11 resultados para Alectryonella plicatula
Resumo:
本文对我国己发表的牡蛎作了详细的比较解剖学研究。在强蛎亚科(Pycnodonteinae)发现了第三个心耳--右上心耳和与其相连的第三条回心静脉--后静脉,这在双壳类中实属首次报道。第一次提出了牡蛎循环系统的两种类型,附心脏型和无附心脏型。两者之间的主要区别是:前者无肌套血管,其外套血液主要来自环外套动脉和附心脏,而后者由于无附心脏和环外套动脉,其外套血液主要来自肌套血管;前者是通过出鳃静脉和外套静脉分别将鳃前部和后部的血液送回心耳,而后者的外套静脉与外入鳃血管不通,鳃中的血液只能通过出鳃静脉回到心耳。根据外套腔的形态特点,本文将中国的牡蛎分为三种类型六个组。第一种类型,左右侧都具侧水腔,包括一个组;第二种类型,仅右侧具有侧水腔,包括四个组;第三种类型;不具侧水腔,包括一个组。在比较解剖学研究的基础上,文章还讨论了消化系统,神经系统,循环系统等一些主要系统的演化过程,并推测了现生牡蛎各属间的演化关系。提出了一些新的分类依据,发现了一个具有重要演化意义的单行属种,爪蛎属(Talonostrea),猫爪牡蛎(T. talonata)。澄清了目前世界上在舌骨蛎属(Hyotissa)、拟舌骨蛎属(Parahyotissa)、小蛎属(Saccostrea)和巨蛎属(Crassostrea)分类中的混乱。解决了我国牡蛎分类中存在己久的疑难问题,将己发表的20种牡蛎重新鉴定为15种,即舌骨牡蛎(Hyotissa hyotis),复瓦牡蛎(Parahyotissa imbricata)。中华牡蛎(P. sinensis),鸡冠牡蛎(Lopha cristagalli)。薄片牡蛎(Dendostren folium),缘齿牡蛎(D. cre-nulifera),褶牡蛎(Alectryonella plicatula),猫爪牡蛎(T. talonata),长牡蛎(Crassostrea gigas),近江牡(C. rivularis),拟近江牡蛎(Crassostrea sp.),僧帽牡蛎(Saccostrea cucullata),棘刺牡蛎(S. echinata),鹅掌牡蛎(Planostrea pestigris)和密鳞牡蛎(Ostrea denselamellosa)。它们分别隶属于二个科,曲蛎科(Grypheidae)和牡蛎科(Ostreidae);四个亚科,强蛎亚科(Pycnodonteinae)。冠蛎亚科(Pycnodonteinae),巨蛎亚科(Lopheinae)和牡蛎亚科(Crassostreinae)。
Resumo:
Oysters are commonly found on rocky shores along China's northern coast, although there is considerable confusion as to what species they are. To determine the taxonomic status of these oysters, we collected specimens from nine locations north of the Yangtze River and conducted genetic identification using DNA sequences. Fragments from three genes, mitochondrial 165 rRNA, mitochondria! cytochrome oxidase I (COI), and nuclear 285 rRNA, were sequenced in six oysters from each of the nine sites. Phylogenetic analysis of all three gene fragments clearly demonstrated that the small oysters commonly found on intertidal rocks in north China are Crassostrea gigas (Thunberg, 1793), not C. plicatula (the zhe oyster) as widely assumed. Their small size and irregular shell characteristics are reflections of the stressful intertidal environment they live in and not reliable characters for classification. Our study confirms that the oysters from Weifang, referred to as Jinjiang oysters or C. rivularis (Gould, 1861), are C. ariakensis (Wakiya, 1929). We found no evidence for the existence of C. talienwhanensis (Crosse, 1862) and other Crassostrea species in north China. Our study highlights the need for reclassifying oysters of China with molecular data.
