Search results for " systematic"

showing 10 items of 6683 documents

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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Rich fen development in CE Europe, resilience to climate change and human impact over the last ca. 3500 years

2017

Here, for the first time in SE Poland, we document the long-term development of a rich fen and assess its sensitivity to climate change and human impacts over the last ca. 3500 years. Our results are based on a high-resolution, continuous plant macrofossil remains, mollusc and pollen record, complemented by geochemical, mineral magnetic and physical characterisation, and radiocarbon dating from Bagno Serebryskie rich fen located in SE Poland. Based on the palaeoecological data we distinguished five stages of wet habitat conditions: 5000–3300, 2800–2150, 1600–1100, 750–230, 150–10 cal yr BP and five dry periods at ca. 3300–2800, 2150–1600, 1100–750, 230–150, 10 to − 64 cal yr BP. The pollen …

010506 paleontologyPeat010504 meteorology & atmospheric sciencesClimate changeOmbrotrophicOceanographymedicine.disease_cause01 natural scienceslaw.inventionlawPollenmedicineRadiocarbon datingBogEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryCladium mariscusbiologyEcologyPaleontologyMacrofossilbiology.organism_classificationGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Vegetation dynamics of Kisima Ngeda freshwater spring reflect hydrological changes in northern Tanzania over the past 1200 years: implications for pa…

2021

13 pages; International audience; Kisima Ngeda (KN), a spring on the northern margin of saline Lake Eyasi, Tanzania, sustains an Acacia-Hyphaene palm woodland and Typha swamps, while the surrounding vegetation is semi-desert. To study the vegetation changes associated with this spring, which represents a plausible modern analog for the fossil springs documented in the nearby paleoanthropological and archaeological sites of Olduvai Gorge, we analyzed the pollen content of a 43 cm-long sediment core that documents vegetation changes since the last ~1200 years (from cal yrs. C.E. 841 to 2011). Our results show that (1) Hyphaene palms, which require meso-halophytic soil conditions were most abu…

010506 paleontologyPeat010504 meteorology & atmospheric sciencesOlduvaClimate[SDE.MCG]Environmental Sciences/Global ChangesOlduvai GorgeOlduvaiWetlandWoodlandOceanography01 natural sciencesPaleovegetationEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyHyphaenegeography.geographical_feature_categorybiologyHydrosystemPaleontologyHomininVegetationGroundwater recharge15. Life on landbiology.organism_classificationArid13. Climate action[SDU]Sciences of the Universe [physics][SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPhysical geographyGeologyNgorongoro
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COMMENT TO LEHRMANN ET AL. NEW SECTIONS AND OBSERVATIONS FROM THE NANPANJIANG BASIN, SOUTH CHINA

2016

In the study of Earth-surface environmental processes during the events associated with the Permian–Triassic boundary, a key issue is the nature of the latest Permian pre-extinction surface in shallow marine limestones in numerous sites, principally within the Tethyan realm. Sediments below this surface pre-date the extinction event, so that the limestones comprising these latest Permian facies contain diverse fossil remains of organisms that lived just before the extinction. At all reported sites, this surface is disconformably overlain by post-extinction sediments, which contain microbialites in many places, particularly in Tethys. The nature of the youngest pre-extinction surface remains…

010506 paleontologyPermianOutcropStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontology14. Life underwaterGeopetal sediemntComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesExtinction eventExtinctionPendent CementsMicrobialitePaleontologyOcean acidification13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSubaerial[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyErosional historyPALAIOS
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Amphibians and reptiles as palaeonvironmental proxies during the Late Pleistocene (MIS3): The case of Stratigraphic Unit V of El Salt, Alcoi, Spain

2021

The locality of El Salt (Alcoi, Spain) is a key site for understanding the extirpation of Neanderthals in the eastern part of Iberia. In this paper, we analyse an assemblage of amphibians and reptiles from Stratigraphic Unit V (45.2 ± 3.4 ka to 44.7 ± 3.4 ka), which corresponds to one of the last regional records of Neanderthals, to improve knowledge of the palaeoecology and palaeoclimate of this event. The assemblage comprises three anurans (Pelodytes sp., Alytes obstetricans, and Epidalea calamita), two lizards (Lacertidae indet. and Chalcides bedriagai), and five snakes (Colubridae indet., Coronella sp., Coronella sp./Zamenis sp., Natrix maura, and Vipera latastei). Palaeoclimatic recons…

