190 research outputs found
A new chondrichthyan fauna from the Late Jurassic of the Swiss Jura (Kimmeridgian) dominated by hybodonts, chimaeroids and guitarfishes
The fossil record of chondrichthyans (sharks, rays and chimaeroids) principally consists of isolated teeth, spines and dermal denticles, their cartilaginous skeleton being rarely preserved. Several Late Jurassic chondrichthyan assemblages have been studied in Europe based on large bulk samples, mainly in England, France, Germany and Spain. The first study of this kind in Switzerland is based on controlled excavations in Kimmeridgian deposits related to the construction of the A16 motorway in the Swiss Jura (Porrentruy, NW Switzerland). This study is based on more than 2000 isolated chondrichthyan remains (teeth, dental plates, spines and dermal denticles) and adds to our knowledge of the chondrichthyan distribution at a regional scale in Europe. We describe and identify this new fauna, define a new species of hybodont with crushing-type dentition (Asteracanthus udulfensis sp. nov.) and report for the first time the carcharhiniform Corysodon cirinensis in Switzerland. By the Late Jurassic, modern neoselachian sharks had overtaken hybodonts in European marine realms, the latter being gradually confined to brackish or freshwater environments. However, while the associated fauna of the Porrentruy platform indicates marine conditions, neoselachian sharks are surprisingly rare. The chondrichthyan assemblage is largely dominated by hybodonts, guitarfishes (rays) and chimaeroids that are all known to be euryhaline. This unexpected chondrichthyan faunal composition questions the presence of fresh to brackish water in the vicinity of the platform, and the occurrence of salinity fluctuations within a general context marine. This could explain the scarcity of neoselachian sharks and the extended success of hybodonts in the Porrentruy area as late as the Late Jurassic.Fil: Leuzinger, Léa Sylvia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Section d'archéologie et paléontologie; SuizaFil: Cuny, Gilles. Université Claude Bernard Lyon 1; FranciaFil: Popov, Evgeny. Saratov State University; Rusia. Kazan Federal University; RusiaFil: Billon Bruyat, Jean Paul. Section d'archéologie et paléontologie; Suiz
Influence of bioturbation by the polychaete Nereis diversicolor on the structure of bacterial communities in oil contaminated coastal sediments
Patterns of change in the structure of bacterial communities monitored by ribosomal intergenic spacer analysis (RISA) in oil contaminated sediments inhabited or not by the marine polychaete Nereis diversicolor were studied during 45 days under laboratory conditions. Results supported by principal component analysis showed a marked response of the bacterial communities to the oil contamination and to the presence of N. diversicolor. Phylogenetic affiliation of specific RISA bands showed that, in the contaminated sediments, the presence of the marine polychaetes favoured the development of bacteria which may play an active role in natural bioremediation processes of oil polluted environments
First record of <i>Lagarodus</i> (Chondrichthyes: Euchondrocephali) from the Carboniferous of Svalbard, Arctic Norway
The rather enigmatic genus Lagarodus is reported for the first time from the Bashkirian of Svalbard. Lagarodus first appeared in the equatorial region during the Tournaisian and then extended its geographical distribution to the intertropical zone around the Euramerican continent. The Svalbard discovery hints at the possibility that the northern species was different from the southern one
Freshwater hybodont sharks from the Late Jurassic - Early Cretaceous of Northeastern Thailand:stratigraphical and palaeobiogeographical implications
Diversity dynamics in the global Permian-Triassic chondrichthyan fauna: taxonomic diversity, palaeoecology and distribution
Associated skeletal and dental remains of a fossil odontaspidid shark (Elasmobranchii: Lamniformes) from the middle eocene Lillebælt clay formation in Denmark
A new site with articulated fish remains (Actinopterygii: Holostei) from the Late Triassic of Thailand
Continental drainage and oceanic circulation during the Jurassic inferred from the Nd isotope composition of biogenic phosphates and sediments
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