119 resultados para southern Yellow Sea
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The apodous holothurian species originally described by Ohshima ( 1915) as Toxodora pacifica has been rediscovered, and its known geographic range extended from Suruga Bay, Japan to the western side of the Yellow Sea, China. As the genus name Toxodora is no longer available, a new genus name, Neotoxodora Liao, Pawson, and Wei, is proposed. The type material of Neotoxodora pacifica is lost, and a Neotype is named for this species.
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The fatty acid compositions of 22 species of marine macrophytes, belonging to the Ceramiales, Cryptonemiales, Nemalionales, Laminariales, Chordariales, Scytosiphonales, Desmarestiales, Dictyosiphonales, Fucales, Dictyotales and Ulvales and collected from the Bohai Sea, were determined by capillary gas chromatography. The contents of polyunsaturated fatty acids (FAs) in the Bohai Sea algae, in comparison with the same species from the Yellow Sea were found to be lower. Red algae had relatively high levels of the acids 16:0, 18:1(n-7), 18:1(n-9), 20:5(n-3) and 20:4(n-6), and those examined were rich in C-20 PUFAs, these chiefly being arachidonic and eicosapentaenoic acids. The major FAs encountered in the Phaeophyta were 14:0, 16:0, 18:1(n-9), 18:2(n-6), 18:3(n-3), 18:4(n-3), 20:4(n-6) and 20:5(n-3). C18PUFAs are of greater abundance in the brown algae than in the red algae examined. All three green algae from the Ulvales had similar fatty acid patterns with major components, 16:0, 16:4(n-3), 18:1(n-7), 18:2(n-6), 18:3(n-3), and 18:4(n-3). They contained 16:3(n-3) and more 16:4(n-3), were rich in C18PUFAs, chiefly 18:3(n-3) and 18:4(n-3) and had 18:1(n-7)/18:1 (n-9) ratios higher than 1. (C) 2002 Elsevier Science Ltd. All rights reserved.
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多细胞趋磁原核生物(Multicellular magnetotactic prokaryotes,MMPs) 是一类由7~45 个含有磁小体的革兰氏阴性细胞聚集而成的球形或者椭圆形 的细胞聚集体,是研究生命起源与进化、细胞分化和生物矿化的模式生物, 目前仅在大西洋沿岸具有一定盐度的层化水体或沉积物中发现。 本文通过光学显微镜和电子显微镜研究了黄海沉积物MMPs 的超微结 构、运动特点和分裂方式等生物学特征,调查了MMPs 的生态分布特征,并 对其尝试培养。 根据形态差别,黄海沉积物的MMPs 可分为花瓣型MMPs(rosette-like MMPs)、菠萝型MMPs(pineapple-like MMPs)和松球型MMPs(pinecone-like MMPs)。花瓣型MMPs 是由23±4 个卵圆形的细胞螺旋形排列而成的球形聚 集体,直径为5.4±0.8 μm,鞭毛周生。细胞内外膜附近有子弹头形/和方形的 铁氧化物型磁小体。菠萝型MMPs 是由39±9 个方形细胞组成的大小为9.6±1.2 μm ×7.8±0.9 μm 的椭圆形聚集体,鞭毛周生。这类MMPs 由多环细胞组成的, 从椭圆体的赤道面向两极,细胞环的直径变小;在每一环内,细胞像书本似 并列相连;相邻两环的细胞为交错式相连。这种结构比花瓣型MMPs 的更为 紧密。菠萝型MMPs 的磁小体均为子弹头形铁氧化物,磁小体的排列与MMPs 的长轴近似平行。松球型MMPs 是由多个长条形的细胞围绕中心的一个凹陷 辐射排列而成的球形聚集体,直径在9.0~14.2 μm 之间。尼罗红和DAPI 染 色发现三种MMPs 均具有脂类颗粒,花瓣型MMPs 和菠萝型MMPs 在聚集体 的表面具有一层外膜,这说明MMPs 的细胞排列具有高度组织性,在一定程 度证明它属于多细胞生物。 花瓣型MMPs 和菠萝型MMPs 分裂时均保持多细胞形式,但花瓣型 MMPs 沿着聚集体的短轴分开,而菠萝型MMPs 沿着长轴分开。两种MMPs 具有MMPs 典型的逃逸运动,花瓣型MMPs 和菠萝型MMPs 的运动速度分别 为55±26 μm/s 和99±50 μm/s。 黄海花瓣型MMPs 的超微结构、运动方式和分裂特点与大西洋沿岸多个 地区发现的MMPs 相似,花瓣型MMPs 可能是MMPs 的优势类群。菠萝型 MMPs 从整体形态、细胞排列和分裂方式上与花瓣型MMPs 显著不同,是一 类新的MMPs。松球型MMPs 是一类尚未报道的MMPs。 对MMPs 的生态分布调查发现,花瓣型MMPs 广泛分布于砂质沉积物中, 最大丰度出现在氧化还原跃层(redoxcline)。菠萝型MMPs 多分布在砾石沉 积物的表层。两种MMPs 占据不同的生态位,暗示着两者可能具有不同的生 理代谢途径。 对MMPs 的培养发现,在实验室内MMPs 可存活8 个月,MMPs 丰度随 着时间变化出现周期性的变化,推测其繁殖周期可能是10~15 天。 本文为太平洋沿岸MMPs 的首次研究,支持MMPs 在全球广泛分布的观 点,并展示了MMPs 的形态多样性。
