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Sedimentary multiproxy response to hydroclimatic variability in Lagunillo del Tejo (Spain)

  • Chapter
Palaeolimnological Proxies as Tools of Environmental Reconstruction in Fresh Water

Part of the book series: Developments in Hydrobiology ((DIHY,volume 208))

Abstract

Lagunillo del Tejo is a small groundwater-fed sinkhole lake in the karst region of the Iberian Range (central-eastern Spain), which undergoes significant lake level fluctuation in response to rainfall variability. The aim of this study is to understand the record of water level fluctuations in Lagunillo del Tejo over the last two-and-a-half centuries. This information could be used in future studies to interpret longer sedimentary sequences. We analysed photosynthetic pigments, diatoms and cladoceran remains in sediment sequences recovered from the deepest part of the lake. The paleoecological proxies traced two different communities which have switched their prevalence during the past: (1) a planktonic community of algae, including diatoms, chlorophytes, cryptophytes and cyanobacteria, and phototrophic bacteria associated with higher lake level and water column seasonal stratification; (2) a littoral community with the higher levels of macrophyte pigments and associated epiphytic diatoms and chydorids, all of which indicate lower lake level. The levels of coherence between different proxies, each having an independent mechanistic link to lake-level variability, enhance the reliability of palaeolimnological inferences. The high-resolution stratigraphical data from the upper part of the core was compared with lake-level inferences from instrumental rainfall series (1859–2005) to establish the correspondence between Lagunillo del Tejo sediment sequences and climate record.

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Authors and Affiliations

  1. Department of Microbiology and Ecology, University of Valencia, 46100, Burjassot, Valencia, Spain

    Lidia Romero-Viana, M. Rosa Miracle, Charo López-Blanco, Antonio Camacho & Eduardo Vicente

  2. Facultad de Estudios Superiores Iztacala, Universidad Nacional Autónoma de México, CP-54090, Mexico, Mexico

    Estela Cuna & Gloria Vilaclara

  3. Departament de Física — Institut de Ciència i Tecnologia Ambientals, Universitat Autónoma de Barcelona, 08193, Bellaterra, Spain

    Jordi Garcia-Orellana

  4. School of Marine and Atmospheric Sciences, State University of New York, Stony Brook, NY, 11794-5000, USA

    Jordi Garcia-Orellana

  5. Department of Chemistry, University of York, Heslington, York, Y010 5DD, UK

    Brendan J. Keely

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  1. Lidia Romero-Viana
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Correspondence to Lidia Romero-Viana .

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  1. Department of Botany, Hungarian Natural History Museum, 1476, Budapest, P.O. Box 222, Hungary

    Krisztina Buczkó

  2. West-Transdanubian District Water Authority, H-8360, Keszthely, Csik F. str. 1, Hungary

    János Korponai

  3. Department of Chemistry and Environmental Sciences, University of West Hungary, Szombathely, Hungary

    János Korponai

  4. Department of Limnology, University of Pannonia, Egyetem u. 10, 8200, Veszprém, Hungary

    Judit Padisák

  5. U.S. Geological Survey, 345 Middlefield Road, Menlo Park, CA, 94025, USA

    Scott W. Starratt

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Romero-Viana, L. et al. (2009). Sedimentary multiproxy response to hydroclimatic variability in Lagunillo del Tejo (Spain). In: Buczkó, K., Korponai, J., Padisák, J., Starratt, S.W. (eds) Palaeolimnological Proxies as Tools of Environmental Reconstruction in Fresh Water. Developments in Hydrobiology, vol 208. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-3387-1_14

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