The DOI matches its Crossref record; 11 of the 11 references it cites were found in a registry or an index.
Vegetational gradients in relation to environmental conditions in northwestern European mires
Abstract
Floristically characterized gradients related to (i) mire surface microtopography, (ii) marginal versus central areas, (iii) ombrotrophy and minerotrophy ("poor and rich mires"), and (iv) distance from the sea can be recognized in the mire vegetation of northwestern Europe. Along these gradients variation occurs in (i) oscillations in the water level, (ii) origin and flow of water, and (iii) supply of minerals. These conditions influence the decay processes and the resulting peat accumulation rate, pH, mineral nutrient supply, and productivity. The differences between marginal and open areas result from differences in nutrient supply (N,P,K), while the differences between "poor and rich" mires are due to differences in the reactions of the peat. In Sphagnum-dominated vegetation, most floristic variation results from effects of differences in peat accumulation rates. Climatic conditions, other than atmospheric supply of minerals, are most important in establishing the regional floristic differences in the bog vegetation.
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Citations
Cites
Distribution and Movement of Elements in Ombrotrophic Peat Bogs
Damman, A. W. H. (1978) · Oikos · doi:10.2307/3543344 · Cited by 357
Profiles of water content and pore size in Sphagnum and peat, and their relation to peat bog ecology
Hayward, P. M., & Clymo, R. S. (1982) · Proceedings of the Royal Society of London. Series B. Biological Sciences · doi:10.1098/rspb.1982.0044 · Cited by 289
Heinselman, M. L. (1970) · Ecological Monographs · doi:10.2307/1942297 · Cited by 257
Glaser, P. H., Wheeler, G. A., Gorham, E., & Wright, H. E. (1981) · Journal of Ecology · doi:10.2307/2259685 · Cited by 249
Sjörs, H. (1948) · KTH Publication Database DiVA (KTH Royal Institute of Technology) · Cited by 194
Vegetation gradients of minerotrophically rich fens in western Alberta
Slack, N. G., Vitt, D. H., & Horton, D. G. (1980) · Canadian Journal of Botany · doi:10.1139/b80-034 · Cited by 165
Vitt, D. H., & Slack, N. G. (1975) · Canadian Journal of Botany · doi:10.1139/b75-042 · Cited by 134
The vegetation and chemical properties of patterned fens in the Swan Hills, north central Alberta
Vitt, D. H., Achuff, P. L., & Andrus, R. E. (1975) · Canadian Journal of Botany · doi:10.1139/b75-306 · Cited by 117
Rosswall, T., Flower-Ellis, J. G. K., Johansson, L., Jonsson, S., Rydén, B. E., & Sonesson, M. (1975) · Cited by 71
Chemical Studies on the Soils and Vegetation of Waterlogged Habitats in the English Lake District
Gorham, E. (1953) · Journal of Ecology · doi:10.2307/2257046 · Cited by 57
Cited by
Multiple limiting gradients in peatlands: A call for a new paradigm
Bridgham, S. D., Pastor, J., Janssens, J. A., Chapin, C., & Malterer, T. J. (1996) · Wetlands · doi:10.1007/bf03160645 · Cited by 270
Alpine Peatlands of the Andes, Cajamarca, Peru
Cooper, D. J., Wolf, E. C., Colson, C., Vering, W., Granda, A., & Meyer, M. (2010) · Arctic, Antarctic, and Alpine Research · doi:10.1657/1938-4246-42.1.19 · Cited by 81
A European map of groundwater pH and calcium
Hájek, M., Jiménez-Alfaro, B., Hájek, O., Brancaleoni, L., Cantonati, M., Carbognani, M., Dedić, A., Dítě, D., Gerdol, R., Hájková, P., et al. (2021) · Earth System Science Data · doi:10.5194/essd-13-1089-2021 · Cited by 55
Metadata
- Authors
- Malmer, N.
- Venue
- Canadian Journal of Botany
- Publisher
- Canadian Science Publishing
- Published
- 1986-02-01
- Volume
- 64
- Issue
- 2
- Pages
- 375-383
- ISSN
- 0008-4026 (ISSN-L)
- OpenAlex
- W2066719378
- Cited by
- 288
- References
- 11
- FWCI
- 5.72
- Type
- journal article
- Language
- en
- Open access
- closed
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.