永定河流域大型底栖动物功能摄食类群时空分布及生态评价

2017年春季(4月)、夏季(7月)、秋季(11月)对永定河流域23个样点的大型底栖动物、水环境和水文因子进行了野外调查,分析了永定河流域大型底栖动物功能摄食类群的群落组成与时空分布特征及其对河流生境变化的响应情况。永定河流域3个季节共采集到大型底栖动物78种,隶属3门6纲39科,其中,春季52种、夏季50种、秋季53种,功能摄食类群以收集者占绝对优势,其次为捕食者,刮食者、滤食者、撕食者所占比例极低。3个季节优势种均属于收集者类群,春季优势种为直突摇蚊属、流水长跗摇蚊属、环足摇蚊属,夏季优势种为雕翅摇蚊属,秋季优势种为多足摇蚊属、摇蚊属、直突摇蚊属。冗余分析结果表明: 水温、流速、盐度以及总磷是影响春季大型底栖动物功能摄食类群的主要影响因子;总磷、溶解氧、电导率以及流量是夏季大型底栖动物功能摄食类群的主要影响因子;总磷和溶解氧是影响秋季大型底栖动物功能摄食类群的主要影响因子;总磷在春、夏、秋季均与收集者类群表现出正相关性,表明永定河流域大型底栖动物功能摄食类群受到了水质污染的影响。基于功能摄食类群参数的评价表明:1)物质循环方面,妫水河初级生产力显著高于其他区域,秋季大于其他季节;洋河次级生产力和分解能力显著高于其他区域,春季大于其他季节,但洋河自养/异养作用显著低于其他区域,春季小于其他季节;2)纵向输入能力方面,桑干河显著高于其他区域,秋季大于其他季节;3)沿岸物质的输入方面,妫水河显著高于其他区域,夏季大于其他季节。     

长江宜昌段桥边河大型底栖动物功能摄食类群时空分布特征

研究河流生境时空变化对大型底栖动物功能摄食类群的影响,分析底栖动物功能摄食类群对环境因子的响应关系,对评估河流生态系统健康具有重要意义。以长江支流桥边河为研究对象,基于2020年8月、2021年1月和2021年4月对桥边河大型底栖动物和水体理化因子的调查数据,分析了大型底栖动物功能摄食类群的构成以及时空分布特征。结果表明：共采集到大型底栖动物3门38种,包括节肢动物门23种、软体动物门13种、环节动物门2种。桥边河大型底栖动物功能摄食类群中滤食者占绝对优势,其次为刮食者、捕食者、撕食者和收集者。滤食者的优势种为闪蚬和河蚬,刮食者的优势种为方格短沟蜷、铜锈环棱螺和卵萝卜螺,捕食者的优势种为河蟌,撕食者的优势种为秀丽白虾,收集者的优势种为黄色羽摇蚊。冗余分析（RDA）表明,影响桥边河大型底栖动物功能摄食类群的主要环境因子为溶解氧（DO）、氨态氮（NH₄⁺-N）、水深（Dep）、pH、温度（T）和硝态氮（NO₃^--N）。研究大型底栖动物功能摄食类群组成和时空分布特征,可为河流生态系统修复提供参考依据。     

漓江大型底栖动物功能摄食类群时空分布及生态效应

基于2009年9月至2012年8月期间对漓江上中下游3个河流区段的4次采样调查,分析了漓江大型底栖动物功能摄食类群的组成与时空分布状况及其对河流生境变化的响应情况。结果表明:漓江大型底栖动物以刮食者占据绝对优势,其次依次是滤食者、收集者、捕食者和撕食者。刮食者中优势种为中华园田螺和黑龙江短沟蜷,滤食者中优势种为河蚬和纹石蚕,收集者中优势种为小蜉和摇蚊幼虫,捕食者中优势种为扁舌蛭和蜻蜓幼虫,撕食者中优势种为泥甲。根据功能摄食类群参数对河流生境以及人类活动影响的评价表明,人类居住生活对生境稳定性的影响显著大于旅游观光带来的影响,环境因子中溶解氧(DO)、pH、电导率(EC)、温度(Temp)、浊度(Tur)、化学需氧量(COD)和总氮(TN)等环境因子与漓江大型底栖动物功能摄食类群的相关性均较强。     

