Host identification by Schistosoma japonicum cercariae

Attachment, the first phase of host identification by Schistosoma japonicum cercariae, can occur in 2 different ways. Cercariae clinging to the water surface simply swing around and transfer to the host skin. Free-swimming cercariae behave like S. mansoni: upon touching a substrate, they switch from tailward to forward movement, swim in an arc, and attach to it with the penetration organ. Neither type of attachment is influenced by chemical, thermal, or specific mechanical stimuli from the host. The second phase, remaining on the host, requires a solid hydrophobic surface and seems to depend only on the cercaria's ability to cling to it. This phase is not influenced by chemical or thermal stimuli. The third phase, creeping across the host surface, is independent of chemical and mechanical stimuli. Cercariae migrate in thermal gradients to a preferred temperature of 37 +/- 3 C and then attempt to penetrate. Penetration, the fourth phase, was evoked by human skin surface lipids. The free fatty acid (FA) fraction was identified as exclusively stimulating components. Saturated FA's were effective at chain lengths between 10 and 14 carbon atoms (pH 7.0), and unsaturated FA's were effective at longer chains and their activity increased with increasing number of double bonds. Dog skin surface components did not stimulate cercarial penetration, which can be attributed to the lack of free FA's. A temperature of 32-40 C also stimulated penetration responses, which might be the main stimulus in animal hosts, whose skin surfaces contain no or only a few free FA's. FA's and heat evoked a transformation of cercarial tegument simultaneous with penetration behavior, making the organisms osmotically sensitive. The host identification of S. japonicum cercariae is very nonspecific compared with the differentiated host recognition of S. mansoni.     

Antagonistic effects of growing season and autumn temperatures on the timing of leaf coloration in winter deciduous trees

Autumn phenology remains a relatively neglected aspect in climate change research, which hinders an accurate assessment of the global carbon cycle and its sensitivity to climate change. Leaf coloration, a key indicator of the growing season end, is thought to be triggered mainly by high or low temperature and drought. However, how the control of leaf coloration is split between temperature and drought is not known for many species. Moreover, whether growing season and autumn temperatures interact in influencing the timing of leaf coloration is not clear. Here, we revealed major climate drivers of leaf coloration dates and their interactions using 154 phenological datasets for four winter deciduous tree species at 89 stations, and the corresponding daily mean/minimum air temperature and precipitation data across China's temperate zone from 1981 to 2012. Results show that temperature is more decisive than drought in causing leaf coloration, and the growing season mean temperature plays a more important role than the autumn mean minimum temperature. Higher growing season temperature and lower autumn minimum temperature would induce earlier leaf coloration date. Moreover, the mean temperature over the growing season correlates positively with the autumn minimum temperature. This implies that growing season mean temperature may offset the requirement of autumn minimum temperature in triggering leaf coloration. Our findings deepen the understanding of leaf coloration mechanisms in winter deciduous trees and suggest that leaf life‐span control depended on growing season mean temperature and autumn low temperature control and their interaction are major environmental cues. In the context of climate change, whether leaf coloration date advances or is delayed may depend on intensity of the offset effect of growing season temperature on autumn low temperature.     

Effects of temperature on survival,infectivity and in vitro encystment of the cercariae of Echinostoma caproni

The effects of temperature on survival, infectivity and in vitro encystment of Echinostoma caproni cercariae in artificial spring water (ASW) were studied. Effects of aging cercariae in ASW at various temperatures showed that at 23 degrees C cercariae achieved 50% survival in 24 h, compared to 92 h at 12 degrees C. Cercariae aged in ASW at 28 and 37.5 degrees C showed 50% survival at 16 and 10 h, respectively. Cercariae aged at different temperatures for various times were used to infect juvenile Helisoma trivolvis (Colorado strain) snails maintained in ASW at 23 degrees C. Index of infectivity was based on counting encysted metacercariae in the snails at 8 to 12 h post-infection. Cercariae aged at 23, 28 and 37.5 degrees C showed 50% encystment at 6, 8 and 4 h, respectively. Cercariae aged at 4 degrees C showed 50% encystment in 10 h and cercariae aged at 12 degrees C showed 50% encystment beyond 16 h. Cercariae showed maximal longevity and infectivity in snails when aged at 12 degrees C in ASW. For E. caproni, as in other digeneans, the infective period of cercariae is markedly shorter than the maximal life-span at any given temperature. Studies on in vitro encystment of E. caproni cercariae in Locke's solution:ASW (1:1) showed that encystment was optimal at 23 degrees C (78% encystment) and that it declined to 44% at 28 degrees C and became almost nil (0.02%) at 12 or 37.5 degrees C.     

