Response of instream animal communities to a short-term extreme event and to longer-term cumulative impacts in a strategic water resource area,South Africa

Disturbance plays an integral part in generating heterogeneity required for ecosystem persistence, but the increased amplitude and duration of disturbances linked to drivers of global change could result in ecosystem shifts or collapse. Biomonitoring over time provides insights into trajectories of ecosystem change. The responses of two instream animal taxa to two contrasting disturbance events, a major flood event and the long-term cumulative effects of land-use changes, were assessed in 1999–2012 by quantifying variation and change in abundance of functional groups based on flow rate sensitivity, water quality and metrics of ecological condition. All metrics recovered to pre-flood conditions within seven months after the flood event. Similarly, cumulative impacts of land use effected significant decreases in some but not all metrics. Indices that did not change, including SASS total score and ASPT, were the result of insufficient consideration of the decrease in the abundance of sensitive taxa specifically, and the abundance of all taxa in general. The decrease in abundance of sensitive taxa could signal imminent collapse in certain metrics. Evidence is also provided for a shift in the structure of fish assemblages linked to the decrease and loss of taxa sensitive to ecosystem degradation caused by the longer-term impacts of land-use change.     

辽宁省菜田生态系统组分优势值与系统优势度分析

辽宁省菜田生态系统组分优势值与系统优势度分析周宝利，葛晓光李宁义（沈阳农业大学园艺系，１１０１６１）（沈阳市城建中专，１１００１３）ＡｎａｌｙｓｉｓｏｎＳｕｐｅｒｉｏｒｉｔｙＶａｌｕｅａｎｄＤｏｍｉｎａｎｃｅＤｅｇｒｅｅｏｆＶａｒｉｏｕｓＣｏｍｐｏｎ...     

辽宁省地表温度时空变化及影响因素

地温是评价气候变化的重要指标,对土壤的成分、结构以及形成和演化都具有很大影响。分析地温自身的时空变化规律以及与气候间的相互关系,对深入了解地气间相互作用的机理、明确气候变化的响应规律、预测未来地温的发展趋势等方面具有重要的科学意义。辽宁省位于内蒙古高原向渤海湾的过渡地带,地形地势复杂,此外辽宁省又处在季节性冻土区,地温的变化机制更具复杂性。利用辽宁省24个气象站点1960—2016年0cm地温(地表温度)数据和各气象要素(气温、日照时数、风速、降水量)数据资料,采用气候倾向率法、Mann-Kendall突变分析、小波周期分析等方法,系统的分析辽宁省地表温度的时空变化特征以及与气候要素间的关系。结果表明:辽宁省地表温度年际变化随时间向暖趋势发展,气候倾向率达0.36℃/10a,不同年代际存在不同的变化趋势,其中20世纪60—80年代低于多年平均地表温度,90年代至21世纪10年代高于多年平均地表温度,此外冬季地表温度增温幅度最大;突变分析显示在1995年发生突变,经检验其升高趋势显著;经周期分析显示辽宁省年地表温度具有30—46a和19—25a的两种时间尺度的周期变化;年地表温度呈西南向东北逐渐降低分布特征。相关分析表明,地表温度与气温的相关性最大,并且其大小在整个区域内呈西高东低的分布特点;在与降水的关系中,降水量高的年份地表温度均比较低,夏季受降水和日照时数的影响最显著,地表温度与风速均呈负相关,但夏季相关性较小,考虑夏季地表温度主要是受气温、日照和降水共同的作用,弱化了风速对地表温度的影响。     

山西省健康人群的肠道菌群组成特征

目的探索山西省健康人群的肠道菌群组成特征及性别和年龄对肠道菌群组成的影响。方法应用16S rRNA基因测序技术,对山西省99名健康个体的粪便细菌DNA进行测序分析。结果山西省健康人群的肠道菌群在属水平分为两个集群,相对丰度最高的分别是拟杆菌属和普氏菌属;在区分这两个集群中,拟杆菌属与普氏菌属的曲线下面积（AUC）分别是0.97、1.00。男性组与女性组的物种丰富度（richness）和多样性（diversity）差异都无统计学意义（均P>0.05）,基于Bray-Curtis距离的主坐标分析（PCoA）图显示两组人群的样本分布没有明显分离（相似性分析：r=-0.0296,P>0.05）,LEfSe分析显示与性别分组有关的细菌很少。30-39岁、40-49岁和50-59岁三组人群的物种丰富度和多样性差异都无统计学意义（均P>0.05）,基于Bray-Curtis距离的PCoA图显示三组人群的样本分布没有明显分离（相似性分析：r=0.0109,P>0.05）,LEfSe分析显示几乎没有与年龄分组有关的细菌。结论山西省健康人群的肠道菌群更倾向分为两种肠型（拟杆菌型和普氏菌型）。性别对肠道菌群组成可能没有显著影响,30-59岁人群的肠道菌群组成比较稳定     

