Evidence of climate trend effects on vegetation patterns in the US Pacific Northwest— Response of epiphytic lichens from 1993-2009 Linda Geiser1, Sarah Jovan2, Doug Glavich1 1US Forest Service, Pacific Northwest Air Resource Management Program, PO Box 1148, 17 Corvallis, OR 97339 2US Forest Service, Pacific Northwest Research Station, Forest Inventory and Analysis program, (FIA) 20 SW Main, Suite 400, Portland, OR 15 97205 Introduction • The FIA Air Quality and Climate Indicator is designed to assess status and trends in air pollution and climate affecting the nation’s forests and to provide evidence of ecological effects from these trends. • Uses lichen community composition • Which shifts as different species reach their tolerance limits. • Shows response before effects on less sensitive flora can be detected. Lichens are symbiotic organisms consisting of a fungus and a photosynthetic green algal +/or blue-green bacterial partner. Unique morphology and physiology underlies special sensitivity of lichens • Epiphytes are little influenced by soil nutrition –no roots, aerial location. Rely on atmospheric deposition for nutrients and moisture. • No barrier cuticle or guard cells…moisture, nutrients, and pollutants are absorbed passively over entire surface of the lichen. • Dehydration concentrates pollutants • Precipitation, if clean, leaches pollutants • Dynamic equilibrium , fast response. • Require wetting and drying for nutrient exchange between symbionts. • Species are differentially adapted to hot, dry vs. cool, wet climate regimes and to atmospheric deposition of nutrients and acidity. Every lichen is adapted to specific atmospheric deposition levels & chemistry Lichens of low fertility, acidic environments. ©Erin Cooper Lichens of high nutrient, more alkaline environments … so lichen species composition can be used to pinpoint a site along regional air pollution gradients. In Oregon’s Willamette Valley, oligotrophic species thrive in clean air. And eutrophic species thrive where nutrient availability is greater Every lichen is also adapted to a specific range of climatic conditions… … © Sharnoff As climate becomes warmer the composition of coastal epiphytes changes dramatically …therefore lichen community composition can be used to pin-point a site along regional climate gradients. Data collection • • • • 0.4 ha plot on the systematic national P3 grid (1 plot/96,000ac) Surveys up to 2 hours Collect sample of each species detected And rate abundance: 1 = Infrequent (< 3 thalli) 2 = Uncommon (4-10 thalli) 3 = Common (>10 thalli; covers < 50% of all boles and branches) 4 = Abundant (>10 thalli covers > 50% of all boles and branches) • ID by regional taxonomic expert Lichens sampled in shaded area The FIA AQ & Climate Network Jovan & McCune. 2005. Eco Apps 15: 1712-1726. Jovan & McCune. 2006. Air, Water, Soil Poll. 170:69-93. McCune et al. 1997. Bryologist 100: 145-158. Geiser & Neitlich. 2007. Env. Poll. 145:203-218. Western PNW model Round 1: 1993-2001 1416 plots were surveyed by: • FIA (23 km grid) • USFS PNW regional Air Program (5.4 km grid) Round 2: 2003-2009 350 Air program plots were re-surveyed • Providing data for this trends analysis Geiser, L.H.; Neitlich, P.N. 2007. Env Poll145: 203-218. Non-metric multi-dimensional scaling (NMS) ordination Coast Distance 2: Climate AxisAxis 2 Elev Continentality Longitude Lichen %N %RH Mean T Min Dec T Axis 1:Axis Air 1 Quality Poll? 0 1 Western PNW model Two major influences : •air quality •climate scored as distance along Axes 1 & 2 Geiser & Neitlich. 