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anches dead <strong>or</strong> dying with b<strong>or</strong>er-related bark ridges obvious on the bark surface; 2 = m<strong>or</strong>e than half of the crown branches<br />
dead <strong>or</strong> dying with bark ridges obvious and b<strong>or</strong>er exit holes often present; and 3 = tree dead, usually with b<strong>or</strong>er-related bark<br />
ridges and exit holes present. Bark ridges (callus tissue) occur on branch and trunk sections in response to larval feeding<br />
(Anderson 1944, Barter 1957, Wilson and Haack 1990, Herms 1991). The presence of b<strong>or</strong>er-related bark ridges was sc<strong>or</strong>ed<br />
in years 12 and 15. Completion of larval development was also sc<strong>or</strong>ed in years 12 and 15 by noting the presence of b<strong>or</strong>er exil<br />
holes. Tree survival was computed f<strong>or</strong> each of the 218 families in years 2, 6, 8, 10, 12, 15, and 16.<br />
Hist<strong>or</strong>ical temperature data were obtained from the Michigan Department of Agriculture, Climatological Division<br />
(MDA 1974). Average annual mean temperature was considered the most relevant climatic variable to use when considering<br />
global warming. The average annual mean temperature assigned to each seed source was obtained from a map showing<br />
annual mean temperatures f<strong>or</strong> Michigan averaged over the 30-year period 1940-1969 (Fig. 1, Table 1, MDA 1974). This was<br />
done by locating all seed collection sites on the map and then assigning a particular annual mean temperature value to each<br />
seed source based on its location relative to the map isotherms. Although actual temperature data f<strong>or</strong> each of the 26 collections<br />
sites would have been preferred, <strong>this</strong> was not possible because many collection sites had no nearby weather stations.<br />
Additional climatic data f<strong>or</strong> each of the 26 collection sites were obtained in similar fashion from other maps (Table 1).<br />
Using the map shown in Figure 1, the annual mean temperature values assigned to the 218 seed sources ranged from<br />
40° to 47°F (4.4*-8.3°C; Table 1). Actual average annual mean temperature values from several official weather stations f<strong>or</strong><br />
<strong>this</strong> same area and time period ranged from 39.7* to 47.1"F (4.30-8.4"C; MDA 1971). The average annual mean temperature<br />
of the plantation site was about 49.00F (9.4°C; MDA 1971). Overall, assuming that the birch seed sources were genetically<br />
acclimated to the average annual mean temperature of their <strong>or</strong>iginal sites, then the birch trees growing at the plantation site<br />
were the<strong>or</strong>etically experiencing levels of climatic warming equivalent to 1.9° to 9.3*F (1.1 ° to 5.2°C; Table 2). F<strong>or</strong> ease of<br />
discussion, I will use the term climatic differential (CD) to represent the difference (in °C) between the average annual mean<br />
temperatures of the seedlot <strong>or</strong>igin and the plantation site.<br />
Table 2.--Average annual mean temperature data and percent of paper birch trees (both live and dead) that had bronze<br />
birch b<strong>or</strong>er-induced ridges and/<strong>or</strong> b<strong>or</strong>er exit holes along their lower trunk in years 12 (1987) and 15 (1990) postestablishment<br />
by climatic differential treatment.<br />
Mean temperature<br />
difference between<br />
C<strong>or</strong>responding <strong>or</strong>igin and Percent of trees with Percent of trees with<br />
isotherms 2 plantation site 3 b<strong>or</strong>er-induced ridges 4 b<strong>or</strong>er exit holes 4<br />
CD j °F °C *F °C Yr 12 Yr 15 Yr 12 Yr 15<br />
CD t ° 46, 47 7.7, 8.3 2 1.1 30ab 32b 10b 13b<br />
CD2 ° 44, 45 6.7, 7.2 4 2.2 24b 33b 8b 18b<br />
CD3 ° 42, 43 5.6, 6.1 6 3.3 39ab 46b 12b 25b<br />
CD4 ° 40, 41 4.4, 5.0 8 4.4 50a 60a 23a 40a<br />
CD = Climatic differential, which is a term that reflects the difference between the average annual mean temperature<br />
of the seed sources within a particular treatment group and the average annual mean temperature of the plantation<br />
site, which was 49°F (9.4"C). The value 1° in CD1 °, f<strong>or</strong> example, reflects the annual mean temperature difference<br />
between the <strong>or</strong>igin and the plantation site, e.g., 1.I*C (see footnote 3 below).<br />
2The isotherms of average annual mean temperature in *F (and the approximate °C equivalent), as given in Fig. 1,<br />
that c<strong>or</strong>respond to each CD grouping.<br />
3F<strong>or</strong> each CD grouping, the mean temperature difference between the <strong>or</strong>igin and the plantation site was calculated<br />
as follows. F<strong>or</strong> CDI*, the c<strong>or</strong>responding isotherms were 46* and 47°F. However, these isotherms span the temperature<br />
range from 46* to 47.9°F, with a mean of about 47"E Thus, the temperature difference between the <strong>or</strong>igin and the :<br />
plantation site in <strong>this</strong> case is 2*F (49°-47 *) <strong>or</strong> about 1.I*C. These values represent the the<strong>or</strong>etical level of climatic<br />
warming that the c<strong>or</strong>responding trees were experiencing while growing at the plantation site in southern Michigan.<br />
4 Percent of trees with b<strong>or</strong>er-induced ridges and/<strong>or</strong> b<strong>or</strong>er exit holes along the lower trunk; percent values followed by<br />
the same letter within a column are not significantly different<br />
followed by the Dunn's test f<strong>or</strong> multiple comparisons).<br />
238<br />
(p