太子河大型底栖动物摄食功能群对河岸带土地利用类型的响应

为研究太子河大型底栖动物摄食功能群对河岸带土地利用类型的响应关系,于2012年5月对太子河流域底栖动物和水环境因子和土地利用类型进行野外调查及数据分析。结果表明：1）太子河流域底栖动物群落在4种不同土地利用类型内具有极显著差异,平均丰度、Shannon-Wiener多样性指数和Pielou均匀度指数在森林用地中最高,分别为8.86、0.73和0.94,平均密度在森林耕作用地中最高（782.75个/m²）,除食碎屑者功能群（S）,其他摄食功能群在不同土地利用类型内无差异（P > 0.05）。2）太子河土地利用类型与水环境因子之间的Pearson分析表明,森林用地与EC、TDS、TN、NH₃-N、COD_Mn之间呈显著负相关性,与DO、IOS之间呈显著正相关性;耕地与DO和IOS之间呈显著负相关性;城镇用地与EC、TDS和TN之间呈正相关性。3）太子河土地利用类型与底栖动物功能群之间的Spearman分析表明森林用地与食碎屑者（S）、刮食者（SC）和收集者（GC）呈正相关性。耕地与食碎屑者（S）、滤食者（FC）之间呈负相关性,城镇用地与刮食者（SC）和收集者（GC）之间呈显著负相关性。4）底栖动物功能群和水环境因子之间的典范对应分析表明,食碎屑者（S）功能群主要受底质指数（IOS）驱动,其他功能群与环境因子之间无相关性。因此,水环境因子和底栖动物群落参数比摄食功能群更能反映人类活动对土地利用的改变,水环境和底栖动物群落研究可为河岸带土地利用保护提供理论依据。     

济南河流大型底栖动物摄食功能群多样性及时空动态

2014年春季(5月)、夏季(8月)和秋季(11月)对济南地区24个样点的大型底栖动物和水环境理化因子进行了野外调查。利用多样性指数以及典范对应分析等方法,分析了大型底栖动物群落组成和空间结构特征。结果表明:共采集到大型底栖动物3门57种,分别为节肢动物门、软体动物门和环节动物门。春季、夏季和秋季采集到大型底栖动物45种、35种和33种,春季优势种为霍甫水丝蚓(Limnodrilus hoffmeisteri)和豆螺(Bithynia fuchsiana),夏季优势种为溪流摇蚊(Chironomus riparius)和豆螺(Bithynia fuchsiana),秋季优势种为喜盐摇蚊(Chironomus salinarius)和豆螺(Bithynia fuchsiana)。春季、夏季和秋季密度平均值为2.49×10~3、0.56×10~3、1.03×10~3个体/m~2;生物量平均值为495.59、137.26、109.45 g/m2;Shannon-Wiener指数平均值分别为1.37、1.33和1.17;均匀度指数平均值分别为0.55、0.67和0.59。全地区共划分出大型底栖动物功能摄食类群5类,春季收集者种类最多为20种,夏季刮食者种类最多为12种,秋季收集者与刮食者种类最多为11种,3个季节中收集者密度均占绝对优势,其次为刮食者。典范对应分析表明,春季影响黄河流域和淮河流域大型底栖动物功能摄食类群的主要环境因子是总磷和总氮;夏季影响黄河流域和淮河流域大型底栖动物功能摄食类群的主要环境因子是pH和溶解氧;秋季影响黄河流域和淮河流域大型底栖动物功能摄食类群的主要环境因子是溶解氧和pH。     

外来植物凋落物分解对底栖动物多样性及其摄食功能群的影响

在亚热带地区一条2级溪流中比较了本地植物(红锥和薏米)和外来植物(托里桉和马缨丹)凋落物的分解速率及底栖动物定殖及其摄食功能群的组成。结果显示,本地植物凋落物的分解速率为:0.020 d-1(红锥)和0.056 d-1(薏米),外来树叶的分解速率则为:0.038 d-1(托里桉)和0.041 d-1(马缨丹),它们均属于快速分解组。定殖在外来和本地树叶凋落物上的大型底栖动物种类分别为21种和24种。在外来和本地树叶上定殖的底栖动物平均密度差异不显著(P0.05)。从大型底栖动物摄食功能群的比例来看,定殖在本地凋落物上的集食者的比例最高(73.5%),其次是撕食者(10.9%)和捕食者(8.7%),刮食者(6.8%)的比例最低,在外来凋落物上,摄食功能群的比例分别为集食者(67.6%)、撕食者(13.9%)、刮食者(12.1%)和捕食者(6.1%),两者相比,底栖动物的摄食功能群均以集食者和撕食者为主,在组成比例上并无显著差异。结果表明2种外来植物凋落物分解对底栖动物多样性及其摄食功能群的影响不明显。     

