• DOI:10.1023/A:1020319923164
• Corpus ID: 127610981

Sunspot-like and ENSO/NAO-like periodicities in lacustrinelaminated sediments of the Pliocene Villarroya Basin (La Rioja,Spain)

@article{Muoz2002SunspotlikeAE,
  title={Sunspot-like and ENSO/NAO-like periodicities in lacustrinelaminated sediments of the Pliocene Villarroya Basin (La Rioja,Spain)},
  author={Arsenio Mu{\~n}oz and Jorge Ojeda and Bel{\'e}n S{\'a}nchez-Valverde},
  journal={Journal of Paleolimnology},
  year={2002},
  volume={27},
  pages={453-463}
}

• A. Muñoz, J. Ojeda, B. Sánchez-Valverde
• Published 1 May 2002
• Environmental Science, Geography
• Journal of Paleolimnology

This is a study of an extremely good outcrop of 1745 varves inthe Villarroya Pliocene Basin (Spain). The thicknesses of the light and darklayers, which were obtained from enlarged photograph negatives, are dealt withseparately, and three time series, of light, dark, and the sum of both layers,are performed. Periodicities of about 12, 6–7 and 2–3 years havebeen obtained. The origin of the recurrent behaviour of the sediments withthese periods could be related to natural phenomena like sunspot cycles, ElNiño-Southern Oscillation (ENSO), North Atlantic Oscillation (NAO) andQuasi-biennial Oscillation (QBO), as these phenomena are capable of modulatingthe climate in this frequency band. From our point of view, there could be aclose relationship between sedimentation in the Villarroya Basin and thesenatural phenomena, which is moved through climate. The light layers record therun-off of gastropods, ostracods and charophytes from a seasonal productivitycycle, and are generated during late summer and autumn. It seems clear that theclimatic information provided by these cycles corresponds mainly to summertime, which would be translated into a variation of the light layer thicknessdue to a more or less intense development of the flora and fauna, being thickerin years of higher temperatures and thinner in years of lower temperatures.Considering the results, we would suggest that the sedimentation of thesematerials in the Pliocene was driven by solar activity or/and ENSO, NAO, andQBO phenomena. Nowadays these phenomena produce rainfall and temperaturechanges with the cyclicities shown in this study and we think they could haveoperated in the same way in Pliocene times.