Adaptations of the reed frog Hyperolius viridiflavus (Amphibia,Anura, Hyperoliidae) to its arid environment

Summary Hyperolius viridiflavus nitidulus inhabits parts of the seasonally very hot and dry West African savanna. During the long lasting dry season, the small frog is sitting unhidden on mostly dry plants and has to deal with high solar radiation load (SRL), evaporative water loss (EWL) and small energy reserves. It seems to be very badly equipped to survive such harsh climatic conditions (unfavorable surface to volume ratio, very limited capacity to store energy and water). Therefore, it must have developed extraordinary efficient mechanisms to solve the mentioned problems. Some of these mechanisms are to be looked for within the skin of the animal (e.g. protection against fast desiccation, deleterious effects of UV radiation and overheating). The morphology of the wet season skin is, in most aspects, that of a normal anuran skin. It differs in the organization of the processes of the melanophores and in the arrangement of the chromatophores in the stratum spongiosum, forming no Dermal Chromatophore Unit. During the adaptation to dry season conditions the number of iridophores in dorsal and ventral skin is increased 4–6 times compared to wet season skin. This increase is accompanied by a very conspicuous change of the wet season color pattern. Now, at air temperatures below 35° C the color becomes brownish white or grey and changes to a brilliant white at air temperatures near and over 40° C. Thus, in dry season state the frog retains its ability for rapid color change. In wet season state the platelets of the iridophores are irregularly distributed. In dry season state many platelets become arranged almost parallel to the surface. These purine crystals probably act as quarter-wave-length interference reflectors, reducing SRL by reflecting a considerable amount of the radiated energy input.EWL is as low as that of much larger xeric reptilians. The impermeability of the skin seems to be the result of several mechanisms (ground substance, iridophores, lipids, mucus) supplementing each other.The light red skin at the pelvic region and inner sides of the limbs is specialized for rapid uptake of water allowing the frog to replenish the unavoidable EWL by using single drops of dew or rain, available for only very short periods.     

Comparative analysis of cutaneous evaporative water loss in frogs demonstrates correlation with ecological habits

Most frog species show little resistance to evaporative water loss (EWL), but some arboreal species are known to have very high resistances. We measured EWL and cutaneous resistance to evaporation (Rc) in 25 species of frogs from northern Australia, including 17 species in the family Hylidae, six species in the Myobatrachidae, and one each in the Bufonidae and the Microhylidae. These species display a variety of ecological habits, including aquatic, terrestrial, and arboreal specialisations, with the complete range of habits displayed within just the one hylid genus, Litoria. The 25 species measured in this study have resistances that range from Rc=0 to 63.1. These include low values indistinguishable from a free water surface to high values typical of "waterproof" anuran species. There was a strong correlation between ecological habit and Rc, even taking phylogenetic relationships into account; arboreal species had the highest resistance, aquatic species tended to have little or no resistance, and terrestrial species tended to have resistance between those of arboreal and aquatic frogs. For one species, Litoria rubella, we found no significant changes in EWL along a 1,500-km aridity gradient. This study represents the strongest evidence to date of a link between ecological habits and cutaneous resistance to water loss among species of frogs.     

Temperature and humidity dynamics of cutaneous and respiratory evaporation in pigeons,Columba livia

Summary Using a two-compartment metabolism chamber, we measured oxygen consumption simultaneously with evaporative water loss (EWL) separately from the skin and respiratory tract of pigeons exposed to various air temperatures and humidities. Both respiratory (REWL) and cutaneous (CEWL) water loss increased markedly with increasing air temperature, and latent heat loss through both routes dissipated large fractions of internal heat production during mild heat stress. CEWL as a percentage of total EWL significantly exceeded REWL (60±1.5%) at thermoneutral air temperatures, and was also a substantial fraction of total EWL at lower and higher temperatures. Both REWL and CEWL were inverse functions (apparently linear) of ambient humidity at 20 and 30 °C. These observations verify suggestions by other investigators that CEWL in birds plays a greater role in water balance and in counteracting heat stress than was previously believed.Abbreviations EWL evaporative water loss - CEWL cutaneous EWL - REWL Respiratory EWL - Oxygen consumption (cm³ g^–1 h^–1) - metabolic heat production per unit external surface area (W/m²) - Water vapor density (g/m³)     

