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Do soil microbes and abrasion by soil particles influence persistence and loss of physical dormancy in seeds of tropical pioneers?

机译:土壤微生物和土壤颗粒的磨蚀是否会影响热带先驱种子的持久性和物理休眠的丧失?

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摘要

Germination from the soil seed bank (SSB) is an important determinant of species composition in tropical forest gaps, with seed persistence in the SSB allowing trees to recruit even decades after dispersal. The capacity to form a persistent SSB is often associated with physical dormancy, where seed coats are impermeable at the time of dispersal. Germination literature often speculates, without empirical evidence, that dormancy-break in physically dormant seeds is the result of microbial action and/or abrasion by soil particles. We tested the microbial/soil abrasion hypothesis in four widely distributed neotropical pioneer tree species (Apeiba membranacea, Luehea seemannii, Ochroma pyramidale, and Cochlospermum vitifolium). Seeds were buried in five common gardens in a lowland tropical forest in Panama, and recovered at 1, 3, 6, and 12 months after burial. Seed permeability, microbial infection, seed coat thickness, and germination were measured. Parallel experiments compared the germination fraction of fresh and aged seeds without soil contact, and in seeds as a function of seed permeability. Contrary to the microbial/soil abrasion hypothesis the proportion of permeable seeds, and of seeds infected by cultivable microbes, decreased as a function of burial duration. Furthermore, seeds stored in dark and dry conditions for 2 years showed a higher proportion of seed germination than fresh seeds in identical germination conditions. We determined that permeable seeds of A. membranacea and O. pyramidale had cracks in the chalazal area or lacked the chalazal plug, whereas all surfaces of impermeable seeds were intact. Our results are inconsistent with the microbial/soil abrasion hypothesis of dormancy loss and instead suggest the existence of multiple dormancy phenotypes, where a fraction of each seed cohort is dispersed in a permeable state and germinates immediately, while the impermeable seed fraction accounts for the persistent SSB. Thus, we conclude that fluctuations in the soil temperature in the absence of soil abrasion and microbial infection are sufficient to break physical dormancy on seeds of tropical pioneer trees.
机译:土壤种子库(SSB)的发芽是热带林间隙物种组成的重要决定因素,SSB中的种子持久性使树木分散后甚至数十年都可以吸收。形成持久性SSB的能力通常与物理休眠有关,在分散时种皮是不可渗透的。萌发文献经常在没有经验证据的情况下推测,物理休眠种子的休眠中断是微生物作用和/或土壤颗粒磨损的结果。我们在四种分布广泛的新热带先锋树物种(Apeiba membranacea,Luehea seemannii,Ochroma pyramidale和Cochlospermum vitifolium)中测试了微生物/土壤磨损假设。种子被埋在巴拿马低地热带森林的五个普通花园中,并在埋葬后的1、3、6和12个月恢复。测量种子的通透性,微生物感染,种皮厚度和发芽率。平行实验比较了没有土壤接触的新鲜和老化种子的发芽率,以及种子中种子的渗透率。与微生物/土壤磨损假说相反,可渗透种子和被可培养微生物感染的种子的比例随埋藏时间的延长而降低。此外,在相同的发芽条件下,在黑暗和干燥条件下保存2年的种子比新鲜种子发芽的比例更高。我们确定了A. membranacea和O. pyramidale的可渗透种子在chalazal区域中有裂缝或缺少chalazal塞,而所有不可渗透种子的表面均完好无损。我们的结果与休眠损失的微生物/土壤磨损假说不一致,而是表明存在多种休眠表型,其中每个种子队列的一部分分散成可渗透状态并立即发芽,而不可渗透种子占持久性的原因。 SSB。因此,我们得出结论,在没有土壤磨损和微生物感染的情况下,土壤温度的波动足以破坏热带先锋树种子的物理休眠。

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