Opinion
Diel growth dynamics in tree stems: linking anatomy and ecophysiology

https://doi.org/10.1016/j.tplants.2015.03.015Get rights and content

Highlights

  • Although tree stem growth is ubiquitous with huge ecological implications, it is poorly understood.

  • Quantification of diel patterns in both water and carbon relations is critical for a complete understanding.

  • Anatomy and ecophysiology should be combined in new experiments and models to build an integrated theory.

  • An integrated theory is much needed to understand and predict trends in stem growth as impacted by climate.

Impacts of climate on stem growth in trees are studied in anatomical, ecophysiological, and ecological disciplines, but an integrative framework to assess those impacts remains lacking. In this opinion article, we argue that three research efforts are required to provide that integration. First, we need to identify the missing links in diel patterns in stem diameter and stem growth and relate those patterns to the underlying mechanisms that control water and carbon balance. Second, we should focus on the understudied mechanisms responsible for seasonal impacts on such diel patterns. Third, information on stem anatomy and ecophysiology should be integrated in the same experiments and mechanistic plant growth models to capture both diel and seasonal scales.

Section snippets

Tree stem growth has huge implications but is poorly understood

Forests cover 30% of Earth's land surface, store 45% of terrestrial carbon, and are responsible for 50% of the terrestrial net primary production 1, 2. Forest productivity has increased globally over the past decades, which has been attributed to the positive effect of increasing CO2 on tree growth, thus far offsetting negative impacts of warming and drought 3, 4. However, the long-term impacts on trees and forests of increasing CO2, rising temperatures, and drought remain highly uncertain 5, 6

Carbon and water fluxes in stem segments

Water is transported upward in the sapwood, downward in the phloem, and radially between sapwood and phloem and is stored in both sapwood and phloem (Figure 1, fluxes/pools steps 1–4). Carbon is transported downward in the phloem in the form of sugars (Figure 1, step 2) and those sugars are used for maintenance of living cells in sapwood, cambium, and phloem (Figure 1, step 6), for growth in the cambium and developing cells (Figure 1, step 5), or for storage in the form of starch (Figure 1,

Stem dynamics in water fluxes and storage

Large forest trees lose up to 99% of their acquired water through leaf transpiration, whereas less than 1% is retained in biomass [9]. On a sunny summer day, an adult tree may lose and acquire several hundred liters of water. Leaf transpiration typically starts minutes to hours earlier than water flow in stem and roots, because transpiration is also supported by water from internal water storage [10]. The daily amount of water withdrawn from storage contributes 5–22% to the total daily water

Stem dynamics in carbon fluxes and storage

Diel patterns in fluxes, use, and storage in tree stems are much less well understood for carbon than for water (Figure 2), even in unstressed conditions with ample soil water reserves. Besides water, radial stem growth depends on carbon as structural material for the formation of new tissue and as a source for metabolic energy [33]. The carbon that is locally used for both processes may come from four sources: recently fixed sugars that are transported in the phloem; transitory leaf starch

Seasonal impacts on diel stem growth

Overall, mechanistic plant models capture the water dynamics and diel stem growth variation 25, 30, 50, but most of the emerging dynamics in carbon remain hypothetical. A second complication is that the models cannot yet capture the gradual changes in those dynamics across the growing season because of rudimentary knowledge of the coordination between stem tissue formation and whole tree function (Figure 3). Seasonal stem growth as measured by dendrometers reflects the formation of both xylem

Concluding remarks

Radial stem growth and its ecological implications have been studied by scientists from rather separate scientific domains (anatomy, ecophysiology, dendrochronology, ecology) and we still lack an integrative and tested theory to understand the causes and consequences of diel stem growth patterns. Such a theory is required to understand diel and seasonal growth patterns in trees and, in turn, the long-term trends in stem growth as impacted by climate. One major gap in our knowledge is the

Acknowledgments

The authors thank R.O. Teskey for helpful comments on the original manuscript, two anonymous reviewers for valuable inputs, and the Research Foundation – Flanders (FWO) (research programs G.0319.13N and G.0941.15N granted to K.S.) for funding. The opinions expressed in this paper were partly inspired by and are linked to the activities conducted within the COST FP1106 network Studying Tree Responses to Extreme Events: A Synthesis (STReESS).

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