2007. Env. Poll. 145: 203-218. Air Quality and Climate scores Round 1: 1993-2001 Geiser, L.H.; Neitlich, P.N. 2007. Air pollution and climate gradients in western Oregon and Washington indicated by epiphytic macrolichens. Environmental Pollution 145: 203-218. % 30 Air scores and all available measures of atmospheric N deposition are correlated 20 10 0 -1 Total Inorg N kg/ ha Linear Fit 0.75 0.5 1 0.25 % Eutrophs 0 0 -0.25 -0.5 -1 CMAQ total N 1 2 1 Bivariate Fit of Mean Air S core By Mean NH4 mBivariate g/L 95-98 Fit of % Eutrophs By V21s_Air Mean Air Score AirScore Leverage Residuals Le verage Pl ot 0 Air Score 3 4 5 6 7 NADP Wet N -0.75 0 8 .025 .05 .075 100 90 80 70 60 50 40 30 20 10 0 % Eutrophs -1 .1 Mean NH4 mg/L 95-98 0 Air Score 1 (ugFitm -3 y-1) Bivaria teTotal Fit of Air N Score NP laglaP<.0001Bivariate Fit of Ai r Score By Am bient fine parti culate NLinear Inorg kg/haBy Leverage, Bivariate Fit of % oligotrophs By V21s_Air 0.75 Linear Fit 0 -1 Lichen % N 0 .1 .2 .3 .4 .5 .6 .7 .8 .9 1 1.11.21.31.41.5 NPlagla 0.5 Mean Air Score = -0.481793 + 12.61532 Mean NH4 mg/L 95- 98 90 Summa ry of Fit 0.25 70 RSquare 0RSquare A dj Root Mean Square Error -0.25 Mean of Response Obs ervations (or Sum Wgts) -0.5 0.738111 0.694463 0.242337 0.072493 8 % Oligotrophs Air Score Air Score 100 Linear Fit 1 60 50 40 30 20 IMPROVE N 10 Analysi s of V ariance -0.75Source DF Sum of Squares Mean Square 0 .2 .4 .6 .8 1 Model 1 0.9931078 0.993108 Ambient f ine par ticulate N (ug m-3 y -1) Error 6 0.3523639 0.058727 C. Total 7 1.3454716 Linear Fit % Oligotrophs 80 F Ratio 0 -1 16.9105 Prob > F 0 Air Score Linear Fit 1 0.0063deposition in western Geiser Linear Fitet al. 2010. Lichen-based critical loads for atmospheric nitrogen Pa rame ter Estima tes Linear Fit and Washington forests, 100 Linear FitEnv. Poll. 158: 2412-2421. Oregon USA. Summa ry of Fit RSquare 0.533013 90 Ter m Estimate Std Error t Ratio Prob>|t| Air Score = -0.758189 + 1.9060603 Ambient fine partic ulate N (ug m-3 y-1) 80 Intercept -0.481793 0.159716 -3.02 0.0235 Summa ry of Fit 70 Mean NH4 mg/L 95-98 12.61532 3.067751 4.11 0.0063 60 RSquare 0.933582 ophs Air Score = -0.828166 + 1.3865437 NPlagla Bivariate Fit of % Eutrophs By V21s_Air Climate Change Anticipated effects PREDICTED CHANGE: • Mean annual temperature to ↑1.5 to 3.2° C by 2040. POTENTIAL RESPONSES: • A 1o C temp Δ ↓probability of finding some lichens 2-10 fold. • Most biodiversity contributed by rare species →Concern for local/regional extirpations → Especially coastal (maritime) and subalpine (high elevation) species. 10/14/2010 02:24 PM o Data Table=Climate Category R1=maritime,Climate Category R1=marit Cli mate Cate gory R1= lowla nd -10-9 -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 -10-9 -8 -7 -6 Distributions 10/14/2010 02:24 PM anMin DeCategory cTem pR1=low 1988-1998 C Me anMin Dela DataMe Table=Climate land,Climate Category R1=low Mean min Dec Temp C at round 1 lichen plots (1988-1998) Cli mate Cate gory R1= montane Distributions 10/14/2010 02:24 PM Maritime Me anMin De Data Table=Climate Category R1=montane,Climate Category R1=mont 10/14/2010 02:24 PM Distributions -10-9 -8 -7 -6Category -5 -4 -3 -2 -1 0 elevation,Climate 1 2 3 4 -10-9 -8 -7 R1= -6 Data Table=Climate R1=high Category Cli mate Cate gory R1=p high elevation Me anMin De cTem 1988-1998 C Me anMin De cTem p 1988-1998 C elev ation Lowland Me anMin De Distributions Cli mate -10-9Cate -8 -7gory -6 -5 R1= -4 -3montane -2 -1 0 1 2 3 4 -10-9 -8 -7 -6 Montane Me anMin Me anMin De 10/14/2010 02:24De PMcTem p 1988-1998 C Data