CICTERRA   20351
CENTRO DE INVESTIGACIONES EN CIENCIAS DE LA TIERRA
Unidad Ejecutora - UE
artículos
Título:
Darriwilian (Middle Ordovician) d13Ccarb chemostratigraphy in the Precordillera of Argentina: Documentation of the middle Darriwilian Isotope Carbon Excursion (MDICE) and its use for intercontinental correlation
Autor/es:
ALBANESI, G. L., BERGSTRÖM, S. M., SCHMITZ, B., F. SERRA, N. FELTES, G. VOLDMAN
Revista:
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
Editorial:
ELSEVIER SCIENCE BV
Referencias:
Lugar: Amsterdam; Año: 2013 p. 48 - 63
ISSN:
0031-0182
Resumen:
Although documented from Estonia, Latvia, Sweden, eastern North America, and China, the Middle Ordovician(Darriwilian) positive δ13C excursion known as the MDICE has previously not been recognized with certainty inSouth America. Themost promising region in South America for detailed Middle Ordovician carbon isotope researchis the Precordillera of western Argentina, where there are many excellent exposures of biostratigraphicallywell-dated carbonate successions spaning the Tremadocian through Sandbian stratigraphic interval. For this project,we collected numerous isotope and conodont samples from the middle Darriwilian Las Chacritas andAguaditas formations at their type localities, which yielded important biostratigraphic data as well as informativeδ13Ccarb values. In the E. pseudoplanus Zone in the upper half of the Las Chacritas Formation, there is a relativelymodest but distinct δ13Ccarb excursion. Because its stratigraphic position and magnitude closely agree with theMDICE in other parts of the world, we recognize it as the first firm record of this excursion in South America.The fact that the δ13Ccarb curve from the Las Aguaditas Formation shows no such excursion is due to the existenceof a stratigraphic gap between the Lower and Middle Members of this formation that cuts out the excursioninterval. The Precordilleran MDICE is used for detailed long-range correlations with successions in Baltoscandia,Newfoundland, and China illustrating the usefulness of also this δ13Ccarb excursion as a global stratigraphic tool.A recent proposal of a greatly extended chronostratigraphic range of the Table Head Group on Newfoundland isrejected based on well-established biostratigraphic evidence.