Search results for "CLASSIFICATION"

showing 10 items of 29475 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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A large temnospondyl humerus from the Rhaetian (Late Triassic) of Bonenburg (Westphalia, Germany) and its implications for temnospondyl extinction

2018

Temnospondyls are a group of basal tetrapods that existed from the Early Carboniferous to the Early Cretaceous. They were characteristic members of Permian and Triassic continental faunas around the globe. Only one clade, the Brachyopoidea (Brachyopidae and Chigutisauridae), is found as relics in the Jurassic of eastern Asia and the Cretaceous of Australia. The other Late Triassic clades, such as Plagiosauridae, Metoposauridae, and Cyclotsauridae, are generally believed to have gone extinct gradually before the end of the Triassic and putative Rhaetian records are stratigraphically poorly constrained. Temnospondyl humeri all show a similar morphological pattern, being stout, short, with wid…

010506 paleontologyFormación ExterbiologyPermianStratigraphyPaleohistologyGeologyBrachyopoideaCyclotosaurusChigutisauridae010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousBrachyopidaePaleontologyTemnospondyliMetoposauridaeCarboniferousCyclotosaurusRhaetic bonebedGeology0105 earth and related environmental sciencesJournal of Iberian Geology
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Translating taxonomy into the evolution of conodont feeding ecology

2016

Conodont research has long been divided between utilitarian applications to solve geological problems versus analysis of their palaeobiology. However recent advances in conodont functional analysis allow these independent stands of research to be unified, decoding the functional implications of their morphological variation. We demonstrate this using synchrotron tomography and Finite Element Analysis, informed by occlusal and microwear analyses, to analyze functionally the classic evolutionary sequence of the genus Polygnathus. Our study shows that the evolution of the platform in Polygnathus occurred to accommodate and dissipate the stress accumulation derived from the tooth-like function …

010506 paleontologyFunctional ecologySynchrotron tomographybiologyPaleobiologyGeology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesPaleontologyPhylogeneticsTaxonomy (biology)ConodontCladeFeeding ecology0105 earth and related environmental sciences
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REWORKING OF FUSULINIDS AND CALCIPHAERIDS IN THE LERCARA FORMATION (SICILY, ITALY); GEOLOGICAL IMPLICATIONS

2004

Different fusulinids have been identified in the Lercara Formation (Sicily). They are: Reichelina sp., Schubertella paramelonica, Toriyamaia (?) sp., Neofusulinella lantenoisi, Yangchienia compressa, Rauserella staffi, Darvasites contractus, Chalaroschwagerina (Taiyuanella?) aff. davalensis, Levenella aff. evoluta, Pamirina darvasica, and Neoschwagerina ex gr. craticulifera. Small Permian foraminifers, as well as the calcispherid Asterosphaera pulchra also exist. The microfossils indicate reworking of different Permian stages, at different periods of time, and possibly also of the Mississippian (Early Carboniferous). All these resediments have been deposited within the Lercara Formation, a …

010506 paleontologyFusulinidaePaleozoicPermianForaminifèresPermianForaminiferaBiostratigraphy010502 geochemistry & geophysics01 natural sciencesPermienForaminiferaPaleontologyPalaeobiogeographyCarboniferousPhanerozoicddc:550TriasFusulinid14. Life underwaterSicilyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesbiologyRemaniementsReworkGeneral Engineeringbiology.organism_classificationTriassicFusulinesSicile[SDU]Sciences of the Universe [physics]Period (geology)GeologyPaléobiogéographie
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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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Not only flint: Levallois on quartzite and limestone at Abrigo de la Quebrada (Valencia, Spain): Implications for neandertal Behavior

2016

This paper investigates the application of the Levallois technique to the knapping of nonflint raw materials (limestone and quartzite) in the upper levels of the Abrigo de la Quebrada rockshelter (Chelva, Valencia, Spain). Besides highlighting the significant flexibility that characterized Neandertal behavior, such an application is of singular interest because goodquality flint—lacking fissures and impurities and presenting a compact and homogeneous texture—is abundant in the site’s immediate vicinity. In other assemblages, the scarcity or poor quality of flint often suffices to explain the recourse to alternatives, but in these Quebrada levels raw material choice must be primarily determi…