湖南省种子植物3种新记录

报道了湖南省种子植物分布新记录3种,隶属于3科3属,分别为浙江冬青Ilex zhejiangensis C.J.Tsengex S.K.Chen&Y.X.Feng、长匍通泉草Mazus procumbens Hemsl.和纤叶钗子股Luisia hancockii Rolfe。凭证标本均存于中南林业科技大学森林植物标本室(CSFI)。     

辽宁鸟类分布新记录5种:小鸦鹃、雪鹀、 红翅凤头鹃、宝兴歌鸫和黄眉姬鹟北大核心CSCD

近年来,随着观鸟活动和鸟类科研工作在辽宁的持续开展(Baietal.2015,汤姆·滨客2016),辽宁各地不断发现鸟种分布新记录种(白清泉等2019)。2012至2020年间,在丹东、大连、抚顺等市先后发现小鸦鹃(Centropus bengalensis)、雪鹀(Plectrophenax nivalis)、红翅凤头鹃(Clamator coromandus)、宝兴歌鸫(Turdus mupinensis)和黄眉姬鹟(Ficedula narcissina)5种,经查阅相关资料(邱英杰等2006,郑光美2017),确定为辽宁省鸟类分布新记录种。     

本溪关门山国家森林公园游客行为特征

研究游客行为特征对于旅游资源的开发、管理以及旅游目的地的可持续发展具有重要的作用。以本溪关门山国家森林公园为研究对象,通过问卷调查的方法对游客的人口统计学特征、地域结构特征、一般行为特征、消费特征及感知特征进行了研究。结果表明:关门山国家森林公园的游客以较高学历的男性中青年为主;客源主要来自本省辽宁,并以沈阳、本溪和大连的游客为主,客源地理集中度指数为35.71;旅游的主要目的是观赏枫叶,出游时间大部分集中在每年"十一"黄金周期间,且半数以上为当日往返的短程游览者;游客偏好与家人一起出游的旅行方式,所选择的交通工具主要为自驾车和旅游专车;游客的消费结构不平衡,主要集中于景区门票和交通费,占总消费的56.7%;游客对景区的喜好度依次为龙门峡景区月台子景区小黄山景区夹砬子景区鸣翠谷景区。总的来说,游客满意度较高,有89.1%的游客愿意重游此地,游客最不满意的地方主要表现在景区卫生方面。基于调查研究结果,对关门山国家森林公园的开发建设和可持续发展提供了相关建议。     

河北省大鸨的分布与保护

报道并探讨了河北省在大鸨迁徙途径中的重要性,河北省大鸨的地理分布与居留期变化,大鸨的保护工作及其保护与研究展望,指出河北省是大鸨重要的越冬地.     

辽宁省虫生真菌的2个新记录种

报道了在辽宁省丹东市白石砬子国家自然保护区采集到的2个辽宁省新记录种,即虫草科(Cordycip-itaceae)的下垂虫草(Cordyceps nutans Pat.)和日本棒束孢(1sariajaponica Yusuda),并描述了其形态特征和生境分布.     

A reconstruction of Palaeo‐Macaronesia,with particular reference to the long‐term biogeography of the Atlantic island laurel forests

Macaronesia is a biogeographical region comprising five Atlantic Oceanic archipelagos: the Azores, Madeira, Selvagen (Savage Islands), Canaries and Cape Verde. It has strong affinities with the Atlantic coast of the Iberian Peninsula and the north‐western fringes of Africa. This paper re‐evaluates the biogeographical history and relationships of Macaronesia in the light of geological evidence, which suggests that large and high islands may have been continuously available in the region for very much longer than is indicated by the maximum surface area of the oldest current island (27 Ma) – possibly for as long as 60 million years. We review this literature, attempting a sequential reconstruction of Palaeo‐Macaronesia from 60 Ma to the present. We consider the implications of these geological dynamics for our understanding of the history of colonization of the present islands of Macaronesia. We also evaluate the role of these archipelagos as stepping stones and as both repositories of palaeo‐endemic forms and crucibles of neo‐endemic radiations of plant and animal groups. Our principal focus is on the laurel forest communities, long considered impoverished relicts of the Palaeotropical Tethyan flora. This account is therefore contextualized by reference to the long‐term climatic and biogeographical history of Southern Europe and North Africa and by consideration of the implications of changes in land–sea configuration, climate and ocean circulation for Macaronesian biogeography. We go on to provide a synthesis of the more recent history of Macaronesian forests, which has involved a process of impoverishment of the native elements of the biota that has accelerated since human conquest of the islands. We comment briefly on these processes and on the contemporary status and varied conservation opportunities and threats facing these forests across the Macaronesian biogeographical region.