Detection and quantitative analysis of polychlorinated biphenyls in tilapia from Hawaiian waters

The purpose of this study was to investigate polychlorinated biphenyls (PCBs) contamination in tilapia (Oreochromis mossambicus) collected from the Manna stream and Ala Wai Canal of O'ahu, an island of the geographically isolated Hawaiian archipelago. Our results show that the average concentrations of PCBs varied from 51.90 to 89.42 ng g(-1) lipid weight for the sampling sites. Relative toxic potencies (RTPs) and toxic equivalencies (TEQs) were determined to be 20.38-40.60 ng TCDD g(-1) lipid weight and 2.89-4.17 ng TEQ g(-1) lipid weight by 7-ethoxy-resorufin-O-deethylase (EROD) activity analysis and calculation of PCB concentrations based on toxic equivalency factors (TEFs), respectively. Penta-chlorinated congeners were found to be predominant, which revealed that Aroclor 1254 was a possible major source of PCBs in our fish samples. PCB 118, an indicator PCBs, constituted more than 55% and 30% of the total PCBs and TEQs, respectively. In addition, PCB 118 was found to have a linear correlation to the total PCBs (R = 0.975) and TEQs (R = 0.782). Detection of concentrated PCBs in Hawaiian waters suggests a potentially adverse impact of this pollutant on human health, as well as ecological systems, and suggests the necessity of environmental monitoring and hazard assessment of PCBs within the Hawaiian Islands. (c) 2008 Published by Elsevier Ltd.

Detection of polybrominated diphenyl ethers in tilapia (Oreochromis mossambicus) from O'ahu, Hawai'i

Polybrominated diphenyl ethers (PBDEs) have been detected for the first time at a range from 231.58 to 685.61 ng g(-1) lipid weight in the muscles of tilapia ( Oreochromis mossambicus) collected from O'ahu, an island of the geographically isolated Hawaiian archipelago.

Egonol龙胆三糖苷及Egonol衍生物促雌二醇生成活性研究

对Egonol龙胆三糖苷及以Egonol衍生物对雌二醇生成活性及其相关机制进行了研究。发现Egonol龙胆三糖苷促雌二醇最高生成率在MCF-7、HepG2、ROS1728中分别为157% 、182.4%、226.8%（以空白组200μg/ml睾酮转换成E2值作为100%生成率）。活性的强弱可能与芳香化酶的组织特异性表达情况一致，说明Egonol龙胆三糖苷促雌二醇活性可能与芳香化酶有关。芳香化酶的组织特异性表达与特异性启动子有关系，Egonol龙胆三糖苷在各组织中皆有促雌二醇活性，说明该化合物不是通过调节该酶的基因表达而起作用。 在探究Egonol龙胆三糖苷及其衍生物是否介导cAMP-PKA途径从而影响芳香化酶的表达中，发现该系列化合物在HEK-293T细胞中对cAMP的影响非常弱小。在人HepG2细胞中显示了极强的提高cAMP的作用。而化合物对cAMP的作用与其促雌二醇活性强弱不呈正相关关系，对c AMP-PKA途径的激活可能与胞内雌激素有关。 Egonol龙胆三糖苷及其衍生物对HepG2细胞增殖影响显示，该系列化合物同雌二醇一样有相似的较弱促HepG2细胞增殖作用。而且存在一定剂量依赖性。在瞬时转染有ERE（雌激素作用元件）的HepG2中，Egonol龙胆三糖苷及其衍生物也显示了类似于雌二醇与ERE结合的作用，进一步提示Egonol龙胆三糖苷及其衍生物在HepG2细胞中具备雌激素样作用。 为研究Egonol龙胆三糖苷及其衍生物是否可能直接提高芳香化酶的活性，我们计划将芳香化酶从芳香化酶阳性细胞中克隆后表达到芳香化酶阴性的细胞中。在MCF-7细胞中以Oligo dT为引物合成的cDNA模板，和在ROS1728细胞中以Oligo dT及大鼠引物F链为引物合成的cDNA模板能成功扩增出与芳香化酶全长编码序列大小一致的片段。 Egonol衍生物在HepG2、ROS1728细胞中促雌二醇活性的实验表明，Egonol苯环上引入其它基团可以提高Egonol的活性。 从雌激素经典的基因组效应和非基因组效应两方面对雌激素信号转导研究进展进行了简单的综述。 The promoting effects of egonol gentiotrioside and egonol derivatives on the synthesis of estrogen E2 were studied. In vitro test, egonol gentiotrioside promoted the synthesis of estrogen E2 in MCF-7, HepG2,ROS1728 cell lines with mean yields of estrogen E2 57%,82.4% and 126.8%, higher than those of blank control at a concentration of 100 mg/ml. The difference of estrogen E2 synthesis promoting effects among the cell lines suggested tissue specificity. It is in accordance with tissue specific character of aromatase expression. The evidence implied that effect of egonol gentiotrioside on promoting the synthesis of estrogen E2 was related to the aromatase. Different expression levels of aromatase in different tissues are attributed to their specific promoters, but egonol gentiotrioside can promote the synthesis of estrogen E2, in many tissues,so the fact is controversary to the estimation that this compound regulates the aromatase on gene level. In order to investigate whether egonol gentiotrioside and its synthetic derivatives regulates aromatase activity through the cAMP-PKA signal pathway,we transfected the p CRE-Luc luciferase reporter gene into the HEK-293T cells and HepG2 cells. These compounds had weak activity in promoting the cAMP activity in HEK-293T cells but strong in HepG2 cells.The compounds’effect of promoting the cAMP may be related to their estrogenic activity in cells. The modified HepG2 cell proliferation assay was used to evaluate the estrogenic activity of egonol gentiotrioside and its derivatives. The weak estrogenic activity of egonol gentiotrioside and its derivatives at various concentrations expressed as proliferative effect relative to that of blank control was examined. We transfected the pERE-Luc luciferase reporter gene into the HepG2 cells. These compounds possessed significant activity on estrogen response element compared with the one treated with 10 n M estrogen E2. This evidence indicated that the estrogenic activity of egonol gentiotrioside and its derivatives. In order to investigate whether the egonol gentiotrioside and its derivatives can upregulate the activity of aromatase directly, The full-length of P450 aromatase cDNA encoding aromatase were amplified by using primer Oligo dT in MCF-7,and specific primer in ROS1728,respectively. The structure-activity relationship of Egonol in promoting the synthesis of E2 in HepG2 and ROS1728 cells indicated that introduction of some group on the basic sketon of egonol could improve the effect. The progress in research of signal pathway of estrogen in recent years was summarized.

