991 resultados para Chondrichthyes, Fossil


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En este artículo se dan a conocer las características de una nueva línea de investigación, abierta y desarrollada por el autor, que integra conocimientos provenientes de cuatro disciplinas académicas distintas: Paleontología, Lingüística, Literatura y Etnología. Asimismo se apuntan algunas posibilidades de aplicación educativa y/o de vinculación curricular.

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En aquest treball es recopilen i estudien, des d’una perspectiva etnopaleontològica, les aportacions i influencies exercides pels fòssils en relació al patrimoni onomàstic toponímic relacionat amb cavitats càrstiques de l’àmbit geogràfic de les Illes Balears. Generalment es tracta de microtopònims moderns o recents, en vies de popularització i/o tradicionalització (neotopònims), establerts pels científics que estudien les coves i/o esportistes del món de l’espeleologia (topocultismes). Es poden distingir entre espeleotopònims de primer ordre (quan es refereixen a cavitats completes) i de segon ordre (quan es refereixen a un sector d’una cavitat). També es realitza una primera aproximació als topònims referits a mines d’extracció de carbó fòssil (antracotopònims).

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We present a new bed of cold Malacological fauna of the Wrm in the Catalan littoral, one af its species is dated for the first time iii the hlediterranean (Sipho curtus). We point out the predorninance of Gasteropoda as regards Bivalves in comparison with the other cold beds known.

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Outcrops of old strata at the shelf edge resulting from erosive gravity-driven flows have been globally described on continental margins. The reexposure of old strata allows for the reintroduction of aged organic carbon (OC), sequestered in marine sediments for thousands of years, into the modern carbon cycle. This pool of reworked material represents an additional source of C-14-depleted organic carbon supplied to the ocean, in parallel with the weathering of fossil organic carbon delivered by rivers from land. To understand the dynamics and implications of this reexposure at the shelf edge, a biogeochemical study was carried out in the Gulf of Lions (Mediterranean Sea) where erosive processes, driven by shelf dense water cascading, are currently shaping the seafloor at the canyon heads. Mooring lines equipped with sediment traps and current meters were deployed during the cascading season in the southwestern canyon heads, whereas sediment cores were collected along the sediment dispersal system from the prodelta regions down to the canyon heads. Evidence from grain-size, X-radiographs and Pb-210 activity indicate the presence in the upper slope of a shelly-coarse surface stratum overlying a consolidated deposit. This erosive discontinuity was interpreted as being a result of dense water cascading that is able to generate sufficient shear stress at the canyon heads to mobilize the coarse surface layer, eroding the basal strata. As a result, a pool of aged organic carbon (Delta C-14 = -944.5 +/- 24.7%; mean age 23,650 +/- 3,321 ybp) outcrops at the modern seafloor and is reexposed to the contemporary carbon cycle. This basal deposit was found to have relatively high terrigenous organic carbon (lignin = 1.48 +/- 0.14 mg/100 mg OC), suggesting that this material was deposited during the last low sea-level stand. A few sediment trap samples showed anomalously depleted radiocarbon concentrations (Delta C-14 = -704.4 +/- 62.5%) relative to inner shelf (Delta C-14 = -293.4 +/- 134.0%), mid-shelf (Delta C-14 = -366.6 +/- 51.1%), and outer shelf (Delta C-14 = -384 +/- 47.8%) surface sediments. Therefore, although the major source of particulate material during the cascading season is resuspended shelf deposits, there is evidence that this aged pool of organic carbon can be eroded and laterally advected downslope.

