Carbon and nitrogen in soil and vegetation at sites differing in successional age

作者: C.G. F De Kovel , A.(J.).E.M. Van Mierlo , Y.J.O. Wilms , F. Berendse

DOI: 10.1023/A:1009898622773

关键词:

摘要: We studied vegetation and soil development during primary succession in an inland drift sand area the Netherlands. compared five sites at which had started different moments past, respectively 0, 10, 43 121 years ago, a site not yet started. In three younger was herbaceous, whereas two older pine forest formed. Forest formation accompanied by of FH-layer soil, increase amount organic matter, nitrogen mineralisation rate from 1.9 to 18 g N m−2 yr−1. Soil moisture content also increased, pH showed steady decrease with age. The changed herbaceous dominated mosses lichens grass species Corynephorus canescens Festuca ovina towards understorey Deschampsia flexuosa and, oldest site, dwarf shrubs Empetrum nigrum Vaccinium myrtillus. At same time total amounts carbon ecosystem relatively stronger pool. establishment trees greatly affects dynamics ecosystem, especially its dynamics.

参考文章(28)
A. M. ELGERSMA, Primary forest succession on poor sandy soilsas related to site factors Biodiversity and Conservation. ,vol. 7, pp. 193- 206 ,(1998) , 10.1023/A:1008884418570
Sarah E. Hobbie, Effects of plant species on nutrient cycling. Trends in Ecology and Evolution. ,vol. 7, pp. 336- 339 ,(1992) , 10.1016/0169-5347(92)90126-V
M. D. Busse, Downed Bole-Wood Decomposition in Lodgepole Pine Forests of Central Oregon Soil Science Society of America Journal. ,vol. 58, pp. 221- 227 ,(1994) , 10.2136/SSSAJ1994.03615995005800010033X
Bryan Finegan, Pattern and process in neotropical secondary rain forests: the first 100 years of succession Trends in Ecology and Evolution. ,vol. 11, pp. 119- 124 ,(1996) , 10.1016/0169-5347(96)81090-1
Michael W. Rode, Leaf‐nutrient accumulation and turnover at three stages of succession from heathland to forest Journal of Vegetation Science. ,vol. 4, pp. 263- 268 ,(1993) , 10.2307/3236113