Mid- to Late Holocene pollen and alluvial record of the arid Andean piedmont between 33° and 34°S,Mendoza, Argentina: Inferences about floodplain evolution |
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| Institution: | 1. Department of Biological, Geological and Environmental Sciences, University of Catania, Via Antonino Longo 19, 95125 Catania, Italy;2. Czech University of Life Sciences Prague, Faculty of Environmental Sciences, Kamýcká 129, 165 21 Praha 6, Czech Republic;1. INENCO (UNSa – CONICET), Av. Bolivia 5150, A4400FVY, Salta, Argentina;2. Istituto per la Dinamica dei Processi Ambientali, Consiglio Nazionale delle Ricerche, Area della Ricerca CNR - ARM3, Via Roberto Cozzi 53, 20125 Milano, Italy;3. College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331-5503, USA;1. GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, 24148 Kiel, Germany;2. V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Kosigin str. 19, 119991 Moscow, Russia;3. Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Strasse 10, 24118 Kiel, Germany;1. Institute of Geography, University of Bern, Hallerstrasse 12, 3012 Bern, Switzerland;2. GeoQuEST Research Centre, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, NSW 2522, Australia;3. Department of Physical Geography and Quaternary Geology, Stockholm University, 10961 Stockholm, Sweden |
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| Abstract: | 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 (33°27′S and 69°03′W), placed in the Cordillera Frontal central piedmont of Mendoza province. Variations in pollen assemblages of the two sequences related to the 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 led us 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. |
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