长江源区同域分布兔狲、藏狐和赤狐的时空重叠度

兔狲(Otocolobus manul)、藏狐(Vulpes ferrilata)和赤狐(V. vulpes)是青藏高原三江源区域分布的重要小型食肉兽。本研究于2014年6月至2019年9月在青海省长江源区沱沱河和通天河沿岸选取208个位点布设红外相机, 通过所获取的时空分布数据比较了上述3种同域分布小型食肉兽的时空利用情况。通过空间重叠度系数的比较分析, 兔狲和藏狐、兔狲和赤狐以及藏狐和赤狐之间的空间重叠度系数分别为0.25、0.48和0.17, 这表明兔狲、藏狐和赤狐三者在空间利用上存在一定的差异。通过核密度估计方法分析, 兔狲和藏狐属典型的昼行性动物, 而赤狐以夜行性活动为主。兔狲、藏狐和赤狐每个物种在冷暖两季的日活动节律重叠指数分别为0.83、0.78和0.88。两两比较分析表明, 兔狲和藏狐二者的日活动节律重叠指数最高(0.84), 兔狲和赤狐在夜间活动时段存在一定重叠(0.63), 而藏狐和赤狐的时间生态位分化最明显, 重叠指数最低(0.48)。此外, 在暖季, 两两物种之间的日活动节律重叠指数均小于其冷季的重叠指数。综上所述, 长江源区兔狲、藏狐和赤狐3种小型食肉兽可通过空间和时间资源的利用差异来降低物种间的干扰和竞争, 从而达到同域物种共存的目的。     

石羊河流域土地覆被空间演化及驱动机制

基于石羊河流域1998年、2002年、2006年、2010年NDVI、夜间灯光数据和TM影像提取的土壤信息,以城市地表人工覆被系统为基础,计算流域土地覆被指数(Land-Cover Index,LCI),利用小波分析、空间变差函数和间隙度指数等方法构建测度模型,分析了石羊河流域地区十多年来的土地人工覆被空间演化过程和格局,然后利用回归拟合方程找出影响地区土地覆被变化的驱动机制。结果表明:LCI大范围分布受地形限制,高值区(城镇用地区域)值越来越高,而低值区(植被覆盖区域)值在2002年形成了峰值后下降,即地区城镇化水平显著提高的同时,林草覆盖率缓慢变好,并且逐渐形成区域簇群,同时地区城镇化水平受人为因素的影响较大,植被覆盖度受自然因素的影响较大。     

下辽河平原降雨中氮素的动态变化

为了了解降雨中氮对农田生态系统的影响,分析了2004-2006年下辽河平原连续3年定位收集的降雨观测资料与历史资料.结果表明:降雨中氮输入量季节变化显著,夏季最高,这主要与降雨量及空气中NH4 -N浓度变化有关;降雨中DON量与NO3--N含量相当,均接近24%,是雨水中氮的重要组分;与1985年相比,近3年降雨输入到该地区农田生态系统的年氮通量已有较大提高,降雨较多的2005年输入的无机氮量更是20年前的2倍以上;2004-2006年随降雨输入农田生态系统的氮平均占可利用肥料氮的28.3%,对农田生态系统有着重要影响.     

The significance of side-arm connectivity for carbon dynamics of the River Danube, Austria

1. Side‐arms connected to the main stem of the river are key areas for biogeochemical cycling in fluvial landscapes, exhibiting high rates of carbon processing. 2. This work focused on quantifying autochthonous and allochthonous carbon pools and, thereby, on comparing transport and transformation processes in a restored side‐arm system of the River Danube (Regelsbrunn). We established a carbon budget and quantified carbon processing from March to September 2003. In addition, data from previous studies during 1997 to 1999 were assessed. 3. Gross primary production (GPP) and community respiration were estimated by diel oxygen time curves and an oxygen mass balance. Plankton primary production was determined to estimate its contribution to GPP under different hydrological conditions. 4. Based on the degree of connectivity, three hydrological phases were differentiated. Most of the organic matter, dominated by allochthonous carbon, was transported in the main channel and through the side‐arm during floods, while at intermediate and low flows (and thus connectivity), transformation processes became more important and autochthonous carbon dominated the carbon pool. The side‐arm system functioned as a sink for particulate matter [total suspended solids and particulate organic carbon (POC)] and a source of dissolved organic carbon (DOC) and chlorophyll‐a. 5. Autochthonous primary production of 4.2 t C day^?1 in the side‐arm was equivalent to about 20% of the allochthonous inputs of 20 t C day^?1 (POC and DOC) entering the area at mean flow (1% of the discharge of the main channel). Pelagic photosynthesis was generally high at mean flow (1.3–3.8 g C m^?2 day^?1), and contributed up to 90% of system productivity. During long stagnant periods at low discharge, the side‐arm was controlled by biological processes and a shift from planktonic to benthic activity occurred (benthic primary production of 0.4–14 g C m^?2 day^?1). 6. The transformation of the organic matter that passes through the side‐arm under different hydrological conditions, points to the importance of these subsystems in contributing autochthonous carbon to the food web of the main channel.     

