Abstract

Climate change will affect radial growth patterns of trees, which will result in different forest productivity, wood properties, and timber quality. While many studies have been published on xylem phenology and anatomy lately, little is known about the phenology of earlywood and latewood formation, also in relation to cambial phenology. Even less information is available for phloem. Here, we examined year-to-year variability of the transition dates from earlywood to latewood and from early phloem to late phloem in Norway spruce (Picea abies) from three temperate sites, two in Slovenia and one in the Czech Republic. Data on xylem and phloem formation were collected during 2009–2011. Sensitivity analysis was performed to determine the specific contribution of growth rate and duration on wood and phloem production, separately for early and late formed parts. We found significant differences in the transition date from earlywood to latewood between the selected sites, but not between growth seasons in trees from the same site. It occurred in the first week of July at PAN and MEN and more than two weeks later at RAJ. The duration of earlywood formation was longer than that of latewood formation; from 31.4 days at PAN to 61.3 days at RAJ. In phloem, we found differences in transition date from early phloem to late phloem also between the analysed growth seasons; from 2.5 weeks at PAN to 4 weeks at RAJ Compared to the transition from earlywood to latewood the transition from early phloem to late phloem occurred 25–64 days earlier. There was no significant relationship between the onset of cambial cell production and the transition dates. The findings are important to better understand the inter-annual variability of these phenological events in spruce from three contrasting temperate sites, and how it is reflected in xylem and phloem anatomy.

Highlights

  • Global warming is expected to shift phenological phases of trees and thereby lengthen the growing season

  • We found that the duration of cambial cell production period was the longest at Panška reka (PAN) and the most variable at RAJ (PAN: 138.4 ± 14.3 days; Menina planina (MEN): 109.9 ± 16.3 days; RAJ: 122.5 ± 20.1 days) [17]

  • At PAN, the xylem widths were in all cases the widest, while at MEN and RAJ the difference in xylem widths depended on the year

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Summary

Introduction

Global warming is expected to shift phenological phases of trees and thereby lengthen the growing season. It has been shown that the same tree species growing in different environments can adjust the structure of vascular tissues to some extent to local conditions, indicating their plasticity of radial growth for optimal tree functioning [11,12,13]. These data may be critically important in evaluating the range of plasticity in species under different environmental conditions as a first step in predicting their responses to future climatic scenarios [12]. Even less is known about phloem phenology and transition from early phloem to late phloem, tissue parts with different main roles in a tree [16]

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