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We present the global phylogeography of the black sea urchin Arbacia lixula, an amphi-Atlantic echinoid with potential to strongly impact shallow rocky ecosystems. Sequences of the mitochondrial cytochrome c oxidase gene of 604 specimens from 24 localities were obtained, covering most of the distribution area of the species, including the Mediterranean and both shores of the Atlantic. Genetic diversity measures, phylogeographic patterns, demographic parameters and population differentiation were analysed. We found high haplotype diversity but relatively low nucleotide diversity, with 176 haplotypes grouped within three haplogroups: one is shared between Eastern Atlantic (including Mediterranean) and Brazilian populations, the second is found in Eastern Atlantic and the Mediterranean and the third is exclusively from Brazil. Significant genetic differentiation was found between Brazilian, Eastern Atlantic and Mediterranean regions, but no differentiation was found among Mediterranean sub-basins or among Eastern Atlantic sub-regions. The star-shaped topology of the haplotype network and the unimodal mismatch distributions of Mediterranean and Eastern Atlantic samples suggest that these populations have suffered very recent demographic expansions. These expansions could be dated 94-205 kya in the Mediterranean, and 31-67 kya in the Eastern Atlantic. In contrast, Brazilian populations did not show any signature of population expansion. Our results indicate that all populations of A. lixula constitute a single species. The Brazilian populations probably diverged from an Eastern Atlantic stock. The present-day genetic structure of the species in Eastern Atlantic and the Mediterranean is shaped by very recent demographic processes. Our results support the view (backed by the lack of fossil record) that A. lixula is a recent thermophilous colonizer which spread throughout the Mediterranean during a warm period of the Pleistocene, probably during the last interglacial. Implications for the possible future impact of A. lixula on shallow Mediterranean ecosystems in the context of global warming trends must be considered.

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Se da un catálogo sistemático y estratigráfico de los pectnidos del Negeno del NE de España.

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El estudio de la serie marina del Ilerdiense del Oeste (le Tremp (Lérida), sobre todo en el corte de la Carretera de Tremp a Pont de Montañana, ha sido ya realizado y sus resultados publicados parcialmente (DE REKZI 1965 y en prensa)...

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Biopolttoaineiden käyttö energiantuotannossa lisääntyy ja syrjäyttää samalla fossiilisia polttoaineita. Etenkin puupohjaisten polttoaineiden käyttö pienenergiantuotannossa on lisääntynyt nopeasti. Tätä kehitystä puoltavat tiukentuneet päästörajat ja yleinen mielipide fossiilisia polttoaineita vastaan sekä biopolttoaineiden verottomuus. Tästä johtuen biopolttoainetta käyttävien laitosten kysyntä kasvaa jatkuvasti. Kysynnän kasvaessa biopolttolaitosten valmistajien on pystyttävä nopeaan, tehokkaaseen ja laadukkaaseen toimintaan, sekä täyttämään asiakkaan tarpeet pystyäkseen vastaamaan alan kasvavaan kilpailuun. Tässä diplomityössä kehitetään standardoitua moduulirakennetta Sermet BioGrate ja BioGrate compact kattilalaitoksille. Moduloinnin tarkoituksena on helpottaa laitoskonseptin kokoonpanon suunnittelua, tarjousten ja tarjouslaskelmien tekemistä sekä yhtenäistää toimintatapoja, mikä vähentää työmäärää ja nopeuttaa toimituksia.

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Se estudian y comparan las trazas de depredación realizadas presumiblemente por crustáceos dedópodos sobre conchas degasterpodos y bivalvos procedentes de las áreas pliocéanicas catalanas del Baix Llobregat y del Empordà.

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En el presente trabajo se describen.16 especies de Euthyneura procedentes del Plioceno ael Empordh. Girona. Para ello se ha tenido en cuenta tanto el material nuevo como el procedente de las colecciones ya existentes, Cuando el numero dc individuos lo ha permitido, la descripcion ha sido acompañada por los siguientes datos numericos: valor maximo (M), minimo (m), media (x). desviación tipica (S). varianza (s2). intervalos media y varianza. asi como elcoeficiente de correlación (r).

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Se estudian y comparan las trazas de depredación realizadas presumiblemente por crustáceos dedópodos sobre conchas degasterpodos y bivalvos procedentes de las áreas pliocéanicas catalanas del Baix Llobregat y del Empordà.

