春季与秋季渤海蓝细菌(聚球蓝细菌属)的分布特点

利用荧光显微镜技术研究渤海中蓝细菌 (聚球蓝细菌属 Synechococcus)的分布特点。发现春季 (1 999年 4～ 5月 )蓝细菌生物量较低 (0 .86～ 0 .0 1 mg C/m3,平均 =0 .1 3 ) ,秋季 (1 998年 9～ 1 0月 )较高 (1 6.6～ 0 .3 7mg C/m3,平均 =3 .2 7)。秋季蓝细菌生物量的平均值 (3 .2 7)是春季的 (0 .1 3 ) 2 5倍。虽然不同水层蓝细菌的生物量与水温分布相反 ,但水温仍是影响蓝细菌季节变化差异的主要原因。春秋季蓝细菌生物量垂直变化都是 1 0 m层 >表层 >底层。蓝细菌生物量在浮游植物总生物量中所占比例 (CB/PB) ,秋季是 0 .3 99～ 0 .0 0 3 (平均 0 .0 64) ,春季是 0 .0 47～ 0 .0 0 0 (平均 0 .0 0 3 ) ,两季相差达2 1倍 (平均值 )。小型浮游生物是渤海蓝细菌的主要捕食者 ,蓝细菌在渤海微食物环中有重要作用。     

浮游细菌在黄海冷水团中的分布

采用荧光显微镜直接计数和分级培养的方法对黄海冷水团水域的浮游细菌分布及其摄食压力来源进行了研究,结果表明：在所研究水域聚球（Synechococcus spp.）蓝细菌生物量的变化是0.78～33.49 mg C/m^3（平均为6.26 mg C/m^3,n=197）,最高值是最低值的40多倍;异养细菌生物量的变化是1.58～21.25 mg C/m^3（平均为5.79 mg C/m^3,n=197）,最高值是最低值的13倍.在垂直方向上聚球蓝细菌生物量表现为中层》表层》底层,异样细菌生物量表现为表层》中层》底层.聚球蓝细菌对浮游植物总生物量的贡献（CB/PB）为2%～99%（平均为42.5%）,而异养细菌生物量与浮游植物生物量的比值为 0.05～6.37（平均为0.85）.在浮游细菌的昼夜变化中,聚球蓝细菌的最高值是最低值的8.8倍,异养细菌最高值是最低值的2.8倍,但二者的昼夜变化规律不明显.浮游细菌的分布与水温和盐度变化基本一致,且浮游细菌生物量最低值出现在冷水团水域.另外在冷水团区域聚球蓝细菌的主要摄食者是小型浮游动物（Microzooplankton,20～200 μm）,摄食率约为0.20～0.42/d.     

三亚湾秋、冬季浮游植物和细菌的生物量分布特征及其与环境因子的关系

分别于2004年10月(秋季)和2005年1月(冬季)对三亚湾进行了现场综合调查,研究了海区浮游植物和细菌生物量的分布特征,探讨了它们与DIN、PO34-、DO、BOD5等环境因子的关系。结果表明,海区平均叶绿素a浓度秋、冬季分别为:(1·40±0·78)mg/m3和(2·25±3·62)mg/m3;浮游植物生物量秋季为:(70·36±38·91)mgC/m3,冬季为:(112·57±181·38)mgC/m3。海区细菌的丰度秋、冬季分别为:(9·87±5·90)×108cells/L和(6·58±2·43)×108cells/L;平均细菌生物量秋季为:(19·73±11·81)mgC/m3,冬季为:(13·15±4·86)mgC/m3。表、底层浮游植物和细菌的生物量分布均呈现三亚河口最高,离岸逐渐降低的态势,三亚河的陆源物质输送及其入海扩散是引起此分布特征的主要原因。温度是造成秋季细菌的生物量高于冬季的原因之一。溶解无机氮为控制表层浮游植物和细菌分布的重要因子。秋季除表层DIN外各环境因子与浮游植物和细菌生物量都不存在明显的相关性;冬季表层DIN、PO43-、DO和BOD5均在p<0·01水平下与二者呈非常显著相关,底层仅DIN和BOD5在p<0·01水平下与二者呈非常显著正相关。三亚湾浮游细菌和浮游植物生物量间的相关性明显,初级生产是水域浮游细菌分布的重要影响因素。     

