Tidal Influence on Spatial Dynamics of Leopard Sharks, Triakis semifasciata, in Tomales Bay, California

We used ultrasonic telemetry to determine the movement directions and movement rates of leopard sharks, Triakis semifasciata, in Tomales Bay, California. To analyze tide and time of day effects, we surgically implanted transmitters in the peritoneal cavities of one male and five female leopard sharks, which we located during summer for three to five sampling sessions lasting 12 to 24h each. All leopard sharks showed strong movement direction patterns with tide. During incoming tides, sharks moved significantly (p<0.0001) towards the inner bay, apparently to exploit the extensive inner bay muddy littoral zones' food resources. On outgoing tides, sharks showed significant (p<0.0001) movements towards the outer bay. During high tide, there was no discernible pattern to their movements (p=0.092). Shark movement rates were significantly (p<0.0001) greater during dark periods (mean±SE: 10.5±1.0m min^–1), compared with fully lighted ones (6.7±0.5m min^–1). Movement rates of longer sharks tended to be greater than those of shorter ones (range means±SE: 5.8±0.6m min^–1 for the 91cm shark, to 12.8±1.6m min^–1 for the 119cm shark), but the leopard sharks' overall mean movement rate (8.1±0.5m min^–1) was slower than other (more pelagic) sharks.     

Effects of some extrinsic factors on the respiratory metabolism of the freshwater leech,poecilobdella viridis (blanchard): desiccation and temperature

The influence of desiccation and temperature on the respiratory metabolism of P. viridis have been investigated. There was a significant (p < 0.05) downfall in the respiratory rates as the period of desiccation increased, but for after 18 hours where it was enhanced significantly. The respiration augmented significantly (p < 0.03) when the temperature of the medium increased. Q₁₀ was significantly high at 32–28°C and was low between 35 and 32°C and 20–10°C Functional significance of these changes to the leeches in combating environmental hazards is briefly discussed.     

Temperature Dependence of Voltage-gated H+ Currents in Human Neutrophils,Rat Alveolar Epithelial Cells,and Mammalian Phagocytes

H⁺ currents in human neutrophils, rat alveolar epithelial cells, and several mammalian phagocyte cell lines were studied using whole-cell and excised-patch tight-seal voltage clamp techniques at temperatures between 6 and 42°C. Effects of temperature on gating kinetics were distinguished from effects on the H⁺ current amplitude. The activation and deactivation of H⁺ currents were both highly temperature sensitive, with a Q ₁₀ of 6–9 (activation energy, E _a, ≈ 30–38 kcal/mol), greater than for most other ion channels. The similarity of E _a for channel opening and closing suggests that the same step may be rate determining. In addition, when the turn-on of H⁺ currents with depolarization was fitted by a delay and single exponential, both the delay and the time constant (τ_act) had similarly high Q ₁₀. These results could be explained if H⁺ channels were composed of several subunits, each of which undergoes a single rate-determining gating transition. H⁺ current gating in all mammalian cells studied had similarly strong temperature dependences. The H⁺ conductance increased markedly with temperature, with Q ₁₀ ≥ 2 in whole-cell experiments. In excised patches where depletion would affect the measurement less, the Q ₁₀ was 2.8 at >20°C and 5.3 at <20°C. This temperature sensitivity is much greater than for most other ion channels and for H⁺ conduction in aqueous solution, but is in the range reported for H⁺ transport mechanisms other than channels; e.g., carriers and pumps. Evidently, under the conditions employed, the rate-determining step in H⁺ permeation occurs not in the diffusional approach but during permeation through the channel itself. The large E _a of permeation intrinsically limits the conductance of this channel, and appears inconsistent with the channel being a water-filled pore. At physiological temperature, H⁺ channels provide mammalian cells with an enormous capacity for proton extrusion.     