Life‐history traits buffer against heat wave effects on predator–prey dynamics in zooplankton

In addition to an increase in mean temperature, extreme climatic events, such as heat waves, are predicted to increase in frequency and intensity with climate change, which are likely to affect organism interactions, seasonal succession, and resting stage recruitment patterns in terrestrial as well as in aquatic ecosystems. For example, freshwater zooplankton with different life‐history strategies, such as sexual or parthenogenetic reproduction, may respond differently to increased mean temperatures and rapid temperature fluctuations. Therefore, we conducted a long‐term (18 months) mesocosm experiment where we evaluated the effects of increased mean temperature (4°C) and an identical energy input but delivered through temperature fluctuations, i.e., as heat waves. We show that different rotifer prey species have specific temperature requirements and use limited and species‐specific temperature windows for recruiting from the sediment. On the contrary, co‐occurring predatory cyclopoid copepods recruit from adult or subadult resting stages and are therefore able to respond to short‐term temperature fluctuations. Hence, these different life‐history strategies affect the interactions between cyclopoid copepods and rotifers by reducing the risk of a temporal mismatch in predator–prey dynamics in a climate change scenario. Thus, we conclude that predatory cyclopoid copepods with long generation time are likely to benefit from heat waves since they rapidly “wake up” even at short temperature elevations and thereby suppress fast reproducing prey populations, such as rotifers. In a broader perspective, our findings suggest that differences in life‐history traits will affect predator–prey interactions, and thereby alter community dynamics, in a future climate change scenario.     

Oxygen uptake and lactate production by Schistosoma mansoni cercaria, cercarial body and tail, and schistosomule.

1. Oxygen consumption by Schistosoma mansoni cercarial bodies varies, with the batch of organisms, the incubation media and the temperature (27-37 degrees C), from 27.4 +/- 3.4 to 55.0 +/- 4.8 microliters O2/mg larval protein per hr. It is proportional to the concentration of organisms incubated, up to 25,000/ml, as calculated from whole protein. 2. Oxygen uptake by cercariae is inhibited by 5.6 mM glucose in the incubation media, a concentration that stimulates the respiration of cercarial bodies. 3. No significant differences in the oxygen uptake were presented by cercarial bodies with and without glycocalyx or glandular secretions, or devoid of all of them. 4. Inhibitors of the Krebs cycle and the respiratory chain, and uncoupling agents influence the oxygen uptake by cercariae, cercarial bodies and schistosomules to the same extent. 5. The permeability change presented by transformed larvae had no influence on the excretion of lactate by cercarial bodies, which is about 0.3 mumoles/mg protein per hr and remains constant for 5 hr; under nitrogen, this amount increased 70%. Cercariae in anaerobiosis, however, excreted as much as 15 times more lactate than under air. 6. Lactic dehydrogenases of cercariae, cercarial bodies and tails, and schistosomules are of the muscle type and do not change during the transformation.     

Sensitivity of leaf size and shape to climate within Acer rubrum and Quercus kelloggii

* Variation in the size and shape (physiognomy) of leaves has long been correlated to climate, and paleobotanists have used these correlations to reconstruct paleo-climate. Most studies focus on site-level means of largely nonoverlapping species sets. The sensitivity of leaf shape to climate within species is poorly known, which limits our general understanding of leaf-climate relationships and the value of intraspecific patterns for paleoclimate reconstructions. * The leaf physiognomy of two species whose native North American ranges span large climatic gradients (Acer rubrum and Quercus kelloggii) was quantified and correlated to mean annual temperature (MAT). Quercus kelloggii was sampled across a wide elevation range, but A. rubrum was sampled in strictly lowland areas. * Within A. rubrum, leaf shape correlates with MAT in a manner that is largely consistent with previous site-level studies; leaves from cold climates are toothier and more highly dissected. By contrast, Q. kelloggii is largely insensitive to MAT; instead, windy conditions with ample plant-available water may explain the preponderance of small teeth at high elevation sites, independent of MAT. * This study highlights the strong correspondence between leaf form and climate within some species, and demonstrates that intraspecific patterns may contribute useful information towards reconstructing paleoclimate.     

