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showing 10 items of 38174 documents

Early Pliocene continental vertebrate fauna at Puerto de la Cadena (SE Spain) and its bearing on the marine-continental correlation of the Late Neoge…

2017

In this paper, we synthesize sedimentological, magnetostratigraphic and paleontological data from the continental vertebrate site of Puerto de la Cadena (Murcia, SE Spain), in order to clarify its age. The study site is located on the northern edge of the Carrascoy mountain range, in the upper part of the Cigarrón Unit. The end-Messinian discontinuity has been detected at the base of this unit, which indicates it has an early Pliocene age. Abundant remains of small and large vertebrates, including rodents, lagomorphs, primates, carnivorans, perissodactyls, artiodactyls, proboscideans, testudines, squamats, and crocodiles, have been found in this area. Some of these elements are of African o…

010506 paleontologyMessinian salinity crisisFaunaEstratigrafíaLate MioceneBiostratigraphy010502 geochemistry & geophysicsOceanographyNeogene01 natural sciencesPaleontologybiology.animalSivatheriumEcology Evolution Behavior and SystematicsMagnetostratigraphy0105 earth and related environmental sciencesEarth-Surface ProcessesMammalsbiologyEcologyMagnetostratigraphyPaleontologyVertebrateReptilesBiostratigraphybiology.organism_classificationHipparionGeologyIberian Peninsula
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The Borschovo section of the Gauja and Amata regional stages (Leningrad Region, Russia): sedimentology and biostratigraphy

2018

The results of the detailed sedimentological study and bed-by-bed collecting of fossils from the Borschovo section exposing the upper Givetian–lower Frasnian boundary beds are discussed. The succession consists of sandstones alternating with argillaceous and clayey packages that contain vertebrate and plant remains in the upper part. The grain size, sedimentary structures and cross-bed orientation considerably differ in the Oredezh Beds and the Staritsa Beds. Fine- to coarse-grained cross-stratified sandstones of the Oredezh Beds most probably are fluvial deposits, whereas the sandstones of the Staritsa Beds yielding tidal structures that show variable directions of the cross-bedding were a…

010506 paleontologyMiddle–Upper Devonianbiologylcsh:QE1-996.5Biostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural scienceslcsh:GeologyPaleontologyAmataSection (archaeology)sedimentary environmentGeneral Earth and Planetary Sciencessiliciclastic depositsSedimentologyvertebrate assemblage.Geology0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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Bone diagenesis in arid environments; An intra-skeletal approach

2014

Bone trace element content and isotopic composition are closely related to human nutrition. The investigation of archaeological bone geochemistry can help us to better understand the relationship between past populations and their environment alongside cultural practices as inferred from dietary reconstruction. However, dietary in- formation may be altered post-mortem by diagenetic processes in soil. In this study, bone mineralogy (Ca/P, sec- ondary minerals, organic matter content and bone apatite crystallinity), histology, element content (Mg, Na, F, Sr, Ba, Mn, Fe, La, Ce and U) and stable isotope composition (δ13Candδ18O carbonate) were investigated at the intra- individual scale in ord…

010506 paleontologyMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesOceanography01 natural sciencesApatitechemistry.chemical_compound0601 history and archaeologyOrganic matterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeschemistry.chemical_classification060102 archaeologyEnamel paintStable isotope ratioBioerosionTrace elementPaleontology06 humanities and the artsDiagenesischemistryvisual_artvisual_art.visual_art_mediumCarbonateGeology
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Influence of dissolved organic matter on rare earth elements and yttrium distributions in coastal waters

2010

International audience; Data collected during this study indicate that dissolved Y and REE (rare earth element) behaviour can be monitored through shale-normalised ratios. Relationships occurring between these ratios suggest that leaching from lithogenic materials is the main source of REE in the studied area. This process involves riverine detrital matter in the inner area of the Gulf of Palermo. Features of shale-normalised patterns and the relationship recognised between dissolved Fe and Y/Ho suggest that REE are released from Fe-rich coatings of atmospheric dust. Observed similarities between dissolved Fe and chlorophyll- content suggest that leaching of Fe-rich atmospheric particulates…

010506 paleontologyMineralogyrare earth elementsMediterranean010502 geochemistry & geophysics01 natural sciencesMediterranean seaDissolved organic carbonMediterranean Sea[SDV.BBM]Life Sciences [q-bio]/Biochemistry Molecular BiologyOrganic matter14. Life underwaterScavengingEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental Sciencechemistry.chemical_classificationEcologyRare-earth elementAuthigenicParticulatesREE; Mediterranean; Ce anomalyREESettore GEO/08 - Geochimica E VulcanologiachemistryCe anomaly13. Climate actionEnvironmental chemistryGeneral Earth and Planetary SciencesSeawaterchlorophyll-YREE Ce anomaly Central Mediterranean late Quaternary Palaeoenvironmental reconstructionGeologyChemistry and Ecology
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Erratum to “Palaeoecological context for the extinction of the Neanderthals: A small mammal study of Stratigraphic Unit V of the El Salt site, Alcoi,…

2021

El Salt is an important reference site for understanding the extinction of Neanderthal populations in the eastern Iberian Peninsula during MIS 3. In this paper, we describe the small mammal assemblage from Stratigraphic Unit V, the youngest unit with evidence of human presence, based on nearly 1300 specimens. A total of seven rodents (Microtus arvalis, Microtus duodecimcostatus, Microtus cabrerae, Sciurus vulgaris, Arvicola sapidus, Eliomys quercinus and Apodemus sylvaticus), three insectivores (Talpa occidentalis, Crocidura sp., Sorex sp.) and one lagomorph (Oryctolagus cf. cuniculus) were identified. Palaeocological analyses point to drier conditions in this part of the stratigraphic sequ…

