2009
DOI: 10.1016/j.quaint.2008.07.010
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Landscape and climatic changes during the end of the Late Prehistory in the Amblés Valley (Ávila, central Spain), from 1200 to 400cal BC

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Cited by 34 publications
(16 citation statements)
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“…This transition correlates with a climatic shift towards cold conditions, detected at 2.8 ka cal BP over the North Atlantic (van Geel et al, 1996;Bond et al, 1997). For the Avila Range, directly to the west of the Jarama catchment, López-Sáez et al (2009) documented an abrupt climatic change at 2.8 ka cal BP, leading to a transition from arid and warm conditions to a cold and humid period resulting in a century-long ecological crises (Fig. 10o).…”
Section: Mid-holocene Warm Period and Climatic Collapse (7e5 Ka Cal Bp)mentioning
confidence: 70%
“…This transition correlates with a climatic shift towards cold conditions, detected at 2.8 ka cal BP over the North Atlantic (van Geel et al, 1996;Bond et al, 1997). For the Avila Range, directly to the west of the Jarama catchment, López-Sáez et al (2009) documented an abrupt climatic change at 2.8 ka cal BP, leading to a transition from arid and warm conditions to a cold and humid period resulting in a century-long ecological crises (Fig. 10o).…”
Section: Mid-holocene Warm Period and Climatic Collapse (7e5 Ka Cal Bp)mentioning
confidence: 70%
“…Si en las primeras fases del Bronce Final se produjo un aumento considerable de la humedad (Burakov et al 2005;López-Sáez et al 2014), es también posible que en torno al siglo IX a. C. el clima sufriera un nuevo deterioro (Jaouadi et al 2016). Hay que tener en cuenta que la fecha proporcionada por nuestra muestra se sitúa antes de la transición al Subat-lántico y aunque, al menos en áreas más septentrionales, se ha planteado que este no solo implica condiciones más frías sino también más húmedas entre 850 y 750 a. C. (López-Sáez et al 2009), la disminución de precipitaciones llega hasta el 600/500 a. C. cuando se asientan las condiciones frías, como se ha indicado para otras áreas (Gaigalas 2004;Van Mourik y Slotboom 2018).…”
Section: Discussionunclassified
“…BP. [90][91][92] and within the Iberian-Roman Humid Period, when climatic conditions were mostly warm and humid [86,87]. At Brezoso and El Perro, Betula slightly spread following this fire episode alongside Erica under low anthropogenic impact, just indicated by minor increases in Cardueae, Asteraceae, and Poaceae.…”
Section: Climatic and Human Influence: 3000-500 Cal Bpmentioning
confidence: 97%