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1.
本实验对安朵仙水母(Cassiopeia andromeda)水母体进行不同程度（伞体、胃囊、口腕和触手）的切割,进行60日再生过程观察。本研究首次记录了安朵仙水母水母体的再生情况：切除部分伞体、全部胃囊、全部口腕和触手的水母体残体能够再生出缺失的部分;切除全部伞体的水母体残体无法再生出新的伞体,而是反向再生出新的口腕和触手;同时切除不同部位的水母体残体在组织修复时表现出一定的再生顺序性。本研究发现安朵仙水母水母体具有较强的组织再生能力,可作为钵水母纲再生研究的潜在模式物种,同时为刺胞动物研究以及再生生物学研究提供一定借鉴。 相似文献
2.
Mnemiopsis leidyi is an invasive comb jelly which has successfully established itself in European seas. The species is known to produce spectacular blooms yet it is holoplanktonic and not much is known about its population dynamics in between. One way to gain insight on how M. leidyi might survive between blooms and how it can bloom so fast is to study how the metabolism of this species actually responds to environmental changes in food and temperature over its different life-stages. To this end we combined modelling and data analysis to study the energy budget of M. leidyi over its full life-cycle using Dynamic Energy Budget (DEB) theory and literature data.An analysis of data obtained at temperatures ranging from 8 to 30 °C suggests that the optimum thermal tolerance range of M. leidyi is higher than 12 °C. Furthermore M. leidyi seems to undergo a so-called metabolic acceleration after hatching. Intriguingly, the onset of the acceleration appears to be delayed and the data do not yet exist which allows determining what actually triggers it. It is hypothesised that this delay confers a lot of metabolic flexibility by controlling generation time.We compared the DEB model parameters for this species with those of another holoplanktonic gelatinous zooplankton species (Pelagia noctiluca). After accounting for differences in water content, the comparison shows just how fundamentally different the two energy allocation strategies are. P. noctiluca has an extremely high reserve capacity, low turnover times of reserve compounds and high resistance to shrinking. M. leidyi adopts the opposite strategy: it has a low reserve capacity, high turnover rates of reserve compounds and fast shrinking. 相似文献
3.
J. S. Bullivant 《新西兰海洋与淡水研究杂志》2013,47(1):135-146
The lophophorates all feed by “impingement” feeding, so named by analogy with certain types of particle separators used in industry. In gymnolaemate bryozoans the feeding current is directed at the mouth where particles impinge and are sucked into the pharynx; in phylactolaemate bryozoans the particles impinge in the trough of the lophophore and are transported to the pharynx by cilia. In phoronids and brachiopods, particles impinge on the frontal surface of the tentacles and are conveyed to the pharynx by tracts of cilia. 相似文献
4.
花刺参(Stichopus monotuberculatus)是中国热带海参中具有较高经济价值的可食用海参之一。本文以花刺参幼参为实验对象,主要研究其摄食器官触手的形态特征与消化器官肠道不同区段的组织结构。结果显示,花刺参的口周围共有20个等长的触手,每个触手由柄部和楯状触手组成。楯状触手向外张开呈掌状,从掌心中央向外形成5～6个主要分支。主要分支上又形成了2～3级的分支,分支的腹面分布多个乳突,2～3个乳突多聚集在一起形成乳突簇。单个乳突的直径为69.99±20.97μm,每簇乳突的直径为104.99±24.15μm,适宜摄食细小的沉积物颗粒。花刺参的前肠和中肠黏膜层较厚,分别为127.42±102.09μm和114.10±35.47μm,均显著高于后肠(18.18±8.38μm)。后肠黏膜下层厚度则显著高于前肠和中肠。肌层和浆膜层厚度在肠道的三个不同区段无明显差异。前肠和中肠的绒毛长度和密度均显著高于后肠,而后肠的隐窝深度显著低于前肠和中肠。上述结果表明花刺参的消化吸收主要发生在前肠和中肠,后肠的消化吸收功能较弱但分泌能力较强。 相似文献
5.
