生物多样性保护优先区对重庆苔藓植物多样性保护的重要性

生物多样性保护优先区的生物多样性十分丰富, 对于生物多样性保护具有重要意义。本文基于野外调查数据和文献资料, 整合大巴山和武陵山两个中国生物多样性保护优先区重庆境内的苔藓植物名录, 通过分析物种丰富度、中国特有种和受威胁物种, 比较了这两个地区的苔藓植物组成特点和相似性。结果显示, 两个保护优先区重庆境内共有苔藓植物77科221属722种, 其物种数分别占重庆市和中国苔藓植物总种数的76.0%和23.9%。两个区域分布有中国特有苔藓植物56种, 占中国苔藓植物总种数的1.9%; 分布有极危苔藓植物1种、濒危4种和易危3种。科、属、种的Jaccard相似性系数分别为0.7、0.6和0.3, 表明两个区域物种组成差异较大。大巴山和武陵山两个中国生物多样性保护优先区都具有较高的苔藓植物物种多样性, 其种类组成具有一定代表性, 对重庆市和中国苔藓植物多样性保护具有重要价值。     

浙江西天目山30年来苔藓物种多样性变化

苔藓物种多样性变化对苔藓植物保护和森林生态系统健康起着重要的预警作用.基于1977-1980年和2010-2011年对西天目山国家自然保护区苔藓植物的两次详细调查,本文比较了该地区1977-2011年间苔藓植物物种多样性的变化.结果表明:(1)在过去的30年间,该地区苔藓植物的科、属、种数均呈下降趋势,苔类植物的属、种数减少尤为显著;(2)青藓科、曲尾藓科、灰藓科和丛藓科一直为该地区的优势科;(3)科的稳定性均高于属、种;(4)缓冲区的总物种数变化最大,新增物种数最多;核心区(进山门-老殿)苔藓植物种类始终最为丰富,两个时期的物种相似性最高,且苔类占新增物种数百分比最高;核心区(老殿-仙人顶)苔藓物种数最少,相似性最低;(5)核心区的物种多样性要高于缓冲区,是该地区保护苔藓植物多样性的关键区域.     

安徽省苔藓植物名录

物种名录是一个地区生物多样性的本底性资料, 及时更新生物物种名录对生物多样性的保护及促进基础数据共享都具有重要意义。为了及时总结安徽省苔藓植物的分类学研究成果, 本文通过对文献的收集和分析, 整理出安徽省苔藓植物名录。结果显示, 安徽省共有苔藓植物95科253属777种, 其中角苔类3科3属3种, 苔类36科62属185种, 藓类56科188属589种。种数多于25的科为青藓科、细鳞苔科、丛藓科、真藓科、灰藓科、提灯藓科、白发藓科、绢藓科和蔓藓科。种数多于15的属为青藓属(Brachythecium)、真藓属(Bryum)、绢藓属(Entodon)、光萼苔属(Porella)、羽苔属(Plagiochila)、灰藓属(Hypnum)、凤尾藓属(Fissidens)、棉藓属(Plagiothecium)和耳叶苔属(Frullania)。区系成分组成上, 安徽苔藓植物以东亚成分占优势, 达到44.40%, 温带成分占31.53% (其中以北温带型最多, 占25.61%), 热带成分占18.92% (其中以热带亚洲成分最多, 达到10.30%)。安徽省共有中国特有苔藓55种, 濒危种1个, 易危种8个。安徽苔藓植物调查呈现出地区不均衡性, 建议在广泛调查的同时加强名录修订和专科专属研究, 对有条件的地区开展时空变化下物种多样性比较研究。     