A quasi-synoptic interpretation of water mass distribution and circulation in the western North Pacific II: Circulation

Using the data of conductivity-temperature-depth (CTD) intensive observations conducted during Oct.-Nov. 2005, this study provides the first three-dimension quasi-synoptic description of the circulation in the western North Pacific. Several novel phenomena are revealed, especially in the deep ocean where earlier observations were very sparse. During the observations, the North Equatorial Current (NEC) splits at about 12A degrees N near the sea surface. This bifurcation shifts northward with depth, reaching about 20A degrees N at 1 000 m, and then remains nearly unchanged to as deep as 2 000 m. The Luzon Undercurrent (LUC), emerging below the Kuroshio from about 21A degrees N, intensifies southward, with its upper boundary surfacing around 12A degrees N. From there, part of the LUC separates from the coast, while the rest continues southward to join the Mindanao Current (MC). The MC extends to 2 000 m near the coast, and appears to be closely related to the subsurface cyclonic eddies which overlap low-salinity water from the North Pacific. The Mindanao Undercurrent (MUC), carrying waters from the South Pacific, shifts eastward upon approaching the Mindanao coast and eventually becomes part of the eastward undercurrent between 10A degrees N and 12A degrees N at 130A degrees E. In the upper 2 000 dbar, the total westward transport across 130A degrees E between 7.5A degrees N and 18A degrees N reaches 65.4 Sv (1 Sv = 10(-6) m(3)s(-1)), the northward transport across 18A degrees N from Luzon coast to 130A degrees E is up to 35.0 Sv, and the southward transport across 7.5A degrees N from Mindanao coast to 130A degrees E is 27.9 Sv.

A subsurface countercurrent along the east coast of Luzon

A hydrographic section in the region east of Luzon was repeated 14 times during the period from 1986 to 1991. The data revealed the existence of a subsurface countercurrent located on the shoreward side of the Kuroshio with its upper boundary at about 500 m. The countercurrent, which should be called the Luzon Undercurrent (LUG), was only about 50 km wide, which is comparable to the baroclinic radius of deformation. Despite considerable variabilities both in velocity profile and intensity, the LUC appears to be a permanent feature. Over the period of observations, the maximum speed in the LUC calculated from the mean temperature and salinity by assuming geostrophy (relative to 2500 db) was 7 cm s(-1) at about 700 m and its mean geostrophic volume transport was 3.6 Sv (1 Sv = 10(6) m(3) s(-1)). About 28% of this transport was composed of the low-salinity North Pacific Intermediate Water (NPIW) advected to the south along the coast of Luzon. (C) 1997 Elsevier Science Ltd.