Natural gas hydrate, as a potential energy resource, deposits in permafrost and marine sediment with large quantities. The current exploitation methods include depressurization, thermal stimulation, and inhibitor injection. However, many issues have to be resolved before the commercial production. In the present study, a 2-D axisymmetric simulator for gas production from hydrate reservoirs is developed. The simulator includes equations of conductive and convective heat transfer, kinetic of hydrate decomposition, and multiphase flow. These equations are discretized based on the finite difference method and are solved with the fully implicit simultaneous solution method. The process of laboratory-scale hydrate decomposition by depressurization is simulated. For different surrounding temperatures and outlet pressures, time evolutions of gas and water generations during hydrate dissociation are evaluated, and variations of temperature, pressure, and multiphase fluid flow conditions are analyzed. The results suggest that the rate of heat transfer plays an important role in the process. Furthermore, high surrounding temperature and low outlet valve pressure may increase the rate of hydrate dissociation with insignificant impact on final cumulative gas volume. 相似文献
6.
Feeding apparatus, mechanism and passage of ingested prey were described forNemopilema nomurai (Scyphozoa: Rhizostomeae).N. nomurai medusae without central mouths have developed complicated canal systems connecting the tip of the tentacle and oral arm to
the gut cavity. The number of junctions in the canal system increases with the bell diameter. The prey is gathered by paralyzing
nematocyst at the tentacles and by adhering cirri at the oral arms and scapulets. They are engulfed into the terminal pore
located at the oral arms and scapulets, and entered into the gut cavity via the canal system. The estimated digestion time
is 1 hour and 20 min. The diameter of terminal pore is always about 1 mm, implying that they could not eat prey larger than
that pore size. On the other hand, ephyrae have central mouths and could swallow prey as large as adults could. Exploitation
of the same size of food by adult and ephyra implies thatN. nomurai can affect seriously the whole food web, massively ingesting micro-and mesozoopl a n k t o n and cutting the energy transfer
toward the higher level of carnivores. 相似文献
7.
2005年7月在台湾海峡南部发现花水母亚纲（Anthomedusae Haeckel，1879）筒螅水母科（Tubulariidae Fleming，1828）刺泳水母属（Plotocnide Wagner，1885）1个新种——台湾刺泳水母（Plotocnixie taiwanensissp．nov．）和软水母亚纲（Leptomedusae Haeckel，1866）和平水母科（EirenidaeHaeckel，1879）伊能水母属（Irenium Haeckel，1879）1个新种——多手伊能水母（Irenium polynenumsp．nov．）． 相似文献
8.
1 Introduction T aking the average riverbed elevation ofthe riverm outh from its upstream side to its dow nstream sidew ithin a m outh area as a base line, there is usually asand sw ell standing higher than the base line. If thesw ellis form ed in the distributary channel,itis consid-ered as “a longitudinalbar”;ifitis offornearthe riverm outh,itis called “m outh bar”(Jiand H uang,1995a),such as the cases in the C hangjiang R iver andQ iantang R iverm outh areas(see Figs 1 and 2). Fig. … 相似文献
9.
利用中国＂大洋一号＂第20航次采集的深海沉积物样品进行了真菌分离鉴定,获得110株深海真菌,这些菌分属于15个属.其中曲霉和青霉最多,共为55株,占50%,且重复较多,只分布于10个种.利用CCK8法及琼脂扩散法对其中的100株深海真菌进行了抗肿瘤及抗菌活性检测,发现深海真菌具有良好的生物活性,细胞毒阳性率占49%,26%的菌株具有明显抗大肠杆菌效果、23%明显抗枯草、5%抗白假丝酵母、21%抗金黄色葡萄球菌.生物活性与培养基成分及筛选用肿瘤细胞株类型相关.对具有生物活性的20株深海真菌发酵粗提物进行了HPLC指纹图谱初步分析,发现其HPLC指纹图谱与培养基成分相关.该研究为后期分离鉴定深海真菌产生的生物活性化合物奠定了良好基础. 相似文献
10.
The dominance of shifts in the location of the Gulf Stream (GS) in the local heat balance was observed in an hourly 15-month record of unprecedented surface mooring measurements at a site in the western North Atlantic occupied from November 2005 to January 2007. Instrumentation on the buoy provided a high quality record of air-sea exchanges of momentum, heat, and freshwater flux; and oceanographic sensors recorded ocean variability in the upper 640 m. The mooring was at times in the GS and at other times north of the GS. Our intent was to isolate the local oceanic response to the atmosphere from the influence of the GS shifts. A one-dimensional heat budget analysis indicated that the advective contribution from the GS shifts dwarfed the heat contribution by atmospheric forcing and therefore played the dominant role for upper oceanic thermal variability during the whole time record. A GS case study (i.e., when the surface mooring was in the GS), isolated the upper oceanic response to the atmospheric forcing in the GS and supported the critical role of GS shifts in total oceanic heat content. Through both an Empirical Orthogonal Function (EOF) analysis and by referencing temperatures to that observed at 200 m, the impact of GS shifts and atmospheric forcing were decomposed, allowing the local oceanic thermal response to be isolated. This local oceanic response was particularly prominent during the period of sustained heating during summer. A case study of summer conditions revealed a near surface flow consistent with Ekman dynamics within a shallow, warm ocean mixed layer. 相似文献
11.
