| Literature DB >> 29018365 |
Shaun Welman1, Andrew A Tuen2, Barry G Lovegrove1.
Abstract
The observation of heterothermy in a single suborder (Strepsirrhini) only within the primates is puzzling. Given that the placental-mammal ancestor was likely a heterotherm, we explored the potential for heterothermy in a primate closely related to the Strepsirrhini. Based upon phylogeny, body size and habitat stability since the Late Eocene, we selected western tarsiers (Cephalopachus bancanus) from the island of Borneo. Being the sister clade to Strepsirrhini and basal in Haplorrhini (monkeys and apes), we hypothesized that C. bancanus might have retained the heterothermic capacity observed in several small strepsirrhines. We measured resting metabolic rate, subcutaneous temperature, evaporative water loss and the percentage of heat dissipated through evaporation, at ambient temperatures between 22 and 35°C in fresh-caught wild animals (126.1 ± 2.4 g). We also measured core body temperatures in free-ranging animals. The thermoneutral zone was 25-30°C and the basal metabolic rate was 3.52 ± 0.06 W.kg-1 (0.65 ± 0.01 ml O2.g-1.h-1). There was no evidence of adaptive heterothermy in either the laboratory data or the free-ranging data. Instead, animals appeared to be cold sensitive (Tb ~ 31°C) at the lowest temperatures. We discuss possible reasons for the apparent lack of heterothermy in tarsiers, and identify putative heterotherms within Platyrrhini. We also document our concern for the vulnerability of C. bancanus to future temperature increases associated with global warming.Entities:
Keywords: evolution; metabolism; primate thermoregulation; tarsiers; tropics
Year: 2017 PMID: 29018365 PMCID: PMC5623056 DOI: 10.3389/fphys.2017.00745
Source DB: PubMed Journal: Front Physiol ISSN: 1664-042X Impact factor: 4.566
Figure 1The thermoregulatory profile of Cephalopachus bancanus. (A) Effect of ambient temperature on resting metabolic rate. (B) Effect of ambient temperature on subcutaneous temperature. (C) Effect of ambient temperature on the rate of evaporative water loss. (D) Effect of ambient temperature on the amount of metabolic heat dissipated through evaporative cooling. Plotted regression lines indicate the best fit for the data based on piecewise regression analysis and the equations are presented in Table 1. Closed circles = males, open circles = females.
Linear regression models describing the relationship between ambient temperature (Ta) and various physiological parameters in Cephalopachus bancanus.
| RMR | Ta < 25°C: | RMR = 16.65 − 0.5212 × Ta |
| Ta > 30°C: | RMR = 0.2479 × Ta − 4.069 | |
| Tsub | Ta < 30°C: | Tsub = 25.64 + 0.2879 × Ta |
| Ta > 30°C: | Tsub = 14.64 + 0.6547 × Ta | |
| EWL | All | EWL = 0.17512 × Ta − 2.41254 |
| EHL/MHP | Ta < 30°C: | EHL/MHP = 3.761 × Ta − 61.52 |
Mass-specific resting metabolic rate = RMR, subcutaneous temperature = T,
p < 0.05,
p < 0.01.
Linear mixed-effect models which best describe the significant relationships between ambient temperature (Ta) and resting metabolic rate (RMR), subcutaneous temperature (Tsub), the rate of evaporative water loss (EWL) and the amount of metabolic heat dissipated through evaporative cooling (EHL/MHP) in Cephalopachus bancanus.
