The application of δ¹⁸O and δD for understanding water pools and fluxes in a Typha marsh

The δ¹⁸O and δD composition of water pools (leaf, root, standing water and soil water) and fluxes [transpiration (T), evaporation (E)] were used to understand ecohydrological processes in a managed Typha latifolia L. freshwater marsh. We observed isotopic steady‐state T and deep rooting in Typha. The isotopic mass balance of marsh standing water showed that E accounted for 3% of the total water loss, T accounted for 17% and subsurface drainage (D) accounted for the majority (80%). There was a vertical gradient in water vapour content and isotopic composition within and above the canopy sufficient for constructing an isotopic mass balance of water vapour during some sampling periods. During these periods, the proportion of T in evapotranspiration (T/ET) was between 56 ± 17% and 96 ± 67%, and the estimated error was relatively high (>37%) because of non‐local, background sources in vapour. Independent estimates of T/ET using eddy covariance measurements yielded similar mean values during the Typha growing season. The various T/ET estimates agreed that T was the dominant source of marsh vapour loss in the growing season. The isotopic mass balance of water vapour yielded reasonable results, but the mass balance of standing water provided more definitive estimates of water losses.     

Modelling non‐steady‐state isotope enrichment of leaf water in a gas‐exchange cuvette environment

The combined use of a gas‐exchange system and laser‐based isotope measurement is a tool of growing interest in plant ecophysiological studies, owing to its relevance for assessing isotopic variability in leaf water and/or transpiration under non‐steady‐state (NSS) conditions. However, the current Farquhar & Cernusak (F&C) NSS leaf water model, originally developed for open‐field scenarios, is unsuited for use in a gas‐exchange cuvette environment where isotope composition of water vapour (δ_v) is intrinsically linked to that of transpiration (δ_E). Here, we modified the F&C model to make it directly compatible with the δ_v–δ_E dynamic characteristic of a typical cuvette setting. The resultant new model suggests a role of ‘net‐flux’ (rather than ‘gross‐flux’ as suggested by the original F&C model)‐based leaf water turnover rate in controlling the time constant (τ) for the approach to steady sate. The validity of the new model was subsequently confirmed in a cuvette experiment involving cotton leaves, for which we demonstrated close agreement between τ values predicted from the model and those measured from NSS variations in isotope enrichment of transpiration. Hence, we recommend that our new model be incorporated into future isotope studies involving a cuvette condition where the transpiration flux directly influences δ_v. There is an increasing popularity among plant ecophysiologists to use a gas‐exchange system coupled to laser‐based isotope measurement for investigating non‐steady state (NSS) isotopic variability in leaf water (and/or transpiration); however, the current Farquhar & Cernusak (F&C) NSS leaf water model is unsuited for use in a gas‐exchange cuvette environment due to its implicit assumption of isotope composition of water vapor (δ_v) being constant and independent of that of transpiration (δ_E). In the present study, we modified the F&C model to make it compatible with the dynamic relationship between δ_v and δ_E as is typically associated with a cuvette setting. Using an experiment conducted on cotton leaves, we show that the modified NSS model performed well in predicting the time constant for the exponential approach of leaf water toward steady state under cuvette conditions. Such a result demonstrates the applicability of this new model to gas‐exchange cuvette conditions where the transpiration flux directly influences δ_v, and therefore suggests the need to incorporate this model into future isotope studies that employ a laser‐cuvette coupled system.     

