琼东近海浮标污损生物研究

为了解南海北部近海石油开发区的污损生物状况,对海南岛东部近海海区的两个浮标及其锚锭系统上的污损生物进行了调查。结果表明,该海区污损生物的种类主要是藻类,水螅,有柄蔓足类和牡蛎;南海沿岸水域常见的无柄蔓足类仅出现在距海南岛相对较近的Ｊ２浮标站。并探讨了该海区的污损生物群落结构与邻近沿岸水域的差异。     

北部湾江洪扇贝养殖区的污损生物

2006年8月至2007年7月,对北部湾江洪扇贝养殖区的污损生物进行周年调查。结果表明:该海区养殖网笼的污损生物有8门20种,优势种为藤壶、钩虾、苔藓虫,其次是翡翠贻贝、牡蛎、海鞘、大型藻类和水螅。污损生物附着高峰在8、11和12月,1月的附着数量最少;藤壶附着高峰在8、11和12月,附着生物量占污损生物总量的56.0%,是养殖区污损生物防除的重点对象;钩虾附着高峰出现在8、9月,12和2月附着量也较高,其生物量占污损生物总量的18.0%;草苔虫附着高峰出现在4月,其生物量占污损生物总量的8.4%。污损生物附着量呈现由表层向底层递减的趋势。     

司氏江珧幼虫培育试验

司氏江珧 Pinna(Atrina)strangei Reeve。广东俗称“割纸刀”,我国南海沿岸的东山岛、汕尾,沃头、海南岛和西沙群岛等地均有分布,是太平洋、印度洋等热带海区较为常见的软体动物。其肉与闭壳肌较其他江珧特别肥大,味极鲜美,闭壳肌可以制成优质江珧柱。江珧柱为名贵的海味珍品,我国古代人民早已有记载,如邻几什志云:“四明海物,江     

湛江地区沿海游泳虾类调查报告Ⅰ

湛江地区位于广东省西部，面临南海，其附近海区东面包括雷州半岛以东至上川岛以西的海区，南面隔琼州海峡与海南岛相对，西面为雷州半岛以西、北部湾的东北部海区。海岸线曲折漫长，海底平缓，水质肥沃，海流不急，加之气候温和，年平均水温较高，适合虾类，     

南海区捕捞渔业副渔获及其利用

南海位于４°Ｎ～２３°３５′Ｎ,１０５°４０′Ｅ～１１７°３０′Ｅ之间,是中国四大海区中最大的海区,面积为３．５×１０６ｋｍ２,其中大陆架面积约占总面积的一半以上,仅南海北部大陆架（２００ｍ等深线以内）海域面积约３．７４×１０５ｋｍ［１］。南海北部地理自然环境优越,渔业资源丰富,渔场广阔。南海渔民在长期的生产实践中,根据资源和渔场的实际情况开发了具有南海特色的各种适应性渔具渔法,大大地推动了南海渔业的发展。１　渔获概况　　南海区（包括广东、广西和海南三省）海洋捕捞业渔获量８０％来自南海北部沿岸近…     

我国的麒麟菜栽培事业

麒麟菜是一种经济价值较高的热带性海藻，全世界分布情况是以赤道为中心向南北延伸，我国只见于南海的部份地区如海南岛、西沙群岛及台湾省等海区(1)。这种海藻在海南岛和西沙群岛都称为石花菜，意思是生长在石花(珊瑚)上的一种蔬菜。我国劳动人民在很久以前就开始研究和利用这种海藻了。     

企鹅珍珠贝主要污损生物的初步研究

企鹅珍珠贝[Pteria(Magnavicula)penguin(R ding)]分布于热带亚热带海域,在台湾、两广沿海和海南岛有野生种群栖息,它是珍珠贝属的一种可生产大规格附壳珠和正圆珠的大型贝类。近年来企鹅珍珠贝的种苗生产、养殖和大型珍珠培育以及生化遗传的研究受到关注。在养殖中,其他海洋生物的附着或寄生成为影响企鹅珍珠贝生长与存活的重要因素,目前相关研究仅见其他贝类的多毛虫寄生病[1-4]、附着敌害生物和网笼污损生物类群等[5-7]的报道,而企鹅珍珠贝的污损生物的研究仅见污损苔虫的文献记录[8]。本文对企鹅珍珠贝的附着生物进行了初步鉴别,并分…     

