Carte de la coste d'Arabie, Mer Rouge et Golfe de Perse: tirée de la Carte de l'Océan Oriental publiée en 1740 par Ordre de Mgr le Comte de Maurepas augmentée sur des remarques particulières et dressée sur des observations astronomiques = Kaart van de Kust van Arabië, de Roode-Zee en de Gulf van Persië Gemaakt na de Fransse-Kaart van den Ooster-Ocean uitgegeven A. 1740 op Bevel van den Hre Grave de Maurepas Vermeederd op byzondere Aanmerkingen, en geschikt volgens Sterrekundige-Waarnemingen

J. V. Schley.

La Région Méditerranéenne en 2020 et son Rôle dans le Réseau Energétique Européen, Vol. II: La production et les eschanges de petrole, de gaz naturel et d'electricite: Situation actuelle et perspectives dans les PSEM et les pays du golfe. May 1994 = The Mediterranean region in 2020 and its Role in European Energy Network, Vol. II: Production and eschanges of oil, natural gas and electricity: Current situation and prospects in MENA countries and the countries of the Gulf. May 1994

None.

Annexe II: Analyse de la situation politique en Mediterranee et dans les pays du golfe el les risques sur les approvisionnements petroliers et gaziers 1) Algerie & Pays D'Afrique du Nord 2) Pays de L'Est Mediterraneen et du Golfe. OME, Draft du 18 April 1995 = Annex II: Analysis of the political situation in the Mediterranean and the Gulf countries and risks on petroleum and gas supplies 1) Pays D'Algerie & North Africa 2) Country of Eastern Mediterraneen and the Gulf. OME, Draft of 18 April 1995

None.

(Tab. XIII.1) TOC content, carbonate content, carbonate mineralogy, percentage of total carbonate, aragonite, low magnesium calcium, and high magnesium calcium, and grain-size contents from samples from the Golfe d'Arguin and from the Western Sahara

Modern carbonate sedimentation takes place on the northern Mauritanian shelf (20°N), where typical tropical components (e.g. hermatypic reefs, calcareous green algae) are absent. Such deposits are reminiscent of extratropical sediment in the geological record. The tropical open shelf of Mauritania is influenced by large siliciclastic dust input and upwelling, highly fertilizing the ocean, as well as strongly limiting the light penetration. In this context, temperature does not appear to be the steering factor of carbonate production. This thesis describes the depositional system of the Golfe d'Arguin off Mauritania and focuses on environmental conditions that control the depositional pattern, in particular carbonate production. The description of this modern analogue provides a tool for paleoenvironmental interpretation of ancient counterparts. The Golfe d'Arguin is a broad shallow shelf comprising extensive shoals (<10 m water depth; i.e. the Banc d'Arguin) on the inner shelf where waters warm up. The sediments collected in water depths between 4 and 600 m are characterized by mixed carbonate and siliciclastic (dust) deposits. They vary from clean coarse-grained, almost pure carbonate loose sediments to siliciclastic-dominated fine-grained sediments. The carbonate content and sediment grain size show a north-south decreasing pattern through the Golfe d'Arguin and are controlled by the hydraulic regime influenced by wind-driven surface currents, swell, and tidal currents. The carbonate grain association is heterozoan. Components include abundant molluscs, foraminifers, and worm tubes, as well as barnacles and echinoderms, elements that are also abundant in extratropical sediments. The spatial distribution of the sedimentary facies of the Golfe d'Arguin does not display a depth zonation but rather a mosaic (i.e. patchy distribution). The depth and climatic signatures of the different sedimentary facies are determined by taxonomic and ecological investigations of the carbonate-secreting biota (molluscs and foraminifers). While certain planktonic foraminifers and molluscs represent upwelling elements, other components (e.g. mollusc and benthic foraminifer taxa) demonstrate the tropical origin of the sediment. The nutrient-rich (and thus also low light-penetration) conditions are reflected in the fact that symbiotic and photosynthetic carbonate-producing organisms (e.g. hermatypic corals) are absent. The Mauritanian deposits represent an environment that is rare in the modern world but might have been more common in the geological past when global temperatures were higher. Taxonomic and ecological studies allow for distinguishing carbonate sediments formed under either tropical high-nutrient or extratropical conditions, thus improving paleoclimate reconstruction.

(Table 1) Quantitative analysis of mollusk taxa from surface sediment samples in the Golfe d'Arguin

Ecological and taxonomic study of the mollusk-rich fauna of the Golfe d'Arguin, North Mauritania, investigates the various environmental influences affecting this tropical shelf. The upwelling of nutrient-rich waters leads to a highly productive environment under tropical conditions. The resulting mixed carbonate-siliciclastic sediment contains a large portion of calcareous components produced by heterotrophic organisms-e.g., mollusks, foraminifers, worms, barnacles-that are reworked on the open shelf. On the basis of mollusk assemblages, six taphocoenoses are defined, all being characterized by a mixed fauna of tropical (e.g., Tellina densestriata), subtropical (e.g., Macoma cumana) and temperate (e.g., Spisula subtruncata) species. Differences between the assemblages are related to the medium-grain size ranging from mud to gravel-that results from local hydrodynamic conditions and water depth. Among carbonate grains, Donax burnupi shells are very abundant in the swell-exposed, northern part of the Golfe d'Arguin and reflect the tropical to subtropical, high-energy, and high-nutrient waters. Mollusk assemblages are demonstrated to be a sensitive tool for deciphering complex environmental conditions in sedimentary archives.

Le golfe de Naples et ses volcans et les volcans en général /

Includes bibliographical references.

Voyage dans l'Inde et dans le Golfe Persique, par l'Egypte et la Mer Rouge /

Mode of access: Internet.

Promenade sur les côtes du golfe de Gascogne, ou Aperçu topographique, physique et médical des côtes occidentales de ce même golfe.

Mode of access: Internet.

Voyage de la côte de Malabar à Constantinople, par le Golfe Persique, l'Arabie, la Mésopotamie, le Kourdistan et la Turquie d'Asie : fait en 1817 /

Mode of access: Internet.