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Thermal regulation of secondary dormancy induction in Polygonum aviculare seeds: a quantitative analysis using the hydrotime model

Published online by Cambridge University Press:  19 June 2017

Diego Batlla*
Affiliation:
I.F.E.V.A./Cátedra de Cerealicultura, C.O.N.I.C.E.T./Facultad de Agronomía, Universidad de Buenos Aires, Av. San Martín 4453, C1417DSE-Buenos Aires, Argentina
Andrés Mateo Agostinelli
Affiliation:
I.F.E.V.A./Cátedra de Cerealicultura, C.O.N.I.C.E.T./Facultad de Agronomía, Universidad de Buenos Aires, Av. San Martín 4453, C1417DSE-Buenos Aires, Argentina
*
*Correspondence Email: batlla@agro.uba.ar
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Abstract

For seed banks showing seasonal changes in their dormancy level, the possibility of predicting temporal patterns of emergence depends on establishing a robust relationship between temperature and the rate of dormancy loss and induction. However, although the effect of temperature on dormancy loss has been extensively studied, less work has been advocated to the quantification of temperature effects on dormancy induction. In the present work, we quantified temperature regulation of dormancy induction in Polygonum aviculare seeds using the hydrotime model. To study induction into secondary dormancy, seeds previously released from primary dormancy through stratification at 5°C were stored at dormancy-inductive temperatures of 10, 15, 20 and 25°C for different periods. During storage, seeds were germinated at different temperatures and water potentials, and hydrotime model parameters were derived. Changes in hydrotime model parameters (mean base water potential for germination and its standard deviation, and the hydrotime required for germination) during dormancy induction were described by adjusting exponential equations. Obtained results indicated a minimum temperature for dormancy induction of 8.7°C and the existence of a bi-linear relationship between rate of induction into secondary dormancy and storage temperature, in which storage temperatures around 25°C showed a higher dormancy induction rate than those below 20°C. Developed model equations were then used to predict changes in germination behaviour during dormancy induction at different temperatures, showing a good agreement between simulated and observed values.

Information

Type
Research Papers
Copyright
Copyright © Cambridge University Press 2017 
Figure 0

Figure 1. Changes in the mean base water potential for germination [Ψb(50)] for P. aviculare seeds incubated at 15 and 10/20°C (12 h/12 h) during moist storage at 5°C. The dotted horizontal line indicates the value of 0 MPa.

Figure 1

Table 1. Estimated population hydrotime parameters for P. aviculare seeds moist-stored at 5°C and germinated at 15 and 10/20°C (12 h/12 h)

Figure 2

Figure 2. Germination of P. aviculare seeds incubated under different water potentials (0, –0.2 and –0.4 MPa). The top four panels show germination of seeds incubated at 10, 15, 20 and 10/20°C (12 h/12 h) after 109 days of moist storage at 5°C (i.e. stratification). The other panels show germination at 10/20°C (12 h/12 h) of previously stratified seeds (109 days at 5°C) moist stored at 10, 15, 20 and 25°C for different periods. The symbols are the experimental data and the curves are predicted from equation 2. Vertical bars indicate SE.

Figure 3

Table 2. Estimated population hydrotime parameters for P. aviculare seeds moist stored at different temperatures in the range 10–25°C and germinated at different temperatures

Figure 4

Figure 3. Changes in the mean base water potential for germination [Ψb(50)], the hydrotime required for seed germination (θH) and the standard deviation of base water potential (σΨb) for P. aviculare seeds incubated at 10, 15, 20 and 10/20°C (12 h/12 h) during moist storage at 10, 15, 20 and 25°C (before storage, seed were stratified at 5°C for 109 days). Incubation temperature is indicated in each panel. Interrupted lines are predicted values according to: y = yi + {[(yi – yf) × exp (–K x)] + (yi – yf)} for panels A to D, and y = yi – (yi +yf) × (1 – exp (–K x)) for panels E to L, where subscripts i and f denote the initial and final values of y, respectively, and K is the exponential changing rate. yi at each incubation temperature are parameter values obtained after 109 days of stratification at 5°C, while yf at each incubation temperature are the highest Ψb(50) and the lowest θH and σΨb obtained during storage under each incubation temperature (see Table 2). Functions for each hydrotime model parameter at the different incubation temperatures were predicted using a single value of K for each storage temperature; for Ψb(50) 10°C: 0.02, 15°C: 0.12, 20°C: 0.22, 25°C: 0.52; for θH 10°C: 0.04, 15°C: 0.15, 20°C: 0.19, 25°C: 2.8; for σΨb 10°C: 0.04, 15°C: 0.1, 20°C: 0.5, 25°C: 2.4 (see Fig. 4). Values of K for each storage temperature were obtained by minimizing the RMSE between simulated and observed values at that temperature for seeds germinated at the four tested thermal regimes. Note that the scales are different between panels.

Figure 5

Figure 4. Values of K (parameter from equations 3, 4 and 5) in relation to storage temperature for each hydrotime model parameter. K values correspond to the exponential rate at which the mean base water potential for germination [Ψb(50)], the hydrotime required for seed germination (θH) and the standard deviation of base water potential (σΨb) change during moist storage under dormancy inductive temperatures of 10, 15, 20 and 25°C (see Fig. 3). K values were obtained through optimization to get the value of K which minimized the RMSE between simulated and observed values of Ψb(50), θH and σΨb at each storage temperature for seeds germinated at the four tested thermal regimes (10, 15, 20 and 10/20°C) according to: y = yi + {[(yi – yf) × exp (–K x)] + (yi – yf)} for panel A and y = yi – (yi + yf) × [1 – exp (–K x)] for panels B and C, where subscripts i and f denote the initial and final values of y, respectively, and K is the exponential changing rate. The continuous lines are adjusted bi-linear equations with a similar R2 of 0.99. Note that the scales are different between panels.

Figure 6

Table 3. Values of K obtained from the adjustment of exponential equations

Figure 7

Figure 5. (A) Simulated progressive shifts in the distribution of the base water potential (Ψb) of the seed population and reductions in the hydrotime required for seed germination (θH) during dormancy induction at 20°C for seeds germinated at 10/20°C. Seeds were stratified for 109 days at 5°C (continuous line) and afterwards moist-stored for 2, 5, 9 and 15 days at 20°C (interrupted lines). Ψb distributions were simulated using equations 3 [Ψb(50)] and 5 (σΨb) with K values of 0.22 and 0.5, respectively, and Ψbi(50) of –2.52 MPa, Ψbf(50) of 0.05 MPa, σΨbi of 1.06 MPa and σΨbf of 0.54 MPa. θH values were simulated using equation 4 with a K value of 0.19, θHi of 304 MPa h and θHf of 122 MPa h. (B) Observed vs simulated germination data for previously stratified seeds (moist-stored for 109 days at 5°C) stored at 10, 15, 20 and 25°C for different periods and germinated at 10, 15, 20 and 10/20°C under water potentials of 0, –0.2 and –0.4 MPa (excluding data for seeds stored and germinated at 10°C, the R2 is 0.85). Simulations were performed using equations 2, 3, 4 and 5. The values of K used in equations 3, 4 and 5 for each storage temperature were those presented in Fig. 4, while initial and final value of each parameter were those indicated in Table 2.

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