Search results for "Laurasia"

showing 7 items of 7 documents

Carboniferous granites on the northern margin of Gondwana, Anatolide-Tauride Block, Turkey - Evidence for southward subduction of Paleotethys

2016

Carboniferous metagranites with U-Pb zircon crystallization ages of 331-315 Ma crop out in the Afyon zone in the northern margin of the Anatolide-Tauride Block, which is commonly regarded as part of Gondwana during the Late Palaeozoic. They are peraluminous, calc-alkaline and are characterized by increase in Rb and Ba, decrease in Nb-Ta, and enrichment in Sr and high LILE/HFSE ratios compatible with a continental arc setting. The metagranites intrude a metasedimentary sequence of phyllite, metaquartzite and marble; both the Carboniferous metagranites and metasedimentary rocks are overlain unconformably by Lower Triassic metaconglomerates, metavolcanics and Upper Triassic to Cretaceous recry…

010504 meteorology & atmospheric sciencesPaleozoicPermianSubductionMetamorphism15. Life on land010502 geochemistry & geophysics01 natural sciencesContinental arcPaleontologyGondwanaGeophysicsLaurasiaCarboniferousInstitut für GeowissenschaftenGeology0105 earth and related environmental sciencesEarth-Surface Processes
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New Permian tetrapod footprints and macroflora from Turkey (Çakraz Formation, northwestern Anatolia): biostratigraphic and palaeoenvironmental implic…

2011

9 pages; International audience; New tetrapod footprints belonging to the ichnogenus Hyloidichnus have been discovered in Turkey for the first time, in the lower part of the Çakraz Formation (Northwestern Anatolia) and together with macrofloral imprints of Annularia and Stigmaria. These discoveries confirm the Permian age of the fossiliferous red beds in which the coniferophyte Walchia was previously recorded. Based on the stratigraphic range of Annularia, Stigmaria and Hyloidichnus known elsewhere, a Cisuralian age is proposed for these beds. These new ichno- and macrofloral remains, together with the sedimentological data (mudcracks, rain drops) suggest the presence of captorhinid reptile…

010506 paleontologyPermianPangaeaTurkeyIchnitesStigmaria010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyStigmariaMacrofloraTetrapod (structure)CaptorhinidMigration0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRed bedsbiologyWalchiaGeneral Engineeringbiology.organism_classificationAnnulariaHyloidichnusLaurasia[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyAnnularia[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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The migration path of Gondwanian dinosaurs toward Adria: New insights from the Cretaceous of NW Sicily (Italy)

2021

Abstract The increasing dinosaur record from Italy questioned classic palaeogeographic scenarios for the Central Mediterranean area and suggest the proximity of landmass areas and a geographical connection between Gondwana and Laurasia during Cretaceous times. Besides several track-sites and exceptionally-preserved specimens (e.g. Scipionyx samniticus), the Italian dinosaur record also consists of isolated bones, among which the bone fragment of a theropod discovered in north-western Sicily. The bone occurs in a shallow-water carbonate succession (i.e. Pizzo Muletta, Palermo Mountains) pertaining to the Panormide Carbonate Platform (PCP). The bone was previously ascribed to the Cenomanian, …

010506 paleontologybiologyAptianCarbonate platformLand bridgePaleontology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousGondwanaPaleontologyLaurasiaScipionyxCenomanianGeology0105 earth and related environmental sciencesCretaceous Research
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Late Cretaceous-Early Eocene origin of yams (Dioscorea, Dioscoreaceae) in the Laurasian Palaearctic and their subsequent Oligocene-Miocene diversific…

2015

Aim: Dioscorea (Dioscoreaceae) is a predominantly pantropical genus (< 600 species) that includes the third most important tropical tuber crop and species of pharmacological value. Fossil records from both the Northern and Southern Hemispheres were used to test hypotheses about the origin of the genus Dioscorea, and to examine potential macroevolutionary processes that led to its current distribution. Location: Pantropical distribution. Methods: Divergence times were estimated using the most comprehensive phylogeny of the group published to date based on plastid sequences and fossil calibrations, applying a relaxed-clock model approach. Ancestral areas and range shifts were reconstructed us…