Resumo:
Karyotype and chromosomal location of the major ribosomal RNA genes (rDNA) were studied using fluorescence in situ hybridization (FISH) in five species of Crassostrea: three Asian-Pacific species (C. gigas, C. plicatula, and C. ariakensis) and two Atlantic species (C. virginica and C. rhizophorae). FISH probes were made by PCR amplification of the intergenic transcribed spacer between the 18S and 5.8S rRNA genes, and labeled with digoxigenin-11-dUTP. All five species had a haploid number of 10 chromosomes. The Atlantic species had 1-2 submetacentric chromosomes, while the three Pacific species had none. FISH with metaphase chromosomes detected a single telomeric locus for rDNA in all five species without any variation. In all three Pacific species, rDNA was located on the long arm of Chromosome 10 (10q)-the smallest chromosome. In the two Atlantic species, rDNA was located on the short arm of Chromosome 2 (2p)-the second longest chromosome. A review of other studies reveals the same distribution of NOR sites (putative rDNA loci) in three other species: on 10q in C. sikamea and C. angulata from the Pacific Ocean and on 2p in C. gasar from the western Atlantic. All data support the conclusion that differences in size and shape of the rDNA-bearing chromosome represent a major divide between Asian-Pacific and Atlantic species of Crassostrea. This finding suggests that chromosomal divergence can occur under seemingly conserved karyotypes and may play a role in reproductive isolation and speciation.
Resumo:
本研究应用显带技术和荧光原位杂交(Fluorescence in situ hybridization,FISH)技术,鉴定了牡蛎的染色体;应用FISH方法定位了一系列的重复序列和大分子的P1克隆DNA;制备了染色体特异性探针。应用FISH特异性探针成功地鉴定了长牡蛎的三体10。结果如下:1.分析了G带和C带在美洲牡蛎染色体上的分布。G带在每一条染色体上的带型不同,某些染色体间(如第1对和第4对染色体,第7对和第9对染色体)的带型差别不是很明显。G带型容易受染色体收缩程度的影响。C带型重复性较好,染色体带型较清楚,分布在染色体的端粒区域和着丝粒区域。G带和C带带型能够用来鉴定牡蛎的染色体,但是重复性低和带型差异不显著,并不适合常规的染色体鉴定。2.早期胚胎和担轮幼虫制备的染色体适合于FISH分析。染色体制备方法重复性好,可适用于其它贝类的染色体制备。3.研究了重复序列基因--rDNA的定位:1)18S-5.8S rDNA在研究的五种巨蛎属Crassostrea牡蛎均只有一个位 点。太平洋种(C.gigas,C. ariakensis和C. plicatula)中,杂交信号位于最短的染色体一第10对染色体长臂的端粒区域,在大西洋种(C. virginica和C. rhizophorae)中,同一序列定位在第2对染色体短臂的端粒区域。2)18S-28S rDNA在两种蛤中有两个位点。rDNA探针定位在侏儒蛤(Mulinis Lateralis)的第15对和第19对染色体的端粒区域,同一序列定位在硬壳蛤(Mercenaria mercenaria)的第10对染色体的长臂和第12对染色体短臂的端粒区域。