长白山源头溪流底栖动物群落结构季节动态

源头溪流是河流生态系统物质循环和能量流动的重要区域,对底栖动物的生物多样性维持具有重要意义。目前,针对我国源头溪流底栖动物群落结构的研究薄弱,对长白山源头溪流底栖动物季节动态的研究尚未见报道。采用野外原位定量取样的方法,力图阐释长白山源头溪流底栖动物群落结构的季节动态特征及其主要环境驱动因子。研究结果表明:(1)共计采集底栖动物90个分类单元,隶属于3纲9目38科。其中,水生昆虫85属,占绝对优势。底栖动物群落结构的季节动态明显,底栖动物密度及多样性在夏、秋季显著高于冬季和春季,并在冬季达到最低值。(2)底栖动物功能摄食类群以收集者占优势,其次为撕食者、捕食者和刮食者,滤食者相对丰度最低。不同功能摄食类群的季节动态不一致,但密度和物种丰富度整体表现为秋季最高。(3)水温、凋落叶分布和流速是长白山源头溪流底栖动物群落结构季节动态的主要环境驱动因子。本研究可为长白山源头溪流后续相关研究及长白山松花江水系生态修复提供基础数据支持及参考。     

香溪河大型底栖动物群落结构季节动态

通过大型底栖动物的量化监测,对香溪河水系大型底栖动物季节动态进行研究.共采集大型底栖动物197种,隶属6纲68科,其中,四节蜉、高翔蜉、短尾石蝇为该水系优势类群,不同季节间大型底栖动物优势类群组成存在较大差异.大型底栖动物群落结构以冬季最为复杂,春、秋季次之,夏季相对简单.大型底栖动物功能摄食类群以集食者占优,其次为刮食者、捕食者和滤食者,撕食者丰度最小.典型对应分析表明,不同季节影响底栖动物群落结构的因子差异较大;夏季和秋季营养盐对底栖动物群落结构影响较大,水深对各季度大型底栖动物群落结构均有影响.     

香溪河水系大型底栖动物功能摄食类群生态学

2004年7月至2007年6月,通过大型底栖无脊椎动物的量化监测,对三峡水库湖北库区最大河流香溪河大型底栖无脊椎动物功能摄食类群生态学进行研究.结果表明:香溪河大型底栖动物以收集者占绝对优势,其次为刮食者,捕食者、滤食者、撕食者相对丰度较小;各功能摄食类群分布明显受时空资源位的限制;香溪河物质循环能力、两岸物质的输入量和粗有机颗粒/ 细有机颗粒在九冲河明显高于其它河流,在冬季高于其它季节;物质输送能力以高岚河最高,在时间方面以冬季明显高于其它季节.逐步回归分析表明,流速、电导、浊度、总氮、二氧化硅对香溪河河流生态系统物质循环具有指示作用;二氧化硅和化学需氧量对物质输送能力具有指示作用;水温、水深、二氧化硅、总磷可作为沿岸物质输入量的指标;水温、二氧化硅可作为评估河道中粗、细有机颗粒比例的重要指标.     

