Seasonal microclimatic dynamics and their impact on the rock art of Cueva del Niño (Aýna, SE Spain)
DOI:
https://doi.org/10.55407/geogaceta113416Keywords:
cave ventilation, cave monitoring, cave paintingsAbstract
The Cueva del Niño (Aýna) contains Palaeolithic cave art in a geological setting of calcarenitic materials. Its microclimate features three thermal zones: the heterothermal zone, influenced by external climate conditions; the thermal inertia zone, with a stable temperature in winter; and a transition zone, regulated by ventilation. In winter, the cave acts as a heat trap, retaining warmth and humidity, while in summer, convective circulation homogenizes the temperature and reduces relative humidity. These processes promote the formation of carbonate concretions through evapocondensation, which may impact the preservation of rock art. The interaction of these factors highlights the need for comprehensive management to maintain environmental balance.
References
Hill, C. A. y Forti, P., 1997. Cave Minerals of the World. National Speleological Society, 463 p.
García-Moreno, A. (Ed.), 2022. La Cueva del Niño (Aýna, Albacete). Estudios en el 50 Aniversario de su descubrimiento. Instituto de Estudios Albacetenses «Don Juan Manuel», 344p. https://doi.org/10.37927/978-84-18165-69-6
Gázquez, F., Quindós, L., Rábago, D., Fuente, I., Celaya, S., & Sainz, C. (2022). Journal of Hydrology, 606, 1-11. https://doi.org/10.1016/j.jhydrol.2021.127416
Sánchez-Gómez, M. y Sanz, D., 2022. En: La Cueva del Niño (Aýna, Albacete). Instituto de Estudios Albacetenses.
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Copyright (c) 2025 David Sanz, Luis Trigueros-Ramos, Diego Gil, Iordanka Dountcheva, Alejandro García-Moreno, Alberto Córcoles, Mario Sánchez-Gómez

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