1998～1999年春秋季渤海中部及其邻近海域叶绿素a浓度及初级生产力估算

根据 1 998年 9月和 1 999年 4月两次调查研究表明 :1 998年秋季 ,调查区 (37°N～ 41°N,1 1 7.5°E～1 2 2 .5°E)表层叶绿素 a浓度介于 0 .0 4 6～ 5.885 mg/ m3,平均为 1 .892 mg/ m3;1 999年春季介于 0 .1 70～8.0 92 mg/ m3,平均为 1 .62 1 mg/ m3。叶绿素 a的平面分布与历史资料相近月份的分布趋势基本一致 ,调查区南部是整个调查海区的高值区 ,而西部及渤海海峡在不同时期出现过高值 ,中央海区叶绿素 a的浓度都比较低。叶绿素 a浓度剖面分布在春季是从调查区西部、渤海中部到渤海海峡依次增高 ,而秋季刚好相反 ;从调查区南部、渤海中部到北部的变化趋势在春季和秋季都是依次降低的。在连续站进行的现场测量碳同化数介于 0 .2 63～ 4.649mg C/ (mg Chla· h)之间 ,平均值为 1 .91 6 mg C/ (mg Chla· h)。 1 998年秋季 ,调查区水柱初级生产力介于 1 0 .1～ 458.3 mg C/ (m2· d) ,平均为 1 63.6 mg C/ (m2· d) ,初级生产力的高值区位于海峡口附近。1 999年春季 ,介于 64.9～ 740 .6mg C/ (m2· d) ,平均为 32 3.7mg C/ (m2· d) ,初级生产力的高值区位于海峡口附近和黄河口附近。同历史资料相比 ,初级生产力有所下降。观测和模型的结果表明 ,渤海浮游植物生物量的分布与水文条件密切相关 ,而初     

2,4-表油菜素内酯和赤霉素对微拟球藻产油率及脂肪酸组成的影响

分别研究了2,4-表油菜素内酯(EBR)、赤霉素(GA_3)对微拟球藻大洋种生长、产油率及脂肪酸组成的影响。结果表明,5、15 mg/L EBR能显著促进微拟球藻生长和提高其产油率,产油率较对照组分别增加了7.85%和13.97%,但对单位质量藻细胞总脂含量影响不大。50 mg/L EBR则显著抑制该藻生长。5、15和50 mg/L GA_3均显著促进微拟球藻生物量积累。50 mg/L GA_3处理组生物量最高(0.337 g/L),但总脂积累受到一定抑制。总体来看,15 mg/L GA_3对微拟球藻产油率提升效果最显著,达8.184 mg/(L·d)。添加EBR(5、15 mg/L)和GA_3(5、15、50 mg/L)浓度后,饱和及单不饱和脂肪酸(16∶0、16∶1、18∶1)占比下降,多不饱和脂肪酸(18∶2、20∶4和20∶5)占比显著提高。     

2010年两个航次獐子岛海域浮游纤毛虫丰度和生物量

2010年7、8月在北黄海獐子岛海域进行了浮游纤毛虫丰度和生物量的调查。7月浮游纤毛虫的平均丰度为(5107±4451) 个/L,平均生物量为(10.17±9.06) μg C/L。8月浮游纤毛虫的平均丰度为(7894±7212) 个/L,平均生物量为(15.24±18.49) μg C/L。7月表层浮游纤毛虫丰度和生物量均呈现近岸多、远岸少的趋势。8月Y1-3、Y2-5两个站表层纤毛虫丰度较高,Y2-5、Y1-1两个站表层纤毛虫生物量较高。7月STA断面浮游纤毛虫丰度呈现表层或次表层高、底层低的特点。8月STA、Y1断面纤毛虫丰度在表层或次表层高、底层低,而Y2断面纤毛虫垂直分布较一致。7月纤毛虫水体丰度及生物量在近岸较远岸高, 8月纤毛虫水体丰度及生物量在离岛较近的Y2-5、Y1-1两站较高。7、8月航次中分别鉴定出砂壳纤毛虫17和21种,其中拟铃虫属(Tintinnopsis)种数最多,Tintinnopsis corniger Hada, 1964为中国海区的新记录种。7、8月砂壳纤毛虫丰度占纤毛虫总丰度的平均比例分别为(19.0±21.6)%和(13.0±16.1)%;7、8月砂壳纤毛虫生物量占纤毛虫总生物量的平均比例分别为(58.2±33.0)%和(42.6±33.2)%。7、8月两个航次中小型无壳纤毛虫在无壳纤毛虫丰度中均占绝对优势。     

