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Mid-Holocene vegetation history and Neolithic land-use in the Lake Banyoles area (Girona, Spain)

机译:Banyoles湖地区(西班牙赫罗那)的全新世中期植被历史和新石器时代的土地利用

摘要

This paper focuses on high-resolution analysis of pollen and sedimentology and botanical macro-remains analysis in a core from Lake Banyoles (Girona, Spain). The core sequence comprises a high resolution mid-Holocene (ca. 8.9-3.35. cal. ka. BP) vegetation succession, and sedimentological, geochemical and geomorphological proxies are related to both climatic and anthropogenic causes. Deforestation processes affected natural vegetation development in the Early Neolithic (7.25-5.55. cal. ka. BP) and Late Neolithic (5.17-3.71. cal. ka. BP), in the context of broadleaf deciduous forest resilience against cooling and drying oscillations. Changes in sedimentation dynamics and in lake water level caused the emergence of dry land on the lake margin where riparian forest was established from 5.55. cal. ka. BP onwards. The data show that in the context of an increasing aridification process, Neolithic land-use played an important role in vegetation history and environmental evolution.
机译:本文着重于Banyoles湖(西班牙赫罗纳)的核心地带的花粉和沉积学高分辨率分析以及植物宏观残留分析。核心序列包括高分辨率的全新世中期(约8.9-3.35。cal。ka。BP)植被演替,沉积学,地球化学和地貌学代理与气候和人为原因相关。在阔叶落叶林抵抗冷却和干燥振荡的情况下,森林砍伐过程影响了新石器时代早期(7.25-5.55。ka。BP)和新石器时代后期(5.17-3.71。ka。BP)的自然植被发育。沉积动力学和湖泊水位的变化导致从5.55开始建立河岸森林的湖缘出现了旱地。校准K a。 BP起。数据表明,在干旱化进程不断增加的背景下,新石器时代的土地利用在植被历史和环境演变中发挥了重要作用。

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