降雨对草地土壤呼吸季节变异性的影响

利用土壤碳通量自动观测系统(LI-8150)对呼伦贝尔草原在自然降雨条件下的土壤呼吸作用进行了野外定位连续观测,研究结果表明:降雨对土壤呼吸作用存在激发效应和抑制效应,降雨发生后1-2 h内土壤呼吸速率可增加约1倍,当单次或者连续降雨累积量大于7-8 mm,或土壤含水量大于29%-30%时,降雨对土壤呼吸会产生明显的抑制作用。土壤呼吸的激发效应往往体现在次日,表现为次日平均土壤呼吸速率的显著升高;而抑制效应则在当日即可体现出来,表现为观测当日平均土壤呼吸速率的明显下降。土壤呼吸季节变异性与降雨频率和降雨强度密切相关,在降雨量一定的情况下,较低的降雨频率和较高的降雨强度会增加土壤呼吸的变异性。呼伦贝尔草甸草原而言,在生长季土壤平均含水量为16.5%时,土壤呼吸的温度敏感性值(Q₁₀)为2.12;而平均土壤含水量为26%时,Q₁₀值为2.82,明显高于前者,土壤含水量与Q₁₀之间存在正相关关系。降雨导致土壤呼吸的激发效应和抑制效应交替发生,使草地土壤呼吸的季节变异性增加,降雨格局变化必然会对草地碳循环和碳通量特征产生深刻影响。     

封育对羊草草地土壤碳矿化激发效应和温度敏感性的影响

土壤碳矿化(或土壤异养呼吸)的温度敏感性和激发效应是深入揭示土壤呼吸控制机理及其对未来气候变化响应与适应的重要研究方向。该文以自由放牧(FG0)、封育11年(FG11)、封育31年(FG31)的羊草(Leymus chinensis)草地为研究对象, 通过0、5、10、15、20、25 ℃培养, 探讨了封育对羊草草地土壤碳矿化激发效应和温度敏感性的影响。结果表明: 封育年限、添加葡萄糖、培养温度和培养时间对土壤碳矿化速率均具有显著的影响, 不同因素间存在显著的交互效应(p < 0.000 1)。FG0的羊草草地土壤碳矿化累积量显著高于FG11和FG31的, 在添加葡萄糖处理下也呈现相同的趋势。长期封育降低了羊草草地土壤碳矿化的激发效应。在添加葡萄糖后, 培养前7天的土壤碳矿化的激发效应随温度增加而增加, 增加2.28-9.01倍; 在整个56天培养期间, 激发效应介于2.21-5.10倍, 最高值出现在10或15 ℃。土壤碳矿化速率可用经典的指数方程来表示, FG0草地的土壤碳矿化的温度敏感性指数(Q₁₀)大于长期封育草地(FG11和FG31); 与未添加处理相比, 添加葡萄糖显著增加了土壤碳矿化速率的温度敏感性, 即在添加葡萄糖后土壤微生物呼吸受温度的影响更大。长期封育会降低羊草草地土壤的碳矿化速率、温度敏感性和激发效应, 从而降低土壤碳周转速率和释放速率, 使内蒙古地区长期封育草地仍然具有碳固持能力。     

Alteration of Oxygen Consumption and Energy Metabolism During Repetitive Exposure of Mice to Hypoxia

Changes in oxygen consumption, body temperature and energy metabolism were studied while mice were repeatedly exposed to a sealed environment. The average tolerance limits of environmental oxygen level (vol%) and the average oxygen consumption rates (ml/g.min) were exponentially decreased and the average body rectal temperatures (°C) were linearly declined while the average tolerable times (min) to hypoxia were linearly increased as animals were repeatedly exposed to hypoxia for 5 runs. The average survival times (min) in sealed environments after administration of normal saline, iodoacetic acid, malonic acid, potassium cyanide, and potassium cyanide plus iodoacetic acid in group exposed repeatedly to hypoxia for three runs were, respectively, 3.1, 3.9, 1.4, 2.6, and 2.8 times those of the control groups that had corresponding administration of the different chemicals, but no exposure to hypoxia. The results indicate that progressive increase in hypoxia tolerance is related to progressively lower rate of oxygen consumption and heat production, and the lowered energy requirement during repetitive exposure to hypoxia is achieved mainly via pathways of the respiratory chain and glycolysis.     

