Ultrastructural and Cytochemical Observations on Sporogenesis of Myxobolus sp. (Myxosporida: Myxobolidae) from the Common Shiner Notropis cornutus*

SYNOPSIS. The structure and cytochemistry of spores of Myxobolus sp. from plasmodia which occur in the gill filaments of the common shiner Notropis cornutus were studied by light microscopy and by scanning and transmission electron microscopy. The thin-walled valves of the pyriform spores are thickened in the lateral sutural and apical regions. Mucous material is associated predominantly with the posterior end of many spores. The plasmodium is surrounded by a syncytial wall bounded by 2 membranes. Pinocytotic channels are formed by the inner membrane and numerous dense vesicles are pinched off at the distal ends of the channels. Sporogenesis is initiated by the envelopment of one vegetative cell by another. The larger, enveloped cell divides to form a disporous pansporoblast, which contains 2 pairs of capsulogenic and valvogenic cells and 2 binucleate sporoplasm cells. Each capsular primordium and connecting external tubule gives rise to a polar capsule which houses a helically coiled polar tubule. The apical end of each polar capsule is plugged by a stopper. The valvogenic cells surround the capsulogenic and posteriorly situated sporoplasm cells to form the spore valves. Iodinophilic (glycogen) inclusions were not seen in spores stained with iodine or Best's carmine. A darkly stained band was observed around the posterior region of most spores stained with Best's carmine. In the electron microscope large aggregates of β glycogen particles were seen in the cytoplasm of sporoplasm cells in mature spores.     

Extensive sampling of polar bears (Ursus maritimus) in the Northwest Passage (Canadian Arctic Archipelago) reveals population differentiation across multiple spatial and temporal scales

As global warming accelerates the melting of Arctic sea ice, polar bears (Ursus maritimus) must adapt to a rapidly changing landscape. This process will necessarily alter the species distribution together with population dynamics and structure. Detailed knowledge of these changes is crucial to delineating conservation priorities. Here, we sampled 361 polar bears from across the center of the Canadian Arctic Archipelago spanning the Gulf of Boothia (GB) and M'Clintock Channel (MC). We use DNA microsatellites and mitochondrial control region sequences to quantify genetic differentiation, estimate gene flow, and infer population history. Two populations, roughly coincident with GB and MC, are significantly differentiated at both nuclear (F_ST = 0.01) and mitochondrial (Φ_ST = 0.47; F_ST = 0.29) loci, allowing Bayesian clustering analyses to assign individuals to either group. Our data imply that the causes of the mitochondrial and nuclear genetic patterns differ. Analysis of mtDNA reveals the matrilineal structure dates at least to the Holocene, and is common to individuals throughout the species’ range. These mtDNA differences probably reflect both genetic drift and historical colonization dynamics. In contrast, the differentiation inferred from microsatellites is only on the scale of hundreds of years, possibly reflecting contemporary impediments to gene flow. Taken together, our data suggest that gene flow is insufficient to homogenize the GB and MC populations and support the designation of GB and MC as separate polar bear conservation units. Our study also provide a striking example of how nuclear DNA and mtDNA capture different aspects of a species demographic history.     

Comparative physiological studies on the growth of cryptic species of Bostrychia intricata (Rhodomelaceae,Rhodophyta) in various salinity and temperature conditions

Inter‐ and intra‐specific physiological variations of intertidal macroalgae have been well investigated. However, studies on physiological responses of cryptic algal species have been poorly documented. Bostrychia intricata is a widespread marine red alga in the Southern Hemisphere, and has many cryptic species. We investigated the effect of different salinities and temperatures on the specific growth rate of three cryptic species (N2, N4 and N5) of B. intricata from New Zealand. Our data indicated that all cryptic species grew at the full range of salinities and temperatures tested, but exhibited a significant difference in their specific growth rates. Cryptic species N4 had a higher growth rate than the other two cryptic species under all experimental conditions, whereas cryptic species N2 occasionally showed a higher growth rate than cryptic species N5 at high salinities and lower temperatures. The distinct physiological properties of these cryptic species may explain their distribution pattern (a wider distribution of cryptic species N4 than N2 and N5) in New Zealand. The physiological divergence between the cryptic species could be related to their levels of evolutionary divergence, with more similar physiology between cryptic species, which share a more recent common ancestor (N2 and N5). Our findings underline that morphologically indistinguishable cryptic algal species are different in many other aspects and are truly independent entities.     

达乌尔黄鼠入眠准备期的体温、代谢率及能量特征

贮脂类动物在冬眠前大量积累脂肪来准备冬眠,并在入眠时迅速降低体温和代谢率。为探究入眠准备期达乌尔黄鼠体温、代谢率、呼吸商及能量代谢的变化,将其入眠准备期分为育肥期、体重高峰期、育肥后期和冬眠前的试降期,使用植入式半导体温度记录元件iButton、开放式代谢仪和改进的代谢笼,监测其体温、代谢率及呼吸商和能量摄入的变化。结果显示:(1)达乌尔黄鼠体温在冬眠前13 - 34 d 开始下降,远早于冬眠但晚于体重高峰期;体重高峰期体温有降低的趋势,持续时间为1 - 3 d;育肥后期体温显著下降,体温日波动幅度增加。(2)体重高峰期的静止代谢率高于育肥期,育肥后期有降低的趋势,试降期最低。(3)呼吸商在体重高峰期先升高,之后迅速衰减;入眠准备期的能量摄入在体重达高峰期前达到最大值。结果表明,达乌尔黄鼠在入眠准备期,其体温和代谢率已开始降低,能源物质已开始转变;体重高峰期可能是达乌尔黄鼠入眠的一个转折点或启动入眠的开关。     

Additional records and notes for Wheeler's (1992) List of the Common and Scientific Names of Fishes of the British Isles

This paper compiles information new to an earlier list published in 1992. Most changes are (1) additions largely resulting from importation of freshwater species, (2) range extensions of neritic and oceanic epipelagic species, together with (3) the incidental capture of species from within the 200 m bathymetric limit of resident deep pelagic and demersal deep‐sea representatives. A list of such species with the potential to stray from residence in the deeper strata of the oceanic region to shelf waters (<200 m) is presented in appendices.