2009
DOI: 10.1016/j.quaint.2008.07.012
|View full text |Cite
|
Sign up to set email alerts
|

Environmental change in NW Iberia between 7000 and 500cal BC

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

1
63
0
3

Year Published

2012
2012
2023
2023

Publication Types

Select...
4
3
1

Relationship

0
8

Authors

Journals

citations
Cited by 65 publications
(67 citation statements)
references
References 42 publications
1
63
0
3
Order By: Relevance
“…There is also evidence that the properties of the soil are affected by a combination of deforestation, fire, erosion and modifications to the vegetation. One of these properties is the reaction of the soil (pH) [67,68]. Thus, the change in the forestry cover is accompanied by the acidification of the soil.…”
Section: Vulnerabilitymentioning
confidence: 99%
“…There is also evidence that the properties of the soil are affected by a combination of deforestation, fire, erosion and modifications to the vegetation. One of these properties is the reaction of the soil (pH) [67,68]. Thus, the change in the forestry cover is accompanied by the acidification of the soil.…”
Section: Vulnerabilitymentioning
confidence: 99%
“…6). However, the episodes of dryness and humidity do not seem to be linked to other records of temperature variation (Martinez Cortizas et al, 2009). …”
Section: Climate Fluctuations and Vegetation Response In The Cantabrimentioning
confidence: 99%
“…Other available palaeo-environmental records date the importance of human activities as being responsible for large-scale changes in the environment from 6000 cal yr BP onward (Mufioz Sobrino et al, 2005;Martinez Cortizas et al, 2009;Lopez-Merino et al, 2010;Martin-Chivelet et al, 2011). From approximately this period, palaeo-environmental records show difficulty in distinguishing the role of climate and human activity, although evidence of climatic variations into the Neolithic and Chalcolithic have been interpreted from pollen sequences (Allen et al, 1996;Mufioz Sobrino et al, 2005) and geochemical signals (Fabregas Valcarce et al, 2003).…”
Section: Climate Fluctuations and Vegetation Response In The Cantabrimentioning
confidence: 99%
“…El uso del MCPSG se ha centrado en dicho periodo pero se puede extender al mundo romano y la tardoantigüedad aunque sus formas respectivas de explotación agrícola son muy diferentes . Durante la Edad del Hierro se observa una progresiva intensificación agrícola en los procesos de reducción del polen arbóreo, cuya dinámica arranca en la Edad del Bronce (Aira et al 1989;Martínez Cortizas et al 2009) . La llegada de Roma supone una ruptura inédita .…”
unclassified
“…Un análisis más contextual exige en principio una aproximación paleoclimática (Verhagen 2002) que existe con carácter general (Font Tullot 1988) y específico para el Noroeste (Martínez Cortizas y Pérez Alberti 1999; Fábregas et al 2003;Martínez Cortizas et al 2009) . Sería necesario determinar si las importantes oscilaciones en el régimen térmico y pluvial documentadas desde el 3 .500 con el periodo neoglaciar, su final en torno al 1.500 a.C. o el periodo cálido romano iniciado con el cambio de era fueron un factor de alteración sustancial de las formas agrícolas .…”
unclassified