010506 paleontologyPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory010502 geochemistry & geophysicsOceanography01 natural sciences//purl.org/becyt/ford/1 [https]HWMLATE PLEISTOCENE//purl.org/becyt/ford/1.5 [https]PALAEOCLIMATEZamenisLacertidaeCoronellaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyChalcides bedriagaiEcologyEpidalea calamitaIBERIAN PENINSULAPaleontology15. Life on landHERPETOFAUNAbiology.organism_classificationAridificationMERPaleoecologyGeology
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Using growth and geochemical composition of Clathromorphum compactum to track multiscale North Atlantic hydro-climate variability

2020

International audience; Records of ocean/atmosphere dynamics over the past centuries are essential to understand processes driving climate variability. This is particularly true for the Northwest Atlantic which is a key region with an essential role in global climate regulation. Over the past two decades, coralline red algae have been increasingly used as environmental and climatic archives for the marine realm and hold the potential to extend long-term instrumental measurements. Here, we investigate the possibility to extract climate and environmental information from annual growth patterns and geochemical composition of the coralline red algae, Clathromorphum compactum, from Saint-Pierre …

010506 paleontologyPopulationClimate change010502 geochemistry & geophysicsOceanography01 natural sciencesCoralline algaeAtmosphereSclerochronologyEnvironmental reconstructionSclerochronologyClathromorphum compactumClimate change14. Life underwatereducationArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeseducation.field_of_studygeographygeography.geographical_feature_categorybiologyACLEnvironmental proxyPaleontologyCoralline algaebiology.organism_classification13. Climate actionArchipelagoPhysical geography[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeology
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2020

Skeletal remains in archaeological strata are often assumed to be of similar ages. Here we show that combined Sr and O isotope analyses can serve as a powerful tool for assessing fish provenance and even for identifying fossil fish teeth in archaeological contexts. For this purpose, we established a reference Sr and O isotope dataset of extant fish teeth from major water bodies in the Southern Levant. Fossil shark teeth were identified within Iron Age cultural layers dating to 8–9th century BCE in the City of David, Jerusalem, although the reason for their presence remains unclear. Their enameloid 87Sr/86Sr and δ18OPO4 values [0.7075 ± 0.0001 (1 SD, n = 7) and 19.6 ± 0.9‰ (1 SD, n = 6), res…

010506 paleontologyProvenanceEcologySouthern LevantChalcolithicEnameloid010502 geochemistry & geophysicsTethys Ocean01 natural sciencesCretaceousOceanographyMediterranean seaIron Age14. Life underwaterEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesFrontiers in Ecology and Evolution
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Micro-PIXE/PIGE analysis of Palaeolithic mammoth ivory: Potential chemical markers of provenance and relative dating

2014

Abstract Micro-Proton Induced X-ray and Gamma-ray Emission (micro-PIXE/PIGE) provide non-destructive methods for the evaluation of the major, minor and trace element compositions of archaeological material. The current study applies micro-PIXE/PIGE analysis to mammoth ivory artefacts from four Palaeolithic sites (Abri Castanet, Vogelherd Cave, Grottes de la Verpilliere I and II) in France and Germany in order to assess the effectiveness of this approach to material older than 30,000 y BP. It has thus far not been established whether such methods of analysis can yield results of scientific and archaeological interest on ivory material that has undergone such extended periods of diagenesis. T…

010506 paleontologyProvenanceMicro pixe[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryMineralogyOceanography01 natural sciencesChemical markerCaveArchéologieEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesMammothgeographygeography.geographical_feature_category[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistorybiology010401 analytical chemistryTrace elementPaleontologybiology.organism_classificationArchaeology0104 chemical sciencesDiagenesis[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryRelative datingGeology
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