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林业资源管理 ›› 2022›› Issue (4): 28-35.doi: 10.13466/j.cnki.lyzygl.2022.04.005

• 科学研究 • 上一篇    下一篇

午潮山杉阔混交林种子雨与土壤种子库特征研究

焦洁洁1(), 李领寰3, 汪建民1, 孙杰杰2, 吴初平1, 姚良锦1, 王志高1, 袁位高1()   

  1. 1.浙江省林业科学研究院,杭州 310023
    2.南京林业大学 生物与环境学院,南京 210037
    3.国家林业和草原局华东调查规划设计院,杭州 310019;
  • 收稿日期:2022-05-26 修回日期:2022-06-20 出版日期:2022-08-28 发布日期:2022-10-13
  • 通讯作者: 袁位高
  • 作者简介:焦洁洁(1987-),女,浙江嘉善人,助理研究员,主要从事森林经营技术研究。Email: 705241632@qq.com
  • 基金资助:
    省属院所扶持专项(2019F065-6)

Characteristics of Seed Rain and Soil Seed Bank in Broad Leaf and Chinese Fir Mixed Forest in Wuchao Mountain

JIAO Jiejie1(), LI Linghuan3, WANG Jianmin1, SUN Jiejie2, WU Chuping1, YAO Liangjin1, WANG Zhigao1, YUAN Weigao1()   

  1. 1. Zhejiang Academy of Forestry,Hangzhou 310023,China
    2. College of Biology and the Environment,Nanjing Forestry University,Nanjing 210037,China
    3. East China Inventory and Planning Institute,Nation Forestry and Grassland Administration,Hangzhou 310019,China
  • Received:2022-05-26 Revised:2022-06-20 Online:2022-08-28 Published:2022-10-13
  • Contact: YUAN Weigao

摘要:

为探索杉木林演替机制,在杭州午潮山自然演替30a左右的杉阔混交林内选择海拔、坡度及坡向等生境相似的区块设置40 m× 40 m的杉阔混交林样地3个,在样地内布置种子雨收集器进行为期2a收集,并对凋落物层、0~5 cm腐殖质层和5~10 cm土壤层进行土壤种子库调查,取样面积为0.20 m×0.20 m,随即袋装并标记,每个样地每次取样75份,共计450份,并进行种子发芽实验。结果表明:研究区群落种子雨物种组成为9个树种,杉木(种子雨密度12.91粒/m2)和秃瓣杜英(种子雨密度7.60粒/m2)是其主要组成部分,占总数的94.16%。杉木落种持续7个月,高峰期为7月与10月,秃瓣杜英落种持续4个月,高峰期为11—12月。土壤种子库的主要物种也为杉木和秃瓣杜英。其中,杉木种子主要留存于凋落物层,秃瓣杜英种子主要留存于0~5cm土层,且秃瓣杜英种子密度和种子发芽率是杉木的2~5倍。土壤种子库非优势物种组成年际变化较大。导致杉木种子更新失败的重要因素是种子雨和种子库密度较低、种子主要留存于凋落物层。杉阔混交林自然演替过程中,阔叶树种可以利用种子进行天然更新。

关键词: 杉木, 秃瓣杜英, 种子雨, 种子库

Abstract:

In order to explore the succession mechanism of Chinese fir forests,three 40 m×40 m mixed fir and broad-leaved forests were set up in blocks with similar habitats,such as altitude,slope and aspect,in the mixed forest of fir and broadleaf that have been in natural succession for about 30 years in Wuchao Mountain,Hangzhou.In the sample plot,a seed rain collector was arranged in the sample plot for two years of collection,and the litter layer,0~5 cm humus layer and 5~10 cm soil layer were collected in a sampling area of 0.20 m×0.20 m,and then bagged and marked.75 samples were taken from each plot,in a total of 450 samples,and the seed germination experiment was carried out.Our results showed that there were nine species in the seed rain,of which Cunninghania lanceolata (seed rain density 12.91 seeds/m2)and Elaeocarpus(seed rain density 7.60 seeds/m2)were the main components,accounting for 94.16% of the total.The duration of C.lanceolata seed dispersal was 70 months,with two peaks in July and October,respectively.The duration of seed dispersal of Elaeocarpus was 4 months,with a peak in November to December.Seed of C.lanceolata and Elaeocarpus were also the main species in the soil seed bank.C.lanceolata seeds were mainly stored in the litter layer.In contrast,Elaeocarpus seeds were mainly stored in the 0~5cm soil layer.The seed density and germination rate of Elaeocarpus were 2~5 times higher than those of C.lanceolata.Moreover,the composition of non-dominant species in soil seed bank varied greatly from year to year.The retention of seeds in the litter layer resulted in low seed density in the C.lanceolata forest soil,which was the main reason for the difficulty of the natural regeneration of C.lanceolata.The results indicated that,broad-leaved species could regenerate via seeds in natural succession.

Key words: Cunninghania lanceolata, Elaeocarpus glabripetalus, seed rain, seed bank

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