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1.
目的：研究疏肝健脾解毒方含药血清对MDA-MB-231三阴性乳腺癌（TNBC）细胞凋亡及相关X蛋白（Bax）、B淋巴细胞瘤-2（Bcl-2）蛋白表达的影响。方法：给大鼠灌胃疏肝健脾解毒方制备含药血清,设置空白对照组、含药血清低剂量组、含药血清中剂量组、含药血清高剂量组及阳性对照组,以流式细胞术检测细胞凋亡,Western Blot测定Bcl-12、Bax蛋白表达量。结果：各给药组凋亡率及Bax、Bcl-12蛋白表达水平与空白对照组比较,差异均有统计学意义（P<0.05）;含药血清低、中、高剂量组Bax、Bcl-2蛋白表达水平与阳性对照组比较,差异均有统计学意义（P<0.05）。结论：疏肝健脾解毒方对MDA-MB-231 TNBC细胞具有凋亡诱导作用,其机制可能与干预Bax、Bcl-2蛋白表达有关。 相似文献
2.
海带采用乙醇提取色素,通过柱层析分离纯化其中的岩藻黄素,并最终通过高效制备液相色谱制备了三种岩藻黄素的异构体。通过紫外光谱(UV)、核磁共振氢谱(1H-NMR)以及质谱(MS)对岩藻黄素及其异构体进行了结构表征和鉴定。采用乳腺癌细胞MDA-MB-231模型,对岩藻黄素的体外抗肿瘤活性进行了研究。结果表明,岩藻黄素对乳腺癌细胞生长有显著的抑制作用,其中13-顺和13′-顺岩藻黄素组分对癌细胞的抑制活性最强, IC50值达到23.71μg/mL。全反式岩藻黄素和9′-顺岩藻黄素两种异构体IC50值分别为45.30和27.09μg/mL。qPCR试验表明岩藻黄素各异构体可以通过抑制癌细胞NF-κB家族基因表达而抑制乳腺癌细胞生长。 相似文献
3.
为探讨耐热直接溶血毒素(Thermostabile direct hemolysin,TDH)在体内和体外对小鼠黑色素瘤细胞B16的抑制作用,本研究通过MTT法、克隆形成试验、凋亡试验、Caspase-8和Caspase-3的活性试验、线粒体膜电位的检测以及体内C57BL/6小鼠(Mus musculus)荷瘤实验,比较TDH作用于不同细胞的半抑制浓度(IC50),评价TDH对小鼠黑色素瘤细胞B16的体内外抑制作用。结果发现:人结肠上皮细胞NCM460、人正常肝细胞LO2、人肝癌细胞SMMC-7721和小鼠黑色素瘤细胞B16在TDH处理24 h之后,细胞的半抑制质量浓度IC50分别为151、118、54和48 μg/mL,正常细胞的IC50高出癌细胞近2~3倍。当质量浓度低于20 μg/mL时,TDH以剂量依赖性的方式抑制B16细胞的克隆形成,6 mg/kg TDH在移植瘤模型中显著抑制体内肿瘤的生长(P<0.001)。流式细胞术和荧光试剂盒检测表明:20 μg/mL的TDH能诱导19.4%的B16细胞发生早期凋亡,并激活Caspase-8和Caspase-3,但不影响线粒体膜电位。TDH具有体内外的抗肿瘤活性,可能通过细胞表面的死亡受体介导的凋亡信号通路引起凋亡,从而发挥抗肿瘤作用。 相似文献
4.
Bcl-xL是Bcl-2家族中一类重要的抗凋亡因子,其功能主要是抑制细胞凋亡、促进肿瘤发生。为了探知Bcl-xL在生物硫化物应激中的作用,本实验以耐硫生物单环刺螠(Urechis unicinctus)为研究对象,RACE扩增获得一个长度为1 426 bp的单环刺螠Bcl-xL全长c DNA序列,推导的氨基酸序列包含Bcl-xL4个保守的BH结构域和1个跨膜区域。使用该c DNA的完整开放阅读框序列,构建了原核表达载体p ET28a-Bcl-xL,体外诱导表达该重组蛋白;镍柱纯化得到纯度为90%的纯化蛋白,并制备多克隆抗体。Western blotting结果显示:单环刺螠暴露于50μmol/L硫化物中2 h-24 h内其呼吸肠中Bcl-xL含量显著增加(P0.05),然而在150μmol/L硫化物中48 h-72 h内其呼吸肠Bcl-xL含量显著降低(P0.05),暗示Bcl-xL抑制细胞凋亡途径在单环刺螠应对低浓度硫化物暴露时发挥作用,而在高浓度硫化物暴露下Bcl-xL不能发挥抑制细胞凋亡的作用。 相似文献
5.
