Academic literature on the topic 'Morbihan Gulf of'

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Journal articles on the topic "Morbihan Gulf of"

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Boujot, Christine, and Serge Cassen. "A pattern of evolution for the Neolithic funerary structures of the west of France." Antiquity 67, no. 256 (September 1993): 477–91. http://dx.doi.org/10.1017/s0003598x00045701.

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The astonishing architectural density and diversity of megalithic monuments along the coastline of the bay of Quiberon and in the gulf of Morbihan have permitted French and foreign archaeologists to establish continually improved classifications. The paper, based on the Morbihan Neolithic data, presents a coherent and dynamic evolutionary sequence of funerary structures from between 5000 and 3000 BC.
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Buffrénil, Vivian De, Albin Dziedzic, and Daniel Robineau. "Répartition et déplacements des Dauphins de Commerson (Cephalorhynchus commersonii (Lacépède, 1804)) dans un golfe des îles Kerguelen; données du marquage individuel." Canadian Journal of Zoology 67, no. 2 (February 1, 1989): 516–21. http://dx.doi.org/10.1139/z89-075.

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Sixteen Commerson's dolphins were tagged in the Gulf of Morbihan, southeast of the Kerguelen Islands, to specify how they use the available space and to determine the structure of their schools. The dolphins use only a small part (about 5%) of the whole area of the gulf, which is located along the northern coast. Their movements are restricted (less than 10 km in the average); they occur mainly along an east–west axis and, more rarely, along a north–south axis. The schools do not seem to have a definite structure. Seasonal migrations towards the gulf (summer) and out of the gulf (winter) are confirmed. Individuals may return to the gulf from one year to another.
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Henkel, Daniela, and Dorte Janussen. "Redescription and new records ofCeltodoryx ciocalyptoides(Demospongiae: Poecilosclerida)—a sponge invader in the north east Atlantic Ocean of Asian origin?" Journal of the Marine Biological Association of the United Kingdom 91, no. 2 (February 7, 2011): 347–55. http://dx.doi.org/10.1017/s0025315410001487.

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In 1996 a sponge was found in a well studied area in the Ria of Etel, Brittany, France, that had never been recorded there before. This sponge was later described as a new species and genus,Celtodoryx girardaeby Perezet al.(2006), who concluded that it is probably an invasive species. Over several yearsC. girardaewas found to occur successively in the Gulf of Morbihan, France, and Oosterschelde estuary, Netherlands. This sponge is characterized by an extensive spatial broading and therewith it rates today among the dominant benthic megafauna in the shallow waters of the Gulf of Morbihan and Dutch inshore waters. During our recent survey of the Chinese Yellow Sea sponge fauna, we found an abundant species with close morphological similarities toC. girardae. Further taxonomic studies have revealed that both the Chinese and European sponges are in fact conspecific withCornulum ciocalyptoidesdescribed by Burton (1935) from Posiet Bay, Sea of Japan and later recorded from other localities of the North West Pacific (e.g. Koltun, 1971; Sim & Byeon, 1989). In this paper we transfer the species of Burton fromCornulumtoCeltodoryxand consequently it becomes the senior synonym ofC. girardae. Furthermore, we conclude thatCeltodoryx ciocalyptoideswas introduced to the North East Atlantic from the North West Pacific with aquaculture of the Pacific oysterCrassostrea gigasas the probable vector. This is probably the first case recorded so far of a sponge species being transferred from one ocean to another by human activity.
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Ong, M. C., D. Menier, N. A. M. Shazili, and V. Dupont. "Geochemistry of Metallic Trace Elements in Surficial Sediments of the Gulf of Morbihan, Brittany, France." Journal of Applied Sciences 12, no. 21 (October 15, 2012): 2215–24. http://dx.doi.org/10.3923/jas.2012.2215.2224.