| Ta | ~1|ID | 4 | −37.92 | 0.74 |
| Ta + Mb | ~1|ID | 5 | −34.89 | 0.16 |
| Ta + Sex | ~1|ID | 5 | −33.34 | 0.07 |
| Ta + Mb + Sex | ~1|ID | 6 | −31.08 | 0.02 |
| Ta | ~1|ID | 4 | −0.69 | 0.7 |
| Ta + Mb | ~1|ID | 5 | 1.01 | 0.3 |
| Ta | ~1|ID | 4 | 51.57 | 0.82 |
| Ta + Sex | ~1|ID | 5 | 56.01 | 0.09 |
| Ta + Mb | ~1|ID | 5 | 56.15 | 0.08 |
| Ta + Mb + Sex | ~1|ID | 6 | 61.34 | 0.01 |
| Ta + Mb + Sex | ~1|ID | 6 | 43.15 | 0.73 |
| Ta + Mb | ~1|ID | 5 | 45.81 | 0.19 |
| Ta | ~1|ID | 4 | 48.06 | 0.06 |
| Ta + Sex | ~1|ID | 5 | 50.88 | 0.02 |
| Ta | ~1|ID | 4 | 117.26 | 0.58 |
| Ta + Sex | ~1|ID | 5 | 119.66 | 0.17 |
| Ta + Mb | ~1|ID | 5 | 119.67 | 0.17 |
| Ta + Mb + Sex | ~1|ID | 6 | 121.47 | 0.07 |
| Ta | ~1|ID | 4 | −52.66 | 0.65 |
| Ta + Mb | ~1|ID | 5 | −50.19 | 0.19 |
| Ta + Sex | ~1|ID | 5 | −49.62 | 0.14 |
| Ta + Mb + Sex | ~1|ID | 6 | −46.19 | 0.03 |
Only models with Akaike weights ≥ 0.01 are presented.
Figure 2The free-ranging temperature profile in western tarsiers (Cephalopachus bancanus). (A) The ambient temperatures (Ta; gray line) and core temperatures (Tcore; black line) recorded in a female from 00:00 24th June 2015 to 00:00 27th July 2015. (B) The ambient temperatures (Ta; gray line) and core temperatures (Tcore; black line) recorded in a male from 00:00 24th June 2015 to 06:30 10th July 2015. The grey and white bars represent night and day, respectively, and the black bars at the base of each plot represent the temperature differential between the Ta and Tcore. (C,D) The frequency distribution of the respective Tas and Tcores observed in the female and male tarsier's temperature profile.
The daily mean, maximum and minimum ambient (Ta) and tarsier core (Tcore) temperatures observed throughout the period of free-ranging data collection (values in parenthesis represent the range in daily means), as well as the times at which these parameters where most frequently observed.
| Mean | 28.6°C (25.75–31.0°C) | 34.4°C (32.9–35.2°C) | 34.7°C (33.9–35.6°C) | 25.8°C (23.8–27.7°C) | 35.1°C (33.5–35.7°C) | 35.3°C (34.1–36.4°C) |
| Maximum | 32.1°C (28.0–35.2°C) | 35.8 (34.9–36.8°C) | 35.7°C (35.0–36.9°C) | 28.2°C (24.3–29.9°C) | 35.8°C (34.0–36.4°C) | 36.1°C (37.1–35.3°C) |
| Minimum | 24.3°C (22.3–27.0°C) | 33.4°C (31.5–34.4°C) | 33.7°C (31.6–35.3°C) | 24.30°C (22.2–27.1°C) | 34.4°C (30.6–35.3°C) | 34.4°C (32.2–35.8°C) |
| ♀ | ♀ | ♂ | ♂ | |||
| Photophase (ρ-phase) | 06:30 (53%); 14:30 (12%); 16:00 (18%) | |||||
| Scotophase (α-phase) | 06:00 (18%); 19:00 (59%) | |||||
Photophase corresponds to the animals rest phase, whereas scotophase corresponds to their active phase. ♂, male; ♀, female; max, highest temperature; min, lowest temperature; n, periods of observations and
indicates a significant (p < 0.05) Rayleigh's test.
Figure 3The frequency distribution of the scotophase and photophase ambient temperatures recorded within the forest at Sama Jaya Nature Reserve from 00:00 24th June 2015 to 00:00 27th July 2015. The arrow indicates the commonly predicted shift of three degree Celsius in the modal temperature associated with global warming.