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Soil Seed Banks of Degraded Alpine Grassland in Headwater Region of the Yellow River: Quantities and Dynamics of Seed Germination
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- Author:
- No author available
- Journal Title:
- CHINESE JOURNAL OF APPLIED & ENVIRONMENTAL BIOLOGY
- Issue:
- 3
- DOI:
- 10.3321/j.issn:1006-687X.2006.03.004
- Key Word:
- 青藏高原;黄河源区;退化高寒草地;土壤种子库;萌发动态
Abstract： 对青藏高原黄河源区不同退化程度高寒草地的土壤种子库土样用土壤分析筛进行浓缩,并以萌发法分析土壤种子库萌发种子数量和动态.结果表明,孔径0.25～2 mm的土壤分析筛分离土样中萌发种子可达萌发种子总量的85%～97%,而小于0.25 mm的土样中未发现种子.因此,用0.25 mm孔径大小的土壤筛对高寒草地土壤种子库土样进行大规模浓缩是一种方便、可靠的方法.4种不同退化程度高寒草地(A:未退化草甸;B:轻度退化草甸;C:中度退化草甸;D:重度退化草甸)的土壤种子库在实验室条件下萌发的种子数量分别为:A 1 194～3 744粒/m2,平均2 421.3粒/m2;B 5 376～1 0912粒/m2,平均7 786.7粒/m2;C 2 304～1 3216粒/m2,平均8 695.5粒/m2;D 4 768～12 352粒/m2,平均8 125.9粒/m2.除样地A外,其它3个样地的可萌发种子数量差异不大.单子叶植物种子在培养到d 10左右开始萌发,双子叶植物在5～7 d内开始萌发,前者3 wk后基本不再萌发,后者5 wk左右停止萌发.4个样地土壤种子库种子萌发主要集中在第2～3周,并表现出近似单峰型格局.图1表3参39
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