东、黄海春秋季小型底栖生物丰度和生物量研究

《北斗号》调查船分别于 2 0 0 0年 10月和 2 0 0 1年 4月在 2 6°N至 36°N,12 0°E至 12 6°30′E东、黄海陆架浅水区调查中进行了小型底栖生物的取样。研究表明 ,两个航次 (秋季、春季 )小型底栖生物的平均丰度分别为 6 5 4 .2 5± 4 4 1.72 ind/10 cm2 和342 .0 0± 2 5 2 .0 0 ind/10 cm- 2 ,平均生物量分别为 80 7.0 6± 5 17.89μg dwt/10 cm2 和 2 85 .2 5± 173.72μg dwt/10 cm2 ;平均生产量分别为 72 6 3.5 8± 4 6 6 4 .18μg dwt/(10 cm2· a)和 2 5 6 7.2 8± 15 6 3.5 0 μg dwt/(10 m2· a)。两个航次小型生物的平面分布类似 ,即高密度和高生物量区分布在水深等深浅 5 0 m左右的站位上 ,特别是在长江口以南的浙江沿海。共鉴定出 14个小型生物类群 ,按丰度自由生活海洋线虫是最优势的类群 ,秋、春季两个航次的优势度分别为 87.2 %和 91.2 %。其他优势类群依次为底栖桡足类、多毛类和动吻类 ;按生物量优势依次为多毛类 38.1%～ 5 4 .0 % ,线虫 2 8.3%～ 38.1%和桡足类 9.0 %～ 9.4 %。垂直分布的研究表明 ,91%的小型生物分布在 0～ 5 cm的表层内 ,线虫和桡足类分布在 0～ 2 cm的比例分别为 6 3%和 86 %。相关分析表明 ,小型底栖生物的数量分布与粘土含量 (% )、粉砂粘土含量 (% )和中值粒     

东海中华哲水蚤的年产量估算

1 997年至 2 0 0 0年在东海陆架区进行了 4个航次的大面调查 ,用获得的大型浮游生物网样品分析资料应用产量 /生物量比值 ( P/ B)法对中华哲水蚤的年产量做了初步估算。中华哲水蚤的 P/ B比值为6.735 3,在东海的平均年产量为 2 63.94C mg/ ( m2 / a)。全测区年产量为 1 1 0 .745× 1 0 3t碳 ,即 1 1万 t,相当于活体重 1 44 .3万 t。     

人工湿地植物对观赏水中氮磷去除的贡献

研究了处理观赏用轻度富营养化水的人工湿地中植物的生长特性和氮磷去除作用。研究发现 ,所选用的 2 1种植物中 ,有17种植物在人工湿地中生长良好 ,稳定生长 10 5 d以后 ,其平均总生物量在 15 5～ 1317g/ m2之间 ,除了鸭跖草的地上地下生物量比 (A/ U)为 2 0 .5外 ,其余都在 1.18～ 4 .2 9之间。植株地上部 N和 P的浓度分别在 10 .99～ 34.74 mg/ g和 0 .5 9～ 3.81mg/ g之间 ;地下部 N和 P浓度分别在 6 .2 0～ 2 9.5 0 mg/ g及 0 .72～ 3.83mg/ g之间。大部分植物地上部 N和 P的浓度大于地下部 (p<0 .0 5 )。植物的 N、P积累量分别在 2 .10～ 2 4 .4 8g/ m2 和 0 .2 3～ 1.95 g/ m2 之间。在处理轻度富营养化水的人工湿地中 ,植物吸收对氮磷的去除起着主要作用——贡献率分别为 4 6 .8%和 5 1.0 %。植物的氮磷积累量与浓度及生物量之间均存在显著相关 ,所以可以直接以生物量为指标选择人工湿地植物。同时考虑净化和景观效果 ,可为处理城镇轻度富营养化水的人工湿地的植物选择提供参考     