浙江天目山国家级自然保护区苔藓植物多样性

苔藓植物因个体普遍细小,更易在野外观察及采集中被忽略,故很难获得一个客观、详尽的地区名录,导致对其多样性的研究和保护受到极大限制。本文以浙江天目山国家级自然保护区为例,采用区系生境调查法和样方法相结合的采样策略,沿海拔梯度对不同生境类型内苔藓植物多样性进行了系统调查,并结合多次历史普查资料整理出该保护区的苔藓植物名录。本研究共获得苔藓植物56科143属394种,包括苔类植物16科30属103种,藓类植物40科113属291种,其中有5种为濒危物种。与该保护区历史数据相比,本研究苔藓植物新增科4个、属31个、种182个,包括浙江省新记录科1个、属8个、种33个。区系生境调查法和样方法分别贡献了总物种数的81%和72%,但当调查范围只限定在树附生生境时,采用样方法所获得的总物种数及新增物种数均大于区系生境调查法。虽然代表更大采样努力程度的8个样方/树的调查获得的物种数显著高于2个样方/树的调查结果,但只针对树干0.3 m和1.5 m的2个样方/树的采样结果贡献了75%的物种数。鉴于本研究采集方法获得的较高苔藓植物物种丰富度及新增物种数以及物种组成在时间梯度上的巨大差异,建议在自然保护地开展...     

安徽石台县与青阳县苔藓植物多样性

生物多样性保护优先区域代表了生物多样性富集区、典型生态系统与关键物种分布区, 对于生物多样性保护具有重要意义, 但优先区域内自然保护地覆盖率通常较低, 存在很大的保护空缺。苔藓植物作为生物多样性的一个重要组成部分, 在生态系统中发挥着重要作用, 但由于个体细小、分类鉴定困难等, 使得其多样性保护成为整个生物多样性保护中较为薄弱的一环。为了了解我国生物多样性保护优先区域苔藓植物多样性及受保护情况, 本文以黄山-怀玉山生物多样性保护优先区域内的石台县和青阳县为例, 通过系统的样线法调查优先区域内自然保护地内、外的苔藓植物多样性, 比较了其物种组成特点及相似性。结果表明, 该区域共有苔藓植物64科140属344种, 包括苔类植物27科40属106种、藓类植物37科100属238种, 其中有5种为濒危物种。自然保护地内有60科120属270种, 保护地外有46科90属185种, 保护地内、外苔藓植物科、属、种的Jaccard相似性系数分别为0.66、0.50和0.32, 表明自然保护地内、外物种组成差异很大。与石台县和青阳县苔藓植物历史数据相比, 本研究新增苔藓植物14科64属273种, 其中包括安徽省新记录2科9属96种, 而且有18种仅分布于自然保护地外。根据对该区域物种累积曲线及外推估计分析, 当采集足够充分时, 基于标本数的物种多样性预测值为485种, 基于样线数的预测值为563种, 说明石台县和青阳县的苔藓植物多样性仍存在被低估的可能。本研究结果一方面表明了自然保护地之外的苔藓植物在保护中有重要价值, 另一方面也反映了苔藓植物的野外就地保护存在空缺。建议在我国其他生物多样性保护优先区域开展类似的调查和研究, 以期为今后对苔藓植物的分布规律及保护研究提供翔实的基础数据。     

祁连山不同景观类型中苔藓植物物种多样性研究

通过对祁连山不同景观类型中的苔藓植物进行样方调查与物种组成统计,采用物种相似性系数、多样性指数对苔藓植物物种多样性进行了分析。结果表明,30个10 m×10 m的样地内共计苔藓植物19科34属48种,其中优势科(≥3种)有6科,含19属31种,分别占本地区苔藓植物总属数和总种数的55.88%和64.58%。在5种景观类型中,针叶林带和高山灌丛带分布的苔藓植物物种相似性最高(相似性系数为0.5357);河岸带和高山草甸带分布的苔藓植物物种相似性最低(为0),表现出祁连山地区苔藓植物分布的丰富性和复杂性;高山灌丛带分布的苔藓植物物种多样性指数最高,但针叶林带苔藓植物最为丰富,是祁连山苔藓物种多样性保护的关键区域。     

