Anatomy of sand beach ridges : evidence from severe Tropical Cyclone Yasi and its predecessors, northeast Queensland, Australia

[1] Four well-identified tropical cyclones over the past century have been responsible for depositing distinct units of predominantly quartzose sand and gravel to form the most seaward beach ridge at several locations along the wet tropical coast of northeast Queensland, Australia. These units deposited by tropical cyclones display a key sedimentary signature characterized by a sharp basal erosional contact, a coarser grain size than the underlying facies and a coarse-skewed trend toward the base. Coarse-skewed distributions with minimal change in mean grain size also characterize the upper levels of the high-energy deposited units at locations within the zone of maximum onshore winds during the tropical cyclone. These same coarse skew distributions are not apparent in sediments deposited at locations where predominantly offshore winds occurred during the cyclone, which in the case of northeast Australia is north of the eye-crossing location. These sedimentary signatures, along with the geochemical indicators and the degraded nature of the microfossil assemblages, have proven to be useful proxies to identify storm-deposited units within the study site and can also provide useful proxies in older beach ridges where advanced pedogenesis has obscured visual stratigraphic markers. As a consequence, more detailed long-term histories of storms and tropical cyclones can now be developed.

Abrasion of beach sand /

Mode of access: Internet.

Prograded Holocene beach-ridges with superimposed dunes in north-east Ireland: mechanisms and timescales of fine and coarse beach sediment decoupling and deposition

Two depositional models to account for Holocene gravel-dominated beach ridges covered by dunes, occurring on the northern coast of Ireland, are considered in the light of infrared-stimulated luminescence ages of sand units within beach ridges, and 14C ages from organic horizons in dunes. A new chronostratigraphy obtained from prograded beach ridges with covering dunes at Murlough, north-east Ireland, supports a model of mesoscale alternating sediment decoupling (ASD) on the upper beach, rather than macroscale sequential sediment sourcing to account for prograded beach ridges and covering dunes. The ASD model specifies storm or fair-weather sand beach ridges forming at high-tide positions (on an annual basis at minimum), which acted as deflationary sources for landward foredune development. Only a limited number of such late-Holocene beach ridges survive in the observed prograded series. Beach ridges only survive when capped by storm-generated gravel beaches that are deposited on a mesoscale time spacing of 50–130 years. The morphodynamic shift from a dissipative beach face for dune formation to a reflective beach face for gravel capping appears to be controlled by the beach sand volume falling to a level where reflective conditions can prevail. Sediment volume entering the beach is thought to have fluctuated as a function of a forced regression associated with the falling sea level from the mid-Holocene highstand (ca. 6000 cal. yr BP) identified in north-east Ireland. The prograded beach ridges dated at ca. 3000 to 2000 cal. yr BP indicate that the Holocene highstand’s regressive phase may have lasted longer than previously specified.

A lognormal size distribution model for estimating stability of beach fill material /

"November 1965."

Molluscan assemblages on an intertidal sandflat in Princess Royal Harbour, Westren Austrailia

The molluscan fauna of an intertidal sand beach in Princess Royal Harbour, W.A.. is divided into two associations. The upper association, located between +0.10 and +0.59 m relative to tidal datum, is characterized by Hydrococcus graniformis and Batillariella estuarina. The lower assemblage, between +0.09 and -0.29 m is dominated numerically by Zeacumantus diemenensis and Katelysia scalarina. The assemblages are equivalent to the midlittoral- and sublittoral-fringe groupings described on both sandy and rocky shores by other authors. There is no supralittoral-fringe component in the molluscan fauna ofprincess Royal Harbour. The break between the two assemblages occurs at + 0.1 m, just below the minimum tide level in the area. Possible reasons for the zonation patterns are discussed and compared with other studies of intertidal zonation on sandy shores.

