Historical variability of subfossil chironomids (Diptera: Chironomidae) in three lakes impacted by natural and anthropogenic disturbances     

Vicky Tremblay  Isabelle Larocque-Tobler  Pascal Sirois 《Journal of Paleolimnology》2010,44(2):483-495

In the eastern boreal forest of Quebec, Canada, harvesting strategies try to mimic the effects of fire on forest ecosystems, assuming that both disturbances have similar impacts. However impacts of both types of perturbations on lacustrine ecosystems, especially on chironomids (non-biting midges), are still poorly understood. The objectives of this study were to determine if logging and fire resulted in chironomid assemblages significantly different than pre-disturbance states and to see if the harvesting strategy (careful logging around advanced growth (CLAAG) and buffer zones) protect lakes from logging effects in the boreal forest. Three statistical tests were used to study the difference between pre- and post-disturbance assemblages: a principal component analysis (PCA), analysis of similarity (ANOSIM) and a non-metric multi-dimensional scaling (MDS) ordination. All statistical analyses suggested that fire did not have any effects on chironomid assemblages. The PCA analysis showed that two logging events in Lac aux Huards created chironomid assemblages slightly outside the pre-disturbance variability. However, ANOSIM showed that these differences were not significant at the 0.5% level of significance. These results suggest that the presence of a buffer zone probably limited the impacts of logging on lakes in this area.  相似文献   

Albeluvisol development with time in loamy marine sediments of southern Norway     

Daniela Sauer  Isabelle Schülli-Maurer  Ragnhild Sperstad  Rolf Srensen  Karl Stahr 《Quaternary International》2009,209(1-2):31

This paper reports a study on soil development in loamy marine sediments on both sides of the Oslofjord (Vestfold, Østfold). This region has been subject to steady glacio-isostatic uplift during the whole Holocene. Hence, land surface age continuously increases from the coast inland. Several sea level curves, based on radiocarbon datings, enable estimation of land surface age for all locations. Clay illuviation starts in less than 1650 years. E horizons become lighter with age, but their lower boundary stays around 40 cm for more than 10 000 years. Albeluvic tongues develop between 4600 and 6200 years. Initially, they form along intersections of cracks. As preferential flow and leaching along the cracks continues, the tongues increase in length and width, progressively consuming the prisms between the cracks in the upper Bt horizon. The Fe_d/Fe_t ratios (weighted means of the upper meter) show a clear linear increase with soil age and may be used for “pedo-dating”, i.e. for estimating the ages of non-dated land surfaces covered with similar sediments. In contrast, the logarithmic decrease of base saturation and pH, with rapid changes in the first time but only very slight changes between 2000 and 10 000 years, makes these parameters unsuitable for “pedo-dating”.  相似文献   

Tidal sediment transport versus freshwater flood events in the Konkouré Estuary, Republic of Guinea     

Sylvain Capo  Isabelle Brenon  Aldo Sottolichio  Patrice Castaing  Patrick Le Goulven 《Journal of African Earth Sciences》2009,55(1-2):52

In comparison to their temperate counterparts, sediment processes in tropical estuaries are poorly known and especially in African ones. The hydrodynamics of such environments is controlled by a combination of multiple processes including morphology, salinity, mangrove vegetation, tidal processes, river discharge, settling and erosion of mud and by physico-chemical processes as well as sediment dynamics.The aim of this study is to understand the sediment processes in this transitional stage of the estuary when the balance between river discharges and marine processes is reversing. Studying the hydrodynamics and sediment dynamics of the Konkouré Estuary has recently been made possible thanks to new data on bathymetry, sedimentary cover, salinity, water elevations, and current velocities. The Lower Konkouré is a shallow, funnel shaped, mesotidal mangrove-fringed, tide-dominated estuary, well mixed during low river discharge and stratified during high river discharge. The Konkouré Estuary is turbid despite the small amount of terrestrial input and its residual velocity at the mouth during low river discharges, landwards for two of the three branches, suggests a landward migration by tidal pumping of the suspended particulate matter. A Turbidity Maximum Zone (TMZ) is identified for typical states of the estuary with regard to fluvial and tidal components. Suspended sediment transport during a transitional stage between the rainy and dry seasons is known thanks to current velocity and Suspended Sediment Concentration (SSC) measurements taken in November 2003. The Richardson layered number calculation assesses that turbulence is the major mixing process in the water column, at least during the flood and ebb stages, whereas stratification occurs during the slack water periods. Tidal currents generate bottom erosion, and turbulence mixes the suspended sediment throughout the water column. As a result, a net sediment input is calculated from the western Konkouré outlet for two consecutive tidal cycles. Despite the net water export, almost 300 tons per tide reach the estuary through this outlet, for a moderate river flow.  相似文献   