目的：探讨血根碱（SAN）对鼻咽癌细胞（CNE2细胞系）增殖和迁移的影响及其可能的作用机制。方法：采用MTT法检测SAN对CNE2细胞增殖的影响,采用细胞划痕实验研究SAN对CNE2细胞迁移能力的影响,采用Western Blot技术检测SAN对CNE2细胞增殖细胞核抗原（PCNA）和上皮-间质转化（EMT）相关蛋白E-钙黏蛋白（E-Cadherin）、N-钙黏蛋白（N-Cadherin）、波形蛋白（Vimentin）表达水平的影响。结果：MTT法检测结果显示,与阴性对照组比较,SAN可以抑制鼻咽癌CNE2细胞的增殖,而且SAN浓度越高,其抑制效应越显著（P<0.05）。细胞划痕实验结果显示,与溶剂对照组比较,SAN可以抑制鼻咽癌CNE2细胞迁移,而抑制效应与药物浓度相关（P<0.05）。Western Blot检测结果显示,与溶剂对照组比较,SAN能降低CNE2细胞中增殖相关蛋白PCNA和EMT相关蛋白N-Cadherin、Vimentin的表达水平,提高E-Cadherin的表达水平（P<0.05）。结论：血根碱能抑制鼻咽癌细胞增殖和迁移,可作为治疗鼻咽癌的潜在药物开展进一步研究。 相似文献
6.
荔枝螺是福建海域常见食用螺类,古方记载和民间长期食用证实具有良好药用价值,但国内外对其生物活性物质的研究还较少.本研究以福建海域疣荔枝螺(Thais clavigera)为研究材料,从疣荔枝螺消化腺部位获得抗癌组分E-EA-2,通过液相色谱、气质联用色谱分析发现其主要成分为6-溴靛红(6-bromoisatine),分子结构式C_8H_4BrNO_2.E-EA-2能有效抑制人乳腺癌MCF-7、人肝癌QGY-7703细胞增殖,药物浓度高于40μg/cm~3时,癌细胞存活率显著降低.E-EA-2能诱导肝癌细胞QGY-7703发生PARP蛋白剪切,加入泛caspase抑制剂使细胞存活率显著提高.同时,E-EA-2使MCF-7细胞核产生固缩,线粒体膜电位显著下降,凋亡细胞数量显著增加.E-EA-2对肝癌细胞QGY-7703的IC50为46μg/cm~3,对乳腺癌细胞MCF-7的IC50为28μg/cm~3,对癌细胞的增殖抑制作用主要是以促凋亡方式实现的. 相似文献
7.
采用小鼠乳腺癌细胞株tsFT210的细胞周期抑制、细胞凋亡诱导、细胞坏死以及对卤虫的毒性为活性指标,对48种海洋微藻的甲醇提取物的抗肿瘤活性进行了筛选。结果表明,以卤虫毒性为活性指标时,9种海洋微藻显示了不同程度的抗肿瘤活性,以tsFT210为筛选模型时,也有9种具有抗肿瘤活性,其中3种为明显的细胞凋亡诱导活性、2种为细胞坏死性活性、1种为G2/M期抑制活性,因此有必要进行开拓海洋微藻药用新资源的研究。 相似文献
8.
目的：运用网络药理学方法探讨阳和汤治疗三阴性乳腺癌的潜在作用机制。方法：通过TCMSP数据库和HERB数据库筛选得到阳和汤的有效成分并预测其相关作用靶点,构建有效成分-靶点相互作用网络图,通过DisGeNET和GeneCards数据库获取三阴性乳腺癌的相关靶点,运用仙桃学术工具在线venny分析获取阳和汤与三阴性乳腺癌的交集靶点,STRING数据库及Cytoscape软件构建蛋白质-蛋白质相互作用（PPI）网络图,并进行基因本体（GO）功能及京都基因与基因组百科全书（KEGG）通路富集分析。进一步通过FerrDb数据库获取铁死亡相关靶点,并与阳和汤、三阴性乳腺癌靶点取交集,进行PPI网络图构建及GO功能、KEGG通路富集分析。结果：筛选得到阳和汤的有效成分86个,其中核心成分为槲皮素、山柰酚等,对应作用靶点207个,三阴性乳腺癌的相关靶点1748个,两者共同靶点89个,其中核心靶点为蛋白激酶B（Akt1）、丝裂原活化蛋白激酶1(MAPK1）、磷脂酰肌醇-3激酶调节亚基1（PIK3R1）等,通过KEGG分析发现,阳和汤治疗三阴性乳腺癌涉及PI3K-Akt信号通路、黏附连接等主要信号通路。进一步获取铁死亡的调控靶点487个,其中MAPK1、过氧化物酶体增殖物激活受体γ(PPARγ)为铁死亡参与阳和汤治疗三阴性乳腺癌的核心靶点。结论：阳和汤治疗三阴性乳腺癌主要涉及多个关键靶点和信号通路,推测铁死亡通路可能是其重要的作用机制。 相似文献
9.