Antimicrobial resistance of heterotrophic marine bacteria isolated from seawater and sands of recreational beaches with different organic pollution levels in southeastern Brazil: evidences of resistance dissemination

Antimicrobial resistance of marine heterotrophic bacteria to different antimicrobials agents were evaluated in seawater, dry and wet sands from three marine recreational beaches with different pollution levels. In all studied beaches, the greatest frequencies of resistance were found in relation to penicillin. on Gonzaguinha, the most polluted beach, 72.3% of all isolated strains showed simple resistance, whilst 8.33% had multiple resistance. The values found on Ilha Porchat beach, were 70.8% and 6.9% for simple and multiple resistances, respectively. on GuaraA(0), the less polluted beach, only 35.3% of isolated strains had simple resistance. Multiple resistance was not observed. While samples from Gonzaguinha and Ilha Porchat beach showed isolated strains resistant to seven and six different antimicrobial agents, respectively, samples from GuaraA(0) beach were resistant only to penicillin and erytromicin. The positive correlations obtained between the degree of seawater contamination and frequency and variability of bacterial resistance indicate that polluted marine recreational waters and sands are sources of resistant bacteria contributing thus, to the dissemination of bacterial resistance.

Antimicrobial resistance and species composition of Enterococcus spp. isolated from waters and sands of marine recreational beaches in Southeastern Brazil

Density, species composition and antimicrobial resistance in bacteria of the Enterococcus genus were evaluated in seawater and sands from 2 marine recreational beaches with different levels of pollution. The 2 beaches showed predominance of Enterococcus faecalis and Enterococcus faecium, in the water and the sand. Dry sand presented higher densities of Enterococcus sp. and higher frequency of resistant strains than wet sand and seawater. The beach with a higher degree of pollution presented higher percentages of resistant strains (66.7% and 61.5%, in sand and in water, respectively) and resistance to a larger number of antimicrobials compared with the less polluted beach, Ilha Porchat (35.7% and 31.25% of resistant strains in sand and water, respectively). in water samples, the highest frequencies of resistance were obtained against streptomycin (38.5%) and erythromycin (25%), whilst in sand, the highest frequencies were observed in relation to erythromycin and tetracycline (38.1% and 14.3%, respectively). These results show that water and sands from beaches with high indexes of faecal contamination of human origin may be potential sources of contamination by pathogens and contribute to the dissemination of bacterial resistance. (C) 2007 Elsevier Ltd. All rights reserved.

Efecto del ejercicio de tiro y arrastre sobre el eje renina-angiotensina-aldosterona y cociente testosterona/cortisol en caballos euhidratados y deshidratados