中国苔藓植物多样性研究进展

苔藓植物是生物多样性的重要组成部分, 包括角苔植物、苔类植物和藓类植物三大类群, 其物种数量仅次于被子植物, 是高等植物的第二大类群。我国是世界苔藓植物多样性最丰富的国家。自2017年以来, 我国苔藓学者在世界范围发现了10个新属, 40个新种, 建立了新的地钱纲分类系统; 更新了我国苔藓植物物种名录, 完成了数本分类学专著, 并在苔藓系统发育基因组、苔藓植物多样性与环境关系、苔藓植物多样性保护等领域取得了可喜的进展。对未来的研究, 我们提出5点建议: (1)加强对重要生态系统、国家公园和关键类群的物种多样性调查; (2)加快基于基因组的苔藓植物多样性研究; (3)加强苔藓植物保护研究; (4)加强西北地区苔藓植物多样性研究人才的培养; (5)进一步加强国际合作, 努力构建“一带一路”国家苔藓植物多样性平台。     

海南岛苔藓植物研究历史、现状与展望

综述了海南岛苔藓植物的研究历史和现状。目前海南岛已记录的苔藓植物共有87科227属806种,其中苔类33科71属366种,藓类51科152属436种,角苔类3科4属4种;苔藓植物的区系组成以热带亚洲成分为主,与香港、台湾地区的种属相似性高;对海南岛苔藓植物的研究集中在尖峰岭、霸王岭、吊罗山3个国家级自然保护区;叶附生苔是海南热带雨林主要的苔藓生态分布类型之一,共有7科23属123种;初步统计濒危苔藓植物有15种。今后应继续开展广泛和持续的物种多样性调查,从生态学、植物化学、分子生物学等领域进行研究,促进合理的开发利用和推动保护工作。     

喀斯特石漠化区苔藓植物物种多样性变化

为了揭示喀斯特石漠化地区苔藓植物的物种多样性,通过野外实地调查对贵州喀斯特地区不同程度石漠化区域苔藓植物进行研究。结果表明,苔藓的科、属、种数量随着石漠化程度加剧而下降,其中,强度石漠化的科数最少且显著低于其他三种石漠化类型,比潜在、轻度、中度石漠化地区苔藓科数分别降低70.00%、57.14%、33.33%;轻度石漠化地区的真藓科、青藓科、丛藓科、曲尾藓科等包含属数较多,占总属数34.62%;Shannon-Wiener指数和Simpson指数变化基本一致,随石漠化程度加剧而下降,其中苔藓植物在潜在石漠化地区Shannon-Wiener指数为1.9393,高于其他三种石漠化区域,比强度石漠化区高43.97%,Simpson指数以轻度石漠化过渡到中度石漠化地区物种丰富度下降最快,下降26.73%;潜在石漠化区较其他三个区域拥有更高的苔藓数量。说明苔藓植物的分布和石漠化程度密切相关,随着石漠化程度加重,苔藓植物的科、属、种总数均有不同程度下降。     

上海城市公园苔藓植物多样性分布格局及其环境影响因子

城市公园的生物多样性十分丰富,在生物多样性保护方面具有重要价值。苔藓植物是公园生物多样性的重要组成成分,但因其体型小、难以鉴定等,容易被人们所忽略,因此对其多样性的研究和保护也相对薄弱。本文基于文献资料和生态调查数据,整合上海市中心城区和郊区共35个样点的苔藓植物名录,应用聚类分析对公园进行分组,比较了市区和郊区两个区域的苔藓植物相似性;采用典范对应分析(CCA)及层次分割的方法,定量研究环境因子与城市公园苔藓植物多样性分布格局的关系。结果表明, 35个公园共有苔藓植物34科74属164种,包括苔类7科8属9种、藓类27科66属155种,其中有12种中国特有种和4种近危种。根据聚类分析结果, 35个公园可划分为两组,主要与人口密度、与市中心距离、与主干道距离及公园面积等因素有关。市区和郊区两个区域的科、属、种的Jaccard相似性系数分别为0.94、0.89和0.30,表明两个区域的物种组成各有特点。层次分割结果显示,环境因子对城市公园苔藓植物多样性分布格局的解释率从高到低分别为人口密度、公园年龄、与市中心距离、与主干道距离、森林覆盖率、湖泊覆盖率及公园面积。整体上,上海城市公园苔藓植...     