目的：探讨健脾消癌方（JPXA）含药血清对人结肠癌HCT116细胞丝氨酸/苏氨酸蛋白激酶（AKT）、哺乳动物雷帕霉素靶蛋白（mTOR）表达以及对细胞增殖、细胞周期及凋亡的影响。方法：取不同浓度的JPXA含药血清作用于HCT116细胞,筛选JPXA含药血清处理HCT116细胞的半抑制浓度（IC50）,并将HCT116细胞分为实验组和对照组,予以相应处理后,采用CCK-8法检测细胞增殖能力,PI-FACS法检测细胞周期变化,Annexin V-APC 单染法流式细胞仪检测凋亡水平,并采用Rt-PCR检测AKT mRNA、mTOR mRNA水平,采用Western Blot检测AKT、p-AKT、mTOR及磷酸化哺乳动物雷帕霉素靶蛋白（p-mTOR）水平。结果：与对照组相比,实验组HCT116细胞增殖能力显著下降,能使细胞周期停留在G1期及S期,且细胞凋亡水平上升,差异均有统计学意义（P<0.05）。与对照组相比,实验组AKT mRNA、mTOR mRNA表达水平及AKT、p-AKT、mTOR、p-mTOR蛋白含量明显下降（P<0.05或P<0.01）。结论：JPXA能抑制AKT、mTOR表达,对结肠癌细胞的增殖、克隆能力有一定抑制作用,并可在一定程度上促进结肠癌细胞的凋亡。 相似文献
10.
目的:研究卫矛醇对C6胶质瘤细胞株的体外增殖及凋亡的影响。方法：将C6大鼠胶质瘤细胞随机分为对照组、卫矛醇干预组、卫矛醇+雷帕霉素组、卫矛醇+3-MA组,各组予不同药物孵育,采用MTT法检测卫矛醇对C6细胞的体外增殖抑制率,筛选出抑制率相对较高且生长状态良好的细胞;应用Hoechest 33342染色透射电镜观察细胞凋亡亚显微结构的改变,采用免疫荧光和Western Blot技术检测与凋亡和自噬相关蛋白的表达水平。结果:卫矛醇对C6胶质瘤细胞增殖有明显的抑制作用,并呈现出良好的浓度-效应相关性,与对照组比较,随着浓度的增加,细胞的增殖抑制率上升(P＜0.01);Hoechst染色结果显示,与对照组相比,共同孵育卫矛醇24 h后的C6细胞出现明显的核固缩现象,证明有大量的细胞出现凋亡;Western Blot结果显示,与对照组相比,促凋亡基因Bax表达上调,抗凋亡基因Bcl-2表达下调。结论:卫矛醇能够抑制C6细胞的增殖,并诱导其凋亡,其作用机制可能与上调Bax、下调Bcl-2有关。 相似文献
11.