全球陆地生态系统光合作用与呼吸作用的温度敏感性

基于全球647套通量数据,定量分析了全球尺度下生态系统光合作用和呼吸作用的温度敏感性(Q10)随纬度、气候和植被的分布规律。结果表明:在全球尺度下,光合作用和呼吸过程的温度敏感性(Q10,G和Q10,R)都随纬度的升高而增加,其中Q10,G和Q10,R的均值分别为3.99±0.21和2.28±0.074。除热带多树草原、常绿落叶林外,Q10,G均大于Q10,R值。不同植被类型的温度敏感性存在显著性差异,表现为:针叶林阔叶林;落叶林常绿林,其中生态系统的季节性变异是造成差异的主要原因。当植被类型和纬度区域共同影响Q10值时,植被类型对Q10值的总变异贡献更大。气候类型对Q10,G和Q10,R都有显著影响。在气候带上,干旱带的Q10,G最小,而冷温带的Q10,G最高。不同气候类型下(除温带草原气候外)的Q10,G都大于Q10,R。在极端条件下,温度可能不在是主导因素,而水分对温度敏感性的影响不可忽略,今后的研究需要更多的关注生态系统温度敏感性对水分变化的响应。     

Temperature effect on maintenance and growth respiration coefficients of young, field-grown hinoki cypress (Chamaecyparis obtusa)

Respiration measurements were made on the entire aboveground parts of young, field-grown hinoki cypress (Chamaecyparis obtusa) trees at monthly intervals over a 5-year period, to examine the effect of temperature on maintenance and growth respiration coefficients. The respiration rate of the trees was grouped on a monthly basis and then partitioned into maintenance and growth components. The maintenance respiration coefficient increased exponentially with air temperature. The maintenance respiration coefficient at a temperature of 0°C and itsQ ₁₀ value were 0.205 mmol CO₂ g⁻¹ d.w. month⁻¹ and 1.81, respectively. The growth respiration coefficient, which was virtually independent of temperature, had a mean value of 38.06±1.95 (SE) mmol CO₂g⁻¹ d.w. The growth rate increased exponentially with increasing temperature up to a peak at around 18°C, and thereafter declined, thereby resulting in the growth respiration rate being increasingly less sensitive to increasing air temperature. The reported decreases in theQ ₁₀ value of total respiration with increasing air temperature is due to the way in which the growth component of respiration responds to temperature.     

Effects of Temperature on Circadian Clock and Chronotype: An Experimental Study on a Passerine Bird

Daily schedules of many organisms, including birds, are thought to affect fitness. Timing in birds is based on circadian clocks that have a heritable period length, but fitness consequences for individuals in natural environments depend on the scheduling of entrained clocks. This chronotype, i.e., timing of an individual relative to a zeitgeber, results from interactions between the endogenous circadian clock and environmental factors, including light conditions and ambient temperature. To understand contributions of these factors to timing, we studied daily activity patterns of a captive songbird, the great tit (Parus major), under different temperature and light conditions. Birds were kept in a light (L)-dark (D) cycle (12.5?L:11.5 D) at either 8°C or 18°C with ad libitum access to food and water. We assessed chronotype and subsequently tested birds at the same temperature under constant dim light (LL_dim) to determine period length of their circadian clock. Thermal conditions were then reversed so that period length was measured under both temperatures. We found that under constant dim light conditions individuals lengthened their free-running period at higher temperatures by 5.7?±?2.1?min (p?=?.002). Under LD, birds kept at 18°C started activity later and terminated it much earlier in the day than those kept under 8°C. Overall, chronotype was slightly earlier under higher temperature, and duration of activity was shorter. Furthermore, individuals timed their activities consistently on different days under LD and over the two test series under LL_dim (repeatability from .38 to .60). Surprisingly, period length and chronotype did not show the correlation that had been previously found in other avian species. Our study shows that body clocks of birds are precise and repeatable, but are, nonetheless, affected by ambient temperature. (Author correspondence: marina.lehmann@uni-konstanz.de)     

CO2 efflux under different grazing managements on subalpine meadows of Shangri-La, Northwest Yunnan Province, China