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Laruelle, F., J. Guillou, and Y. M. Paulet. "Reproductive pattern of the clams, Ruditapes decussatus and R. philippinarum on intertidal flats in Brittany." Journal of the Marine Biological Association of the United Kingdom 74, no. 2 (May 1994): 351–66. http://dx.doi.org/10.1017/s0025315400039382.

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Since the introduction of the Manila clam Ruditapes philippinarum (Mollusca: Bivalvia) to aquaculture clam beds, this species has spread to several sites. As a result, an extensive fishery has developed around this species. Its reproductive cycle and that of a native clam species, Ruditapes decussatus (Mollusca: Bivalvia) from two Brittany sites are examined here and the seasonal variations in the condition index, the scale of maturation stages, the histology and the oocyte size-frequencies of both species are compared. The differences observed between the species and between sites were attributed to environmental conditions. Ruditapes philippinarum showed a more extended breeding period and a greater number of spawning events than R. decussatus. In the Morbihan Gulf, the reproductive activity of R. philippinarum appeared particularly great in terms of number of spawning events, and speed of maturation. For both species, synchronism was more apparent during the first maturation, while spawning, and particularly partial spawning, tended to decrease the level of synchronization.
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Le Grand, A., V. Maxime, M. Kedzierski, H. Duval, P. Douzenel, O. Sire, and V. Le Tilly. "Assessment and monitoring of water quality of the gulf of Morbihan, a littoral ecosystem under high anthropic pressure." Marine Pollution Bulletin 124, no. 1 (November 2017): 74–81. http://dx.doi.org/10.1016/j.marpolbul.2017.07.003.

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Diz, P., F. J. Jorissen, G. J. Reichart, C. Poulain, F. Dehairs, E. Leorri, and Y. M. Paulet. "Interpretation of benthic foraminiferal stable isotopes in subtidal estuarine environments." Biogeosciences Discussions 6, no. 4 (July 24, 2009): 7453–80. http://dx.doi.org/10.5194/bgd-6-7453-2009.

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Abstract. Here we present a novel approach for the interpretation of stable isotope signatures recorded in benthic foraminifera from subtidal estuarine environments. The stable isotopic composition (δ18O and δ13C) of living Ammonia tepida and Haynesina germanica is examined in four stations in the Auray River estuary (Gulf of Morbihan, France) sampled in two contrasting seasons, spring 2006 and winter 2007. Comparing benthic foraminiferal δ18O measurements with theoretical oxygen isotopic equilibrium values, calculated on the basis of water temperature and salinity measurements in the upper and lower estuary, i.e., T−S−δ18Oeq. diagrams, strongly suggests that foraminiferal faunas sampled at the four stations calcified during different periods of the year. This interpretation can be refined by using the benthic foraminiferal δ13C which is mainly determined by the mixing of sea and river water. In the upper estuary foraminifera mainly calcified in early spring and winter, whereas in the lower estuary calcification took mainly place in spring, summer and autumn. This new method provides insight into the complexity of estuarine benthic foraminiferal stable isotope records. In addition, it can also be used to obtain new information on preferred calcification periods of benthic foraminiferal taxa in different parts of the estuary.
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Diz, P., F. J. Jorissen, G. J. Reichart, C. Poulain, F. Dehairs, E. Leorri, and Y. M. Paulet. "Interpretation of benthic foraminiferal stable isotopes in subtidal estuarine environments." Biogeosciences 6, no. 11 (November 13, 2009): 2549–60. http://dx.doi.org/10.5194/bg-6-2549-2009.