010506 paleontologyHearthLevalloisLevallois technique01 natural sciencesPoor qualityLithic technologyArts and Humanities (miscellaneous)Middle PaleolithicMiddle Palaeolithic0601 history and archaeology:HISTORIA [UNESCO]Lithic technologyValencia0105 earth and related environmental sciencesUNESCO::HISTORIA060102 archaeologybiologyKnappingNeandertal behaviorLithic technology Levallois limestone quartzite Middle Paleolithic Neandertal behavior Iberian Peninsula06 humanities and the artsLimestonebiology.organism_classificationArchaeologyQuartziteHomogeneousAnthropologyGeologyIberian Peninsula
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Annually resolved δ<sup>2</sup>H tree-ring chronology of the lignin methoxyl groups from Germany reflects averaged Wester…

2019

Abstract. Stable hydrogen isotopes ratios of lignin methoxyl groups (expressed as δ2HLM) of wood have been shown to reflect the climate-sensitive δ2H values of precipitation (expressed as δ2Hprecip) modulated by a large uniform negative isotope fractionation. However, a detailed calibration study among temporal variabilities of δ2HLM in tree-ring series, site-specific δ2Hprecip and climate parameters has not been performed yet. Here, we present annually resolved δ2HLM values from nine tree-ring series (derived from four Fagus sylvatica L. trees) collected near stations of the Global Isotope Network of Isotopes in Precipitation (GNIP) and the Deutsche Wetterdienst (DWD) meteorological observ…

010506 paleontologyIsotopebiologybiology.organism_classificationAtmospheric sciences01 natural scienceschemistry.chemical_compoundSurface air temperatureIsotope fractionationFagus sylvaticachemistryMeteorological observatoryEnvironmental scienceLigninPrecipitation0105 earth and related environmental sciencesChronology
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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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Report on the 4th International Meeting of the IUGS Lower Cretaceous ammonite working group, the "Kilian Group" (Dijon, France, 30th August 2010).

2011

8 pages; International audience; The 4th Kilian Group meeting (Dijon, France, 30th August 2010) focused on the Aptian and Albian Stages. For the Aptian, a two-fold division of the stage was adopted for the Mediterranean area with a boundary between the Dufrenoyia furcata and Epicheloniceras martini Zones. The main changes to the zonal scheme concern the Lower Aptian with: the introduction of a Deshayesites luppovi Subzone in the upper part of the Deshayesites oglanlensis Zone; the replacement of Deshayesites weissi by Deshayesites forbesi as new indexspecies of the second interval zone; the introduction of a Roloboceras hambrovi Subzone in the upper part of the D. forbesi Zone; and the subd…

010506 paleontologyKilian GroupAptian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyStage (stratigraphy)AmmonitesGroup (stratigraphy)Lower CretaceousAptianMortoniceras0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmonitebiologyDouvilleicerasPaleontologyAlbianbiology.organism_classificationCretaceouslanguage.human_language[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyStandard zonationDipoloceraslanguage[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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A new species ofPlesiodimylus(Dimylidae, Eulipotyphla, Mammalia) from the Early Miocene of Spain

2017

AbstractWe report a new dimylid species, Plesiodimylus ilercavonicus sp. nov., from the Early Miocene locality of Mas d’Antolino B-5 (Ribesalbes-Alcora, Castello, Spain). This new species of Plesiodimylus is an amblyodont form of the genus and exhibits some primitive characters. The phylogenetic and palaeoenvironmental implications of this southern occurrence of Plesiodimylus in Lower Miocene sediments are discussed.urn:lsid:zoobank.org:act:EB5435A4-EECE-4B88-B5AC-4B77E2E13029

010506 paleontologyLSIDPhylogenetic treeEcologyZoologyInsectivoreBiology010502 geochemistry & geophysicsSoricomorphabiology.organism_classification01 natural sciencesGenusGeneral Agricultural and Biological Sciences0105 earth and related environmental sciencesHistorical Biology
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