Nutrient dynamics in 3 morphological different tropical seagrasses and their sediments

Seasonality of nutrient dynamics in three morphologically different seagrass species and their sediments was examined for 1 year between November 2006 and November 2007 at four sites in the Andaman Sea, Thailand. The smaller species, Cymodocea serrulata and Halophila ovalis, showed major seasonal variation in shoot density, above- and belowground biomass, much more than expected from seasonal changes in water temperature and light conditions. All parameters showed minimum values in the dry season due to desiccation during neap tides. In contrast Enhalus acoroides showed less seasonal variation. Only limited seasonality was found in tissue N content of all species, whereas tissue P content responded to the low P concentration in the water column during the wet season. There were no differences in sediment conditions among species, and nutrient pools were generally low. Furthermore there were no significant spatial differences in seagrass and sediment nutrient dynamics, despite varying anthropogenic activity at the study sites, reflecting the oligotrophic conditions in this region.     

枯水季节赣江近岸水洼与浅滩中浮游动物的群落差异

为探究水洼与邻近浅滩中浮游动物群落是否存在差异, 于2015年1月22日和3月1日, 选择赣江南昌段的3个水洼和邻近浅滩采集浮游动物, 对浮游动物的物种组成、密度、生物量、多样性指数和群落结构进行比较研究。通过单因子方差分析(One-way ANOVA)检验水洼与浅滩中水环境因子及浮游动物密度和生物量的差异。使用非度量多维尺度分析(Non-metric multi-dimensional scaling, NMDS)和群落相似性分析(Analysis of similarity, ANOSIM)对暂时性水洼及邻近浅滩的浮游动物群落进行排序。1月和3月共发现浮游动物44种, 轮虫有30种, 占总捕获数的68%。枝角类和桡足类各有7种, 分别占总捕获数的16%。相对重要性指数(Index of relative importance, IRI)大于1000的优势物种有5种, 分别为汤匙华哲水蚤Sinocalanus dorrii、长肢多肢轮虫Polyarthra dolichoptera、桡足类无节幼体Copepod nauplii、角突臂尾轮虫Brachionus angularis和长圆疣毛轮虫Synchaeta oblonga。单因子方差分析表明, 1月份水洼的水深、电导率和总氮含量显著高于浅滩(P<0.05), 浅滩的水温、pH、溶解氧、浊度和总磷含量略高于水洼。3月份水洼的水深、pH和总氮含量略高于浅滩, 浅滩的溶解氧、浊度和总磷含量较水洼高, 水温和电导率在2种水体中非常接近。1月份水洼中浮游动物的密度(7.90 ind./L)和生物量(7.78 μg/L)均低于浅滩(9.34 ind./L, 19.03 μg/L), 3月份水洼中浮游动物的密度(24.27 ind./L)和生物量(332.14 μg/L)均高于浅滩(22.86 ind./L, 146.10 μg/L)。浅滩中浮游动物的多样性指数(H′)、均匀度指数(J)和物种丰富度指数(D)均大于水洼。非度量多维尺度分析和群落相似性分析表明, 仅1月份水洼与浅滩的浮游动物群落结构具有边缘显著差异(P=0.067), 可大致划分为2个: 水洼群落和浅滩群落。3月份由于水位上涨, 研究的水洼与赣江河道处于连通或半连通状态, 2种生境中浮游动物群落结构无显著差异(P=0.313)。斯皮尔曼相关分析(Spearman correlation coefficient)发现水深和溶解氧是导致水洼和浅滩中浮游动物密度差异的主要环境因子。2种生境中浮游动物的密度与pH、电导率、总氮和总磷均具有显著相关性(P<0.05)。     

Culex mosquitoes in temporary urban rain pools: seasonal dynamics and relation to environmental variables.

