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- W5907427 abstract "Aridos 1 and Aridos 2, excavated in 1976 (Santonja et al. 1980), are situated within the Arganda Formation I (Fig. 1). This formation, about 30 m thick, is part of a terrace sunken syndepositionally due to an underlying karst (Perez-Gonzalez 1971). Based on its relative position in the terrace system of the Jarama valley and correlations with other terrace systems of the central Iberian Peninsula, Arganda I has been dated as Middle Pleistocene (PerezGonzalez 1994). The fauna found in this formation, especially the microfauna of Aridos 1 (Lopez Martinez 1980), is considered to be of a younger age than Cullar-Baza and older than the TD 10 and G II levels of Atapuerca, and represent climatic conditions similar to the present (Sese & Sevilla 1996). According to chronological estimates proposed for Atapuerca (Perez-Gonzalez et al., in press), the age of the Aridos sites might correspond to isotope stages 9 or 11. 2. ARIDOS-1" @default.
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- W5907427 date "2001-01-01" @default.
- W5907427 modified "2023-09-24" @default.
- W5907427 title "Elephants in the archaeological sites of Aridos (Jarama valley, Madrid, Spain)." @default.
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