mid to late Holocene pollen alluvial recordsof the arid Andean piedmont between 33 and 34S Mendoza Argentina:inferences about floodplain evolution

LEANDRO ROJO; ADRIANA MEHL; MARTA PAEZ; MARCELO ZÁRATE

JOURNAL OF ARID ENVIRONMENTS

ACADEMIC PRESS LTD-ELSEVIER SCIENCE LTD

Lugar: Amsterdam; Año: 2012 vol. 77 p. 110 - 122

0140-1963

In arid and semiarid regions of Central West Argentina, paleoenvironmental conditions and history of the Holocene vegetation is still scanty. This paper presents the analysis of palynological records of two Mid- to Late Holocene alluvial sequences (La Escala -LES- and Brazo Abandonado -BA-) in the fluvial basin of the Arroyo La Estacada (33º27? S and 69º03? W), placed in the Cordillera Frontal central piedmont of Mendoza province . Variations in pollen assemblages of the two sequences related to the sub environments developed in the floodplains of the arroyo allowed us to infer the evolution of local plant communities. Between the ca. 4000 and 3000 14C years BP and between ca. 500 and 400 14C years BP, a larger representation of hydrophytic communities related to environments with local water availability was inferred; and between ca. 3000 and 500 14C years BP an increase in shrubby xerophytic communities related to environments with lower water availability was detected. These results permitted to propose that the Holocene pollen spectra fluctuations observed in the alluvial sedimentary sequences prove mainly changes in plant communities of the floodplain environment  in response to the fluvial dynamics of the arroyo.