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Marine sponges (Porifera) possess an extraordinary diversity of bioactive metabolites for new drug discovery and development. In vitro cultivation of sponge cells in a bioreactor system is very attractive for the sustainable production of sponge-derived bioactive metabolites; however, it is still a challenging task. The recent establishment of sponge primmorphs, multicellular aggregates from dissociated mixed-cell population (MCP), has been widely acknowledged to hold great promise for cultivation in vitro. Here we present a new method to establish an in vitro sponge primmorph culture from archaeocyte-dominant cell population (ADCP) enriched by a Ficoll gradient, rather than a mixed-cell population (MCP). Our rationale is based upon the totipotency (the ability of a cell to differentiate into other cell types) of archaeocyte cells and the different biological functions of various sponge cell types. A sponge, Hymeniacidon perleve collected from the China Yellow Sea was used as a model system for this investigation. Distinct dynamics of primmorph formation were observed while significant increases in DNA synthesis, cell proliferation (up to threefold), and cell growth (up to fourfold) were achieved. Furthermore, a time-dependent spiculogenesis was clearly demonstrated in our longterm culture, indicating high metabolic activity of primmorphs from the ADCP. This new method represents an important step forward to advance sponge cell culture in vitro that may lead to commercial exploitation of sponge-derived drugs. (C) 2003 Wiley Periodicals, Inc.
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Conductive polyaniline was found to have special marine antifouling property. The coating from conducting polyaniline and epoxy resin(or polyurethane) can last 6-9 months in Southern China sea, i.e., less than 10% of the coating surface was fouled during this period. The conducting polyaniline has special synergetic antifouling effect on other antifouling agents like cuprous oxide or 4, 4'-dichlorodiphenyltrichloroethane. The conductivity of the polyaniline was found to be extremely important for its antifouling effect. Moreover, employing aliphatic polyamine as solvent of emeraldine base and curing agent of epoxy resin, a new technique to process corrosion prevention coating containing emeraldine base was developed, therefrom the emeraldine base and epoxy resin was in molecular level blending. This technique was solvent free and extremely effective, i.e., only 1wt% of emeraldine base in the coating can have good corrosion prevention property.
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Genetic differentiation of the shrimp Penaeus chinensis in the Yellow Sea and Bohai Sea was investigated using the mitochondrial control region (CR). RFLP of a partial CR segment (613 bp) shows that 106 out of 122 (86.9%) individuals from six sampling localities along the coast of northern China and the west coast of the Korean Peninsula share the same haplotype, and the haplotype frequencies among localities are not significantly different. The findings are further confirmed by sequencing the complete CR. Divergence of the complete CR (992 bp) is less than 1.6% in 14 individuals from the six localities. F-statistics based on RFLP data and the TCS network of sequencing data suggest little genetic differentiation of P. chinensis in the Yellow Sea and Bohai Sea. Mismatch analysis suggests a rapid expansion of P. chinensis population to the Yellow Sea and the Bohai Sea, which probably occurred with the rapid rise in sea level after the last glacial maximum. Despite the lack of genetic heterogeneity, we propose that P. chinensis populations in this region should be treated as separate management units, as fishery management programs have to be applied on a local basis by different governments.
