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Secondary succession in a fallow central European wet grassland

机译:休耕中欧湿草原的次生演替

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摘要

This long-term study (23 yr) aims at specifying the characteristic features of secondary progressive successions in abandoned wet eutrophic grasslands as a precondition for better understanding causal relationships and improving the predictability of successions on such habitats The vegetation of inundated fen grasslands (Calthion) at the lower course of the river Wumme near Bremen (Northwest Germany) was studied annually on three permanent plots (each 10 x 10 m(2)) where hay making had ceased in 1983, 1985 and 1992, respectively In the initial succession phase of three to five years a fast increase of tall-growing, rhizomatous, deciduous reed species (e g Phalaris arundinacea) occurred This strongly changed vegetation structure and within-canopy light climate, which was the reason for the strong decrease in species diversity Rhizomes are hypothesized to be a key factor of high competitiveness in abandoned wet grasslands because this organ combines multiple advantageous functions low-risk vegetative propagation, nutrient storage and nutrient re-allocation between above- and below-ground plant organs, all these functions allowing for a gradual build-up of a high biomass Extinct grassland species (e g Senecio aquaticus) represent a contrasting set of plant traits such as small stature, short lifespan, prevailing generative reproduction and evergreen leaves. The subsequent succession phase commencing about five years after mowing was ceased was characterized by persistence of the established reed vegetation, which prevented tree colonisation until today. Secondary successions in abandoned wet eutrophic grasslands can be predicted on the level of plant communities and functional species groups considering changes in the habitat (esp. light climate), the presence of reed species with a specific set of plant traits in the "Initial Floristic Composition" and their potentially high competitive vigour.
机译:这项长期研究(23年)旨在确定废弃的富营养化湿地草原次生渐进演替的特征,作为更好地了解因果关系并提高此类生境演替可预测性的先决条件淹没fen草的植被(Calthion)每年对不莱梅(德国西北部)乌姆河下游的三个永久样地(每个10 x 10 m(2))进行研究,在三个永久样地上分别于1983年,1985年和1992年停止了干草的生产。在三到五年内,生长着高大的,有根茎的,落叶的芦苇物种(例如Ph草)迅速增加。这极大地改变了植被结构和冠层内部的轻型气候,这是根茎被假定为在这个废弃的湿草原中成为高竞争力的关键因素,因为该器官结合了多种优势功能地上部和地下植物器官之间的树皮营养繁殖,养分储存和养分再分配,所有这些功能都允许逐渐积累高生物量的绝种草原物种(例如千里光水草)代表了一组相反的植物性状例如身材矮小,寿命短,生殖繁殖盛行和常绿叶子。在割草停止后大约五年开始的后续演替阶段,其特征是已建立的芦苇植被持续存在,从而阻止了树木的定植直至今天。可以根据栖息地的变化(尤其是轻度气候),芦苇物种在“初始植物区系组成”中的特定植物性状的存在,在植物群落和功能物种群的水平上预测废弃的富营养化草原的次生演替。以及他们潜在的高度竞争活力。

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