |
| 593 | |a Depto. de Ciencias Geológicas, Fac. de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón n, 1428, Buenos Aires, Argentina | ||
| 593 | |a Fac. Cie. Nat. y Museo de La Plata, Paseo del Bosque s/n, 1900, La Plata, Argentina | ||
| 593 | |a Univ. des Sci. et Technol. de Lille, UFR des Sciences de la Terre, URA 1365 du CNRS, 59655 Villneuve d'Ascq Cédex, France | ||
| 690 | 1 | 0 | |a BIOSTRATIGRAPHY |
| 690 | 1 | 0 | |a FORAMINIFERA |
| 690 | 1 | 0 | |a INVERTEBRATE |
| 690 | 1 | 0 | |a PALAEOZOIC |
| 651 | 4 | |a BOLIVIA | |
| 700 | 1 | |a Rossello, E.A. | |
| 700 | 1 | |a Simanauskas, T. | |
| 700 | 1 | |a Vachard, D. | |
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