Larval development of the circular crab,Atelecyclus rotundatus (Olivi) (Crustacea: Brachyura: Atelecyclidae) reared in the laboratory

The complete larval development is described of laboratory-reared Atelecyclus rotundatus and the stages are compared with larvae of other cancrideans (= corystoideans). The results suggest that the subfamily Atelecyclinae requires reappraising and that present larval evidence does not support the currently accepted grouping of families in the Cancridea.     

The shore fishes of Trindade Island,western South Atlantic

Trindade Island (20°30'S, 29°20'W) is located approximately 620 nautical miles (1160km) off the eastern Brazilian coast. Due to its geographical isolation, its ichthyofauna arouses great biogeographic interest. This work intends to provide the first comprehensive checklist for the shore fishes of Trindade Island. Six expeditions were undertaken (1995, 1997, two in 1998, 1999 and 2000—in total 86 days of fieldwork) to survey the ichthyofauna from tidal pools to reefs 30 m deep. A checklist of 97 species belonging to 44 families is presented, with information on the ecology and geographical distribution of each species. The most representative families were the Carangidae (nine species), Serranidae (nine), Labridae (seven), Pomacentridae (five) and Muraenidae (five). Trindade is zoogeographically related to the western Atlantic, since 32% of its species are also found in the continental margin and 12.3% are shared with the western and central Atlantic. Nearly thirty-five percent of the shore fish fauna of Trindade are widespread pan-Atlantic warm-water species. Another 14.6% are restricted to the Brazilian Province. At least six endemic species (6.2%) were found: Malacoctenus sp. (Labrisomidae), Scartella sp., Entomacrodus sp. (Blenniidae), Arcos sp. (Gobiesocidae), Elacatinus sp. and Lythrypinus sp. (Gobiidae). This endemism level is lower than that found on the tropical mid-Atlantic Ridge islands of St. Helena (13.9%), Ascension (15.7%) and St. Paul's Rocks (12.1%).     

Parasitic copepods of Carcharhinidae and Sphyridae (Elasmobranchia) from the Atlantic Ocean

Seventy-four sharks of the families Carcharhinidae and Sphyridae, mainly from the central Atlantic Ocean, were examined. Fourteen species of Copepoda were found on them. Prionace glauca and Sphyrna zygaena are new hosts for the copepod Pandarus floridanus. Kroyeria carchariaeglauci is reported from the nasal cavities of Prionace glauca for the first time.     

A new species of Valettia (Crustacea: Amphipoda) and the relationship of the Valettidae to the Lysianassoidea

The family Vallettidae is re-established to accommodate Valettia coheres Stebbing, 1888 and V. hystrix sp. nov. Although closer to the Lysianassoidea than to any other gammaridean superfamily, characters of the mandible, maxillae, gnathopods and oostegites preclude membership of that superfamily. Further assessments of the Valettidae and other family groups peripheral to the Lysianassoidea will be required before formal high-level classification can be established.     

Little-known Atlantic Cheilostome Bryozoans at the entrance to the Mediterranean

Seven little-known Atlantic species of Bryozoa have been found in the Straits of Gibraltar and are re-described in this paper. For six species their known geographical ranges are significantly increased. They are illustrated by SEM for the first time. New ecological and anatomical data are included. Escharella hexaespinosa Arístegui, 1984 is considered to be a junior synonym of Escharella praealta (Calvet, 1907), n. comb.     

Apodidymochelia,a new genus of gammaridean amphipod from the tropical Atlantic Ocean (Crustacea: Amphipoda: Didymochellidae)

Apodidymochelia castellata, new genus, new species is the second genus and fourth species in the rare and poorly known family Didymocheliidae. Apodidymochelia is separated from Didymochelia primarily on mandible structure. This record extends the known range of the family into the Atlantic Ocean.     