1998／1999年南极普里兹湾邻近海域浮游植物的分布特征

中国第 1 5次南大洋考察从普里兹湾邻近海域获得 2 5个测站的浮游植物样品 ,主要研究了其种类组成、分布及其与环境的关系。浮游植物有 5门 1 6科 2 1属 48种 (变种和变型 ) ,浮游植物平均细胞密度为 2 2 .46× 1 0 3个 /dm3,其中以硅藻类占优势 (84.51 % )。浮游植物分布以近海岸陆架区的细胞密度最高 (4 6 .0 3× 1 0 3个 /dm3) ,其次为陆坡 (4 .40× 1 0 3个 /dm3) ,深海区最低 (3.34× 1 0 3个 /dm3)。表层叶绿素a浓度为 0 .1 6～ 3.99μg/dm3,普里兹湾内和湾西部四女士浅滩海域浓度在 3.5μg/dm3以上 ;平面分布趋势浓度从湾内向西北方向递减 ,深海区浓度在 0 .5μg/dm3以下。浮游植物优势种为硅藻的短拟脆杆藻 (Fragilariopsiscurta)。浮游植物垂直分布密集区位于 0～ 50m水层 ,1 0 0m或 1 0 0m以下水层随深度的增加而细胞密度逐渐减少 ,2 0 0m水层稀少或未见。其密集区位于普里兹湾近岸陆架区 ,而陆坡及深海区细胞密度显著减少。叶绿素a浓度的最大值同样分布在 2 5m或 50m层 ,50m以下的浓度随深度的增加而降低 ,2 0 0m层叶绿素a浓度分布范围为 0 .0 1～ 0 .95μg/dm3。粒径分级叶绿素a浓度以微小型浮游生物的贡献占优势 (56 % ) ,微型浮游生物的贡献占 2 4% ,微微型浮游生物的贡献占 2 0 %。经回     

Modelled larval dispersal and measured gene flow: seascape genetics of the common cockle Cerastoderma edule in the southern Irish Sea

The role of marine currents in shaping population connectivity in the common cockle Cerastoderma edule was investigated in the southern Irish Sea. C. edule is one of the most valuable and exploited shellfish species in the area, yet very little is known about its population dynamics. In the present study, coupled hydrodynamic and particle tracking models are used in conjunction with genetic data collected at twelve microsatellite loci to estimate the influence of the Celtic Sea front on larval transport between the coasts of Britain and Ireland. Genetic analysis highlights the presence of at least three genetic clusters partitioned within locations, suggesting a contact zone between separate subpopulations. Samples collected from the Irish coast are most similar to each other. On the British coast, the Burry Inlet appears genetically isolated while samples collected from the coast of Pembrokeshire show evidence of connectivity between Britain and Ireland. These results agree with the model’s predictions: away from the coastal zone, residual baroclinic currents develop along tidal mixing fronts and act as conduit systems, transporting larvae great distances. Larvae spawned in south Wales are capable of travelling west towards Ireland due to the Celtic Sea front residual current, confirming the action of the Celtic Sea front on larval transport. Sheltered, flood-dominant estuaries such as the Burry Inlet promote self-recruitment. The validation of the model using genetic data represents progress towards a sustainable future for the common cockle, and paves the way for a more effective approach to management of all Irish Sea shellfisheries.     

