毛里塔尼亚外海乌贼成熟个体的体征研究

体征表征动物个体的健康状况,影响个体的体型及其生殖价值。乌贼(Sepia officinalis)营终生一次繁殖产卵,但性腺发育成熟个体的体征变化过程尚未可知。为此,本研究利用残差指标分析方法,对毛里塔尼亚外海分布的乌贼成熟个体的体征及其与体型、摄食强度关系进行了分析研究。结果显示,乌贼雌性成熟个体胴长范围为138～323mm,雄性成熟个体胴长范围为135～343mm;两者胴长呈单峰值区间分布,体质量与胴长呈显著的幂函数关系,幂函数拟合b值小于3。雌性、雄性成熟个体的体征存在一定的波动变化但不显著,在功能性成熟产卵期仍保持较好状态。同时,体征与胴长没有显著的函数关系,但是与胃饱满度密切相关,胃饱满度越高、体征越好;并且雌性、雄性成熟个体的空胃率比较低,在14%～34%之间。结果表明,毛里塔尼亚外海乌贼成熟个体保持个体生长,通过正常的摄食活动保持较好的体征。     

Do shorebirds graze down zoobenthic biomass at the Banc d'Arguin tidal flats in Mauritania?

The 500 km² of tidal flats at the Banc d'Arguin, Mauritania, are a wintering site for over 2 million shorebirds, making this one of the areas with the highest density of shorebirds in the world. In earlier studies, it was found that these huge numbers of birds are dependent on a rather low biomass of benthic animals. To explain this paradoxical situation, we hypothesized that the earlier assessments of biomass in late winter and early spring do not reflect a year-round situation. Benthic biomass may be high when the birds arrive in autumn to be subsequently grazed down in the course of winter. To test this hypothesis, we have determined benthic biomass in September 1988. The result has been compared with a biomass value obtained in February–April 1986 with the same methods and at the same stations. These two biomass values do not differ significantly; so our hypothesis has to be rejected. It has to be admitted, however, that our experimental design cannot discern between differences due to the year of sampling and those due to the season.     

Environmental assessment of frozen common octopus (Octopus vulgaris) captured by Spanish fishing vessels in the Mauritanian EEZ

Mauritania, one of the most dependent fish trade nations in the world, has an important octopus fishery within its EEZ. Fishing treaties between the EU and this Sub-Saharan nation have permitted 24 Spanish cephalopod trawling vessels to target this species for its export as a frozen product, mainly to Spain, Italy and Japan. This article presents Life Cycle Assessment (LCA) methodology in order to assess and compare the environmental impacts related to the capture, processing and exportation of packed frozen octopus from this fishery to the main importing nations. Environmental results show that frozen common octopus presented a remarkable dominance of the fishing vessel activities, due to the high energy intensity of the fishery and to the fact that these activities include harvesting, processing and preliminary packaging. Post-harvesting activities presented low relative contributions in all impact categories, minimizing the food mile effect of exporting to Japan, thanks to the slow transportation through marine freight of frozen octopus. The results for fishery-specific indicators showed regular trends for trawling fleets, with high discard and seafloor impact rates. Therefore, improvement actions focused on the minimization of energy use and fishery-specific impacts and the shift to less ozone layer damaging cooling agents are the main targets in order to improve the sustainability of this product, as long as the slow freighting characteristics of the imported product are maintained.     

Controls on hydrothermal Fe oxide–Cu–Au–Co mineralization at the Guelb Moghrein deposit, Akjoujt area, Mauritania

The Guelb Moghrein Fe oxide–Cu–Au–Co deposit, with a total resource of 23.6 Mt at 1.88% Cu, 1.41 g/t Au, and 143 g/t Co, is hosted by an extensive metacarbonate body. However, it is restricted to up to 30-m wide tabular breccia zones developed parallel to discrete shear zones that transect the host metacarbonates. The Fe–Mg clinoamphibole–chlorite schists represent up to 1-m thick interlayer metasediments and localized viscous shearing in these shear zones. Siderite of the metacarbonate body was deformed into a breccia and was replaced by an ore and alteration assemblage comprised of Fe–Mg clinoamphibole, magnetite, pyrrhotite, chalcopyrite, graphite, Fe–Co–Ni arsenides, arsenopyrite, cobaltite, uraninite, and Bi–Au–Ag–Te minerals. In contact with wall rock amphibolites, the metacarbonate body is enveloped by an alteration halo up to 40 m wide, consisting of biotite, actinolite, grunerite, chlorite, calcite, albite, and quartz. The Guelb Moghrein ore body is structurally controlled by shear zones that developed in the footwall of a regional thrust zone. This thrust separates greenschist facies quartz–sericite schists and biotite–garnet–quartz schists of the Sainte Barbe volcanic unit in the hanging wall from amphibolite facies metavolcanic rocks, metacarbonates, and the Guelb Moghrein ore body of the Akjoujt metabasalt unit in the footwall. Peak temperatures of the latter unit are estimated by hornblende–plagioclase thermometry at 580±40°C. Thrusting was retrograde for the Akjoujt metabasalt unit, but prograde for the Sainte Barbe volcanic unit at P–T conditions of about 410±30°C and 2–3 kbar (garnet–biotite thermometry). Structural and petrological evidences suggest that the ore fluids migrated along the shear zones and reacted with the siderite in the metacarbonate. This evolution and the setting of Guelb Moghrein in the fold-and-thrust belt of the Pan-African to Variscan Mauritanides (Mauritania, West Africa) resemble Proterozoic Fe oxide–Cu–Au–Co deposits such as examples from the Tennant Creek and Mount Isa Inliers, Australia.Electronic Supplementary Material Supplementary material is available for this article at