Bioturbaciones de Tagelus plebeius (Lightfoot, 1786) (Mollusca: Bivalvia) en un ambiente estuárico holoceno (río Quequén Grande, Buenos Aires, Argentina)

Elongated traces´ showing a lower v-shape closed end have been identified in mid Holocene estuarine deposits exposed along the lower reach of the Quequén Grande River Argentina (38"34´35" S and 58"42´45" W) associated with shells in life position of the infaunal bi´al´e Tagelus p...

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Detalles Bibliográficos
Autores: de Francesco, Claudio German, Zárate, Marcelo Arístides
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2001
País:Argentina
Institución:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:español
OAI Identifier:oai:ri.conicet.gov.ar:11336/81828
Acceso en línea:http://hdl.handle.net/11336/81828
Access Level:acceso abierto
Palabra clave:Holoceno
Estuarios
Tagelus Plebeius
Bioturbaciones
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Descripción
Sumario:Elongated traces´ showing a lower v-shape closed end have been identified in mid Holocene estuarine deposits exposed along the lower reach of the Quequén Grande River Argentina (38"34´35" S and 58"42´45" W) associated with shells in life position of the infaunal bi´al´e Tagelus plebeius (Líghtfoot). These traces, Iocated in a stratigraphic level dated in circa 6,900 years 14 C B.p, were originated by the burrowing activity of T.  plebeius based upon  the cómparison of their morphological characteristics (width, general shape, colour) with those of T. plebeius and the traces resulting from its burrowing activity at present estuarine environments in the region. The high percentages- of the estuarine gastropod Heleobia aus- tralis (d´Orbigny; found in the sedimentary infilling  of the traces, come from the overlying strata´ abundant Heleobia australis remains. The traces are stratigraphically transgressive within a depth interval of up to 80 cm