湘江鳡仔稚鱼个体和耳石生长发育研究

2008 年6 月至7 月间于鳡(Elopichthys bambusa Richardson)的主要繁殖季节在湘江采集鳡仔稚鱼共370尾, 耳石分析表明这些仔稚鱼日龄在4-25d 间, 推算孵化日期为5 月27 日至6 月22 日。仔鱼前弯曲期向弯曲期转化时间为第6 日龄, 弯曲期向后弯曲期转化为第10 日龄, 后弯曲期向稚鱼期转化为15.5 日龄。体长生长和耳石生长均在进入后弯曲期后(12-13 日龄)出现1 个节点: 节点后体长生长速度是节点前的5 倍,节点后耳石生长速度是节点前的2 倍。早期生活史不同阶段鳡微耳石形态显著改变: 前弯曲期耳石为圆形;弯曲期耳石前后轴的生长速度明显超过背腹轴生长, 耳石也变为椭圆形; 后弯曲期耳石进一步延长, 耳石后端形成略尖的突起, 耳石呈梨形; 进入稚鱼期后, 耳石后突起变得较为平滑, 耳石形状呈贝形。耳石半径和体长的关系在后弯曲期阶段出现节点, 节点前后呈不同的直线关系。       

Water loss and viability in Zizania (Poaceae) seeds during short-term desiccation

How Texas wild rice, Zizania texana, became isolated in the San Marcos River of Central Texas, hundreds of kilometres from other wild rice populations is not known. Zizania seeds are intolerant of short-term desiccation. Seeds desiccated at 14% relative humidity (RH) and 75% RH do not survive after only 5-6 d and 2-3 wk of drying. Water loss is rapid and reaches a maximum at the time of seed death due to drying. And although all Zizania seeds germinate well following a long, cold dormancy period, Z. texana seeds readily germinate in the isothermic water (22°C) of the San Marcos River and Springs without an obligate, cold dormant period. Within 30-60 d of collection, Z. texana seeds germinate in substantial numbers, unlike seeds of Z. palustris, which require a long, cold dormant period. The Texas population of Z. texana may represent a relict population of a once more widely dispersed wild rice population, since the San Marcos springs probably have never gone dry.     

不同生境条件下滨海芦苇湿地C、N、P化学计量特征

为阐明不同生境对黄河三角洲滨海芦苇湿地土壤和植物碳(C)氮(N)磷(P)含量及生态化学计量特征的影响,选取新生湿地和退耕湿地两种湿地类型为研究对象,对土壤和植物体C、N、P含量及其化学计量特征进行研究。研究表明:1)退耕芦苇湿地土壤TC、TN的含量明显增加,TP的含量变化不大。2)新生湿地和退耕湿地土壤R_(C、N、P)分别为42.6:1.6:1、71.2:2.0:1,R_(NP)低于全球平均水平(13.1)和我国平均水平(5.2),土壤表现为N限制。新生湿地土壤剖面中,R_(CN)和R_(CP)变化剧烈;R_(NP)值随深度的增加而减小;退耕湿地土壤R_(C、N、P)值规律性较好,R_(CN)随深度的增加而变大,R_(CP)和R_(NP)值随深度的增加而减小。3)新生湿地和退耕湿地中芦苇整株R_(CN)、R_(CP)和R_(NP)平均值分别为78.2、1753、22.4;67.0、1539、23.0。开垦活动可以降低芦苇植物体R_(CN)和R_(CP)值,但由于芦苇植物体本身对R_(NP)的约束性较高,对R_(NP)值的影响不大,芦苇植株R_(NP)约为23。以上结论可以为黄河三角洲国家级自然保护区正在进行的湿地保护与恢复工作提供借鉴和参考。     

辽西大凌河流域生态安全评价

生态安全包括自然生态安全、经济生态安全和社会生态安全,尤指自然和半自然生态系统的安全,即生态系统完整性和健康的整体水平反映.通过专家评议,从生态系统的状态-压力-效应3个方面选取28项指标,对辽西大凌河流域不同时期的生态安全进行综合评价.结果表明,1987年(7.48)与2002年(7.51)大凌河流域生态安全处于良好状态,但2002年面临的生态压力比1987年增加了32.5%.1987～2002年大凌河流域生态安全水平没有显著下降的主要原因是朝阳市政府实施了大规模的小流域治理.大凌河流域2002年生态状态和生态效应分别是1987年1.29和1.42倍.     

Evidence of a genetically distinct population of Vrljika softmouth trout Salmo obtusirostris Heckel evolved by vicariance

Mitochondrial DNA haplotypes (control region, partial cytochrome b and ATPase6 genes) indicate a sister relationship between Vrljika and Neretva softmouth (Adriatic) trout Salmo obtusirostris . This relationship was supported by a tree of individuals based on microsatellite results [allele sharing distances ( D _AS)], which revealed three distinctive clusters, corresponding to Jadro softmouth, Neretva brown trout Salmo trutta and Neretva softmouth trout. Within the latter taxon, Vrljika trout are clearly separated from other trout. The genetic results contradict the synonymy of Jadro with Vrljika softmouth trout, as recently proposed in the Red Book of Freshwater Fish in Croatia. Vrljika softmouth trout appear to have originated from a vicariance that split a common ancestor into large (Neretva) and small (Vrljika) fragmented populations 135 000–270 000 years ago. Vrljika softmouth trout can be distinguished by an array of derived phenotypic and molecular character states. For conservation, this population should be recognized formally at the same taxonomic level as the other geographically separated populations of softmouth trout.