Instructor materials

Overview

The aspen leaf miner (Phyllocnistis populiella) is a tiny moth that feeds inside the epidermal tissue of aspen leaves. The species has caused widespread damage to aspen trees in Alaska and northern Canada for several decades. This exercise challenges students to use data on the physiology of damaged and undamaged leaves to assess the impact of the leaf miner for aspen photosynthesis and water balance, and more generally to better understand the important role of the leaf epidermis in leaf function.


Key Concepts


Student Learning Outcomes


Prior Knowledge

Students should have a basic understanding of 


Background

The aspen leaf miner moth (Phyllocnistis populiella) is a tiny herbivorous insect that has caused major damage to aspen trees in Alaska and parts of Canada since around the year 2000. Larvae of the moth feed in an unusual manner. They dwell throughout the juvenile period within the leaf’s epidermal layer - a single cell layer deep - slicing a path through the cells and drinking the cell contents released. The damaged portion of the epidermis appears as a white serpentine mine on either the top or the bottom of the leaf. This targeted damage to one leaf tissue provides an opportunity to better understand the function and importance of the leaf epidermis.


To disentangle the effects of leaf mining on the top and bottom of the leaf, researchers at the University of Alaska Fairbanks removed leaf miner eggs from the top, bottom, or both sides of aspen leaves. When the damage was at its maximum in mid-summer, they measured gas exchange on the leaves, including photosynthesis - the rate at which CO2 was assimilated by leaves - and stomatal conductance - the rate at which water vapor was lost from leaves through stomata.  


To disentangle the effects of leaf mining on the top and bottom of the leaf, researchers at the University of Alaska Fairbanks removed leaf miner eggs from the top, bottom, or both sides of aspen leaves. When the damage was at its maximum in mid-summer, they measured gas exchange on the leaves, including photosynthesis - the rate at which CO2 was assimilated by leaves - and stomatal conductance - the rate at which water vapor was lost from leaves through stomata. 

Materials 


Teaching Tips 

Working with the data


Running the activity


Additional Reading


Basic biology of the aspen leaf miner

U.S. Forest Service. 2011. Aspen leaf miner. Forest Health Protection, Rocky Mountain Region. https://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5347213.pdf


Impact of the aspen leaf miner on aspen physiology and productivity

Boyd, Melissa A., M. A., T. B. Logan, D. Patricia, G. Scott, R. Brendan, W. Diane, W. Xanthe, and C. M. Michelle. 2019. Impacts of climate and insect herbivory on productivity and physiology of trembling aspen (Populus tremuloides) in Alaskan boreal forests. Environmental Research Letters:085010.https://doi.org/10.1088/1748-9326/ab215f 

Wagner, D., L. Defoliart, P. Doak, and J. Schneiderheinze. 2008. Impact of epidermal leaf mining by the aspen leaf miner (Phyllocnistis populiella) on growth, physiology, and leaf longevity of quaking aspen. Oecologia 157:259–267.https://doi.org/10.1007/s00442-008-1067-1 

Wagner, D., J. M. Wheeler, and S. J. Burr. 2020. The leaf miner Phyllocnistis populiella negatively impacts water relations in aspen. Tree Physiology 40:580–590. https://doi.org/10.1093/treephys/tpz109 


Aspen and the changing boreal forest 

Johnstone, J. F., T. N. Hollingsworth, F. S. Chapin, and M. C. Mack. 2010. Changes in fire regime break the legacy lock on successional trajectories in Alaskan boreal forest. Global Change Biology 16:1281–1295. https://doi.org/10.1111/j.1365-2486.2009.02051.x

Mack, M. C., X. J. Walker, J. F. Johnstone, H. D. Alexander, A. M. Melvin, M. Jean, and S. N. Miller. 2021. Carbon loss from boreal forest wildfires offset by increased dominance of deciduous trees. Science 372:280–283. http://doi.org/10.1126/science.abf3903


Extensions to the module

The data set that students work with in this activity contains a large number of variables that are not used in this particular activity, but that could be used to extend the activity for students. Some examples of extension follow. 


Leaf mining - Students could explore the extent of mining damage to the leaves; or explore top and bottom leaf mining as a continuous effect on photosynthesis rather than a nominal effect as we do here. Students might also explore the effect of the location of leaf mining on other variables in the dataset, such as the water content of the leaves (% water content). 


Leaf water potential - Advanced students could explore the effects of top and bottom epidermal mining on leaf water potential. Water potential is a measure of the free energy of water, reported in units of pressure. Plant water potentials are always negative, because they are measured in relation to pure water. A brief video introducing leaf water potential and how it is measured can be accessed here. A broader video explaining how water moves through plants, including the role of water potential and leaf conductance, can be accessed here. Water moves from high to low water potential. Evaporation from leaves causes a strong negative water potential in the leaf, which draws water up from the roots. The data set reports aspen leaf water potential measured at midday, when we assume the rate of water loss through stomata is relatively high (and leaf water potential strongly negative), and pre-dawn, when no active photosynthesis is occurring and we assume the stomata are closed. The latter allows us to investigate the role of leaf mining on the rate water vapor is lost across the leaf cuticle (called cuticular conductance), rather than through stomata. This information can be used to address the question, does leaf mining weaken the ability of the cuticle to resist water loss? (Whole leaf water content (%) can also be informative in this regard.) 


Leaf carbon stable isotope composition - Another advanced investigation could examine the effect of upper and lower epidermal mining on leaf carbon stable isotope composition. There are two stable isotopes of carbon: 12C and the rarer 13C. Relative to the heavier isotope, 12C diffuses more rapidly into the leaf from the atmosphere and enters more rapidly into the reaction that fixes C in photosynthesis. As a result, the ratio of 13C to 12C in leaf tissue is lower (more negative) than that in the atmosphere. The stable isotope composition is reported as 𝛿13C, with units of ‰ (per mil). (More information about delta notation and stable isotopes in general can be found here.) When the stomata are narrowed or closed, there is less opportunity for fractionation and the 𝛿13C of the carbon fixed in photosynthesis is less negative; closer in value to the atmosphere. Leaf 𝛿13C can be used to test the hypothesis that stomata of mined leaves are more often closed and unresponsive relative to unmined leaves. 


Answer Guide