Notulae de Ranunculaceis sinensibus (ⅩⅩⅢ)

(1) In this paper, differences among the five genera constituting the tribe Cimi cifugeae of the family Ranunculaceae are discussed. Beesia, the first genus, with compound cymes and flowers bearing neither petals nor staminodes, is different from the other four genera with simple or compound racemes and flowers bearing either petals or staminodes, and may occupy a primitive position within the tribe. As to the other four genera, Souliea is characterized by the stem without basal leaf but with 2～5 sheath-like cataphylls, the sepals being deciduous but not caducous, moderate in size and petaloid, the petals being much smaller than sepals, but pink in color and more or less petaloid, the pollen grains being pan tocolpate or pantoporate, the carpels being 1～3 per flower, when mature forming dry linear follicles conspicuously reticulate on the surface and dehiscent along the ventral suture, and the seeds being reticulate-foveolate on the surface. These diagnostic characters indicate clear ly that Souliea might have deviated from the lineage formed by the next three genera, i. e. Anemopsis, Cimicifuga, and Actaea, which have their own well-recognizable diagnostic characters. Anemopsis is characterized by the normally developed basal leaf, the racemose inflorescence with sparse and few long pedicellate flowers, the sepals 7～10 in number, mod erate in size, and petaloid, the petals slightly smaller than sepals, the tricolpate pollen grains, the carpels 2～4 per flower, stalked, when mature forming dry oblong follicles with transverse veins on the surface, and the seeds with scaly membranous wings. Cimicifuga is distinguished by the normally developed basal leaf, the caducous, small, often sepaloid sepa ls, the organs of the second floral whorl sometimes with empty sterile anthers being stamin odes not petals, the tricolpate pollen grains, the carpels 1～8 per flower, when mature form ing dry oblong or ovoid follicles with transverse veins on the surface, and the seeds usually with scaly membranous wings. The last genus Actaea is different by the basal leaf trans formed into a small scale, the caducous, small, often sepaloid sepals, the organs of the sec ond floral whorl being clawed petals, the pollen grains with 3(4～6) colpi, carpel 1 per flow er, when mature forming a fleshy indehiscent berry smooth on the surface and without any veins, the seeds roughish or slightly rugose, neither foveolate nor winged on the surface, and the advanced most asymmetric karyotype. According to the diagnostic characters given above, we believe that Beesia, Souliea, Anemopsis, Cimicifuga, and Actaea do represent five independent genera, and the treatment of the tribe Cimicifugeae including these five genera in it by Hutchinson (1923), Janchen (1949) and some other authors, has precisely shown the taxonomic diversity within the tribe. We are therefore unable to accept the treatment published by Compton et al. (1998) to lump the two genera, Souliea and Cimicifuga, into the genus Actaea. (2) Compton et al. (1998, 1997) found out that the Chinese plants previously identified by various authors as Cimicifuga foetida L., in which the terminal and lateral racemes of the compound raceme flower more or less simultaneously, differ from the true C. foetida L. in northern Asia, in which the terminal raceme of the compound raceme flowers before the lateral ones, and thus restored the species name Cimicifuga mairei Lévl. , which was formerly reduced to the synonymy of C. foetida L. , for the Chinese plants. After examining the specimens collected from Siberia and from Southwest China we failed to find out any other differences in both vegetative and reproductive organs between the plants of the two regions, and we consider that it is better to treat the populations in Southwest and Central China as a geographical variety of Cimicifuga foetida L. A new combination, Cimicifuga foetida L. var. mairei (Lévl.) W. T. Wang & Zh. Wang, is thus made. (3) 3 species of Delphinium, 1 species and 1 variety of Clematis are described as new.     

