Search results for "vol"

showing 10 items of 19880 documents

Seasonal and habitat effects on the nutritional properties of savanna vegetation: Potential implications for early hominin dietary ecology.

2019

The African savannas that many early hominins occupied likely experienced stark seasonality and contained mosaic habitats (i.e., combinations of woodlands, wetlands, grasslands, etc.). Most would agree that the bulk of dietary calories obtained by taxa such as Australopithecus and Paranthropus came from the consumption of vegetation growing across these landscapes. It is also likely that many early hominins were selective feeders that consumed particular plants/plant parts (e.g., leaves, fruit, storage organs) depending on the habitat and season within which they were foraging. Thus, improving our understanding of how the nutritional properties of potential hominin plant foods growing in mo…

010506 paleontologyForagingWetlandWoodlandBiologyForests01 natural sciencesGrasslandSoilSouth AfricaSavannaDry seasonAnimals0601 history and archaeologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciences2. Zero hungergeography060101 anthropologygeography.geographical_feature_categoryEcologyProteinfungifood and beveragesHominidae06 humanities and the artsVegetation15. Life on landPlantsbiology.organism_classificationDietary fiberGrasslandKenyaHominin dietHabitatAnthropologyWetlandsParanthropusSeasonsNutritive ValueJournal of human evolution
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La radiation des échinodermes au Paléozoïque inférieur, l'exemple des blastozoaires.

2009

10 pages; Le sous-phylum Blastozoa est un des groupes d'échinodermes les plus diversifiés (dix classes) au début du Paléozoïque. Après révision critique de leur squelette, leurs morphologies en apparence très variées sont en fait homogènes. Leur diversité montre deux pics (Drumien, Sandbien) liés par un événement de fortes apparitions génériques au Cambrien supérieur-Ordovicien inférieur. Les blastozoaires montrent un fort endémisme au Cambrien et un important provincialisme à l'Ordovicien inférieur et moyen. Ils deviennent cosmopolites à l'Ordovicien supérieur, par plusieurs événements migratoires. Ils sont restreints à la Laurentia et à Baltica au Silurien inférieur.

010506 paleontologyGeneral EngineeringÉvolutionBiostratigraphyBlastozoaEAT010502 geochemistry & geophysics01 natural sciencesPhylogenèse[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyHumanitiesGeology0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyEchinodermataPaléozoïque
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Timber Logging in Central Siberia is the Main Source for Recent Arctic Driftwood

2015

Abstract Recent findings indicated spruce from North America and larch from eastern Siberia to be the dominating tree species of Arctic driftwood throughout the Holocene. However, changes in source region forest and river characteristics, as well as ocean current dynamics and sea ice extent likely influence its spatiotemporal composition. Here, we present 2556 driftwood samples from Greenland, Iceland, Svalbard, and the Faroe Islands. A total of 498 out of 969 Pinus sylvestris ring width series were cross-dated at the catchment level against a network of Eurasian boreal reference chronologies. The central Siberian Yenisei and Angara Rivers account for 91% of all dated pines, with their oute…

010506 paleontologyGlobal and Planetary Changegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesbiologyLoggingDrainage basinDriftwoodbiology.organism_classification01 natural sciencesArcticBorealClimatology550 Earth sciences & geologySea icePhysical geographyLarchEcology Evolution Behavior and SystematicsGeologyHolocene0105 earth and related environmental sciencesEarth-Surface Processes
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The ELSA tephra stack: Volcanic activity in the Eifel during the last 500,000 years

2016

Abstract Tephra layers of individual volcanic eruptions are traced in several cores from Eifel maar lakes, drilled between 1998 and 2014 by the Eifel Laminated Sediment Archive (ELSA). All sediment cores are dated by 14C and tuned to the Greenland interstadial succession. Tephra layers were characterized by the petrographic composition of basement rock fragments, glass shards and characteristic volcanic minerals. 10 marker tephra, including the well-established Laacher See Tephra and Dumpelmaar Tephra can be identified in the cores spanning the last glacial cycle. Older cores down to the beginning of the Elsterian, show numerous tephra sourced from Strombolian and phreatomagmatic eruptions,…

010506 paleontologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEarth scienceGeochemistry010502 geochemistry & geophysicsOceanography01 natural sciencesLapilliStrombolian eruptionMaarVolcanoMagmaPhreatomagmatic eruptionTephraTephrochronologyGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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Conjunctive use of spectral gamma-ray logs and clay mineralogy in defining late Jurassic-early Cretaceous palaeoclimate change (Dorset, U.K.).

