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Blister Rust Alters Whitebark Pine Ecology at Treeline: Implications for Treeline at Treeline: Implications for Treeline Response to Climate Change 1 University of Colorado Denver 2 Virginia Tech University University of Iowa 3 University of Iowa Whitebark Pine Ecosystem Foundation, Whitebark Pine Science and Management Workshop, September 19, Coeur d’Alene, Idaho Diana F. Tomback, 1 Lynn M. Resler, 2 George P. Malanson, 3 Emily K. Smith-McKenna, 2 Sarah C. Blakeslee, 1 Jill C. Pyatt 1, and Aaron C. Wagner 1
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Treeline environments Treeline environments are climatically harsh. Soils are often nutrient-poor and unstable. Facilitation between plant species, or a “nurse” object and a plant, may improve plant survival (e.g., Callaway et al. 2002, Brooker et al. 2007). These same processes are essential at the upper treeline limit, enabling communities to respond to climate warming.
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Whitebark Pine (Pinus albicaulis) at Treeline Whitebark pine inhabits upper the subalpine and treeline zone throughout its distribution. It provides important ecosystem services and functions. Seeds dispersed to treeline by Clark’s nutcrackers. In the alpine–treeline ecotone (ATE), there is a mix of solitary krummholz trees and tree islands composed of two or more krummholz trees. Tree islands form when a solitary tree becomes established, and other trees establish leewardTree islands form when a solitary tree becomes established, and other trees establish leeward.
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Tree establishment often occurs in protected locations leeward of: nurse objects nurse plants in microtopography, Lee of Salix ‘ Steps and risers ’
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White pine blister rust and treeline dynamics In some Rocky Mountain communities, whitebark pine is an important nurse tree and tree island initiator. Most common forest associates are subalpine fir (Abies lasiocarpa) and Engelmann spruce (Picea engelmannii). White pine blister rust (pathogen = Cronartium ribicola) is present in all treeline communities examined. Whitebark pine mortality disrupts its role as a tree island initiator. This Impacts community development at and above treeline. Will declines in whitebark pine alter treeline community response to climate warming?
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Where is whitebark pine a tree island initiator? Major initiator Study locationLat. N Standley Glacier, Kootenay NP, BC51˚ 11' Lee Ridge, Glacier NP, MT48˚ 55' Divide/White Calf Mountains, Glacier NP, MT48˚ 40' Line Creek RNA, Custer NF, MT45˚ 02' Not major initiator Willmore Wilderness Park, AB53˚ 46' Parker Ridge, Banff NP, AB52˚ 10' Gibbon Pass, Banff N P, AB51˚ 11' Tibb's Butte, Shoshone NF, MT44˚ 56' Resler et al. 2014, Tomback et al. 2014, Tomback and Resler, in prep
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Why is whitebark pine a majority tree island initiator in some areas? Hypothesis Whitebark pine’s prevalence as a tree island initiator is correlated to its relative abundance as a solitary tree.
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Is whitebark pine’s prevalence as a tree island initiator proportional to its relative abundance as a solitary tree? NO. But it is generally abundant. Tomback et al. 2014, Resler et al. 2013; Tomback & Resler in prep.
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Regression analysis Spearman rank correlation: 0.2619, n = 8, P = 0.501
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Why is whitebark pine so abundant within climatically harsh treeline communities? Hypothesis: Whitebark pine has greater hardiness under harsh treeline conditions: We compared hardiness among whitebark pine, Engelmann spruce, and subalpine fir. We defined hardiness in three ways: Qualitative assessment of vigor. Requirements for a protective microsite. Annual shoot length, reflecting carbon acquisition and allocation.
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Primary study areas Research from 2006 through 2014. Divide/White Calf Mountains--Glacier National Park and Blackfeet Tribal Land, MT--elevation ca. 2,200 m. Line Creek Research Natural Area, Custer National Forest, Beartooth Plateau, MT--elevation ca. 2,950 m.
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Relative hardiness 1) Qualitative assessment of vigor (1 to 4 = best), based on: windward needle death, condition of new shoots, and needle color. Divide Mtn.—Whitebark pine had significantly higher vigor than both fir and spruce (Kruskal-Wallis, χ 2 = 18.9, df = 2, P = 7.8e-5, post hoc W = 19557, P = 0.037,post hoc, W = 13026.5, P = 2.08e-5) Line Creek—No differences. 2) Association of solitary trees with a protective microsite. At both Divide Mtn. and Line Creek, fewer whitebark pine were associated with a protective microsite than fir or spruce. (χ 2 = 9.769, df = 2, P = 0.008, χ 2 = 11.3217, df = 2, P = 0.003) Blakeslee et al., 2012, MS.
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Shoot lengths—bootstrapped 95% confidence intervals (Blakeslee et al. in prep., Wagner) Whitebark PineSubalpine FirEngelmann Spruce Divide Mountain1715 Line Creek RNA211220
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Why is whitebark pine a majority tree island initiator? Hypotheses Whitebark pine offers greater microsite protection than other conifer species.
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Does whitebark pine offer better leeward protection than associated conifers? Measured 11 biophysical variables leeward of four common treeline microsites: whitebark pine, Engelmann spruce, rock, and unprotected microsite. Air & soil temp., soil moisture, wind speed & gusts, PAR. Soil for total carbon and nitrogen; leeward sky exposure. Pyatt 2013; Pyatt et al, MS.
