1 Supplementary materials 2 Plant community composition regulates the responses of Prairie soil respiration to 3 experimental warming 4 Xia Xu, Zheng Shi, Dejun Li, Xuhui Zhou, Rebecca A. Sherry, Yiqi Luo 5 1 6 Supplementary references 7 McCune B, Grace JB (2002) Analysis of Ecological Communities. MjM Software Design, 8 9 10 Gleneden Beach, OR, USA. Palmer MW (1993) Putting things in even better order: the advantages of canonical correspondence analysis. Ecology, 74, 2215-2230. 2 11 12 Supplementary Table S1 For Tsoil and Wsoil, values are mean SE. Variable Treatment 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 1007 863 833 647 966 515 744 1307 726 1017 906 549 678 UC 17.90.5 19.40.5 16.40.4 17.10.4 16.70.4 16.90.4 17.30.4 16.80.4 16.10.4 16.70.4 16.60.5 18.90.5 19.80.5 UW 20.00.5 19.10.5 17.80.4 18.50.4 18.40.4 19.00.4 19.50.4 18.20.4 17.20.4 17.30.4 17.90.5 20.20.5 21.10.5 CC 18.80.5 17.9.0.5 16.70.4 17.20.4 17.00.4 17.50.4 17.90.4 17.10.4 16.00.4 17.00.4 16.70.4 20.10.5 21.00.5 CW 21.30.5 20.50.5 18.00.4 19.20.4 19.00.4 20.20.4 20.60.4 19.50.4 18.20.4 19.60.4 19.10.5 22.20.5 23.10.5 UC 22.91.2 29.80.7 27.30.9 22.00.7 27.60.7 24.81.1 23.50.9 29.90.4 27.00.8 26.62.88 30.32.6 22.01.8 19.42.1 UW 19.20.8 28.80.3 26.51.1 21.00.5 27.50.4 21.70.7 22.00.5 28.70.5 25.20.7 24.63.2 28.73.1 21.41.6 18.22.2 CC 21.61.0 28.80.7 27.11.1 22.30.8 27.50.7 24.10.8 23.10.7 29.70.4 26.10.6 26.02.8 29.82.7 21.71.4 18.92.1 CW 17.40.8 28.40.3 26.31.0 20.20.7 26.30.6 20.90.8 20.90.6 28.60.4 24.40.6 24.02.9 28.03.0 21.31.9 18.32.6 AP (mm) Tsoil (°C) Wsoil (%) 13 Annual precipitation (AP), soil temperature and moisture (Tsoil, Wsoil) under different treatments at the experimental site. Note: UC: unclipped control temperature; UW: unclipped and warming; CC: clipped and control temperature; CW: clipped and warming. 3 Supplementary figure legends Figure S1 Variation in ANPP under the four treatments (A-B) and warming-induced changes in ANPP (C-D) and C4 grasses (E-F) from 2000 to 2012. ANPP: aboveground net primary production. Values are mean ± SE with 6 replicates. Fig. S2 Variation in ANPP contributed by C3 forbs under the four treatments (A-B) and warming-induced changes in C3 forbs (C-D) from 2000 to 2012. In 2000, 2001, and 2002, the biomass C3 forbs is obtained based on the correlation between C3/C4 cover ratio and C3 biomass in clipped subplots each year (all P<0.01, n=12) because we did not separate ANPP into C3 forbs and C4 grasses when measuring ANPP during those years. C4 biomass is calculated as the difference between ANPP and C3 (Xu et al., 2012b). Values are mean ± SE with 6 replicates. Figure S3 Variation in BNPP under the four treatments (A-B), the absolute (C-D) and the relative (E-F) warming-induced changes in BNPP from 2000 to 2012. BNPP: belowground net primary production. Values are mean ± SE with 6 replicates. Figure S4 Seasonal variation in soil respiration under the four treatments (A-B) and warming-induced changes in soil respiration (C) from 2000 to 2012. Monthly data are used in this figure and values are mean ± SE with 6 replicates. Figure S5 Relationships of warming-induced changes in annual soil respiration with warming-induced changes in soil temperature (A) and soil moisture (B) from 2000 to 2012. The abnormal point (smaller than 0 based on the X-axis) shown in panel A is from the unclipped subplot in 2001, which probably resulted from measurement errors. The relationship in panel A is not statistically significant (P>0.05) even with removal of the abnormal point. Yearly data are 4 used in this figure. Figure S6 Warming-induced changes in soil respiration