globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2012.10.027
Scopus记录号: 2-s2.0-84870179649
论文题名:
Holocene vegetation, fire and climate interactions on the westernmost fringe of the Mediterranean Basin
作者: Morales-Molino C.; García-Antón M.; Postigo-Mijarra J.M.; Morla C.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2013
卷: 59
起始页码: 5
结束页码: 17
语种: 英语
英文关键词: Betula ; Charcoal ; Fire ecology ; Forest management ; Heathlands ; Macrofossils ; Pollen ; Spain
Scopus关键词: Betula ; Fire ecology ; Heathlands ; Macrofossils ; Pollen ; Spain ; Charcoal ; Conservation ; Fires ; Secondary recovery ; Vegetation ; Forestry ; boreal forest ; charcoal ; coniferous forest ; fire history ; forest fire ; forest management ; fossil record ; grassland ; heathland ; Holocene ; human activity ; paleoecology ; palynology ; replacement ; secondary succession ; shrubland ; vegetation cover ; basin ; climate change ; maturation ; Mediterranean environment ; mountain region ; succession ; temperate environment ; transgression ; vegetation ; Basins ; Betula ; Charcoal ; Conservation ; Forest Fires ; Fossils ; Plants ; Pollen ; Spain ; Fires ; Forest Management ; Forestry ; Recovery ; Iberian Cordillera ; Mediterranean Region ; Mediterranean Sea ; Spain ; Central Iberian Zone ; Betula ; Pinus pinaster ; Pinus sylvestris
英文摘要: A new palaeoecological sequence from the western Iberian Central Range significantly contributes to the knowledge on the Holocene vegetation dynamics in central Iberia. This sequence supports the existence of time-transgressive changes in the vegetation cover during the beginning of the Holocene over these central Iberian mountains, specifically the replacement of boreal birch-pine forests with Mediterranean communities. Anthracological analyses also indicate the replacement of boreal pines (Pinus sylvestris) with Mediterranean ones (Pinus pinaster) during the early Holocene. The observed vegetation changes were generally synchronous with climatic phases previously reconstructed for the western Mediterranean region, and they suggest that the climatic trends were most similar to those recorded in the northern Mediterranean region and central Europe. Several cycles of secondary succession after fire ending with the recovery of mature forest have been identified, which demonstrates that the vegetation of western Iberia was highly resilient to fire disturbance. However, when the recurrence of fire crossed a certain threshold, the original forests were not able to completely recover and shrublands and grasslands became dominant; this occurred approximately 5800-5400 cal yr BP. Afterwards, heathlands established as the dominant vegetation, which were maintained by frequent and severe wildfires most likely associated with human activities in a climatic framework that was less suitable for temperate trees. Finally, our palaeoecological record provides guidelines on how to manage protected areas in Mediterranean mountains of southwestern Europe, especially regarding the conservation and restoration of temperate communities that are threatened there such as birch stands. © 2012 Elsevier Ltd.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/60748
Appears in Collections:过去全球变化的重建

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作者单位: Departamento de Silvopascicultura (U.D. Botánica), E.T.S.I. de Montes, Universidad Politécnica de Madrid, Ciudad Universitaria s/n, 28040 Madrid, Spain; Departamento de Biología (Botánica), Facultad de Ciencias, Universidad Autónoma de Madrid, c/Darwin 2, 28049 Cantoblanco, Madrid, Spain

Recommended Citation:
Morales-Molino C.,García-Antón M.,Postigo-Mijarra J.M.,et al. Holocene vegetation, fire and climate interactions on the westernmost fringe of the Mediterranean Basin[J]. Quaternary Science Reviews,2013-01-01,59
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