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Microclimate and microsite: summary Compared to rock and open microsites, leeward conifer microsites had more favorable microclimates: Reduced maximum air and soil temperatures. Higher minimum soil temperatures. Lower PAR. Reduced wind and gust speeds. Whitebark pine microsites and spruce microsites offered similarly protective microclimates. No statistical difference in soil C and N. BUT, whitebark pine had significantly lower sky exposure in leeward microsites in comparison with subalpine fir, rock, and open sites (Boggs, Bevency Kruskall-Wallis, n = 8, R = 48.61, P =0.000).
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Whitebark pine offers leeward protection Pyatt 2013
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Is facilitation really occurring? Simulating the impact of blister rust In 2010, we selected 22 control and 22 experimental dyads on Divide/White Calf Mtn. Dyad = windward whitebark pine; leeward spruce or fir. We girdled and defoliated the experimental windward whitebark pine in 2010. Note: all experimental whitebark pine were infected by blister rust. We measured shoot lengths on leeward conifers in 2010, 2011, and 2012. Blakeslee 2012; Blakeslee et al. MS.
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Leeward conifer shoot lengths— bootstrapped 95% confidence intervals (Blakeslee et al. MS., Wagner)
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Is facilitation occurring? seeds and seedlings We examined survival rates of planted seedlings and the germination rates of sown seeds among four leeward microsites: whitebark pine, spruce, rock, and open. Divide Mtn.—sowed spruce seeds and planted fir seedlings. Line Creek—sowed spruce seeds and planted spruce seedlings. 20 replicates for each microsite type for seedlings and for seeds. (Blakeslee 2012; Blakeslee et al. in prep)
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Facilitation: seeds and seedlings Seedlings Divide Mtn.—90% mortality of fir seedlings. Line Creek—63.1% mortality of spruce seedlings. No significant differences in seedling survival among microsite types at Divide Mountain or Line Creek RNA. Seeds Divide Mtn.— 20% of fir seeds germinated. Higher than expected germination occurred in rock microsites and fewer than expected in whitebark microsites (Fisher’s Exact Test, P = 0.01). On Divide, 42 out of 80 germinants survived to September. Line Creek—1.8% of spruce seeds germinated. No differences among microsites.
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Comparison of observed vs. expected cotyledon seedling survival among microsites. --Seedlings in whitebark microsites had a 5.7 times greater than expected survival advantage over the summer. --Very low comparative risk of death (0.18 times expected). MicrositeRelative Survival AdvantageRelative Risk of Death Whitebark5.700.18 Spruce0.891.12 Rock1.080.93 Open0.641.56 Divide Mtn. Summer survival of seedlings
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Blister rust at treeline Intensive sampling using 15 m x 15 m plots indicates widespread blister rust infection: Divide Mountain, 23.6% Line Creek RNA, 19.2% Previous sampling at six other treeline sites in Glacier NP (15 x 15 m plots): Infection rates of 36-96%. Overall infection rate of 47%. (Smith-McKenna et al. 2011; Smith- McKenna 2013)
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Decline in treeline whitebark pine Whitebark pine shows little or no response to global warming in upper treeline boundary Reduced ability of treeline to respond (or lag in response time) to global warming at the upper boundary Reduced ability of treeline to respond (or lag in response time) to global warming at the upper boundary Will declines in whitebark pine alter treeline response to climate warming? Fewer seeds dispersed to treeline by nutcrackers: blister rust in subalpine whitebark pine Blister rust damages and kills whitebark pine at treeline Fewer tree islands initiated by whitebark pine (less facilitation)
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Agent Based Models: climate and blister rust Smith-McKenna et al., in press In the ‘Climate’ scenario, both pine and spruce “agents” increased when conditions improved, and trees advanced to higher elevations into previous tundra cells. This scenario increased whitebark pine numbers by 28.8%. Both pine and spruce populations increased as tundra concurrently declined. In the ‘Climate+Disease’ scenario, mortality from blister rust reduced pine populations despite improved site quality conditions. Both spruce populations and tundra increased. The threshold of change from dominating pine agents to spruce appeared around year 630.
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Agent Based Model preliminary results Smith-McKenna et al., in press
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Conclusion Our collective studies suggest: Whitebark pine tolerates harsh treeline better than associated conifers. It provides protective leeward microsites. Whitebark pine decline from blister rust will delay or impede treeline response to climate warming. Postscript What are possible reasons why whitebark pine is not a majority tree island initiator in some regions? Cold, snowy sites support more spruce and fir than whitebark pine. Whitebark tolerates the harshest exposed sites and ridgelines.
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Postscript
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ACKNOWLEDGMENTS Field assistance: Libby Pansing, Solé Diaz, Kodi Augare.Logistics: Glacier National Park (thanks to Tara Carolin) Blackfeet Nation (thanks to Mark Magee) Shoshone and Custer National Forests (thanks to Ken Houston) Rocky Mountain Research Station, Ft. Collins Financial Support: National Science Foundation, Geography Program: National Science Foundation, Geography Program: L. Resler, D. Tomback, and G. Malanson L. Resler, D. Tomback, and G. Malanson NSF BCS-0850548
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