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134 documentos corresponden a la consulta.
Palabras contadas: america: 211, south: 315
de Romero, M.E.M. - Espinar, L.A.
Darwiniana 2010;48(2):208-209
2010

Descripción: Chenopodium stuckertii is identified as Holmbergia tweedii and lectotypified.
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Tipo de documento: info:ar-repo/semantics/artículo

Cornelius, C. - Cockle, K. - Politi, N. - Berkunsky, I. - Sandoval, L. - Ojeda, V. - Rivera, L. - Hunter Jr., M. - Martin, K.
Ornitol. Neotrop. 2008;19(SUPPL):253-268
2008

Tipo de documento: info:ar-repo/semantics/artículo

Pardiñas, U.F.J. - Ramírez-Llorens, P.
Mammalia 2005;69(1):103-107
2005

Descripción: Fil:Ramírez-Llorens, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
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Adamowicz, S.J. - Hebert, P.D.N. - Marinone, M.C.
Zool. J. Linn. Soc. 2004;140(2):171-205
2004

Descripción: Although the temperate regions of South America are known to have a diverse daphniid fauna, there has been no genetic evaluation of the existing taxonomic system or of the affinities between the North and South American faunas. The present study analyses mitochondrial DNA sequences and allozyme variation to investigate species diversity in 176 Daphnia populations from Argentina. This work established the presence of at least 15 species in Argentina, six of which are either undescribed or are currently misidentified and two of which represent range extensions of North American taxa. Eleven of the Argentine species appear endemic to South America, while the remaining four also occur in North America. In the latter cases, the close genetic similarity between populations from North and South America indicates the recent exchange of propagules between the continents. While biological interactions and habitat availability have undoubtedly contributed to the observed species distributions, chance dispersal has apparently played a dominant role in structuring large-scale biogeographical patterns in this genus and probably in other passively-dispersed organisms. © 2004 The Linnean Society of London.
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Teta, P. - Malzof, S. - Quintana, R. - Pereira, J.
Ornitol. Neotrop. 2006;17(3):441-444
2006

Descripción: Fil:Quintana, R. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
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Jahn, A.E. - Cueto, V.R. - Sagario, M.C. - Matnani, A.M. - Vidoz, J.Q. - De Casenave, J.L. - Di Giacomo, A.G.
Ornitol. Neotrop. 2009;20(2):275-283
2009

Temas:   Caparú -  Cerrado -  Chaco -  El bagual -  Monte -  Ñacuñán -  Philopatry

Descripción: Very little information currently exists on site fidelity patterns among Neotropical Austral migratory birds, which migrate wholly within South America. We banded migratory birds at three sites in South America, one located in the tropics and two at south temperate latitudes. We document breeding site fidelity among seven species and winter site fidelity among four species. Knowledge of patterns of site fidelity among migratory birds in South America is important for understanding the constraints affecting their populations throughout the annual cycle and ultimately for conservation planning. Accepted 8 April 2009. © The Neotropical Ornithological Society.
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Kay, R.F. - Madden, R.H. - Vucetich, M.G. - Carlini, A.A. - Mazzoni, M.M. - Re, G.H. - Heizler, M. - Sandeman, H.
Proc. Natl. Acad. Sci. U. S. A. 1999;96(23):13235-13240
1999

Descripción: Isotopic age determinations (40Ar/39Ar) and associated magnetic polarity stratigraphy for Casamayoran age fauna at Gran Barranca (Chubut, Argentina) indicate that the Barrancan 'subage' of the Casamayoran South American Land Mammal 'Age' is late Eocene, 18 to 20 million years younger than hitherto supposed. Correlations of the radioisotopically dated magnetic polarity stratigraphy at Gran Barranca with the Cenozoic geomagnetic polarity time scale indicate that Barrancan faunal levels at the Gran Barranca date to within the magnetochronologic interval from 35.34 to 36.62 megannums (Ma) or 35.69 to 37.60 Ma. This age revision constrains the timing of an adaptive shift in mammalian herbivores toward hypsodonty. Specifically, the appearance of large numbers of hypsodont taxa in South America occurred sometime between 36 and 32 Ma (late Eocene-early Oligocene), at approximately the same time that other biotic and geologic evidence has suggested the Southern high latitudes experienced climatic cooling associated with Antarctic glaciation.
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Confalonieri, V.A. - Sequeira, A.S. - Todaro, L. - Vilardi, J.C.
Heredity 1998;81(4):444-452
1998