贵州罗甸纳水上石炭统(宾夕法尼亚亚系)地层的再研究

本文详细描述了贵州罗甸纳水上石炭统(宾夕法尼亚亚系)剖面的生物地层和年代地层,其牙形刺序列自上而下可详细划分为：Streptognathodus isolatus, S. wabaunsensis, S. tenuialveus, S. firmus, Idiognathodus nashuiensis , Streptognathodus simulator, S. guizhouensis , S. gracilis-S, excelsus , S. cancellosus , S. clavatulus , S. nodocarinatus , Idiognathodus podolskensis , Mesogondolella clarki -Idiognathodus robustus , Diplognathodus ophanus-D, ellesmerensis, Idiognathoides ouachitensis, Streptognathodus expansus, Idiognathoides sulcatus parva, Idiognathodus primulus-Neognathodus bassleri, Idiognathodus primulus-Neognathodus symmetricus, Neognathodus symmetricus, Idiognathoides corrugatus-I, pacificus, I. sinuatus, I. sulcatus sulcatus, Declinognathodus noduli ferus 和 Gnathodus bilineatus bollandensis 等带。 Declinognathodus noduliferus 和 Streptognathodus isolatus 的首次出现分别代表上石炭统(宾夕法尼亚亚系)和二叠系的开始。根据牙形刺和有孔虫的序列,罗甸纳水剖面的上石炭统(宾夕法尼亚亚系)地层自下而上可划分为罗苏阶(Luosuan)、滑石板阶(Huashibanian)、达拉阶(Dalaan)和马平阶(Mapingian),并可与俄罗斯的巴什基尔阶(Bashkirian)、莫斯科阶(Moscovian)、卡西莫夫阶(Kasimovian)和格舍尔阶(Gzhelian),北美的莫罗阶(Morrowan)、阿托克阶(Atokan)、得梅因阶(Desmoinesian)、密苏里阶(Missourian)和弗吉尔阶(Virgilian)进行对比。另外,本文也详细讨论了剖面中的石炭系中间界线及石炭-二叠系界线。     

Early Cretaceous Palynofloras from Tarim Basin,Xinjiang

One hundred and eight species of fossil spores and pollen referred to 55 genera found from the Lower Cretaceous Kapushaliang (Kizilsu) Group in the Tarim Basin of Xinjiang have been studied in this paper. The Kapushaliang Group may be divided into the Yageliemu Formation, the Shushanhe Formation and Baxigai Formation in ascending order. The Yageliemu palynoflora is characterized by the predominance of gymnospermous pollen, the relative abundance of pteridophytic spores and the absence of angiospermous pollen. Coniferae is dominant, while Lygodiaceae and Schizaeaceae are important in the flora. The most common species of palynomorphs are Todisporites minor, Cicatricosisporites dorogensis, C. australiensis, Lygodiumsporites subsimplex, Schizaeoisporites cretacius, S. zizyphinus, S. certus. Cibotiumspora paradoxa, Cyathidites australis, C. minor, Biretisporites potoniael, Cycadopites minimus, Pseudowalchia hiangulina, Parvisaccites radiatus, Podocarpidites multesimus, P. canadensis, Alisporites bilateralis, Cedripites cretaceus, C. canadenris, Abietineaepollenites microalatus, Clarsopollis classoides, C annulatus, C. xinjiangensis (sp. nov.), Ephedripites multicostatus, E. tarimensis (sp. nov.), etc . The palynoflora is comparable with those of the lower part of the Lower Xinminbu Formation in northwestern China and the lower part of the Lower Mannville Formation in western Canada, which is considered corresponding from Berriasian to Valanginian in age. The Shushanhe palynoflora is also characterized by dominance of gymnosperms and subdominance of pteridophyta. Some primitive angiospermons pollen grains are found in the upper part of the formation. In addition to the most common species of the above mentioned palynoflora, the important species in the present palynoflora comprise Cicatricosisporites potomacensis, C. orbiculatus, C. subrotundus, Concavissimisporites punctatus, C. verrucosus, C. globosus, lmpardecispora apiverrucata, Trilobosporites crassus, T. trioreticulosus, Pilosisporites verus, P. trichopapillosus, Klukisporites pseudoreticulatus, Verrucosisporites obscurilaesuratur, Converrucosisporites saskatchewanensis, Foraminisporis wonthaggiensis, Cingulatisporites valdensis, C. ruginosus, Jiaohepollis verus, Pityosporites constrictus, etc. More than 40 in dicative species of Early Cretaceous occur in the assemblage. The palynoflora compares clcsely with those of the middle part of the Lower Xinminbu Formation and the Quartz Sand Member of the Lower Mannville Formatton. It is suggested that the Shushanhe Formation should belong to Hauterivian of Barremian in age. The Baxigai palynoflora is basically similar to the Shushanhe palynoflora. But the palynoflora shows an obvious increase in abundance of lygodiaceous spores and angiospermous pollen accompanied by a great reduction of Classopollis and Ephedripltes. Most of the Early Cretaceous species occurring in the above mentioned palynofloras are present. In addition, some Cretaceous species recorded from Aptian and Albian Stages in Europe, North America and Australia, such as Trilobosporites tribotrys, T. trioreticulosus, Coptospora paradoxa, Camarozonosporites insignis, Crybelosporites punctatus, etc., appear in the assemblage. In comparison with the microfloras of the upper part of the Lower Xinminbu Formation, the Upper Mannville Formation and the lower part of the Lower Colorado Group, the Baxigai Forma- tion should be referred to Aptian to Albian in age. Judging from the palynofloras, the early Cretaceous palaeoclimate in the basin should belong to the arid or semi-arid type of the subtropic zone. However, from Barremtan through Albian the climatic conditions might appear relatively wet.     

