1 1 Supplemental Tables 2 Table S1. Sampled species and populations, sample sizes for adults in the wild and common 3 garden seedlings (J=Jonaskop garden, K=Kirstenbosch garden), locality name, latitude, 4 longitude, rainfall, and elevation. H.H. = Hottentots Hollands. EC =Eastern Cape. KZN=Kwa- 5 Zulu Natal. All localities excluding those marked EC or KZN are in the Western Cape Province. Sample Mean sizes, Elevation (mm/yr) (m) Species Pop. adult/J/K Locality name Latitude P. aurea DR 20/16/16 Doringrivier, Outeniqua -33.87775 22.31026 669 792 aurea LW 15/17/15 Langeberg-Wes, Robertson -33.74354 19.90748 440 646 MP 40/14/13 Marloth, Langeberg-Wes -33.99629 20.45651 882 239 RP 39/11/14 Robinson’s pass, Outeniqua -33.90872 22.02348 723 544 RV 20/9/10 Riviersonderend -34.06276 19.70707 473 584 P. aurea KP 17/11/12 Klipspringer, De Hoop -34.37912 20.58325 489 493 potbergensis PB 18/13/22 Potberg, De Hoop -34.42262 20.65524 420 228 P. lacticolor GW 15/16/15 Grabouw, H.H. -34.11947 18.97258 1218 618 LI 13/10/11 Limietberg, H.H. -33.69506 19.13143 880 1263 LK 19/12/13 Landroskop, H.H. -34.03944 18.99126 2069 1372 PK 40/15/16 Pofaddersnek, H.H. -34.01826 19.07807 1260 836 PO2 23/15/15 Purgatory outspan, H.H. -33.96764 19.14433 926 435 BS 18/5/4 Baviaanskloof, EC -33.60970 24.50043 458 809 KM 13/16/16 Kleinmond, Kogelberg -34.32715 19.00270 972 228 MS 20/12/16 Maanschynkop, Vogelgat -34.38826 19.35095 534 866 OB 15/9/16 Oudebos, Kogelberg -34.33402 18.93185 1089 403 TK 15/14/12 Tsitsikamma, EC -33.94140 24.18693 784 251 P. mundii Longitude rainfall 2 P. punctata BBP 13/2/8 Blesberg, Swartberg -33.41927 22.68854 255 1959 CB 12/3/7 Cederberg -32.51260 19.18215 414 1408 GB 27/3/3 Gydoberg, Ceres -33.25397 19.48446 394 1363 JK 18/0/0 Jonaskop, Riviersonderend -33.96950 19.50170 323 1396 KS 20/13/12 Kammanassieberg -33.64508 22.95381 444 1105 SPP 20/12/11 Swartberg pass -33.36256 22.06647 932 1208 P. hybrid TW 17/13/11 Towerkop, Klein Swartberg -33.44548 21.28841 348 975 P. subvestita SE 15/6/10 Somerset East, Bosberg, EC -32.69389 25.58685 543 1465 TD 20/7/10 Tor Doone, Hogsback, EC -32.58046 26.93345 1169 1536 MC 16/4/0 Maclear, Potrivier Pass, EC -30.92358 28.20812 905 1718 WZ 14/0/1 Near Weza, Kokstad, EC -30.54535 29.6563 852 1638 SA 36/1/2 Sani Pass, KZN -29.60925 29.36219 1063 1851 RN 35/0/0 Royal Natal, KZN -28.68338 28.9178 969 1833 BBV 12/2/6 Blesberg, Swartberg -33.41856 22.68702 255 2037 KSV 11/0/1 Kammanassieberg -33.64890 22.78194 419 1833 MJV 8/0/0 Swartberg pass -33.35318 22.05030 744 1522 SPV 17/1/2 Oliewenberg,Swartberg -33.34692 22.09973 796 1848 WB 17/2/5 Waboomsberg, Swartberg -33.35238 22.03304 679 1880 P. venusta 3 6 7 8 9 Table S2. Regression coefficients from multiple regressions on traits of plants measured in the wild and in the Kirstenbosch and Jonaskop common gardens. Inter-trait and trait-climate correlations in were tested in a multiple regression for each leaf trait (log transformed and standardized), with random effects of species and population. See Fig. 2A-C for diagrams of analyses for wild adults and common gardens seedlings. Numerator degrees of freedom = 1 for all. *** = p<0.01, ** = p ≤ 0.05, * = p < 0.1 Regression coefficients for each predictor (denominator degrees of freedom) Location Responses Wild (2008-2009) SLA Kirstenbosch (Jan 2009) Jonaskop (Jan 2009) SLA - LWR Leaf area Stomatal d. DRYPCA COLDPCA PPTCON FERTPCA -0.019 (665) 0.113** (494) -0.0505 (664) 0.249** (30) 0.220** (31) 0.074 (30) 0.086 (31) -0.386*** (630) -0.104** (674) -0.015 (27) 0.208 (29) -0.199 (32) -0.173* (28) LWR -0.023 (676) Leaf area 0.050** (674) -0.150*** (668) - -0.0618** (673) 0.152** (23) 0.053 (24) 0.397*** (26) 0.089 (25) Stomatal density -0.049 (668) -0.094** (657) -0.138** (612) - -0.167** (26) 0.087 (28) 0.182 (23) 0.065 (30) - -0.002 (295) -0.369*** (303) 0.259*** (309) 0.265** (18) 0.238* (24) -0.101 (28) -0.019 (18) LWR -0.003 (309) - 0.161*** (316) 0.0599 (298) -0.106 (15) 0.375** (18) -0.360** (21) -0.069 (17) Leaf area -0.240*** (304) 0.127** (310) - -0.131*** (303) 0.312** (16) 0.340* (24) 0.384** (19) 0.071 (24) Stomatal density 0.226*** (277) 0.073 (147) -0.226*** (218) - 0.027 (25) -0.159* (34) 0.245** (20) -0.052 (25) - -0.036 (276) -0.258*** (270) 0.095* (261) 0.040 (15) 0.283** (21) -0.271* (25) -0.017 (16) LWR -0.039 (276) - -0.089 (272) -0.0004 (266) -0.021 (21) 0.388*** (29) -0.122 (35) -0.113 (23) Leaf area -0.154*** (275) -0.045 (273) - -0.147*** (262) 0.260** (14) 0.308** (25) 0.316** (27) 0.111 (19) Stomatal density 0.067 (184) 0.022 (113) -0.295*** (123) - -0.058 (17) -0.020 (38) 0.206*** (20) -0.066 (22) SLA SLA - 4 10 11 Supplemental Appendices 12 APPENDIX 1 (A1) 13 The climate layers used in our study were extracted from the widely used and recently updated 14 South African Atlas of Agrohydrology and Climatology (Schulze 2007). Our focal layers were 15 interpolated from long-term records of daily rainfall and temperature from thousands of weather 16 stations throughout southern Africa. Data were available at a resolution of approximately 1.55 by 17 1.85 km, or 1 by 1 minute. We extracted site-specific climate data for each sampled population, 18 and from these, we created three focal climate axes. The first axis (PPTCON) reflects the 19 percentage of total annual rainfall that falls during a single month. PPTCON was taken directly 20 from Schulze, and it was calculated from monthly rainfall data using Markham’s technique (see 21 Schulze 2007 for additional details). 22 The second axis (COLDPCA) serves as an index of winter cold stress, reflecting 23 limitations on growth during the winter and the severity of cold stress. COLDPCA is the first 24 axis of a PCA on two climate layers from Schulze (2007), TMINAV07C and HU10_WINC. 25 This PCA explains 89% of the variation in the two layers, and the loading for each climate layer 26 is 0.7. TMINAV07C is the average daily minimum temperature in the coldest winter month 27 (July). HU10_WINC is the number of heat units during the winter months. Winter heat units are 28 calculated as the number of degrees by which daily maximum temperature exceeded 10° C, 29 summed across the winter months. COLDPCA is strongly positively correlated with elevation 30 and the number of days above 0 C⁰, and it is negatively correlated with summertime 31 temperatures (see also Discussion). 32 33 The third axis (DRYPCA) serves as an index of the duration and severity of drought during the dry season. This axis was created from two sets of monthly rainfall layers, which were 5 34 each combined into a single variable and then used in a PCA. DRYPCA is the first axis, 35 explaining 79% of variation, and again, each layer has a loading of 0.7. The first set of layers 36 was GMEDNRFL1-12, or the average median rainfall for each month. From these 12 layers, we 37 selected the driest 3 per site, and summed them. The second set of layers was RFLGE2MM, or 38 monthly averages of the number of days to receive fewer than 2 mm rainfall. We summed these 39 data for the driest 3 months per site as an estimate of the duration drought during the dry season. 