Descripción: Trimerotropis pallidipennis is an American grasshopper whose South American populations are polymorphic for pericentric inversions. Colonization of southern latitudes was by North American grasshoppers with basic chromosome arrangements, presumably along the Andean dry lands of South America. In Argentina, the frequencies of some of the rearrangements are correlated with geographical and climatic variables, following similar patterns among different ecological gradients, and are probably maintained by geographically variable coefficients of selection. Restriction site variation of mitochondrial DNA is used as a tool for determining the species history in relation to the formation of clines. Populations located along an altitudinal gradient, and others outside the cline, are analysed through phylogeographical studies. There is no strong geographical orientation in the unrooted tree connecting all 17 mitochondrial DNA haplotypes found. Many of them are present in most of the populations analysed, indicating high gene flow. The fact that there is no obvious differentiation in haplotype distribution between both extremes of the cline nor between chromosomally differentiated populations shows that the cline is not the result of a hybrid zone and reinforces the selection hypothesis. The estimation of the overall nucleotide divergence between the hypothetical ancestral haplotype and the other molecules shows that T. pallidipennis haplotypes started diverging from each other about 3 Myr ago. This result is in agreement with the time when the Isthmus of Panama rose (2-3 Myr ago), probably favouring the migration of many species between both hemispheres.
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Peña, N.I. - Arambarri, A.M.
Darwiniana 1997;35:69-74
1997

Descripción: Five species of lignicolous marine fungi from the coast of Buenos Aires province (Argentina) are described. Haligena salina Farrant & Jones, Nautosphaeria cristaminuta Jones and Ocostaspora apilongissima Jones, Johnson & Moss, were collected from driftwood and intertidal wood. Cumulospora marina I. Schmidt and Helicascus kanaloanus Kohlmeyer were found growing on Spartina densiflora Brongn. N. cristaminuta is a new record for Argentina, while the remaining ones are new records for South America.
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Antico, P.L.
Int. J. Climatol. 2009;29(5):719-727
2009

Descripción: The classification of El Niño events was performed based on the time evolution of sea surface warming in the tropical Pacific Ocean during the period 1950-2000. Two sets of events were constructed: one in which the warming core migrates eastward along the tropical Pacific until April-June of the following year, and another one in which it evolves westward until November-January. The first type has associated positive precipitation anomalies over southeastern South America during April-June. It results from a favourable combination of cyclonic vorticity advection and humidity convergence. At high levels, cyclonic vorticity advection is explained in terms of an eastward extension of the subtropical jet. Enhanced humidity advection takes place by an increased low-level northwesterly flow to the east of the Andes. It provides enough moisture availability that, in combination with the upper-level cyclonic vorticity advection, supports heavy precipitation during April-June. The second type of event exhibits slight negative or near-normal precipitation anomalies over the same region. Both low and high-level circulation anomalies are also weaker in this case. The 1997-1998 El Niño is analysed separately because it cannot be classified into any of the previously described event types. The observed distribution of both types of events along the analysed period changes after the 1970s. Comparison with other authors' results suggests the influence of low-frequency processes such as the Pacific Decadal Oscillation (PDO). Copyright © 2008 Royal Meteorological Society.
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Nicolini, M. - Salio, P. - Katzfey, J.J. - McGregor, J.L. - Saulo, A.C.
J. Geophys. Res. D Atmos. 2002;107(22):12-1-12-13
2002

