| Literature DB >> 32551058 |
Maria Adelena Tonione1, So Mi Cho1,2, Gary Richmond1,3, Christian Irian1, Neil Durie Tsutsui1.
Abstract
Thermal phenotypic plasticity, otherwise known as acclimation, plays an essential role in how organisms respond to short-term temperature changes. Plasticity buffers the impact of harmful temperature changes; therefore, understanding variation in plasticity in natural populations is crucial for understanding how species will respond to the changing climate. However, very few studies have examined patterns of phenotypic plasticity among populations, especially among ant populations. Considering that this intraspecies variation can provide insight into adaptive variation in populations, the goal of this study was to quantify the short-term acclimation ability and thermal tolerance of several populations of the winter ant, Prenolepis imparis. We tested for correlations between thermal plasticity and thermal tolerance, elevation, and body size. We characterized the thermal environment both above and below ground for several populations distributed across different elevations within California, USA. In addition, we measured the short-term acclimation ability and thermal tolerance of those populations. To measure thermal tolerance, we used chill-coma recovery time (CCRT) and knockdown time as indicators of cold and heat tolerance, respectively. Short-term phenotypic plasticity was assessed by calculating acclimation capacity using CCRT and knockdown time after exposure to both high and low temperatures. We found that several populations displayed different chill-coma recovery times and a few displayed different heat knockdown times, and that the acclimation capacities of cold and heat tolerance differed among most populations. The high-elevation populations displayed increased tolerance to the cold (faster CCRT) and greater plasticity. For high-temperature tolerance, we found heat tolerance was not associated with altitude; instead, greater tolerance to the heat was correlated with increased plasticity at higher temperatures. These current findings provide insight into thermal adaptation and factors that contribute to phenotypic diversity by revealing physiological variance among populations.Entities:
Keywords: adaptation; chill‐coma recovery; climate change; knockdown time; phenotypic plasticity; thermal tolerance
Year: 2020 PMID: 32551058 PMCID: PMC7297759 DOI: 10.1002/ece3.6229
Source DB: PubMed Journal: Ecol Evol ISSN: 2045-7758 Impact factor: 2.912
FIGURE 1Map of California with sampled localities. Localities colored according to elevation
For each locality, altitude (m), GPS coordinates, mean mass, chill‐coma recovery times (CCRT ± SE), and knockdown times (±SE) after a 10°C and 27°C acclimation are reported
| Population | Longitude | Latitude | Alt (m) | Mass | Mean CCRT | Mean knockdown | ||||
|---|---|---|---|---|---|---|---|---|---|---|
| 10°C | 27°C | Acclimation capacity | 10°C | 27°C | Acclimation capacity | |||||
| Berkeley | −122.26317 | 37.87281 | 71 | 1.00 | 174 ± 9 | 744 ± 36 | 570 | 41 ± 5 | 87 ± 11 | 46 |
| Whittier | −118.05395 | 34.00381 | 100 | 0.78 | 180 ± 9 | 768 ± 38 | 588 | 60 ± 7 | 127 ± 15 | 67 |
| Stebbins | −122.09678 | 38.50867 | 109 | 0.90 | 189 ± 9 | 807 ± 39 | 618 | 50 ± 6 | 106 ± 13 | 56 |
| Quail Ridge | −122.14895 | 38.48307 | 388 | 0.88 | 149 ± 7 | 636 ± 30 | 487 | 46 ± 6 | 98 ± 12 | 52 |
| Castle Rock | −122.09495 | 37.22829 | 973 | 0.82 | 137 ± 6 | 583 ± 28 | 446 | 47 ± 6 | 101 ± 12 | 54 |
| Mt Diablo | −121.916667 | 37.219167 | 1,130 | 0.83 | 144 ± 7 | 616 ± 29 | 472 | 48 ± 6 | 102 ± 13 | 54 |
| Yosemite | −119.58584 | 37.74763 | 1,233 | 1.28 | 143 ± 10 | 612 ± 39 | 469 | 85 ± 11 | 182 ± 22 | 97 |
| Palomar | −116.92146 | 33.34078 | 1,442 | 0.95 | 145 ± 7 | 619 ± 32 | 474 | 46 ± 6 | 99 ± 12 | 53 |
Units for CCRT and knockdown are reported in seconds as calculated from predicted means. Acclimation capacity is also reported across the different populations.
Indicates mean dry weight of individuals tested.
Acclimation temperature.