Table=Climate Category R1=montane,Climate Category R1=mont Cli mate Cate -10-9 -8 -7gory -6 -5 R1= -4 -3mari -2 -1time 0 1 2 3 4 -10-9 -8 -7 -6 Distributions Hi Elevation 10/14/2010 02:24 PM anMin DeCategory cTem pR1=maritime,Climate 1988-1998 C Me anMin De DataMe Table=Climate Category R1=marit -10-9 -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 -10-9 -8 -7 -6 Distributions Me anMin De cTem p 1988-1998 C Me anMin De M Category R1=maritime,Climate -5 -4 -3 -2 -1 0 1 2 3 4 Category -10-9 -8 -7 -6 -4 -5 -3 -4 -2 -3 -1 -2 -1 -10-9 -8 R1=maritime -7 -6 -5 0 0 1 21 32 43 4 Change in mean annual min Dec T (C) at lichen plots, 1988-98 vs. 1999-2008 Cli mate Cate gory R1= mari time -10-9 -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 10/14/2010 02:24 PM cTem 1988-1998 C Me anMin DeR1= c Te -3 mp-21999-2008 ry R1= p mari time Cli mate Cate nd0 1 2 3C 4 Category -10-9 -8gory -7 -6Category -5 -4lowla -1 -10-9 -8 -6 -7 -5 -6 -4 -5 -3 -4 -2 -3 -1 -2 0 -1 10 21 32 43 4 -1 Data Table=Climate R1=maritime,Climate R1=maritime -10-9 -8 -7 M 10/14/2010 02:24 PM Distributions Category R1=maritime,Climate R1=maritime Data Category Table=Climate Category R1=low land,Climate Category R1=low land Me anMin De cTem 1988-1998 C MeCate anMin DeR1= c Telowla mp 1999-2008 C Cli mate Cate gory R1= p mari time Cli mate gory nd Distributions 10/14/2010 02:24 PM 10/14/2010 02:24 PM oC oC Maritime + 0.7 -5 -4 -3p-21988-1998 -1 0 1 2 C 3 4 MeMe -10-9 -8De -7 De -6 c -5+Te -40.1 -3 -21999-2008 -1 0 1 C 2 3C 4 MeLowland cTem anMin mp anMin cTem p 1988-1998 anMin De c Te mp 1999-2008 C Data Table=Climate Category R1=maritime,Climate R1=maritime Data Category Table=Climate Category R1=low land,Climate Catego Distributions Cli mate Cate gory R1= high elevation Distributions ry R1= montane I999-2008 10/14/2010 02:24 -10-9 -8 PM -7 De -6 cTem -5 means -4 -3p-21988-1998 -1 0 1 2 C 3 4 MeMe -10-9 -8De -7 De -6 c -5 Te -4pmp -3 -21999-2008 -1 0 1 C 2 3C 4 Me Me anMin anMin anMin cTem 1988-1998 M Data Table=Climate Category R1=high elevation,Climate Category R1=high Cli mate Cate gory R1= high elevation Category R1=montane,Climate Category R1=montane -5 -4 -3 -2 -1 0 1 2 3elev 4 ation -10-9 -8 -7 -6 -4 -5 -3 -4 -2 -3 -1 -2 -1 -10-9 -8 -7 -6 -5 0 0 1 21 32 43 4 -10-9 -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 Cli mateI988-1997 Cate gory means R1= montane 10/14/2010 02:24 PM Distributions Data Table=Climate Category R1=high elevation,Climate C 10/14/2010 02:24 PM cTem 1988-1998 C Me anMin De c Te mp 1999-2008 C 4 Me Me anMin De cTem p 1988-1998 C anMin De c-6Te mp 1999-2008 C ry R1= p montane Cli mate Cate-8gory R1= time ation -10-9 -7 -6Category -5 -4mari -3 -2 -1 0 1 2 3elev -10-9 -8 -7 -5 -5 -3 -4 -2 -3 -1 -2 0 -1 10 21 32 43 4 -1 Data Table=Climate R1=montane,Climate Category R1=montane -10-9 -8 -7 -6 -4 M 10/14/2010 02:24 PM Distributions Distributions Category R1=montane,Climate Category R1=montane Data Table=Climate Category R1=maritime,Climate Category R1=maritime MeMe anMin De cTem pmari 1988-1998 C C Me Me anMin De cTem 1988-1998 C anMin DeR1= c Te mp 1999-2008 Cli mate Cate gory R1= p montane Cli mate Cate gory time Distributions 10/14/2010 02:24 PM 10/14/2010 02:24 PM -5 -4 -3p-21988-1998 -1 0 1 2 C 3 4 Me -10-9 -8De -7 De -6-4 -5-3 -4p-2 -3 -21999-2008 2 43C 4 Me -10-9 -8 -7 -6 -5 -1 0-1 10 21 3C -10-9 -8 -7 De -6 -5 -4 -3 -2 1999-2008 -1 0 1 2 3C4 cTem Me anMin c Te mp cTem 1988-1998 anMin c Te mp Data anMin Table=Climate Category R1=montane,Climate Category R1=montane Data Table=Climate Category R1=maritime,Climate