Holocene vegetation and fire dynamics in the supra-mediterranean belt of the Nebrodi Mountains (Sicily, Italy)

被引:31
|
作者
Bisculm, Martina [1 ,2 ]
Colombaroli, Daniele [1 ,2 ]
Vescovi, Elisa [1 ,2 ,3 ]
van Leeuwen, Jacqueline F. N. [1 ,2 ]
Henne, Paul D. [1 ,2 ]
Rothen, Julian [1 ,2 ]
Procacci, Giovanni [1 ,2 ]
Pasta, Salvatore
La Mantia, Tommaso [4 ]
Tinner, Willy [1 ,2 ]
机构
[1] Univ Bern, Inst Plant Sci, CH-3013 Bern, Switzerland
[2] Univ Bern, Oeschger Ctr Climate Change Res, CH-3013 Bern, Switzerland
[3] CNR, Inst Environm Dynam, Dalmine, Italy
[4] Univ Palermo, Dept DEMETRA, Palermo, Italy
基金
瑞士国家科学基金会;
关键词
climate change; human impact; Ilex aquifolium; macrofossils; Quercus ilex; pollen; LAGO-DI-PERGUSA; POLLEN; CHARCOAL; CLIMATE; RECORD; LAKE; TRANSITION; EVOLUTION; TUSCANY; NUMBER;
D O I
10.1002/jqs.2551
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
High-resolution pollen, macrofossil and charcoal data, combined with accelerator mass spectrometry 14C dating and multivariate analysis, were used to reconstruct Holocene vegetation and fire dynamics at Urio Quattrocchi, a small lake in the supra-mediterranean belt in the Nebrodi Mountains of Sicily (Italy). The data suggest that after 10?000?cal a BP increasing moisture availability supported closed forests with deciduous (Quercus cerris, Fagus sylvatica and Fraxinus spp.) and evergreen (Quercus ilex) species. Species-rich closed forest persisted until 6850?cal a BP, when Neolithic activities caused a forest decline and affected plant diversity. Secondary forest with abundant Ilex aquifolium recovered between 6650 and 6000?cal a BP, indicating moist conditions. From 5000?cal a BP, agriculture and pastoralism led to the currently fragmented landscape with sparse deciduous forests (Quercus cerris). The study suggests that evergreen broadleaved species were more important at elevations above 1000?m a.s.l. before ca. 5000?cal a BP than subsequently, which might reflect less human impact or warmer-than-today climatic conditions between 10?000 and 5000 cal a BP. Despite land use since Neolithic times, deciduous supra-mediterranean forests were never completely displaced from the Nebrodi Mountains, because of favourable moist conditions that persisted throughout the Holocene. Reconstructed vegetation dynamics document the absence of any pronounced mid- or late-Holocene aridification trend at the site, an issue which is controversially debated in Italy and the Mediterranean region. Copyright (C) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码:687 / 698
页数:12
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