长白山生态功能区气候变化特征

为探究长白山生态功能区气候变化特征,本研究利用区域内及周边36个气象站数据与CN05.1格点数据集,采用线性倾向估计法、Mann-Kendall突变检验、累积距平法、Morlet小波分析等方法研究1961—2016年长白山生态功能区内温度(平均气温、四季气温、极端气温)、水分(年降水量、四季降水量、降水日数、相对湿度)、光照(日照时数与日照百分率)和风速因子的时空变化规律.结果表明: 1961—2016年,长白山生态功能区气温升高、日照减少、风速减弱、降水量周期振荡变化.其中,冬季气温[0.45 ℃·(10 a)^-1]与最低温度[0.74 ℃·(10 a)^-1]大幅上升.年平均风速显著降低[-0.21 m·s^-1·(10 a)^-1]但并未发生气候突变.年降水日数大幅降低[-7.01 d·(10 a)^-1],使其与东北地区气候变化特点有所不同.虽然功能区内年降水量倾向率为16.06 mm·(10 a)^-1,但不能以简单的趋势增加或减少来描述降水量变化特征,功能区内降水量变化以26年长周期叠加3年的短周期为主.研究结果对区域生态评估、生态系统响应气候变化、物候变化等研究具有指示意义.     

The Influence of Diurnal Temperature Variation on Degree-Day Accumulation and Insect Life History

Ectotherms, such as insects, experience non-constant temperatures in nature. Daily mean temperatures can be derived from the daily maximum and minimum temperatures. However, the converse is not true and environments with the same mean temperature can exhibit very different diurnal temperate ranges. Here we apply a degree-day model for development of the grape berry moth (Paralobesia viteana, a significant vineyard pest in the northeastern USA) to investigate how different diurnal temperature range conditions can influence degree-day accumulation and, hence, insect life history. We first consider changes in diurnal temperature range independent of changes in mean temperatures. We then investigate grape berry moth life history under potential climate change conditions, increasing mean temperature via variable patterns of change to diurnal temperature range. We predict that diurnal temperature range change can substantially alter insect life history. Altering diurnal temperature range independent of the mean temperature can affect development rate and voltinism, with the magnitude of the effects dependent on whether changes occur to the daily minimum temperature (Tmin), daily maximum temperature (Tmax), or both. Allowing for an increase in mean temperature produces more marked effects on life history but, again, the patterns and magnitude depend on the nature of the change to diurnal temperature range together with the starting conditions in the local environment. The study highlights the importance of characterizing the influence of diurnal temperature range in addition to mean temperature alone.     

Schistosoma mansoni: eicosanoid production by cercariae

Cercariae of Schistosoma mansoni are stimulated to penetrate skin by certain free fatty acids. The cercariae have an active arachidonate cascade, presumably using host skin essential fatty acids as cascade precursors. Exposing cercariae to 3.3 mM linoleate for 1, 10, and 60 min resulted in production of a wide variety of eicosanoids. Using high-performance liquid chromatography, eicosanoids coeluting with prostaglandin E2, D2, and A2, leukotriene B4, and 5-hydroxyeicosatetraenoic acid standards were identified, as well as unidentified peak positions. Radioimmunoassay confirmed the presence of immunoreactive prostaglandin E1, and E2, and 5- and 15-hydroxyeicosatetraenoic acids in cercarial extracts. No eicosanoid production occurred when cercariae were exposed to 3.3 mM oleate and 1 or 330 microM linoleate. Both high-performance liquid chromatography and radioimmunoassay data indicated that cercariae regulate the production of eicosanoids through time. It is postulated that arachidonate metabolism and subsequent eicosanoid production are required for successful cercarial penetration.     

Effects of exogenous glucose on survival and infectivity of Schistosoma mansoni cercariae

The effects of exogenous glucose in artificial spring water (ASW) were studied on the survival and infectivity of Schistosoma mansoni cercariae. The mean percent survival of cercariae maintained in 1% glucose in ASW for 36 and 48 hr was significantly greater than that of cercariae maintained identically in ASW. Cercariae maintained in ASW with or without glucose for 24 hr, fixed in neutral buffered formalin, and stained in Oil Red O, showed an accumulation of neutral lipid in the tail. Cercariae maintained as described above and stained in periodic acid-Schiff exhibited depleted glycogen, mainly from the tail. Cercariae maintained in ASW with glucose for 24 hr did not resynthesize glycogen. Cercariae maintained in ASW with glucose for 24 hr were as capable of infecting male FVBN202 mice as were freshly emerged cercariae, and increased the percent of worm recovery. Exogeneous glucose added to ASW prolonged the survival of S. mansoni cercariae and increased infectivity in terms of worm recovery.     