Categ Distributions Distributions Cli mate Cate gory nd -10-9 -8 -7 -6 -5 -1 0-1 10 21 3 -10 -10-9 -8 -7 De -6R1= -5 -4lowla -3p-21988-1998 -1 0 1 2 C 3 4 Me -10-9 -8De -7 De -6-4 -5-3 -4p-2 -3 -21999-2008 Me anMin cTem Me anMin c Te mp anMin cTem 1988-1998 C2 43C 4 Me 10/14/2010 02:24 PM o o land -5 -4 -3 -2 -1 0 1 2 3Data 4 Table=Climate -10-9 -8 -7 -6 -4 -5 -3 -4 R1=low -3 -1 -2 -1 0 4 -10-9R1=low -10-9 -8 -7 -6Category -5 -2 0 land,Climate 1 21 32 43 Category -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 Montane + 1.2 C Distributions High elevation +2.0 C Cli mate Cate gory R1= lowla nd 10/14/2010 02:24 PM Me anMin cTem p -3 1988-1998 C Me anMin De c-6Te mp 1999-2008 C Cli mate Cate-8De gory -10-9 -7 -6 R1= -5 -4montane -2 -1 0 1 2 3Data 4 Table=Climate -10-9 -8 -6 -7Category -5 -3 -4 R1=low -3 -1 -2 0 -1land,Climate 4 -1 -10-9 -8 -7 -5 -4 -2 10 21 32 43 Catego =high elevation,Climate Category -10-9 -8 -7 R1=high -6 -5 -4 -3 -2 -1 0 1 2 3 4 Change in mean annual min Dec T (C) at -10 lichen plots, by climate zone, 1988-2008 Cli mate Cate gory R1= montane 988-1998 C Me anMin De c Te mp 1999-2008 C means for R2 High Elevation plots 10/14/2010 I998-2008 02:24 PM Data Table=Climate Category R1=montane,Climate Categ 1 0 1 2 3 4 Distributions Me anMin De cTem p 1988-1998 C -10-9 -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 Me a la nd -10-9 -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 =low land,Climate CategoryI988-1997 R1=lowmeans landfor R1 Montane Plots -10 What actually happened: PRISM temperatures 1988-2008 • Warming rates ↑ with elevation • Low elevations, valleys and the coast range did not warm • No sites became cooler What actually happened: Lichens 1993-97 vs. 2003-07 Lichen community based climate scores also showed greatest increases at highest elevations. Like temperature, lichen-indicated warming increased with elevation Climate change direction indicated by lichen communities (1993-2009) N Mean elevation (m) much warmer 5 813 warmer 34 705 no change detected 248 583 cooler 37 539 much cooler 12 470 What actually happened: Lichens But lichen-community based climate scores show cooling—where PRISM mean min Dec temps have not changed. What’s happening? But what actually happened? Poll? Coast Distance Axis 2: Climate Elev Continentality Longitude Lichen %N ? %RH Mean T Min Dec T Axis 1: Air Quality 0 1 Could shifts in other climate-axis variables be influencing lichen response? What actually happened: % RH 1988-2009 • Humidity ↓ in the high elevation Cascades • Humidity ↑ in the lower elevation Cascades & Coast Ranges Comparing climate & lichen responses Mean Min Dec Temp % Relative humidity • warmer temps • less humidity Lichen-based climate scores • warmer and less humid R2 climate scores were correlated with climate variables 10/5/2010 09:45 AM Data Table=MegaDB2 Fit Y by X Group Bivaria te Fit of Clim S core R2 By Ele v ft 2 1.5 1.5 0.5 0 -0.5 1. 1 • Data from Round 2 (2003-2009). • Low climate0.5scores → low elevations 0 with warm, humid climates, • High climate-0.5scores → high elevations -1 climates. with cool, dry, r2 adj = 0.72 -1 -9 -8 -7 -6 -5 -4 -3 -2 -1 0 1 2 3 4 5 0 MeanMin Dec Temp 1999-2008 C ClimBivaria S core R2 By of MeClim anMin De cR2 TeBy mpMe 1999-2008 C Bivaria te Fit of Clim S core R2 By Ele v ft te Fit S core an%RH 1999-2009 2 Linear Fit 2 Linear Fit 1 Summa ry of Fit RSquare 0.5 RSquare Adj Root 0 Mean Square Err or Mean of Response Obs -0.5 ervations (or Sum Wgts ) r2 adj = 0.23 0.722646 0.721731 0.264458 0.550792 305 Clim Scor eR2 Clim