Effects of diuron in microcosms on natural riverine bacterial community composition: new insight into phylogenetic approaches using PCR-TTGE analysis   总被引：1，自引：0，他引：1  

Stéphane Pesce  Corinne Bardot  Anne-Catherine Lehours  Isabelle Batisson  Jacques Bohatier  Céline Fajon 《Aquatic Sciences - Research Across Boundaries》2008,70(4):410-418

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Report of the Treasurer     

Isabelle Cojan 《Sedimentology》1999,46(1):209-210

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RAPD-typing of Central and Eastern North Atlantic and Western North Pacific minke whales, Balaenoptera acutorostrata     

Martinez  I.; Pastene  L. A. 《ICES Journal of Marine Science》1999,56(5):640-651

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Predation on the southwestern Atlantic fiddler crab (Uca uruguayensis) by migratory shorebirds (pluvialis dominica, P. squatarola, arenaria interpres, and numenius phaeopus)     

Oscar O. Iribarne  Mariano M. Martinez 《Estuaries and Coasts》1999,22(1):47-54

In Bahia Samborombon (SW Atlantic; 35°30′–36°22′S; 56°45′–57°23′W) migratory American golden plover (Pluvialis dominica), black-billed plover (P. squatarola), ruddy turnstone (Arenaria interpres), and whimbrel (Numenius phaeopus) forage on fiddler crabs (Uca uruguayensis). These shorebirds have distinct patterns of feeding behavior and capture different proportions of each sex and size. P. dominica made short runs, capturing mostly juvenile crabs, which are eaten whole. P. squatarola use a similar feeding strategy but capture females primarily. A. interpres walks continuously, capturing almost exclusively large male crabs (71%). N. phaeopus walk in the Uca patch and probe burrows by inserting the bill; they primarily capture females. The feeding rate of A. interpres is higher than that of P. dominica, P. squatarola, and N. phaeopus. Handling time shown by P. dominica and A. interpres was greater than the other two species for all categories of crabs. In all cases, handling time of male crabs was greater than those of either females or juveniles. All the evidences suggest that U. uruguayensis is an important food source for all these species and should be accounted in any conservation endeavor. *** DIRECT SUPPORT *** A01BY085 00006  相似文献   

The interstellar extinction and distance modulus to M10 from infrared photometry     

S. Arribas  C. Martinez Roger  E. Paez  F. Caputo 《Astrophysics and Space Science》1990,169(1-2):45-47

From a new infrared photometry of the globular cluster M10 its interstellar extinction and distance modulus are discussed. This is done by comparison with the well-studied clusters M3, M13, and M92. Final values ofE(B-V)=0.17±0.05 and (M _v-V)=14.0±0.3 are proposed. The dependence on metallicity of these values is briefly discussed.Paper presented at the 11th European Regional Astronomical Meetings of the IAU on New Windows to the Universe, held 3–8 July, 1989, Tenerife, Canary Islands, Spain  相似文献   

Lower Paleozoic extensional tectonics in the limit between the West Asturian-Leonese and Central Iberian Zones of the Variscan Fold-Belt in NW Spain   总被引：1，自引：1，他引：0  

J. R. Martinez Catalan  M. P. Hacar Rodriguez  P. Villar Alonso  A. Perez-Estaun  F. Gonzalez Lodeiro 《International Journal of Earth Sciences》1992,81(2):545-560

