Great Lakes Vegetation Dynamics: The Role of Fluctuating Water Levels and Buried Seeds
Great Lakes Vegetation Dynamics: The Role of Fluctuating Water Levels and Buried Seeds
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DOI:
10.1016/s0380-1330(86)71697-3
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发表时间:
1986
影响因子:
2.2
通讯作者:
P. Keddy;A. Reznicek
中科院分区:
文献类型:
--
作者:
P. Keddy;A. Reznicek
The objective of this study was to review the relationship between fluctuating water levels and shoreline vegetation dynamics in the Great Lakes. Low water periods allow many plant species and vegetation types to regenerate from buried seeds. A review of published seed bank densities shows that some lakeshores have densities of buried seeds greater than l04seeds m−2, an order of magnitude greater than densities reported from prairie marshes. High water periods kill dominant species (e.g.,Typhasp.), thereby creating gaps which other species can colonize during low water periods. High water also kills woody plants, thereby extending marshes landward. Fluctuating water levels therefore increase the area of shoreline vegetation, and the diversity of vegetation types and plant species. Any stabilization of water levels would likely reduce marsh area, vegetation diversity, and plant species diversity. Four basic shoreline vegetation types (forest and shrub thickets, wet meadow, marsh, and aquatic) can be recognized; both wet meadow and marsh largely result from fluctuating water levels.