Descripción: [i] This work presents results, over the South American region, from the CSIRO Division of Atmospheric Research limited area model (DARLAM) and from the ninelevel general circulation model (GCM) of CSIRO (CSIRO Mk 2), within which it was nested in a one-way mode. Ten separate 30-day DARLAM simulations were performed for both January and July with a resolution of 125 km and were averaged to obtain a climatology for those months. This paper presents for the first time simulations of the January South American climate using a limited area model; previous similar studies simulated only the July climate. The goal of this study was to examine the capability of the CSIRO Mk 2 - DARLAM nested modeling system for simulating the climate in the South American region. Further, it was desired to investigate whether the higher resolution of DARLAM improves the simulated climate over various subregions, compared with the GCM and observations. With this purpose, a representative set of variables was analyzed and statistically compared. Overall, the fields simulated by the nesting system provide a better representation of the South American climate than the GCM. In particular, significant improvements are found in the nested model climatology for near-surface temperature and mean sea level pressure. Comparison of the January and July simulations shows a better wintertime performance. Some significant summertime features, like the Bolivian High, are reasonably well simulated by DARLAM, but not by the GCM. Copyright 2002 by the American Geophysical Union.
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Marengo, J.A. - Liebmann, B. - Grimm, A.M. - Misra, V. - Silva Dias, P.L. - Cavalcanti, I.F.A. - Carvalho, L.M.V. - Berbery, E.H. - Ambrizzi, T. - Vera, C.S. - Saulo, A.C. - Nogues-Paegle, J. - Zipser, E. - Seth, A. - Alves, L.M.
Int. J. Climatol. 2012;32(1):1-21
2012

Descripción: This paper reviews recent progress made in our understanding of the functioning and variability of the South American Monsoon System (SAMS) on time scales varying from synoptic to long-term variability and climate change. The SAMS contains one of the most prominent summertime climate patterns in South America, featuring a strong seasonal variability in a region lying between the Amazon and the La Plata Basin. Much of the recent progress is derived from complementary international programs, such as the Monsoon Experiment South America (MESA), as well as from ongoing international programs such as the Large Scale Biosphere Atmosphere Experiment in the Amazon Basin (LBA) and the La Plata Basin (LPB) Regional Hydroclimate Project, which includes the CLARIS LPB Europe-South America Network for Climate Change Assessment and Impact Studies in La Plata Basin Project. The latter assesses atmosphere-land surface interactions, the role of land use changes and aerosols from biomass burning considered as sources of variability and change in the SAMS functioning, characteristics and behaviour. The SAMS region is particularly susceptible to variations of climate due to the importance of hydroelectricity generation and the agricultural base of local economies. Also addressed in this report are projections of climate change and extremes, which are important for impact and vulnerability assessments. This discussion includes the need to identify and understand important processes that control the monsoonal climate, how these processes may vary and change, and how they may interact with key societal sectors, including water resource management, hydroelectric generation, agriculture, and agribusiness. This paper reports on the major contributions of MESA to the knowledge of characteristics, functioning and variability of the SAMS, and is based on recent studies and publications, and can be considered as an update of a previous review by C. S. Vera et al. (2006a). © 2010 Royal Meteorological Society.
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Vadell, E.M. - Cavender, J.C.
Mycologia 2007;99(1):112-124
2007

Descripción: Thirteen new species and varieties of dictyostelid cellular slime molds (csm) were isolated from soils of the Atlantic Subtropical Rain Forest at the Iguazu' Falls, Northeastern Misiones Province, Argentina. Seven new species are described herein, one of them is a Polysphondylium, while the rest of the species belong to the genus Dictyostelium. Also, six taxa are new varieties of Dictyostelium and Acytostelium, which will be reported later. Fourteen Northern Hemisphere (Tikal) species have also been isolated from Iguazu' soils, some of them new records for Southern South America. This csm community, when compared with others from forests of the Northern Hemisphere, particularly Tikal, Guatemala, give some insight into a possibly different evolutionary history and/or natural selection in the two areas. © 2007 by The Mycological Society of America.
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Hladki, A.I. - Romero, A.I.
Mycologia 2009;101(5):733-744
2009

Descripción: The holotypes and isotypes of 20 Hypoxylon taxa described by Spegazzini have been examined and their taxonomic positions and nomenclatural problems are discussed. Two new combinations, Annulohypoxylon apiahynum comb. nov. and A. subeffusum comb. nov., are proposed. H. goliath is considered a synonym of Rosellinia bunodes. H. albostigmatosum and H. guarapiense are synonyms of H. anthochroum, H. anthracoderma of H. monticulosum, H. mbaiense of H. notatum, H. paulistanum of H. diatrypeoides, H. plumbeum and H. rubiginosum var. microcarpum of H. perforatum. H. porteri and H. intermedium belong in Biscogniauxia capnodes, H. puiggarii in Annulophypoxylon subeffusum, H. subvinosum. in H. lenormandii, H. turbinatum var. guaraniticum in Phylacia turbinata and H. valsarioides in Creosphaeria sassafras. H. leptascum is transferred to A. leptascum, H. circostomum to Nemania circostoma and H. latissimum to N. latissima. The holotype of H. albostigmatosum has been recovered, thus the lectotypification by Shear no longer is needed. H. subnigricans and H. umbilicatum are confirmed as good taxa. H. anthochroum and H. lenormandii are reported as first records from Argentina (Tucumán). © 2009 by The Mycological Society of America, Lawrence, KS 66044-8897.
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Hierro, R. - Llamedo, P. - De La Torre, A. - Alexander, P. - Rolla, A.
J. Geophys. Res. D Atmos. 2012;117(3)
2012