2006

Abstract Detrital clay mineralogy is controlled by weathered source rock, climate, transport and deposition that in turn influence the spectral gamma-ray (SGR) response of resultant sediments. Whilst a palaeoclimate signal in clay mineralogy has been established in some ancient successions, the SGR response remains contentious, largely because the data sets have yet to be collected at the same or appropriate vertical scales to allow comparison. In addition, the influence of organic matter on SGR is not always considered. Here, we present clay mineralogical, total organic carbon (TOC) and SGR analyses from the late Jurassic and early Cretaceous of the Wessex Basin, a period of previously doc…

010506 paleontologyJurassic-Cretaceous boundary[SDE.MCG]Environmental Sciences/Global ChangesSpectral gamma raychemistry.chemical_elementStructural basin010502 geochemistry & geophysicsOceanographyPalaeoclimate[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontology[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgDorsetKaoliniteOrganic matter[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/MineralogyEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesTotal organic carbonchemistry.chemical_classificationPaleontologyThoriumClay mineralogyCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesSource rockchemistry[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyPurbeck facies[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Évolution rétrograde de Neospathodus au cours de la crise Permo - Triasique

2016

The Permian - Triassic evolution of platform conodonts (Gondolellidae) consists mainly in developing the carina and the platform. During the sublethal environmental stress conditions subsequent to the Permian - Triassic extinction, the Wuchiapingian - Griesbachian Clarkina lineage is replaced by the primitive looking platform-lacking Dienerian - Aegean Neospathodus kummeli - Kashmirella timorensis lineage. Moreover, above Jinogondolella denticulata, end of the Capitanian Jinogondolella lineage, “Neospathodus” arcucristatus, an atavistic blade-like homeomorph that lacks a platform, underlies Protoclarkina crofti, of the base of the anagenetic Clarkina lineage. These primitive-looking forms a…

010506 paleontologyLineage (genetic)ExtinctionPermianbiologyEvolutionTriasConodontsPaleontologyÉvolutionProteromorphosis010502 geochemistry & geophysicsbiology.organism_classificationTriassic01 natural sciencesEnvironmental stressPaleontologyPhylogenèseTriasAtavismPeriod (geology)ConodontesProtéromorphosePhylogeny0105 earth and related environmental sciencesRevue de Micropaléontologie
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High-resolution geochemical and biotic records of the Tethyan 'Bonarelli Level' (OAE2, latest Cenomanian) from the Calabianca-Guidaloca composite sec…

2004

Abstract High-resolution micropalaeontological and chemostratigraphic records for the upper Cenomanian portion of the Calabianca–Guidaloca composite section (NW Sicily) provide new insight into the palaeoclimatic and palaeoceanographic evolution of the Tethys Ocean. The Bonarelli Level equivalent was identified on the basis of lithology and well constrained by calcareous plankton biostratigraphy and radiolarian assemblages, as well as by the δ 13 C curve showing a marked positive excursion (up to 4.7‰). The Bonarelli Level equivalent deposition is characterized by highly eutrophic conditions as testified by radiolarian proliferation. Black shale samples from the Calabianca–Guidaloca composi…

010506 paleontologyLithologyBiostratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesMicrofossilsCretaceousForaminiferaPaleontologyPalaeoceanography14. Life underwaterSicilyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyPaleontologyCretaceous Sicily Corg-rich deposits Bonarelli level equivalent Microfossils Geochemical proxies Palaeoceanography15. Life on landbiology.organism_classificationTethys OceanAnoxic watersCretaceous13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBonarelli level equivalentCenomanianGeology
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Griesbachian and Dienerian (Early Triassic) ammonoid faunas from Northwestern Guangxi and Southern Guizhou (South China).

2008

30 pages; International audience; Intensive sampling of the Luolou (northwestern Guangxi) and the Daye (southern Guizhou) Formations in South China leads to the recognition of a regional Griesbachian and Dienerian ammonoid succession for this key palaeobiogeographical area. The new biostratigraphical sequence comprises the upper Griesbachian ‘Ophiceras beds' and the lower Dienerian ‘Proptychites candidus beds', which are separated from the uppermost Dienerian ‘Clypites beds' by an unfossiliferous interval. These faunas contain some taxa with wide geographic distribution (e.g. Ambites, Pleurambites, Pleurogyronites, Proptychites candidus), thus facilitating correlation with faunal succession…

010506 paleontologyLuolou Fm.food.ingredientDaye FmFaunaEarly TriassicBiostratigraphyEarly Triassic010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesbiostratigraphy.PaleontologySequence (geology)foodAmmonoideaAnotocerasSouth ChinaEcology Evolution Behavior and Systematics0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologybiologyPaleontologyAmmonoideabiology.organism_classificationLuolou FmDaye Fm.ArcticOphiceras[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphybiostratigraphy[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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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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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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