Search results for "cretaceous"

showing 10 items of 182 documents

First record ofColoborhynchus (Pterosauria) from the Santana Formation (Lower Cretaceous) of the Chapada do Araripe, Brazil

2001

The anterior tips of associated upper and lower jaws of a pterosaur from the Lower Cretaceous of Brazil are described and assigned to the taxonColoborhynchus in the family Ornithocheiridae. It is characterized by the shape and position of the sagittal crest on the upper and lower jaw, the arrangement and length of the teeth and the spoon-like lateral expansion of the anterior parts of the jaws. It closely resemblesColoborhynchus wadleighi from North America andColoborhynchus clavirostris from England. Diagnostic anatomical characteristics permit a revision of the genusTropeognathus, which is shown here to be a junior synonym of other described taxa.Tropeognathus mesembrinus is referred toCr…

SystematicsPterodactyloideabiologyPaleontologyAnatomyOrnithocheiridaebiology.organism_classificationCretaceousstomatognathic diseasesPaleontologystomatognathic systemTropeognathusSagittal crestSantana FormationColoborhynchusGeologyPaläontologische Zeitschrift
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Dinosaur bonebed amber from an original swamp forest soil

2021

AbstractDinosaur bonebeds with amber content, yet scarce, offer a superior wealth and quality of data on ancient terrestrial ecosystems. However, the preserved palaeodiversity and/or taphonomic characteristics of these exceptional localities had hitherto limited their palaeobiological potential. Here we describe the amber from the Lower Cretaceous dinosaur bonebed of Ariño (Teruel, Spain) using a multidisciplinary approach. Amber is found in both a root layer with amber strictly in situ and a litter layer namely composed of aerial pieces unusually rich in bioinclusions, encompassing 11 insect orders, arachnids, and a few plant and vertebrate remains, including a feather. Additional palaeont…

TaphonomyForests010502 geochemistry & geophysics01 natural sciencesCretaceousDinosaursSoilAmbreAssemblage (archaeology)Biology (General)insectsgeography.geographical_feature_categoryFossilsGeneral NeuroscienceQRGeneral MedicineBiodiversityCretaceouspalaeobiologyPaleoecologiaMedicineTerrestrial ecosystemecologyGeologyResearch Article010506 paleontologyQH301-705.5SciencePaleontologiaSwampGeneral Biochemistry Genetics and Molecular BiologyPaleontologíaPaleontologyNoneInsectes fòssilsAnimalsresin production0105 earth and related environmental sciencesgeographyEvolutionary BiologyGeneral Immunology and MicrobiologyPaleontology15. Life on landautochthonyAmberSpainWetlandsInsects fossilPaleoecology[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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Latest Cretaceous storm-generated sea grass accumulations in the Maastrichtian type area, the Netherlands – preliminary observations

2019

Abstract Ever since the first description of fossil material during the mid-nineteenth century, sea grass has been shown to be quite commonly preserved in ‘pockets’ or ‘clumps’ at certain levels within the Gulpen, Maastricht and Kunrade formations in southern Limburg (the Netherlands) and contiguous areas in northeast Belgium. In those places where silicification occurred during early diagenesis, even completely silicified and three-dimensionally preserved stems and roots can be found, mostly of Thalassocharis bosquetii, in association with fully marine molluscs such as dentaliid scaphopods and a range of larger foraminifera, bivalves, gastropods and ammonites. Such occurrences are best kno…

TaphonomybiologyThalassotaenia debeyiPosidoniaTempestitesMaastrichtianRange (biology)PaleontologyGeologyStormBiotaTempestitesbiology.organism_classificationCretaceousDiagenesisForaminiferaPaleontologyMaastrichtianGroup (stratigraphy)PosidoniaThalassotaemia debeyiGeology
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The complex nature of progenetic species — examples from Mesozoic ammonites

1991

Several examples of progenetic species among Mesozoic ammonites are investigated. The ammonites are Middle Jurassic kosmoceratids, Upper Jurassic oppeliids, and Upper Cretaceous scaphites. As assessed through outgroup comparison, the progenetic species in each of these examples is characterized by small size at maturity and the presence of morphological features typical of those of the juveniles of more primitive species. However, in none of these examples is the progenetic species a duplicate form of the juvenile stage of more primitive species. There are at least three kinds of features of progenetic species that differ from those of the juveniles of more primitive species: (1) symplesiom…

TaxonbiologyEvolutionary biologyEcologyScaphitesPaleontologyJuvenileMorphology (biology)Mesozoicbiology.organism_classificationHeterochronyEcology Evolution Behavior and SystematicsCretaceousLethaia
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Early Cretaceous termites in amber from northern Spain (Isoptera)

2020

Abstract Two virtually complete termites in Lower Cretaceous amber from the Penacerrada I outcrop, Spain, are described and figured, representing the most well-preserved Isoptera yet discovered from the Albian stage. The material is described as Ithytermes montoyai gen. et sp. nov., and is similar in many details to the slightly younger Krishnatermes yoddha Engel, Barden, and Grimaldi from northern Myanmar amber. Given the presence of distinct soldiers in this grade of Cretaceous termites, it is likely that I. montoyai also exhibited such a tripartite caste system. In addition to the type material of I. montoyai, two fragmentary termites are recorded for the first time in Albian amber from …