Western boundary currents flow poleward from low latitudes until they ultimately separate from the coast and turn eastward into the ocean interior. The separation is mainly due to either: (i) the variation of the Coriolis parameter with latitude (β) which causes vanishing of the near-wall depth; (ii) vanishing wind stress curl over the ocean interior which forces zero meridional transport; or (iii) opposing currents that flow toward the equator and force the northward flowing currents to turn offshore (Agra and Nof, Deep Sea Research I, 40, 2259–2282). Here, we focus on the third kind of separated currents and show that, due to β, such separated currents migrate along the wall. A nonlinear “reduced gravity” one-and-a-half layer model is used to compute the desired migration speed. Solutions of the primitive equations are constructed analytically assuming that the translation rate is steady. It is found that the migration rate along the wall is given by βRd2 cosα/2 sinγ, where Rd is the Rossby radius, α an angle that measures the inclination of the joint offshore currents relative to the north, and γ is the angle between the axis of the joint offshore currents and the wall. The migration meridional component can be either northward or southward (depending on the inclination of the wall) but the zonal component is always westward. When the separated joint offshore flow is in the east-west direction (i.e. α = π/2 or 3π/2 so that the separated flow is zonal) no migration is taking place. It turns out that the above migration formula is so robust that it is also describes the migration rate in a two-and-a-half layer model where one current is allowed to, at least partially, dive under the other. For most separated currents the computed migration rate is a few centimeters per second.Possible application of this theory to the Confluence zone in the South Atlantic (where significant seasonal movement of the separation latitude has been observed) is discussed. 相似文献
12.
Using the moored MnO2-fiber method, we have obtained 38 determinations of Th and Pa isotope concentrations from 18 sites along the margin of the western North Pacific near Japan, from water depths of 1,330 to 5,873 m. From our data, we are able to show that (1)228Ra and227Ac are being supplied to the seawater from the slope sediments of Honshu, Japan, (2) our230Th and231Pa concentrations match those obtained byin situ pumping with a MnO2-fiber adsorber in the Japan and Izu-Ogasawara trenches but are significantly higher than those from the Panama and Guatemala basins, and (3) our232Th concentrations show a similar systematic decrease with depth as do those of trace metals like Mn, Al, Te and Bi whose concentrations are strongly controlled by particulate matter scavenging.In contrast, our data fail to show (1) that enhanced removal of230Th and231Pa by scavenging from the water column is taking place near the western margins and (2) that231Pa is being removed in preference to230Th from the water column to the marginal sediments. This is probably due to rapid mixing of the deep waters as compared to the scavenging rates of230Th and231Pa in the water column and at the sediment/seawater interface. 相似文献
13.
Intertidal blue mussels, Mytilus edulis, experience hypoxia reoxygenation during tidal emersion and resubmersion cycles, and this is often suggested to represent a major stress for the animals, especially for their respiratory tissues, the gills. We exposed mussels to experimental short and prolonged anoxia and subsequent reoxygenation and analyzed the respiratory response in excised gill tissue and the effects of treatment on reactive oxygen species (mainly ROS: superoxide anion, O2·− and hydrogen peroxide, H2O2), formation using live imaging techniques and confocal microscopy. Our aim was to understand if this “natural stress” would indeed produce oxidative damage and whether antioxidant defenses are induced under anoxia, to prevent oxidative damage during reoxygenation. Exposure to declining pO2 in the respiration chamber caused an increase of gill metabolic rate between 21 and 10 kPa, a pO2 range in which whole animal respiration is reported to be oxyregulating. Exposure of the animals to severe anoxia caused an onset of anaerobiosis (succinate accumulation) and shifted high and low critical pc values (pc1: onset of oxyregulation in gills, pc2: switch from oxyregulation to oxyconformity) to higher pO2. Concentrations of both ROS decreased strongly during anoxic exposure of the mussels and increased upon reoxygenation. This ROS burst induced lipid peroxidation in the mantle, but neither were protein carbonyl levels increased (oxidative damage in the protein fraction), nor did the tissue glutathione concentration change in the gills. Further, analysis of apoptosis markers indicated no induction of cell death in the gills. To our knowledge, this is the first paper that directly measures ROS formation during anoxia reoxygenation in mussels. We conclude that hypoxia tolerant intertidal mussels do not suffer major oxidative stress in gill and mantle tissues under these experimental conditions. 相似文献
14.
Hisashi Narita Ryota Abe Kazuhisa Tate Young-Ill Kim Koh Harada Shizuo Tsunogai 《Journal of Oceanography》2003,59(5):739-750
We report the role of particle composition and lateral particle movement that influences the oceanic distribution of 231Pa and 230Th. Settling particles were collected during sediment trap experiments. These and surface sediments were obtained from five
stations along 38 to 44°N in the northwestern North Pacific. The high total mass flux and seasonal variations in the marginal
area of the western North Pacific are controlled by the supply of lithogenic materials and primary productivity. The high
content of the lithogenic material in the settling particles in this area contributes to 230Thex fluxes that exceed the local rate of supply. The lithogenic materials are important as a carrier of 230Th and contribute to the fractionation between 230Th and 231Pa in the ocean, as the 231Paex/230Thex ratio in the settling particles decreases with increasing 232Th concentration. The 231Paex/230Thex ratio in the settling particles collected in the abyssal basin decreases with water depth, which indicates that lateral transport
of the lithogenic particles from the marginal area and/or shallower depth plays an important role in determining the 231Paex/230Thex ratio in a population of settling particles and remineralization. This indicates that lateral redistribution of particles
and sediment focusing influence the 231Paex/230Thex ratios in surface sediments. Thus, the observations reported here mean that the use of the sediment 231Paex/230Thex ratio as a paleoproductivity proxy will be problematic in the northwestern North Pacific.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
15.