降雨和非降雨日兴安落叶松天然林蒸腾及蒸散发特征

综合利用树干液流法和涡动相关技术,对大兴安岭北部寒温带兴安落叶松(Larix gmelinii)天然林的林木蒸腾(T)和生态系统蒸散发(ET)进行连续监测;采用边材面积对单木蒸腾耗水进行尺度扩展,分析降雨和非降雨日林木总蒸腾(T_(tot))及其蒸腾组分(优势木蒸腾T_d、中等木蒸腾T_i和劣势木蒸腾T_s)与生态系统ET的变化特征,探讨T_(tot)与ET对水汽压亏缺(VPD)和净辐射(R_n)变化的响应。结果表明:降雨和非降雨日各分化等级林木液流速率的日变化均呈典型单峰格局,且降雨日的T_(tot)(9.7mm)低于非降雨日(31.4 mm),同时T_d在降雨和非降雨日均明显高于T_i和T_s。降雨日的ET(24.7 mm)同样低于非降雨日(50.6mm),而潜热通量与同期R_n之比(31%)则高于非降雨日(25.1%),表明非降雨日的环境条件较有利于植物-大气界面的水汽通量交换。降雨日T_(tot)/ET、T_d/ET、T_i/ET和T_s/ET(分别为38.1%、27.2%、8.5%和2.4%)均低于非降雨日(分别为65.0%、45.5%、15.3%和4.2%),说明降雨日的ET以自由水蒸发为主,而非降雨日时则以T_d占优;同时,仅以优势木蒸腾耗水作为平均水平进行尺度上推易高估林分的蒸腾能力。总体上,T_(tot)与VPD、R_n的相关性均较ET的高,即T_(tot)对环境因子的响应略敏感;同时R_n与T_(tot)、ET的相关性均较VPD高,说明R_n是驱动生态系统水汽通量的首要条件。     

Effect of atoms evaporated from the anode on the structure of the vacuum arc space charge sheath

The structure of the anode space charge sheath of a vacuum arc is studied with allowance for the dependence of the negative anode fall on the ratio of the directed electron velocity v ₀ to the electron thermal velocity v _T for different values of the flux density of atoms evaporated from the anode. Poisson’s equation for the sheath potential is solved taking into account the electron space charge, fast cathode ions, and slow ions produced due to the ionization of atoms evaporated from the anode. The kinetic equation for atoms and slow anode ions is solved with allowance for ionization in the collision integral. Analytic solutions for the velocity distribution functions of atoms and slow ions and the density of slow ions are obtained. It is shown that the flux of slow ions substantially affects the spatial distribution of the electric field E(z) in the sheath. As the flux density increases, the nonmonotonic dependence E(z) transforms into a monotonic one and the sheath narrows. For a given flux of evaporated atoms Πa, the increase in the ratio of the directed electron velocity to the electron thermal velocity leads again to a nonmonotonic dependence E(z). As z increases, the electric field first increases, passes through the maximum, decreases, passes through the minimum E _min, and then again increases toward the anode. There is a limiting value of the ratio (v ₀/v _T )* at which E _min(z) vanishes. At v ₀/v _T > (v ₀/V _T )*, the condition for the existence of a steady-state sheath is violated and the profiles of the field and potential in the sheath become oscillating. The dependence of (v ₀/v _T )* on the flux density of evaporated atoms Π _a is obtained. It is shown that the domain of existence of steady-state solutions in the sheath broadens with increasing Π _a .     

Challenge from the simple: some caveats in linearization of the Boyle-van't Hoff and Arrhenius plots

Some aspects of proper linearization of the Boyle-van’t Hoff (BVH) relationship for calculation of the osmotically inactive volume v_b, and Arrhenius plot (AP) for the activation energy E_a are discussed. It is shown that the commonly used determination of the slope and the intercept (v_b), which are presumed to be independent from each other, is invalid if the initial intracellular molality m₀ is known. Instead, the linear regression with only one independent parameter (v_b) or the Least Square Method (LSM) with v_b as the only fitting LSM parameter must be applied. The slope can then be calculated from the BVH relationship as the function of v_b. In case of unknown m₀ (for example, if cells are preloaded with trehalose, or electroporation caused ion leakage, etc.), it is considered as the second independent statistical parameter to be found. In this (and only) scenario, all three methods give the same results for v_b and m₀. AP can be linearized only for water hydraulic conductivity (L_p) and solute mobility (ω_s) while water and solute permeabilities P_w ≡ L_pRT and P_s ≡ ω_sRT cannot be linearized because they have pre-exponential factor (RT) that depends on the temperature T.     

