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https://doi.org/10.1016/j.quaint.2016.02.036

has been cited by the following article:

• TITLE: Isotopic and Petrographic Evidence as a Proxy in Paleoclimatic Reconstructions from Flowstones in Southern Spain

  AUTHORS: Concepción Jiménez de Cisneros, Antonio González-Ramón, Cristina Sequero, Bartolomé Andreo, Ian J. Fairchild

  KEYWORDS: Speleothems, Flowstones, Fabrics, Isotopic Characterization, Cave, Paleoclimatic Changes

  JOURNAL NAME: Open Journal of Geology, Vol.10 No.6, June 10, 2020

  ABSTRACT: Changes in the morphology and mineralogy of speleothems (flowstones) clearly respond to climate-related phenomena, such as drip rate variability and temperature-modulated cave ventilation. Detailed petrographic observations have been coupled with δ18Oand δ13C values. Fabrics may show changes related to variations in supersaturation, drip rate or input of detrital particles or organic compounds. Fabrics formed under relatively constant and regular drips (columnar compact, open and elongated) show similar δ18O and δ13C values, which are more negative than those of micrite and microsparite. The combination of internal microstratigraphy studies and isotopic data (δ18O and δ13C) from two flowstones collected from two caves in the north of Almeria province (SE Spain), suggest a spectrum of environmental conditions ranging from wetter to drier periods. Both records constitute a very useful tool for screening and interpreting high-resolution paleoclimate reconstructions.