企鹅珍珠贝主要污损生物的初步研究

企鹅珍珠贝[Pteria（Magnavicula）penguin（Roeding）]分布于热带亚热带海域，在台湾、两广沿海和海南岛有野生种群栖息，它是珍珠贝属的一种可生产大规格附壳珠和正圆珠的大型贝类。近年来企鹅珍珠贝的种苗生产、养殖和大型珍珠培育以及生化遗传的研究受到关注。在养殖中，其他海洋生物的附着或寄生成为影响企鹅珍珠贝生长与存活的重要因素，目前相关研究仅见其他贝类的多毛虫寄生病、附着敌害生物和网笼污损生物类群等的报道，而企鹅珍珠贝的污损生物的研究仅见污损苔虫的文献记录。本文对企鹅珍珠贝的附着生物进行了初步鉴别，并分析它们的附着或寄生状态。     

南海北部陆架区海域深水金线鱼的产卵场

根据 1997年 12月至 1999年 6月在南海北部陆架区海域进行的底拖网渔业资源调查的资料 ,统计分析了南海北部陆架区海域深水金线鱼性腺成熟期的组成及分布、季节性变化和水深变化规律。结果表明 ,南海北部陆架区海域深水金线鱼的产卵场位于广东沿海水深 6 0～ 15 0m海区 ,尤其是珠江口外海区的群体更为密集 ;该生殖群体的产卵期较长 ,且分布范围大 ,未见有显著性变化。     

湛江地区沿海游泳虾类调查报告Ⅰ

前言湛江地区位于广东省西部,面临南海,其附近海区东面包括雷州半岛以东至上川岛以西的海区;南面隔琼州海峡与海南岛相对;西面为雷州半岛以西、北部湾的东北部海区。海岸线曲折漫长,海底平缓,水质肥沃,海流不急,加之气候温和,年平均水温较高,适合虾类,特别是起源于热带海洋的对虾类的生长繁殖。因此,湛江地区沿海的虾类资源丰富,种类繁多,是广东省的主要产虾区。对本地区的主要经济虾类资源,1976年省水产研究所和我校曾进行调查和报道。去年湛     

Marine biofouling in offshore areas south of Hainan Island, northern South China Sea

ＩＮＴＲＯＤＵＣＴＩＯＮＢｉｏｆｏｕｌｉｎｇｃａｎｃａｕｓｅｒｏｕｇｈｎｅｓｓｏｆｓｕｂｍｅｒｇｅｄｓｕｒｆａｃｅｓｏｆｍａｒｉｎｅｓｔｒｕｃｔｕｒｅｓ(Ｃｈａｋｒａｂａｒｔｉ,1991),ｉｎｃｒｅａｓｅｈｙｄｒｏｄｙｎａｍｉｃｌｏａｄｉｎｇｓ(ＷｏｌｆｒａｍａｎｄＴｈｅｏｐｈａｎａｔｏｓ,1985),ａｃｃｅｌｅｒａｔｅｃｏｒｒｏｓｉｏｎｐｒｏｃｅｓｓ(Ｐａｔｉｌｅｔａｌ.,1988),ａｎｄｉｍｐｅｄｅｕｎｄｅｒｗａｔｅｒｉｎｓｐｅｃｔｉｏｎａｎｄｍａｉｎｔｅｎａｎｃｅ(Ｈｏｕｇｈｔｏｎ,1978).Ｔｈｅｌａｃｋｏｆｄ…     