The limit between the West Asturian-Leonese and Central-Iberian Zones in the NW of the Iberian Peninsula is described in the area of Caurel-Truchas (Provinces of Orense and León). From the distribution of the sedimentary formations and the Variscan structures it is inferred that the transition between the two zones was a fault system, which was active during, at least, the Ordovician and Lower Silurian. The faults were supposedly normal, though they had probably some strike-slip component, and gave rise to a half-graben in which a syn-rift sequence was deposited. The latter underwent inversion at the onset of the Variscan tectonism, producing a ramp anticline-syncline pair that forms the more important folds in the area. The varying geometry of these folds is interpreted partly as being due to the existence of previous en échelon folds related to the strike-slip component of the faults and, partly, as a result of the variable intensity of the shear strain undergone during the first variscan phase.

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Zusammenfassung Die Grenze zwischen der West-Asturischen-Leonesischen und Zentral-Iberischen Zone im NW der Iberischen Halbinsel wird aus dem Gebiet von Caurel-Truchas (Provinz Orense und León) beschrieben. Aufgrund der Verteilung der sedimentären Formationen, sowie der variszischen Strukturen wird abgeleitet, daß der Übergang zwischen den beiden Zonen durch ein Störungssystem bedingt wurde, das zumindest zwischen Ordovizium und Untersilur aktiv war. Dabei handelte es sich vermutlich um Abschiebungen mit einer Horizontalverschiebungskomponente. Diese Ausbildung führte zu einem Halbgraben mit darin abgelagerter sedimentärer Syn-Riftsequenz. Letztere wurde während der Anfangsphase der variszischen Tektonik invertiert, so daß es zu einem Rampen-Antiklinal-Synklinal Paar kam, welches die wichtigsten Falten der Gegend bildet. Die variable Geometrie der Falten wird zum einen der Existenz von frühen En-échelon Falten zugeschrieben, die durch die Horizontalverschiebungskomponente der Störungen hervorgerufen wurden; zum anderen sind sie das Resultat der veränderlichen Intensität der Scherspannung während der ersten variszischen Phase.

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Resumen Se describe el límite entre las Zonas Asturoccidental-Leonesa y Centroibérica en el NO de la Península Ibérica en el área del Caurel-Truchas (Provincias de Orense y León). Partiendo de la distribución de las formaciones sedimentarias y de la geometría de las estructuras varíscicas, se deduce que la transición entre las dos zonas fue un sistema de fallas, que fue activo al menos durante el Ordovício y el Silúrico Inferior. Se supone que la principal componente de las fallas fue normal, aunque debió de existir también una componente de desgarre, y su juego originó un semi-graben en el que se acumuló una secuencia sin-rift. Esta última experimentó una inversión al principio de la tectogénesis Varíscica, formándose un par de pliegues de rampa que son los pliegues más importantes del área. La geometría variable de esos pliegues se interpreta como debida, en parte, a la existencia previa de pliegues en escalón relacionados con la componente de desgarre de las fallas y, en parte, como consecuencia de la variable intensidad de la deformación por cizallamiento sufrida durante la primera fase de deformación varíscica.

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The oldest galactic open clusters: New CCD photometry and colour-magnitude diagrams     

E. Paez  C. Martinez Roger  S. Arribas  O. Straniero  F. Caputo  V. Castellani 《Astrophysics and Space Science》1990,169(1-2):41-44

We present CCD photometry for stars in three fields centered on the old open cluster NGC 188 and in four fields on the intermediate-age cluster NGC 7789, which has been performed with the aim of investigating the HR diagram distribution of the cluster's Main-Sequence (MS) stars. A sufficiently well-defined sequence of subgiant, turn-off (TO), and MS stars have been detected, extending the observed lower MS down to aboutV=20 mag.Paper presented at the 11th European Regional Astronomical Meetings of the IAU on New Windows to the Universe, held 3–8 July, 1989, Tenerife, Canary Islands, Spain.  相似文献