The impacts of invasive Nile tilapia (Oreochromis niloticus) on the fisheries in the main rivers of Guangdong Province,China

Nile tilapia (Oreochromis niloticus) is one of the most widespread invasive fish species, and this species has successfully established populations in the major rivers of Guangdong Province, China. Field surveys and manipulative experiments were conducted to assess the impacts of Nile tilapia on fisheries. We determined that the increase of Nile tilapia in these rivers not only affects the CPUE (catch-per-unit-per-effort) of the fish community and native fish species but also reduces the income of fishermen. In the manipulative experiments, we observed that the growth of native mud carp decreased in the presence of Nile tilapia. Our results suggest that the invasion of Nile tilapia negatively affected the fishery economy and native fish species, and suitable control measurements should be taken.     

Middle paleozoic waulsortian-type mud mounds in Southern Fergana (Southern Tien-Shan,commonwealth of independent states): The shallow-water atoll model

Summary Several Waulsortian-type mud mounds nearly 500 m thick and about 5 km long occur in the Middle Paleozoic carbonate section of the Aktur nappe in the mountains on the right bank of Isfara river. These buildups form a well developed barrier system that stretches along the South Ferganian carbonate platform margin and divides the carbonate complex into a fore-reef and a back-reef part. The time of the mounds' most active growth was from the Late Silurian (Ludlow) to the Middle Devonian (Eifel). Three main facies types can be recognized in the mud mounds: 1. micritic core facies, 2. sparitic flank facies and 3. loferitic capping facies. The central massive or crudely bedded part of the mounds consists of white or light grey clotted micrite. Macrofossils are rare. The sparitic flank facies in contrast consists of coarse and densely packed crinoidal wackestone-floatstones with some brachiopod shell debris. Solitary rugose corals, tabulate corals, stromato-poroids and fragments of mollusks are also abundant. The tops of the mounds are usually covered with loferitic pelmicrites or oolitic grainstone caps. Stromatactis-like structures are very rare and poorly developed in the South Ferganian mud mounds. However, almostin all such mounds horizons of calcitic breccias can be found. In order to explain all the features found in the Fergana mounds an ‘atoll-like’ model has been proposed which starts the evolution of the mud mounds with a small nucleus bioherm. The main stage of the evolution corresponds to an atoll-like structure developing on the surface of shallow water platforms. White clotted micrite of the mound core facies is interpreted as a accumulation of fine-grained sediment in an inner lagoon flanked by crinoidal bar deposits. The mound flank facies represents the atoll rim deposits from where the carbonate mud is derived. The capping loferitic facies is considered as tidal flat deposit that developed on top of the buildups during the last stage of its evolution. The knoll shape of the mounds is explained by the retreat of the atoll flanking crinoidal bars back into the inner lagoon during the rise in sea level. Stromatactis-like structures of small cavities filled with sparry calcite owe their existence to burrowing organisms. Calcitic breccias are interpreted as paleokarst collapse breccias. They indicate that the tops of the mud mound became subaerially exposed. Other evidence for a subaerial exposure can be seen in the occurrence of Variscian ‘black and white’ limestone gravel on the tops of some mud mounds. According toWard et al. (1970) these sediments were produced above the sea level at the edge of hypersaline lakes situated on islands.     

The introduction to Japan of the Titan barnacle,Megabalanus coccopoma (Darwin, 1854) (Cirripedia: Balanomorpha) and the role of shipping in its translocation

The Titan Acorn barnacle, Megabalanus coccopoma, a native of the tropical eastern Pacific, has become established in the western Atlantic (Brazil and the northern Gulf of Mexico to the Carolinas), northwestern Europe and the western Indian Ocean (Mauritius), and therefore its dispersal capabilities are well known. This study reports its introduction to Japan and confirms its occurrence in Australia. In an attempt to determine the source of this introduction, phylogeographic techniques, involving cytochrome c oxidase I sequences of various widely separate populations of M. rosa and M. volcano, were utilized. No significant genetic differentiation or haplotype patterns between widely separated populations of each of the three species were found. Lack of such differentiation indicates recent geographical isolation and thus negates a null hypothesis predicting that the occurrence of one of more of these species in Australia was natural.     

