Long-term deforestation in NW Spain: linking the Holocene fire history to vegetation change and human activities

被引:83
作者
Kaal, Joeri [1 ]
Carrion Marco, Yolanda [2 ]
Asouti, Eleni [3 ]
Martin Seijo, Maria [4 ]
Martinez Cortizas, Antonio [5 ]
Costa Casais, Manuela [1 ]
Criado Boado, Felipe [6 ]
机构
[1] CSIC, Inst Estudios Gallegos Padre Sarmiento, LaPa, Santiago De Compostela 15704, Spain
[2] CSIC, CIDE, Valencia 46470, Spain
[3] Univ Liverpool, SACE, Liverpool L69 3GS, Merseyside, England
[4] Univ Santiago de Compostela, Fac Xeog & Hist, Grp Estudos Prehist Noroeste, Dept Hist 1, Santiago De Compostela 15782, Spain
[5] Univ Santiago de Compostela, Fac Biol, Dept Edafol & Quim Agr, Santiago De Compostela 15782, Spain
[6] CSIC, Inst Heritage Sci, Incipit CSIC, Santiago De Compostela 15704, Spain
关键词
IBERIAN PENINSULA; CENTRAL-EUROPE; ERICA-ARBOREA; BLACK CARBON; ENVIRONMENTAL-CHANGE; NORTHWEST IBERIA; PYROLYSIS-GC/MS; COLLUVIAL SOILS; LAGO DELLACCESA; ARBUTUS-UNEDO;
D O I
10.1016/j.quascirev.2010.10.006
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The Holocene fire regime is thought to have had a key role in deforestation and shrubland expansion in Galicia (NW Spain) but the contribution of past societies to vegetation burning remains poorly understood. This may be, in part, due to the fact that detailed fire records from areas in close proximity to archaeological sites are scarce. To fill this gap, we performed charcoal analysis in five colluvial soils from an archaeological area (Campo Lameiro) and compared the results to earlier studies from this area and palaeo-ecological literature from NW Spain. This analysis allowed for the reconstruction of the vegetation and fire dynamics in the area during the last ca 11 000 yrs. In the Early Holocene, Fabaceae and Betula sp. were dominant in the charcoal record. Quercus sp. started to replace these species around 10 000 cal BP, forming a deciduous forest that prevailed during the Holocene Thermal Maximum until similar to 5500 cal BR Following that, several cycles of potentially fire-induced forest regression with subsequent incomplete recovery eventually led to the formation of an open landscape dominated by shrubs (Erica sp. and Fabaceae). Major episodes of forest regression were (1) similar to 5500-5000 cal BP, which marks the mid-Holocene cooling after the Holocene Thermal Maximum, but also the period during which agropastoral activities in NW Spain became widespread, and (2) similar to 2000-1500 cal BP, which corresponds roughly to the end of the Roman Warm Period and the transition from the Roman to the Germanic period. The low degree of chronological precision, which is inherent in fire history reconstructions from colluvial soils. made it impossible to distinguish climatic from human-induced fires. Nonetheless, the abundance of synanthropic pollen indicators (e.g. Plantago lanceolata and Urtica dioica) since at least 6000 cal BP strongly suggests that humans used fire to generate and maintain pasture. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:161 / 175
页数:15
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