Effects of dehydration on organ metabolism in the frogPseudacris crucifer: hyperglycemic responses to dehydration mimic freezing-induced cryoprotectant production

The metabolic effects of evaporative water loss at 5 °C were assessed for both fall- and spring-collected spring peepersPsuedacris crucifer. Frogs readily endured the loss of 50% of total body water. During dehydration organ water content was defended with no change in water content in skeletal muscle, gut, and kidney of 50% dehydrated frogs and reduced water content in liver, brain and heart. Dehydration stimulated a rapid and massive increase in liver glucose production. In fall-collected frogs liver glucose rose by 120-fold to 2690±400 nmol · mg protein^-1 or 220 mol · g ww^-1 in 50% dehydrated frogs and glucose in other organs increased by 2.6- to 60-fold. Spring-collected frogs showed the same qualitative response to dehydration although absolute glucose levels were lower, rising maximally by 8.4-fold in liver. Glucose synthesis was supported by glycogenolysis in liver and changes in the levels of glycolytic intermediates in liver indicated that an inhibitory block at the phosphofructokinase locus during desiccation helped to divert hexose phosphates into the production of glucose. Liver energy status (ATP, total adenylates, energy charge) was maintained even after the loss of 35% of total body water but at 50% dehydration all parameters showed a sharp decline; for example, energy charge fell from about 0.85 to 0.42. Severe dehydration also led to an accumulation of lactate in four organs, probably hypoxia-induced the to impaired circulation. The hyperglycemic response ofP. crucifer to dehydration mimics the cryoprotectant synthesis response seen during freezing of this freeze-tolerant frog, suggesting that these share a common regultory mechanism and that the cryoprotectant response may have arisen out of pre-existing volume regulatory responses of amphibians. The hyperglycemic response to dehydration might also be utilized during winter hibernation to help retard body water loss by raising the osmolality of the body fluids in situations where hibernaculum conditions become dry.Abbreviations bin body mass - bw body water - CrP creatine phosphate - dw dry weight - F6P fructose-6-phosphate - FBP fructose-1,6-bisphosphate - G6P glucose-6-phosphate - PEP phosphoenolpyruvate - PFK phosphofructokinase - PYR pyruvate - ww wet weight     

Aspects of Reproductive Biology of the Scalloped Hammerhead Shark, Sphyrna Lewini, off Northeastern Brazil

Ninety four scalloped hammerhead sharks, Sphyrna lewini (53 females and 41 males) ranging in size from 121 to 321cm total length (TL), were collected from surface gillnetters operating off northeastern Brazil and throughout the southwestern equatorial Atlantic Ocean between January and December 1996. A common regression for TL and eviscerated weight (EW) was calculated as, logEW = –11.786 + 2.889 logTL. Females and males were categorised into reproductive stages (4 and 2, respectively) according to morphological changes in their gonads. Size at sexual maturity for females was estimated to be 240cm, while males appeared to mature at between 180 and 200cm. Gravid females had between 2 and 21 embryos or pups, varying in TL from 3 to 38cm. There was no relationship between maternal length and size of litter. Copulation and parturition appear to occur outside the sampled area and possibly closer to the coast. With the exception of slightly lower uterine and ovarian fecundities, the results support the few existing data on the reproductive cycle of S. lewini in other areas.     

Adaptations of the reed frogHyperolius viridiflavus (Amphibia,Anura, Hyperoliidae) to its arid environment