Marine fouling in offshore areas east of Hainan Island, northern South China Sea

INTRODUCTIONBiofoulingonunderwaterpartsofman mademarinestructuresisamajoreconomicandtechni calproblemhavinginternationaldimensionsforthedevelopmentofoceanengineeringbecauseitnotonlyincreasesstaticandhydrodynamicloading,butalsoaffectscorrosioncharacteristicsandim pedesunderwaterinspectionandmaintenance (CallowandEdyvean ,1 990 ) .Duetodifferencesingeographicalpositionsandenvironmentalconditions,thedistributionofsessileorganismsvarieswitharea .Therefore ,understandingtheformationofbiofoulin…     

Fouling acorn barnacles in China—a review

We review the species composition,distribution, and seasonal variation of fouling acorn barnacles in Chinese waters-from Bohai Sea and Yellow Sea to East and South China Seas. Thirty-two species of acorn barnacles were found, of which, the dominant species are Amphibalanus amphitrite, A. reticulatus, A. variegates, Balanus trigonus, Fistulobalanus kondakovi, Megabalanus tintinnabulum, Striatobalanus amaryllis, and Eurapha withersi in the fouling communities. A. amphitrite is the dominant species in the coastal waters of Bohai Sea and Yellow Sea and A. reticulatus is dominant in the East and South China Seas. The settlement period of fouling acorn barnacles is usually in summer and autumn. From north to south with the decrease of latitude, their settlement period obviously extends, even to the whole year, and the species number also increases.0ther environmental factors, such as salinity and distance from shore, also play an important role in the distribution of fouling acorn barnacles.     

Onshore warm tongue and offshore cold tongue in the western Yellow Sea in winter: the evidence

A winter onshore warm tongue extending from the Yellow Sea Warm Current to the southern Jiangsu coast, and an of fshore cold tongue extending from the southern Jiangsu coast to the southwest of Jeju Island(South Korea), are newly identified based on the sea-surface temperature from satellite remote sensing, and further confirmed by the distribution of suspended sediments. In addition, there are two obvious thermal fronts associated with the onshore warm tongue and off shore cold tongue. The narrow gap between the two thermal fronts is supposed to be the pathway for the off shore transport of cold coastal water and suspended sediments. The concurrence of onshore warm and of fshore cold tongues suggests the concurrence of onshore and off shore currents in the western Yellow Sea in winter, which seems to be inconsistent with the previously accepted view that, in winter, the Yellow Sea Coastal Current flows from the Old Huanghe Delta to the southwest of Jeju Island. This distinctive phenomenon helps establish an updated view of the circulation in the western Yellow Sea in winter.     

A NEW SPECIES OF RANINOIDES (CRUSTACEA: DECAPODA: RANINIDAE) FROM OFF THE SOUTHEASTERN COAST OF HAINAN ISLAND AND NANSHA ISLANDS

ＩＮＴＲＯＤＵＣＴＩＯＮＲａｎｉｎｏｉｄｅｓｆｏｕｎｄｂｙＨ .ＭｉｌｎｅＥｄｗａｒｄｓ,1 83 7,ｎｏｗｉｎｃｌｕｄｅｓｓｉｘｓｐｅｃｉｅｓｉｎＩｎｄｏ ＰａｃｉｆｉｃＯｃｅａｎｓ:Ｒ .ｐｅｒｓｏｎａｔｕｓＨｅｎｄｅｒｓｏｎ ,1 888,Ｒ .ｓｅｒａｔｉｆｒｏｎｓＨｅｎｄｅｒｓｏｎ,1 888,Ｒ .ｈｅｎｄｅｒｓｏｎｉＣｈｏｐｒａ,1 93 1 ,Ｒ .ｂａｒｎａｒｄｉｉＳａｋａｉ,1 974 ,Ｒ .ｃｒｏｓｎｉｅｒｉＲｉｂｅｓ,1 989ａｎｄＲ .ｉｎｔｅｒｍｅｄｉｕｓＤａｉｅｔＸｕ,1 993 .ＲｅｃｅｎｔｌｙｒｅｐｏｒｔｅｄＲ .ｐｅｒｓｏ…     

Epi- and endobiont faunal communities on an Egyptian Mediterranean rocky shore: species composition and their competition for space

