Spatiotemporal pattern of seed bank in the annual psammophyte Agriophyllum squarrosum Moq. (Chenopodiaceae) on the active sand dunes of northeastern Inner Mongolia, China

2008 ◽  
Vol 311 (1-2) ◽  
pp. 97-107 ◽  
Author(s):  
Junling Ma ◽  
Zhimin Liu
Ecoscience ◽  
2002 ◽  
Vol 9 (3) ◽  
pp. 407-413 ◽  
Author(s):  
Christopher J. Lortie ◽  
Roy Turkington

2008 ◽  
Vol 121 (5) ◽  
pp. 473-482 ◽  
Author(s):  
Yuanrun Zheng ◽  
Glyn M. Rimmington ◽  
Zhixiao Xie ◽  
Lei Zhang ◽  
Ping An ◽  
...  

Phytotaxa ◽  
2021 ◽  
Vol 527 (4) ◽  
pp. 284-292
Author(s):  
XIAOLIANG LIU ◽  
TOLGOR BAU ◽  
ZHU L. YANG

A new saprotrophic species in Amanita sect. Lepidella, A. orientisororia, was discovered on lawn and sand dunes in Northeast China. This species was macroscopically characterized by a small white pileus, conical to subconical to pyramidal volval remnants on pileal surface, large broadly ellipsoid to ellipsoid basidiospores measuring 9–13×7–9.5 μm, and the common presence of clamps in all parts of basidiomata. It was described and compared with related species in the genus, based on morphological characteristics and phylogenetic evidence inferred from sequences of the nuclear ribosomal internal transcribed spacer (ITS) and the large subunit of the nuclear ribosomal region (nrLSU).


2015 ◽  
Vol 16 (6) ◽  
pp. 490-499 ◽  
Author(s):  
Yong-Cui Wang ◽  
Mark K.J. Ooi ◽  
Guo-Hua Ren ◽  
De-Ming Jiang ◽  
Ala Musa ◽  
...  

Author(s):  
M. Anwar Maun

The soil seed bank refers to a reservoir of viable seeds present on the soil surface or buried in the soil. It has the potential to augment or replace adult plants. Such reservoirs have regular inputs and outputs. Outputs are losses of seeds by germination, predation or other causes, while inputs include dispersal of fresh seeds from local sources and immigration from distant sources (Harper 1977). Since sand dunes are dynamic because of erosion, re-arrangement or burial by wind and wave action, efforts to find seed banks have largely been unsuccessful. Following dispersal, seeds accumulate in depressions, in the lee of plants, on sand surfaces, on the base of lee slopes and on the driftline. These seeds are often buried by varying amounts of sand. Buried seeds may subsequently be re-exposed or possibly lost over time. However, the existence of a seed bank can not be denied. Plant species may maintain a transient or a persistent seed bank depending on the longevity of seeds. In species with transient seed banks, all seeds germinate or are lost to other agencies and none is carried over to more than one year. In contrast, in species with a persistent seed bank at least some seeds live for more than one year. The four types of seed banks described by Thompson and Grime (1979) provide useful categories for discussion of coastal seed bank dynamics of different species. Type I species possess a transient seed bank after the maturation and dispersal of their seeds in spring that remain in the seed bank during summer until they germinate in autumn. Type II species possess a transient seed bank during winter but all seeds germinate and colonize vegetation gaps in early spring. Seeds of both types are often but not always dormant and dormancy is usually broken by high temperatures in type I and low temperature in type II. Type III species are annual and perennial herbs in which a certain proportion of seeds enters the persistent seed bank each year, while the remainder germinate soon after dispersal, and Type IV species are annual and perennial herbs and shrubs in which most seeds enter the persistent seed bank and very few germinate after dispersal.


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