Phreatophytes under stress: transpiration and stomatal conductance of saltcedar (Tamarix spp.) in a high-salinity environment

Background and aims

We sought to understand the environmental constraints on an arid-zone riparian phreatophtye, saltcedar (Tamarix ramosissima and related species and hybrids), growing over a brackish aquifer along the Colorado River in the western U.S. Depth to groundwater, meteorological factors, salinity and soil hydraulic properties were compared at stress and non-stressed sites that differed in salinity of the aquifer, soil properties and water use characteristics, to identify the factors depressing water use at the stress site.

Methods

Saltcedar leaf-level transpiration (E_L), LAI, and stomatal conductance (G_S) were measured over a growing season (June–September) with Granier and stem heat balance sensors and were compared to those for saltcedar at the non-stress site determined in a previous study. Transpiration on a ground-area basis (E_G) was calculated as E_L?×?LAI. Environmental factors were regressed against hourly and daily E_L and G_S at each site to determine the main factors controlling water use at each site.

Results

At the stress site, mean E_G over the summer was only 30 % of potential evapotranspiration (ET_o). G_S and E_G peaked between 8 and 9 am then decreased over the daylight hours. Daytime G_S was negatively correlated with vapor pressure deficit (VPD) (P?<?0.05). By contrast, E_G at the non-stress site tracked the daily radiation curve, was positively correlated with VPD and was nearly equal to ET_o on a daily basis. Depth to groundwater increased over the growing season at both sites and resulted in decreasing E_G but could not explain the difference between sites. Both sites had high soil moisture levels throughout the vadose zone with high calculated unsaturated conductivity. However, salinity in the aquifer and vadose zone was three times higher at the stress site than at the non-stress site and could explain differences in plant E_G and G_S.

Conclusions

Salts accumulated in the vadose zone at both sites so usable water was confined to the saturated capillary fringe above the aquifer. Existence of a saline aquifer imposes several types of constraints on phreatophyte E_G, which need to be considered in models of plant water uptake. The heterogeneous nature of saltcedar E_G over river terraces introduces potential errors into estimates of ET by wide-area methods.     

Living in sympatry: The effect of habitat partitioning on the thermoregulation of three Mediterranean lizards

The ability for effective, accurate and precise thermoregulation is of paramount importance for ectotherms. Sympatric lizards often partition their niche and select different microhabitats. These microhabitats, however, usually differ in their thermal conditions and lizards have to adapt their thermoregulation behavior accordingly. Here, we evaluated the impact of habitat partitioning on the thermal biology of three syntopic, congeneric lacertids (Podarcis peloponnesiacus, P. tauricus and P. muralis) from central Peloponnese, Greece. We assessed thermoregulation effectiveness (E) using the three standard thermal parameters: body (T_b), operative (T_e) and preferred (T_pref) temperatures. We hypothesized that the microhabitats used by each species would differ in thermal quality. We also predicted that all species would effectively thermoregulate, as they inhabit a thermally challenging mountain habitat. As expected, the partition of the habitat had an effect on the thermoregulation of lizards since microhabitats had different thermal qualities. All three species were effective and accurate thermoregulators but one of them achieved smaller E values as a result of the lower T_b in the field. This discrepancy could be attributed to the cooler (but more benign) thermal microhabitats that this species occupies.     

Measurements of the temperature of subsonic CO<Subscript>2</Subscript> induction plasma flows by analyzing their emission spectra

Results are presented from measurements of the temperature characteristics of subsonic CO² plasma flows generated by a 100-kW induction plasmatron at the Institute for Problems of Mechanics, Russian Academy of Sciences. The atomic excitation temperature T _a and the population temperature T _e of the electronic states of C2 molecules (both averaged over the jet diameter) were measured from the absolute intensities of the atomic spectral lines and the spectrum of C2 molecules in different generation regimes at gas pressures of 25–140 hPa and anode supply powers of 29–72 kW. The longitudinal and radial profiles of the temperatures were determined for some of these regimes and compared to those obtained from numerical calculations of equilibrium induction plasma flows in the discharge channel. For some generation regimes, the dependences of the averaged (over the line of sight) rotational and vibrational temperatures (T _r and T _v) on the discharge parameters, as well as the radial profiles of these temperatures, were determined from the best fit of the measured and calculated spectra of C₂ molecules (Swan bands). The self-absorption of molecular emission was observed at sufficiently high temperatures and gas pressures, and its influence on the measured values of the molecular temperatures T _e, T _v, and T _r was examined.     