北太平洋低纬度西边界流的时空特征和变异规律研究

北太平洋低纬度西边界流连接着太平洋热带环流和副热带环流，对于世界大洋经向质量、热量和盐量输送起着重要的作用，对北赤道流（NEC）、源区黑潮（KC）和棉兰老流（MC）的时空特征和变异规律进行研究，对认识北太平洋西边界流海洋在全球气候系统中的作用具有重要的理论和实践意义。 本文利用1957-2006年共50年的涡解高分辨率OFES（OGCM for the Earth Simulator）海洋模式资料，对北太平洋低纬度西边界流的时空特征和变异规律进行了分析，结果表明： （1）涡解高分辨率的OFES模式数据结果较SODA能更好地刻画NMK流系三维空间结构的分布特征；黑潮源区涡结构的变化，MUC、 LUC及NEC下的东向流也得到了较好的刻画；其空间结构与实测结果相吻合。 （2）北太平洋低纬度西边界流NMK流系流量具有明显的季节、年际和年代际变化，NEC、KC和MC流量的变化周期频谱较宽,主要为3－6个月的季节振荡和2-7年左右ENSO尺度周期以及10年以上周期的年代际变化。MC主要表现为准两年周期振荡。 （3）NEC、MC流量变化表现为单峰型分布，春季最大（5月），秋季最小（11月）；KC流量的变化为双峰型，大值出现在春季和夏末秋初，春季最大（4月），秋季次之，冬季最小（1月）。在季节时间尺度上，NEC、MC流量同相变化，除冬季外，KC与MC输运反向。 （4） 在年际时间尺度上，受北赤道流流量变化的影响，NEC与KC、MC流量之间为正相关关系；KC与MC分配量（北赤道流向北、向南的经向分配量）之间则为强的负相关关系，其年际异常变化与NEC分叉位置的变化和冷、暖ENSO事件发生密切相关。分叉位置偏北（南）时，KC分配量小（大）而MC分配量大（小）；在El Nino年，KC分配量小，MC分配量大，La Nina年情况则刚好相反。 （5）在年代际时间尺度上，在70年代末气候跃变以后，NEC、KC和MC流量明显减少，NMK环流系统减弱。NEC的减弱主要受上世纪80年代以后ENSO暖事件发生频率和强度的增加所影响，而KC和MC的减弱则主要受NEC减弱控制。同时发现，NEC分叉位置存有明显的年代际变化，在气候跃变以后有长期偏北的趋势，受其影响，与之相对应的是北赤道流向南经向分配量的增加和向北流量分配率的减少。 关键词：北太平洋，低纬度西边界流，北赤道流分叉，ENSO