Scor eR2 1.5 1.5 Clim Scor eR2 = 0.2995646 - 0.1858041 MeanMin Dec Temp 1999- 2008 C 1 0.5 0 -0.5 Analysi s of V aria nce -1 Source 65 DF 70 Sum of Squares 80 Mean Square F Ratio 85 90 -6 -5 -4 -3 -2 -1 0 1 2 3 4 755 Model 1 55.213705 1999-2009 55.2137 789.4683 MeanMin Dec Temp 1999-2008 Mean%RH C Error 303 21.191165 0.0699 Prob > F C. Linear Total Fit 304 76.404869 <.0001 Linear Fitter Estim ates Pa rame Clim Scor eR2 = 3.8408658 - 0.0435131 Mean% RH 1999-2009 0. -0. - 1000 2000 3000 4000 5000 6000 7000 Elev ft Bivaria te Fit of Clim S cor 2 Linear Fit Linear Fit 1.5 Clim Scor eR2 = -0.129624 + 0.0002429 Elev ft Summa ry of Fit RSquare RSquare Adj Root Mean Square Err or Mean of Response Obs ervations (or Sum Wgts ) r2 adj = 0.66 0.662637 0.661679 0.289994 0.545156 354 Clim Scor eR2 1 Bivari Clim Scor eR2 2 Clim Scor eR2 Clim Scor eR2 Bivaria te Fit of Clim S core R2 By Me anMin De c Te mp 1999-2008 C 1 0.5 0 -0.5 Analysi s of V aria nce L Line Clim Su R R R M O An -1 -1 Source DF Sum of Squares Mean Square F Ratio S 0 1000 2000 3000 4000 5000 6000 7000 65 70 7 Model 1 58.143161 58.1432 691.3878 M Elev ft Mean%R Error 352 29.601899 0.0841 Prob > F E C. Total 353 87.745061 C Linear Fit Linear Fit<.0001 Linear Fit Pa rame ter Estim ates Linear Fit Pa What actually happened: α-Diversity Climate Score Shift Category R1 αR2 αΔ in αdiversity diversity diversity % Δ in αdiversity N much cooler 14 20 19 -1 -3 cooler 42 20 19 -1 -3 no change 270 22 26 4 18 warmer 38 19 24 5 27 much warmer 5 14 21 7 53 α-diversity = mean species richness per survey site N = number of sites Conclusions 1. The composition of epiphytic lichen communities are highly sensitive to climate and are used by FIA to indicate climate. 2. A preliminary analysis of 10-year trends in lichen community composition provides initial evidence of climate-driven effects on species composition & diversity of PNW lichens. 3. Since lichen monitoring began in 1993, mean min Dec temperatures have clearly increased in the mid and upper elevation Cascades, but not in the Coast Range, major river valleys or other low elevation sites. 4. Trends in lichen-community based climate scores are consistent with temperature trends data: species composition shifts indicate greatest warming effects at the highest elevations. Conclusions 5. ‘Cooler’ lichen-based climate scores in the Coast Range and low elevation Cascades, where temperature has not decreased, may be related to increases in relative humidity. 6. Both mean species richness at survey sites and landscape level diversity increased with warming temperatures and decreased with cooling temperatures. 7. With regard to other plant communities, these results imply that managers can expect different responses and different response rates across the landscape with differing directions and rates of change in climate variables. Acknowledgements We thank!— • Our many dedicated field biologists who tramped through the brush and surveyed lichens • The lichenologists who assisted with identifications, especially Jim Riley and Pekka Halonen. • Our office staff for digitizing our data, especially Anne Ingersoll and Larissa Lasselle • Our cooperators on the Gifford Pinchot, Mt. Hood, Willamette, Umpqua, and Siuslaw national forests and the Columbia River Gorge National Scenic Area who helped with logistics, field support, and funding • The USFS PNW Region Air Resource Management Program and USFS PNW Research Station/FIA Program for major funding and support of this work.
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