Abstract

Seasonal periodicity of seed germination and its relationship to seasonal changes in temperature and soil moisture have been well studied in seeds of species with physiological dormancy. However, relatively little information is available on the role of these environmental factors in controlling germination of seeds with physical dormancy (PY). Our primary aim was to determine if seeds of the cold desert sand dune semi-shrub Eremosparton songoricum exhibits seasonal periodicity of seed germination and the relationship between seed dormancy break and soil temperature and moisture. In the laboratory, seeds incubated on dry, wet, wet-dry and dry-wet sand were exposed to a 1-year sequence of temperature regimes simulating those in the field. In the field, seeds were buried at different depths on a sand dune, and germination of periodically exhumed seeds was tested at five temperature regimes during a 2-year period. In the one-year sequence of simulated natural temperature regimes, breaking of PY was more effective under constantly wet than under constantly dry conditions, and germination percentage was significantly higher under dry-wet than under wet-dry conditions. Seeds buried in the field exhibited a distinct peak of germination in spring and little or no germination in other seasons. The final (two-year) monthly cumulative germination percentage differed among burial depths and temperature, and it was highest (47%) in seeds buried at 3 cm and tested at 25/10 °C. A seed cohort of E. songoricum likely exhibits a long-term annual periodicity of spring germination in the field, and dormancy break appears to be driven by low (winter) temperatures and relatively high sand moisture content. To our knowledge this is the first study to document seasonal periodicity in seed germination in a cold desert species with PY and to identify the mechanism (at the whole-seed level) of its occurrence.

Highlights

  • Physical dormancy (PY) in seeds is caused by a water impermeable seed or fruit coat, and seeds cannot imbibe water when placed in a hydrated environment (Jayasuriya et al 2013; Baskin and Baskin 2014)

  • Mature seeds with PY are dispersed from maternal plants and may become buried in the soil, where PYbreak is controlled via soil temperature and moisture conditions (Hu et al 2009; Baskin and Baskin 2014)

  • Fluctuation of soil moisture in different seasons was higher at the sand surface than at burial depths of 3 and 8 cm

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Summary

Introduction

Physical dormancy (PY) in seeds is caused by a water impermeable seed or fruit coat, and seeds cannot imbibe water when placed in a hydrated environment (Jayasuriya et al 2013; Baskin and Baskin 2014). Studies on the ecological factors affecting PY release have shown that high temperatures and/or dry heat (McKeon and Mott 1982; Lonsdale 1993; Norman et al 2002), alternate wetting and drying (Baskin and Baskin 1984), wet heat (Van Klinken and Flack 2005; Van Klinken et al 2006) and low (5C) temperature (Van Assche et al 2003) are effective for dormancy-break, depending on the species. Studies generally have focused on burial depth in relation to breaking of PY and have not been concerned with temperature or soil moisture (see Baskin and Baskin 2014)

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