Extreme resistance to desiccation and microclimate-related differences in cold-hardiness of gall wasps (Hymenoptera: Cynipidae) overwintering on roses in southern Canada
Jason B. Williams1,*,
Joseph D. Shorthouse2 and
Richard E. Lee, Jr1
1 Department of Zoology, Miami University, Oxford, OH 45056, USA
2 Department of Biology, Laurentian University, Sudbury, Ontario, Canada P3E
2C6

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Fig. 1. Weekly mean temperatures from September to May 1999-2000 (A) and daily
minimum temperatures from 30 December to 26 February 1999-2000 (B) near
Sudbury, Ontario, Canada. Snow cover indicates continuous days of at least 10
cm of snowpack, the period represented in B. Subnivean temperatures were
recorded at the ground surface while supranivean temperatures were recorded 25
cm above the ground.
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Fig. 2. Supercooling point (A), glycerol concentration (B), rate of water loss (C)
and body water content (D) for Diplolepis spinosa, D. gracilis and
D. radicum prepupae during winter acclimation at 5 °C. Data
points that have, but do not share, letters are significantly different.
Values are means ± S.E.M. (N=8). Some S.E.M. are within the
size of the symbol.
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Fig. 3. Supercooling point (mean ± S.E.M., N=8) for cynipid
prepupae overwintering in supranivean and subnivean galls. S.E.M. values for
D. gracilis are within the symbol.
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Fig. 4. Total hemolymph osmolality and the glycerol component of total osmolality
for the six cynipid species examined under midwinter conditions. Values are
means ± S.E.M. (N=5-8).
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Fig. 5. Effects of temperature on water permeability for prepupae of Diplolepis
spinosa collected at Medicine Hat, Alberta, Canada. The transition
temperature for this species was 33.5 °C. The equation for the regression
line below the transition temperature is y=0.028x+0.18
(r2=0.99), where y is cuticular permeability
(µg h-1 cm-2 mmHg-1) and x is
temperature (°C), and the equation for the regression line above the
transition temperature is y=0.426x-13.08
(r2=0.91). Values are means ± S.E.M.
(N=5-8).
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© The Company of Biologists Ltd 2002