40 Analysis of all of the above climate variables in a single PCA showed that the first three 41 components accounted for 93% of the variance. The first principal component (66% of the 42 variance) contrasted PPTCON against drought variables and winter temperatures. The second 43 principal component (17% of the variance) contrasted drought variables against winter 44 temperatures and PPTCON. The third principal component (10% of the variance) contrasted 45 winter temperatures against drought variables and PPTCON. In other words, each of the first 46 three components contrasted one set of climate variables with the other two. Hence we focus on 47 separate PCAs that individually describe each of those climate variables, making the results 48 easier to interpret. 49 50 51 52 53 54 55 56 57 6 58 APPENDIX 2 (A2) 59 To understand how local selection gradients are related to local environments, we performed a 60 hierarchical regression in which local selection gradients and their relationship to environmental 61 covariates were estimated in a single Bayesian model. We standardized the data within each 62 population prior to analysis (mean fitness equal to 1; mean of each trait equal to 0 and standard 63 deviation of each trait equal to 1). Thus, we were estimating standardized selection differentials 64 (Lande and Arnold 1983) separately within each population. Specifically, if wi is the fitness of 65 the ith individual in our sample, we assume that 2 w i N( i , pop[i] ) 66 i 0, pop[i] area, pop[i]area i SLA, pop[i]SLA i LW R, pop[i]LWR i dens, pop[i]dens i 67 where 0, pop[i] is the intercept, the , pop[i] are the local selection gradients for each trait, and 68 2pop[i] is the error variance associated with the multiple regression of fitness on traits within each 69 70 71 population. To examine the relationship between local selection gradients and environmental covariates we further assume that each of the , pop[i] is described by a regression on those covariates. Specifically, 2 area, pop[i] N( area, pop[i], area ) 2 SLA, pop[i] N(SLA, pop[i], SLA ) 72 2 LW R, pop[i] N( LW R, pop[i], LW R) 2 dens, pop[i] N(dens, pop[i], dens ) 7 73 area, pop[i] 0,area[sp[i]] area,PPTCON PPTCON pop[i] area,DRYPCADRYPCA pop[i] area,COLDPCA COLDPCA pop[i] area,FERTPCAFERTPCA pop[i] SLA, pop[i] 0,SLA[sp[i]] SLA,PPTCONPPTCON pop[i] SLA,DRYPCADRYPCA pop[i] 74 SLA,COLDPCA COLDPCA pop[i] SLA,FERTPCAFERTPCA pop[i] LW R, pop[i] 0,LW R[sp[i]] LW R,PPTCON PPTCON pop[i] LW R,DRYPCADRYPCA pop[i] LW R,COLDPCA COLDPCA pop[i] LW R,FERTPCAFERTPCA pop[i] dens, pop[i] 0,dens[sp[i]] dens,PPTCON PPTCON pop[i] dens,DRYPCADRYPCA pop[i] dens,COLDPCA COLDPCA pop[i] dens,FERTPCAFERTPCA pop[i] 75 76 where the 0, are the intercepts, the ,env are the regression coefficients of local selection 77 gradients for each trait on environmental covariates, and the 2 are the error variances of each 78 regression. We complete the Bayesian model by specifying vague normal priors on the 0, and 79 the ,env (mean = 0, s.d. = 1) and uniform priors (0, max.sd) on the standard deviation for 80 variance parameters (Gelman et al. 2004). The upper bound (max.sd) for the uniform distribution 81 on the standard deviation was chosen as 4 times the observed maximum within population 82 standard deviation for fitness (max.sd = 6.35 for the analysis with fitness as seed heads, max.sd = 83 9.87 for the analysis with fitness as total fecundity). The code and data used in the Bayesian 84 selection analysis are available through Kent Holsinger’s website (http://darwin.eeb.uconn.edu/). 