917 resultados para holocene beach sand


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Josephine and Albert Sloman are pictured in this undated black and white photograph. The beach location is unknown. This photo was among the Sloman - Bell family memorabilia in the possession of Rick Bell, grandson of Josephine and Albert. The family is descended from Black slaves who escaped from the United States and settled in southern Ontario.

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Board with six postcards of Crystal Beach. First postcard, Steamer "Americana" leaving foot of Main St. Second postcard, Divers at Crystal Beach, Canada. Third postcard, Cyclone Coaster, Crystal Beach, Ontario. Fourth postcard, Scenic Railway, Crystal Beach, Ont. Fifth postcard, Scene in the Park, Crystal Beach, Ont. Sixth postcard, Scene on the Midway, Crystal Beach, Canada.

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Sluice Pond is a small (18 ha) and deep (Zmax 20.0 m) partially meromictic, pond in Lynn, Massachusetts that contains a diverse dinocyst record since the early Holocene. High dinocyst concentrations, including morphotypes not previously described, as well as the preservation of several specimens of cellulosic thecae are attributed to low dissolved oxygen (DO) in the basin. The fossil protozoan record supports the interpretation- thecamoebians were unable to colonize the basin until the middle Holocene and only became abundant when the drought-induced lowstand oxygenated the bottom waters. Protozoans tolerant of low DO became abundant through the late Holocene as water levels rose and cultural eutrophication produced a sharp increase in biochemical oxygen demand (BOD) beginning in the 17th century. Recent sediments contain a dominance of Peridinium willei, indicating cultural eutrophication and the planktonic ciliate Codonella cratera and the thecamoebian Cucurbitella tricuspis in the deep basin. Above the chemocline however, a diverse difflugiid thecamoebian assemblage is present.

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Receipt from E.C. Staples, proprietor of Old Orchard House, Old Orchard Beach, Maine for bath house and laundry, Aug. 15, 1887.

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UANL

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UANL

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UANL

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Sauf par des regards fugitifs et distraits sur son travail d’illustrateur et son théâtre de marionnettes, l’histoire culturelle et littéraire n’a en général retenu de Maurice Sand que son état de fils bien-aimé de la plus célèbre écrivaine du 19e siècle. Étudiée pour elle-même, son œuvre multidisciplinaire - qui allie peinture, dessin, illustration, théâtre, histoire de l’art, sciences naturelles - se propose pourtant avec cohérence, marque d’une création soutenue plutôt que du dilettantisme où son souvenir s’est incrusté. Maurice Sand apparaît alors comme un de ces individus situés aux interstices des récits majeurs de la littérature et des arts qui, bien qu’ayant figure de minores, amènent à des réflexions nuancées sur la constitution de ces récits. Explorer son cas permet ainsi de scruter de plus près les mécanismes de la méconnaissance qui a pu et peut encore affecter un créateur et une œuvre soumis aux arbitrages mémoriels. Discrets angles morts de l’histoire, certains de ces mécanismes jalonnent clairement son parcours et les aléas de sa trace posthume. D’une part le vaste corpus des études sur George Sand, notamment des écrits biographiques et autobiographiques, fait voir à l’œuvre le mode déformant de la constitution de la mémoire d’un être saisi à partir des positions d’autrui : son existence devient cliché, elle se réduit peu à peu au rôle d’adjuvant dans des débats, passés ou actuels, qui font l’impasse sur le cours autonome de sa carrière, voire de sa vie. D’autre part la mise au jour de son œuvre, enfin vue comme un ensemble, dévoile une cause encore plus déterminante de sa méconnaissance. Presque tous les travaux de Maurice Sand sont traversés par une ligne de fantastique, au surplus connotée par son intérêt pour les sciences liées à la métamorphose, de l’ethnogénie à l’entomologie. Réinvention constante du passé, sa démarche cognitive et créatrice ignore les frontières disciplinaires, son objet est hybride et composé. L’œuvre se constitue ainsi par transversalité, trait et trame irrecevables en un siècle qui n’y perçut que dispersion, mais paradoxalement marque supérieure de qualité dans le champ éclaté où se déploient les arts de notre temps.

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The present study addresses to understand the sedimentological properties of the coasts of kodungallur and chellanam, central Kerala to bring out the relationship between the textural, mineralogical and geochemical characters with that of the respective environment. The grain size study of the beach ridge sediments from different pits has been investigated at close intervals, which enables to understand the grain size variations with depth. The sediment samples from various pits of the beach ridges indicate that the sediments range primarily from medium to very fine sand, well to moderately sorted, fine to coarse skewed and leptokurtic to platykurtic. The study area is considered as a prograding coast. Variations in grain size down the pit give three phases of beach building activities i.e.; a coarsening upward sequence in the bottom layers, a fining upward in the middle and coarsening upward in the top. Beach ridges are formed by swash built sediments with cross bedding and setting lag type sediments with seaward dipping/horizontal units. Geochemical signatures in the study area have been brought out through the analysis of major and trace elements. Iron is significantly enriched and its control over many trace elements is evident. Copper, chromium, cobalt, lithium, lead and zinc show decreasing trend with depth, while sodium, potassium,strontium,nickel and organic carbon increases. The association of many trace elements with organic carbon has also been established. Dissolution of trace elements in anoxic environment, at depth and reprecipitation in the oxic layers, at near or subsurface, are the major mechanism that brought out the variation of certain environmentally sensitive elements

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During an interstitial faunal survey along the south-west coast of Kerala, India, gastrotrich fauna were found in abundance. Together with species of the genera Xenotrichula, Halichaetonotus and Tetranchyroderma, were present several undescribed thaumastodermatid gastrotrichs belonging to the buccal palp bearing genus Pseudostomella. Adults of the new species are characterized by the following traits: total body length of about 300 μm; cuticular armature made up of medium sized pentancres covering the entire dorsolateral surface; pre-buccal, grasping palps bearing five, large papillae dorsally and 4-6 smaller papillae ventrally; adhesive apparatus made up of six anterior, 22-24 ventrolateral, two dorsolateral and six posterior adhesive tubes; caudal organ pear-shaped; frontal organ spherical. Pseudostomella cheraensis sp. nov. is the fourth taxon of the genus known from India; however, all the previous species reported hitherto from India have tetrancres instead of pentancres.

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The present investigations have considerably enhanced the existing knowledge on the biology and distribution/availability pattern of D.incarnatus in the Malippuram region. The species occurs in good concentration during October - March/April, and disappears from the area during late premonsoon and monsoon months. Recolonising the area in September, it grows fast in the subsequent months. The life span of the species is estimated to be about an year. Studies on the reproductive biology of the species have revealed that there are two spawning peaks, the major peak in February - March and minor peak, in December. The salinity regime of the area influences the reproductive activity. These observations form the original contribution in the thesis. The information on variation in water content, protein,glycogen and lipid levels in relation to reproductive cycle has helped to a better understanding of the gametogenic activity and spawning of the species. Similarly, the findings on salinity tolerance and filtration rate have shown that small sized clams exhibit greater tolerance range than larger clams, and grow at a faster rate with active metabolism. It is hoped that these information would considerably add to the present knowledge of the basic facts which are relevant to the improvement and management of the clam fishery of this region.