Abstract

Most tree species in the temperate climatic zone (including Douglas fir) disperse seeds in autumn. Some of them must be exposed to cold (0–10 °C) and moist conditions (cold stratification) to overcome dormancy and trigger germination. In the Northern Hemisphere, winter warm spells occur more frequently and last longer than in recent decades from eastern Canada to Europe. Our main research objective was to investigate the influence of current (1 or 3 days at day/night temperatures: 15 °C/10 °C) and future predicted (5 days at day/night temperatures: 25 °C/15 °C) winter warm spells on dormancy breaking and germination traits (germination energy—GE; germination capacity—GC; final germination capacity—FGC) of Douglas fir seeds from four old-growth stands in northern Poland. For this purpose, we interrupted cold stratification of seeds at different time points, i.e., after 3 weeks; 6 weeks; 9 or 3 weeks and 6 weeks; 3 and 9 weeks; 6 and 9 weeks; 3 and 6 weeks and 9 weeks. We found that for GE and GC, all main effects (populations—P; days of warm spell—D; stratification duration—W) and interactions were significant (except interaction P×D). FGC was significantly affected by the effects P and D and interactions of D × W and P × D × W. In addition, we found that the predicted warm spells negatively affected the early germination stage (GE and GC) of Douglas fir, but both current and future predicted winter conditions will not negatively affect the late germination stage (FGC).

Highlights

  • Introduction iationsClimate change, especially rising temperatures and decrease in snow cover during winter, could have serious consequences for seed biology and ecology [1]

  • Populations significantly affected the germination of Douglas fir seeds in the case of germination after 2 (GE) (Wald χ2 = 11.1, p < 0.001), germination capacity (GC) (Wald χ2 = 171.1, p < 0.001) and final germination capacity (FGC) (Wald χ2 = 194.3, p < 0.001)

  • The highest average FGC was observed in seeds from JAM and CHO, which were significantly different from population LEB and CZA (Table 1)

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Summary

Introduction

Especially rising temperatures and decrease in snow cover during winter, could have serious consequences for seed biology and ecology [1]. The result of these consequences could be manifested in changes in population dynamics by increased seedling mortality and/or a complete lack of plant regeneration from seeds. These responses would be devastating for species that are sensitive to climate conditions during flowering, seed and fruit set and for species with dormant seeds that require a cold period to break dormancy [1,2]. An average of three to five warm spells was recorded

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