Climate-Induced Changes in Grapevine Yield and Must Sugar Content in Franconia (Germany) between 1805 and 2010

When attempting to estimate the impacts of future climate change it is important to reflect on information gathered during the past. Understanding historical trends may also aid in the assessment of likely future agricultural and horticultural changes. The timing of agricultural activities, such as grape harvest dates, is known to be influenced by climate and weather. However, fewer studies have been carried out on grapevine yield and quality. In this paper an analysis is undertaken of long-term data from the period 1805–2010 on grapevine yield (hl/ha) and must sugar content (°Oe) and their relation to temperature. Monthly mean temperatures were obtained for the same time period. Multiple regression was used to relate the viticulture variables to temperature, and long-term trends were calculated. Overall, the observed trends over time are compatible with results from other long term studies. The findings confirm a relationship between yield, must sugar content and temperature data; increased temperatures were associated with higher yields and higher must sugar content. However, the potential increase in yield is currently limited by legislation, while must sugar content is likely to further increase with rising temperatures.     

2000—2020年青藏高原植被净初级生产力时空变化及其气候驱动作用

青藏高原是我国乃至全世界的“气候变化实验室”,在气候变化驱动下,青藏高原植被净初级生产力(NPP)发生了显著变化。本研究利用归一化植被指数、数字高程、年降水量和年气温等数据,探究2000—2020年青藏高原植被NPP的时空变化特征及其与气候因子的关系。结果表明: 2000—2020年,青藏高原植被NPP呈显著增加趋势,NPP增加速率为1.67 g C·m^-2·a^-1。青藏高原植被NPP空间分布表现为从东南向西北逐渐递减,该分布格局与气温、降水量的空间分布格局基本吻合。植被NPP与气温和降水量变化显著正相关。暖湿化气候变化趋势是促进植被NPP显著增加的重要动力,如果气候持续更暖更湿,青藏高原植被NPP将会持续增加。     

Further studies on the carbohydrate metabolism of immature Schistosoma mansoni

Further studies on the carbohydrate metabolism of immature Schistosoma mansoni. International Journal for Parasitology 3: 783–787. Analysis of whole cercariae, cercarial bodies and tails and schistosomula shows the tail contains 26 per cent of the cercarial nitrogen, 46 per cent of the glycogen and 59 per cent of the cytochrome oxidase. 32 per cent of the total nitrogen and 22 per cent of the glycogen of the cercarial body is lost during penetration. Oxygen uptake of adult worms but not of cercariae increases between 30 and 37°C. A temperature of 41°C partly inhibits cercarial oxygen uptake but not that of adult worms. Incubation of schistosomula, 21-day-old and adult worms in nitrogen increases the rate of glycolysis.     

气候变化对中国农作物病害发生的影响

基于全国农区527个气象站点1961—2010年逐日气象资料、逐年农作物病害发生面积以及产量资料,从气温、降水、日照等角度,采用相关分析方法,研究了气候变化背景下各气象要素变化对中国农作物病害发生的影响。结果表明:近50年来,气候变化导致的各气象因子变化总体有利于病害发生,年平均温度以0.27℃·10a-1的速率升高,其每升高1℃,可导致病害发生面积增加6094.4万hm2次;年平均降雨强度以0.24mm·d-1·10a-1的速度增加,其每增加1mm·d-1,可导致病害发生面积增加6540.4万hm2次;年平均日照时数以47.4h·10a-1的速率减少,其每减少100h,可导致病害发生面积增加3418.8万hm2次;在气候变化导致的光、温、水变化中,温度增加对病害发生面积增加的影响最为显著,其次为日照时数减少、第三为平均降雨强度增大,其标准化回归系数依次为0.508、-0.374、0.112。     

晋南地区冬小麦生育期气候变化特征及其对产量的影响

明确气候变化特征及其对小麦生产的影响,有助于为农业适应气候变化方案的制定提供理论依据.本研究分析了晋南小麦主产区临汾、运城市1957-2015年降水量、气温、日照时长、潜在蒸散量、干燥度等变化及其对冬小麦生育期及产量的影响.结果 表明:1957-2015年,临汾、运城市全年降水量和冬小麦生育期日照时长均呈下降趋势,冬小...     