Correlations between North Atlantic Oscillation Index in winter and eastern China Flood/Drought Index in summer in the last 530 years

The time series of winter North Atlantic Oscillation Index （NAOI） in the period of 1429-1983 developed by Glueck and summer Flood/Drought Index （FDI） of eastern China in the period of 1470-1999 from I00 stations are used in this paper to study the potential impact of North Atlantic Oscillation on the climate in China. The analysis has explored some significant lag correlations between FDI and NAOI. The maximum positive correlation coefficients between NAOI and area-mean FDI in eastern and northern China lagging 2-3 years reach at 0.001 significance level, and while there are also negative correlation between NAOI and FDI in central and southern China at significance level of 0.05-0.01. The correlation between FDI and NAOI is time-dependent, i.e. the correlation coefficients between two indices vary from period to period. The highest correlation appeared in the period of 1636-1742, around the Little Ice Age, with the significant level of far above 0.001. The second significant period was from 1951 to 1999, at the level of 0.005-0.002. Both the power spectrum analysis and Morlet wavelet transformation have presented an interesting phenomenon： the area-mean FDIs in eastern and northern China share almost the same oscillation periods with NAOI in the inter-annual, decadal and centurial scales＇ oscillations, i.e. 4-5, about I0, 20-30, around 50 and 80-100 years, etc. The Mann-Kendall Rank Statistic test reveals the significant trend and decadal abrupt changes in the series of area-mean FDIs in eastern and northern China in the past 530 years, while the NAOI in the past 400 years, did not show such trend at the significance level, but presented more frequent changes than those of FDI in China. This difference is perhaps due to the fact that the amplitude of the extremes of reconstructed NAOI series is less than that from instrumental records.     

基于多卫星融合数据的海平面特征分析

利用1993—2008年法国空间局的AVISO多卫星融合高度计资料,采用随机动态、EOF等方法分析全球海平面变化的长期趋势、变化幅度以及季节变化的空间分布特征.结果表明:(a)1993—2008年间太平洋海平面呈西升东降的形态,印度洋绝大部分海区海平面呈上升趋势,大西洋除湾流流域外的其他海区海平面的长期趋势以上升为主;(b)全球海平面变化存在显著的年变化和半年变化等季节信号,无论是半球平均还是洋盆平均,北半球海平面季节变化的振幅明显大于南半球,中纬度海区季节变化的振幅最大;(c)北印度洋海平面季节变化的振幅高于同纬度带的北太平洋和北大西洋;(d)太平洋、印度洋、大西洋三大洋受西边界流、赤道流系等强流影响的海域海平面变化幅度大于周围海域;(e)赤道海域各大洋东、西边界和大洋内区海平面变化不同步,可能受赤道海洋波动的影响较大;(f)厄尔尼诺年,西太平洋暖池和赤道太平洋中部海平面明显降低,赤道东太平洋海域海平面明显升高,赤道印度洋海域东、西边界的海平面变化与其相反.     

南大西洋15°S热液区玄武岩中熔融包裹体组成及意义

熔融包裹体中的硅酸盐子矿物、金属相和流体相可以动态地反映岩浆演化过程中岩浆的成分变化和金属成矿物质从熔浆中出熔分离的过程.本文选取南大西洋中脊15°S(SMAR15°S)热液区玄武岩斜长石熔融包裹体作为研究对象,通过扫描电镜能谱分析和激光拉曼分析,揭示熔融包裹体中熔体相的成分和金属矿物的种类,探讨岩浆作用对成矿的贡献.研究表明,斜长石熔融包裹体中存在黄铜矿、黄铁矿、磁铁矿和铬铁矿等金属子矿物,它们随脱气作用从岩浆中分离并进入岩浆流体相中冷凝结晶.熔融包裹体中金属子矿物与母岩无明显蚀变,共同指示岩浆流体对SMAR15°S热液区块状硫化物的形成可能具有一定贡献.SMAR15°S热液区热液硫化物可能存在岩浆来源.