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首页> 外文期刊>Plant and Soil >Spatiotemporal pattern of seed bank in the annual psammophyte Agriophyllum squarrosum Moq. (Chenopodiaceae) on the active sand dunes of northeastern Inner Mongolia, China
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Spatiotemporal pattern of seed bank in the annual psammophyte Agriophyllum squarrosum Moq. (Chenopodiaceae) on the active sand dunes of northeastern Inner Mongolia, China

机译:一年生沙生植物Agriophyllum squarrosum Moq种子库的时空格局。内蒙古东北部活跃沙丘上的藜科(藜科)

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摘要

The seed banks of active sand dunes are critical for the adaptation of psammophytes to unstable habitats. However, existing reports have failed to effectively elucidate the spatiotemporal structure of these seed banks and the factors regulating them. The seed bank pattern of the annual psammophyte Agriophyllum squarrosum Moq. in active sand dunes was studied by taking into consideration the time, the depth of the soil profile, dune positions, and seed bank type (released seed bank, belowground and aboveground canopy seed banks). Most canopy-stored seeds were unburied before the following March of the maturation year; however, they were buried from March to May. The seed bank mainly comprised the aboveground canopy-stored seeds from September of the year of seed maturation to the following March. The seed bank was concentrated in the surface soil layers (0-10 cm) from March of the year following seed maturation to June and was concentrated in the deep soil layers (10-50 cm) after June. The seed bank in the lower leeward slope tended to be larger than those in the other dune positions. The canopy-stored seed:released seed ratio differed between dune positions. The findings of this study are: (1) sand burial and wind erosion play key roles in shaping the spatiotemporal pattern of the seed banks of active sand dunes, and (2) delayed seed release may be a major factor regulating the spatiotemporal pattern of the seed banks of certain psammophytes.
机译:活性沙丘的种子库对于沙生植物适应不稳定生境至关重要。但是,现有报告未能有效阐明这些种子库的时空结构及其调控因素。一年生沙生植物Agriophyllum squarrosum Moq的种子库模式。通过考虑时间,土壤剖面深度,沙丘位置和种子库类型(释放的种子库,地下和地下冠层种子库)来研究活跃沙丘中的沙丘。成熟的次年3月之前,大多数被冠层存储的种子尚未被埋葬。然而,他们从三月到五月被埋葬。从种子成熟年的9月到次年的3月,种子库主要由地上的冠层存储种子组成。从种子成熟后的一年的3月到6月,种子库集中在表土层(0-10厘米),6月之后,种子库集中在深土层(10-50厘米)。下风向倾斜处的种子库往往比其他沙丘位置的种子库大。沙丘位置之间冠层存储的种子与释放的种子比率不同。这项研究的结果是:(1)埋葬和风蚀在塑造活性沙丘种子库的时空格局中起关键作用;(2)种子释放延迟可能是调节沙丘种子时空格局的主要因素。某些沙生植物的种子库。

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