The study was conducted in a park of Buenos Aires City, where a total of 89 rain pools were sampled weekly for mosquito immature stages over a one-year period. The aim of the present paper was to investigate the seasonal dynamics of three Culex species breeding in temporary rain pools and to analyze the relationships of the presence of these species to pool dimensions, pool age, vegetation, and insolation degree. The three species showed differences in their seasonal patterns, Culex dolosus being present during the whole year, Culex pipiens mainly in the summer season, and Culex maxi almost exclusively during the fall. The variable explaining most of the variation among sampling dates in species composition was weekly mean temperature. A significant positive association was detected among mosquito species, as they were recorded together more frequently than expected by chance. The statistical analyses performed revealed significant positive relationships of all three mosquito species to increasing surface area, whereas no relationship to insolation degree was detected in the studied pools. Culex pipiens and Culex dolosus showed positive relationships to increasing vegetation cover, whereas the presence of Culex dolosus was also related to pool age.     

Flux of organic carbon in a riverine mangrove wetland in the Florida Coastal Everglades

Short-term (daily) and seasonal variations in concentration and flux of dissolved organic carbon (DOC) were examined over 15 tidal cycles in a riverine mangrove wetland along Shark River, Florida in 2003. Due to the influence of seasonal rainfall and wind patterns on Shark River’s hydrology, samplings were made to include wet, dry and transitional (Norte) seasons. We used a flume extending from a tidal creek to a basin forest to measure vertical (vegetated soil/water column) and horizontal (mangrove forest/tidal creek) flux of DOC. We found significant (p < 0.05) variations in surface water temperature, salinity, conductivity, pH and mean concentration of DOC with season. Water temperature and salinity followed seasonal patterns of air temperature and rainfall, while mean DOC concentration was highest during the dry season (May), followed by the wet (October) and ‘Norte’ (December) seasons. This pattern of DOC concentration may be due to a combination of litter production and inundation pattern of the wetland. In contrast to daily (between tides) variation in DOC flux between the mangrove forest and tidal creek, daily variations of mean water quality were not significant. However, within-tide variation of DOC flux, dissolved oxygen content and salinity was observed. This indicated that the length of inundation and water source (freshwater vs. saltwater) variation across tidal cycles influenced water quality and DOC flux in the water column. Net DOC export was measured in October and December, suggesting the mangrove forest was a source of DOC to the adjacent tidal creek during these periods. Net annual export of DOC from the fringe mangrove to both the tidal creek and basin mangrove forest was 56 g C m⁻² year⁻¹. The seasonal pattern in our flux results indicates that DOC flux from this mangrove forest may be governed by both freshwater discharge and tidal range.     

Effect of season on thermoregulation, metabolism and ventilation of the southern brown bandicoot Isoodon obesulus (Marsupialia: Peramelidae)

Seasonal variation in various thermoregulatory, metabolic and ventilatory parameters was examined for southern brown bandicoots (Isoodon obesulus fusciventer) from a Mediterranean climate near Perth, Western Australia. There was significant seasonal variation over the four annual seasons at thermoneutrality (Ta=30 degrees C) in body temperature, oxygen consumption, carbon dioxide production, respiratory exchange ratio, total evaporative water loss, wet and dry thermal conductance and tidal volume but not mass, ventilatory frequency, minute volume or oxygen extraction efficiency. Only carbon dioxide production and respiratory exchange ratio showed an annual pattern that was significantly related to season, with both being significantly higher in winter, presumably as a result of greater and higher quality food availability.     

Water temperature instead of acclimation stage and oxygen concentration determines responses to winter floods

Field observations suggest that flooding events in the growing season are more detrimental than in winter. To clarify mechanisms producing these seasonal differences we analysed the role of plant acclimation, water temperature and oxygen concentration. We first tested the relative effects of seasonal acclimation and water temperature with three grassland species that differed in tolerance to summer floods (i.e. Rumex crispus, Rumex acetosa and Daucus carota). Our second experiment addressed the role of oxygen level relative to water temperature on biomass decay rate on a moderately intolerant species (i.e. R. acetosa).Irrespective of acclimation, biomass loss in warm water was considerably faster than in cold water. Given the concomitant decline in total non-structural carbohydrates, this was ascribed to the impact of water temperature on respiration rate. However, we only found a significant decline in carbohydrates for R. crispus and R. acetosa. D. carota seemed unable to access stored carbohydrates, which may explain its sensitivity for winter- and summer floods. Our second experiment provided no indication that the higher oxygen concentration may mitigate effects of flooding in cold water since a lower oxygen level of the water did not accelerate the rate of biomass loss.These findings indicate that temperature-driven respiration of carbohydrate reserves determines a species’ response to winter flooding, whereas oxygen level or plant acclimation are unimportant.     

