小兴安岭黑河胜山林区冬季驼鹿的生境选择

2002年、2003年和2004年的12月至3月,在小兴安岭黑河胜山林场开展了驼鹿生境选择的研究。研究中选择了9类与驼鹿生境选择相关的生态因子：植被型、离公路距离、离采伐点距离、平均雪深、隐蔽程度、坡向、坡位、坡度、海拔,运用SPSS软件进行交叉汇总定量分析。结果表明,胜山驼鹿冬季以落叶阔叶林、灌丛为主要生境,影响驼鹿分布的主要生态因子为隐蔽程度、坡位,其次为雪深、坡向、离采伐点距离、离公路距离,坡度、海拔对驼鹿分布的影响不明显。     

天山南麓山前平原柽柳灌丛地上生物量

基于天山南麓山前平原柽柳灌丛样地调查和实验,研究了柽柳的地上生物量及其分布规律.结果表明,不同地貌带柽柳的地上生物量差异较大.在溢出带,柽柳的地上生物量最大,达1428.53 kg·hm^-2,其次是三角洲带和洪水剥蚀带,柽柳的平均地上生物量分别为745.97和544.37 kg·hm^-2,而两河交汇区柽柳的地上生物量最小,仅为111.18 kg·hm^-2.造成这种差异的主要原因是不同地貌带柽柳的密度不同.在轮台天山南麓山前平原4个地貌样带中,柽柳的地上生物量与表层土壤盐分含量均随地下水埋深的增加而下降,呈良好的相关性,但土壤盐分并不是影响柽柳地上生物量的主要因素,影响柽柳生长的主要生态因子是地下水埋深.     

火干扰对大兴安岭北部原始林下层植物多样性的影响

在景观尺度自然火干扰历史研究的基础上,采用1个物种丰富度指数（物种数 S）、2个均匀度指数（Pielou均匀度指数Eh＇和Alatalo均匀度指数E）、3个物种多样性指数（Shannon-Wiener指数H＇,Hill多样性指数N1和N2）共6个？多样性指数,研究了长期火干扰与最近一次火干扰对大兴安岭北部原始林下木层、草本层及下层总体的植物多样性的影响.研究结果表明,本区下层植物的物种数、均匀度指数和多样性指数都以下木层显著大于草本层,因而下木层对下层植物总体生物多样性的贡献最大,也是主要影响因子.火干扰对下木层、草本层和下层总体的物种丰富度和物种多样性有显著影响,而对均匀度的影响不显著.长期的火干扰影响下,下木层、草本层和下层总体的物种数、各类均匀度指数和物种多样性指数都呈现如下格局：高频类＞中频类＞低频类,低强类＞中强类＞高强类.最近一次火干扰影响下,各个生物多样性指数都表现为一致的趋势：低强类＞中强类＞高强类;短期类＞长期类＞中期类.下层植物多样性与火干扰的关系是长期适应的结果.     

Habitat Assessment, Phytosociology and Conservation of the Tunbridge Filmy-fern Hymenophyllum tunbrigense (L) Sm. in its Isolated Locations in the Vosges Mountains

The Tunbridge Filmy-fern, Hymenophyllum tunbrigense, has been discovered within the last 10 years in several places in a 15 km long by 2 km wide area located in the western part of the Vosges Mountains. After the disappearance of the Saxony and Ardennes sites, these Vosgian locations have to be considered as one of the last continental areas for this fern in Europe, meriting the same level of interest as the well-known Luxembourg locations. In its Vosgian area, the fern occurs in Abies alba forests on small (less than 2.5 m high) and moist sandstone rocks, generally located near running water in wet valleys, at altitudes between 400 and 640 meters a.s.l. As assessed through the impact of the 26 December 1999 storm on one Hymenophyllum location, this fern appears to be sensitive to direct sunlight in the Vosges mountains. Therefore the main measure to ensure its conservation would be to maintain a dense and permanent forest canopy above the Hymenophyllum sites in order to avoid any direct sunlight.     

Gene lineages and eastern North American palaeodrainage basins: phylogeography and speciation in salamanders of the Eurycea bislineata species complex

Contemporary North American drainage basins are composites of formerly isolated drainages, suggesting that fragmentation and fusion of palaeodrainage systems may have been an important factor generating current patterns of genetic and species diversity in stream-associated organisms. Here, we combine traditional molecular-phylogenetic, multiple-regression, nested clade, and molecular-demographic analyses to investigate the relationship between phylogeographic variation and the hydrogeological history of eastern North American drainage basins in semiaquatic plethodontid salamanders of the Eurycea bislineata species complex. Four hundred forty-two sequences representing 1108 aligned bases from the mitochondrial genome are reported for the five formally recognized species of the E. bislineata complex and three outgroup taxa. Within the in-group, 270 haplotypes are recovered from 144 sampling locations. Geographic patterns of mtDNA-haplotype coalescence identify 13 putatively independent population-level lineages, suggesting that the current taxonomy of the group underestimates species-level diversity. Spatial and temporal patterns of phylogeographic divergence are strongly associated with historical rather than modern drainage connections, indicating that shifts in major drainage patterns played a pivotal role in the allopatric fragmentation of populations and build-up of lineage diversity in these stream-associated salamanders. More generally, our molecular genetic results corroborate geological and faunistic evidence suggesting that palaeodrainage connections altered by glacial advances and headwater erosion occurring between the mid-Miocene and Pleistocene epochs explain regional patterns of biodiversity in eastern North American streams.     