Introducción. El estado hídrico previo al inicio de un ejercicio (hiperhidratación-deshidratación o hipohidratación y euhidratación) modifica la respuesta neurohumoral. En personas, la deshidratación origina una liberación incrementada de las hormonas implicadas en el mantenimiento de la volemia y del estado hidroelectrolítico, tales como la renina (REN), angiotensina (ANG) y aldosterona (ALD). La testosterona (T) es una hormona anabólica, mientras que el cortisol (C) es una hormona de estrés, con funciones catabólicas. El cociente T/C es un reflejo de la intensidad anabólica/catabólica de un ejercicio y en atletas humanos, se ve afectada por el estado hídrico. Objetivos. 1) Describir las variaciones en las concentraciones de REN, ANG, ALD, T, C y ratio T/C en caballos durante un ejercicio de tiro y arrastre, en relación con otros marcadores de equilibrio hidroelectrolítico y en función de la carga arrastrada; 2) Analizar si la respuesta de estas hormonas al ejercicio difiere entre animales con deshidratación hipertónica y euhidratados; Hipótesis: 1) Que las concentraciones de REN, ANG, ALD, T, C serán más elevadas en los caballos deshidratados que en los euhidratados; 2) Que el ejercicio de tiro y arrastre, particularmente en los animales de mayor peso corporal, inducirá una mayor activación del eje REN, ANG, ALD y una liberación superior de T; 3) Que los animales deshidratados experimentarán un incremento más intenso de estas hormonas en respuesta al ejercicio. Material y métodos. Se han llevado a cabo dos estudios simultáneos. En el estudio I, se han analizado los siguientes parámetros: valor hematócrito (HTO), albúmina (ALB), sodio (Na), potasio (K), cloro (Cl), lactato (LA) y concentraciones séricas de REN, ANG y ALD y en el estudio II, se han determinado las concentraciones de ALB, T, C y ratio T/C. En el estudio I, se han incluido 64 caballos machos, enteros y castrados, divididos en dos grupos según su estado hídrico: grupo control o euhidratado (CTR, n=11) y grupo deshidratado (DH; n=53), con deshidratación hipertónica inducida por restricción de agua y comida. Además, según su peso corporal, los animales se han dividido en 3 categorías de peso: I (<350 kg; n=3 para grupo CTR; n=23 para DH), II (351-450 kg; n=3 para CTR; n=18 para DH) y III (>451 kg; n=5 para CTR; n=12 para DH). En el estudio II, se han incluido los mismos animales, con excepción de la categoría de peso III para el grupo CTR, que solo está constituida por 3 animales, en lugar de 5, al descartar a los machos castrados, debido a la medición de T. Todos los animales, realizaron un ejercicio consistente en recorrer una pista de arena de playa de 60 m de longitud, tirando de un carruaje, con 2, 2,25 y 2,5 veces su peso corporal para las tres categorías de peso. La pista de arena se dividió en cuatro áreas de 15 m, en cada una de las cuales, el animal hizo una parada obligatoria, de duración decidida por el acompañante, y que se incluyó como tiempo de carrera. Los animales eran eliminados si se superan los 5 min de duración. En los dos estudios, se tomaron muestras de sangre en los siguientes tiempos: en reposo, antes del ejercicio (R), dentro del primer minuto tras finalizar el ejercicio (E) y a los 5, 10, 15 y 30 minutos de una recuperación pasiva (5REC, 10REC, 15REC y 30REC). Resultados. Estudio I. La diferencia de peso de los caballos tuvo una influencia mínima en los valores basales y en la respuesta al ejercicio. En reposo, los caballos DH tuvieron valores superiores de HTO, ALB, LA, Na, K y ANG en comparación con los CTR. El ejercicio condicionó una elevación de HTO, ALB, LA y Na, tanto en los caballos CTR como en los DH. Se encontró un incremento de ANG en los caballos DH y de ALD en los caballos CTR. La elevación con el ejercicio experimentada por los parámetros analizados fue de magnitud similar en los grupos CTR y DH, con excepción del LA (incrementó más en DH) y ALD (aumentó más en CTR). Estudio II. El ejercicio dio lugar a un aumento de T en las categorías I y III de los grupos CTR y DH, así como un descenso en la categoría II del grupo CTR. El C mostró un aumento progresivo en las tres categorías y en los dos grupos de estado hídrico, con los valores máximos en el tiempo 30REC. El ratio T/C aumentó en la categoría III del grupo DH, descendió en la categoría II del grupo CTR y no varió en los otros casos. Los animales DH, independientemente de la categoría de peso, tuvieron valores superiores de T y C, en la mayoría de los tiempos de extracción de muestras. Sin embargo, si se consideran los cambios experimentados por estas hormonas durante el ejercicio o en la recuperación, en relación a los valores basales, el aumento del C fue más marcado en el grupo CTR que en el DH, para las tres categorías de peso. Las variaciones de la concentración de T fueron superiores en las categorías de peso I y III del grupo CTR que en el grupo DH. El ratio T/C fue estadísticamente igual entre caballos CTR y DH en las categorías I y III, mientras que en la categoría II, los caballos DH presentaron cocientes T/C mayores. Conclusiones. La deshidratación hipertónica altera la concentración de las hormonas implicadas en la regulación del equilibrio hidro-electrolítico, de la presión sanguínea y del metabolismo. Sin embargo, el estado hídrico previo al ejercicio tiene una acción mínima sobre la magnitud de estos cambios en respuesta a un ejercicio de tiro y arrastre de corta duración (inferior a 5 min). Relevancia. Se ha demostrado que la respuesta neurohumoral, determinada en base a las concentraciones circulantes de las hormonas REN, ANG, ALD, T y C, se ve afectada por el ejercicio cuando el animal empieza el mismo en estado de euhidratación o de deshidratación.