Observations on the limnology and primary production of a small man-made lake in the West African savanna

1. The results of limnological studies on a small, 35-ha, triangular man-made lake and a small adjacent fish pond in the coastal savanna of Ghana are described. 2. The lake, which has a renewal time of approximately 0.96 years, is subject to large, predictable seasonal changes. Water volume and surface area rapidly reach maximum values in the wet season from April to June despite the low runoff values which average only 1.2% of the precipitation. Minimum values occur in the dry season when up to 76% of the lake area may be exposed. Most of the water is lost by evaporation which may amount to 193 cm annually. 3. The annual cycle in water temperature follows that in solar radiation with peaks towards the end of the dry season in March to April and deep troughs in the wet season from April to June. During the dry season the water column is characterized by greater stability, a higher degree of stratification, and a much higher amplitude of diurnal temperature change (4-5°C) than in the wet season (1°C). Isothermal conditions tend to be approached nocturnally and even during the day in the wet season. 4. The ionic content of the water is low and dominated by bicarbonate, sodium, silica and iron. During the wet season flood water results in a decline in conductivity from 214 to 30 μmhos/cm², a decrease in pH and transparency, and an increase in oxidizable organic material. Except for the conductivity these values return to normal in about 6 weeks as a result of rapid decomposition of allochthonous materials. 5. The oxygen pulse is strong and photosynthetic activity by phytoplankton high during the dry season whereas in the wet season the converse is true. As a result of the low concentration of organic carbon (0.10–0.35%) in the sediments their oxygen demands are low. Consequently, dissolved oxygen values near the sediment are relatively high and oxygen stratification poorly-developed. Most of the organic carbon appears to be recycled in the water column rather than in the sediments as is generally the case in tropical ecosystems. 6. Rooted vegetation became permanently established in the fish pond but not i n the lake itself. Emergent and floating vegetation which grows profusely in the draw-down area in the wet season is for the most part exported from the system by wind and biological agencies and, therefore, contributes little to the energy and mineral budgets of the lake. Primary production in the water column is mainly by Myxophyceae and Bacillariophyceae and is low during the dry season (1.35 gC/m²/day) and very low in the wet season. Possible reasons for the low level of primary production are discussed.     

Patchiness in the abundance of metacercariae parasitizingPoecilia gillii (Poeciliidae) isolated in pools of an intermittent tropical stream

Synopsis Prevalence and intensity of a clinostomatid in the fishPoecilia gilliii were measured in six dry season pools of a small intermittent Costa Rican stream, and the prevalence of two diplostomulid parasites (‚diplostomulum’ and ‚neascus’) were monitored in 14 residual pools of a second intermittent stream of the same drainage. There were significant among-pool differences in the prevalence of the three parasites. There was no evidence to suggest that clinostomatid or ‚diplostomulum’ prevalence was influenced by the position of pools within the downstream gradient; however, ‚neascus’ prevalence tended to decrease with distance downstream. Host length accounted for some of the variation in parasite prevalence among pools for both diplostomulids. Prevalence and intensity of a clinostomid in the body cavity varied with host gender and body size. There was a positive relationship between body size and clinostomatid parasitization in female hosts. Most males examined were less than 50 mm (total length). For fish less than 50 mm, males were more parasitized than females. Prevalence of the two diplostomulids was not related to the relative net periphyton production or the dissolved oxygen concentration of the pools. However, a positive correlation between the density ofP. gillii and ‚diplostomulum’ prevalence was found across the fourteen pools, and ‘neascus’ prevalence was positively related to pool area.     