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ISSR analysis was used to investigate genetic variations of 184 haploid and diploid samples from nine North Atlantic Chondrus crispus Stackhouse populations and one outgroup Yellow Sea Chondrus ocellatus Holmes population. Twenty-two of 50 primers were selected and 163 loci were scored for genetic diversity analysis. Genetic diversity varied among populations, percentage of polymorphic bands (PPB) ranged from 27.0 to 55.8%, H(Nei's genetic diversity) ranged from 0.11 to 0.20 and I(Shannon's information index) ranged from 0.16 to 0.30. Estimators PPB, H and I had similar values in intra-population genetic diversity, regardless of calculation methods. Analysis of molecular variance (AMOVA) apportioned inter-population and intra-population variations for C crispus, showing more genetic variance (56.5%) occurred in intra-population, and 43.5% variation among nine populations. The Mantel test suggested that genetic differentiation between nine C. crispus populations was closely related with geographic distances (R = 0.78, P = 0.002). Results suggest that, on larger distance scale (ca. > 1000 km), ISSR analysis is useful for determining genetic differentiations of C crispus populations including morphologically inseparable haploid and diploid individuals. (c) 2007 Elsevier B.V. All rights reserved.
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Fenneropenaeus chinensis is confined to the Yellow Sea and Bohai Sea in China and the West Coast of the Korean Peninsula. Intra- and intercross populations were produced between Rushany (YP) and Korean (KN) populations. Seven traits were recorded. The heterosis of hybrids was computed and comparison between treatments was performed by ANOVA. At the fourth month after post-larvae, six indexes of growth trait and viability showed a range of heterosis, ranging from 0.514% to 14.950%. At the fifth month after post-larvae, six indexes of growth trait and viability ranged from -9.000% to 19.090%. The negative heterosis was observed in CL, HST and viability. The heterosis of KN female xYP male tended generally to increase as the age of the Chinese shrimp increased while the heterosis of YP female xKN male tended to decrease. The results indicated that the viability of reciprocal hybrids were not significantly different (P > 0.05) from their parents during the experiment. The result of ANOVA indicated that the F1 hybrids were significantly different (P < 0.05) in WST and TW at the fourth month. The multiple comparisons of LSD test indicated that the hybrids of YP female xKN male were significantly different (P < 0.05) from their parents in TW. The hybrids of YP female xKN male were significantly different (P < 0.05) from the other three combinations in WST. At the fifth months, the F1 hybrids had significant difference (P < 0.05) in body weight while other traits showed no significant differences (P > 0.05) from their parents. The multiple comparisons of LSD test indicated that the hybrids of KN female xYP male were significantly different (P < 0.05) from the KN parents in TW. The results indicate that in experimental conditions, the F-1 hybrids created from two populations of Chinese shrimp showed a certain level of heterosis for growth performance and viability. The crossing scheme may improve growth performance and viability in Chinese shrimp, but the improvement may be limited because effective crossbreeding requires the maintenance of pure, preferably inbred, lines and possibly involves specialized sire and dam lines. Therefore, the exploitation of heterosis through single crossbreeding in Chinese shrimp is of limited utility in practical commercial shrimp aquaculture in spite of the potential of significant heterosis. The crossbreeding of different populations can be applied in the establishment of base populations.
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This study investigates the distribution of black carbon (BC) and its correlation with total polycyclic aromatic hydrocarbons (I PAH) pound in the surface sediments of China's marginal seas. BC content ranges from < 0.10 to 2.45 mg/g dw (grams dry weight) in the sediments studied, and varied among the different coastal regions. The Bohai Bay sediments had the highest BC contents (average 2.18 mg/g dw), which comprises a significant fraction (27%-41%) of the total organic carbon (TOC) preserved in the sediments. In comparison, BC in the surface sediments of the North Yellow Sea, Jiaozhou Bay, East China Sea and the South China Sea is less abundant and accounted for an average of 6%, 8%, 14% and 5%, respectively, of the sedimentary organic carbon pool. The concentration of I PAH pound in the surface sediments ranges from 41 to 3 667 ng/g dw and showed large spatial variations among the sampling sites of different costal regions. The Bohai Bay has the highest I PAH pound values, ranging from 79 to 3 667 ng/g dw. This reflects the high anthropogenically contaminated nature of the sediments in the bay. BC is positively correlated to TOC but a strong correlation is not found between BC and I PAH pound in the surface sediments studied, suggesting that BC and PAHs preserved in the sediments are derived from different sources and controlled by different biogeochemical processes. Our study suggests that the abundance of BC preserved in the sediments could represent a significant sink pool of carbon cycling in China's marginal seas.