Importance of biological and abiotic factors for geochemical cycling in a freshwater eutrophic lake

Here we report the results of a comprehensive biogeochemical monitoring of Rostherne Mere in 1998, including changes in dissolved oxygen, organic carbon and nitrogen, nitrate/nitrite, ammonia, Al, Na, S, K, Mg, Ca, Si, Fe, Mn, orthophosphate, particulate N & P, suspended solids, temperature, pH, chlorophyll-a and zooplankton. The results demonstrated the major influence of primary producers on the overall geochemical cycling of N, P and Si, and suggested that the significance of zooplankton might have been previously underestimated. For major anions and cations, however, the influence of biota on lake water concentrations appeared to be negligible, reflecting the fact that these chemicals were present far in excess of plankton requirements. Thus changes in concentrations of Ca, K, Na, Mg and S were rather limited and must have reflected changes in hydrological and meteorological parameters. K, however, demonstrated a transitional pattern, reflecting some influence of biological uptake. During the stratification period, the slow processes of bacterial decomposition in the hypolimnion gradually released chemicals contained in the materials accumulated in the bottom layer, remarkably increasing the concentrations of dissolved compounds of those elements present in amounts comparable with the pool stored in the sedimenting detritus (e.g. orthophosphate P, ammonia N, Si and DOC). The decomposition also resulted in a drop in the redox potential, followed by partial denitrification and chemical release from the sediments. The hypolimnion of the Mere was confirmed to remain at the stage of Mn release, characterised by accumulation of DOC, orthophosphates, ammonia and initial stages of denitrification. High levels of P released from the sediments during the stratification period suggest that the lake’s recovery after sewage diversion might be further delayed.     

