全新世植被层的建立:朝向地块的完整建模

Fernand David
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引用次数: 10

摘要

在法国北部阿尔卑斯山脉cha ne des hurti的第6个地点(1 800 m的La Gouille)对花粉和大型遗骸进行了分析。9个ams日期支持这个年表。因此,一个地块的植被带的建立可以模拟在法国阿尔卑斯山北部。桦树早在10000 14C BP就侵入亚高山草原。在冷杉类传播之前,在约8200 BP的14C BP遗址上已建立了约9600个14C BP的灌木林,其中有山楂、桤木和酢浆草。在8 100 14C BP之前,冷杉的减少发生在Venediger气候振荡期间。在2940 - 14C BP左右,由于人类活动,冷杉发生了强烈的退化,绿桤木(Alnus viridis)扩大。近年来,冷杉的第二次退缩导致了目前空间的青花桤木和翠绿桤木植被覆盖。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Établissement des étages de végétation holocène : vers la modélisation complète d’un massif

Pollen and macro-remains were analysed in a sixth site (La Gouille 1 800 m) of the Chaîne des Hurtières (northern French Alps). Nine A.M.S. dates support the chronology. Thus, the establishment of the vegetation belt of a massif can be modelled in the northern French Alps. Betula invaded sub-Alpine grasslands as early as 10 000 14C BP. Around 9 600 14C BP shrublands with Corylus, Alnus and Sorbus were established before the spread of Abies at the site approximately 8 200 14C BP. A decrease in Abies prior to 8 100 14C BP occurred during the Venediger climatic oscillation. At around 2 940 14C BP, a strong regression of Abies due to human action is noted with the expansion of Alnus viridis. Recently, a second Abies retraction led to the present sparce P. cembra and Alnus viridis vegetation cover.

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