Summary Of all amphibians living in arid habitats, reed frogs (belonging to the super speciesHyperolius viridiflavus) are the most peculiar. Froglets are able to tolerate dry periods of up to 35 days or longer immediately after metamorphosis, in climatically exposed positions. They face similar problems to estivating juveniles, i.e. endurance of long periods of high temperature and low RH with rather limited energy and water reserves. In addition, they must have had to develop mechanisms to prevent poisoning by nitrogenous wastes that rapidly accumulate during dry periods as a metabolic consequence of maintaining a non-torpid state.During dry periods, plasma osmolarity ofH. v. taeniatus froglets strongly increased, mainly through urea accumulation. Urea accumulation was also observed during metamorphic climax.During postmetamorphic growth, chromatophores develop with the density and morphology typical of the adult pigmentary pattern. The dermal iridophore layer, which is still incomplete at this time, is fully developed within 4–8 days after metamorphosis, irrespective of maintenance conditions. These iridophores mainly contain the purines guanine and hypoxanthine. The ability of these purines to reflect light provides an excellent basis for the role of iridophores in temperature regulation. In individuals experiencing dehydration stress, the initial rate of purine synthesis is doubled in comparison to specimens continuously maintained under wet season conditions. This increase in synthesis rate leads to a rapid increase in the thickness of the iridophore layer, thereby effectively reducing radiation absorption. Thus, the danger of overheating is diminished during periods of water shortage when evaporative cooling must be avoided. After the development of an iridophore layer of sufficient thickness for effective radiation reflectance, synthesis of iridophore pigments does not cease. Rather, this pathway is further used during the remaining dry season for solving osmotic problems caused by accumulation of nitrogenous wastes. During prolonged water deprivation, in spite of reduced metabolic rates, purine pigments are produced at the same rate as in wet season conditions. This leads to a higher relative proportion of nitrogen end products being stored in skin pigments under dry season conditions. At the end of an experimental dry season lasting 35 days, up to 38% of the accrued nitrogen is stored in the form of osmotically inactive purines in the skin. Thus the osmotic problems caused by evaporative water loss and urea production are greatly reduced.     

Water relations of the burrowing sandhill frog, Arenophryne rotunda (Myobatrachidae)

Arenophryne rotunda is a small (2–8 g) terrestrial frog that inhabits the coastal sand dunes of central Western Australia. While sand burrowing is a strategy employed by many frog species inhabiting Australia’s semi-arid and arid zones, A. rotunda is unique among burrowing species because it lives independently of free water and can be found nocturnally active on the dune surface for relatively extended periods. Consequently, we examined the physiological factors that enable this unique frog to maintain water balance. A. rotunda was not found to have any special adaptation to reduce EWL (being equivalent to a free water surface) or rehydrate from water (having the lowest rehydration rate measured for 15 Western Australian frog species), but it was able to maintain water balance in sand of very low moisture (1–2%). Frogs excavated in the field were in dune sand of 4.4% moisture content, as a consequence of recent rain, which was more than adequate for these frogs to maintain water balance as reflected by their low plasma and urine osmotic concentrations. We suggest that in dry periods of the year, A. rotunda can achieve positive water balance by cutaneous water uptake by burrowing deeper into the substrate to where the percent water content is greater than 1.5%.     

Competition and the distribution of spring peeper larvae

Studies of tadpole distributions have shown that despite overlapping affinities for semipermanent and permanent ponds, distributions of the spring peeper (Pseudacris crucifer) and the green frog (Rana clamitans) tend to be nonoverlapping. Because spring peepers are believed to be poor competitors, I hypothesized that competition from green frog larvae limits the distribution of spring peeper larvae. I stocked field enclosures with a constant density of spring peeper larvae, and one of four densities of green frog larvae (a target-neighbor design). Increased green frog density had a small effect on metamorphic size and no effects on survivorship, larval period or growth rates of spring peepers. In contrast to these small interspecific effects, green frogs had a large effect on their own performance. Intraspecific competition resulted in a 50% decline in growth rate and an 11% decline in metamorphic size. These results suggest that the species are segregated in resource use, or that compared with green frogs, spring peepers are better able to cope with depressed resource densities. In either case, this field experiment provides no evidence that interspecific competition from green frogs limits distributions of spring peepers. Other factors such as predation and breeding site choice by adults may contribute to the absence of spring peeper larvae from many semipermanent and permanent ponds.     

