INVESTIGADORES
TRIPALDI Alfonsina
artículos
Título:
Late Quaternary paleoenvironments and paleoclimatic conditions in the distal Andean piedmont, southern Mendoza, Argentina
Autor/es:
TRIPALDI, A.; ZÁRATE, M.A.; BROOK, G.; GUO-QIANG LI
Revista:
QUATERNARY RESEARCH
Editorial:
ACADEMIC PRESS INC ELSEVIER SCIENCE
Referencias:
Lugar: Ámsterdam,; Año: 2011 vol. 76 p. 253 - 263
ISSN:
0033-5894
Resumen:
The Andean piedmont of Mendoza is a semiarid region covered
by very extensive and partially vegetated dune fields consisting of mostly
inactive aeolian landforms of diverse size and morphology. This paper is focused
on the San Rafael plain (SRP) environment, situated in the distal Andean
piedmont of Mendoza (34º 30´S), and reports the sedimentology and OSL chronology
of two representative exposures of late Quaternary deposits discussing their
paleoenvironmental and paleoclimatic significance. Eleven facies, including
channel, floodplain, fluvio-aeolian interaction, reworked pyroclastic and
aeolian deposits, were described and grouped into two facies associations (FA1
and FA2). FA1 was formed by unconfined sheet flows, minor channellized streams
and fluvial-aeolian interaction processes. FA2 was interpreted as aeolian dune
and sand sheet deposits. OSL chronology from the SRP sedimentary record
indicates that between ca. 58-39 ka and ca. 36-24 ka, during MIS 3, aggradation
was governed by ephemeral fluvial processes (FA1), under generally semiarid
conditions. During MIS 2, the last glacial maximum (ca. 24-12 ka), a major
climatic shift to much more arid conditions is documented by significant
aeolian activity (FA2) that became the dominant sedimentation process north of
the Diamante-Atuel fluvial system. The inferred paleoenvironmental conditions
from the SRP sections are in broad agreement with regional evidence.