云南省把边江流域不同土地利用方式对大型底栖动物群落的影响

研究土地利用对大型底栖动物群落的影响,对流域土地利用规划修编和河流生态修复等有重要意义。以红河上游的把边江流域为研究区,调查大型底栖动物群落现状,计算37个样点上游集水区土地利用组分、配置、多样性和水文距离4个方面20个土地利用指标,分析不同土地利用方式对大型底栖动物群落的影响。本次调查共鉴定出25个大型底栖动物分类单元,其中水生昆虫最多,占分类单元总数的72%;摄食功能群以捕食者（PR）、刮食者（SC）和直接收集者（GC）为主。把边江流域城镇用地和林地对大型底栖动物群落的影响占主导地位,而耕地对大型底栖动物群落的影响较小。影响把边江流域大型底栖动物群落的关键土地利用指标为城镇用地面积比（3PLA）、城镇用地最大斑块指数（3LPI）、城镇用地聚合指数（3AI）、城镇用地水流长度（3FLOW）、林地最大斑块指数（1LPI）和林地形状指数（1LSI）。土地利用组分、配置和水文距离是影响把边江流域大型底栖动物群落的主要方面,而土地利用多样性对大型底栖动物群落的影响较小。大型底栖动物物种密度和物种多样性与3PLA、3LPI、3AI、3FLOW和1LSI呈负相关,与1LPI呈正相关。1LPI与浮游目（如小蜉科、扁蜉科）为代表的清洁物种呈现较明显的正相关关系。城镇用地指标与SC和SH（撕食者）密度具有显著的负相关关系,与GC密度有较弱的正相关关系,而与其他功能群没有明显的相关关系。SC和SH对水质和环境条件敏感,而GC对人类干扰耐受性较强。1LPI与SC和FC（滤食收集者密度）正相关,而与PR和GC密度负相关。SC和FC对生境的完整性要求较高,而GC和PR对人为干扰和较为破碎的生境更为适应。一方面,随着城镇用地的规模、边界复杂性和聚集程度增加,研究区大型底栖动物密度和多样性降低;另一方面,随着林地完整性降低,大型底栖动物物种均匀度降低。土地利用与大型底栖动物物种多样性和功能群多样性的关系不完全一致,1LSI和3FLOW与物种多样性负相关,而与功能群多样性呈正相关关系,土地利用对物种-功能群-群落不同尺度上的影响差异还需要更深入的研究。     

Macroinvertebrates on Eichhornia crassipes roots in two lakes of the Paraná River floodplain

Changes in the abundance, biomass and in the relativeproportions of functional feeding groups ofmacroinvertebrates were studied for 17 months duringlow and high water periods in two floodplain lakeswith indirect connections to the Paraná River.At low water, Eichhornia crassipes root clusterswere colonized by comparatively low densities ofmacroinvertebrates, especially in the lake moredistant to the river. Collector-gatherers andpredators were the most abundant functional feedinggroups, but different taxa of these groups dominatedin the two lakes during low water.At high water, macroinvertebrates densities increasedas a result of increased flow through the roots. Inthis period, collector-filterers dominated at bothlakes and constituted over 34% of themacroinvertebrates. Four independent variables(conductivity, hydrological periods, dissolved oxygenand site) explain 87% of the variability inmacroinvertebrates density expressed as the number ofindividuals per m2. No significant relationshipwere found between macroinvertebrate biomass and anyof the independent variables.     

Habitat preferences of Ukrainian brook lamprey Eudontomyzon mariae ammocoetes in the lowland rivers of Central Europe

The pattern of microhabitat preferences of Ukrainian brook lamprey Eudontomyzon mariae ammocoetes was examined in two rivers of central Poland: the Pilica River (the Vistula River basin) and the Grabia River (the Odra River basin). A comparison of abiotic factors of the rivers revealed differences in water speed and principal components: PC1 (determining gradient from decreasing medium sand to the increasing share of three fractions of gravel), PC2 (a gradient from the declining share of very coarse and coarse sand fractions to the growing content of fine sand) and PC3 (correlated with an increasing proportion of silt). The sites did not differ significantly in terms of water depth. Relative abundance and frequency of ammocoete occurrence in the Grabia River were higher than in the Pilica River. Only speed, PC1 and PC2 made a significant contribution to the prediction of larval occurrence. Eudontomyzon mariae larvae preferred substrata with a reduced amount of medium sand and increased content of gravel (PC1) as well as with a lower content of coarse sand and higher proportion of fine‐grained sand (PC2). The ammocoetes also preferred areas with a water speed of 0·2 m s^?1 but avoided speeds ≥0·6 m s^?1. The abundance of E. mariae was affected by water speed, as well as by all PCs. The mean ± s.e. optimal current speed was 0·265 ± 0·007 m s^?1, while abundance decreased with increasing amounts of gravel (PC1) and increased with increasing amounts of fine sand and silt in the bottom substratum (PC2 and PC3). Comparison of ammocoete microhabitat use in the Pilica and Grabia Rivers showed the lack of differences in distribution in the preferred values of current speed, PC1 and PC2.     

