Abstract
We excavated the root systems of Pinus ponderosa trees growing on a steeply sloped, volcanic ash-influenced soil in the northern Rocky Mountains of the United States to assess their functional coarse-root traits and root system architecture. Trees, outplanted as one-year-old seedlings from a container nursery, were in their 32nd growing season on the site. We found that the trees had deployed more roots, in terms of length and volume, in the downslope and windward quadrants than in their upslope and leeward quadrants, likely a response to mechanical forces toward improving stability. Moreover, we observed the development of three types of root cages (tight, enlarged, and diffused) that likely reflect micro-site characteristics. As the cage type transitioned from tight to enlarged to diffused we measured a decrease in the overall volume of the roots associated with the cage and the taproot becoming a more prominent contributor to the overall volume of the cage. Finally, we noted the development of specialty roots, namely those with I-beam and T-beam shapes in cross section, in the downslope quadrant; these types of roots are known to better counteract compression mechanical forces. These observations improve our understanding of root plasticity and tree rooting response to environmental stimuli, which is becoming an increasingly critical topic as changes in climate increase the frequency and intensity of storms.
Highlights
The global need for forest restoration continues to increase; attempting to meet that challenge is a host of current initiatives spanning scales from local to global and addressing nearly 500 million hectares
Our objective was to use an information-theoretic approach to understand how P. ponderosa trees modify the growth of their root systems in slope conditions on an ash-cap soil type to adjust to different rooting environment stimuli
The variability observed among the root systems of different tree species, and within a particular species, is considered to be an adaptation response to the variability of the rooting environment (Henderson et al, 1983; Coutts et al, 1990)
Summary
The global need for forest restoration continues to increase; attempting to meet that challenge is a host of current initiatives spanning scales from local to global and addressing nearly 500 million hectares (see Haase and Davis, 2017). Extreme weather events (i.e., drought and windstorms) that occur with greater year-to-year variation are expected to occur more frequently or with greater severity (Meehl et al, 2000; Harris et al, 2006; Allen, 2009; Allen et al, 2010) This shortterm change to climate, along with longer-term changes to climatic means (i.e., temperature and precipitation) are likely important drivers of forest degradation (Stanturf et al, 2014) that will increase the need for restoration across all scales (Chen et al, 2011)
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