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Abstract. Here we present a novel approach for the interpretation of stable isotope signatures recorded in benthic foraminifera from subtidal estuarine environments. The stable isotopic composition (δ18O and δ13C) of living Ammonia tepida and Haynesina germanica is examined at four stations in the Auray River estuary (Gulf of Morbihan, France) sampled in two contrasting seasons, spring 2006 and winter 2007. Comparing benthic foraminiferal δ18O measurements with theoretical oxygen isotopic equilibrium values, calculated on the basis of water temperature and salinity measurements in the upper and lower estuary, i.e., T-S-δ18Oeq. diagrams, strongly suggests that foraminiferal faunas sampled at the four stations calcified during different periods of the year. This interpretation can be refined by using the benthic foraminiferal δ13C, which is mainly determined by the mixing of sea and river water. In the upper estuary foraminifera mainly calcified in early spring and winter, whereas in the lower estuary calcification mainly took place in spring, summer and autumn. This new method provides insight into the complexity of estuarine benthic foraminiferal stable isotope records. In addition, it can also be used to obtain new information on preferred calcification periods of benthic foraminiferal taxa in different parts of the estuary.
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Perez-Belmonte, Lucia, and Evelyne Goubert. "Surface distribution of foraminifera from the Morbihan's Gulf, France: study for paleoenvironmental reconstructions." Anuário do Instituto de Geociências 29, no. 1 (January 1, 2006): 559–60. http://dx.doi.org/10.11137/2006_1_559-560.

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Hardouin, Kevin, Romain Bouyer, Hugo Pliego-Cortés, Timothée Le Men, Stéphane Cérantola, Christel Marty, Philippe Douzenel, Gilles Bedoux, and Nathalie Bourgougnon. "Chemical characterization of the introduced red alga Polyopes lancifolius (Halymeniales, Rhodophyta) from the Gulf of Morbihan, France." Phycologia, September 18, 2022, 1–12. http://dx.doi.org/10.1080/00318884.2022.2117942.

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Books on the topic "Morbihan Gulf of"

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Oyster river: One summer on an inland sea. Wimborne: Dovecote, 2003.

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2

Perraudin, Paul. Mémoire du golfe. Paris: Editions de la Mer, 1985.

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Book chapters on the topic "Morbihan Gulf of"

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Vejby, Mara. "Enduring Past: Megalithic Tombs of Brittany and the Roman Occupation in Western France." In The Lives of Prehistoric Monuments in Iron Age, Roman, and Medieval Europe. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780198724605.003.0016.

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The extended lives of prehistoric monuments, whether or not they were interacted with once their initial phase of use had ended and how they were treated, can reveal valuable details about a culture. To interact with a place means that the action or influence is reciprocal. The individual, or group of individuals, is somehow affected by the physical contact they’ve had with the site, and the place in turn has been altered. Interactions are more than just reuse of a space. In fact, missing pieces of monuments’ biographies, evidence of subsequent use and treatment, are details that may tell us how a people dealt with their own past as well as that of others. The focus of this study is a region in which the biographies of a group of monuments appear to be intimately tied to clashing cultures during the Roman occupation: Morbihan, Brittany. Brittany is the westernmost province of France, roughly 30 kilometres north-west of the mouth of the Loire river, and extending over 200 kilometres westward into the Celtic Sea. The south-easternmost department of this province is Morbihan, which makes up over 6,800 square kilometres and centres on the Gulf of Morbihan, a few kilometres south of Vannes (Darioritum), the Roman-period civitas-capital of the Veneti. Darioritum was not only a port for commercial ships, but was also on the major road network connecting the Coriosolitae (Corseul), Osismes (Carhaix-Plouguer) and Namnetes (Nantes) civitates (Galliou and Jones 1991, 77, 81, 84). Evidence found in a thorough survey of Iron Age and Roman materials at megalithic tombs in Atlantic Europe revealed that Brittany is by far the region with the highest concentration of direct Roman period interactions, despite both the distribution of megalithic tombs across the peninsula and subsequent habitation patterns during the Iron Age and Roman periods (Scarre 2011, 29–33; Vejby 2012) . It also revealed that this activity is a major shift from the comparatively low number of megalithic tombs at which Iron Age materials have been found.
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Pian, Soazig, and David Menier. "Spatial and Statistical Analyses of Clifftop Retreat in the Gulf of Morbihan and Quiberon Peninsula, France: Implications on Cliff Evolution and Coastal Zone Management." In Coastal Zone Management, 131–53. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-12-814350-6.00006-9.

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