The estuarine character of the Gulf of Nicoya,an embayment on the Pacific coast of Central America

Hydrography and exchange processes in a tropical estuary, the Gulf of Nicoya, Costa Rica, are described from data collected in 1979 and 1980. The measurements and analyses were made in both the dry season and wet season and include temperature, salinity, and density at twenty locations in the gulf and currents (over a semi-diurnal tidal cycle) at five locations. These new results enlarge on the early study by Peterson (1958). Circulation in the lower gulf shows a marked east-west asymmetry due to the predominant runoff along its eastern shore from Rio Barranca and Tarcoles. The freshened surface water from the upper gulf combines with the runoff from these rivers and flows southward along the eastern side of the lower gulf. This flow is compensated by a northward flow of more saline water on the western side at all depths and on the eastern side along the bottom. The boundary between the southward and northward surface flow is marked by a strong salinity front in the rainy season. There is a rapid increase in tidal energy density toward the shoaling northern reaches of the lower gulf, between San Lucas Island and Puntarenas Peninsula. Enhanced mixing must accompany this increase, and direct measurements in the constriction between San Lucas and Puntaneras show that tidal mixing is dominant in transporting salt into the upper gulf against the freshwater runoff.     

不同潮气量机械通气对大鼠肺组织HMGB1表达的影响

目的观察不同潮气量机械通气大鼠肺组织高迁移率族蛋白1（HMGB1） mRNA及其蛋白的表达水平,探讨HMGB1在呼吸机相关性肺损伤（VILI）发病中的作用。方法24只雄性Wister大鼠随机分为对照组、小潮气量组和大潮气量组,分别采用原位分子杂交技术和免疫组织化学染色法检测肺组织HMGB1 mRNA及其蛋白的表达水平。结果与对照组和小潮气量组比较,大潮气量组大鼠肺组织HMGB1 mRNA及其蛋白表达水平明显升高（均P〈0.01）,小潮气量组与对照组各项指标比较差异无统计学意义（P〉0.05）。结论大潮气量机械通气可诱导肺组织HMGB1 mRNA及其蛋白高表达;HMGB1分泌增多导致肺组织炎症反应扩大,可能是呼吸机相关性肺损伤（VILI）发生的重要因素之一。     

Pancreatic polypeptide is not involved in the regulation of the migrating motor complex in man

The role of pancreatic polypeptide (PP) and motilin in the regulation of the migrating motor complex (MMC) was studied in normal subjects. Both plasma motilin and PP levels changed cyclically in the fasted state and were highest in the late phase II period preceding the activity front in the duodenum. A continental breakfast invariably disrupted the MMC and induced a fed pattern of motility. After the meal plasma motilin levels decreased whereas PP levels rose significantly. Infusion of pure porcine motilin during the fasted state induced an activity front and a rise in plasma PP levels. Infusion of bovine PP in doses producing plasma PP levels above the postprandial values neither induced an activity front nor prevented its occurrence. During PP infusion, however, plasma motilin levels were low, although the activity front was not inhibited. PP seems to have no clear role in the regulation of the motor component of the MMC of man. The role of motilin in the production of the activity front of the MMC is discussed.     

Topographically generated fronts, very nearshore oceanography and the distribution and settlement of mussel larvae and barnacle cyprids

Flow patterns adjacent to shore may prevent or aid shorewardmigration of benthic invertebrate larvae. We hypothesized thata front at the mouth of Sunset Bay, Oregon, prevents shorewarddispersal of larvae, significantly altering settlement of mussellarvae and barnacle cyprids. Settlement was measured at threesets of moorings (three moorings per site) distributed acrossthe front at Sunset Bay. From 6 July to 4 September 2000, sampleswere collected roughly every other day. Concurrently, we madevertical zooplankton tows adjacent to each mooring site andcollected physical oceanographic data. During upwelling-favorablewinds, the front was always present at the bay mouth, separatingsignificantly cooler, saltier and denser offshore water fromthat within the bay. During downwelling winds, the front brokedown and we found no significant difference in the surface physicaloceanographic parameters across the bay mouth. During upwelling,the concentration of mussel larvae was higher seaward of thefront than landward, but there was no significant differencein concentration during downwelling, suggesting that the frontmay act as a barrier to the shoreward dispersal of mussels.Mussel settlement was too low and sporadic to allow statisticalanalysis. There was no difference in cyprid concentrations acrossthe bay mouth whether the front was present or not. Cyprid settlementwas, however, nearly an order of magnitude lower at mooringsseaward of the front than at those landward. A significant cross-correlationwas found between settlement at the offshore mooring and tidalrange (r = 0.464, lag = 0 days) and between settlement at themid and inner moorings and downwelling winds (r = 0.532 midbay, r = 0.532 inner bay, lag = 0 days). Seaward of the front,settlement varied with tidal range, while landward of the front,most settlement occurred as brief pulses during downwellingwinds, periods when the front was not present. We found largedifferences in the distribution of cyprids, and mussel larvaeand cyprid settlement relative to the front; larval distributionsand settlement varied with upwelling versus downwelling windsand was due to differences in the very nearshore (i.e. within100–1000 m of shore) coastal oceanography.     

