Search results for "Foothills"

showing 4 items of 4 documents

A tough travesía: Mobility constraints among late Holocene Patagonian hunter-gatherers through oxygen stable isotopes in enamel and water sources

2020

Central-eastern North Patagonia is characterized by a severe environmental fragmentation due to the scarce and heterogeneous distribution of fresh water. The main local wet zones, the Negro and Colorado river valleys in the North and the Somuncura Foothills in the South are separated by a large and harsh dry land, the travesia. In this paper, we assess the effects of this environmental fragmentation in the mobility of the Late Holocene hunter-gatherers through the analysis of the stable isotopes of oxygen in both enamel and water sources. We analyzed the δ18O of the enamel carbonate of 64 human teeth from 42 individuals from the Negro River valley (n = 30) and the Somuncura Foothills (n = 1…

010506 paleontologyArcheologyHistoria y Arqueologíaδ18O01 natural sciencesArqueologíachemistry.chemical_compoundHUMANIDADESPatagoniaCiencias Naturales0601 history and archaeologyFoothillsStable oxygen isotopesHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_category060102 archaeologyStable isotope ratioBaseline (sea)Fragmentation (computing)06 humanities and the artsPaleomobilitychemistryHunter-gatherersCarbonatePhysical geographySurface waterGeology
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Dust mobilization due to density currents in the Atlas region: Observations from the Saharan Mineral Dust Experiment 2006 field campaign

2007

[1] Evaporation of precipitation is a ubiquitous feature of dry and hot desert environments. The resulting cooling often generates density currents with strong turbulent winds along their leading edges, which can mobilize large amounts of dust. Mountains support this process by triggering convection, by downslope acceleration of the cool air, and by fostering the accumulation of fine-grained sediments along their foothills through the action of water. For the Sahara, the world's largest dust source, this mechanism has been little studied because of the lack of sufficiently high resolution observational data. The present study demonstrates the frequent occurrence of density currents along th…

ConvectionAtmospheric ScienceMeteorologySoil ScienceAquatic ScienceMineral dustOceanographyAtmospheric sciencesWind speedHaboobGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)FoothillsEarth-Surface ProcessesWater Science and Technologygeographygeography.geographical_feature_categoryEcologyPaleontologyForestryWind directionGeophysicsDew pointMountain chainSpace and Planetary ScienceEnvironmental scienceJournal of Geophysical Research
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The body mass of the roe deer (Capreolus capreolus L.) in the foothills of the East Sudety Mountains / Masa tusz saren (Capreolus capreolus L.) na Po…

2013

Roe deergeographyCapreolusgeography.geographical_feature_categorybiologybiology.animalZoologyGeneral Materials ScienceFoothillsbiology.organism_classificationAnnales UMCS, Zootechnica
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A terminal Cretaceous giant pterosaur from the French Pyrenees

1997

A very large pterosaur cervical vertebra is described from the Upper Maastrichtian deposits of Mérigon, in the foothills of the French Pyrenees. It resembles the vertebrae of Quetzalcoatlus, from the Maastrichtian of Texas, more than those of Arambourgiania, from the Maastrichtian of Jordan. The estimated wing span of the Mérigon pterosaur is close to 9 m, which makes it one of the largest known flying creatures. Giant pterosaurs still had a wide geographical distribution at the end of Maastrichtian time, which is not suggestive of a declining group, although it is difficult to obtain an accurate estimate of taxonomic diversity of terminal Cretaceous pterosaurs on the basis of available dat…

geographyQuetzalcoatlusgeography.geographical_feature_categoryCreaturesbiologyArambourgianiaGeologybiology.organism_classificationCretaceousPaleontologyGroup (stratigraphy)FoothillsGeologyAzhdarchidaeGeological Magazine
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