Pelovirga terrestris gen. nov., sp. nov., anaerobic,alkaliphilic, fumarate-, arsenate-, Fe(III)- and sulfur-reducing bacterium isolated from a terrestrial mud volcano

A novel anaerobic, mesophilic, alkaliphilic, chemoorganotrophic bacterium (strain M08fum^T) was isolated from a salsa lake of a terrestrial mud volcano (Taman Peninsula, Russia). Cell of strain M08fum^T were Gram-stain-negative, rod-shaped, non-spore forming motile rods. The temperature range for growth was 10–45 °C (optimum at 30 °C). The pH range for growth was 7.0–11.0, with an optimum at pH 8.5–9.0. The isolate was capable of organic acids fermentation and anaerobic respiration with elemental sulfur, Fe(III) and arsenate. The end products of fumarate fermentation were succinate, acetate and CO₂. The closest phylogenetic relatives of strain M08fum^T were members of the family Geopsychrobacteraceae, class Desulfuromonadia. The genome of strain M08fum^T had a size of 3.10 Mb with a DNA G + C content of 53.1% (WGS). Genome analysis revealed the presence of genes involved in fumarate fermentation, arsenate reduction and resistance, sulfur respiration and Fe (III) reduction. Based on the phenotypic, genotypic and phylogenetic characteristics we propose to assign strain M08fum^T to a new species of a novel genus Pelovirga terrestris gen. nov., sp. nov. within the family Geopsychrobacteraceae. The type strain of Pelovirga terrestris is M08fum^T (=KCTC 15919^T = VKM B-3407^T). This is the first representative of the class Desulfuromonadia, isolated in pure culture from a mud volcano and the first alkaliphile in the family Geopsychrobacteraceae.     

The sexual function of wallowing in male wild boar (Sus scrofa)

The wild boar (Sus scrofa) is a medium-sized ungulate that produces a large variety of marks. Traditionally, wallowing is an activity that has fundamentally been related to several processes such as thermoregulation, reduction in the number of ectoparasites or disinfection of wounds in the skin of males resulting from fights to reach females. In this study, I analysed another possible function of wallowing in free-ranging wild boar populations when temperatures are low and parasitic numbers are not significant. The results indicate that during the sampling time, from October to February, the number of wild boars with a mud layer on their skin was 47, out of a total of 558 wild boar analysed. Of these 47 wild boars, 44 were males and within this group, 40 individuals were adult males. The wallowed males were bigger and older than non-wallowed males hunted at the same time. In addition, I found that males wallowed mainly during autumn (90.9% of all cases). In the total number of wild boars analysed, I did not notice individuals with wounds resulting from fights other than from the hunting day. On the other hand, the analysis of the females reproductive systems indicated that the rut period took place during the last days of October and the first days of November. From these results, the coincidence of the rut period with the maximum of wallowing in adult males could be indicative of a sexual function of this activity.     

Follicular development in the volcano mouse (Neotomodon alstoni alstoni, Rodentia: Muridae) from birth to maturity: A morphological approach

The present study describes the morphology and ultrastructural features of postnatal follicular development in the volcano mouse ( Neotomodon alstoni alstoni ), an endemic Mexican rodent. By the first week of age, germ cells were organized in clusters within the ovigerous cords, and only 51.8% of them were associated with somatic cells. At the ultrastructural level, pairing chromosomes and cellular junctions between germ and pregranulosa cells, such as desmosomes, were observed. At this time, the zona pellucida could not be detected in the formed follicles. From 15 to 28 days postpartum, growing follicles were located at the medulla and inner cortex of the ovary, but most were atretic. The first preovulatory follicles were seen at 40 days. Likewise, corpora lutea were observed at this stage of development, which shows that the volcano mouse is a spontaneous ovulator. The follicular development of the volcano mouse shows strong similarities with that of the golden hamster, particularly during the first week. The morphological changes observed during postnatal follicular development of the volcano mouse follow the same general histological pattern as reported for other mammals, although the timing of these events is species-specific.     

Molecular cloning and characterization of crustin from mud crab<Emphasis Type="Italic"> Scylla paramamosain</Emphasis>

Antimicrobial peptides (AMPs) are important components of the host innate immune response against microbial invasion. In the present study, we report the identification and characterization of a crustin (CrusSp) from the hemocyte of mud crab, Scylla paramamosain using an expressed sequence tag (EST) and rapid amplification cDNA end (RACE) approaches. Analysis of the nucleotide sequence revealed seven different variances of the CrusSp cDNA in mud crab. The open reading frame encodes a protein of 111 amino acids with 21 residues signal sequence. The predicted molecular mass of the mature protein (90 amino acids) is 10.27 kDa with an estimated pI of 8.54. Analysis of the protein domain features indicated typical conserved cysteine residues containing a single whey acidic protein (WAP) domain at the C-terminus. A neighbour-joining tree showed that S. paramamosain crustin is closely related to other crustin homologues, and displays the highest similarity to crustin antimicrobial peptide in shore crab Carcinus maenas. Four exons and three introns were identified within the 999 bp genomic DNA sequence of CrusSp. Tissue distribution analysis showed that CrusSp was highly expressed in hemocytes, gills, intestines and muscle but it was not expressed in hepatopancreas and eyestalks. To gain insight into the in vitro antimicrobial activities of CrusSp, the mature peptide coding region was cloned into E. coli for heterologous expression. The recombinant CrusSp could inhibit the growth of gram-positive bacteria but had no inhibition activity against gram-negative bacteria. These results indicated the involvement of CrusSp in the innate immunity of S. paramamosain.     

