globalchange  > 气候减缓与适应
DOI: 10.1016/j.quascirev.2017.08.025
Scopus记录号: 2-s2.0-85028920933
论文题名:
Human-environment interaction during the Mesolithic- Neolithic transition in the NE Iberian Peninsula. Vegetation history, climate change and human impact during the Early-Middle Holocene in the Eastern Pre-Pyrenees
作者: Revelles J.; Burjachs F.; Palomo A.; Piqué R.; Iriarte E.; Pérez-Obiol R.; Terradas X.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 184
起始页码: 183
结束页码: 200
语种: 英语
英文关键词: Anthracology ; Early Neolithic ; Holocene ; NE Iberia ; Paleoclimatology ; Pollen analysis ; Vegetation dynamics ; Western Europe
Scopus关键词: Deforestation ; Expansion ; Forestry ; Vegetation ; Anthracology ; Early Neolithic ; Holocenes ; Paleoclimatology ; Pollen analysis ; Vegetation dynamics ; Western Europe ; Climate change ; anthropogenic effect ; broad-leaved forest ; climate change ; deciduous forest ; deforestation ; grassland ; Holocene ; landscape change ; Mesolithic ; nature-society relations ; Neolithic ; pollen ; succession ; territory ; vegetation history ; woodland ; Catalonia ; Gerona [Catalonia] ; Iberian Peninsula ; Lake Banyoles ; Pyrenees ; Spain ; Coniferophyta
英文摘要: The synthetic analysis of several pollen records from sub-Mediterranean lowland Pre-Pyrenean regions evidences expansion of forests during the Early Holocene in Northeastern Iberia and the establishment of dense deciduous broadleaf forests during the Holocene Climate Optimum. Pollen records show the broadleaf deciduous forests resilience against cooling phases during the Mid-Holocene period, with slight regressions of oak woodlands and expansion of conifers or xerophytic taxa contemporary to some cooling episodes (i.e. 8.2 and 7.2 kyr cal. BP). Major vegetation changes influenced by climate change occurred in the transition to the Late Holocene, in terms of the start of a succession from broadleaf deciduous forests to evergreen sclerophyllous woodlands. The lack of evidence of previous occupation seems to support the Neolithisation of the NE Iberian Peninsula as a result of a process of migration of farming populations to uninhabited or sparsely inhabited territories. In that context, remarkable changes in vegetation were recorded from 7.3 kyr cal. BP onwards in the Lake Banyoles area, where the establishment of permanent farming settlements caused the deforestation of oak woodlands. In La Garrotxa region, short deforestation episodes affecting broadleaf deciduous forests, together with expansion of grasslands and presence of Cerealia-t were documented in the period 7.4–6.0 kyr cal. BP. Finally, in the coastal area, where less evidence of Early Neolithic occupations is recorded, evidence of Neolithic impact is reflected in the presence of Cerealia-t in 6.5–6.2 kyr cal. BP, but no strong human transformation of landscape was carried out until more recent chronologies. © 2017 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112278
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作者单位: Departament de Prehistòria, Universitat Autònoma de Barcelona, Bellaterra, 08193, Spain; ICREA, Pg. Lluís Companys 23, Barcelona, 08010, Spain; Institut Català de Paleoecologia Humana i Evolució Social (IPHES), Tarragona, 43007, Spain; Àrea de Prehistòria, Universitat Rovira i Virgili (URV), Tarragona, 43002, Spain; Laboratorio de Evolución Humana, Departamento Ciencias Históricas y Geografía, Universidad de Burgos, Plaza Misael Bañuelos, Edificio I+D+i, Burgos, 09001, Spain; Departament de Biologia Vegetal, de Biologia Animal i d'Ecologia, Unitat de Botànica, Universitat Autònoma de Barcelona, Bellaterra, 08193, Spain; Archaeology of Social Dynamics, Institución Milà y Fontanals, Consejo Superior de Investigaciones Científicas (IMF-CSIC), C/Egipcíaques, 15, Barcelona, 08001, Spain

Recommended Citation:
Revelles J.,Burjachs F.,Palomo A.,et al. Human-environment interaction during the Mesolithic- Neolithic transition in the NE Iberian Peninsula. Vegetation history, climate change and human impact during the Early-Middle Holocene in the Eastern Pre-Pyrenees[J]. Quaternary Science Reviews,2018-01-01,184
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