L’abri du Pas de l’Échelle (Rovon, Isère) : évolution du couvert végétal d’après les analyses polliniques et anthracologiques

J. Argant, S. Thiébault
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Abstract

The Pas de l’Échelle (980 m a. s. l.) is a natural passage from the Isère valley to the Hauts-Plateaux of the Vercors massif. At this place a rock shelter has yielded an important Mesolithic and Neolithic sequence, well dated by artefacts and by a series of 14C datings. Pollen analysis was mainly performed on this sequence, and on the gravels at the base of the excavation (Dryas III), as well as on Neolithic layers. As for charcoal analysis it covers a larger chronological range, from Mesolithic to Early Middle Ages. It enables to describe the dynamics of the vegetation through several thousands of years under human influence. Therefore, these two botanical approaches are chronologically complementary. The vegetation dynamics is divided in three steps characterized for the first by pine and broadleaved oak forest, then by yew during the Neolithic, next by ash tree and by the fir-beech forest from Bronze Age onwards.
l ' abri du Pas de l ' escala (Rovon, isere):花粉和炭疽学分析后植被覆盖的演变
Pas de l ' Échelle(公元980米)是从is re山谷到Vercors地块的上高原的天然通道。在这个地方,一个岩石掩蔽处发现了一个重要的中石器时代和新石器时代序列,通过人工制品和一系列14世纪年代测定可以很好地确定年代。花粉分析主要在该序列、挖掘底部的砾石(Dryas III)以及新石器时代地层上进行。至于木炭分析,它涵盖了更大的时间范围,从中石器时代到中世纪早期。它能够描述几千年来植被在人类影响下的动态变化。因此,这两种植物学方法按时间顺序是互补的。植被动态分为三个阶段,首先是松树和阔叶栎林,然后是新石器时代的紫杉,其次是青铜器时代以来的白蜡树和冷杉山毛榉林。
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