Euniphysa, originally a genus of the family Eunicidae, was erected by Wesenberg-Lund in 1949, and for a longtime there has been only one species in this genus. The present report is based on our samples collected from the South China Sea, and we consider that the differences between Euniphysa and Eunice are very significant: Five occipital tentacles distributed unequidistantly; the jaw consists of 6 pairs of maxillary plates; the body may be divided into anterior region and posterior region, etc. Therefore we suggest that Euniphysa should be separated from Eunicidae, and become a new family Euniphysi-dae. At present this family includes 3 genera, namely, Euniphysa , Paraeuniphysa and 1 new genira Heterophysa; Totally there are 7 species, including 3 new species and 1 new combination species. 相似文献
12.
Kohei Mizobata Koji Shimada Rebecca Woodgate Sei-Ichi Saitoh Jia Wang 《Journal of Oceanography》2010,66(3):405-424
We estimated the northward heat flux through the eastern channel of the Bering Strait during the ice-free seasons between
1999 and 2008. This is likely about half of the total heat flux through the strait. The net volume transport and heat flux
through the eastern channel of the strait were estimated from multiple linear regression models with in-situ/satellite remotely sensed datasets and NCEP reanalysis 10 m wind. The net volume transport was well explained by the west-east
slope of sea level anomaly and NNW wind component at the strait. On the heat flux, the contributions of both barotropic and
baroclinic components were taken into account. Estimated volume transport and vertical profile of temperature were used to
calculate northward heat flux through the eastern channel of the strait. The magnitude of the estimated heat flux is comparable
to estimates from in-situ measurements. Averaged heat flux in the eastern Bering Strait between 2004 and 2007 was about 1.9 times larger than that
between 2000 and 2003. Maximum heat flux occurred in 2004, and same magnitude of heat flux was estimated from 2005 to 2007.
This resulted not only from the increase in northward volume transport but also anomalous warm water intrusion from the Bering
Sea. Our results suggest a candidate among the important parameters controlling heat budget, which contributes to the Arctic
sea ice reduction, whereas more studies are required to confirm that this mechanism is actually responsible for the interannual
and longer timescale variability. 相似文献
13.
中国牡蛎的种类繁多,多样性极为丰富,由于其形态变异大,已报道的中国牡蛎物种组成及分布争议甚大,中国北方沿海常见"褶牡蛎"的分类也一直存在很大的争议,这严重阻碍了其他相关研究的进行.作者系统综述了中国北方沿海"褶牡蛎"的分类历史和研究现状,并对中国北方沿海"褶牡蛎"进行了系统的分类研究,取得了最新研究成果.确立了中国北方沿海"褶牡蛎"的分类地位,改变其分类长期混乱的局面,这对于"褶牡蛎"的养殖和其他相关研究均具有重要的意义. 相似文献
14.
Ji Hyung Kim JunMo Lee Md-Abu Affan Dae-Won Lee Do-Hyung Kang 《Ocean Science Journal》2017,52(3):359-366
Mangrove forests are known to be inhabited by diverse symbiotic cyanobacterial communities that are capable of N2 fixation. To investigate its biodiversity, root sediments were collected from a mangrove forest in Chuuk State, Federated States of Micronesia (FSM), and an entangled yellow-brown coccoid cyanobacterium was isolated. The isolated cyanobacterium was reproduced by multiple fission and eventually produced baeocytes. Phylogenetic analysis revealed that the isolate was most similar to the genera Myxosarcina and Chroococcidiopsis in the order Pleurocapsales. Compositions of protein, lipid and carbohydrate in the cyanobacterial cells were estimated to be 19.4 ± 0.1%, 18.8 ± 0.4% and 31.5 ± 0.1%, respectively. Interestingly, total fatty acids in the isolate were mainly composed of saturated fatty acids and monounsaturated fatty acids, whereas polyunsaturated fatty acids were not detected. Based on the molecular and biochemical characteristics, the isolate was finally classified in the genus Myxosarcina, and designated as Myxosarcina sp. KIOST-1. These results will contribute to better understanding of cyanobacterial biodiversity in the mangrove forest in FSM as well as the genus Myxosarcina, and also will allow further exploitation of its biotechnological potential on the basis of its cellular characteristics. 相似文献
15.