The exposed calcareous rocky area of the Abu Qir Headland,east of Alexandria,Egypt which range from coarse grains,through pebbles,cobbles,and boulders to rocky platforms,was significantly colonized by sclerobionts(epibionts and endobionts).The epibiont species diversity was comparatively higher than that of endobionts.Epibiont communities included bryozoans(the anascan-grade cheilostome Bifiustra savartii),serpulid(Hydroides elegans,Spirobranchus cf.tetraceros,Vermiliopsis striaticeps and Protula or Apomatus) and spirorbid(Spirorbis) wormtubes,and balanoid barnacles(Amphibalanus amphitrite,Balanus trigonus,and Perforatus perforatus).The cheilostome bryozoan colonies,which developed extensive sheets,proliferated on the study rocky shore either encrusting the bioeroded basement directly,or encrusting other epilithic taxa,particularly balanoid barnacles and serpulid worms.Encrusters displayed a remarkable marginal competitive interaction(overgrowth and stand-off) for space on the study rocky shore.On the other hand,endobionts were not well represented on the studied rocky shore exposure.It was possible to identify three ichnotaxa:Gastrochaenolites,Maeandropolydora,and Finichnus.The findings documented represent a significant contribution to our knowledge of sclerobionts composition,sequence of their colonization and/or bioero sion,and their mutual relationships on the intertidal rocky shore of the Abu Qir Headland.     

A NEW SPECIES OF RANINOIDES （CRUSTACEA ： DECAPODA ： RANINIDAE） FROM OFF THE SOUTHEASTERN COAST OF HAINAN ISLAND AND NANSHA ISLANDS

Ranlnoides longifions new species, off SE coast of Hainan Island, dorsal surface of carapace with an arched granular edge across carapace between the anterolateral teeth, median frontal tooth longest, second frontal teeth subquadrate.     

Numerical simulation of the structure and variation of upwelling off the east coast of Hainan Island using QuikSCAT winds

The spatial structure and variation of the upwelling in the waters east and northeast of Hainan Island, China during 2000-2007 were investigated using a nested high-resolution Princeton Ocean Model (POM) forced by QuikSCAT winds. The model produced good simulations of the summer upwelling and the seasonal and annual variability. Strong upwelling occurs from mid-July to mid-August with a peak east of Hainan Island associated with the southwesterly monsoon in the South China Sea. Sensitivity experiments indicated that when the local wind stress controls the variability of the upwelling, the large-scale circulation significantly enhances the upwelling northeast of Hainan Island by inducing a local upwelling and transporting cold water northeast-ward along the island’s east coast. The joint effects of the local wind stress and large-scale circulation result in stronger upwelling northeast of Hainan Island. This implies that the annual variation of the upwelling northeast of Hainan Island is controlled not only by the local alongshore wind stress but also by the large-scale circulation. This result will help us investigate the decadal variation of the upwelling in this region in the future.     

Contribution of Mountain River Materials to the Continental Shelf off Southeastern Hainan Island Since the Mid-Holocene

The concentrations of rare earth elements(REEs) in the bulk sediment of Core X2, which was collected from southeastern Hainan Island, were analyzed to investigate the relative contributions of various provenance regions since mid-Holocene. The results show that sediments in Core X2 were primarily derived from Hainan Island with lesser amounts from Taiwan and limited input from the Pearl River. Based on the application of quantitative inversion to model the REE data, the average contributions of river materials from southeastern Hainan Island and southwestern Taiwan to the study area were 68% and 32%, respectively. Furthermore, starting at 4.0 kyr BP, the transport of fluvial sediments from Taiwan to the study region increased due to enhanced hydrodynamics in South China Sea(SCS). These results indicate that the contributions of mountain river materials from Hainan Island and Taiwan to the continental shelf of northern SCS are non-negligible. Furthermore, these results demonstrate that mountain rivers can play an important role in the material cycle of continental margins and may feature a greater impact than large river systems in specific continental shelf areas.