Thermal and hydric implications of diurnal activity by a small tropical frog during the dry season

Amphibians are typically intolerant of high temperatures and dehydrating conditions, and small species are particularly susceptible to desiccation. The rockhole frog, Litoria meiriana (Hylidae), is diurnal and is often observed on rocks in the sun near streams in tropical Australia. These hot, desiccating conditions are avoided by most frog species. We measured the microclimate in the areas used by frogs and the activity, body temperatures and hydric state of free‐ranging individuals of this small frog. We also used plaster models to further explore the dynamic nature of hydric state by combining estimates of water loss and water uptake with behavioural observations of activity and microhabitat selection. Both direct measures and estimates of dynamic hydric state indicated that free‐ranging frogs generally maintained a hydric state above 95% of full hydration, but occasionally, particularly during the afternoon, frogs allowed their hydric state to fall as low as 85%. Body temperatures of frogs remained below the critical thermal maximum (CT_max) even when the frogs were in the sun, because this species has no cutaneous resistance to evaporative water loss and so they cool by evaporation. However, during the hotter part of the day, on dry sunny substrates, the hydric state of the frogs could fall to near lethal hydration states (approximately 70% of full hydration) within a short period (approximately 20 min). Thus, the threat of desiccation appears to be more limiting than the threat of overheating. These diurnal frogs rely on frequent bouts of rehydration to support their ability to venture onto hot, dry rocks during the day.     

Effect of cooling rate on the survival of frozen wood frogs,Rana sylvatica

Summary Wood frogs (Rana sylvatica) were frozen to-2.5°C under five distinct cooling regimes to investigate the effect of cooling rate on survival. Frogs survived freezing when cooled at -0.16°C · h^-1 or -0.18°C · h^-1, but mortality resulted at higher rates (-0.30°C · h^-1,-1.03°C · h^-1, and -1.17°C · h^-1). Surviving frogs in the latter groups required longer periods to recover, and transient injury to the neuromuscular system was evident. Some of the frogs that died had patches of discolored, apparently necrotic skin; vascular damage, as indicated by hematoma, also occurred. It is concluded that slow cooling may be critical to the freeze tolerance of wood frogs. Additional studies examined the effect of cooling rate on physiological responses promoting freeze tolerance. Mean glucose concentrations measured in plasma (15–16 mol · ml^-1) and liver (42–45 mol · g^-1) following a 2-h thaw did not differ between slowly- and rapidly-cooled frogs but in both groups were elevated relative to unfrozen controls. Thus freezing injury to rapidly-cooled frogs apparently was not mitigated by the presence of elevated glucose. Water contents of liver tissue, measured 2 h post-thawing, did not differ between slowly-cooled (mean = 77.6%) and rapidly-cooled (mean = 78.5%) frogs. However, the mean hematocrit of slowly-cooled frogs (48%) was significantly higher than that (37%) of frogs cooled rapidly, possibly owing to differences in the dynamics of tissue water during freezing.     

Diurnal variation in thermal and metabolic parameters of the golden hamster (Mesocricetus auratus)

The purpose of this study is to examine diurnal variation in several thermal and metabolic parameters of the golden hamster, Mesocricetus auratus. Metabolic rate, core temperature, and evaporative water loss were measured during night and day at several ambient temperatures. Wet minimal thermal conductance, dry minimal thermal conductance, basal metabolic rate, minimal net heat production and the lower critical temperature difference were estimated from these measurements. Wet and dry minimal thermal conductance, evaporative water loss, core temperature, basal metabolic rate, and lower critical temperature difference were greater during the active phase than during the resting phase. The diurnal variation in wet minimal thermal conductance was much smaller than that predicted from published allometric equations. The diurnal variation in wet minimal thermal conductance was 9% of the 24-h mean. The diurnal variation in dry minimal thermal conductance was 26% of the 24-h mean. The higher active-phase core temperature and basal metabolic rate may function to enhance peak metabolic performance during the active phase. The lower resting phase metabolism and core temperature may reduce energetic costs. The greater active-phase lower critical temperature difference may be a result of the greater active-phase basal metabolic rate. Diurnal variation in minimal thermal conductance may be caused by changes in peripheral circulation.Abbreviations BMR basal metabolic rate - T difference between core and ambient temperatures - T _1c lower critical temperature difference - EWL evaporative water loss - MTC minimal thermal conductance - MR metabolic rate - Q _ev evaporative heat loss - RQ respiratory quotient - T _a ambient temperature - T _c core temperature - T _1c lower critical temperature     