Climate change and heat-related mortality in six cities Part 2: climate model evaluation and projected impacts from changes in the mean and variability of temperature with climate change

Previous assessments of the impacts of climate change on heat-related mortality use the “delta method” to create temperature projection time series that are applied to temperature–mortality models to estimate future mortality impacts. The delta method means that climate model bias in the modelled present does not influence the temperature projection time series and impacts. However, the delta method assumes that climate change will result only in a change in the mean temperature but there is evidence that there will also be changes in the variability of temperature with climate change. The aim of this paper is to demonstrate the importance of considering changes in temperature variability with climate change in impacts assessments of future heat-related mortality. We investigate future heat-related mortality impacts in six cities (Boston, Budapest, Dallas, Lisbon, London and Sydney) by applying temperature projections from the UK Meteorological Office HadCM3 climate model to the temperature–mortality models constructed and validated in Part 1. We investigate the impacts for four cases based on various combinations of mean and variability changes in temperature with climate change. The results demonstrate that higher mortality is attributed to increases in the mean and variability of temperature with climate change rather than with the change in mean temperature alone. This has implications for interpreting existing impacts estimates that have used the delta method. We present a novel method for the creation of temperature projection time series that includes changes in the mean and variability of temperature with climate change and is not influenced by climate model bias in the modelled present. The method should be useful for future impacts assessments. Few studies consider the implications that the limitations of the climate model may have on the heat-related mortality impacts. Here, we demonstrate the importance of considering this by conducting an evaluation of the daily and extreme temperatures from HadCM3, which demonstrates that the estimates of future heat-related mortality for Dallas and Lisbon may be overestimated due to positive climate model bias. Likewise, estimates for Boston and London may be underestimated due to negative climate model bias. Finally, we briefly consider uncertainties in the impacts associated with greenhouse gas emissions and acclimatisation. The uncertainties in the mortality impacts due to different emissions scenarios of greenhouse gases in the future varied considerably by location. Allowing for acclimatisation to an extra 2°C in mean temperatures reduced future heat-related mortality by approximately half that of no acclimatisation in each city.     

Leaf life span as a simple predictor of evergreen forest zonation in China

Aim Our aim was to investigate how the average life span of canopy leaves might be used to predict the geographical distribution of natural forests at large geographical scales, and to explore the link between leaf characteristics and ecosystem functioning. We examine whether there is a general relationship between canopy mean leaf life span and climate (i.e. temperature and precipitation) that can be used to predict evergreen forest zonation in China. Location Forest areas in China. Methods During July and August of 2002–2004, we conducted a latitudinal forest transect spanning about 30° of latitude in eastern China. The canopy mean leaf life span was calculated to include all tree species (groups) in each forest plot through weighted averages scaled up from branch‐level measurements. Data from our previous work conducted in the Tibetan Alpine Vegetation Transects (TAVT) and from other investigators were compiled to supplement our results. Based on regression equations developed on the pooled data, and using gridded temperature and precipitation datasets, we simulated the distribution of canopy mean leaf life span for forests in China. The predicted leaf life span zonation was compared with a map of Chinese forest vegetation divisions published in 1980. Results Canopy mean leaf life span across 10 evergreen forest plots in eastern China showed a decreasing trend as mean annual temperature increased, following a common logistic pattern consistent with the data from the TAVT and other investigators. In pooled data for 40 evergreen forest plots across tropical and boreal regions, canopy mean leaf life span generally showed a negative relationship with mean annual temperature (r² = 0.72, P < 0.001), and a positive correlation with mean annual precipitation where mean annual temperature was > 8°C (r² = 0.45, P < 0.01). The climate‐based simulations of leaf life span zonation compared well with the previously published boundaries of forest vegetation divisions in eastern China. Main conclusions Our results reveal that mean leaf life span in evergreen forests follows a common logistic pattern associated with mean annual temperature and precipitation, which can in turn be used to predict evergreen forest zonation in eastern China.     

