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Redalyc.Lower Paleozoic Biostratigraphy of South America Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España ALBANESI, G.L.; ORTEGA, G. Lower Paleozoic Biostratigraphy of South America: New contributions and advances Geologica Acta: an international earth science journal, vol. 6, núm. 2, junio, 2008, pp. 111-113 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50513115001 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol.6, Nº 2, June 2008, 111-113 DOI: 10.1344/105.000000245 Available online at www.geologica-acta.com Lower Paleozoic Biostratigraphy of South America: New contributions and advances G.L. ALBANESI and G. ORTEGA CONICET - Museo de Paleontología, Facultad de Ciencias Exactas, Físicas y Naturales, Universidad Nacional de Córdoba CC 1598, 5000 Córdoba, Argentina. E-mail Albanesi: [email protected] E-mail Ortega: [email protected] The early Paleozoic was the most critical time inter- record (see Aceñolaza, 2003 and 2005, and cites herein). val for the diversification of the biota on planet Earth. A number of contributions on the lower Paleozoic basin This phenomenon was driven by important paleoconti- research, biostratigraphy and paleogeography have been nental and paleoceanographic changes, caused by inten- gathered in these issues and makes up a significant deal sive plate tectonic and climatic processes. The Cambrian of basic knowledge on this subject. The present issue explosion of life providing bauplans, the great Ordovi- consists of a series of selected papers that were presented cian biodiversification event, the second most important as abstracts in the “9º Congreso Argentino de Paleon- mass extinction of life in the Phanerozoic that occurred tología y Bioestratigrafía” held in Córdoba, Argentina, in the Late Ordovician, and the appearance of land on September 18-22, 2006. These contributions were plants represent benchmarks in this evolutionary process invited papers from the total presented in the 2nd sym- (e.g., Albanesi et al., 2003; Webby et al., 2004; Mun- posium of the congress, entitled “Bioestratigrafía del necke and Servais, 2007; Li et al., 2007) Paleozoico inferior” (i.e. Lower Paleozoic Biostratigra- phy). Sixteen co-authors contributed six papers that The chronostratigraphic status of the lower Paleo- compose this varied volume on lower Paleozoic paleon- zoic, indispensable to correlate globally all of these tological and biostratigraphic subjects. important events, has changed dramatically in the last decade. The International Commission on Stratigraphy The paper by Bordonaro et al. (this issue) proposes a (ICS) of the International Union of Geological Sciences biostratigraphic model for the early Marjumian (Middle (IUGS), through the work of respective subcommissions Cambrian) of the Argentine Precordillera involving trilo- for each time period, has made significant advances in bite biofacies and biozonation. The trilobite assemblages establishing new global chronostratigraphic references. represent three biofacies that respond to segregated envi- The Ordovician, Silurian and Devonian systems have ronmental conditions within an essentially synchronous been fully established and the Cambrian System is being interval that correspond to three biozones defined previ- rapidly reorganized in terms of stages, series and respec- ously for the Middle Cambrian of western Laurentia. tive intra-systemic boundaries to accomplish the interna- tional time chart (see most recent advances at ICS-IUGS Zeballo et al. (this issue) provide new paleontologi- web site: www.stratigraphy.org) cal data for the Eastern Cordillera of northwestern Argentina, in particular on conodont and graptolite fau- This Geologica Acta issue is included in a series of nas, which allow for the refinement of regional biostrati- them that have been published thanks to the editorial graphic schemes. The analysis of the conodont fauna efforts carried out by research members of the CONI- reveals a succession of the conodont zones Cordylodus CET who focus its activity on the lower Paleozoic angulatus, Paltodus deltifer, and Acodus deltatus-Parois- © UB-ICTJA 111 G.L. ALBANESI and G. ORTEGA todus proteus. Graptolites of the Aorograptus victoriae ACKNOWLEDGEMENTS Zone are linked with conodonts of the Acodus deltatus- Paroistodus proteus Zone, and trilobites of the Noto- peltis orthometopa Zone. The authors conclude that the We thank the CONICET, ANPCyT (FONCyT), and Uni- Early Ordovician conodont fauna of northwestern versidad Nacional de Córdoba, Argentina, for their continuing Argentina represent a separate province in the southern support on our research