Effect of hydropower peaking flow fluctuations on community structure and feeding guilds of invertebrates colonizing artificial substrates in a large impounded river

Artificial substrates were used to monitor the invertebrate communities below a power peaking impoundment and a flow re-regulating impoundment on the Missouri River on northeastern Nebraska, USA. Invertebrate communities on shallow samplers subjected to exposure from diel fluctuations in flow averaged 3 taxa per sampler and 91 organisms per square meter. In the absence of diel fluctuations, number of taxa per sampler increased to 12 and mean densities increased to 743 per square meter. Fluctuating discharges had no significant effect on numbers of taxa or densities on continually submerged artificial substrates. However, greater numbers of taxa and total densities were observed on deep (107 cm) versus shallow (30 cm) samplers below both impoundments.Polycentropodidae (Trichoptera), Chironomidae (Diptera) and Oligochaeta were observed to tolerate diel fluctuations and exposure below Fort Randall Dam while Hydropsychidae (Trichoptera) and Heptageniidae (Ephemeroptera) were extremely intolerant.Collector-gatherers and predator-engulfers were the predominant functional groups colonizing samplers below both impoundments. Higher numbers of collector-gatherers, collector-filterers and scrapers were observed from samplers in the absence of diel flow fluctuations.This study corroborates results from a number of other investigations, separated in space and time. Examined collectively, these studies provide the framework for understanding power peaking as a stress to benthic stream communities.     

Community structure of Trichoptera in a mountain stream: spatial patterns of production and functional organization

SUMMARY. 1. Annual production was estimated for Trichoptera occurring in each of three distinct habitats of a mountain stream: bedrock-outcrops, riffles and pools. Production was greatest on bedrock-outcrops (2608 mg ash-free dry weight m^?2), followed by riffles (1038) and pools (950). 2. Annual production in bedrock-outcrops and pools was dominated by single functional groups, with collector-filterers and shredders contributing 73% and 75% of the annual production, respectively. Production in riffles was due primarily to shredders (46%), followed by collector-filterers (27%). 3. Taking account of the amount of stream area occupied by each habitat type, total annual production was estimated at 1336 mg AFDW m^?2. 53% of this production was attributable to four taxa: Parapsyche cardis Ross (25%), Pycnopsyche gentilis (MacLachlan) (10%), Neophylax mitchelli Carpenter (9%) and Rhyacophila nigrita Banks (9%). 4. Habitat-weighted production was distributed among functional groups as follows: collector-filterers (41%), shredders (29%), engulfing-predators (15%), scrapers (13%) and collector-gatherers (2%). 5. The distinct taxonomic and functional structures of trichopteran sub-communities were shaped by the distinct physical characteristics of their principal habitats. Bedrock-outcrops were characterized by low roughness and high current and were sites of low deposition or organic matter; thus the predominance of collector-filterers. In contrast, the other habitats of greater roughness (riffles) and/or lower current (pools) were sites of deposition of food (e.g. leaf litter) and greatest shredder production. 6. By distinguishing discrete mesoscale habitats, each with a functionally distinct caddisfly sub-community, we speculate that small mountain streams provided the diverse physical templates essential for the evolution of the major feeding tactics (e.g. scraping, shredding, filter-feeding) of the. Trichoptera.     

不同肥力条件下黑土及其有机无机复合体的腐殖质组成

采用Kumada法研究了不同肥力黑土及其复合体的腐殖质组成.结果表明,黑土培肥后,粉粒和细砂复合体含量增多;土壤及各级复合体游离态和结合态腐殖质含量得到不同程度提高,但游离态腐殖质的腐殖化度降低.这种作用在粉粒和细砂复合体中表现得更为明显.随复合体粒径增大,复合体有机碳含量、腐殖质提取率、游离态腐殖质含量及游离态胡敏酸的腐殖化度等均有降低趋势.胡敏酸分类结果表明,高肥土壤游离态胡敏酸均为R_p型,低肥则为R_p型和B型.随复合体粒径增大,游离态胡敏酸类型变化序列主要为:A型(粘粒)→B型(粉粒)→R_p型(细砂);无论粒径大小,结合态胡敏酸大多为A型.土壤培肥后,可使全土及各级复合体的游离态腐殖质的腐殖化度降低,进而会发生型变.在黑土中,游离态胡敏酸的型变主要体现在粉粒复合体中,结合态胡敏酸的型变主要体现在细砂复合体中.     