Seasonal flow variation allows 'time-sharing' by disparate aquatic insect communities in montane desert streams

1. Flow variation can drive major abiotic changes in stream environments between seasons. Theoretically, disparate biotic communities could be maintained during different seasons at a single site if suitable refuges and colonist sources were available. Using isolated montane desert streams in south‐east Arizona as a model system, we hypothesised that two disparate aquatic insect faunas (montane temperate and neotropical) could be maintained at the same sites through strong seasonal variation in abiotic conditions. 2. We collected aquatic insects representing 59 families from seven streams during high‐flow (March–April) and low‐flow (June) sampling periods across two years. We assessed changes in aquatic insect community and functional feeding group composition by habitat (riffle, pool) and season (high flow, low flow). 3. Within sites, wetted stream area decreased by an average of 97% between high‐flow (predominately riffles) and low‐flow (predominately pools) seasons. Community composition likewise showed strong seasonal patterns; the montane temperate fauna was strongly associated with the high‐flow season while neotropical hemipterans and coleopterans were associated with the low‐flow season. Increased water temperature was significantly associated with this shift from temperate to neotropical assemblages. 4. Functional feeding group composition shifted dramatically by season. The proportion of predators increased from 24.5% (high flow) to 75.2% (low flow) while collector–filterers and shredders declined from 38.4% (high flow) to 1.7% (low flow). 5. We suggest that habitat ‘time‐sharing’ by disparate communities is facilitated via strong seasonal variation in temperature and flow and the presence of high elevation refuges or diapause stages for temperate montane taxa to survive the dry season.     

The seasonal pattern of CO2 exchange of Festuca rubra L. in a montane meadow community in Northern Germany

Summary Completely climatized cuvettes were used to follow the CO₂ gas exchange of red fescue (Festuca rubra L.), growing on a fertilized and an unfertilized plot, during a growing season from May through October. Objective of the study was to determine the effect of environmental factors on the seasonal CO₂ gas exchange.Gas exchange rates were calculated on the basis of leaf dry weight, surface area and chlorophyll content. Photosynthetic rates differed between the fertilized and unfertilized plants when based on leaf dry weight or leaf surface area but were similar when based on chlorophyll.Multiple regression analysis was used to related photosynthetic rates to radiation, temperature, water vapor concentration difference, chlorophyll content and time. A cubic regression equation based on daily radiation alone explained 85% of the variation for the fertilized plants and 87% of the variation for the unfertilized plants.During the growing season the unfertilized plants had a continual decline in their photosynthetic rates. The fertilized plants had high photosynthetic rates in the spring and in the fall.Light response curves indicated greater photosynthetic rates at light saturation as well as in the light limited portion of the light response curve for the fertilized plants. Photosynthetic rates of the fertilized plants were generally depressed during periods of warm temperature and high light intensity in June and July.Photosynthetic rates declined at temperatures above 24°C. The decline was greater for the more mesomorphic fertilized plants. A similar response was noted to increasing water vapor difference, although it was difficult to separate from the temperature effect. Maximum photosynthetic rates were found between 14°C and 22°C, although there was considerable variation in the maximum rates.The effects of cutting (mowing) on the gas exchange were difficult to determine due to the interaction of the environmental factors.Chlorophyll content showed significant correlation with photosynthetic rates.     

MARINE BACTERIA OF CARDIGAN BAY. II. BACTERIA IN ROCK POOLS

SUMMARY: Two pools of different characteristics were examined for bacterial content, marine and alien. Comparative monthly counts showed little consistency over the sampling periods and no definite seasonal variation. Temperature, pH and light had little direct influence. Chromogenic strains were few. Most marine bacteria were small Gram-negative rods; a high proportion liquefied gelatin, but other biochemical reactions were weak.
The amount of dissolved oxygen increased with exposure of the pools but decreased in a third pool devoid of visible flora and fauna. All three pools showed a marked increase in marine bacterial content during intertidal exposure. The coli-aerogenes organisms content was low and, as in the case of soil and fresh water, the strains showed no definite seasonal variation.     