FIGURE 2Monthly mean temperatures (±SE) both above ground (solid lines) and 60 cm below ground (dashed lines). (a) Berkeley, (b) Whittier, (c) Stebbins, (d) Quail Ridge, (e) Castle Rock, (f) Mt. Diablo, (g) Yosemite, and (h) Palomar Mtn
FIGURE 3Chill‐coma recovery time for populations of Prenolepis imparis. (a) Chill‐coma recovery times after acclimation to 10°C and (b) chill‐coma recovery times after acclimation to 27°C. Individuals were pooled and represented by single lines colored according to population of origin
Post hoc contrasts within and between populations of Prenolepis imparis chill‐coma recovery time after acclimation to 10°C (low acclimation) and 27°C (high acclimation)
| Comparison | Fixed factor | β ± |
|
|
|---|---|---|---|---|
| Whittier–Quail Ridge | Low acclimation | 0.44 ± 0.09 | 4.87 | <.0001 |
| Whittier–Castle Rock | Low acclimation | 0.38 ± 0.09 | 4.24 | <.001 |
| Whittier–Mt Diablo | Low acclimation | 0.42 ± 0.09 | 4.70 | <.0001 |
| Whittier–Yosemite | Low acclimation | 0.49 ± 0.13 | 3.62 | .0246 |
| Stebbins–Quail Ridge | Low acclimation | 0.38 ± 0.09 | 4.24 | <.001 |
| Stebbins–Castle Rock | Low acclimation | 0.32 ± 0.09 | 3.59 | .029 |
| Stebbins–Mt Diablo | Low acclimation | 0.36 ± 0.09 | 4.08 | <.01 |
| Berkeley–Palomar | High acclimation | 0.46 ± 0.09 | 5.25 | <.0001 |
| Whittier–Palomar | High acclimation | 0.37 ± 0.09 | 4.16 | <.001 |
| Stebbins–Castle Rock | High acclimation | 0.35 ± 0.09 | 3.88 | <.001 |
| Stebbins–Palomar | High acclimation | 0.54 ± 0.09 | 6.10 | <.0001 |
| Quail Ridge–Palomar | High acclimation | 0.39 ± 0.09 | 4.46 | <.001 |
| Mt Diablo–Palomar | High acclimation | 0.32 ± 0.09 | 3.66 | .023 |
| Berkeley | Low/high acclimation | −1.52 ± 0.09 | −17.03 | <.0001 |
| Whittier | Low/high acclimation | −1.23 ± 0.09 | −13.86 | <.0001 |
| Stebbins | Low/high acclimation | −1.47 ± 0.09 | −16.22 | <.0001 |
| Quail Ridge | Low/high acclimation | −1.70 ± 0.09 | −19.55 | <.0001 |
| Castle Rock | Low/high acclimation | −1.45 ± 0.09 | −16.43 | <.0001 |
| Mt Diablo | Low/high acclimation | −1.61 ± 0.09 | −18.47 | <.0001 |
| Yosemite | Low/high acclimation | −1.68 ± 0.14 | −12.29 | <.0001 |
| Palomar | Low/high acclimation | −1.04 ± 0.09 | −11.89 | <.0001 |
Population and acclimation temperature were included as fixed factors, the replicates were included as random factors and differences are given as β ± SE standard error. Only pairs that were significantly different are shown.
FIGURE 4Modeled thermal tolerance after a high‐temperature acclimation (s) in relation to modeled low‐temperature acclimation (s), altitude (m), mass (mg), and acclimation capacity (s). (a) Chill‐coma recovery time (CCRT) after 27°C acclimation with respect to CCRT after 10°C acclimation. (b) CCRT with respect to altitude. (c) CCRT with respect to mass. (d) CCRT with respect to acclimation capacity. (e) Knockdown after 27°C acclimation with respect to knockdown after 10°C acclimation. (f) Knockdown time with respect to altitude. (g) Knockdown time with respect to mass. (h) Knockdown time with respect to acclimation capacity
FIGURE 5Knockdown for populations of Prenolepis imparis. (a) Knockdown times after acclimation to 10°C and (b) knockdown times after acclimation to 27°C. Individual knockdown times were pooled and colored according to population of origin
Post hoc contrasts within and between populations of Prenolepis imparis knockdown time after acclimation to 10°C (low acclimation) and 27°C (high acclimation)
| Comparison | Fixed factor |
|
|
|
|---|---|---|---|---|
| Berkeley–Whittier | Low acclimation | −0.72 ± 0.21 | −3.46 | .04 |
| Berkeley–Yosemite | Low acclimation | −0.83 ± 0.21 | −3.94 | <.001 |
| Berkeley–Palomar | Low acclimation | −0.79 ± 0.21 | −3.76 | .02 |
| Berkeley–Yosemite | High acclimation | −0.93 ± 0.21 | −4.46 | <.0001 |
| Berkeley | Low/high acclimation | −0.89 ± 0.21 | −4.23 | <.001 |
| Stebbins | Low/high acclimation | −0.88 ± 0.20 | −4.18 | <.001 |
| Quail Ridge | Low/high acclimation | −1.01 ± 0.21 | −4.84 | <.0001 |
| Castle Rock | Low/high acclimation | −1.42 ± 0.21 | −6.79 | <.0001 |
| Mt Diablo | Low/high acclimation | −1.10 ± 0.21 | −5.26 | <.0001 |
| Yosemite | Low/high acclimation | −0.99 ± 0.21 | −4.73 | <.0001 |
Population and acclimation temperature were included as fixed factors, the replicates were included as random factors, and differences are given as β ± SE standard error. Only pairs that were significantly different are shown.