Embryology of Swertia (Gentianaceae) relative to taxonomy

The embryological features of three species of Swertia ( s.l.) – S. erythrosticta , S. franchetiana , and S. tetraptera – were characterized, and the observations were used, together with previously gathered data on other species, to evaluate a recently proposed polyphyly, based on molecular data, of Swertia s.l. Comparisons of species within the genus showed that they have diversified embryologically, and there are significant between-species differences. Notable features that vary between species include the number of cell layers that form the anther locule wall, the construction of the wall of the mature anther, tapetum origin, the cell number in mature pollen grains, the structure of the fused margins of the two carpels, the ovule numbers in placental cross-sections, the shape of the mature embryo sac, the degree of ovule curvature, antipodal variation and the presence of a hypostase, and seed appendages. They share characters that are widely distributed in the tribe Gentianeae, such as a dicotyledonous type of anther wall formation, a glandular tapetum with uninucleate cells, simultaneous cytokinesis following the meiosis of the microsporocytes, tetrahedral microspore tetrads, superior, bicarpellary and unilocular ovaries, unitegmic and tenuinucellar ovules, Polygonum -type megagametophytes, progamous fertilization, nuclear endosperm, and Solanad-type embryogeny. The presence of variation in embryological characters amongst the species of Swertia s.l. strongly supports the view that Swertia s.l. is not a monophyletic group. Frasera is better separated from Swertia s.l. as an independent genus, and is only distantly related to Swertia s.s. judging from the numerous differences in embryology. Swertia tetraptera is very closely related to Halenia , as they show identical embryology.  © 2007 The Linnean Society of London, Botanical Journal of the Linnean Society , 2007, 155 , 383–400.     

小鼠基因组中的微卫星重复序列的数量、分布和密度

作者分析了老鼠基因组中各染色体及其内含子、外显子和基因间区上各种类型的微卫星(1-6个碱基的重复序列)的数量及其密度。SSR约占老鼠基因组的2.85%,其中46.2%存在于基因间区,4.75%存在于外显子,49.05%在内含子区域,即非编码区富含微卫星。微卫星的数量与染色体或基因区域的大小有关,但密度与染色体或基因区域的大小的关系并不十分密切。第4染色体的外显子区域中6种类型的SSR含量都比其它区域少。A,T,AC,AG,AT,AAC,AAG,AGG,AAAC,AAAG,AAAT,AACC,AAAAC,AAAAG,AAAAT,AAACC,AAAGG,AAGAG,AAAAAC,AAAAAG,AAAAAT,AAAGAG,ACACAT,ACAGAG,ACAGGC,ACATAT是老鼠基因组中主要的SSR类型,而一些5碱基重复单元的SSR在老鼠基因组的某一条甚至某几条染色体都不存在     

Patterns and processes of heterochrony in Mesozoic goniasterid sea-stars

Heterochronic processes are obvious in the most common family of Mesozoic asteroids, the Goniasteridae, whether studied from entire fossils or, as is more frequently the case, from isolated ossicles. When phylogeny is poorly known, comparison between species leads to such unsatisfactory interpretations as 'A is more paedomorphic than B' or 'C, compared with other species, has many peramorphic characters'. When the phylogeny is known, heterochronic trends appear amongst the lineages. The peramorphocline Metopaster parkinsoni - M. loirensis-M. trichilae-M. chilipora-M. hypertelicus is studied here from the Cenomanian to the Upper Campanian of France. Different morphological characters evolved at different speeds. Among each polymorphous population, some morphotypes foreshadowed the next step. Juveniles of one species look like the adults of one of the ascendants. The cline developed irrespective of the substrate, and proceeded together with a migration from the Anglo-Paris Basin to the Aquitanian Basin. Metopaster hunteri , during the Coniacian, and Metopaster meudonensis , during the Upper Campanian, both evolved from Metopaster parkinsoni by neoteny, and provide a good example of reiterated and canalized morphological evolution. Some non-heterochronic canalizations are described.     

Occluded Umbilicus In The Pinacitinae (Devonian) And Its Palaeoecological Implications

Eifelian (Middle Devonian) ammonoids of the Pinacitinae Hyatt, 1900 ( Exopinacites , Pinacites )with preserved shell structures from the eastern Anti–Atlas (Morocco) have revealed unusual morphological features. The Pinacitinae belong to the earliest ammonoids which closed their umbilici. As an approach to an interpretation of these structures, the representatives of the subfamily Pinacitinae ( Exopinacites singularis , Pinacites jugleri , P. eminens ) are compared with other ammonoids, e.g. Acrimeroceras , Araucanites , Clistoceras , Gaudryceras , Nathorstites , Prolobites , and Synpharciceras , which produced umbilical plugs and covers. Some of these are comparable in structure to Nautilus pompilius and N. belauensis . In contrast to all of these taxa, the lateral shell wall of the Pinacitinae reached the centre of the umbilicus and formed an umbilical lid. The umbilical shell wall rests on the umbilical lid of the previous whorl. This construction probably had the advantage that it improved the hydrodynamic properties of the conch, along with the oxyconic conch shape and the approximately horizontal orientation of the aperture.     

