0000000000434731

AUTHOR

Nieves Meléndez

showing 2 related works from this author

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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Middle Jurassic–Early Cretaceous tectono-sedimentary evolution of the southwestern Iberian Basin (central Spain): Major palaeogeographical changes in…

2019

Abstract The Middle Jurassic-Early Cretaceous tectono-sedimentary evolution of the southwestern part of the intraplate Iberian Basin (Spain) was mostly controlled by the Alto Tajo-Montes Universales (ATMU) and Landete-Teruel (LT) faults. During the Middle Jurassic, the ATMU fault separated a western area dominated by shallow marine carbonates, and an eastern area with open marine facies. During the Bathonian-Callovian, the area located to the west of the ATMU fault and north of the LT fault (Cuenca domain) was progressively exposed, and remained uplifted until the late Barremian. A widespread unconformity with a variable gap around the Callovian to mid-Oxfordian has been related to the onse…

010504 meteorology & atmospheric sciencesAptianStructural basin010502 geochemistry & geophysicsTethys Ocean01 natural sciencesUnconformityCretaceousGrabenPaleontologyFaciesIntraplate earthquakeGeneral Earth and Planetary SciencesGeology0105 earth and related environmental sciencesEarth-Science Reviews
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