基于SWAT模型的浑河中上游水源涵养服务价值评估

浑河中上游流域的森林覆盖率高达68%,是辽宁省饮用水的重要水源保护地。本研究基于SWAT模型和影子工程法,评估2000—2019年浑河中上游流域的水源涵养量及其服务价值,并分析其时空变化的原因,以期为流域内生态补偿和生态恢复提供依据。结果表明:2000—2019年浑河中上游水源涵养量及其价值量呈先增加后减少趋势;年均水源涵养总量和水源涵养服务价值分别为24.6亿m³和150.4亿元;研究区水源涵养量存在明显的空间差异,高值区主要分布在清原县和新宾县,低值区集中于沈阳市辖区;不同生态系统的水源涵养服务价值差异较大,森林的单位面积水源涵养量远高于草地、农田和城市。     

底栖动物功能摄食类群对酸性矿山废水的响应

为研究底栖动物功能摄食类群对酸性矿山废水的响应机理及高岚河硫铁矿对香溪河生态环境的影响状况,2006年9月、11月及2007年1月、3月、5月、7月对高岚河3个河段12个样点(受损河段G1—G3、恢复河段G4—G8、对照河段D1—D4)底栖动物进行了调研,同时测定了各样点水体金属含量(Cd、Cr、Cu、Mn、Pb、Zn、Fe、Al、Ca和Mg)、pH值、电导、水温、总溶解性固体、盐度、溶氧、流速、水深、水面宽度等理化指标。对3个河段底栖动物群落功能摄食类群群落结构及理化指标进行了对比分析,结果表明,受酸性矿山废水的影响,受损河段金属含量及电导、总固体悬浮物明显高于对照河段和恢复河段,受损河段pH值显著低于其他河段;而对照河段和恢复河段各项理化指标不存在明显差异。共采集底栖动物213种,隶属7纲,59科,四节蜉(Baetis sp.)、侧枝纹石蛾(Ceratopsyche sp.)、锯形蜉(Serratella sp.)和扁蜉(Heptagenia sp.)为研究区域优势类群;功能摄食类群相对丰度收集者最大,刮食者和滤食者次之,捕食者和撕食者最小,分别为48.8%、20.6%、17.0%、9.0%、4.7%。受损河段底栖动物各功能摄食类群密度和生物多样性指数明显低于对照河段和恢复河段,且组成相对单一;刮食者对酸性矿山废水反应最为敏感。非度量多维标度排序和多响应置换过程分析表明,受损河段底栖动物各功能摄食类群群落结构同对照河段和恢复河段存在较大差异,而对照河段和恢复河段群落结构相似性较高。典型对应分析发现,矿山酸性废水的排放是影响底栖动物功能摄食类群分布的主要因素。     

Factors influencing the extent and development of the oxic zone in sediments

Dissolved oxygen concentrations in river-sediment porewaters are reported and modelled using a zero-order reaction rate and the Monod equation. After mixing the sediments and allowing settling, the dissolved oxygen profile in the bed-sediment was expected to reach a steady-state rapidly (< 1 h). However changes in the vertical profile of oxygen over a period of 38 days revealed that the penetration of oxygen increased and the dissolved oxygen flux at the interface decreased with time, probably as the oxidation kinetics of organic matter and redox reactions in the sediment changed. Experiments with three contrasting silt and sand dominated sediments (organic matter content between 0.9 and 18%) at two water velocities (ca 10 and 20 cm s^–1) showed that the dissolved oxygen profiles were independent of velocity for each of the sediments. The most important controls on the reaction rate were the organic matter content and specific surface area of the sediment. A viscous diffuse-boundary-layer above the sediment was only detected in the experiments with the silt sediment where the sediment oxygen demand was relatively high. In the coarser sediments, the absence of a diffuse layer indicated that slow oxidation processes in the sediment controlled the dissolved oxygen flux at the interface. The problem of determining a surface reference in coarse sediment is highlighted. The results are discussed with reference to other studies including those concerned with estuarine and marine sediments.