Effects of soil water content on soil respiration in forests and cattle pastures of eastern Amazonia

The effect of soil water content on efflux of CO₂ from soils has been described by linear, logarithmic, quadratic, and parabolic functions of soil water expressed as matric potential, gravimetric and volumetric water content, water holding capacity, water-filled pore space, precipitation indices, and depth to water table. The effects of temperature and water content are often statistically confounded. The objectives of this study are: (1) to analyze seasonal variation in soil water content and soil respiration in the eastern Amazon Basin where seasonal temperature variation is minor; and (2) to examine differences in soil CO₂ emissions among primary forests, secondary forests, active cattle pastures, and degraded cattle pastures. Rates of soil respiration decreased from wet to dry seasons in all land uses. Grasses in the active cattle pasture were productive in the wet season and senescent in the dry season, resulting in the largest seasonal amplitude of CO₂ emissions, whereas deep-rooted forests maintained substantial soil respiration during the dry season. Annual emissions were 2.0, 1.8, 1.5, and 1.0 kg C m^-2 yr^-1 for primary forest, secondary forest, active pasture, and degraded pasture, respectively. Emissions of CO₂ were correlated with the logarithm of matric potential and with the cube of volumetric water content, which are mechanistically appropriate functions for relating soil respiration at below-optimal water contents. The parameterization of these empirical functions was not consistent with those for a temperate forest. Relating rates of soil respiration to water and temperature measurements made at some arbitrarily chosen depth of the surface horizons is simplistic. Further progress in defining temperature and moisture functions may require measurements of temperature, water content and CO₂ production for each soil horizon.     

Long-term seasonal variation in the biological traits of benthic-macroinvertebrates in two Mediterranean-climate streams in California, U.S.A.

1. We investigated the seasonal variation of biological traits and the influence of interannual rainfall variability on this pattern. Using long‐term survey data (6–19 years) from an intermittent and a perennial stream in the Mediterranean‐climate region of northern California, we examined 16 fuzzy‐coded biological traits (e.g. maximum size, life cycle duration, and mode of respiration). 2. Seasonal habitat variability is higher in the intermittent stream than in the perennial stream. During the winter and spring wet‐season both streams flood; however, during the summer dry‐season, the intermittent stream forms isolated pools in (occasionally drying completely). 3. Seasonal habitat variability influenced both taxonomic and biological trait composition. Distinct taxonomic communities were present in each season, particularly in the intermittent stream. The intermittent stream also exhibited more seasonal variation in biological traits than the perennial stream. 4. Despite statistically significant seasonal variation, trait composition was relatively stable among seasons in comparison with taxonomic composition and abundance. Taxonomic composition varied considerably between seasons, because of high seasonal and interannual replacement of taxa resulting from seasonal habitat changes. 5. The seasonality of taxonomic composition and abundance was sensitive to interannual rainfall variability. In dry years, the taxonomic composition of communities was more similar between seasons than in wet years, while trait composition was relatively insensitive to rainfall variability. 6. Despite high seasonal variation in abundance and taxonomic composition, biological traits of aquatic macroinvertebrates varied less and exhibited seasonal stability, which may be a result of the unpredictability and harshness of stream environments.     

Coexistence of similar genotypes of Daphnia magna in intermittent populations: response to thermal stress

We investigated the diversity and thermal response of a fitness related trait, juvenile growth rate, in seasonal population samples of Daphnia magna from two temperate ponds. Both populations were intermittent, i.e. they disappeared from the water body and recolonized seasonally by hatching from resting eggs in the sediment.
Temporally isolated clones of Daphnia magna showed the typical asymmetric response for growth rate with temperature and a sharp decline after the maximum response at 26°C (TMR). There was no evidence for genetically adapted seasonal groups. Despite significant genetic variation among clones and for phenotypic plasticity (G×E interactions without genetic correlations), seasonal groups of clones showed no shift in TMR and mean temperature reaction norms were similar among groups and both populations. Heritabilities remained similar among temperatures despite a large increase in genetic variance at stressfully high temperatures of 29°C and 32°C, due to simultaneous increase in environmental variance. Further, heritabilities remained high among sample periods and were not eroded during several months of asexual reproduction.
Regular diapause, an intrinsic feature of intermittent Daphnia populations, may replace the need for physiological temperature adaptation and promote maintenance of diversity through phenotypic similarity by reducing the time over which competitive interactions occur. Such populations are unlikely to be directly affected by elevated temperatures. They have a large potential for phenotypic plasticity as their TMR is higher than the temperature normally encountered.     