010506 paleontologyNeanderthalZoologySorex010502 geochemistry & geophysicsOceanography01 natural sciencesMicrotus cabrerae//purl.org/becyt/ford/1 [https]//purl.org/becyt/ford/1.5 [https]El SaltCrocidurabiology.animalSmall mammalsEliomysMicrotusEcology Evolution Behavior and SystematicsNeanderthals0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyMicrotus duodecimcostatusPaleontologyExtinctionbiology.organism_classificationPleistocenePalaeoclimatologyArvicolaGeologyIberian PeninsulaPalaeogeography, Palaeoclimatology, Palaeoecology
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Palaeoecological context for the extinction of the Neanderthals: A small mammal study of Stratigraphic Unit V of the El Salt site, Alcoi, eastern Spa…

2019

El Salt is emerging as a reference site for the study of the extinction of Neanderthal populations in the Eastern Iberian Peninsula during MIS 3. The small vertebrate assemblage analysed in this work is framed within this general objective and comes from Stratigraphic Unit V, the most recent unit with human presence. Nearly 1300 small mammal remains have been studied in order to reconstruct the palaeoecological conditions of this debated period. A total of seven rodents (Microtus arvalis, Microtus duodecimcostatus, Microtus cabrerae, Sciurus vulgaris, Arvicola sapidus, Eliomys quercinus and Apodemus sylvaticus), three insectivores (Talpa occidentalis, Crocidura sp., Sorex sp.) and one lagom…

010506 paleontologyNeanderthalbiologyMicrotus duodecimcostatusPaleontologyZoologySorex010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesMicrotus cabreraeCrocidurabiology.animalArvicolaEliomysMicrotusEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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First shark record from the Upper Cretaceous of the Kuril Islands, Far East Russia

2020

Abstract The first find of a Late Cretaceous shark tooth, or of any cartilaginous fish for that matter, from the Kuril Islands in the Russian Far East is recorded as Carcharias sp. (Lamniformes, Carchariidae). The specimen originates from Maastrichtian strata on the island of Shikotan that are assigned to the Malokurilsk Formation. It constitutes an extremely rare find from rocks of this age in the northwest Pacific region. External and internal dental structures have been reconstructed by the use of computed tomography. The vasculature of this lamniform tooth is first modelled by CT scanning and shown under different angles, which allows an assessment of the spatial arrangement of hierarch…

010506 paleontologyNorthwest PacificCartilaginous fishComputed tomography010502 geochemistry & geophysics01 natural sciencesMaastrichtianPaleontologystomatognathic systemmedicineComputed tomography0105 earth and related environmental sciencesbiologymedicine.diagnostic_testPaleontologybiology.organism_classificationCretaceousCarchariasCarchariasstomatognathic diseasesVascular systemLamniformesVascular channelFar EastGeologyElasmobranchiiCretaceous Research
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The end of the Messinian salinity crisis: Evidences from the Chelif Basin (Algeria).

2007

How did the Messinian Salinity Crisis end is a matter of intense debate between two opposite concepts i.e., the generalised dilution event, the so-called Lago–Mare, followed by the sudden restoration of the marine conditions at the base of the Zanclean, or the early partial or complete marine refill that would have happened earlier during the upper Messinian. The Chelif Basin of Northwestern Algeria, one of the greatest Messinian marginal basins of the Mediterranean, provides an exceptional opportunity to study in detail how this major paleoenvironmental change occurred through continuous sedimentary records of the Miocene–Pliocene boundary. Five sections representative of both the central …

010506 paleontologyOstracodSettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18OForaminiferaStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaPaleontologyMessinianOstracodZanclean14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyStable IsotopesMediterranean basinPaleontologySedimentologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationSettore GEO/08 - Geochimica E VulcanologiaOceanographyBenthic zoneAlgeriaClastic rockLago–MareSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyChelif basinGeologyMarine transgression
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Middle Triassic sharks from the Catalan Coastal ranges (NE Spain) and faunal colonization patterns during the westward transgression of Tethys

2020

Abstract Palaeogeographic changes that occurred during the Middle Triassic in the westernmost Tethyan domain were governed by a westward marine transgression of the Tethys Ocean. The transgression flooded wide areas of the eastern part of Iberia, forming new epicontinental shallow-marine environments, which were subsequently colonized by diverse faunas, including chondrichthyans. The transgression is recorded by two successive transgressive–regressive cycles: (1) middle–late Anisian and (2) late Anisian–early Carnian. Here, we describe the chondrichthyan fauna recovered from several Middle Triassic stratigraphic sections (Pelsonian-Longobardian) located at the Catalan Coastal Basin (western…

010506 paleontologyPalaeocurrentsFaunaPaleontologiaStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesCoastal chondrichthyansHybodusDispersal strategiesPaleontologyPeninsula14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyPaleontologyLadinianTethys Oceanbiology.organism_classificationLadinianAnisianTransgressiveGeologyMarine transgressionPalaeogeography, Palaeoclimatology, Palaeoecology
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Graphic correlation of the upper Eifelian to lower Frasnian (Middle-Upper Devonian) conodont sequences in the Spanish Central Pyrenees and comparison…

2016

010506 paleontologyPaleontologybiologyEifelian010502 geochemistry & geophysicsOceanographyConodontbiology.organism_classification01 natural sciencesGeologyDevonian0105 earth and related environmental sciencesPalaeontologia Electronica
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