若干大洋西边界潜流的分布特征及其形成机制

大洋环流是海盆尺度上海水的持久流动，是海洋中质量、热量输运的主要通道，对全球气候变化有重要影响。经过二十年来的大量调查研究，对海洋上层的风生大洋环流有了比较充分的认识。然而，近几十年来的大量观测显示，大洋环流的垂直结构并非像传统认识的那样单一，在很多区域存在与之反向的次表层潜流，如北赤道流（NEC）下方的北赤道逆流（NEUC）、棉兰老海流（MC）下方的棉兰老潜流（MUC），吕宋岛附近黑潮（KC）下方的吕宋潜流（LUC），东澳大利亚海流（EAC）下方的大堡礁潜流（GBRUC）和东澳大利亚潜流（EAUC），阿加勒斯海流（AC）下方的阿加勒斯潜流（AUC）等。这些潜流一般分布在西边界，或者在西边界处增强，称为“西边界潜流（WBUC）”。与表层环流相比，对次表层潜流的结构和形成机制认识不足，因此利用不断更新的各种实测数据和高分辨率同化数据，通过理论分析和数值试验，探讨研究次表层潜流的分布特征和形成机制，对于大洋环流动力学理论的进一步发展具有重要的科学意义。 本文利用中国ARGO资料中心提供的ARGO资料、全球简单海洋资料同化分析系统产生的SODA同化资料和日本地球模拟器模拟出来的OFES资料，分析了北太平洋潜流（NEUC、MUC和LUC）、南太平洋潜流（GBRUC和EAUC）和南印度洋潜流（AUC）的时间和空间分布特征，并基于温跃层以下转向的地转判据分析了其形成机制。主要结果如下： （1）在菲律宾以东海域，表层的NEC在12N附近的西边界分叉，形成向北的KC和向南的MC。在400-800米左右棉兰老岛东侧128E-130E处出现与上层海流方向相反的潜流MUC，MUC在9N和12N附近转向东并分成2支，汇入NEC下方的2支并行向东流的NEUC。到了1000米左右，吕宋岛东侧122E-124E处出现LUC，而MUC也有向岸的趋势，限制在127E以西的范围，两者在12Ｎ附近相遇，然后转向东汇入NEUC。随着深度的加深，NEUC的北侧分支流轴向北偏移。从SODA资料和OFES资料在8N、18N和138E断面的气候态年平均和月平均温度剖面可以很清晰的看出，温跃层分别呈现东高西低、西高东低和南高北低的趋势，这与各个断面上表层流和次表层逆流之间等值线倾斜方向一致。从月平均的速度剖面可以看出，MC一般位于600db以上，600db以下出现北向次表层潜流MUC，MUC春夏较强，秋冬较弱；KC一般位于500db以上，个别月份深入到2000db，其下方均有南向的LUC出现，LUC春夏较弱，秋冬较强；上层西向NEC的主体一般位于400db以上，其下方均有东向的NEUC出现，NEUC春夏较强，秋冬较弱。 在北太平洋菲律宾以东海域，同时满足两个判据的区域与潜流的发生区域符合情况较好，唯一的不同在于LUC汇入NEUC的区域没有同时满足两个判据。这是由于在吕宋岛和棉兰老岛东侧，海底地形较为陡峭，海流情况较为清晰，沿岸涡较少，而且在此区域内温跃层较浅，这些都为形成温跃层以下的地转流反向提供了充分的条件。 （2）在澳大利亚以东海域，表层的南赤道流（SEC）在澳大利亚东岸15S附近分叉，分为向北的北昆士兰海流（NQC）和向南的东澳大利亚海流（EAC）。500m-1000m，23S附近出现一支北向的次表层海流，沿着澳大利亚陆坡经过大堡礁抵达巴布亚新几内亚沿岸转向东，汇入新几内亚沿岸潜流（NGCUC），这支海流就是大堡礁潜流（GBRUC）。1000m-2000m，SEC下方15S附近出现东向的逆流。在2000m以下，由于地形的影响，海流局限在几个不连续的部分，而且流型较乱。从SODA资料和OFES资料在18S和30S断面的气候态年平均和月平均温度剖面可以很清晰的看出，温跃层均呈现西高东低的趋势。在18S，南向的EAC一般位于400db以上，其下方均有持续的GBRUC出现，一般有两个中心，春夏季较强，秋冬季较弱。在30S断面，EAC一般存在于2000db以上，其下方的次表层流并不规则。从此海域的气候态月平均分布来看，在大多月份没有北向的逆流存在，这说明其下方的次表层逆流并不是一个常年存在的现象。 在南太平洋，同时满足两个判据的区域包括SEC下方逆流的发生区域和澳大利亚东岸的沿岸区域，这些区域部分与潜流的发生区域符合较好，只是在30S左右并没有发生潜流的区域也同时满足判据。这是由于在30S附近，温跃层较深，导致了地转流较深，同时此区域内海底地形变化比较大，虽然在此位置形成了逆向的地转流，但是因为地形的限制，在此区域内不能形成有体系的逆流。 （3）在西南印度洋，SEC在非洲东岸分叉，形成一支源于25S的西南向海流——AC，这支海流平均流速达90cm/s左右，最大速度超过140cm/s。在其下方2000m左右，从35S开始在岸边出现东北向逆流——AUC，速度较小，仅为2cm/s左右。从31S、33S和35S断面的气候态年平均温度断面可以很清晰的看出，温跃层明显呈现西高东低的趋势。从月平均经向流速断面可以看出，在各个月份AC下方均出现不同强度的AUC，AC和AUC之间的等值线倾斜方向与温跃层的倾斜方向一致。 在南印度洋，满足判据的区域包括南非沿岸AUC的发生区域和南非东南的部分海域，南非沿岸的AUC紧靠岸边且深度较深，这是因为此区域内温跃层较深，导致形成的地转流位置较深，而形成的逆流由于与海底的摩擦而大大削弱。南非东南部分海域满足判据，大概是由于此区域海流比较复杂，而且此海域多涡。 表面风应力的强迫以及风生环流的斜压调整，使得潜流所在海域的海平面高度和温跃层倾斜方向相反，热带流涡和副热带流涡西向强化加强了该海域温跃层的倾斜程度，从而导致了次表层地转流反向。因此，大洋中次表层潜流是大洋斜压风生环流不可缺少的重要部分。但是在不同的海域存在不同的地形分布和海流分布，所以此理论只在某些合适的区域得到很好的体现。