The use of stable isotopes to study ecosystem gas exchange

Stable isotopes are a powerful research tool in environmental sciences and their use in ecosystem research is increasing. In this review we introduce and discuss the relevant details underlying the use of carbon and oxygen isotopic compositions in ecosystem gas exchange research. The current use and potential developments of stable isotope measurements together with concentration and flux measurements of CO₂ and water vapor are emphasized. For these applications it is critical to know the isotopic identity of specific ecosystem components such as the isotopic composition of CO₂, organic matter, liquid water, and water vapor, as well as the associated isotopic fractionations, in the soil-plant- atmosphere system. Combining stable isotopes and concentration measurements is very effective through the use of ”Keeling plots.” This approach allows the identification of the isotopic composition and the contribution of ecosystem, or ecosystem components, to the exchange fluxes with the atmosphere. It also allows the estimation of net ecosystem discrimination and soil disequilibrium effects. Recent modifications of the Keeling plot approach permit examination of CO₂ recycling in ecosystems. Combining stable isotopes with dynamic flux measurements requires precision in isotopic sampling and analysis, which is currently at the limit of detection. Combined with the micrometeorological gradient approach (applicable mostly in grasslands and crop fields), stable isotope measurements allow separation of net CO₂ exchange into photosynthetic and soil respiration components, and the evapotranspiration flux into soil evaporation and leaf transpiration. Similar applications in conjunction with eddy correlation techniques (applicable to forests, in addition to grasslands and crop fields) are more demanding, but can potentially be applied in combination with the Keeling plot relationship. The advance and potential in using stable isotope measurements should make their use a standard component in the limited arsenal of ecosystem-scale research tools. Received: 8 July 1999 / Accepted: 10 January 2000     

华北低丘山地人工林蒸散的季节变化及环境影响要素

蒸散（ET）是生态系统水分平衡和能量平衡的重要组分,中国人工林对区域水分循环及平衡发挥着重要作用。本文基于2007—2008年涡度相关观测资料,分析了华北低丘山地近30年生栓皮栎-刺槐-侧柏人工林生态系统蒸散的变化特征及其环境影响要素。结果表明,2007—2008年实验区气候较常年偏暖、偏旱。ET表现出单峰季节变化特征,秋冬季节较低,春夏季节（4—9月）蒸散旺盛。全年最高值出现在每年5月份,日峰值出现于午后13时左右。2007—2008年平均蒸散量为546.1 mm,降水量为354.1 mm,夏季（7—8月）和冬季（12—1月）的日蒸散量分别为2.19 mm/d和0.44 mm/d。温度是驱动ET季节变化的主要环境因子,饱和差也是影响蒸散季节变化的重要环境要素。土壤含水量对ET季节变化的影响并不显著,有近1/3日数的土壤含水量为0.16—0.18 m3/m3,期间日蒸散量平均值为1.0 mm/d。年蒸散量均高于降水量,蒸散量高于降水量的部分来自深层土壤水分的供给。     

Transpiration rate relates to within‐ and across‐species variations in effective path length in a leaf water model of oxygen isotope enrichment

Stable oxygen isotope ratio of leaf water (δ¹⁸O_L) yields valuable information on many aspects of plant–environment interactions. However, current understanding of the mechanistic controls on δ¹⁸O_L does not provide complete characterization of effective path length (L) of the Péclet effect, – a key component of the leaf water model. In this study, we collected diurnal and seasonal series of leaf water enrichment and estimated L in six field‐grown angiosperm and gymnosperm tree species. Our results suggest a pivotal role of leaf transpiration rate (E) in driving both within‐ and across‐species variations in L. Our observation of the common presence of an inverse scaling of L with E in the different species therefore cautions against (1) the conventional treatment of L as a species‐specific constant in leaf water or cellulose isotope (δ¹⁸O_p) modelling; and (2) the use of δ¹⁸O_p as a proxy for g_s or E under low E conditions. Further, we show that incorporation of a multi‐species L‐E scaling into the leaf water model has the potential to both improve the prediction accuracy and simplify parameterization of the model when compared with the conventional approach. This has important implications for future modelling of oxygen isotope ratios.     

