盐度胁迫下点带石斑鱼(Epinephelus malabaricus) 胚胎及卵黄囊仔鱼的形态变化

将点带石斑鱼的受精卵置于不同盐度的水体中,观察受盐度胁迫下点带石斑鱼胚胎的沉浮 情况、卵径、油球径、孵化率、畸形率,以及卵黄囊仔鱼的形态变化和营养物质的消耗状况.结果 表明,点带石斑鱼受精卵在盐度25(含25)以下的水体中为沉性,在盐度35(含35)以上的海水中全部 漂浮于水表层,在盐度30和对照组31的水体中大部分胚胎浮在水上层.受精卵卵径随孵化盐度降低而减小.在水温26-28℃的条件下,点带石斑鱼受精卵经21-26h可孵化成仔鱼,盐度对孵化时间影响不显著(P>0.05).盐度在15-50范围内都能孵出仔鱼,但孵化率和畸形率因盐度不同而有显著差异.综合分析表明点带石斑鱼受精卵孵化的适合盐度范围为26.7-41.1.最适孵化盐度范围在30.5-32.5之间.盐度对卵黄囊仔鱼可量性状的影响主要表现在卵黄囊容积和全长的变化,高盐度(≥45)下胚后仔鱼卵黄囊容积、全长和体高显著减小(P<0.05),油球径不因盐度不同而改变.     

烟台第一海水浴场沙源匮乏型海滩地貌和表层沉积物粒度特征

在烟台第一海水浴场,利用经纬仪进行2条海滩横剖面形态测量,并在不同地貌单元采集沉积物样品进行粒度分析。测量显示,该海滩仅有小规模沙坝和沟槽体系。后滨上有风成沉积,但滩肩和海岸沙丘发育均不明显。粒度分析结果表明,海滩沉积物以中砂、粗砂为主,杂以砾或细砂,比山东半岛其他海滩沉积物明显要粗。由陆向海沉积物呈带状分布,平均高潮线附近和沙坝迎水坡侵蚀作用均显著。因此认为缺乏沙源供应的基岩岬湾式海岸是导致沙滩地貌发育不典型、海滩侵蚀作用显著的主要原因。     

Modeling the tidal channel morphodynamics in a macro-tidal embayment,Hangzhou Bay,China

The Hangzhou Bay is a macro-tidal bay located to the south of the Changjiang estuary in China. Along its northern shore, a large-scale tidal channel system has developed, which includes a main northern tidal channel, with a length of more than 50 km and a width up to 10 km, and a secondary southern tidal channel. A process-based morphodynamic model, incorporating the cohesive sediment transport module of Delft3D, is used to analyze the physical processes and mechanisms underlying the formation and evolution of this tidal channel system. The results show that spatial gradients of flood dominance, caused by boundary enhancement via current convergences, is responsible for the formation of the channel system, due to a combination of the various factors such as funnel-shaped geometry hindering associated with the presence of islands, and flow deviation by the southern tidal flat and so on. The model results agree well with the real morphological features. This study also indicates that the reclamation of the southern tidal flat imposes a profound influence on the morphological evolution of the tidal channel system in the Hangzhou Bay. It is feasible to use the model to simulate long-term estuarine morphological changes with cohesive sediment settings.     

Graphite morphologies from the Borrowdale deposit (NW England,UK): Raman and SIMS data