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Well-dated, high-resolution records of planktonic foraminifera and oxygen isotopes from two sediment cores, A7 and E017, in the middle Okinawa Trough reveal strong and rapid millennial-scale climate changes since similar to 18 to 17 thousand years before present (kyr B.P.). Sedimentation rate shows a sudden drop at similar to 11.2 cal. kyr B.P. due to a rapid rise of sea level after the Younger Dryas (YD) and consequently submergence of the large continental shelf on the East China Sea (ECS) and the retreat of the estuary providing sediment to the basin. During the last deglaciation, the relative abundance of warm and cold species of planktonic foraminifera fluctuates strongly, consistent with the timing of sea surface temperature (SST) variations determined from Mg/Ca measurements of planktonic foraminifera from one of the two cores. These fluctuations are coeval with climate variation recorded in the Greenland ice cores and North Atlantic sediments, namely Heinrich event 1 (H1), Bolling-Allerod (B/A) and YD events. At about 9.4 kyr B.P., a sudden change in the relative abundance of shallow to deep planktonic species probably indicates a sudden strengthening of the Kuroshio Current in the Okinawa Trough, which was synchronous with a rapid sea-level rise at 9.5-9.2 kyr B.P. in the ECS, Yellow Sea (YS) and South China Sea (SCS). The abundance of planktonic foraminiferal species, together with Mg/Ca based SST, exhibits millennial-scale oscillations during the Holocene, with 7 cold events (at about 1.7, 2.3-4.6, 6.2, 7.3, 8.2, 9.6, 10.6 cal. kyr BP) superimposed on a Holocene warming trend. This Holocene trend, together with centennial-scale SST variations superimposed on the last deglacial trend, suggests that both high and low latitude influences affected the climatology of the Okinawa Trough. (c) 2006 Elsevier B.V. All rights reserved.
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A new ocean wave and sea surface current monitoring system with horizontally-(HH) and vertically-(VV) polarized X-band radar was developed. Two experiments into the use of the radar system were carried out at two sites, respectively, for calibration process in Zhangzi Island of the Yellow Sea, and for validation in the Yellow Sea and South China Sea. Ocean wave parameters and sea surface current velocities were retrieved from the dual polarized radar image sequences based on an inverse method. The results obtained from dual-polarized radar data sets acquired in Zhangzi Island are compared with those from an ocean directional buoy. The results show that ocean wave parameters and sea surface current velocities retrieved from radar image sets are in a good agreement with those observed by the buoy. In particular, it has been found that the vertically-polarized radar is better than the horizontally-polarized radar in retrieving ocean wave parameters, especially in detecting the significant wave height below 1.0 m.
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该文对中国黄海和东海的蓝细菌在春、秋两季的生态分布特点进行了研究和比较,对黄海蓝细胞从10月至次年6月的生态分布进行了研究.1.东黄海海区:在秋季(2000年10月19日至11月29日)和春季(2001年3月26日至4月24日)两个季节中蓝细菌丰度在0.19~7.84×10<'4>cell/ml之间,生物量在0.56~13.74μgC/L之间,整体水平上春季比秋季高(蓝细菌的丰充与生物量平均值春季分析为4.83×10<'4>cell/ml和7.25μgC/L;秋季分别为1.72×10<'4>cell/ml和5.07μgC/L),东海比黄海高(蓝细菌生物量平均值春季黄海和东海分别为4.42μgC/L和5.52μgC/L;秋季黄海和东海分别为7.02μgC/L和7.45μgC/L).2.黄海海区:黄海蓝细菌丰度与生物量随时间变化趋势为10月至12月降低(蓝细菌丰度分别为15×10<'4>cell/ml和1.19×10<'4>cell/ml,生物量分别为4.41μgC/L和3.49×10<'4>cell/ml),4月(蓝细菌丰度与生物量分别为4.68×10<'4>cell/ml和7.02μgC/L)与12月相比有明显增高,蓝细菌丰度4月是12月的3.93倍,生物量4月是12月的2.01倍,4月至6月蓝细菌生物量大致稳定,略有增加(5月和6月蓝细菌丰度分别为5.23×10<'4>cell/ml和5.25×10<'4>cell/ml,生物量分别为7.85μgC/L和7.88μgC/L).研究发现蓝细菌在水体中的垂直分布与温度变化比较一致.