Soil carbon stored on the Tibetan Plateau appears to be stable under current temperature, but it may be sensitive to global warming. In addition, different grazing systems may alter carbon emission from subalpine meadow ecosystems in this region. Using a chamber-closed dynamic technique, we measured ecosystem respiration (ER) and soil respiration (SR) rates with an infrared gas analyzer on a perennial grazing meadow (PM) and a seasonal grazing meadow (SM) of Shangri-La in the Hengduan Mountain area. Both PM and SM showed strong unimodal seasonal variations, with the highest rates in July and the lowest in January. Significant diurnal variations in respiration were also observed on PM, affected mainly by air and soil temperatures, with the highest rates at 14:00 and the lowest before dawn. Both ER and SR rates were higher on PM than on SM from June to October, suggesting that the higher grazing pressure on PM increased respiration rates on subalpine meadows. The exponential model F = ae^{bT<,/sup> of soil temperature (T) explained the variation in respiration better than the model of soil moisture (W) (R2 = 0.50–0.78, P < 0.0001), while the multiple model F = aebT<,/sup>Wc gave better simulations than did single-factor models (R2 = 0.56–0.89, P < 0.0001). Soil respiration was the major component of ER, accounting for 63.0%–92.7% and 47.5%–96.4% of ER on PM and SM, respectively. Aboveground plant respiration varied with grass growth. During the peak growing season, total ecosystem respiration may be dominated by this above-ground component. Long-term (annual) Q₁₀ values were about twice as large as short-term (one day) Q₁₀. Q₁₀ at different time scales may be controlled by different ecological processes. The SM had a lower long-term Q₁₀ than did the PM, suggesting that under increased temperature, soil carbon may be more stable with reduced grazing pressure.}     

Dependence of the Q10 values on the depth of the soil temperature measuring point

The parameter Q₁₀ is commonly used to express the relationship between soil CO₂ efflux and soil temperature. One advantage of this parameter is its application in a model expression of respiration losses of different ecosystems. Correct specification of Q₁₀ in these models is indispensable. Soil surface CO₂ efflux and soil temperature at different depths were measured in a 21-year-old Norway spruce stand and a mountain grassland site located at the Experimental Ecological Study Site Bily Kriz, Beskydy Mts. (NE Czech Republic), using automated gasometric systems. A time-delay and goodness-of-fit between soil CO₂ efflux and soil temperature at different measuring depths were determined. Wide ranges of values for the time-delay of CO₂ efflux in response to temperature, Q₁₀ and the determination coefficient (R²) between CO₂ efflux and temperature were obtained at the both sites. The values of Q₁₀ and the CO₂ time-delay increased with depth, while the R² of the CO₂-temperature relationship significantly decreased. Soil temperature records obtained close to the soil surface showed the highest values of R² and the lowest value of the time-delay at both sites. Measurement of soil temperature at very shallow soil layer, preferably at the soil surface, is highly recommended to determine useable values of Q₁₀. We present a new procedure to normalize Q₁₀ values for soil temperatures measured at different depths that would facilitate comparison of different sites.     

土壤呼吸的温度敏感性——全球变暖正负反馈的不确定因素

基于模型模拟结果表明,全球变暖与大气CO2浓度增加将形成正反馈关系,这种正反馈效应将明显加速21世纪的气候变暖。然而,这些模拟模型都基于一个重要假设,即不同平均驻留时间的土壤有机质分解具有相同的温度敏感性(Q10)。这一假设与酶动力学理论相悖,而且不同学者对不同质量土壤有机质分解温度敏感性的差异的认识存在严重分歧,所以,全球变暖与大气CO2浓度增加的正反馈关系的显著性仍值得商榷。围绕土壤呼吸的温度敏感性问题进行了讨论和评述,涉及1)土壤有机质分解温度敏感性争论的焦点问题;2)通过经验模型曲线拟合估计Q10值存在的分歧及Q10变异的机理解释;3)实验室土壤培养实验估计Q10值存在的问题;4)土壤培养实验中Q10值计算方法的改进。进一步深化有关土壤有机质分解温度敏感性不确定性的认识,将为今后土壤呼吸及其对气候变化响应的相关研究提供参考。     

Combined efficacy of tamoxifen and coenzyme Q10 on the status of lipid peroxidation and antioxidants in DMBA induced breast cancer