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The linking of North and South America by the Isthmus of Panama had major impacts on global climate, oceanic and atmospheric currents, and biodiversity, yet the timing of this critical event remains contentious. The Isthmus is traditionally understood to have fully closed by ca. 3.5 million years ago (Ma), and this date has been used as a benchmark for oceanographic, climatic, and evolutionary research, but recent evidence suggests a more complex geological formation. Here, we analyze both molecular and fossil data to evaluate the tempo of biotic exchange across the Americas in light of geological evidence. We demonstrate significant waves of dispersal of terrestrial organisms at approximately ca. 20 and 6 Ma and corresponding events separating marine organisms in the Atlantic and Pacific oceans at ca. 23 and 7 Ma. The direction of dispersal and their rates were symmetrical until the last ca. 6 Ma, when northern migration of South American lineages increased significantly. Variability among taxa in their timing of dispersal or vicariance across the Isthmus is not explained by the ecological factors tested in these analyses, including biome type, dispersal ability, and elevation preference. Migration was therefore not generally regulated by intrinsic traits but more likely reflects the presence of emergent terrain several millions of years earlier than commonly assumed. These results indicate that the dramatic biotic turnover associated with the Great American Biotic Interchange was a long and complex process that began as early as the Oligocene-Miocene transition.

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Oceans, or other wide expanses of inhospitable environment, interrupt present day distributions of many plant groups. Using molecular dating techniques, generally incorporating fossil evidence, we can estimate when such distributions originated. Numerous dating analyses have recently precipitated a paradigm shift in the general explanations for the phenomenon, away from older geological causes, such as continental drift, in favour of more recent, long-distance dispersal (LDD). For example, the 'Gondwanan vicariance' scenario has been dismissed in various studies of Indian Ocean disjunct distributions. We used the gentian tribe Exaceae to reassess this scenario using molecular dating with minimum (fossil), maximum (geological), secondary (from wider analyses) and hypothesis-driven age constraints. Our results indicate that ancient vicariance cannot be ruled out as an explanation for the early origins of Exaceae across Africa, Madagascar and the Indian subcontinent unless a strong assumption is made about the maximum age of Gentianales. However, both the Gondwanan scenario and the available evidence suggest that there were also several, more recent, intercontinental dispersals during the diversification of the group.

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The history of biodiversity is characterized by a continual replacement of branches in the tree of life. The rise and demise of these branches (clades) are ultimately determined by changes in speciation and extinction rates, often interpreted as a response to varying abiotic and biotic factors. However, understanding the relative importance of these factors remains a major challenge in evolutionary biology. Here we analyze the rich North American fossil record of the dog family Canidae and of other carnivores to tease apart the roles of competition, body size evolution, and climate change on the sequential replacement of three canid subfamilies (two of which have gone extinct). We develop a novel Bayesian analytic framework to show that competition from multiple carnivore clades successively drove the demise and replacement of the two extinct canid subfamilies by increasing their extinction rates and suppressing their speciation. Competitive effects have likely come from ecologically similar species from both canid and felid clades. These results imply that competition among entire clades, generally considered a rare process, can play a more substantial role than climate change and body size evolution in determining the sequential rise and decline of clades.

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Kasvihuonekaasujen päästökauppa ja vihreät sertifikaatit liittyvät kehitysvaiheessa olevaan ilmastopoliittiseen kokonaisuuteen, jonka tarkoitus on rajoittaa ihmisen toiminnasta aiheutuvaa kasvihuoneilmiön voimistumista. Työssä tutkittiin Euroopan Unionin sisäisen päästökaupan ja vihreiden sertifikaattien vaikutusta energian toimittajaan. Tarkastelu tehtiin kohdeyrityksinä toimineiden yritysten näkökulmasta keskittyen energianhankintatapojen kilpailukykyyn ja kustannusmuutoksiin sekä niiden vaikutusten selvittämiseen. Päästökauppa tulee toteutuessaan heikentämään energiantuotannossa käytettyjen fossiilisten polttoaineiden ja turpeen kilpailukykyä hiilidioksidipäästöttömiin tuotantomuotoihin nähden ja aiheuttamaan lisäkustannuksia hiilidioksidia aiheuttavien tuotantomuotojen käytölle. Vihreät sertifikaatit ovat tapa tukea uusiutuvista energianlähteistä tuotettua sähköä. Niistä on kehittymässä Euroopassa erilaisia järjestelmiä eikä yhtenäisten eurooppalaisten markkinoiden toteutumisesta ole varmuutta. Suomalaisiin sähköntoimittajiin vihreät sertifikaatit voivat vaikuttaa myös, mikäli Suomeen perustetaan kansallinen sertifikaattijärjestelmä tai sähköntuottajat pystyvät hyödyntämään muiden maiden järjestelmiä.