Thermoregulation in a large bird,the emu (Dromaius novaehollandiae)

The emu is a large, flightless bird native to Australia. Its habitats range from the high snow country to the arid interior of the continent. Our experiments show that the emu maintains a constant body temperature within the ambient temperature range-5 to 45°C. The males regulate their body temperature about 0.5°C lower than the females. With falling ambient temperature the emu regulates its body temperature initially by reducing conductance and then by increasing heat production. At-5°C the cost of maintaining thermal balance is 2.6 times basal metabolic rate. By sitting down and reducing heat loss from the legs the cost of homeothermy at-5°C is reduced to 1.5 times basal metabolic rate. At high ambient temperatures the emu utilises cutaneous evaporative water loss in addition to panting. At 45°C evaporation is equal to 160% of heat production. Panting accounts for 70% of total evaporation at 45°C. The cost of utilising cutaneous evaporation for the other 30% appears to be an increase in dry conductance.Abbreviations A _r Effective radiating surface area - BMR basal metabolic rate - C _dry dry conductance - CEWL cutaneous evaporative water loss - EHL evaporative heat loss - EWL evaporative water loss - FECO₂ fractional concentration of CO₂ in excurrent air - FF_H2O water content of chamber excurrent air - FEO₂ fractional concentration of O₂ in chamber excurrent air - FICO₂ fractional concentration of CO₂ in incurrent air - FIO₂ fractional concentration of O₂ in chamber incurrent air - MHP metabolic heat production - MR metabolic rate - REWL respiratory evaporative water loss - RH relative humidity - RQ respiratory quotient ; - SA surface area - SEM standard error of the mean - SNK Student-Newman-Keuls multiple range test - STPD standard temperature and pressure dry - T _a ambient temperature(s) - T _b body temperature(s) - T _e surface temperature(s) - flow rate of air into the chamber - carbon dioxide production - oxygen consumption - vapour pressure of water     

Correlation between rainfall in the dry season and the occurrence of the white rice borer (Scirpophaga innotata Wlk.) in Java

The amount of rain which falls sporadically in the relatively dry season at the time that the white rice borer is diapausing as a full grown larva in the rice stubble, has a very important influence on the size of population of the borers in the following wet season when rice is grown. If this dry season is wet or very wet (according to our standard, based on the figures of rainfall and borer damage over 26 years in five regions of Eastern Java), no damage can be expected in the following planting season. If the dry season is really dry or very dry, outbreaks of borers may occur (in the period under survey this occurred in nine out of fourteen years). We have tried to give an outline of a method of prediction of borer damage in the planting season, based on the rainfall dates of the foregoing dry season.

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Zusammenfassung Der Weisse Reisbohrer (Scirpophaga innotata Wlk.) kommt nur in Gebieten vor, wo jährlich eine ausgeprägte Regen- und Trockenzeit (Monsun) auftritt. Am Ende der Regenzeit gehen die vollerwachsenen Raupen, die im Stengel der reifenden Reispflanze leben, in Diapause. Während der folgenden relativ trockenen Jahreszeit, wenn nur gelegentlich Regenschauer fallen, ruhen die Raupen in der Stoppel. Bald nachdem die ersten heftigen Regenfälle der neuen Regenzeit einsetzen, verpuppen sich die Larven und alle Falter schlüpfen gemeinsam zum Stoppelflug.Dieser Zünsler ist in gewissen Gebieten Javas einer der Hauptschädlinge des Reises, obwohl sein Auftreten sehr unregelmäßig ist. Jahrelang war man allgemein der Auffassung, daß relativ reichlicher Regenfall während der Trockenzeit die Reisbohrerpopulation erheblich vermindere und daß in diesem Falle keine schweren Schäden durch Reisbohrerbefall erwartet werden können.Während eines Zeitraums von 26 Jahren (1915–1940) wurden in fünf Gebieten Ost-Javas sowolhl der Niederschlag wie der Bohrerschaden untersucht und Berechnungen der jährlichen Niederschlagsmenge in der Trockenzeit und des Bohrerschadens verglichen. Dies erhärtete die alte Auffassung, daß nach einer relativ feuchten oder sehr feuchten Trockenzeit kein Bohrerbefall von Bedeutung während des Beobachtungszeitraumes auftritt. Dagegen folgten in neun von 14 Jahren mit einer trockenen oder sehr trockenen Trockenzeit schwere oder ziemlich schwere Ausbrüche der Weißen Reisstengelbohrer während der folgenden feuchten Jahreszeiten. Obwohl auch andere Faktoren von einiger Bedeutung sein dürften, wird geschlossen, daß die Niederschlagsmenge während der Trockenzeit einen sehr entscheidenden Einfluß auf die Möglichkeit des Auftrétens einer Reisbohrer Kalamität im darauffolgenden Jahre hat. Diesen Daten entsprechend wird auf der Grundlage der Niederschlagszahlen in der vorangegangenen Trockenzeit ein Prognose-Schema entwickelt, wann Bohrerschaden zu erwarten ist.

