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Original Articles

Diatom-based reconstruction of Middle to Late Holocene paleoenvironments in Lake Lonkoy, southern Pampas, Argentina

Pages 473-486 | Received 10 Aug 2012, Accepted 27 Sep 2013, Published online: 06 Nov 2013
 

Abstract

Diatoms recovered from shallow Lake Lonkoy sediment core in southern Pampas, Argentina, were studied in order to assess past environmental conditions. A total of 47 samples were selected from a 1.42-m long core that spans the last 4840 cal. years. Diatoms were extracted by chemical cleaning and studied under light and scanning electron microscopy. A total of 89 diatom taxa were recorded, including 36 taxa that reached>2% relative abundance and were used in statistical analyses. A cluster analysis allowed five significant diatom association zones (DAZ) to be defined. DAZ I (142–92 cm) was dominated by Cyclotella meneghiniana Kützing, Cocconeis placentula Ehrenberg and Nitzschia hustedtiana Salah, and a low abundance of aerophilic taxa, indicating brackish water conditions probably related to the Holocene sea-level high stand. DAZ II (90–48.5 cm) was dominated by C. meneghiniana and Aulacoseira granulata (Ehrenberg) Simonsen, representing a period of high nutrient loading and turbid conditions in the lake, associated with higher water levels and lower salinities than the environmental conditions in DAZ I. The upper 50 cm of the core (DAZ III to V) showed an increase in the dominance of brackish epiphytic and hypereutrophic benthic taxa, indicating an increase in nutrient concentrations associated with agricultural human impacts in the basin. Overall, diatoms allowed major paleoenvironmental changes to be inferred for the lake during the Holocene.

Acknowledgements

I would like to thank the GEPaCo Team (S. Stutz, D. Navarro, M. Tonello, C. De Francesco, M. A. González Sagrario, E. Tietze, P. Cristini and L. Ferrero) for their support in the core extraction and sampling, as well as for the long and inspirational discussions. Mónica Oppedisano assisted in SEM microphotography. Josefina Pueyrredón de Lanús gave us permission to work on Lake Lonkoy. C. De Francesco, S. Stutz, R. Flower and two anonymous reviewers made helpful commentaries on earlier versions of this manuscript. Financial support for this work was provided by Agencia Nacional de Promoción Científica y Tecnológica (PICT 2008-0088), CONICET (PIP 2010-0063), and University of Mar del Plata (EXA 587/12). G.S.H. is a member of the Scientific Research Career of the Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET).

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