Graphite in the Borrowdale (Cumbria, UK) deposit occurs as large masses within mineralized pipe-like bodies, in late graphite–chlorite veins, and disseminated through the volcanic host rocks. This occurrence shows the greatest variety of crystalline graphite morphologies recognized to date from a single deposit. These morphologies described herein include flakes, cryptocrystalline and spherulitic aggregates, and dish-like forms. Colloform textures, displayed by many of the cryptocrystalline aggregates, are reported here for the first time from any graphite deposit worldwide. Textural relationships indicate that spherulitic aggregates and colloform graphite formed earlier than flaky crystals. This sequence of crystallization is in agreement with the precipitation of graphite from fluids with progressively decreasing supersaturation. The structural characterization carried out by means of Raman spectroscopy shows that, with the exception of colloform graphite around silicate grains and pyrite within the host rocks, all graphite morphologies display very high crystallinity. The microscale SIMS study reveals light stable carbon isotope ratios for graphite (δ ¹³C = −34.5 to −30.2‰), which are compatible with the assimilation of carbon-bearing metapelites in the Borrowdale Volcanic Group magmas. Within the main mineralized breccia pipe-like bodies, the isotopic signatures (with cryptocrystalline graphite being lighter than flaky graphite) are consistent with the composition and evolution of the mineralizing fluids inferred from fluid inclusion data which indicate a progressive loss of CO₂. Late graphite–chlorite veins contain isotopically heavier spherulitic graphite than flaky graphite. This agrees with CH₄-enriched fluids at this stage of the mineralizing event, resulting in the successive precipitation of isotopically heavier graphite morphologies. The isotopic variations of the different graphite morphologies can be attributed therefore, to changes in the speciation of carbon in the fluids coupled with concomitant changes in the XH₂O during precipitation of graphite and associated hydrous minerals (mainly epidote and chlorite).     

基于空间句法的泉州城区道路网形态研究

根据空间句法理论对泉州城区道路网进行量化描述,并利用量化后的泉州城区道路网的形态变量对其空间特征形态进行研究分析.结果表明,泉州中心城区总体呈格网状特征,空间智能性较高,道路网形态较合理,同时也存在智能值与集成度均与交通实际不符的道路空间.最后在此形态基础上提出泉州道路网的优化建议,为城市的空间扩展、规划建设提供参考依...     

The rudist bivalve Pironaea milovanovici Kühn, 1935, a multiple-fold Hippuritidae,from south-eastern Spain. Taxonomic implications. Pore and canal system constructional morphology

The study of the external and internal shell characters of Pironaea milovanovici Kühn, as well as of their ontogenetic and intra-specific variability, observed on abundant, well preserved, and matrix-free specimens from Tavernes de la Valldigna, Valencia province, Spain, revealed that other Pironaea species (e.g. P. bacevicensis Milovanović, P. petkovici Milovanović, Sladić-Trifunović, and Grubić, P. postdalmatinica Pamouktchiev, P. signumpraeverta Pamouktchiev, and Pironaea sp. ex gr. polystyla in Lupu), based on one or a very small number of specimens, are junior synonyms of P. milovanovici Kühn. The pore and canal system of the left valve is described in detail, based on differently weathered valves and differently oriented sections; it is constrained by the presence of secondary pillars in both valves. Being the pore and canal system and its relation with the secondary pillars relatively simple and well understood in P. milovanovici, by comparison, an interpretation of these structures in more complex multiple-fold Hippuritidae such as those of the Americas is hypothesized.     

黄河与长江入海沉积物中碳酸盐含量和矿物颗粒形态特征及影响因素

利用X射线物相分析、扫描电镜及能谱分析等方法分析了长江和黄河入海沉积物矿物颗粒形态特征及不同粒级的碳酸盐矿物百分含量分布。结果表明,长江和黄河入海沉积物的碳酸盐矿物含量均在9%左右,差异不大。长江碳酸盐矿物含量在粗粒级较高,随着粒度变细波动式降低,黄河碳酸盐矿物含量则随粒度变细而逐步增加;黄河方解石含量高而白云石低,长江的情况正好相反。长江和黄河入海沉积物中的白云石颗粒大多比较完整,侵蚀沿完全解理面发生,菱面体形态明显。长江白云石上可以见到大量的磨蚀和溶蚀形态。黄河白云石保存较好,侵蚀程度较低,磨蚀和碰撞形态明显,溶蚀形态很少,发现典型的马鞍状白云石颗粒。长江和黄河的方解石均遭受强烈侵蚀。长江方解石溶蚀特征特别明显,深入矿物颗粒内部。黄河方解石侵蚀深度相对浅表,侵蚀形态多为磨蚀、碰撞和溶蚀等物理和化学综合侵蚀特征。长江某些方解石表面布满细小鲕状方解石颗粒,似为局部自由空间的胶体-陈化成因特征。黄河方解石呈现多个次生微晶集合体,显示其黄土粘粒空隙胶结物成因形态。碳酸盐矿物的菱面体形态和菱面体完全解理所特有的60°和120°交角,是其电镜下的最佳识别特征。长江和黄河沉积物物源、流域风化强度以及矿物晶体结构本身的特...     

