波科诺荒原:生长在适于森林的土壤上的灌木稀树草原

R. Latham, J. Thompson, Sarah A. Riley, Anne W. Wibiralske
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引用次数: 32

摘要

LATHAM, R. E., J. E. THOMPSON, S. A. RILEY和A. W. WIBIRALSKE(宾夕法尼亚大学地质系,费城,19104-6316)。波科诺荒原:生长在有利于森林的土壤上的灌木稀树草原。公牛。托里机器人。俱乐部123:330-349。1996.-先前描述过的灌木稀树草原群落,我们称之为波科诺荒原,主要发生在宾夕法尼亚州波科诺高原南部伊利诺斯州冰川时期的土壤上。与北美中东部的大多数“不毛之地”不同,这里的土壤不是沙质的,也不是浅到基岩的;这片贫瘠的土地和附近的北方阔叶林也有着同样深厚、细密的壤土。在这片不毛之地及其附近,稀有动植物种类异常丰富,吸引了科学家和生物多样性保护专家的注意。为了了解波科诺荒原的生态动态,以及为什么荒原与周围的森林环境不同,我们对植被历史、景观格局、植物物种分布和地下水位进行了研究。波科诺荒原是古老的,早于欧洲人在该地区定居;(二)在有记载的历史中曾发生过频繁、大面积的火灾;(3)目前覆盖面积超过22平方公里,毗邻干旱脊顶荒地带,总面积约为18平方公里;(4)有大量通常生长在潮湿或潮湿土壤条件下的植物与通常生长在干旱生境的植物并存;(5)包括几种植被类型,它们在景观上的分布部分与土壤湿度梯度有关。Pocono till的贫瘠似乎藐视了传统观念,即贫瘠的植被反映了干旱、营养贫乏的土壤。尽管波科诺荒原在欧洲人定居该地区之前就已经出现了,但在这个系统中,火显然是维持荒地植被的关键。我们假设生物因子比非生物因子更能决定波科诺高原南部的荒地和森林植被的分布。
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The Pocono till barrens: shrub savanna persisting on soils favoring forest1
LATHAM, R. E., J. E. THOMPSON, S. A. RILEY AND A. W. WIBIRALSKE (Department of Geology, University of Pennsylvania, Philadelphia, PA 19104-6316). The Pocono till barrens: shrub savanna persisting on soils favoring forest. Bull. Torrey Bot. Club 123: 330-349. 1996.-A previously undescribed shrub savanna community, which we refer to as the Pocono till barrens, occurs mainly on soils weathered from glacial till of Illinoian age on the southern Pocono Plateau of Pennsylvania. Unlike most "barrens" in east-central North America, its soils are not sandy or shallow to bedrock; the same deep, fine-loamy soil series underlie the barrens and nearby northern hardwoods forest. An unusual abundance of rare plant and animal species in and near the barrens has attracted the attention of scientists and biodiversity conservation professionals. In an effort to understand the ecological dynamics of the Pocono till barrens and why the barrens are different from their mostly forested surroundings, we undertook studies of vegetation history, landscape patterns, plant species distributions and water table depth. The Pocono till barrens (1) are old, pre-dating European settlement of the area; (2) have burned frequently and over large areas throughout their recorded history; (3) presently cover more than 22 km2 adjacent to a belt of xeric ridgetop barrens totaling approximately 18 kM2; (4) have in abundance plants usually found in moist or wet soil conditions living side-by-side with those normally associated with xeric habitats; and (5) include several vegetation types which are distributed on the landscape, in part, in association with a soil moisture gradient. The Pocono till barrens appear to flout the conventional wisdom that barrens vegetation reflects droughty, nutrient-poor soils. Although the Pocono till barrens substantially pre-date European settlement of the area, fire is clearly the key to maintenance of barrens vegetation in this system. We hypothesize that biotic factors are more important than abiotic factors in determining distributions of barrens and forest vegetation on the southern Pocono Plateau.
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