Effects of silicon nutrition on cadmium uptake, growth and photosynthesis of rice plants exposed to low-level cadmium

The effect of silicon (Si) nutrition on low-level cadmium (Cd) toxicity symptoms was investigated in hydroponically-grown rice seedlings (Oryza sativa L.). Silicon (0.0, 0.2, or 0.6 mM) was added when seedlings were 6 or 20 days old representing early (Si^E) or late (Si^L) Si treatment, respectively. Cadmium (0.0 or 2.5 μM) was added when seedlings were 6 days old. Measurements included generation of CO₂ and light response curves; chlorophyll fluorescence analysis; growth; and tissue-element content analysis. Our results showed that low-level Cd treatment generally inhibited growth and photosynthesis. However, the addition of 0.2 or 0.6 mM Si^E or Si^L significantly reduced root- and leaf-Cd content. Consequently, the addition of 0.6 mM Si^L significantly alleviated low-level Cd-induced inhibition of growth. Furthermore, 0.2 mM Si treatment significantly reduced g _s compared to 0.0 or 0.6 mM Si without inhibiting A, especially in +Cd plants, suggesting an increase in instantaneous water-use-efficiency (IWUE). Additionally, in +Cd plants, the addition of 0.6 mM Si^E significantly reduced F _o but increased F _v/F _m, while treatment with 0.2 mM Si^L significantly increased q_P, suggesting an increase in light-use-efficiency. We thus, propose that 0.6 mM Si^L treatment is required for the alleviation of low-level Cd-mediated growth inhibition. Furthermore, we suggest that 0.2 mM Si concentration might be close to the optimum requirement for maximum Si-induced increase in IWUE in rice plants, especially when under low-level Cd-stress. Our results also suggest that Si alleviates low-level Cd toxicity by improving light-use-efficiency.     

不同土壤水分条件下杨树人工林水分利用效率对环境因子的响应

运用涡度相关(Eddy covariance,EC)开路系统和微气象观测系统,于2007年对位于北京市大兴区永定河沙地杨树(Populus euramertcana)人工林与大气间碳、水和能量交换进行了连续测定.通过分析总生态系统生产力(GEP)、蒸发散(ET)以及水分利用效率(WUE=GEP/ET)随相对土壤含水量(REW)的变化趋势,探讨杨树人工林不同土壤水分条件下水分利用效率对气象因子以及下垫面因素的响应,为杨树人工林经营管理提供理论依据.研究结果表明:当REW＜0.1时,GEP和ET受到严重水分胁迫的影响维持在较低水平,环境因子对GEP、ET和WUE的影响较小;当0.1＜REW＜0.4时,GEP和ET随着土壤体积含水量(VWC)的增加而增大,WUE随VWC的增大而减小;REW＞0.4时,气象因子是影响碳固定和水分损耗的主要原因,由于ET对气象因子变化的响应较GEP更为敏感,因此,WUE随空气饱和水汽压差(VPD)的增大而减小.沙地土壤保水能力较差,不能保证土壤水分被植物有效利用,因此当VWC处于5.2%-8.8％(0.1＜REW＜0.4)范围时,碳固定与水分消耗达到最高效率.研究表明杨树人工林WUE随降水变化而变化,未来气候变化和变异有可能影响杨树林耗水和生产力之间的关系.     