Comparative morphology of male reproductive systems in Mediterranean blennies (Blenniidae)

The male reproductive organs of 16 species of Mediterranean Blenniidae ( Aidablennius sphynx, Blennius ocellaris, Coryphoblennius galerita, Lipophrys adriaticus, L. canevae, L. dalmatinus, L. nigriceps, Parablennius gattorugine, P. incognitus, P. sanguinolentus, P. rouxi, P. tentacularis, P. zvonimiri, Paralipophrys trigloides, Salaria pavo and Scartella cristata ) consist of pairs of testes, testicular glands, spermatic ducts, and blind pouches. Three main types of accessory sex organs were found by comparing the external morphology of the male gonads. Differences between species were observed in the volume of the testicular gland in relation to the volume of the testis and in the size and length of the spermatic ducts, and blind pouches. The anatomy of the testicular glands of all species investigated do not differ. Each gland consists of ducts that appear to be tubules which terminate at the testis periphery on one side and at the spermatic duct on the other side. Contrary to previous claims, A. sphynx has no fat body in place of the testicular gland; the gland of this species was not distinguishable from that of the other species investigated. In the Lipophrys species, in P. trigloides , and in B. ocellaris , a transition zone between testis and testicular gland is present. The testicular blind pouches empty into the spermatic ducts, into the ureter, or separately on the genital papilla. In most species, the epithelium has no or low folds, while in S. pavo it possesses high folds that nearly fill the lumen of the blind pouches. The morphological results are discussed in connection with taxonomy, ecology, and behaviour of the fishes.     

Morphology of the gynoecium and systematic position of the Ochnaceae

The gynoecium is syncarpous in all Ochnaceae. In the Ochnoideae carpels are peltate with a conventional cross-zone bearing one ovule, or, in Lophira , a very broad cross-zone with an horizontal ovular row. In Ochna and Brackenridgea , the style is gynobasic, each carpel develops transmitting tissue on its morphologically dorsal surface, and this tissue lines a canal or originates a solid inner strand in each carpel at style level. The style is tubular, with an inner cuticle, and compound, each component with its own transmitting tissue. In Ouratea the style is solid with a single compound transmitting strand. In Lophira and Elvasia the transmitting tissue seems to be developed by the morphologically ventral carpellary surfaces. Ovules are unitegmic with a bivalent integument.
In the Sauvagesioideae carpels are peltate, but with ovules above the cross-zones, on margins of the symplicate zone. In Euthemis , there is one ovule on each side of, and close to, each cross-zone. The single stylar canal is bounded by the morphologically dorsal carpellary surfaces. In Sauvagesia ovules occur on both sides of the cross-zones but most of them are above on carpel margins, as are all ovules of Cespedesia. The stylar canal of Sauvagesia is bounded by the ventral carpel surfaces, three strips of the outer surface passing inside at the sutures and developing into transmitting tissue. The stylar canal of Cespedesia is bounded by the dorsal carpel surfaces. The gynoecium of Wallacea has two epeltate carpels with a laminar placentation, the carpel margins being displaced on to the topographically ventral carpel surfaces with a row of ovules along each margin. Ovules are bitegmic.
The Ochnoideae, which shows relationships with the Rutaceae, Meliaceae, Simaroubaceae and Hippocastanaceae, is more advanced than the Sauvagesioideae, which clearly belongs in the Violales. The Ochnaceae is to be placed in the Violales.