     

Low temperature X-ray investigation of structural distributions in myoglobin

The results of X-ray structure analysis of metmyoglobin at 300 K, 185 K, 165 K, 115 K and 80 K are reported. The lattice vectorsa andb decrease linearly with temperature whilec shows non-linearity above 180 K, indicating some type of phase transition. Cooling does change the myoglobin structure but only within the structural distribution as determined by individual x ² at room temperature. Two residues showed significant alternative positions for sidechains at higher temperatures while only one position is occupied at low temperatures. In the case of LEU 61 a jump between different positions of the side-chain reduces the potential barrier for the entrance of the O₂ molecule to the heme pocket.The mean square displacements, x ², of the individual residues decrease linearly with temperature in most cases, indicating a parabolic envelope for the potential responsible for motions. A separation of rotational and translational disorder of the entire molecule is discussed. Comparison with Mössbauer spectroscopy indicates that protein dynamics on a time scale faster than 10^-7 s is not simply a harmonic process. Extrapolation of the structural distributions toT=0 K shows that a large zero point distribution of the myoglobin structure exists, thus proving that there is no absolute energy minimum for one well defined conformation.Dedicated to Prof. H. Frauenfelder on his 65^th birthday     

Holes photogeneration in phthalocyanine-doped polysilane

Polysilane polymers are attractive photoconductive materials, due to the high mobility of the charge carriers (holes). The photoconductivity in the visible region is greatly enhanced by the addition of a phthalocyanine, because the dopant increases the absorption of light and the quantum yield of the holes photogeneration. The quantum yield has been measured by the technique of xerographic discharge at several values of the polarisation field. From these data the intrinsic quantum yield ₀ and the thermalisation distance r ₀ were calculated. r ₀ is similar to the value measured in the trinitrofluorenone doped polyvinylcarbazole system (27.5 ) while ₀ is much lower (2.8·10^–2 compared to 0.11). In fact, r ₀ is assumed to be mainly dependent on the polymeric environment, while ₀ depends on the nature of the coupling between the dopant and the polymer.     

Mechanisms contributing to seasonal homeostasis of minimum leaf water potential and predawn disequilibrium between soil and plant water potential in Neotropical savanna trees

Seasonal regulation of leaf water potential (_L) was studied in eight dominant woody savanna species growing in Brazilian savanna (Cerrado) sites that experience a 5-month dry season. Despite marked seasonal variation in precipitation and air saturation deficit (D), seasonal differences in midday minimum _L were small in all of the study species. Water use and water status were regulated by a combination of plant physiological and architectural traits. Despite a nearly 3-fold increase in mean D between the wet and dry season, a sharp decline in stomatal conductance with increasing D constrained seasonal variation in minimum _L by limiting transpiration per unit leaf area (E). The leaf surface area per unit of sapwood area (LA/SA), a plant architectural index of potential constraints on water supply in relation to transpirational demand, was about 1.5–8 times greater in the wet season compared to the dry season for most of the species. The changes in LA/SA from the wet to the dry season resulted from a reduction in total leaf surface area per plant, which maintained or increased total leaf-specific hydraulic conductance (G_t) during the dry season. The isohydric behavior of Cerrado tree species with respect to minimum _L throughout the year thus was the result of strong stomatal control of evaporative losses, a decrease in total leaf surface area per tree during the dry season, an increase in total leaf-specific hydraulic conductance, and a tight coordination between gas and liquid phase conductance. In contrast with the seasonal isohydric behavior of minimum _L, predawn _L in all species was substantially lower during the dry season compared to the wet season. During the dry season, predawn _L was more negative than bulk soil estimated by extrapolating plots of E versus _L to E=0. Predawn disequilibrium between plant and soil was attributable largely to nocturnal transpiration, which ranged from 15 to 22% of the daily total. High nocturnal water loss may also have prevented internal water storage compartments from being completely refilled at night before the onset of transpiration early in the day.     