信号强度在两对染色体之间有差异。 3)5s rDNA位于美洲牡蛎的第5对染色体的短臂上靠近着丝粒区域和第6 对染色体的短臂的中间区域。信号强度在两对染色体之间没有显著差异。5S rDNA探针可以作为鉴定和识别第5对和第6对染色体的特异性探针。4.研究了一些重复序列的定位1)两个短的重复序列1G8,1P2均产生很强的荧光信号分布在美洲牡蛎所有的染色体上。在低严谨条件下,这些序列均产生很强的信号散布在所有的染色体上。在高严谨条件下,信号强度大大减弱,但是信号仍散布在所有的染色体上。这些重复序列散布在美洲牡蛎的整个基因组中。2)高度重复序列Cgl70产生的信号分布在长牡蛎的7对染色体的着丝粒区域,没有发现间区信号。在第1对,第2对,第4对和第7对染色体上的荧光信号强且稳定。在第5对,第8对和第10对染色体上的信号相对弱且不稳定。在剩余的染色体上(第3对,第6对和第9对染色体)没有检测到荧光信号。结果表明此卫星序列是一个着丝粒卫星序列。在美洲牡蛎的染色体上没有检测到荧光信号,表明了这个着丝粒卫星序列在这两种牡蛎中的分布存在着显著的差异。3)脊椎动物端粒序列(TTAGGG)n的FISH信号局限在四种双壳贝类(美洲牡蛎,the mangrove oyster,硬壳蛤,侏儒蛤)所有染色体的端粒区域,没有发现间区信号的存在。研究结果与已报道的研究结果表明脊椎动物端粒序列或许存在于所有双壳贝类的染色体末端。双壳贝类是目前研究过的唯一含有脊椎动物端粒序列DNA的无脊椎动物。4)研究了RAPD探针在美洲牡蛎染色体上的定位。大多数RAPD探针产生了多个信号散布在间期细胞核和所有的染色体上。引物OPX-03,OPX-04,OPX—06,OPG-02,OPM—04,OPM-11,0PS-02制备的探针在适宜的条件下产生特异性荧光 信号,分布在牡蛎的特定的染色体上。PCR特异性带产生的探针OPX—06—310和0PG-02—300产生了特异性的荧光信号:OPX—06—310产生的信号位于第5对染色体的短臂的近端粒区域,0PG—02—300探针定位到第3对染色体的短臂上。这两个探针是鉴定美洲牡蛎单条染色体的特异性探针。5.研究了大分子Pl克隆DNA(插入片断为80~100 kb)在美洲牡蛎染色体上的定位。Pl克隆DNA通过切口平移方法标记digoxigenin—11-dUTP用作FISH的探针。Cot-1 DNA作为竞争剂有效地抑制了Pl克隆序列中的重复序列产生的信号。杂交信号用fluorescein标记的anti—digoxigenin抗体来检测,用两层抗体rabbit-anti-sheep抗体和FITC anti—rabbit抗体来扩增信号。9个P1探针成功地定位在特定的染色体上。46—1探针杂交到第1对染色体的长臂靠近着丝粒区域;47-10探针定位到第2对染色体的长臂近端粒区域;Cvpl和48-13两探针定位到第3对染色体上:Cvpl位于短臂的端粒区域,48-13探针位于长臂的近着丝粒区域;48—10探针杂交到第4对染色体的长臂上;48-1探针杂交到第5对染色体长臂的近着丝粒区域;49-11探针位于第7对染色体长臂上;探针49-10和44-11位于第8对染色体长臂上。同时我们成功地将2个P1探针杂交到同一染色体分裂相中,进一步确定了Pl探针在美洲牡蛎染色体 上的定位。6.应用18S-28S rDNA探针成功地鉴定出长牡蛎非整倍体中的三体10。经鉴定AF-35,AF-39和AF-3三体家系属于三体10家系。rDNA探针分布在三条染色体上,即多出的一条染色体为染色体10。相应地在间期细胞核上有三个信号出现。AF-34和AF-36家系不属于三体10家系。rDNA探针分布在两条染色体上,相应地在间期细胞核上有两个信号出现。FISH和染色体特异性探针为非整倍体的鉴定提供了一个快速准确可靠的方法和途径。
Resumo:
Two hundred and seventy five mollusc species from the continental shelf off Southern Spanish Sahara (depth: 32-60 m) were identified. Their distribution pattern is strongly influenced by the nature of the bottom (firm substrate, shelter, stability of sediment) rather than other factors at that depth interval. This faunal assemblage shows great affinity to the Mediterranean and Lusitanian faunas, and comprises only few (22 %) exclusively Senegalese and species living south of Senegal.
Resumo:
Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.