Taxonomia (Biologia)Cretaci010506 paleontologyCretaceous PeriodOutcropPaleontology010502 geochemistry & geophysics01 natural sciencesCretaceousAmberInsectesInsectsPaleontologyTaxonomy (Biology)Type (biology)TaxonGeographyStage (stratigraphy)Ambre0105 earth and related environmental sciencesCretaceous Research
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Sedimentary dynamics and extensional structuring related to early Cretaceous rifting of Neocomian and Barremian deposits of the interior basin of Gab…

2008

18 pages; International audience; Recent field and subsurface data about the early Neocomian N'dombo series and the Neocomian to mid-Barremian Schistes series of the interior basin of Gabon further our understanding of the initial stages of early Cretaceous N40–60E extensional rifting. The syn-rift series comprise fluvial–lacustrine claystones–sandstones, rare conglomerates, and carbonates. The syn-rift fill begins with braided-stream feldspathic sandstones. These are overlain first by fluvial–lacustrine deposits and then by predominantly lacustrine–palustrine claystones, which are potential petroleum source rocks. The claystones are eroded in part and are capped by the pre-Aptian angular u…

Tectono-sedimentary010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesPalaeoenvironment010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesUnconformitySedimentary depositional environmentPaleontologySedimentary dynamicsLower CretaceousGabon0105 earth and related environmental sciencesEarth-Surface Processes[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsRiftGeologySubsidence[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesSource rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSedimentary rockSyn-riftGeology
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Cenomanian–Turonian carbonate and organic-carbon isotope records, biostratigraphy and provenance of a key section in NE Sicily, Italy: Palaeoceanogra…

2008

In eastern Sicily, a series of highly organic-rich black shales occur as exotic blocks (~ 100 m across) floating in tectonized sediments (Argille Varicolori Unit containing olistoliths of Cretaceous-Palaeogene age). A 19-metre section, through one of these blocks near the town of Novara di Sicilia, includes cyclically bedded black shales, marlstones and claystones, which have been dated using planktonic foraminiferal and nannofossil biostratigraphy. On this basis, the section is assigned to the latest Cenomanian and clearly represents a manifestation of the Oceanic Anoxic Event characteristic of that interval. Total organic-carbon values range up to 23% and the relatively high hydrogen indi…

Total organic carbonProvenanceRange (biology)PaleontologyBiostratigraphyOceanographyCretaceousPaleontologychemistry.chemical_compoundchemistrySection (archaeology)CarbonateCenomanianEcology Evolution Behavior and SystematicsGeologySicily OAE Bonarelli Level Carbon-isotope stratigraphy TOC Biostratigraphy Palaeoceanography PalaeogeographyEarth-Surface Processes
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The Valanginian positive carbon isotope event in Arctic Russia: Evidence from terrestrial and marine isotope records and implications for global carb…

2010

The data presented here comprise Ryazanian–Valanginian carbon isotope ratios analyzed from fossil wood and belemnites from the shallow marine Boyarka River succession in Siberia. Additional belemnite carbon isotope ratios from the Izhma River succession (also Ryazanian–Valanginian) in Russia are also presented. The wood-derived and belemnite-derived isotope ratios are considered to primarily reflect changes in the terrestrial and marine carbon isotope reservoirs respectively. The δ13Ccarb and δ13Cwood records reveal a distinct mid-Valanginian positive carbon isotope excursion, with the initiation occurring near the Boreal Russian michalskii–polyptychus zone boundary, which is broadly time-e…

Total organic carbonbiologyPaleontologychemistry.chemical_elementbiology.organism_classificationCretaceousCarbon cyclePaleontologychemistry.chemical_compoundArcticchemistryIsotopes of carbonCarbonateBelemnitesCarbonGeologyCretaceous Research
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Evolution of neodymium isotopic signature of seawater during the Late Cretaceous: implications for intermediate and deep circulation.

2016

20 pages; International audience; Neodymium isotopic compositions (εNd) have been largely used for the last fifty years as a tracer of past ocean circulation, and more intensively during the last decade to investigate ocean circulation during the Cretaceous period. Despite a growing set of data, circulation patterns still remain unclear during this period. In particular, the identification of the deep-water masses and their spatial extension within the different oceanic basins are poorly constrained. In this study we present new deep-water εNd data inferred from the Nd isotope composition of fish remains and Fe–Mn oxyhydroxide coatings on foraminifera tests, along with new εNd data of resid…

Water mass010504 meteorology & atmospheric sciences010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousBottom waterPaleontologyOcean circulation[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterSouthern Ocean0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryNeodymium isotopesNorth Atlantic Deep WaterOcean currentAbyssal plainGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousOceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyThermohaline circulationOceanic basinGeology
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Revisión de la sección del yacimiento del Mas de la Chimenea Alta (Formación Arcillas de Morella, Castellón) y significado en el contexto paleoambien…

2012

Desde los primeros estudios estratigráficos y paleontológicos, que datan de principios del siglo XX, la Fm Morella se ha caracterizado por su coloración rojiza y su contenido fósil. La mayor parte de sus depósitos se han interpretado como continentales, aunque con intercalaciones locales de materiales marinos. En esta unidad se da la paradoja de que muchos de los lugares descritos con fauna de vertebrados continentales se encuentran en depósitos interpretados como ambientes marinos poco profundos y de transición. La sección del Mas de la Chimenea Alta es un ejemplo. Ésta contiene yacimientos con fósiles de vertebrados que son claramente alóctonos, pero también otros, con icnitas que permite…

Wave-dominated deltaMaestrat BasinIberian SystemLower CretaceousSistema IbéricoCretácico InferiorDinosauriosCuenca del MaestrazgoDelta dominado por el oleajeDinosaurs
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