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海洋浮游纤毛虫是在海洋中浮游生活的一类单细胞原生动物,主要是指寡毛类纤毛虫(Oligotrich ciliates),隶属原生动物界(Protozoa)、纤毛门(Ciliophora)、寡毛纲(Oligotrichea),分属于Oligotrichina 和Tintinnina两个亚纲。它们个体微小,粒径在5-200 µm之间,是微型浮游动物和海洋微食物环(Marine Microbial Food Web)的重要组成部分。 2006年4月至2007年12月,在黄海(包括胶州湾)采样分析海洋浮游纤毛虫的种类组成(砂壳纤毛虫)、丰度和生物量,分析纤毛虫在这一海区的季节变化和空间变化。 纤毛虫丰度和生物量的研究方法为:Rosette采水器(胶州湾用Niskin采水器)采集水样,取1 L水样,加Lugol’s试剂固定(终浓度1%),Utermöhl方法100倍镜检。测量虫体的体长、体宽,按最接近的几何形状(圆柱体、球体和圆锥体)计算体积。生物量由体积乘转换系数(0.19 pgC/µm3)得到,砂壳纤毛虫的肉体体积按照壳体积的1/3近似。 本文的结果表明,胶州湾各站纤毛虫平均丰度于6月达到全年最高值6065 ind./L,12月为全年丰度最低值843 ind./L。平均生物量8月达全年最高值(18.5 µg C/L),6月为全年最低值(0.6 µg C/L)。砂壳纤毛虫种丰富度于8月达到最高值,共发现25种砂壳纤毛虫,1月种类最少(6种)。湾内站位的纤毛虫平均丰度比湾外的高(6月和8月除外)。砂壳纤毛虫在纤毛虫总丰度中的比例较小,平均为25%,范围为8-57%,分别于1月和8月达到最低和最高值。 两次冷水团大面调查结果表明,4月表层纤毛虫平均丰度(1490 ind./L)要高于10月(972 ind./L)。10月表层纤毛虫生物量0.14-5.33 µg C/L,14194站、15694站和15894站生物量较高,为4.08-5.33 µg C/L。无壳纤毛虫优势种Laboea strobila在两个航次中均呈现斑块分布,4月航次丰度0-10000 ind./L,10月航次丰度11-350 ind./L;砂壳纤毛虫优势种Ptychocylis obtusa仅在4月航次发现,最大丰度2895 ind./L,10月航次未发现。4月航次砂壳纤毛虫有百乐拟铃虫(Tintinnopsis beroidea),丰度为0-1920 ind./L;卡拉直克拟铃虫(Tintinnopsis karajacensis),丰度很小(10-93 ind./L)。10月航次砂壳纤毛虫优势种Tintinnidium primitivum,丰度为35-700 ind./L;也出现了尖底类瓮虫(Amphorellopsis acuta)和网纹虫(Favella spp.),但丰度不大(0-210 ind./L);运动类铃虫(Codonellopsis mobilis)、筒状拟铃虫(Tintinnopsis tubulosoides)和Eutintinnus sp.丰度也较低(35-105 ind./L);Craterella torulata丰度为0-120 ind./L,主要分布于15694站。10月航次已经出现了温跃层,位于30 m左右水层,纤毛虫主要分布于温跃层之上。 六次黄海断面航次表明:温跃层在5月已经出现,到12月消失。在有温跃层的5月、6月、8月、9月,纤毛虫主要分布于温跃层(30 m左右)之上。其中8月份航次纤毛虫丰度最高,表层平均丰度3103 ind./L。12月份纤毛虫丰度最低,表层平均丰度406 ind./L。纤毛虫生物量春夏季为0.02-5.5 µg C/L,冬季为0.04-1.99 µg C/L。小型无壳纤毛虫占优势,砂壳纤毛虫东方拟铃虫(Tintinnopsis orientalis)、筒状拟铃虫、运动类铃虫、Craterella torulata和Tintinnidium primitivum几乎在各个航次均有分布。