Electronic structure,rovibrational, and dipole moment calculations for the AsCl molecule

The potential energy curves of the 19 lowest-lying singlet and triplet electronic states in the ^2S+1Λ^(+/?) representation of the AsCl molecule have been investigated using the complete active space self-consistent field (CASSCF) with multireference configuration interaction (MRCI+Q) method including single and double excitations and with the Davidson correction. The harmonic frequency ω _e, the internuclear distance R _e, the dipole moment, and the electronic energy with respect to the ground state T _e were calculated for the electronic states considered. By using the canonical functions approach, the eigenvalue E _v, the rotational constant B _v, and the abscissae of the turning points R _min and R _max were calculated for the electronic states up to the vibrational level v?=?60. The values obtained in the present work agree well with corresponding values available in the literature for several electronic states. Fifteen new electronic states were investigated here for the first time.     

Estimation of intracellular pH in muscle of fishes from different thermal environments

A technique based on homogenisation of rapidly frozen tissue was used to investigate the regulation of intracellular pH (pH_i) in freshwater and marine fish from diverse environmental temperatures. The following species were held at ambient temperatures of ca. 1°C (Notothenia coriiceps; Antarctica), 5°C (Pleuronectes platessa, Myoxocephalus scorpius; North Sea), and 26°C (Oreochromis niloticus; African lakes). The effects of seasonal acclimatisation to 4, 11 and 18°C were also examined in rainbow trout in the winter, autumn and summer, respectively. Extracellular (whole blood) pH (pH_e) did not follow the constant relative alkalinity relationship, where pH⁺=pOH⁻ for any particular temperature, over a range of 1–26°C (overall δpH_e/δT=0.009±0.002 U °C⁻¹; P<0.001), apparently being regulated by ionic fluxes and ventilation. Intracellular pH (pH_i) was also regulated independently of pN(=0.5 pK water) in all species of fish examined. The inverse relationship between pH_i and environmental temperature gave an overall δpH_i/δT of −0.010±0.001 U °C⁻¹ (for both white and red muscle) and −0.004±0.003 U °C⁻¹ (cardiac muscle). However, between 1 and 11°C δpH_i/δT was much higher (P<0.001), −0.022±0.003 U °C⁻¹ (white muscle) and −0.022±0.004 U °C⁻¹ (red muscle). The possible adaptive roles for these different acid–base responses to environmental temperature variation among tissues and species, and the potential difficulties of estimating pH_i, are discussed.     

Transpiration in a eucalypt plantation and a savanna in Venezuela

In Venezuela 30,000?km² of land is covered by savannas, of which 410,000?ha have been planted with several species and hybrids of Eucalyptus for lumber and pulp production. Popular concern about possible diminutions in water availability of reservoirs near eucalypt plantations prompted our interest in measuring water use by these trees. Since these savannas are markedly seasonal, the response of species to seasonal drought is important. We aimed to compare the seasonal changes in single-leaf and whole-plant transpiration in a seasonally dry savanna with that of trees of E. urophylla in an experimental plantation. We also examined the seasonal changes in xylem water potential and stomatal response to air water-vapour saturation deficit (D). Transpiration in eucalypts and the dominant savanna species Trachypogon vestitus and Curatella americana was evaluated using measurements of leaf gas exchange in all three species, sap flux in eucalypts, microclimatic variables and allometric and photometric determinations of green area. In E. urophylla and T. vestitus, but not in C. americana, stomatal conductance (g _s) proved sensitive to D. Integrated values of daily courses of transpiration rate were scaled to one ha in a preliminary approach to estimating ecosystem transpiration (E _ha). The E _ha of the savanna (the sum of E _ha of T. vestitus and C. americana) was on average 2.4 times that of eucalypts during the daytime; when nocturnal eucalypt transpiration was included, the value was 1.9. The evapotranspiration calculated by the Penman–Montieth equation (ET_c) of eucalypts was lower than the savanna all year round. The reference crop ET (ET_o) varied little throughout the seasons, the highest value occurring in March. The ratio E _ha/ET_o for the savanna was on average near one during the dry season and almost two during the rainy season; the corresponding value for E. urophylla was 0.6 for both seasons. The ratio E _ha/ET_c was on average 0.8 for the species and the savanna. The cumulative E _ha for the days of measurements was higher in the savanna than in the eucalypts during the daytime (39.8 and 17.3?mm, respectively), as was the cumulative ET_c (37.5 vs. 20.3?mm). Measured and calculated cumulative ET in eucalypts, including nocturnal values, were 22.0 and 28.4?mm, respectively. At the leaf level, both eucalypts and trees of C. americana apparently may have accessed water from deep horizons, since their values of Ψ changed less seasonally than in T. vestitus. At the ecosystem level, the species that presented the largest changes in transpiration was T. vestitus, which markedly increased savanna transpiration during the rainy season. Our results suggest that, for the days of this study, and considering the environmental conditions of the ecosystems studied, the type of measurements and the scaling procedures, stands of E. urophylla transpire less water than the savanna.     