Five manganese nodules collected from the Northern Mid - Pacific have been analysed for their U and Th isotopes.lt is found that the enrichment of thorium compared to uranium is universal in deep- sea manganese, nodules and in the top sides of the nodules there are large excesses of Th and Pa decreasing exponentially with depth. For each of the nodules, the concordant growth rates are obtained from three different methods: 230Thex 230Thex/232Th and 231Paex.The growth rates of manganese nodules are closely related to the chemical compositions of the nodules and the types of the underlying sediments. The growth rates of five nodules are determined to be in the range of 0.79-7.4 mm/106a, in agreement with those predicted from the chemical compositions of the nodules. By the comparison of the extrapolated 230Thex,230Thex/232 Th and 231PaeX data from the top and bottom surfaces of the nodule from Site M21 yields, the nodule turnover time is (9.83-13.7)×104a. 相似文献
16.
The integrity of the caprock of a storage formation is the most crucial parameter for the long-term performance of a geological CO2 storage site. The Sleipner area in the Southern Viking Graben hosts the first and longest operating industrial scale CO2 storage project, where CO2 is injected in a saline aquifer of the Utsira Formation. Time-lapse seismic monitoring shows neither that CO2 has left the Utsira Formation nor indications for fracturing of the caprock by the CO2 injection activity, which is in agreement with previous numerical simulations. However, large chimney structures as close as 7 km from the injection point indicate that the caprock has been breached in the geological past, which may raise questions about the integrity of the caprock above the Sleipner CO2 storage site. Here, we present seismically constrained numerical fluid flow simulations that evaluate the influence of chimney structures on the long-term performance of the CO2 storage operation at Sleipner. The simulation could reproduce the spreading of the Sleipner CO2 plume, which is controlled by the anisotropic permeability field of the Utsira Formation and the regional dip of the formation top. We have performed long-term plume evolution simulations, which show that the injected CO2 will not reach the existing chimney structures assuming a realistic injection duration of 30 years. Our simulations indicate that an unrealistically long injection period between 92 and 140 years would be required for the CO2 to reach the existing chimney structures. In this case, a comparably low chimney permeability of 10 mD may be sufficient to facilitate CO2 migration from the storage formation to the seafloor, once the CO2 has reached a chimney structure. However, the simulations indicate that it is very unlikely that the CO2 may migrate along existing chimney structures at Sleipner. Our results highlight that the reconstruction of palaeo fluid flow systems and the identification of focused fluid conduits should be considered in the assessment of CO2 storage sites. 相似文献
17.
The Shijiutuo uplift is an oil enriched uplift in the offshore Bohai Bay Basin. Petroleum migration is a key factor for oil enrichment in Neogene reservoirs far away from the hydrocarbon kitchen. In this article, an integration of geological, geophysical and geochemical analyses are employed to investigate the petroleum migration and accumulation on the Shijiutuo uplift. Hydrocarbons in the QHD32-6 and QHD33 oilfields are mainly originated from the third (E2s3) and first (E2s1) member of the Shahejie Formation. The shallow traps have significant contributions of late-stage E2s1-derived oil. Lateral petroleum migration is a major mechanism forming large oilfields on the Shijiutuo uplift. The large oilfields have multiple hydrocarbon kitchens, multiple source rocks, and numerous preferential petroleum migration pathways (PPMPs). Once petroleum arrives at the structural highs on the Shijiutuo uplift through the Guantao Formation (N1g) carrier-beds, neotectonic faults cutting through Guantao (N1g) and Minghuazhen (N1mL) formations could serve as effective conduits for vertical petroleum migration. Neotectonic faults have experienced polycyclic fault activities. Fluid inclusions indicate episodic hydrocarbon charging. Crude oils display duplex properties of biodegradation and non-biodegradation, which is strong evidence for multiple and episodic oil charging on the Shijiutuo uplift. Finally, episodic petroleum charging along polycyclic neotectonic faults causes the late-stage E2s1-derived oils to occur in the shallow reservoirs. 相似文献
18.