Francesco Canganella Giovanna Bianconi Agata Gambacorta Chiaki Kato Katsuyuki Uematsu 《Marine Ecology》2002,23(S1):1-10
Abstract. Hydrothermal vent ecosystems have been extensively investigated during the last 20 years; shallow water hot springs (typically found below 50 m depth) have also been studied, and from these ecosystems many thermophilic and hyperthermophilic organisms were isolated and described.
The submarine caves of Cape Palinuro were discovered long ago, but only during the last decades were geological and biological investigations carried out, yielding a large number of reports on this fascinating environment. During the last two years, several samples of water, mud, and/or bacterial mat were collected within the "Grotta Azzurra", and enrichment experiments were performed using peptone, starch, glucose or pullulan as main organic nutrients. Many heterotrophic strains were isolated and most of them grew optimally between 37 and 43 ° C with the addition of 0-2 % NaCl. Growth was usually observed between 10 and 50 ° C the range of growth pH was 4 to 9, and NaCl concentrations up to 10–12 % were tolerated in most cases.
The analysis of 16S rDNA performed with the most representative isolates showed a close phylogenetic relationship with the genera Bacillus, Vibrio, Citrobacter and Escherichia. Moreover, an isolate showing morphological and physiological similarities with the genus Enterococcus was characterised and taxonomically described based on the 16S rDNA sequence. 相似文献
The submarine caves of Cape Palinuro were discovered long ago, but only during the last decades were geological and biological investigations carried out, yielding a large number of reports on this fascinating environment. During the last two years, several samples of water, mud, and/or bacterial mat were collected within the "Grotta Azzurra", and enrichment experiments were performed using peptone, starch, glucose or pullulan as main organic nutrients. Many heterotrophic strains were isolated and most of them grew optimally between 37 and 43 ° C with the addition of 0-2 % NaCl. Growth was usually observed between 10 and 50 ° C the range of growth pH was 4 to 9, and NaCl concentrations up to 10–12 % were tolerated in most cases.
The analysis of 16S rDNA performed with the most representative isolates showed a close phylogenetic relationship with the genera Bacillus, Vibrio, Citrobacter and Escherichia. Moreover, an isolate showing morphological and physiological similarities with the genus Enterococcus was characterised and taxonomically described based on the 16S rDNA sequence. 相似文献
16.
The annual mean volume and heat transport sketches through the inter-basin passages and transoceanic sections have been constructed based on 1 400-year spin up results of the MOM4p1. The spin up starts from a state of rest, driven by the monthly climatological mean force from the NOAA World Ocean Atlas(1994). The volume transport sketch reveals the northward transport throughout the Pacific and southward transport at all latitudes in the Atlantic. The annual mean strength of the Pacific-Arctic-Atlantic through flow is 0.63×106 m3/s in the Bering Strait. The majority of the northward volume transport in the southern Pacific turns into the Indonesian through flow(ITF) and joins the Indian Ocean equatorial current, which subsequently flows out southward from the Mozambique Channel, with its majority superimposed on the Antarctic Circumpolar Current(ACC). This anti-cyclonic circulation around Australia has a strength of 11×106 m3/s according to the model-produced result. The atmospheric fresh water transport, known as P-E+R(precipitation minus evaporation plus runoff), constructs a complement to the horizontal volume transport of the ocean. The annual mean heat transport sketch exhibits a northward heat transport in the Atlantic and poleward heat transport in the global ocean. The surface heat flux acts as a complement to the horizontal heat transport of the ocean. The climatological volume transports describe the most important features through the inter-basin passages and in the associated basins, including: the positive P-E+R in the Arctic substantially strengthening the East Greenland Current in summer; semiannual variability of the volume transport in the Drake Passage and the southern Atlantic-Indian Ocean passage; and annual transport variability of the ITF intensifying in the boreal summer. The climatological heat transports show heat storage in July and heat deficit in January in the Arctic; heat storage in January and heat deficit in July in the Antarctic circumpolar current regime(ACCR); and intensified heat transport of the ITF in July. The volume transport of the ITF is synchronous with the volume transport through the southern Indo-Pacific sections, but the year-long southward heat transport of the ITF is out of phase with the heat transport through the equatorial Pacific, which is northward before May and southward after May. This clarifies the majority of the ITF originating from the southern Pacific Ocean. 相似文献
17.