0106 biological sciencesRange (biology)Thulean – Beringian land bridgesBiogeographyDispersal-extinction-cladogenesis modelPantropicalBiologySoutheast asianN-S American Long-Distance Dispersal010603 evolutionary biology01 natural sciencesPalaearctic – Nearctic colonizationPaleontologyLaurasian originEcology Evolution Behavior and SystematicsEcologyEcologyLand bridgePantropical distributionFossil constrainsWestern Palaearcticbiology.organism_classificationYamsPhylogenetic datingBiogeographyBiological dispersalDioscorea010606 plant biology & botany
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World distribution of middle Jurassic ammonites (Upper Aalenian to Middle Bathonian): relationships between biodiversity and palaeogeography

2004

Abstract The break up of the Pangea takes place in the Jurassic; the palaeoceanographic consequences are the opening of seaways, particularly at the place of the future Atlantic and Indian oceanic areas. During the Toarcian, and from the late Aalenian to the middle Bathonian, the so-called “Hispanic corridor” (or “Atlantic seaway”) exists between the “western Tethys” and the “American Pacific border”, through the “Caribbean Tethys”. Two additional seaways which play as by-passes of the Pangea are proposed, one along the northern border of Laurasia (Boreal sea), and a second along the southern border of Gondwana (South Pacific Sea); however, if these two last could be effectively used for fa…

AmmonitebiologyRange (biology)AmmonitinaGeologyBiozoneDiachronousbiology.organism_classificationlanguage.human_languagePaleontologyGondwanaLaurasialanguageEndemismGeologyBulletin de la Société Géologique de France
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Ancient proteins resolve the evolutionary history of Darwin's South American ungulates.

2015

No large group of recently extinct placental mammals remains as evolutionarily cryptic as the approximately 280 genera grouped as 'South American native ungulates'. To Charles Darwin, who first collected their remains, they included perhaps the 'strangest animal[s] ever discovered'. Today, much like 180 years ago, it is no clearer whether they had one origin or several, arose before or after the Cretaceous/Palaeogene transition 66.2 million years ago, or are more likely to belong with the elephants and sirenians of superorder Afrotheria than with the euungulates (cattle, horses, and allies) of superorder Laurasiatheria. Morphology-based analyses have proved unconvincing because convergences…

ProteomicsAncient proteinsNotoungulataBiologíaPlacentaCiencias de la Tierra y relacionadas con el Medio Ambiente//purl.org/becyt/ford/1 [https]//purl.org/becyt/ford/1.5 [https]Genética y HerenciaPregnancyNotoungulataToxodonUngulateAfrotheriaPhylogenyMammalsMultidisciplinaryLaurasiatheriaLitopternabiologyAncient DNAFossilsLaurasiatheriaToxodonLitopternaFemaleCIENCIAS NATURALES Y EXACTAS1000UngulateZoologyPaleontologíaBone and BonesCollagen Type ICiencias BiológicasAnimalsAmino Acid Sequence//purl.org/becyt/ford/1.6 [https]BiologyPerissodactylaMAMMALIA2700MacraucheniaSouth Americabiology.organism_classificationCOLLAGEN (I)MacraucheniaAncient DNACattleMeteorología y Ciencias AtmosféricasZoologyAfrotheriaNature
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Upper Givetian and Frasnian (Middle and Upper Devonian) conodonts from Ampriú (Aragonian Pyrenees, Spain): global correlations and palaeogeographic r…

2012

This report describes for the first time a part of the Middle and Upper Devonian conodont sequence of the Sierra Negra Subfacies in the Aragonian Pyrenees (Spain), establishing the basis for further sound correlations both across the distinct Pyrenean facies and subfacies and on other relevant world areas. The description of 20 conodont taxa and their stratigraphical distribution permits recognition of two separate time intervals. The older one corresponds to the lower Upper Givetian (Middle Devonian), hermanni to crista- tus ectypus zones. The younger interval is uppermost Lower Frasnian to lower Middle Frasnian (Upper Devonian) and is equivalent to MN4-MN6 zones. The combination of litho-…

biologyPaleontologyBiostratigraphyStructural basinbiology.organism_classificationDevonianSequence (geology)PaleontologyGondwanaLaurasiaFaciesConodontEcology Evolution Behavior and SystematicsGeologyPalaeontology
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