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本论文通过对冲绳海槽南部的MD05-2908孔、北黄海的B-U35、B-U41、B-L44孔和北黄海的299份表层样中的孢粉组成、堆积速率、有机碳氮同位素的综合研究,分析了北黄海的孢粉来源、传播动力和途径,并与其它古气候记录对比,重建了末次冰消期以来东亚季风的演化。 MD05-2908孔孢粉组合特征显示6800-3800a BP间气候温暖干燥,其间存在着两次明显的温度降低、湿度增加阶段,即6800-6600a BP和5800-4850a BP;3800a BP以后,气候变得比较寒冷湿润,中世纪暖期和小冰期分别位于990-480a BP和480-230a BP。 北黄海表层孢粉百分含量等值线图显示北黄海不同海域孢粉来源不同,北黄 海东部海域(123.5°E以东的陆架区域)孢粉主要来源于鸭绿江;北黄海中部海域(123.5°E-122.6°E的陆架区域)孢粉来源比较复杂,既有来自辽东半岛、沿海岛屿、山东半岛,还有由黄海暖流携带而来的;北黄海西部海域(122.6°E以西的陆架区域)孢粉以黄海沿岸流携带而来的黄河来源的为主。 北黄海表层孢粉百分含量等值线图还显示,北黄海东部海域孢粉分布主要受 鸭绿江冲淡水影响,波浪和潮汐的作用较弱;北黄海中部海域孢粉分布受黄海暖流和辽东沿岸流的分支共同影响;黄海暖流与黄海沿岸流在山东半岛东北部相遇,形成一逆时针方向的涡旋,该涡旋控制着北黄海西部海域孢粉的分布。 B-U35孔、B-U41和B-L44孔孢粉组合特征显示,12830-12350a BP时气候 寒冷干燥,植被以旱生草本植物为主,时间上可能对应YD事件;12350-10100a BP时植被以针叶林为主,林下生长着大量蕨类植物,气候寒冷湿润,可能对应着YD事件;10100-6600a BP时植被以落叶阔叶林为主,伴生大量旱生草本植物,气候温暖干燥;6600-5000a BP时植被以针叶-落叶阔叶混交林为主,旱生草本植物含量下降,相对上一阶段温度有所降低,但气候更湿润,可能对应全新世最佳期;5000-4000a BP时针叶林所占比例扩大,温度再次降低,湿度变化不明显;4000-500a BP旱生草本植物含量增加,气候寒冷干燥;500a BP-至今,受人类活动影响,植被遭到严重破坏。 B-U35孔和B-U41孔淡水水生植物花粉百分含量曲线显示11750a BP以来黄河河口地区沼泽湿地面积几经变化。10100-6600a BP时沼泽湿地范围在上一阶段的基础上进一步扩大;6600-2850a BP间沼泽湿地大面积缩小,水生植物属种式微;2850a BP之后黄河河口地区沼泽湿地面积再次扩大,水生植物重新繁盛。 MD05-2908孔蕨类孢子百分含量被用来作为中国东南部季风演化的代用指标。结果显示6800-3800a BP时夏季风较强,其间有两次夏季风减弱阶段,分别位于6800-6600a BP和5800-4850a BP,3800a BP以来,夏季风明显减弱,此期的夏季风减弱除受太阳辐射量的减少影响外,可能还与El Nino的频繁爆发有关。 B-U35孔和B-U41孔蒿属、藜科、麻黄科百分含量被用来作为中国中北部夏季风演化的代用指标。研究表明,11750a BP以来东亚夏季风强度在10100-6600a BP时,显著加强,6600a BP左右,夏季风开始减弱,4000a BP以后夏季风显著减弱。 将MD05-2908孔、B-U35孔和B-U41孔夏季风代用指标进行对比发现,中晚全新世以来中国南-北湿度变化特征正好相反,东亚夏季风强度变化以及由此引起的雨锋的南进北撤可能是导致中国不同区域中晚全新世以来降雨量不同的主要原因。
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该文论述了春秋季黄东海大型底栖动物的生态学特点,并结合历史资料,对底栖动物的季节变化及年际变化作了初步探讨.论文所需资料由2000年10~11月与2001年3~4月在黄东海进行的春秋季调查获得,在121~127<'0>E.26~26<'0>N之间海域共设49个大型底栖动物取样站.除少数种类待鉴定外,两次调查共发现四大类群底栖动物543种,其中多毛类39科147种,软件动物56科182种,甲壳类41科144种,棘皮动物21科70种.该文对黄东海大型栖动物种类分布特点、生物量及栖息密度的分布与季节变化进行研究,并计算生物多样性指数,作生物多样性分析.