negatively affected by the proportion of ANPP contributed by C4 grasses across the 13 years. Yearly data are used in this figure. Figure S7 Negative impact of the proportion of ANPP contributed by C4 grasses on aboveground net primary production (ANPP, A) and belowground net primary production (BNPP, B) under warming. Yearly data are used in this figure. Figure S8 Effects of warming and clipping on plant community structure. Blocked canonical correspondence analysis (CCA) ordination showed similar community structure in the control and warmed plots in 2000-2004 (A) but different structure in 2005-2012 (B). Canonical correspondence analysis (CCA) is a multivariate ordination technique with constraints added from a matrix of environmental variables (McCune & Grace, 2002). All ordination techniques attempt to order or cluster data characterized by multiple variables by collapsing multiple variables into a few axis. Canonical ordination techniques limit the structure the ordinations can take on based on environmental variables. CCA maximizes differences that correlate to the measured environmental variables (and may ignore differences in community structure that are unrelated to the environmental variables). For an experimental design with only 2 levels of each environmental factor (such as this experiment), dummy variables (i.e. 0 or 1) can be used in the environmental matrix. CCA assumes a hump-shaped distribution of species responses (unlike principle component analysis (PCA) and redundancy analysis (RDA) which assume linear responses). CCA performs well with skewed distributions, correlated environmental variables, and missing factors (Palmer, 1993). Yearly data are used in the CCA 5 Year Fig. S1 6 20 20 12 10 08 UW-UC 20 0 -1 (d) 06 100 (c) 20 200 UC (b) UW 04 300 (a) 20 02 00 (e) C4-ANPP 20 20 12 10 08 06 -2 ANPP (g m yr ) 400 20 20 20 20 04 02 00 -1 120 20 20 20 -2 Warming-induced chages in ANPP (g m yr ) 500 CC CW CW-CC 80 40 0 (f) C4-ANPP 120 80 40 0 Year Fig. S2 7 12 (b) 20 10 08 06 04 UW-UC 20 20 20 20 (c) 02 00 UC UW 20 20 -1 (a) 12 10 08 06 04 -2 C3-ANPP (g m yr ) 150 20 20 20 20 20 02 00 0 80 20 20 Warming-induced chages -2 -1 in C3-ANPP (g m yr ) 180 CC CW 120 90 60 30 (d) 40 0 -40 -80 CW-CC Year Fig. S3 8 20 20 12 10 08 UW-UC 20 -1 (d) 06 0 (c) 20 200 UC (b) UW 04 400 (a) 20 02 00 (e) 20 20 12 10 08 06 -2 600 20 20 20 20 04 -1 350 20 02 00 0 120 20 20 -2 Warming-induced changes in BNPP (g m yr , C, D) and (%, E, F) BNPP (g m yr ) 800 CC CW CW-CC 280 210 140 70 (f) 90 60 30 0 -2 -1 Rs (umol m s ) 9 (a) UC UW 6 3 0 CC CW 6 -2 -1 Rs (umol m s ) (b) 4 2 Warming-induced -2 -1 changes in Rs (umol m s ) 0 3 (c) UW-UC CW-CC 2 1 0 -1 20 00 20 01 20 02 20 03 20 04 20 05 20 06 20 07 Year Fig. S4 9 20 08 20 09 20 10 20 11 20 12 20 13 Warming-induced -2 -1 increases in R s (gC m y ) 350 (a) (b) 280 210 140 70 0 0 1 2 3 -4 -3 o -2 -1 Warming-induced changes in Tsoil ( C, A) and Wsoil (%, B) Fig. S5 10 0 Warming-induced -2 -1 increases in Rs (gC m y ) 450 y=-6.65x+155.19 2 r =0.24, P=0.017 360 270 180 90 0 -10 -5 0 5 10 Warming-induced changes in the proportion of ANPP from C4 grasses (%) Fig. S6 11 160 y=-2.94x+58.69 2 r =0.20, P=0.023 (a) Warming-induced changes in -2 -1 ANPP (A) and BNPP (B) (g m y ) 120 80 40 0 (b) 300 200 100 0 -100 -10 y=-5.57x+123.68 2 r =0.14, P=0.057 -5 0 5 10 Warming-induced changes in the proportion of ANPP from C 4 grasses (%) Fig. S7 12 UC UW CC CW 0.2 0.0 -0.4 0.4 0.0 -0.4 0.8 0.4 0.0 -0.8 2005-2012 -0.4 0.4 0.0 -0.8 -0.4 -0.8 Axis2 0.8 0.4 0.0 2000-2004 -0.4 0.0 -0.8 -0.3 -0.6 Axis2 Ax is1 -0.2 Ax is1 Axis3 0.4 (b) Axis3 (a) Fig. S8 13