Hydro-thermo-chemo and mechanically coupled processes determine hydrate morphology and control gas production from hydrate-bearing sediments. Force balance, together with mass and energy conservation analyses anchored in published data provide robust asymptotic solutions that reflect governing processes in hydrate systems. Results demonstrate that hydrate segregation in clayey sediments results in a two-material system whereby hydrate lenses are surrounded by hydrate-free water-saturated clay. Hydrate saturation can reach ≈2% by concentrating the excess dissolved gas in the pore water and ≈20% from metabolizable carbon. Higher hydrate saturations are often found in natural sediments and imply methane transport by advection or diffusion processes. Hydrate dissociation is a strongly endothermic event; the available latent heat in a reservoir can sustain significant hydrate dissociation without triggering ice formation during depressurization. The volume of hydrate expands 2-to-4 times upon dissociation or CO2CH4 replacement. Volume expansion can be controlled to maintain lenses open and to create new open mode discontinuities that favor gas recovery. Pore size is the most critical sediment parameter for hydrate formation and gas recovery and is controlled by the smallest grains in a sediment. Therefore any characterization must carefully consider the amount of fines and their associated mineralogy. 相似文献
18.
Two toxic polypeptides BTTX I and BTTX II were isolated from the sea anemone Bolocera tuediae. Toxin isolation was achieved by alcoholic extraction of the homogenized tentacles and filaments, batchwise adsorption onto ion-exchangers (QAE-Sephadex A25, CM-Cellulose, Se-Cellulose, Sp-Sephadex C25), gel filtration on Sephadex G50 and G25 and ion-exchange chromatography on SP-Sephadex C25 and QAE-Sephadex A25. The toxins were tested on the shore crab Carcinus maenas by intramuscular injection. LD100 for BTTX I is 500 μg kg−1 C. maenas, whereas the BTTX II it is 40 μg kg−1. The molecular weights of both toxins are estimated to be 5000 Dalton. 相似文献
19.
大连地区中国对虾“红腿病”病原体及其感染寄主细胞的电镜观察 总被引：1，自引：0，他引：1
对虾红腿病国内最早发现于１９８１年８月下旬山东潍坊市一养虾场,１９８８年８月在辽宁庄河、东沟县一带虾场开始流行［２］。此病流行广、发病期短、死亡率比较高,是危害对虾主要病害之一。作者自１９９０年８月～１９９２年９月,对大连地区养虾场流行的红腿病进行了调查、采样,并着重作了病原菌的形态及其侵染寄主细胞的病变观察,为虾病防治提供了科学依据。１材料与方法１·１材料来源典型对虾红腿病样品采自大连市金州区重家沟、营城区西小磨两个虾场。１,２样品的处理１．２．１病原菌的分离与菌种鉴定,病原菌的分离分别由辽宁… 相似文献
20.
T. Feseker T. Pape K. Wallmann S.A. Klapp F. Schmidt-Schierhorn G. Bohrmann 《Marine and Petroleum Geology》2009
The sediment temperature distribution at mud volcanoes provides insights into their activity and into the occurrence of gas hydrates. If ambient pressure and temperature conditions are close to the limits of the gas hydrate stability field, the sediment temperature distribution not only limits the occurrence of gas hydrates, but is itself influenced by heat production and consumption related to the formation and dissociation of gas hydrates. Located in the Sorokin Trough in the northern Black Sea, the Dvurechenskii mud volcano (DMV) was in the focus of detailed investigations during the M72/2 and M73/3a cruises of the German R/V Meteor and the ROV Quest 4000 m in February and March 2007. A large number of in-situ sediment temperature measurements were conducted from the ROV and with a sensor-equipped gravity corer. Gas hydrates were sampled in pressurized cores using a dynamic autoclave piston corer (DAPC). The thermal structure of the DMV suggests a regime of fluid flow at rates decreasing from the summit towards the edges of the mud volcano, accompanied by intermittent mud expulsion at the summit. Modeled gas hydrate dissociation temperatures reveal that the gas hydrates at the DMV are very close to the stability limits. Changes in heat flow due to variable seepage rates probably do not result in changes in sediment temperature but are compensated by gas hydrate dissociation and formation. 相似文献