Climate changes during the Early-Middle Triassic transition in the E. Iberian plate and their palaeogeographic significance in the western Tethys continental domain
Olenekian alternating arid to semi-arid climates in near equator continental areas
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Two main arid periods located at the end of the Smithian and middle of the Spathian
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Olenekian alternating arid to semi-arid climates in periods shorter than 0.4 m.a
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A late Spathian first subhumid period coincides with the beginning of fauna and flora recovery.
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South of the Iberian Basin a generalized wetter climate extended towards the equator during the Olenekian–Anisian
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