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The dialectic between deciduous and coniferous forests in central Iberia: A palaeoenvironmental perspective during the late Holocene in the Gredos range

机译:伊比利亚中部落叶林和针叶林之间的辩证法:格列多斯山脉全新世晚期的古环境视角

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Pollen analyses supported by fifteen AMS C-14 dates from Fuente de la Leche (1382 m) and Fuente del Pino Blanco (1343 m) peat sequences, in the Gredos range (central Spain), are used to reconstruct the late Holocene vegetation history in this mountain region. These results are compared with other sequences from the Spanish Central System in order to better understand the past dynamics of the main forest constituents and to provide a critical view of the dialectic between conifers and deciduous forests. The vegetation record at Fuente de la Leche starts at 3000 cal yr BP, with the occurrence of rather closed forests composed of Pinus sylvestris and Betula. Pinus sylvestris was the dominant pollen taxa for almost the entire period. However, during the last 850 years, Pinus sylvestris forests were progressively replaced by Quercus pyrenaica woodlands and grasslands, as a result of a high pastoral pressure, until forming mixed woodlands similar to 400 years ago. The interpretation of Fuente del Pino Blanco record is that dramatic changes started about 265 years ago. Prior to this date, an open canopy woodland included species (Alnus glutinosa, Quercus pyrenaica) whose distributions no longer exist in the studied area. We suggest that the increase in agricultural (rye and other cereals) and livestock activities forced a change in the role of fire in the supramediterranean belt of the Gredos range, thus Pyrenean oak canopy was consumed by fires, providing openings for Pinus pinaster and broom communities better adapted to fire. (c) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:由格勒多斯山脉(西班牙中部)的15个AMS C-14日期(来自西班牙中部)的泥炭序列进行的花粉分析得到了重建,该花粉分析来自丰特-德拉莱什(1382 m)和丰特·德尔皮诺·布兰科(1343 m)。这个山区。将这些结果与西班牙中央系统的其他序列进行了比较,以便更好地了解主要森林成分的过去动态,并提供针叶树与落叶林之间辩证法的批判性观点。 Fuente de la Leche的植被记录始于BP 3000 cal yr,出现了由樟子松和桦树组成的相当封闭的森林。樟子松几乎是整个时期的主要花粉类群。但是,在过去的850年中,由于牧草压力高,樟子松森林逐渐被比勒斯栎林和草地所取代,直到形成类似于400年前的混合林地。 Fuente del Pino Blanco唱片的解释是戏剧性的变化始于265年前。在此日期之前,开放的冠层林地包括物种(Al木,拟南芥),其分布在研究区域中不再存在。我们建议,农业(黑麦和其他谷物)和牲畜活动的增加迫使格雷多斯山脉的地中海上带火的作用发生改变,因此比利牛斯栎树冠层被大火吞噬,为松树针aster和扫帚群落提供了开阔的空间。更适合射击。 (c)2017年爱思唯尔有限公司和INQUA。版权所有。

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