A paleoclimatic review of southern South America during the late Paleozoic: A record from icehouse to extreme greenhouse conditions
This paper provides a review of the Late Mississippian to Permian paleoclimatic history for southern South America based on lithologic indicators, biostratigraphic information, and chronostratigraphic data. The region is divided into three major types of basins: 1. Eastern intraplate basins (e.g., P...
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Elsevier Inc.
2014
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| LEADER | 58199caa a22030737a 4500 | ||
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| 001 | PAPER-14623 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518204511.0 | ||
| 008 | 190411s2014 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84896401882 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Limarino, C.O. | |
| 245 | 1 | 2 | |a A paleoclimatic review of southern South America during the late Paleozoic: A record from icehouse to extreme greenhouse conditions |
| 260 | |b Elsevier Inc. |c 2014 | ||
| 270 | 1 | 0 | |m Limarino, C.O.; Departamento de Ciencias Geológicas - IGEBA, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires - CONICET, Ciudad Universitaria, Pabellón 2, 1428 Buenos Aires, Argentina; email: limar@gl.fcen.uba.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a This paper provides a review of the Late Mississippian to Permian paleoclimatic history for southern South America based on lithologic indicators, biostratigraphic information, and chronostratigraphic data. The region is divided into three major types of basins: 1. Eastern intraplate basins (e.g., Paraná Basin), 2. Western retroarc basins (e.g., Paganzo Basin) and 3. Western arc-related basins (e.g., Río Blanco Basin). Four major types of paleoclimatic stages are recognized in these basins: 1. glacial (late Visean-early Bashkirian), 2. terminal glacial (Bashkirian-earliest Cisuralian) 3. postglacial (Cisuralian-early Guadalupian), and 4. semiarid-arid (late Guadalupian-Lopingian). The glacial stage began in the late Visean and continued until the latest Serpukhovian or early Bashkirian in almost all of the basins in southern South America. During the Bashkirian-earliest Cisuralian (terminal glacial stage), glacial deposits disappeared almost completely in the western retroarc basins (e.g., Paganzo Basin) but glaciation persisted in the eastern basins (e.g., Paraná and Sauce Grande Basins). A gradual climatic amelioration (postglacial stage) began to occur during the earliest Permian when glacial deposits completely disappeared across all of South America. During this interval, glacial diamictites were replaced by thick coal beds in the Paraná Basin while north-south climatic belts began to be delineated in the western basins, which were likely controlled by the distribution of mountain belts along the Panthalassan Margin of South America. Towards the late Permian, climatic belts became less evident and semiarid or arid conditions dominated in the southern South America basins. Eolian dunes, playa lake deposits, and mixed eolian-fluvial sequences occur in the Paraná Basin and in the western retroarc basins. Volcanism and volcaniclastic sedimentation dominated along the western margin of South America at that time. The stratigraphic record obtained in southern South America supports a long duration transition from icehouse to extreme greenhouse conditions. © 2013 International Association for Gondwana Research. |l eng | |
| 536 | |a Detalles de la financiación: National Science Foundation, OPP-0943935, OPP-0944532, OISE-0825617 | ||
| 536 | |a Detalles de la financiación: Agencia Nacional de Promoción Científica y Tecnológica, PICT 1499, PIP 512 | ||
| 536 | |a Detalles de la financiación: University of Wisconsin-Milwaukee, UW Milwaukee | ||
| 536 | |a Detalles de la financiación: We thank Dr. Zhong Chen and anonymous reviewers for their constructive reviews of the manuscript. Financial support for this study was provided by ANPCyT (Agencia Nacional de Promoción Científica y Tecnológica) PICT 1499 and Conicet — PIP 512 grants. Support from the National Science Foundation (grants OISE-0825617 , OPP-0943935 , and OPP-0944532 ) to the University of Wisconsin-Milwaukee is also acknowledged. Paleogeographic reconstructions were performed by using GMAP XP Standard Edition by T.H. Torsvik. | ||
| 593 | |a Departamento de Ciencias Geológicas - IGEBA, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires - CONICET, Ciudad Universitaria, Pabellón 2, 1428 Buenos Aires, Argentina | ||
| 593 | |a Museo Argentino de Ciencias Naturales Bernardino Rivadavia (CONICET), Av. Ángel Gallardo 470, 1405 Buenos Aires, Argentina | ||
| 593 | |a Centro de Investigaciones Geológicas (FCNyM, UNLP - CONICET), Calle 1 no. 644, 1900 La Plata, Argentina | ||
| 593 | |a Facultad de Ciencias Naturales, Sede Esquel, Universidad Nacional de la Patagonia - LIEB (CONICET), Edificio de Aulas RN 259, Km. 16.5, 9200 Esquel, Chubut, Argentina | ||
| 593 | |a Department of Geosciences, University of Wisconsin, Milwaukee, WI 53201, United States | ||
| 593 | |a Department of Geology, University of California, One Shields Avenue, Davis, CA 95616, United States | ||
| 690 | 1 | 0 | |a GONDWANA |
| 690 | 1 | 0 | |a LATE PALEOZOIC |
| 690 | 1 | 0 | |a PALEOCLIMATE |
| 651 | 4 | |a SOUTH AMERICA | |
| 700 | 1 | |a Césari, S.N. | |
| 700 | 1 | |a Spalletti, L.A. | |
| 700 | 1 | |a Taboada, A.C. | |
| 700 | 1 | |a Isbell, J.L. | |
| 700 | 1 | |a Geuna, S. | |
| 700 | 1 | |a Gulbranson, E.L. | |
| 773 | 0 | |d Elsevier Inc., 2014 |g v. 25 |h pp. 1396-1421 |k n. 4 |p Gondwana Res. |x 1342937X |t Gondwana Research | |
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| 856 | 4 | 0 | |u https://doi.org/10.1016/j.gr.2012.12.022 |y DOI |
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