锯缘青蟹卵黄发生期卵母细胞和卵泡细胞之间的结构变化

通过电镜研究了锯缘青蟹二次卵巢发育过程中卵黄发生期（分为初期和后期）卵母细胞表面的结构和胞质的变化。卵黄发生初期分为：内源性卵黄发生阶段和有卵泡细胞直接参与的外源性卵黄合成阶段,前者特征为：在卵母细胞中充满了内质网泡,在泡内有不同程度的卵黄物质合成,此时在卵母细胞的表面区域,可见很多卵泡细胞向卵母细胞表面迁移,并包围卵母细胞。后者其特征是在卵母细胞的表面,有大量的胞饮小泡出现在卵膜的内面,随着两细胞表面膜的逐步融合和胞饮作用加强最后形成链锁状结构,胞质中靠近卵质周围有卵黄体的积极合成和大更换 脂肪滴积累,在此阶段的后期,卵泡细胞质已基本吸收完毕,卵泡细胞膜和卵母细胞膜融合,某些界面已无膜结构。卵黄发生后期在亲蟹孵出幼体后的第11d至第27d基本结束,此期也主要以外源性卵黄发生为主,在卵母细胞的周围,卵泡细胞迅速扩大,其间分布着大量的大小不同的囊泡和线粒体,在接近卵母细胞表面,还常可见大量的脂肪滴存在。卵泡细胞与卵母细胞间其膜结构完全消失,从而可使滤泡大片细胞质直接融入卵母细胞中,以后随着卵黄发生的进一步发展,卵母细胞与卵泡细胞的交界面逐步形成一个网状的膜结构屏障,同时在卵巢中可见正在降解的卵母细胞,在卵黄发生近结束以后,在卵母细胞的表面,逐步形成两层卵膜,这时的卵母细胞质中几乎充满了卵黄体和脂肪滴。     

新疆泥火山细菌群落PCR-SSCP 分析

采用单链构象多态性(SSCP)技术, 以16S rDNA 基因的V3 区为靶对象, 分析泥火山细菌多样性及其群落结构。通过对泥火山不同月份的不同深度土样DNA 提取后, 针对16S rDNA 进行PCR 扩增出236 bp 大小片段, 通过SSCP 电泳对泥火山细菌进行季节性多样性分析, 并对主要条带进行克隆分析。结果显示: 新疆泥火山细菌不同季节多态性明显, 而且这种多态性容易受生态和气候的影响; 假单胞菌属是泥火山土壤优势菌群, 在泥火山区土壤中广泛分布, 受生态和气候环境影响较小。     

Morphological variation in Gallotia atlantica from the volcanic island of Lanzarote: subspecies designations and recent lava flows

A detailed uni‐ and multivariate analysis of within‐island geographical variation in scalation and body dimensions of the lacertid lizard, Gallotia atlantica, from Lanzarote (and two neighbouring offshore islets) was carried out. Two main morphological groupings were detected: four populations clustered within a putative malpaís group, i.e. from relatively recent volcanic lava fields (seven populations were sampled from these areas), while the other 19 populations (including the three remaining malpaís populations, and those from the offshore islets of Montaña Clara and Alegranza) also clustered together. Thus, while there is a tendency for occupation of malpaís areas to be related to morphological variation, this model does have some inconsistencies. The differentiated malpaís group comprises populations from two geographically isolated areas, one from the central‐western part of the island (Timanfaya) and the other from the north (Malpaís de la Corona). The divergence of these populations is considered to have arisen recently, rather than their being relicts of an ancient, formerly widespread, lineage. The morphological variation partially supports the previous use of two different subspecies to describe the within‐island variation. However, if such a scheme were applied then one of the subspecies would need to encompass populations from the geographically separated southern Timanfaya and Malpaís de la Corona areas, as opposed to just the latter. We reject previous observations that either malpaís individuals in general, or those corresponding to the north‐eastern subspecies, are larger than individuals from other areas. The pattern of morphological variation of G. atlantica within Lanzarote is less pronounced but shows some similarities with patterns of morphological variation in lizards from neighbouring islands. © 2005 The Linnean Society of London, Biological Journal of the Linnean Society, 2005, 85 , 395–406.