Existence,morphology and structure of the Yellow Sea Warm Current Branch approaching waters offshore Qingdao,China

In this study, we focused on full-region cruise survey data, near-bottom continuous mooring observations and sea surface wind products from the western South Yellow Sea in winter; after ensuring the data reliability and accuracy, we processed and analyzed the data. Image resolution experiments were carried out to determine the lowest recognition resolutions for all image types, which represent the resolution characteristics of the data. The existence of a warm water tongue originating from the Yellow Sea Warm Current(YSWC) that approached waters offshore Qingdao was confirmed. For the first time, a high salinity water tongue, corresponding to the warm water tongue, was described and found to be more representative of the YSWC branch path. This warm tongue is a sign of the branch originating from the YSWC, which we defined as the Yellow Sea Warm Current Branch approaching waters offshore Qingdao(YSWC-QDB). The pattern of the warm and salty water tongues showed remarkable rear, branching middle, shrinking neck and expanding top regions. These patterns showed a temporal feature of the tongues, and were the result of multi-temporal branches in front of the YSWC main section as well as the YSWC-QDB crossing the southwestward path of the extension of the North Shandong Coastal Current flowing along the southeast coast of the Shandong Peninsula(NSCC-SESE). Analysis using mooring data at a sensitive and representative station also showed the existence of the YSWC-QDB. It is a probabilistic event that manifests as a northwestward flow that decreases gradually from the bottom to the surface in the early cold air transit stage and consistent in the whole water column profile in the later stage. It varies quasi-periodically with weather processes. It also transports some of the YSWC water stored in the entrance area of the Bohai and Yellow seas under winter wind conditions to the western South Yellow Sea as a compensatory current. This current, caused by northerly winds, especially northwest winds and obstruction of the NSCC-SESE, was present, and strong water reduction and compensation caused significant residual sea level oscillations. The compensatory current, if caused by strong northwest wind,began to appear when its direction was opposite to the wind direction. In addition, confirmation of the YSWC-QDB provides an oceanographic basis for the short cooling time and rapid warming in the Qingdao area in winter. This research provides a basis for further studies of the YSWC-QDB at high spatial and temporal resolutions using large sea surface datasets. For monsoon basin dynamics, this study can also be extended to the whole Bohai and Yellow seas and closed or semi-closed basins on the continental margin.     

数字地图制图中的地图数据处理方法

首先提出如何在1∶100万GIS数据支持下编制1∶200万欧洲地图要解决的问题,详细介绍了基于图形曲率化简线状要素和基于形态滤波化简面状要素和地貌综合数据处理的技术和方法。     

MORPHOLOGY AND GROWTH PATTERNS OF THE USRI RIVER POINT BARS, BIHAR, INDIA

1 INTRODUCTIONThe exact mechanism of accumulation of sediments in point bars is not clearly known. Many scientistsinvestigated the problem. In the river Klaralven, Sundborg (1956) observed the development of sometransverse bars in the initial stage of the point bar formation. These transverse bars tend to becomelongitudinal as they extend close to the stream bed. Martvall and Nilsson (1972) investigated the problemof point bar formation experimentally in a laboratory flume. The flume st…