Distribution of Upper Cretaceous deep water agglutinated foraminifera in sediments of the North Atlantic and its marginal seas (Tab. 1)

The stratigraphic and biogeographic distribution of more than 170 species of deep-water agglutinated benthic foraminifers (DWAF) from the North Atlantic and adjacent marginal seas has been compared with paleoenvironmental data (e.g. paleobathymetry, oxygenation of the bottom waters, amount of terrigenous input and substrate disturbance). Six general types of assemblages, in which deep water agglutinated taxa occur, are defined from the Turonian to Maastrichtian times: 1. High latitude slope assemblages 2. Low to mid latitude slope assemblages 3. Flysch-type assemblages 4. Deep water limestone assemblages (,,Scaglia,,-type) 5. Abyssal mixed calcareous-agglutinated assemblages 6. Abyssal purely agglutinated assemblages Latitudinal differences in faunal composition are observed, the most important of which is the lack or extreme paucity of calcareous forms in high latitude assemblages. East-to-west differences appear to be of comparatively minor importance. Most DWAF species occur in all studied regions and are thus considered as cosmopolitan. Biostratigraphic turnovers in the taxonomic content of assemblages are observed in the lowermost Turonian, mid-Campanian and in the upper Maastrichtian to lowermost Paleocene. These datum levels correspond to inter-regional and time-constant paleooceanographic events, which probably also affected the deep-water benthic biota. This allows us to use deep-water agglutinated foraminifers for biostratigraphy in the North Atlantic sequences deposited below CCD and to geographically extend the currently used zonal schemes which have been established in the Carpathian and Alpine areas.

Biogenic opal and diatoms in surface sediments of the South Western Atlantic

Based on 66 surface sediment samples collected in the SW Atlantic Ocean between 27 and 50°S, this study presents an overview of the spatial distribution of biogenic opal and diatom concentrations, and diatom assemblages. Biogenic opal has highest values in the deepest, pelagic stations and decreases toward the slope. Diatoms closely follow the spatial trend of opal. Diatom assemblages reflect the present-day dominant hydrographical features. Antarctic diatoms are the main contributors to the preserved diatom community in core top sediments, with coastal planktonic and tropical/subtropical diatoms as secondary components. Dominance of Antarctic diatoms between 35 and 50°S in the pelagic realm mirrors the northward displacement of Antarctic-source water masses, characterized by high nutrient content and low salinity. Northward of ca. 35°S, the highest contribution of tropical/subtropical, pelagic diatoms, typical for nutrient-poor and high salinity waters, matches the main southward path of the Brazil Current. Mixing of Antarctic and tropical waters down up to 45°S is clearly illustrated by the diatom assemblage. Concentrations of biogenic opal and diatoms rather reflect the path of predominant water masses, but are less correlated with surface water productivity in the SW Atlantic.

Distribution of diatom species as abundance estimates from vertical multinet hauls from 150 m water depth in the Indian Ocean

During the Indian Ocean Expedition of R/V METEOR phytoplankton samples were taken with a multiple closing net (Multinet) at 103 stations. In this material the diatoms were investigated. In all 247 taxa could be identified which belong to 242 species and 5 varieties of formae of 80 genera. Of these 1 variety, 15 pecies, and 3 genera are newly described. New combinations were made for 18 species, and a number of old combinations was reinstated.

Pesca artesanal del Puerto Supe (Provincia de Barranca, Departamento de Lima) en el año 1998

Durante el año 1998 (*) la pesca artesanal en el Puerto Supe se registra el desembarque de 699 t de recursos hidrobiológicos, constituido por 35 especies hidrobiológicas entre peces (31) e invertebrados (4), entre los peces destacó el ayanque (Cynoscion analis) con 147808 k, el bagre (Galeichthys peruvianus) con 165095 k, la lisa (Mugil cephalus) con 53828 k, la lorna (Sciaena deliciosa) con 27898 k, el machete (Ethmídium maculatum) con 19663 k y el perico (Coryphaena hippurus) con 16472 k y entre los invertebrados el mas importante fue el langostino tití (Xíphopenaeus rivetí) con 220 t de captura. Operaron un promedio de 218 embarcaciones mensuales que realizaron faenas de pesca en 30 zonas, desde las Zorras a Ancón obteniendo un esfuerzo pesquero de 2621 viajes y un rendimiento promedio de 267 k/viaje, se capturaron especies asociadas al fenómeno "El Niño", tales como el perico (Coryphaena híppurus) y langostino tití (Xiphopenaeus rive i), que incrementaron su desembarque y las ausencias de otras especies como el pejerrey (Odontesthes regia regia) y el cangrejo morado (Platyxan thus oÍbignyi) . En Puerto Supe se desembarcaron recursos costeros provenientes de la flota industrial, para ser procesados e las plantas pesqueras harineras, se desembarco 723. 669 t, constituido por 3 especies, en este volumen de captura destacó el ayanque (Cynoscion analís) con 616.006 t, lorna (Sciaena deliciosa) con 105.265 t y el coco (Paralonchurus peruanus) con 2398 t, operaron 19 E/P industriales, que realizaron faenas de pesca en Bermejo y Paramonga con un esfuerzo pesquero de 48 viajes y un rendimiento promedio de 15,076 k/viaje. Los meses que se registraron, estos viajes, fue junio, julio, agosto, y octubre. En Puerto Supe se desembarcó un total de 1422.676 t tanto de la flota industrial y artesanal, obteniendo la pesca industrial 3.4% más que la flota artesanal, que operó en el año 357 días, (Los días 1,2,23 y 29 de Junio, 19 y 28 de Julio 3 y 4 de Octubre no salieron a la pesca por condiciones meteorológicas o fiestas) . La flota industrial opero solo 14 días en el año (01 días en Junio, 06 Julio, 01 en Agosto, y 06 días en Octubre). El arte que utilizaron las embarcaciones industriales fue el cerco anchovetero de tamaño de malla de 1/2 Pulg.