work, and especially to the contribu- South American margin of Gondwana. tors of this volume, who made it all possible. The editors are grateful to the colleagues and friends who kindly helped with An Early Ordovician (Floian) conodont fauna is the reviewing of the papers included in this Geologica Acta reported for the first time from the Eastern Cordillera of issue. These reviewers made important contributions by Peru by Gutiérrez-Marco et al. (this issue). The cono- improving critically the final version of the papers. We thank dont assemblage is referred to the upper part of the all of them for this responsibility: Allison Palmer, Franco Oepikodus evae Zone and characterizes a South Gond- Tortello, Claudia Rubinstein, Dianne Edwards, Stig Berg- wana Province of the Cold Domain in the Shallow-Sea ström, Svend Stouge, Yong Yi Zhen, Juan Carlos Gutiérrez- Realm. Regarding previous biostratigraphic reports on Marco, Daniel Goldman, Edsel Brussa, Alfred Lenz, Anita the San José Formation, this conodont record in the Löfgren, Enrico Serpagli, and Christopher Barnes. We also study area indicates a highly diachronic lower boundary acknowledge gratefully the editorial board of Geologica Acta, of the formation at a regional scale. in particular the scientific editor Lluís Cabrera and the manag- ing editor Angeles Santos, and also the whole managing scien- A conodont-graptolite high resolution biostratigra- tific committee of the journal for supporting us with continu- phy is presented by Ortega et al. (this issue) for Middle- ous professional assistance and enthusiasm throughout the Upper Ordovician siliciclastic facies of the Central Pre- editorial process of this publication. cordillera, Argentina. These records verify that the lower strata of the Sierra de La Invernada Formation are located to the east, contrary to conclusions of previous studies. REFERENCES The deposition of this unit developed as a response to sea level changes, which are also made evident by varia- Aceñolaza, G.F. (ed.), 2003. Advances in the knowledge of the tions on the graptolite-conodont faunas along the revisit- Cambrian System. Geologica Acta, 1(1), 1-150. ed section. Six graptolite biozones and corresponding Aceñolaza, G.F. (ed.), 2005. Ordovician revisited: Recon- conodont zones are determined in this section, allowing structing a unique period in Earth history. Geologica Acta, for regional and global correlations of the upper Darri- 3(4), 307-409. wilian, Sandbian and lower Katian stages (Middle- Albanesi, G.L., Beresi, M.S., Peralta, S.H. (eds.), 2003. Upper Ordovician). Ordovician from the Andes. Proceedings of the 9th Inter- national Symposium on the Ordovician System, Serie Cor- The lower Silurian Itacurubí Group exposed in the east- relación Geológica 17, INSUGEO, Tucumán: 1-552. ern Paraguay yielded an interesting graptolite fauna that is Bordonaro, O.L., Banchig, A.L., Pratt, B.R., Raviolo, M.M., described and discussed firstly by Uriz et al. (this issue) The 2008. Trilobite-based biostratigraphic model (biofacies and Llandovery monograptids of the Vargas Peña Formation biozonation) for the Middle Cambrian carbonate platform from this group allows the correlation of units from the East- of the Argentina Precordillera. Geologica Acta, 6(2), 115- ern Cordillera and the Precordillera of Argentina. Regarding 129. paleoenvironments, the association of graptolites and inver- Di Pasquo, M.M., Noetinger, S., 2008. First record of Early tebrate macrofossils of the Vargas Peña Formation suggest Devonian (Lochkovian) flora from the Santa Rosas Forma- an oxygen-rich environment in a shallow shelf. tion – Alarache, Southern Bolivia. Geologica Acta, 6(2), 191-210. Finally, an association of plants and palynomorphs Gutiérrez-Marco, J.C., Albanesi, G.L., Sarmiento, G.N., Car- from the Lower Devonian Santa Rosa Formation at lotto, V., 2008. An Early Ordovician (Floian) Conodont Angosto de Alarache, Cinco Picachos Range in South Fauna from the Eastern Cordillera of Peru (Central Andean Bolivia, is presented in the contribution by Di Pasquo Basin). Geologica Acta, 6(2), 147-160. and Noetinger (this issue). Taphonomic evidences from Li, J., Fan, J., Percival, I. (eds.), 2007. The global Ordovician the early plant remains and preserved palynomorphs and Silurian. Proceedings of the 10 International Sympo- added to the absence of rooting systems allow interpret- sium on the Ordovician System. Acta Palaeontologica ing the fossil remains as para-autochthonous to allo- Sinica, 46, 1-566. chthonous, probably due to deposition under very low Munnecke, A., Servais, T. (eds.), 2007. Early Palaeozoic energy
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