Carrer Marco, Castagneri Daniele, Prendin Angela L, Petit Giai, von Arx Georg
Dipartimento Territorio e Sistemi Agro-Forestali, Universitá degli Studi di PadovaLegnaro, Italy.
Swiss Federal Institute for Forest, Snow and Landscape Research WSLBirmensdorf, Switzerland.
Front Plant Sci. 2017 May 8;8:737. doi: 10.3389/fpls.2017.00737. eCollection 2017.
The study of xylogenesis or wood formation is a powerful, yet labor intensive monitoring approach to investigate intra-annual tree growth responses to environmental factors. However, it seldom covers more than a few growing seasons, so is in contrast to the much longer lifespan of woody plants and the time scale of many environmental processes. Here we applied a novel retrospective approach to test the long-term (1926-2012) consistency in the timing of onset and ending of cambial activity, and in the maximum cambial cell division rate in two conifer species, European larch and Norway spruce at high-elevation in the Alps. We correlated daily temperature with time series of cell number and lumen area partitioned into intra-annual sectors. For both species, we found a good correspondence (1-10 days offset) between the periods when anatomical traits had significant correlations with temperature in recent decades (1969-2012) and available xylogenesis data (1996-2005), previously collected at the same site. Yet, results for the 1926-1968 period indicate a later onset and earlier ending of the cambial activity by 6-30 days. Conversely, the peak in the correlation between annual cell number and temperature, which should correspond to the peak in secondary growth rate, was quite stable over time, with just a minor advance of 4-5 days in the recent decades. Our analyses on time series of wood anatomical traits proved useful to infer on past long-term changes in xylogenetic phases. Combined with intensive continuous monitoring, our approach will improve the understanding of tree responses to climate variability in both the short- and long-term context.
木质部形成或木材形成的研究是一种强大但劳动强度大的监测方法,用于研究树木对环境因素的年内生长响应。然而,它很少涵盖超过几个生长季节,因此与木本植物长得多的寿命以及许多环境过程的时间尺度形成对比。在此,我们应用了一种新颖的回顾性方法,来测试欧洲落叶松和挪威云杉这两种针叶树在阿尔卑斯山高海拔地区形成层活动开始和结束时间以及最大形成层细胞分裂率的长期(1926 - 2012年)一致性。我们将每日温度与划分为年内各时段的细胞数量和管腔面积时间序列进行了关联。对于这两个物种,我们发现近几十年(1969 - 2012年)解剖学特征与温度有显著相关性的时期与之前在同一地点收集的可用木质部形成数据(1996 - 2005年)之间存在良好的对应关系(偏移1 - 10天)。然而,1926 - 1968年期间的结果表明形成层活动开始时间较晚且结束时间较早,相差6 - 30天。相反,年度细胞数量与温度之间的相关性峰值,应对应于次生生长速率的峰值,随时间相当稳定,近几十年仅提前了4 - 5天。我们对木材解剖学特征时间序列的分析证明有助于推断木质部形成阶段过去的长期变化。结合密集的连续监测,我们的方法将提高对树木在短期和长期背景下对气候变化响应的理解。