Daily and annual patterns of thermoregulation in painted turtles (Chrysemys picta marginata) living in a thermally variable marsh in Northern Michigan

The capacity for an ectothermic reptile to thermoregulate has implications for many components of its life history. Over two years, we studied thermoregulation in a population of Midland painted turtles (Chrysemys picta marginata) in a shallow, thermally variable wetland during summer in Northern Michigan. Mean body temperature (T_b) of free-ranging turtles was greater in 2008 (25.8 °C) than in 2010 (19.7 °C). Laboratory determined thermoregulatory set point (T_set) ranged from 25 °C (T_set-min) to 31 °C (T_set-max) and was lower during the fall (17–26 °C). Deviations of T_b distributions from field measured operative temperatures (T_e) and indices of thermoregulation indicated that C. picta marginata were capable of a limited degree of thermoregulation. Operative temperatures and thermal quality (d_e=|T_set-min−T_e| and |T_e−T_set-max|) cycled daily with maximal thermal quality occurring during late morning and late afternoon. The accuracy of thermoregulation (d_b=|T_set-min−T_b| and |T_b−T_set-max|) was maximal (d_b values were minimal) as T_b declined and traversed T_set during the late afternoon–early evening hours and was higher on cloudy days than on sunny days because relatively low T_e values decreased the number of T_b values that were above T_set. Our index of thermal exploitation (E_x=frequency of T_b observations within T_set) was 36%, slightly lower than that reported for an Ontario population of C. picta marginata. Regression of d_b (thermal accuracy) on d_e (thermal quality) indicated that turtles invested more in thermoregulation when thermal quality was low and when water levels were high than when they were low. There were no intersexual differences in mean T_b throughout the year but females had relatively high laboratory determined T_b values in the fall, perhaps reflecting the importance of maintaining ovarian development prior to winter.     

Thyroid Hormone Treatments Differentially Affect the Temperature Kinetics Properties of FoF1 ATPase and Succinate Oxidase as well as the Lipid/Phospholipid Profiles of Rat Kidney Mitochondria: A Correlative Study

Effect of thyroidectomy (Tx) and subsequent treatment with 3,5,3′-triiodo-l-thyronine (T₃) or replacement therapy (T_R) with T₃ + l-thyroxine (T₄) on the temperature kinetics properties of FoF₁ adenosine triphosphatase (ATPase, ATP synthase, H⁺-translocating ATP synthase EC 3.6.3.14) and succinate oxidase (SO) and on the lipid/phospholipid makeup of rat kidney mitochondria were examined. Tx lowered ATPase activity, which T₃ treatment restored. SO activity was unchanged in Tx but decreased further by T₃ treatment. T_R restored both activities. The energies of ATPase activation in the high and low temperature ranges (E _H and E _L) increased in the Tx and T₃ animals with decrease in phase transition temperature (Tt). T_R restored E _H and E _L but not Tt to euthyroid levels. E _H and E _L of SO decreased in Tx animals. T₃ and T_R restored E _H whereas E _L was restored only in the T_R group; Tt increased in both groups. Total phospholipid and cholesterol contents decreased significantly in Tx and T₃-treated animals. In Tx animals, sphingomyelin (SPM) and phosphatidylcholine (PC) components decreased, while phosphatidylserine (PS) and diphosphatidylglycerol components increased. T₃ and T_R treatments caused decreases in SPM, phosphatidylinositol and PS. PC and phosphatidylethanolamine (PE) increased in the T₃ group. T_R resulted in increased lysophospolipids and PE. Changes in kinetic parameters of the two enzymes were differently correlated with specific phospholipid components. Both T₃ and T_R regimens were unable to restore normal membrane structure-function relationships.     

