SPREAD OF BROAD-LEAVED TREES IN ESTONIA

L. Saarse, S. Veski
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引用次数: 22

Abstract

The spread of broad-leaved trees ( Ulmus, Tilia, Quercus, Fraxinus, Carpinus, and Fagus) is reviewed on the basis of 46 radiocarbon dated pollen diagrams from lake and mire sediments from Estonia. Ulmus immigrated into Estonia in the second half of the Pre-Boreal, expanded between 9000 and 7800 BP, and reached its maximum values 7900-4200 BP. The immigration of Tilia began between 8800 and 6200 BP; it expanded at 8200-5200 BP, and culminated between 7200 and 4000 BP. Quercus was the next tree to arrive in Estonia, about 7900-7500 BP. Oak spread between 6800 and 4000 BP, with a maximum intermittent between 4200 and 3100 BP. Fraxinus was first recorded about 6500 BP from East Estonia. Carpinus is a late immigrant which reached Estonia in the Sub-Boreal. Comparison of the immigration and expansion of elm, lime, and oak manifests their different response to climate, with elm forest being most broadly distributed between 9000 and 7000 BP, lime between 7000 and 4000 BP (forming then up to 30% of the total forest area), and oak between 4000 and 3500 BP. Elm showed a very rapid colonization from the south; the immigration of lime was more time-transgressive and took place from the south and east. Oak immigrated from the southwest and, in contrast to elm, spread very slowly. The broad-leaved forest reached its maximum density in the second half of the Atlantic and at the beginning of the Sub-Boreal. A gradual retreat of thermophilous trees started with the elm decline at about 5500- 5000 BP, which was quite asynchronous, being caused by the combination of climate deterioration, anthropogenic forest clearances, and fungal diseases.
爱沙尼亚阔叶树的分布
根据爱沙尼亚湖泊和沼泽沉积物的46个放射性碳定年花粉图,综述了阔叶树(榆木、椴、栎木、黄曲霉、卡皮努斯和Fagus)的分布情况。乌尔穆斯在前北寒带后期移民到爱沙尼亚,在9000 - 7800 BP之间扩张,并在7900-4200 BP之间达到最大值。提利亚人的移民开始于公元前8800年至6200年之间;它在8200-5200 BP之间扩张,在7200 - 4000 BP之间达到顶峰。栎树是下一棵到达爱沙尼亚的树,大约在距今7900-7500年前。橡树分布在6800 - 4000 BP之间,最大间歇分布在4200 - 3100 BP之间。最早的记录是在距今6500年前的东爱沙尼亚。卡皮努斯是一个晚期移民,在亚北方到达爱沙尼亚。榆树、石灰和橡树对气候的迁移和扩张的比较表明,榆树林在9000 ~ 7000 BP之间分布最广,石灰在7000 ~ 4000 BP之间分布最广(占森林总面积的30%),橡树在4000 ~ 3500 BP之间分布最广。榆树显示了来自南方的快速殖民;石灰的迁移更具时代性,主要从南部和东部迁移。橡树是从西南部迁移过来的,与榆树不同,它的传播非常缓慢。阔叶林的密度在大西洋后半段和亚北纬带初期达到最大值。在5500 ~ 5000 BP左右,榆树的衰落开始于嗜热树木的逐渐退缩,这是一个相当不同步的过程,是由气候恶化、人为森林砍伐和真菌疾病共同造成的。
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