Quanyan Tian , Zhibin He , Shengchun Xiao , Xiaomei Peng , Pengfei Lin , Xi Zhu , Xiangyan Feng
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引用次数: 0
Abstract
Tree stem radial growth could be used to estimate forest productivity, which plays a dominant role in the carbon sink of terrestrial ecosystems. However, it is still obscure how intra-annual stem radial growth is regulated by environmental variables. Here, we monitored Qinghai spruce stem radial growth over seven years and analyzed the environmental drivers of the intra-annual stem radial changes in the Qilian Mountains at low (2700 m) and high altitudes (3200 m). We found that stem radial growth initiated when the daily mean minimum air temperature reached 1.6oC, while the cessation of stem growth was unrelated to temperatures and water conditions. Initiations of stem growth at 2700 m were significantly earlier than that at 3200 m. Maximum growth rates were observed before the summer solstice at low altitude, whereas at high altitude, the majority of them occurred after the summer solstice. Most variability in annual stem increment (AI) can be explained by the rate (Rm) than by the duration of stem growth (∆t), and 78.9 % and 69.6 % of the variability in AI were attributable to Rm for the lower and upper site, respectively. Structural equation modeling revealed that precipitation (P) could both directly positively influence stem radial increment (SRI) and indirectly positively influence SRI through influencing relative humidity (RH), but the positive effect of P on SRI was higher at low altitude than at high altitude. Daily minimum air temperature (Tmin) was also the main direct diver of SRI, and the positive effect of Tmin on SRI was higher at high altitude than at low altitude. Considering the trends in climate warming and humidification over the past decades, climate changes would result in earlier initiation of Qinghai spruce stem growth and promote the growth through positive response to increased precipitation in low altitude and through elevated temperature in high altitude, respectively.
树干径向生长可用于估算森林生产力,而森林生产力在陆地生态系统的碳汇中起着主导作用。然而,环境变量如何调节茎径向年生长量仍是一个未知数。在此,我们对青海云杉茎径向生长进行了长达七年的监测,并分析了祁连山低海拔(2700米)和高海拔(3200米)地区年内茎径向变化的环境驱动因素。我们发现,当日平均最低气温达到1.6oC时,茎的径向生长开始,而茎生长的停止与温度和水条件无关。2700 米处茎干生长的开始时间明显早于 3200 米处。在低海拔地区,夏至前就能观察到最大生长率,而在高海拔地区,大部分生长率出现在夏至后。茎杆生长速率(Rm)比茎杆生长持续时间(Δt)更能解释年茎杆增量(AI)的变化,在低海拔和高海拔地区,Rm分别占AI变化的78.9%和69.6%。结构方程模型显示,降水(P)既能直接对茎径向增量(SRI)产生积极影响,也能通过影响相对湿度(RH)间接对SRI产生积极影响,但低海拔地区降水对SRI的积极影响高于高海拔地区。日最低气温(Tmin)也是 SRI 的主要直接影响因素,Tmin 对 SRI 的正向影响在高海拔地区高于低海拔地区。考虑到过去几十年气候变暖和增湿的趋势,气候变化将导致青海云杉茎干提前开始生长,并分别通过对低海拔地区降水增加和高海拔地区温度升高的正反应促进其生长。
期刊介绍:
The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere.
The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.