Biofacies analysis of the pilmatué member of the agrio formation, lower cretaceous, neuquén basin, Argentina
A biofacies analysis based on benthic macrofossils was carried out. The study unit is the Pilmatué Member of the Agrio Formation in three sections in the Neuquén Province. Six biofacies controlled by relative sea level changes, sedimentation rate, substrate consistency, oxygenation and salinity were...
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| Lenguaje: | Español |
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2007
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| LEADER | 12695caa a22010457a 4500 | ||
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| 001 | PAPER-22681 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205416.0 | ||
| 008 | 190411s2007 xx ||||fo|||| 00| 0 spa|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-34347325985 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Lazo, D.G. | |
| 245 | 1 | 0 | |a Biofacies analysis of the pilmatué member of the agrio formation, lower cretaceous, neuquén basin, Argentina |
| 246 | 3 | 1 | |a Análisis de biofacies y cambios relativos del nivel del mar en el Miembro Pilmatué de la Formación Agrio, Cretácico Inferior de cuenca Neuquina, Argentina |
| 260 | |c 2007 | ||
| 270 | 1 | 0 | |m Lazo, D.G.; Consejo Nacional de Investigaciones Científicas y Técnicas, Departamento de Cientias Geológicas, Ciudad Universitaria, 1428 Buenos Aires, Argentina; email: dlazo@gl.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Aguirre-Urreta, M.B., Rawson, P.F., Lower Cretaceous ammonites from the Neuquén Basin, Argentina: The Hauterivian genus Holcoptychites (2003) Cretaceous Research, 24, pp. 589-613 | ||
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| 504 | |a Lazo, D.G., The genus Steinmanella (Bivalvia, Trigonioida) in the Agrio Formation (Lower Cretaceous), Neuquén Basin, Argentina (2003) Journal of Paleontology, 77, pp. 1069-1085 | ||
| 504 | |a Lazo, D.G., Taxonomy, facies relationships and palaeobiology of bakevelliid bivalves from the Lower Cretaceous of west-central Argentina (2003) Cretaceous Research, 24, pp. 765-788 | ||
| 504 | |a Lazo, D.G. 2004. [Análisis de concentraciones fósiles del Cretácico Inferior de cuenca Neuquina. Tesis doctoral, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, 337 pp., Inédito.]; Lazo, D.G., Análisis tafonómico e inferencia del grado de mezcla temporal y espacial de la macrofauna del Miembro Pilmatué de la Formación Agrio, Cretácico Inferior de cuenca Neuquina, Argentina (2006) Ameghiniana, 43, pp. 311-326 | ||
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| 504 | |a Steinmann, G. 1881. Zur Kenntniss der Jura- und Kreideformation von Caracoles (Bolivia). Neues Jahrbuch für Mineralogie, Geologie und Palaeontologie, Beilage-Band I, 239-301, lám. 9-14; Stenzel, H. 1971. Oysters. En: R.C. Moore y C. Teichert (eds.), Treatise on Invertebrate Paleontology. Part N. Mollusca 6. Bivalvia 3, University of Kansas and Geological Society of America, pp. N953-N1224; Taylor, E.M. y Glover, E.A. 2000. Functional anatomy, chemosymbiosis and evolution of the Lucinidae. En: E.M. Harper, J.D. Taylor y J.A. Crame (eds.), The Evolutionary Biology of the Bivalvia. Geological Society, London, Special Publication 177: 207-225; Ten Hove, H.A., van den Hurk, P., A review of recent and fossil serpulid "reefs"; actuopalaeontology and the "Upper Malm" serpulid limestones in NW Germany (1993) Geologie en Mijnbouw, 72, pp. 23-67 | ||
| 504 | |a Weaver, C.E., Paleontology of the Jurassic and Cretaceous of West Central Argentina (1931) Memoirs of the University of Washington, 1, pp. 1-595 | ||
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| 520 | 3 | |a A biofacies analysis based on benthic macrofossils was carried out. The study unit is the Pilmatué Member of the Agrio Formation in three sections in the Neuquén Province. Six biofacies controlled by relative sea level changes, sedimentation rate, substrate consistency, oxygenation and salinity were recognised. The "Cucullaea-Mimachlamys-Steinmanella biofacies" is highly diverse and recorded in a shoreface environment characterized by a well-oxygenated soft sandy and patchy bioclastic substrate, reduced siliciclastic input, normal marine salinity, and warm-temperate waters. The "coral colonies biofacies" is associated with the former biofacies, but in a more shallow setting and probably temperatures above 16°-18° C The "Cucullaea and Steinmanella biofacies" occurred in an open shelf environment characterized by low water energy, reduced siliciclastic input, firm muddy substrate, and normal marine conditions. The "Modiolus biofacies" also occurs on the shelf, but under low oxygenation. The "gregarious serpulids" and "gregarious oysters" biofacies correspond to an inner shelf setting characterized by an alternation of high and low water energy, low siliciclastic input, firm muddy substrate, well-oxygenated bottom, and mixo-euharine conditions. The "Cucullaea-Mimachlamys-Panopea" and "Cucullaea and Steinmanella" biofacies are related to changes of relative sea level in the scale of parasequences, while the "coral colonies", "Modiolus", "gregarious oysters", and "gregarious serpulids" respond to changes in the scale of sequences. ©Asociación Paleontológica Argentina. |l eng | |
| 593 | |a Consejo Nacional de Investigaciones Científicas y Técnicas, Departamento de Cientias Geológicas, Ciudad Universitaria, 1428 Buenos Aires, Argentina | ||
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a NEUQUEN BASIN | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a BENTHIC MACROFOSSILS |
| 690 | 1 | 0 | |a PALEOECOLOGY |
| 690 | 1 | 0 | |a PALEOENVIRONMENTS |
| 690 | 1 | 0 | |a VALANGINIAN- HAUTERIVIAN |
| 690 | 1 | 0 | |a BENTHOS |
| 690 | 1 | 0 | |a BIOFACIES |
| 690 | 1 | 0 | |a CRETACEOUS |
| 690 | 1 | 0 | |a FOSSIL |
| 690 | 1 | 0 | |a OXYGENATION |
| 690 | 1 | 0 | |a PALEOECOLOGY |
| 690 | 1 | 0 | |a PALEOENVIRONMENT |
| 690 | 1 | 0 | |a SALINITY |
| 690 | 1 | 0 | |a SEA LEVEL CHANGE |
| 690 | 1 | 0 | |a SEDIMENTATION |
| 690 | 1 | 0 | |a ANTHOZOA |
| 690 | 1 | 0 | |a CUCULLAEA |
| 690 | 1 | 0 | |a MIMACHLAMYS |
| 690 | 1 | 0 | |a MODIOLUS |
| 690 | 1 | 0 | |a OSTREIDAE |
| 690 | 1 | 0 | |a PANOPEA |
| 690 | 1 | 0 | |a SERPULIDAE |
| 690 | 1 | 0 | |a STEINMANELLA |
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