Alessia M. Rodriguez y Baena Juan Carlos Miquel Pere Masqu Pavel P. Povinec Jerome La Rosa 《Marine Chemistry》2006,100(3-4):269
234Th is a particle-reactive radionuclide widely used to trace biogeochemical oceanic processes occurring over short timescales. During the last few years, small-volume techniques based on the co-precipitation of 234Th with MnO2 coupled with beta-counting have been developed as an alternative to large volume gamma-spectrometric techniques. Here a procedure has been developed to enhance quantitative measurement of 234Th in MnO2 precipitates. The main objectives were to obtain a purified Th fraction for beta-counting and to determine the chemical recovery of 234Th using Th spikes and alpha-spectrometry as an alternative to ICP-MS based methods. Two variations of the procedure are presented. In the first “1 spike” method a 230Th tracer is added to the sample prior to precipitation of MnO2, and UTEVA® extraction chromatography is used to obtain a NdF3(Th) purified source that can be used for both beta-counting of 234Th and alpha-spectrometry of 230Th. In the “2 spike” method a 230Th spike is added and the MnO2(Th) precipitate is directly beta-counted for 234Th and subsequently spiked with 228Th or 229Th prior to UTEVA® purification and alpha-spectrometry. The results confirm the need to process small-volume seawater samples for 234Th measurement in presence of a yield tracer, and show that both the 1 spike and 2 spike methods allow an accurate and precise determination of 234Th (relative percent difference, RPD, between expected and mean measured value < 1%; CV between replicate samples < 3%). Our work also suggests that, although the combined analytical uncertainty on total 234Th measurements accomplished with both versions of the NdF3 procedure is promising (6% for 2-L samples), the precision of the 234Th flux estimation will ultimately depend on the degree of disequilibrium between 234Th and 238U. 相似文献
19.
Intense thermochemical sulfate reduction (TSR) and up to 18% H2S are found in the Upper Permian Changxing Formation (P3ch) in the northeast (NE) Sichuan Basin, China, despite that rare gypsum or anhydrite was found in this formation. Here, we present new concentration data of carbonate-associated sulfate (CAS) from carbonate host rocks, C, O, and Sr isotope data for TSR-related calcites, and S isotope data for sulfur compounds obtained during this study. These data along with spatial-temporal changes in palaeogeopressure conditions, hydraulic conductivity and the physical capacity indicate that the H2S was generated locally from TSR within the P3ch reservoirs. We propose that the reactive sulfates were derived from CAS released during dolomitization and recrystallization of earlier dolomite within the P3ch Fm. and from the cross-formational migration of evaporative brines from the Lower Triassic Feixianguan Formation (T1f) to P3ch Fm. Our calculation shows that the two sources could provide enough SO42− for the generation of H2S within the P3ch reservoirs. Early downward migration of sulfate-rich evaporative brines from the T1f formation occurred in near-surface and shallow burial diagenetic settings (mainly <1000 m). The evaporative brines seeped into porous grainstones and displaced preexisting seawater, causing pervasive dolomitization within the P3ch Fm. Subsequently, TSR calcites precipitated from the pore water have high Sr concentrations (up to 7767 ppm), close to the T1f TSR calcites, and 87Sr/86Sr ratios mainly from 0.7074 to 0.7078, which are significantly higher than those of Late Permian seawater but within the range of early Triassic seawater. 相似文献
20.
《African Journal of Marine Science》2013,35(1):395-400
Long-distance migration patterns of deep-water rock lobster Palinurus delagoae were investigated using tagrecapture data obtained over a period of 6 years (1995–2000). Of 7 654 animals tagged, 363 (4.7%) were recovered from South African and seven (0.1%) from Moçambican waters. Lobsters remained at large for up to 3.2 years and migrated distances of up to 495 km. Some 48.3% of juvenile lobsters (carapace length <65 mm) but only 2.1% of larger lobsters migrated further than 20 km. Movements were mostly north-eastwards (91.7% of migrants), for both sexes, and the migration rate of the fastest 5% of migrants was 0.43 km day?1. P. delagoae seems to have evolved long-distance, counter-current migrations as a retention mechanism to maintain its populations off both South Africa and Moçambique. The resource needs to be managed jointly between the two countries. 相似文献