An increasing amount of experimental and epidemiological evidence implicates the involvement of oxygen derived radicals in the pathogenesis of cancer development. It is well known that chemical carcinogenesis is multistage process. Free radicals are found to be involved in both initiation and promotion of multistage carcinogenesis. Tamoxifen (TAM) is a potent antioxidant and a non-steroidal antiestrogen drug most used in the chemotherapy and chemoprevention of breast cancer. Besides its anticarcinogenic potential, it also produces some adverse toxic side effects, while taken for a long time. In order to minimise the side effects and to improve the antioxidant efficacy of tamoxifen, coenzyme Q₁₀ (CoQ₁₀) was added. Hence the present study was designed to investigate the combined efficacy of TAM along with CoQ₁₀ in 7, 12 dimethyl benz(a)anthracene (DMBA) induced peroxidative damage in rat mammary carcinoma. The experimental setup comprised of one control and five experimental groups and it was carried out in adult female Sprague-Dawley rats. Mammary carcinoma was induced by oral administration of DMBA (25 mg kg^–1 body wt) and the treatment was started by the oral administration of TAM (10 mg kg^–1 body wt day^–1) and CoQ₁₀ (40 mg kg^–1 body wt day^–1) dissolved in olive oil and continued for 28 days. Rats induced with DMBA showed a decline in the thiol capacity of the cell accompanied by high malondialdehyde content levels along with lowered activities of antioxidant status (superoxide dismutase, catalase, glutathione peroxidase and reduced glutathione). In contrast, glutathione metabolising enzymes (glutathione reductase, glucose-6-phosphate dehydrogenase and glutathione-S-transferase) were increased significantly in chemically induced carcinoma bearing rats. Administration of TAM along with CoQ₁₀ restored the activities to a significant level thereby preventing cancer cell proliferation. This study highlights the increased antioxidant enzyme activities in relation to the susceptibility of cells to carcinogenic agents and the response of tumour cells to the chemotherapeutic agents.     

放牧对若尔盖高寒草甸土壤氮矿化及其温度敏感性的影响

过度放牧和气候暖干化是若尔盖高寒草甸面临的严峻生态问题,它对土壤氮矿化过程的影响将在某种程度上决定高寒草甸生态系统的氮素利用状况。基于野外放牧实验,(禁牧(CK)、轻度放牧(L)、中度放牧(M)、重度放牧(H)),通过室内培养方法(5、10、15、20、25℃),探讨了不同放牧强度对若尔盖高寒草甸土壤氮矿化及其温度敏感性的影响。实验结果表明:放牧增加了土壤硝化速率和净氮矿化速率,其整体趋势为LMHCK。培养温度较低时(5—10℃),温度升高对硝化和净氮矿化速率无显著影响,而培养温度较高时(15—25℃),温度升高显著增加了硝化和净氮矿化速率。土壤硝态氮和无机氮积累量随培养时间增长显著增加,而铵态氮无显著增长。此外,放牧显著提高了土壤氮矿化的温度敏感性,重度放牧样地的土壤具有最高的氮矿化温度敏感性(Q10=2.72)。上述结果预示着在未来温度升高情景下,重度放牧将使土壤氮矿化速率的增速更快,短期内将通过提高氮的可利用性促进植物生长,但长远而言可能加速土壤氮素流失,从而对植物生长和高寒草甸生态系统结构与功能造成负反馈效应。     

Age and Growth of the Whiskery Shark, Furgaleus macki, from Southwestern Australia

Age and growth of the whiskery shark, Furgaleus macki, from southwestern Australia were examined using vertebral ageing and tag-recapture data. The readability of bands on the vertebral centra varied markedly between individuals. Four readers were used to make band counts, with the most experienced reader having the lowest index of average percent error and the highest level of agreement with final counts. Marginal increment analysis indicated that opaque bands form in January. With parturition occurring from August to October, size data suggests that the first band is probably formed 15–17 months after birth. The age at maturity was estimated to be 4.5 years for males, and 6.5 years for females. The oldest male was 10.5 years, and oldest female was 11.5 years. Von Bertalanffy growth parameters for males were L =121.5cm fork length, K=0.423 year^–1, t ₀=–0.472 years, were L =120.7cm fork length, K=0.369 year^–1, t ₀=–0.544 years for females, and were L =118.1cm fork length, K=0.420 year^–1, t ₀=–0.491 years for combined sexes. Data from a tag recapture study were analysed using a maximum likelihood method to verify the estimates of growth parameters from vertebral ageing. Von Bertalanffy growth parameters from the tag recapture study were L =128.2cm fork length, K=0.288 year^–1, t ₀=–0.654 years. The two methods of estimating growth parameters produced similar results, with rapid growth until approximately 5 years of age, after which there was little increase in length.     