The effect of sodium bicarbonate supplementation on growth and biochemical composition of marine microalgae cultures

The addition of bicarbonate (NaHCO₃; 0, 1, or 2 g L^?1) to microalgal cultures has been evaluated for two species (Tetraselmis suecica and Nannochloropsis salina) in respect of growth and biochemical composition. In batch cultures, addition of bicarbonate (1 g L^?1) resulted in significantly (P?<?0.05) higher final mean cell abundances for both species. No differences in specific growth rates (SGRs) were recorded for T. suecica between treatments; however, increasing bicarbonate addition decreased SGR values in N. salina cultures. Bicarbonate addition (1 g L^?1) significantly improved nitrate utilisation from the external media and photosynthetic efficiency (F _v /F _m ) in both species. For both T. suecica and N. salina, bicarbonate addition significantly increased the cellular concentrations of total pigments (3,432–3,587 and 19–37 fg cell^?1, respectively) compared to cultures with no additional bicarbonate (1,727 and 11 fg cell^?1, respectively). Moreover, final concentrations of total cellular fatty acids in T. suecica and N. salina cultures supplemented with 2 g L^?1 bicarbonate (7.6?±?1.2 and 1.8?±?0.1 pg cell^?1, respectively) were significantly higher than those cells supplemented with 0 or 1 g L^?1 bicarbonate (3.2–3.5 and 0.9–1.0 pg cell^?1, respectively). In nitrate-deplete cultures, bicarbonate addition caused species-specific differences in the rate of cellular lipid production, rates of change in fatty acid composition and final lipid levels. In summary, the addition of sodium bicarbonate is a viable strategy to increase cellular abundance and concentrations of pigments and lipids in some microalgae as well as the rate of lipid accumulation in nitrate-deplete cultures.     

Asymmetric response of Amazon forest water and energy fluxes to wet and dry hydrological extremes reveals onset of a local drought-induced tipping point

Understanding the effects of intensification of Amazon basin hydrological cycling—manifest as increasingly frequent floods and droughts—on water and energy cycles of tropical forests is essential to meeting the challenge of predicting ecosystem responses to climate change, including forest “tipping points”. Here, we investigated the impacts of hydrological extremes on forest function using 12+ years of observations (between 2001–2020) of water and energy fluxes from eddy covariance, along with associated ecological dynamics from biometry, at the Tapajós National Forest. Measurements encompass the strong 2015–2016 El Niño drought and La Niña 2008–2009 wet events. We found that the forest responded strongly to El Niño-Southern Oscillation (ENSO): Drought reduced water availability for evapotranspiration (ET) leading to large increases in sensible heat fluxes (H). Partitioning ET by an approach that assumes transpiration (T) is proportional to photosynthesis, we found that water stress-induced reductions in canopy conductance (G_s) drove T declines partly compensated by higher evaporation (E). By contrast, the abnormally wet La Niña period gave higher T and lower E, with little change in seasonal ET. Both El Niño-Southern Oscillation (ENSO) events resulted in changes in forest structure, manifested as lower wet-season leaf area index. However, only during El Niño 2015–2016, we observed a breakdown in the strong meteorological control of transpiration fluxes (via energy availability and atmospheric demand) because of slowing vegetation functions (via shutdown of G_s and significant leaf shedding). Drought-reduced T and G_s, higher H and E, amplified by feedbacks with higher temperatures and vapor pressure deficits, signaled that forest function had crossed a threshold, from which it recovered slowly, with delay, post-drought. Identifying such tipping point onsets (beyond which future irreversible processes may occur) at local scale is crucial for predicting basin-scale threshold-crossing changes in forest energy and water cycling, leading to slow-down in forest function, potentially resulting in Amazon forests shifting into alternate degraded states.