Tidal dispersal of salt marsh insect larvae within the Westerschelde estuary

In the Westerschelde estuary, salt marshes are present as isolated patches fringing the estuary. In the present paper tidal transport of stem-boring larvae of Agapanthia villosoviridescens (Coleoptera) from salt marshes of the upper reaches of the Westerschelde estuary to marshes of the lower reaches is demonstrated. The evidence for the origin of the larvae is based on comparisons of growth and development characteristics of larvae found in flood debris belts and resident larval populations. These characteristics are different on the various salt marshes along the Westerschelde, probably as a result of estuarine gradients. Additional evidence for the larval origin comes from the plant composition of the flood debris. The occurrence of upward tidal transport is discussed. Considering the comparatively large area of salt marshes in the upper estuary, tidal dispersal of larvae probably will be dominated by transport in seaward direction. So far, very little is known on the role of tidal currents with regard to the exchange between salt marsh populations. The present results suggest that tidal transport may not only be important for dispersal of aquatic organisms in an estuary, but also for organisms inhabiting the semi-terrestrial estuarine salt marshes.     

底栖生物影响下的潮滩微地貌演化数值模拟

潮滩是海岸带湿地的主要类型之一,其中分布的底栖生物对生态环境具有重要的调节作用。潮滩底栖微藻、泥沙与水动力之间存在相互作用,影响潮滩微地貌形态,明晰底栖生物对潮滩微地貌的演化机制至关重要。以黄河三角洲潮滩湿地为研究区,通过构建潮滩微地貌动力模型,探究底栖生物对微地貌格局演化的作用机制,分析底栖生物对微地貌系统稳定性的影响。结果表明(1)底栖微藻生长与泥沙扩散、水流再分配过程交互作用驱动下,潮滩上可形成底栖微藻覆盖的高丘与积水洼地交替分布的规则性微地貌斑图;(2)微地貌斑图的形成提高了潮滩生态系统初级生产力和泥沙淤积高度;(3)底栖微藻与泥沙、水流的交互作用使得潮滩微地貌系统对侵蚀扰动呈现非线性响应行为,系统存在临界点,且在一定侵蚀率范围内存在双稳态;(4)黄河口泥螺入侵使得微地貌系统抵抗侵蚀扰动能力减小,且系统稳定性随泥螺生物量的增加而降低。     

Development of the Drosophila retina,a neurocrystalline lattice

Pattern formation in the Drosophila retina proceeds by the recruitment of cells, along a morphogenetic front, into a lattice. At the advancing front, marked by a dorso-ventral furrow in the eye imaginal disc, cells are organized into ommatidial precursors, each containing cells destined to become photoreceptors 2, 3, 4, 5, and 8. Behind the front, a mitotic wave produces photoreceptors 1, 6, and 7, plus the remaining cells needed to complete the ommatidia. During the third larval instar, the front sweeps anteriorly across the eye disc, leaving a highly ordered pattern in its wake. Preceding the dorso-ventral furrow is a groove that bisects the eye disc into dorsal and ventral halves and presumably plays a role in establishing the equatorial symmetry line. Cell lineage plays little role in pattern formation in the eye. Genetic mosaics show that the cells of each ommatidium are not derived from a single mother cell; the cells appear to be recruited at random at the morphogenetic front. Similarly, the mirror symmetry above and below the equator is not established by a clonal mechanism; a single clone can contribute cells to ommatidia on both sides of the equator.