Long-Term Effects of Elevated CO2 on Woody Tissues Respiration of Norway Spruce Studied in Open-Top Chambers

In an open-top chamber experiment located in a mountain stand of 14-years-old Norway spruce (Picea abies [L.] Karst.), trees were continuously exposed to either ambient CO₂ concentration (A), or ambient + 350 µmol mol^–1 (E) over four growing seasons. Respiration rates of different woody parts (stem, branches, coarse roots) were measured during the last growing season. The calculated increase in the respiration rate related to a 10 °C temperature change (Q₁₀) was different in stem compared to branches and roots. Differences between the E and A variants were statistically significant only for roots in the autumn. Stem maintenance respiration (R_Ms) measured in April and November (periods of no growth activity) were not different. The stem respiration values (R_s) were recalculated to a standard temperature of 15 °C to estimate the seasonal course. The obtained R_s differed significantly between used variants during July and August. At the end of the season, R_s in E decreased slower than in A, indicating some prolongation of the physiological activity under the elevated CO₂ concentration. The total stem respiration carbon losses for the investigated growing season (May – September) were higher for A (2.32 kg(C) m^–2 season^–1) compared to E (2.12 kg(C) m^–2 season^–1). The respiration rates of the whorl branches (R_b) were lower compared with the stem respiration but not significantly different between the used variants. The root respiration rate was increased in E variant.     

模拟氮沉降对石栎和苦槠幼苗土壤呼吸的影响

用LI-8100开路式土壤碳通量测量系统测定模拟氮沉降4种不同处理水平(0、60、120\,240 kg · hm^-2 · a^-1)下石栎(Lithocarpus glabra)和苦槠(Castanopsis sclerophylla)幼苗的土壤呼吸速率及土壤温度、含水量对其土壤呼吸的影响。结果表明,氮沉降对土壤呼吸的影响根据施氮水平和幼苗的种类不同而异。低氮(60 kg · hm^-2 · a^-1)处理下石栎和苦槠的土壤呼吸速率平均值分别为(4.014±0.812)μmol · m^-2 · s^-1和(5.170±0.689)μmol · m^-2 · s^-1,比对照组(0 kg · hm^-2 · a^-1)土壤呼吸速率平均值(3.802±0.948)μmol · m^-2 · s^-1和(3.557±0.906)μmol · m^-2 · s^-1分别高5%和45%;两树种在中、高氮处理下均出现对土壤呼吸明显的抑制。其中石栎中、高氮实验组的土壤呼吸速率分别为(2.653±0.681)μmol · m^-2 · s^-1、(2.592±0.736)μmol · m^-2 · s^-1, 比对照组低27%和29%。苦槠中、高氮实验组的土壤呼吸速率为(3.563±0.402)μmol · m^-2 · s^-1、(3.466±0.994)μmol · m^-2 · s^-1, 比对照组低7%和8%;石栎在高氮(240 kg · hm^-2 · a^-1)处理水平下,其土壤呼吸速率同10cm土壤温度之间呈现显著的指数关系(R²=0.811,P=0.001),而在低、中氮实验均未发现有明显指数关系。苦槠各处理水平下其土壤呼吸与土壤温度之间均未发现有明显的指数关系;在土壤呼吸与5cm土壤含水量的相关性方面,仅有苦槠高氮实验组表现出明显的二次方程关系(R²=0.722),而其低、中氮实验组及石栎各实验组均未有明显的相关性;与单因素(温度、含水量)拟合它们与土壤呼吸速率的方程相比,多元回归分析得到的土壤呼吸速率同土壤温度和含水量之间的拟合方程在P=0.05水平上能更好地解释土壤呼吸的变化情况。石栎和苦槠在氮沉降处理下的土壤呼吸温度系数Q₁₀值分别为2.29、1.95、1.59和1.46、1.41、1.76,同对照组2.64和1.78相比,均有明显降低,且两者Q₁₀值的变化分别呈递减和先减小后增大的趋势,表明氮沉降是影响石栎和苦槠土壤CO₂通量的一个重要因素。