Sedimentology and paleoenvironments of the Las Chacritas carbonate paleolake, Cañadón Asfalto Formation (Jurassic), Patagonia, Argentina
The Las Chacritas Member is the lower part of the Cañadón Asfalto Formation (Jurassic). The unit is a completely continental limestone succession with volcanic contributions that were deposited during the development of the Cañadón Asfalto Rift Basin (Chubut province, Patagonia, Argentina). A detail...
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2013
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| LEADER | 31964caa a22021497a 4500 | ||
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| 001 | PAPER-24337 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205610.0 | ||
| 008 | 190411s2013 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84873058059 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Cabaleri, N.G. | |
| 245 | 1 | 0 | |a Sedimentology and paleoenvironments of the Las Chacritas carbonate paleolake, Cañadón Asfalto Formation (Jurassic), Patagonia, Argentina |
| 260 | |c 2013 | ||
| 270 | 1 | 0 | |m Cabaleri, N.G.; Instituto de Geocronología y Geología Isotópica, Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Ciudad Universitaria, C1428EHA, Buenos Aires, Argentina; email: cabaleri@ingeis.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Tasch, P., Volkheimer, W., Jurassic conchostracans from Patagonia (1970) Paleontological Contributions, 50, pp. 1-23. , The University of Kansas, USA | ||
| 504 | |a Turner, J.C.M., Descripción geológica de la Hoja 44d Colan Conuhé, provincia del Chubut (1983) Boletín, 197, pp. 1-92. , Servicio Geológico Nacional, Buenos Aires, Argentina | ||
| 504 | |a Vallatti, P., Conchostracos jurásicos de la Provincia del Chubut, Argentina (1986) 4 Congreso Argentino de Paleontología y Bioestratigrafía, Asociación Paleontológica Argentina, Buenos Aires, Argentina, 4, pp. 29-38 | ||
| 504 | |a Vázquez-Urbez, M., Arenas, C., Pardo, G., Facies fluvio-lacustres de la Unidad superior de la Muela de Borja (Cuenca del Ebro): modelo sedimentario (2002) Revista de la Sociedad Geológica de España, 15, pp. 41-54 | ||
| 504 | |a Volkheimer, W., Quattrocchio, M., Cabaleri, N.G., García, V., Palynology and paleoenvironment of the Jurassic lacustrine Cañadón Asfalto Formation at Cañadón Lahuincó locality, Chubut province, central Patagonia, Argentina (2008) Revista Española de Micropaleontología, 40, pp. 77-96 | ||
| 504 | |a Volkheimer, W., Narváez, P.L., Cabaleri, N.G., Armella, C., Palinología de humedales jurásicos del Miembro Puesto Almada, Formación Cañadón Asfalto (Depocentro Fossati, Cuenca Cañadón Asfalto, Patagonia, Argentina) (2010) 4th Simposio Argentino del Jurásico, p. 42. , (Bahía Blanca) | ||
| 504 | |a Volkheimer, W., Quattrocchio, M.E., Cabaleri, N., Narváez, P.L., Scafati, L., Melendi, D.L., Jurassic lacustrine and palustrine environments in Argentina: a review (2011) 5th International Limnogeology Congress, , Konstanz Alemania, (CD-Rom) | ||
| 504 | |a Woo, K.S., Khim, B.K., Yoon, H.S., Lee, K.C., Cretaceous lacustrine stromatolites in the Gyeongsang Basin (Korea): records of cyclic change in paleohydrological condition (2004) Geosciences Journal, 8, pp. 179-184 | ||
| 504 | |a Wright, P.V., The role of fungal biomineralization in the formation of Early Carboniferous soil fabrics (1986) Sedimentology, 33, pp. 831-838 | ||
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| 504 | |a Yang, W., Feng, Q., Liu, Y., Tabor, N., Miggins, D., Crowley, J.L., Lin, J., Thomas, S., Depositional environments and cyclo- and chronostratigraphy of uppermost Carboniferous-Lower Triassic fluvial-lacustrine deposits, southern Bogda Mountains, NW China - a terrestrial paleoclimatic record of mid-latitude NE Pangea (2010) Global and Planetary Change, 73, pp. 15-113 | ||
| 520 | 3 | |a The Las Chacritas Member is the lower part of the Cañadón Asfalto Formation (Jurassic). The unit is a completely continental limestone succession with volcanic contributions that were deposited during the development of the Cañadón Asfalto Rift Basin (Chubut province, Patagonia, Argentina). A detailed sedimentological analysis was performed in the Fossati depocenter to determine the paleoenvironments that developed in the context of this rift. The Las Chacritas Member represents a carbonate paleolake system with ramp-shaped margins associated with wetlands that were eventually affected by subaerial exposure and pedogenesis. This process is represented by three main subenvironments: a) a lacustrine setting sensu stricto (lacustrine limestone facies association), represented by Mudstones/. Wackestones containing porifera spicules (F1), Intraclastic packstones (F6) and Tabular stromatolites (F10) in which deposition and diagenesis were entirely subaqueous; b) a palustrine setting (palustrine limestone facies association) containing Microbial Mudstones (F2), Intraclastic sandy packstone with ostracode remains (F3), Oncolitic packstone (F5), Brecciated limestone (F7) and Nodular- Mottled limestone (F8) representing shallow marginal areas affected by groundwater fluctuations and minor subaerial exposure; and c) a pedogenic paleoenvironment (pedogenic limestone facies association) including Intraclastic limestone (F4) and Packstones containing Microcodium (F9) facies displaying the major features of subaerial exposure, pedogenic diagenesis and the development of paleosols. The fluvial-palustrine-lacustrine succession shows a general shallow upward trend in which contraction-expansion cycles are represented (delimited by exposure and surface erosion). The variations in the successive formations reflect the responses to fluctuations in a combination of two major controls, the tectonic and local climatic variables. The predominance of the palustrine facies associations was determined by its accommodation space as well as the local climate conditions. The variations in the lacustrine limestone facies associations reflect differential patterns of subsidence within the sub-basin. The diagnostic features of the palustrine limestone facies associations (organic matter (OM) content, microinvertebrate fauna, abundant mud cracks, brecciation, presence of evaporitic minerals) frame the sub-basin in a climatic context intermediate between arid and subhumid conditions. © 2012 Elsevier B.V. |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: This study was supported by grants PIP 5760 and 112/201001/00034 (N.C.) from CONICET . The authors are grateful to Dr. Cabrera for helpful comments that improved the manuscript and to Dr. Jones (Editor), Dr. Alonso-Zarza and an anonymous reviewer for their detailed advice on revising the manuscript. CNEA (Comisión Nacional de Energía Atómica) provided logistical support at the Campamento Los Adobes. We are grateful to Mr. and Mrs. Fossati for allowing access to the Estancia Fossati locality. Dr. Armella assisted us during the field trips. Mr. Llambias prepared the thin sections, and Mr. Giordanengo prepared the graphs. | ||
| 593 | |a Instituto de Geocronología y Geología Isotópica, Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Ciudad Universitaria, C1428EHA, Buenos Aires, Argentina | ||
| 593 | |a Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales, Centro Científico-Tecnológico Mendoza, Consejo Nacional de Investigaciones Científicas y Técnicas, C.C. 330, (5500) Mendoza, Argentina | ||
| 690 | 1 | 0 | |a CARBONATE |
| 690 | 1 | 0 | |a LACUSTRINE |
| 690 | 1 | 0 | |a PALEOENVIRONMENTS |
| 690 | 1 | 0 | |a PALUSTRINE |
| 690 | 1 | 0 | |a ACCOMMODATION SPACE |
| 690 | 1 | 0 | |a CLIMATIC VARIABLES |
| 690 | 1 | 0 | |a DIAGNOSTIC FEATURES |
| 690 | 1 | 0 | |a GROUNDWATER FLUCTUATION |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a LACUSTRINE |
| 690 | 1 | 0 | |a LOCAL CLIMATE |
| 690 | 1 | 0 | |a MUD CRACKS |
| 690 | 1 | 0 | |a PACKSTONE |
| 690 | 1 | 0 | |a PALEO-ENVIRONMENT |
| 690 | 1 | 0 | |a PALEOENVIRONMENTS |
| 690 | 1 | 0 | |a PALUSTRINE |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a RIFT BASIN |
| 690 | 1 | 0 | |a SEDIMENTOLOGICAL ANALYSIS |
| 690 | 1 | 0 | |a SUB-HUMID |
| 690 | 1 | 0 | |a SUBBASINS |
| 690 | 1 | 0 | |a SURFACE EROSION |
| 690 | 1 | 0 | |a UPWARD TREND |
| 690 | 1 | 0 | |a CARBONATES |
| 690 | 1 | 0 | |a CARBONATION |
| 690 | 1 | 0 | |a GROUNDWATER |
| 690 | 1 | 0 | |a PETROLEUM GEOLOGY |
| 690 | 1 | 0 | |a SEDIMENTOLOGY |
| 690 | 1 | 0 | |a LIMESTONE |
| 690 | 1 | 0 | |a CARBONATE SEDIMENT |
| 690 | 1 | 0 | |a CLIMATE CONDITIONS |
| 690 | 1 | 0 | |a CONTINENTAL MARGIN |
| 690 | 1 | 0 | |a DIAGENESIS |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a LACUSTRINE ENVIRONMENT |
| 690 | 1 | 0 | |a LIMESTONE |
| 690 | 1 | 0 | |a MUDSTONE |
| 690 | 1 | 0 | |a PALEOENVIRONMENT |
| 690 | 1 | 0 | |a PALEOSOL |
| 690 | 1 | 0 | |a PEDOGENESIS |
| 690 | 1 | 0 | |a RIFTING |
| 690 | 1 | 0 | |a SEDIMENTOLOGY |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a MICROCODIUM |
| 690 | 1 | 0 | |a OSTRACODA |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a CHUBUT | |
| 650 | 1 | 7 | |2 spines |a PORIFERA |
| 650 | 1 | 7 | |2 spines |a PORIFERA |
| 700 | 1 | |a Benavente, C.A. | |
| 773 | 0 | |d 2013 |g v. 284-285 |h pp. 91-105 |p Sediment. Geol. |x 00370738 |w (AR-BaUEN)CENRE-87 |t Sedimentary Geology | |
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