85 8 86 APPENDIX 3 (A3) 87 To calculate standardized selection gradients and differentials within each garden, first we 88 standardized all trait variables to a mean of 0 and a standard deviation of 1. We then analyzed 89 trait-survival associations in a multiple logistic regression on a binary response. Because we used 90 a logistic regression, the standardized regression coefficient we obtained for each trait was not 91 directly comparable to a standardized selection gradient as originally defined by Lande and 92 Arnold (1983). A Lande-Arnold coefficient corresponds to the change in trait value given that 93 all other traits are at the mean, whereas the logistic coefficient corresponds to the change in log 94 odds of survival –i.e., log(p/(1-p))– for a unit change in that trait, again with all other traits held 95 at their mean. To convert the logistic coefficients into standardized selection gradients, we use a 96 method similar to the one originally proposed by Janzen and Stern (1998). We also converted 97 standardized selection differentials, which correspond to the observed change in the trait value. 98 Details on our models and conversions are as follows: 99 The multiple logistic regression focused on the four traits (SLA, LWR, leaf area, and 100 stomatal density), but we included home environment characteristics (PPTCON, DRYPCA, 101 COLDPCA, FERTPCA) as covariates and population nested within species to control for 102 unmeasured among-population differences that might bias the estimates. In short, the multiple 103 logistic model is given by 9 104 p log i 0 SLA SLAi LW RLWRi areaareai densdensi 1 pi PPTCON PPTCON pop[i ] DRYPCADRYPCA pop[i ] COLDPCACOLDPCApop[i ] FERTPCAFERTPCApop[i ] pop[i ] sp[i ] i 105 We illustrate the calculations by focusing on the relationship between SLA and the 106 corresponding selection gradient and selection differential. The selection gradient for SLA, bSLA, 107 is given by b SLA 108 1 SLAi pˆ i N i pˆ log i ˆ0 ˆSLA SLAi ˆPPTCON PPTCON pop[i ] ˆDRYPCADRYPCA pop[i ] 1 pˆ i ˆCOLDPCACOLDPCApop[i ] ˆFERTPCAFERTPCApop[i ] ˆ pop[i ] ˆsp[i ] 109 where hats refer to estimates derived from fitting the multiple logistic regression model. 110 Coefficients for LWR, leaf area, and stomatal density are not included in the gradient 111 calculation, because the corresponding means are zero as a result of standardizing the data prior 112 to analysis. The selection differential is calculated using a similar approach. pˆ i is calculated 113 using all trait covariates for each individual and used to obtain a mean trait value after selection, 114 x after 115 the mean trait value before any individuals have died. 1 SLAi pˆ i , and the selection differential is calculated as x after x before , where x before is N i 116 117 Literature cited for appendices: 118 Gelman, A., J. B. Carlin, H. S. Stern, and D. B. Rubin. 2004. Bayesian Data Analysis, 2nd ed. 119 Chapman & Hall, Boca Raton, FL. 10 120 121 122 123 124 125 Janzen, F. J., and H. S. Stern. 1998. Logistic regression for empirical studies of multivariate selection. Evolution 52:1564-1571. Lande, R., and S. J. Arnold. 1983. The measurement of selection on correlated characters. Evolution 37:1210-1226. Schulze, R. E. 2007. South African atlas of climatology and agrohydrology: WRC Report 1489/1/06. Water Research Commission, Pretoria, RSA.