Search results for " behavior"

showing 10 items of 11374 documents

Dental calculus indicates widespread plant use within the stable Neanderthal dietary niche.

2018

The ecology of Neanderthals is a pressing question in the study of hominin evolution. Diet appears to have played a prominent role in their adaptation to Eurasia. Based on isotope and zooarchaeological studies, Neanderthal diet has been reconstructed as heavily meat-based and generally similar across different environments. This image persists, despite recent studies suggesting more plant use and more variation. However, we have only a fragmentary picture of their dietary ecology, and how it may have varied among habitats, because we lack broad and environmentally representative information about their use of plants and other foods. To address the problem, we examined the plant microremains…

010506 paleontologyNeanderthalAnimal foodRange (biology)Ecology (disciplines)NicheArqueologia01 natural sciencesbiology.animalCalculusAnimals0601 history and archaeologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesNeanderthals2. Zero hungerPaleodontology060101 anthropologybiologySubsistence agriculture06 humanities and the artsFeeding Behavior15. Life on landPlantsDietEuropeGeographyHabitatArchaeologyAnthropologyIdentification (biology)Journal of human evolution
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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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Pre-Hirnantian (latest Ordovician) benthic community assemblages: controls and replacements in a siliciclastic-dominated platform of the eastern Anti…

2007

17 pages; International audience; Lower-middle Ashgill sedimentary strata from the Mediterranean region have recorded a key episode of temperate-to-cold water, carbonate productivity predating the onset of the Hirnantian glaciation. The latitudinal position of the Moroccan margin of North Gondwana during Ashgill should have been adequate for the recorded development of carbonate factories. However, carbonate productivity was neither homogeneous nor laterally persistent, as documented in the eastern Anti-Atlas. Whereas in the Erfoud area, the bryozoan-dominated limestones of the Ashgill Khabt-el-Hajar Formation indicate the intensive activity of carbonate factories, these were dramatically r…

010506 paleontologyNorthern Gondwana010502 geochemistry & geophysicsOceanographyCarbonate factory[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesUnconformitychemistry.chemical_compoundPaleontologyBenthic communities14. Life underwaterGlacial periodCoquinaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesLate OrdovicianPaleontologyGondwanaMoroccochemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrdovicianCarbonateSedimentary rockSiliciclasticGeology
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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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Ichnological evidence of semi-aquatic locomotion in early turtles from eastern Iberia during the Carnian Humid Episode (Late Triassic)

2018

Abstract Some of the earliest European records of fossil turtle footprints (Late Triassic, Middle Carnian, ~ 227–237 Ma) are interpreted from 46 footprints from three outcrops, Domeno, Quesa and Cortes de Pallas, located in the Iberian Range (eastern Spain). The samples were obtained from Upper Triassic rocks in Keuper Facies. They are characterized in the studied area by two well-defined evaporitic sequences, separated by a detrital stratigraphic interval, constituting the Manuel Sandstones Formation in which the studied fossil footprints were recorded. These fluvial deposits are correlatable with the Carnian Humid Episode. The footprints are tridactyl and tetradactyl, mainly digitigrade, …

010506 paleontologyPaleontologyFluvialKeuperTrackwayTrace fossil010502 geochemistry & geophysicsOceanography01 natural scienceslaw.inventionPaleontologylawFaciesSubaerialTetrapod (structure)Turtle (robot)Ecology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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TRACKING DINOSAURS IN COARSE-GRAINED SEDIMENTS FROM THE UPPER TRIASSIC OF ARDÈCHE (SOUTHEASTERN FRANCE)

2020

ABSTRACT Coarse-grained sediments deposited in high-energy environments are usually considered unfavorable to the preservation of fossil tracks. Here we report dinosaur footprints showing good physical preservation, despite being found in coarse-grained sandstones of alluvial origin from the Upper Triassic of Ardèche, southeastern France. The ichnoassemblage, dominated by Grallator isp., raises questions about the processes leading to the formation and preservation of tracks in coarse-grained sediments. The track-bearing surface is a medium- to coarse-grained quartz arenite that is microconglomeratic locally. The tracking surface grain size ranges from 0.2 to 2 mm and numerous pebbles are p…

010506 paleontologyPaleontologyPaleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology010502 geochemistry & geophysicsTracking (particle physics)01 natural sciencesEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesPALAIOS
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Unravelling extrinsic and intrinsic factors of the early Palaeozoic diversification of blastozoan echinoderms

2010

19 pages; International audience; The Subphylum Blastozoa represents more than one third of the early Palaeozoic echinoderm fauna. A comprehensive database including all records of blastozoans was built to provide quantitative analyses of palaeogeography and diversity patterns and processes, for the 10 classes currently included in this subphylum during the early Palaeozoic. The global pattern of taxonomic diversity shows two peaks during the Cambrian Series 3 and the Late Ordovician intervals. In Cambrian times, the high taxonomic diversity seems to be related with a high turnover rate and a high endemicity of blastozoan genera, whereas in Ordovician times, the rise in diversity is associa…

010506 paleontologyPaleozoicEvolutionBlastozoaEvolutionary fauna010502 geochemistry & geophysicsOceanography01 natural sciencesBlastozoaPaleontologyEcology Evolution Behavior and Systematics[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesEarth-Surface ProcessesExtinction eventDiversitybiologyCambrian Series 3EcologyEarly PalaeozoicPaleontology15. Life on landbiology.organism_classification13. Climate actionOrdovicianSiliciclastic[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalaeogeographyOriginationGeologyEchinodermataPalaeogeography, Palaeoclimatology, Palaeoecology
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Late Paleozoic microfaunas in the pebbles of the Podlipoglav conglomerate, Central Slovenia

2020

Abstract The Paleozoic conglomerate at Podlipoglav in the transitional area between the External and Internal Dinarides of Slovenia contains limestone pebbles that have been examined micropaleontologically. The recovered conodont faunas are marked by the obvious absence of shallow-water taxa. The Lower to Middle Devonian faunas are characterized by relatively abundant polygnathids that are assigned to the Emsian and early Eifelian excavatus-nothoperbonus, laticostatus and costatus Zones. The Pennsylvanian conodont faunas contain relatively deep-water Neolochriea or gondolellids indicating an early Bashkirian and Moscovian age. A presence of the radiolarian species Pseudoalbaillella nodosa s…

010506 paleontologyPaleozoicbiologyFaunaPaleontology010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesDevonianConglomeratePaleontologyPennsylvanianEifelianConodontEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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