Temperature can interact with landscape factors to affect songbird productivity

Increased temperatures and more extreme weather patterns associated with global climate change can interact with other factors that regulate animal populations, but many climate change studies do not incorporate other threats to wildlife in their analyses. We used 20 years of nest‐monitoring data from study sites across a gradient of habitat fragmentation in Missouri, USA, to investigate the relative influence of weather variables (temperature and precipitation) and landscape factors (forest cover and edge density) on the number of young produced per nest attempt (i.e., productivity) for three species of songbirds. We detected a strong forest cover × temperature interaction for the Acadian Flycatcher (Empidonax virescens) on productivity. Greater forest cover resulted in greater productivity because of reduced brood parasitism and increased nest survival, whereas greater temperatures reduced productivity in highly forested landscapes because of increased nest predation but had no effect in less forested landscapes. The Indigo Bunting (Passerina cyanea) exhibited a similar pattern, albeit with a marginal forest cover × temperature interaction. By contrast, productivity of the Northern Cardinal (Cardinalis cardinalis) was not influenced by landscape effects or temperature. Our results highlight a potential difficulty of managing wildlife in response to global change such as habitat fragmentation and climate warming, as the habitat associated with the greatest productivity for flycatchers was also that most negatively influenced by high temperatures. The influence of high temperatures on nest predation (and therefore, nest predators) underscores the need to acknowledge the potential complexity of species' responses to climate change by incorporating a more thorough consideration of community ecology in the development of models of climate impacts on wildlife.     

Histidine 190-D1 and glutamate 189-D1 provide structural stabilization in photosystem II

In photosynthesis, photosystem II (PSII) conducts the light-driven oxidation of water to oxygen. Tyrosine Z is Tyr 161 of the D1 polypeptide; Z acts as an intermediary electron carrier in water oxidation. In this report, EPR spectroscopy was used to study the effect of His 190 and Glu 189 on Z* yield and reduction kinetics. Neither mutation has a significant impact on the EPR line shape of Z*. At room temperature and pH 7.5, the E189Q-D1 mutation has a single turnover Z* yield that is 84% compared to wild-type. The H190Q-D1 mutation decreases the Z* yield at room temperature by a factor of 2.6 but has a more modest effect (factor of 1.6) at -10 degrees C. The temperature dependence is shown to be primarily reversible. Neither mutation has a dramatic effect on Z* decay kinetics. The Z* minus Z FT-IR spectrum, recorded at pH 7.5 on H190Q, reveals perturbations, including an increased spectral contribution from a PSII chlorophyll. The Z* minus Z FT-IR spectrum, recorded at pH 7.5 on E189Q, shows perturbations, including a decreased contribution from the carboxylate side chain of a glutamate or aspartate. Temperature-dependent changes in H190Q-D1 and E189Q-D1 Z. yield are attributed to a reversible conformational change, which alters the electron-transfer rate from Z to P(680)(+). On the basis of these results, we conclude that H190 and E189 play a role in the structural stabilization of PSII. We postulate that some or all of the phenotypic changes observed in H190Q and E189Q mutants may be caused by structural alterations in PSII.     

The influence of climate change on the body mass of woodrats Neotoma in an arid region of New Mexico, USA

Earth system scientists have recently concluded that anthropogenic induced climate change is detectable. Because many aspects of an organism's ecology and evolution are influenced by environmental temperature, this suggests temperature mediated changes may be already occurring in natural ecosystems. Using archived mammal trapping and meteorological data, we investigated local changes in climate over the past 8 yr at the Sevilleta National Wildlife Refuge in an arid region of New Mexico to determine i) if environmental conditions had altered, ii) if mean body mass of woodrats had changed over this time period, and iii) if the answers to i) and ii) were positive, were the results correlated? Body mass was chosen because it is highly sensitive to temperature and many crucial ecological and evolutionary parameters are affected by it. Our results indicate that winter temperature measures (average cold and minimum), and maximum summer temperature have changed significantly over the past 8 yr. Summer and winter temperatures have both increased by ca 2.5 to 3°C. When compared to long-term means, all years have had significantly warmer than average minimum temperatures. Mean body mass of woodrat populations has also changed significantly over the past 8 yr, and the changes are negatively correlated with both winter and summer temperatures. We predict that additional climatic warming will lead to further decreases in the mean body mass of woodrats at the Sevilleta NWR. Since many important ecological parameters are tightly linked with body mass (e.g. fecundity, dietary strategy, home range, extinction rates, energetic requirements, predation risk, etc.), our results suggest that further climate change may lead to profound alterations in woodrat life history, and indirectly, on the dynamics and Structure of the entire community. This is in addition to any direct effect temperature may have on other plants and animals.