The lateglacial vegetation and radiocarbon dating of Lake Trilistnika, Rila Mountains (Bulgaria)

Pollen analysis, supplemented by 5 ¹⁴C dates, was carried out on the lateglacial section (160 cm) of a core retrieved from the glacial Lake Trilistnika (2216 m) in the northwestern Rila Mountains (Bulgaria). The reconstruction of the lateglacial vegetation history is linked for the first time to a chronological framework for the time window 13000–10000 b.p. The delimitation of an interstadial/stadial cycle, analogous with the Bølling/Allerød-Younger Dryas from Western Europe, is based on important changes in the pollen stratigraphy. Mountain-steppe vegetation composed of Artemisia, Chenopodiaceae, Poaceae and other cold-resistant herbs, with isolated stands of Pinus and Juniperus-Ephedra shrubland, dominated the landscape after the ice-retreat. Interstadial conditions were established before 12815±130 b.p. The spread of tree vegetation at lower elevation as a response to the climate improvement was confined to the time interval 12110±95–11140±75 b.p. The Younger Dryas stadial is characterised by a re-advance of the mountain-steppe vegetation. The results are compared with other sites of lateglacial age from the high mountains (Rila, northern Pirin, western Rhodopes) in southern Bulgaria.     

A new species of Noccaea (Brassicaceae) from South Anatolia, Turkey

Noccaea camlikensis sp. nov. (Brassicaceae) is described and illustrated from a localized serpentine range in southern Turkey. Its close relationship to N. cariensis , from which it differs in leaf and carpological characters, is discussed. The protologue of this fairly unknown species can now be amended to cover better the morphological variability of this taxon. A comparative study of seed-coat anatomy advocates its move from Thlaspi to Noccaea ; the relevant combination N. cariensis (Carlström) Parolly, Nordt & Aytaç is made. The ecology of both vicarious species is discussed and their distribution mapped.  © 2006 The Linnean Society of London, Botanical Journal of the Linnean Society , 2006, 150 , 409–416.     

秦岭川金丝猴群在非移动时的空间结构

本研究在个体识别的基础上 ,采用瞬时扫描取样法 (Instantaneousandscansampling)和行为的全事件取样法 (Alloccurrencesampling) ,对秦岭川金丝猴 (Rhinopithecusroxellana)的一个投食群的空间结构进行研究。发现秦岭川金丝猴社群的空间结构是以类似于“家庭”的社会单元为基本单位 ,属于同一社会单元的个体主要集中在同一棵树上 (占观察频率的 6 0 6 % ) ,其次是在距离相近的两棵树上 (占 2 9 1% ) ,个体间的直线距离通常保持在 0 - 10m之间 ,主要是在 0 - 5m之间 ,不同的社会单元个体间的空间直线距离主要集中在 10 - 30m之间 ,通常是在 2 0 - 2 5m之间 ,明显大于同一社会单元的个体间的空间直线距离 ,这些研究结果可以作为一种野外鉴别猴群社会单元的尺度 ,供未来的研究人员参考。通过对空间形状近似圆形的猴群进行分层 ,统计表明高社会等级的单元常出现在猴群的内层和中层内侧 (df =1,χ2 =16 6 97,P <0 0 0 5 ) ,中社会等级的单元主要出现在猴群的中层 (df=1,χ2 =2 1 5 4 ,P <0 0 0 5 ) ,而低社会等级的单元出现在猴群的外层 (df =1,χ2 =12 6 0 ,P <0 0 0 5 ) ;等级较高的单元在猴群中占有的空间大小与空间质量也较高 ,随着单元社会等级的降低 ,其占有空间的大小与质量也随之降低 ;变化的     

天山乌鲁木齐河源区3．6ka BP以来的植被变化和环境变迁：以大西沟剖面为例

天山乌鲁木齐河源区大西沟剖面孢粉鉴定结果表明：在3．6～3．2ka BP,该区气候较今温暖湿润;在3.2～2．0ka BP,气候变为寒冷干燥,这一时期乌鲁木齐河源地区曾出现一次冰进;在2．0～1．4ka BP,气候又转为暖湿;在1．4～0．5ka BP,出现了3．6ka BP以来气候最适宜的时期。整个剖面自下而上都有一定量的淡水水生植物出现,这反映了该剖面3ka BP以来一直处于淡水沼泽的环境中。通过对云杉属生态习性、传播特性等综合分析,认为剖面中的云杉丰值可能与林线上移、山谷风搬运以及冰川退缩等有一定的相关性。通过对孢粉样品中炭屑浓度统计以及磁化率测试结果的综合研究,提出在0．5ka BP左右,该地区可能出现过多次火灾;炭屑的峰值可能与人类活动有关。