西双版纳热带雨林土壤与叶片生态化学计量特征的干湿度效应

基于地理格局对西双版纳热带雨林的干湿度梯度效应和生态化学计量学的研究思路,结合野外试验监测和室内分析,对西双版纳热带雨林土壤-植物系统元素化学计量特征对海拔和干湿度效应响应进行了研究探讨,结果发现:西双版纳热带雨林土壤和叶片碳氮磷化学计量特征均不同程度的受到海拔和干湿季影响。季雨林与山地雨林的水热梯度受海拔梯度重要影响,随海拔梯度升高,土壤含水率变化显著,且含水率在干湿季均对土壤有机碳(SOC)存在显著影响(P0.01),雨季其对土壤全氮(STN)和土壤全磷(STP)的影响要显著于干季;叶片全磷(TP)随含水率的增大而升高,而叶片全氮(TN)在干季会随含水率的升高而增大,雨季含水率升高到一定程度时会抑制TN含量的增加并出现单峰现象;而土壤C/P与海拔和干季土壤含水率的极显著相关性(P0.01)及干季叶片C/N与叶片含水率的显著相关关系(P0.05)说明,干季水分匮乏条件下,土壤含水率影响土壤P的矿化度和植物对P的吸收利用水平,而且叶片C/N对反馈植物水分含量具有明显指示作用。因此,水热梯度是土壤-叶片系统碳氮磷生态化学计量特征变化的重要驱动因素。此外,全球变化区域响应方面,多雨高温可能会削弱季雨林叶片C的同化能力,且叶N含量降低,但受氮沉降的影响,对C/N的影响尚无法确定;由于P循环对其他元素的耦合作用,雨林土壤-叶片系统的元素循环周期将会被缩短,但干季山地雨林植物生态系统P的限制作用有可能会减弱。     

四川都江堰地区桢楠林、杉木林和常绿阔叶林土壤N库的季节变化

通过对四川都江堰地区桢楠（Phoebe zhennan）林、杉木（Cunninghamia lanceolata（Lamb．））林以及常绿阔叶林为期1a的研究,比较不同森林群落类型中N库各组分的大小以及季节动态,同时研究不同群落类型中N库各组分之间的关系,探讨植被、土壤特性以及微生物对N转化的影响。结果表明：①3种群落类型中土壤NH4^＋-N含量有明显的季节变化,均在冬季（12月份）达到最大。随着植物的生长,NH4^＋-N含量逐渐下降;②3种类型的群落土壤中NO3^--N含量的平均值差别很大,同一个森林群落类型在不同季节NO3^--N含量有明显的季节变化,但并不是所有的季节之间都存在显著差异;③3种森林群落类型在采样期内的土壤平均全N含量存在显著差别,在不同季节,土壤全N含量变化并不大;④微生物量N在采样期内的波动很大,就每个样地来说也具有一定的规律。得出的结论认为：不同的森林群落类型中的N循环同该群落内的土壤和植被类型有密切的联系,土壤微生物量N同环境因素（土壤温度和湿度）的关系存在时空变化。     

Genetic variance in the composition of two functional groups (diazotrophs and cyanobacteria) from a hypersaline microbial mat

Examination of variation in ecological communities can lead to an understanding of the forces that structure communities, the consequences of change at the ecosystem level, and the relevant scales involved. This study details spatial and seasonal variability in the composition of nitrogen-fixing and cyanobacterial (i.e., oxygenic photosynthetic) functional groups of a benthic, hypersaline microbial mat from Salt Pond, San Salvador Island, Bahamas. This system shows extreme annual variability in the salinity of the overlying water and the extent of water coverage. Analysis of molecular variance and F(ST) tests of genetic differentiation of nifH and cyanobacterial 16S rRNA gene clone libraries allowed for changes at multiple taxonomic levels (i.e., above, below, and at the species level) to inform the conclusions regarding these functional groups. Composition of the nitrogen-fixing community showed significant seasonal changes related to salinity, while cyanobacterial composition showed no consistent seasonal pattern. Both functional groups exhibited significant spatial variation, changing with depth in the mat and horizontally with distance from the shoreline. The patterns of change suggest that cyanobacterial composition was more insensitive to water stress, and consequently, cyanobacteria dominated the nitrogen-fixing community during dry months but gave way to a more diverse community of diazotrophs in wet months. This seasonal pattern may allow the mat community to respond quickly to water-freshening events after prolonged dry conditions (system recovery) and maintain ecosystem function in the face of disturbance during the wet season (system resilience).     

