CICYTTP   12500
CENTRO DE INVESTIGACION CIENTIFICA Y DE TRANSFERENCIA TECNOLOGICA A LA PRODUCCION
Unidad Ejecutora - UE
capítulos de libros
Título:
ANÁLISIS FITOLÍTICOS DE DEPÓSITOS EÓLICOS PARCIALMENTE EDAFIZADOS (PLEISTOCENO TARDÍO-HOLOCENO) EN LA REGIÓN DE TANDILIA (PROVINCIA DE BUENOS AIRES, ARGENTINA)
Autor/es:
MARÍA DE LOS MILAGROS COLOBIG, NOELIA ISABEL PATTERER, ALEJANDRO FABIÁN ZUCOL, GUSTAVO MARTÍNEZY ESTEBAN PASSEGGI
Libro:
IV Congreso Argentino de Cuaternario y Geomorfología, XII Congresso da Associação Brasileira de Estudos do Quaternário y II Reunión sobre el Cuaternario de América del Sur
Editorial:
Universidad Nacional de La Plata, 2009
Referencias:
Lugar: La Plata; Año: 2009; p. 280 - 289
Resumen:
The phytolith assemblages of aeolian depositional sequences with partially edaphic conditions (Late Pleistocene- Holocene) from Tandilia region (Buenos Aires Province, Argentina) were analyzed. Siliceous remains were obtained by densimetric separation (with sodium polytungstate as heavy liquid) of the cleaned samples (with elimination of carbonates, organic matter and dispersion of clastic elements). The multivariate analysis of phytolith assemblages composition allows to differ two different groups across the studied profile. The lower component was dominated by morphotypes with danthoniod affinity, the presence of arecoid morphotypes, and a scarce presence of chloridoid, stipoid and panicoid elements. The upper component of the sequence is characterized by a smaller abundance of danthoniod elements and an important increase of phytoliths with stipoid and chloridoid affinity in the mean levels that decreases towards the top of the profile where the relative frequency of panicoid phytoliths increases. In this unit different ciperoid morphotypes were also observed. This analysis allows to interpret that from the parental deposits, the development of this sequence was accompanied in its initiated stages by a vegetation conformed by stipoid and chloridoid elements mainly, with a scarce water availability. Later would have been replaced by a panicoid dominated community, which added to the evidence of presence of sedges allows to suppose a superior hydric availability.