Antimicrobial resistance of heterotrophic marine bacteria isolated from seawater and sands of recreational beaches with different organic pollution levels in southeastern Brazil: evidences of resistance dissemination

Antimicrobial resistance of marine heterotrophic bacteria to different antimicrobials agents were evaluated in seawater, dry and wet sands from three marine recreational beaches with different pollution levels. In all studied beaches, the greatest frequencies of resistance were found in relation to penicillin. on Gonzaguinha, the most polluted beach, 72.3% of all isolated strains showed simple resistance, whilst 8.33% had multiple resistance. The values found on Ilha Porchat beach, were 70.8% and 6.9% for simple and multiple resistances, respectively. on GuaraA(0), the less polluted beach, only 35.3% of isolated strains had simple resistance. Multiple resistance was not observed. While samples from Gonzaguinha and Ilha Porchat beach showed isolated strains resistant to seven and six different antimicrobial agents, respectively, samples from GuaraA(0) beach were resistant only to penicillin and erytromicin. The positive correlations obtained between the degree of seawater contamination and frequency and variability of bacterial resistance indicate that polluted marine recreational waters and sands are sources of resistant bacteria contributing thus, to the dissemination of bacterial resistance.

Antimicrobial resistance and species composition of Enterococcus spp. isolated from waters and sands of marine recreational beaches in Southeastern Brazil

Density, species composition and antimicrobial resistance in bacteria of the Enterococcus genus were evaluated in seawater and sands from 2 marine recreational beaches with different levels of pollution. The 2 beaches showed predominance of Enterococcus faecalis and Enterococcus faecium, in the water and the sand. Dry sand presented higher densities of Enterococcus sp. and higher frequency of resistant strains than wet sand and seawater. The beach with a higher degree of pollution presented higher percentages of resistant strains (66.7% and 61.5%, in sand and in water, respectively) and resistance to a larger number of antimicrobials compared with the less polluted beach, Ilha Porchat (35.7% and 31.25% of resistant strains in sand and water, respectively). in water samples, the highest frequencies of resistance were obtained against streptomycin (38.5%) and erythromycin (25%), whilst in sand, the highest frequencies were observed in relation to erythromycin and tetracycline (38.1% and 14.3%, respectively). These results show that water and sands from beaches with high indexes of faecal contamination of human origin may be potential sources of contamination by pathogens and contribute to the dissemination of bacterial resistance. (C) 2007 Elsevier Ltd. All rights reserved.

Measurement of resistivity and dielectric constant of beach-sand minerals

Resistivity and dielectric constant are important parameters which influence the separation of particles in a drum-type electrostatic separator. The paper provides details of the measurement of the parameters and data on the magnitude of resistivity and dielectric constant of the minerals of beach sand.

Beach monitoring project Sand Key Phase II Beach nourishment program (North Redington Beach and Redington Shores) Post-Nourishment Report Part II Offshore Profiles and Wave Data

This study presents the third post-nourishment survey (January 1989) results for the Sand Key Phase II beach nourishment project carried out in June, 1988. The monitoring program to this beach nourishment project is a joint effort between the University of South Florida and University of Florida. The field surveys include a total of 26 profiles, encompassing approximately 3 miles of shoreline extending from DNR R-96 to R-1ll. The total calculated volume loss of sand in the nourished segment (from R-99G to R-107) between the July 88 and January 89 surveys is 51,113 cubic yards, which is a loss about 9.7 percent of 529,150 cubic yards actually placed in the nourishment project. The total loss of sand computed in the entire survey area is 26,796 cubic yards, which is only 5.1 percent of the sand placed in the nourishment project. It is stressed that a part of these net volume reductions is due to the background erosion and not due to spreading losses induced by the nourishment project. (PDF contains 168 pages.)

The effect of shore armoring on beach slope in mixed sand-and-gravel beaches

Senior thesis written for Oceanography 445