Descripción: Meteorological phenomena are closely linked to the presence of water vapor. They mainly originate and develop in the troposphere, where almost all the atmospheric water is concentrated. The Global Positioning System radio occultation (GPS RO) technique provides vertical profiles of refractivity from which other properties such as temperature and water vapor can be derived. The GPS RO capability to reproduce global, synoptic, and regional climatological patterns over South America, which is a mostly oceanic continent, is tested. From FORMOSAT-3/COSMIC mission data (2006-2010), our previous knowledge regarding global and synoptic/regional patterns of temperature, equivalent potential temperature, specific humidity, and pressure is verified. Special cases such as baroclinic disturbances arriving at South American midlatitudes and storm events over a mountain region near the Andes are analyzed. The temporal evolution and the latitude-longitude distribution in several layers of the variables listed above are well described with this technique. Copyright 2012 by the American Geophysical Union.
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Eherenhaus, C. - Vigna, M.S.
Darwiniana 2008;46(1):46-50
2008

Descripción: A Microcystis aeruginosa bloom occurred in the Planetario Lake (Parque Tres de Febrero, Ciudad Autónoma de Buenos Aires, Argentina) that led to the restoration of the lake. Before and after the restoration (since October 1999 to September 2000), samples were collected to assess changes in the phytoplankton structure. The genus Interfilum (Chlorococcales, Chlorophyta) was recorded in the samples for February and May 2000 for the first time in America. Furthermore, it is a new variety for science: I. paradoxum var regulare var. nov.
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Segura, D.F. - Utgés, M.E. - Liendo, M.C. - Rodríguez, M.F. - Devescovi, F. - Vera, M.T. - Teal, P.E.A. - Cladera, J.L.
J. Appl. Entomol. 2013;137(SUPPL1):19-29
2013

Descripción: Fil:Segura, D.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
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Ottone, E.G.
Rev. Asoc. Geol. Argent. 2011;68(3):370-379
2011

Descripción: Plant fossil findings published in the nineteenth century by page, Grondona, Villegas, rhode, bove, Ave ́-lallemant, bodenbender and roth, references by Ameghino, Valentin, rickard, brackebusch, sarmiento and latzina, and these published in catalogues and memoirs of local and international exhibitions, together with plant fossil findings by Canard, Claraz, Hatcher, olascoaga and pietrobelli, that remained unpublished up to the twentieth century, are commented.
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Tomezzoli, R.N. - Japas, M.S.
Rev. Asoc. Geol. Argent. 2006;61(3):370-382
2006

Descripción: During the Early Permian an extensive deformation belt well-known as Gondwánides developed in the southwest Gondwana margin. A foreland basin has been settled during the Late Carboniferous - Early Permian in the western end of this strip, and is represented by the El Imperial Formation, which crops out in the San Rafael Block. The upper section of this unit records an inversion of the ancient slopes, which has been interpreted as the first evidence of the migration of the orogenic front towards the foreland. Therefore, a paleomagnetic study has been carried out on this unit, searching for elements that allow to constraint the deformation age to evaluate the possible diachronism of it. First paleomagnetic results obtained in EI Imperial Formation, from the lower member in the Represa Agua del Toro and from the upper member in the Puesto La Josefa, are presented and discussed. These rocks have reverse magnetizations carried by hematite, of possible Permian age. Pole positions are discordant with the apparent polar wander path from South America. These differences could be explained because: secular variation was not properly averaged; rotations about vertical axes of the sampling localities; or the combination of these factors. © 2006 Asociación Geológica Argentina.
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