垂叶榕榕小蜂群落及种间互作网络季节动态

群落中的物种相互作用构成了复杂的生态网络。有关物种的数量和组成的季节性动态变化已有较多的研究, 但是对于生态网络的动态变化知之甚少。揭示生态网络的动态变化对于理解群落的稳定性以及群落的动态变化过程和机理具有重要意义。本研究以垂叶榕(Ficus benjamina)榕小蜂群落为研究对象, 分别在西双版纳的干季和雨季采集了榕小蜂的种类和数量信息。比较了两个季节榕小蜂群落的动态变化以及共存网络的参数(例如网路直径、连接数、嵌套性和群落矩阵温度)变化。结果显示: 雨季榕果内传粉榕小蜂Eupristina koningsbergeri所占比例高于干季, 传粉榕小蜂的种群数量也高于干季, 而在干季非传粉榕小蜂的种类增加(干季15种小蜂, 雨季14种)。从榕树-传粉榕小蜂互利共生系统的适合度来看, 干季非传粉小蜂的增加对传粉榕小蜂和榕树的适合度是不利的。在干季, 共存网络物种间的连接数(干季0.95, 雨季0.47)多于雨季, 群落矩阵温度(干季23.24, 雨季2.64)也显著高于雨季。表明干季榕小蜂群落组成及种间关系较雨季更为复杂而多样, 高的矩阵温度暗示群落受到的干扰更大。     

南方红壤丘陵区杜仲人工林土壤水分动态

利用时域反射仪(TDR)定位监测方法,研究了南方红壤丘陵区杜仲人工林土壤水分分配规律.结果表明:不同月份间土壤蓄水量差异极显著(P<0.01),研究时段内土壤水分呈低-高-低的单峰变化.杜仲人工林土壤水分垂直变化显著,且不同季节变化规律各异:根据土壤水分的季节消长和物候变化趋势可将土壤水分变化分为土壤水分积累期和消耗期;按降雨量的季节分配可将土壤水分变化分为干季和湿季两个时段.土壤蓄水量与大气相对湿度(RH)、大气温度(t)、饱和水汽压差(VPD)、降雨量(R)显著相关(P<0.05),降雨量是最直接的影响因子,其次是大气温度.次降雨后土壤水分损失率与干旱天数呈显著的双曲函数关系(P<0.05),土壤蓄水量与雨后干旱天数呈显著线性负相关(P<0.05),在次降雨后的持续干旱条件下,土壤水分损失随着土层深度的增加逐渐趋于缓和.     

Hydrology,Physiochemistry, and Amphibians in Natural and Created Vernal Pool Wetlands

This study compared the hydrology, physiochemistry, and amphibian biomass between a complex of created vernal pools and a complex of natural vernal pools in 2007 in central Ohio, United States. Hydrologic connectivity of surface water and groundwater differed between the natural and the created pool complexes. Surface inundation duration for created pools exceeded that of natural pools, although spring water depths were similar. Dissolved oxygen (p= 0.05) and hourly temperature (p= 0.00) were 1.2% and 1.1% higher, respectively, in the created pools, and conductivity was 1.5% higher (p= 0.00) in the natural pools. Amphibian dip net results found no significant difference in biomass between natural and created pools or family (hylid, ranid, and ambystomatid) biomass in both pool types. Amphibian families were evenly represented by both capture methods in the created wetlands; however, the distribution of families was not even in natural pools and the proportion of ranids was four times greater for samples obtained by funnel traps than dip netting. Eleven years after construction, the created vernal pools did not mimic natural pools in surface inundation and groundwater–surface water exchange, dissolved oxygen, and water temperature. The created pools are perched wetlands and are never likely to mimic reference pool hydrology. Dissolved oxygen and temperature differences are likely due to the separation of surface water and groundwater in the created pools. However, the created pools exhibited a higher taxa diversity than the natural pools due to a more even distribution of organisms between the three families.