Behaviour and mechanism of feeding of Lathonura rectirostris (Cladocera, Macrothricidae). [Translation from: Zoologicheskie Zhurnal 50, 1002-1010, 1971.]

The behaviour in the feeding process and the functional morphology of Lathonura rectirostris O.F. Muller - one of the widely distributed species of macrothricids - is studied. The current work is an attempt at morpho-functional analysis of the apparatus of the trunk appendages of Lathonura rectirostris O.F. Muller. This highly specialized species, the method of feeding of which basically comes to the mechanical scraping-off and collection of epiphytic single-celled algae and particles deposited on the surface of aquatic plants.

Densidade de plantas e espaçamento entrelinhas para o híbrido de milho BRS 1002.

2008

Recueil de copies et de pièces originales, manuscrites et imprimées, sur la Marine (listes d'officiers, revues, états, procès de discipline, ports de Marseille, Toulon, Dunkerque, Brest, Rochefort, etc., les Galères et les Colonies) de 1663 à 1754. II Années 1663-1699. — Lettres orig. notamment du chevalier de Valbelle, Messine 1676 (p. 191), de Me Agnès de Bonvoison, Toulon 1687 (p. 576 et 588), de M. de la Planche, Boulogne 1687 (p. 582), de M. d'Argenson, Paris 1699 (p. 1002 et 1014).

Contient : Réception d'ambassadeurs (1663-1686) ; Pièces sur l'Acadie et le Canada ; « Lettera scritta da Venetia da un partiale del popolo di Messina all' Eccellentiss. Senato de quella città ». Impr. S. l. n. d., in-8° de 14 pages ; « Arrest de la Cour du Parlement contre la nommée Jeanne Moyon, veuve Jean Lesur, et autres, accusées de prostitution publique. » Impr. Paris, P.-G. Simon, 1750, in-4° de 4 pages ; Extrait de la relation envoyée par M. de Terron du combat naval du 8 janvier 1776 ; Inscriptions de l'Arsenal de Brest, par Victorin Santeul et P. Corneille ; « Discorso sopra le due comete apparse l'anno corrente 1682 gl'ultimi giorni d'agosto... dedicate all' ill. et eccell. sig. Nicolo Doria, senatore della Republica de Genova... » Impr. Gênes, Antonio Casamara, s. d., in-4° de 8 pages ; « Coppie d'une lettre qu'un François écrit à un de ses amis, contenant ce qui s'est passé à Gênes pour célébrer la naissance de Mgr le duc de Bourgogne. » Impr. Marseille, P. Mesnier, 1682, in-4° de 12 pages ; Liste des vaisseaux danois armés à Copenhague en 1683 ; « Liste des officiers qui sont dans les forts Cataracoüy et Niagara. » ; Pièces sur Cayenne ; Pêche de la baleine ; Envoi de denrées en Irlande

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 1002 - Auskunft über den Wohnort der Familie Mertens sowie Mitteilung über den Besitz einiger Schopenhauer-Briefe

u.a. Gustav Mertens; Sibylle Mertens-Schaaffhausen; Nachlass; Professor Heimsoeth; Universitätsbibliothek Bonn;

Stable oxygen isotopes of Globigerinoides ruber and biostratigraphic datums at ODP Site 165-1002

Ocean Drilling Program Site 1002 in the Cariaco Basin was drilled in the final two days of Leg 165 with only a short transit remaining to the final port of San Juan, Puerto Rico. Because of severe time constraints, cores from only the first of the three long replicate holes (Hole 1002C) were opened at sea for visual description, and the shipboard sampling was restricted to the biostratigraphic examination of core catchers. The limited sampling and general scarcity of biostratigraphic datums within the late Quaternary interval covered by this greatly expanded hemipelagic sequence resulted in a very poorly defined age model for Site 1002 as reported in the Leg 165 Initial Reports volume of the Proceedings of the Ocean Drilling Program. Here, we present for the first time a new integrated stratigraphy for Site 1002 based on the standard of late Quaternary oxygen-isotope variations linked to a suite of refined biostratigraphic datums. These new data show that the sediment sequence recovered by Leg 165 in the Cariaco Basin is continuous and spans the time interval from 0 to ~580 ka, with a basal age roughly twice as old as initially suspected from the tentative shipboard identification of a single biostratigraphic datum. Lithologic subunits recognized at Site 1002 are here tied into this new stratigraphic framework, and temporal variations in major sediment components are reported. The biogenic carbonate, opal, and organic carbon contents of sediments in the Cariaco Basin tend to be high during interglacials, whereas the terrigenous contents of the sediments increase during glacials. Glacioeustatic variations in sea level are likely to exert a dominant control on these first-order variations in lithology, with glacial surface productivity and the nutrient content of waters in the Cariaco Basin affected by shoaling glacial sill depths, and glacial terrigenous inputs affected by narrowing of the inner shelf and increased proximity of direct riverine sources during sea-level lowstands.

Tie points and goechemical analysis from different Holes of ODP Site 165-1002

The fine-grained sediments of the Cariaco Basin, Venezuela, of the last 130 ky, whose deposition history is well characterized, were analyzed geochemically in order to test the validity of sediment bulk geochemistry as an indicator of detrital provenance. Several binary and ternary diagrams as well as the chemical index of alteration (CIA) were tested for their capacity to discriminate the poorly contrasted detrital sources to the Cariaco Basin, and to describe the temporal evolution of the contributions of these different sources. Most of the diagrams tested did not allow a good discrimination of sources or, when sources were well discriminated, did not allow an interpretation of the temporal variations consistent with the known history. A relatively good discrimination of sources and a consistent interpretation of temporal variations were however obtained using Hf vs. Th and La/Yb vs. Gd/Yb binary diagrams, as well as Ti-Zr-Th, Ti-Zr-La, and Lu-Hf-Th ternary diagrams. Compared to the previous studies of the detrital content of the Cariaco Basin sediments, the geochemical approach permitted the recognition of a sediment contribution eroded from the Unare platform and Gulf of Cariaco during rapid sea level oscillations, and the contribution of Saharan eolian particles during the Younger Dryas-Preboreal and MIS6-5 transition. The choice of plotted elements was determined after considering carrier minerals, so that different elements may be informative in different sedimentary contexts. Overall, mineral sorting during transport appears as a major limit to quantitative estimation of the different contributions. In particular mineral sorting leads to the selective enrichment of elements associated with clays (Al, Rb, Th and LREE) in sediments deposited in the basin. Unless the geochemical effect of mineral sorting can be measured, it appears that quantitative provenance analysis should be performed on fractions of similar grain size instead of bulk sediment.