当前位置: X-MOL 学术Seed Sci. Res. › 论文详情
Our official English website, www.x-mol.net, welcomes your feedback! (Note: you will need to create a separate account there.)
Cold stratification in winter is more than enough for seed dormancy-break of summer annuals in eastern North America: implications for climate change
Seed Science Research ( IF 2.1 ) Pub Date : 2022-06-29 , DOI: 10.1017/s0960258522000125
Carol C. Baskin , Jerry M. Baskin

Germination of seeds of some summer annuals in Kentucky (eastern USA) in late-winter lead to the hypothesis that under present climate conditions the whole length of the winter cold stratification (CS) period is not required for dormancy-break of seeds of summer annuals with physiological dormancy (PD). We evaluated our data from germination phenology studies of 45 species (69 datasets) and buried-seed studies of 33 species (44 datasets). We determined time and temperature of germination after CS and percentage of the total number of hours of CS during winter (% of winter CS) seeds received prior to start of germination. In the phenology studies, mean temperature during the week of first germination for C3 and C4 species was 11.1 and 14.4°C, respectively, and % of winter CS was 80.8 and 87.4, respectively. In the buried-seed studies, % of CS for C3 and C4 species was 40.8 and 48.1, respectively, when they germinated to 25% at 20/10°C. For 32 of 33 species in the buried-seed studies, the minimum temperature at which seeds germinated decreased with increased CS; thus, seeds had Type 2 non-deep PD. The time of germination is controlled by a number of hours of CS, a decrease in minimum temperature at which seeds can germinate and a temperature increase in early spring. Seeds can germinate at relatively high temperatures as early as December and January, but they continue to be CS until spring. Temperature increases in eastern North America due to global warming are not likely to inhibit the germination of summer annuals with PD in spring.



中文翻译:

冬季的冷分层对于北美东部夏季一年生植物的种子休眠期来说绰绰有余:对气候变化的影响

肯塔基州(美国东部)的一些夏季一年生植物种子在冬末发芽导致了这样一种假设,即在目前的气候条件下,夏季一年生植物种子的休眠中断不需要整个冬季寒冷分层(CS)期具有生理休眠(PD)。我们评估了来自 45 个物种(69 个数据集)的萌发物候学研究和 33 个物种(44 个数据集)的埋藏种子研究的数据。我们确定了 CS 后发芽的时间和温度,以及在发芽​​开始之前收到的冬季 CS 总小时数(冬季 CS 的百分比)的百分比。在物候研究中,C3 和 C4 物种第一次发芽一周的平均温度分别为 11.1 和 14.4°C,冬季 CS 百分比分别为 80.8 和 87.4。在埋藏种子研究中,当 C3 和 C4 物种在 20/10°C 下发芽至 25% 时,CS 的百分比分别为 40.8 和 48.1。在埋种子研究的 33 个物种中,有 32 个物种萌发的最低温度随着 CS 的增加而降低;因此,种子具有 2 型非深度 PD。发芽时间由几个小时的 CS、种子发芽的最低温度降低和早春温度升高来控制。种子早在 12 月和 1 月就可以在相对较高的温度下发芽,但它们一直持续到春季。由于全球变暖,北美东部的气温升高不太可能抑制夏季一年生植物在春季的发芽。种子萌发的最低温度随着 CS 的增加而降低;因此,种子具有 2 型非深度 PD。发芽时间由几个小时的 CS、种子发芽的最低温度降低和早春温度升高来控制。种子早在 12 月和 1 月就可以在相对较高的温度下发芽,但它们一直持续到春季。由于全球变暖,北美东部的气温升高不太可能抑制夏季一年生植物在春季的发芽。种子萌发的最低温度随着 CS 的增加而降低;因此,种子具有 2 型非深度 PD。发芽时间由几个小时的 CS、种子发芽的最低温度降低和早春温度升高来控制。种子早在 12 月和 1 月就可以在相对较高的温度下发芽,但它们一直持续到春季。由于全球变暖,北美东部的气温升高不太可能抑制夏季一年生植物在春季的发芽。种子早在 12 月和 1 月就可以在相对较高的温度下发芽,但它们一直持续到春季。由于全球变暖,北美东部的气温升高不太可能抑制夏季一年生植物在春季的发芽。种子早在 12 月和 1 月就可以在相对较高的温度下发芽,但它们一直持续到春季。由于全球变暖,北美东部的气温升高不太可能抑制夏季一年生植物在春季的发芽。

更新日期:2022-06-29
down
wechat
bug