Water loss in Anolis lizards: evidence for acclimation and intraspecific differences along a habitat gradieNT

• 1.1. Rates of evaporative water loss (EWL) were measured in Anolis roquet and A. marmoratus each from three localities which varied in conditions of aridity.
• 2.2. There were significant interpopulational differences in rates of EWL for both species which correlated with habitat aridity.
• 3.3. Rates of EWL were significantly lower in A. roquet after 6 weeks acclimation to more xeric conditions, populational differences were still evident.
• 4.4. Acclimational effects on rates of EWL were 2 to 3 times greater than populational differences.

     

Seasonal patterns of gas exchange,water relations and growth of it Roupala montana,an evergreen savanna species

Roupala montana is an evergreen species widespread in the seasonal savannas of the central plains of Brazil. I examined the degree of coupling of photosynthetic gas-exchange characteristics, water relations and growth responses of R. montana with regard to seasonal changes in soil water availability. Despite a rainless period of over three months soil water potential at 60 cm depth reached values of only about -1.0 MPa, while pre-dawn leaf water potential (^l) reached about -0.4 MPa by the end of the three-month drought. Thus, R. montana had access to deep soil water in the dry period, but pre-dawn ^l did not reach the high wet season values of -0.2 MPa. Most of the shoot growth was concluded in the onset of the rainy season. Although some individual branches might have shown some extension thereafter, most of them remained inactive during the rest of the rainy season and the subsequent dry season. New leaf production was also restricted to the first part of the wet period. R. montana remained evergreen in the dry season, but there was a 27% decrease in the number of leaves and herbivory removed about 16% of the leaf area still present in the plant. CO₂-exchange rates of these leaves reached only ca. 55% of the maximum rainy season values of 14 µmol m^-2 s^-1. Thus, the estimated potential daily carbon gain was about 34% of the maximum by the end of the dry period. These values will be even lower, if we considered the decrease in photosynthetic rates that occurred around midday. These reductions in photosynthetic rates as a result of partial stomatal closure were measured both in the wet and dry season and they were related to increases in the evaporative demand of the atmosphere. In conclusion, the combined effect of herbivory, leaf loss and reductions in photosynthetic rates limited plant productivity in the dry season.     

Phenotypic Differences in Buoyancy and Energetics of Lean and Siscowet Lake Charr in Lake Superior

At least two phenotypes of lake charr, Salvelinus namaycush, coexist in Lake Superior. A lean morph frequents the shallow inshore waters (< 50m) and the fat morph (siscowet) occupies the deeper offshore waters (50–250 m). The objective of this study was to determine if the elevated lipid concentration of siscowets reduces the costs of swimming in deep water. First, we modelled the effects of body composition (lipids) on the costs of swimming by lake charr, and then compared these theoretical results with empirical evidence obtained from Cesium 137-based estimates of food consumption, gross energy conversion, and swimming costs (activity multiplier). The attributes of growth, energy content (kJg^-1), lipid concentrations, and Cesium 137 concentration (Bqg^-1) were obtained from multimesh gillnet catches in eastern Lake Superior (1998 and 1999). The model showed that siscowet (fat) lake charr expended less energy than lean lake charr moving through the water column. Empirical evidence derived from Cesium 137 analysis confirmed that the activity multipliers of siscowets (fat) were less than those for lean charr. These findings support the view that the restoration of the fish community of the predominately deep water of the Great Lakes might be facilitated by the introduction of the fat phenotype.