Search results for "Logica"

showing 10 items of 25541 documents

Muridae from the late Miocene site of Venta del Moro (Eastern Spain)

2016

AbstractMurids are usually the dominant faunas of the late Miocene and early Pliocene micromammal assemblages. The present work deals with the murid faunas of the well-known late Miocene locality of Venta del Moro, comprising over 2700 molars ascribed to the taxa Apodemus gorafensis, Occitanomys alcalai, Paraethomys meini and Stephanomys dubari. This list differs from those of previous studies by the presence of A. gorafensis instead of A. gudrunae. The presence of A. gudrunae in younger localities than Venta del Moro implies that both species, considered ancestor and descendant, coexisted for some time. In addition, the analysis of such an extensive collection has allowed us to check the v…

010506 paleontologybiologyFaunaLate Miocene010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesPaleontologyTaxonApodemusCharacter displacementGeneral Agricultural and Biological Sciences0105 earth and related environmental sciencesMuridaeAncestorHistorical Biology
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Tree-ring δ2H values from lignin methoxyl groups indicate sensitivity to European-scale temperature changes

2020

Abstract Stable hydrogen isotope ratios of lignin methoxyl groups (δ2HLM) of wood have been shown to reflect climate-sensitive δ2H values of precipitation (δ2Hprecip). However, a detailed calibration study between high-resolution δ2HLM and δ2Hprecip data 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 a station of the Global Isotope Network of Isotopes in Precipitation (GNIP) and the meteorological observatory at Hohenpeisenberg (Germany; ~48°N, 11°E). The nine δ2HLM tree-ring series show highly significant inter-series correlations (Rbar = 0.52) over the common period of overl…

010506 paleontologybiologyIsotopePaleontologyScale (descriptive set theory)010502 geochemistry & geophysicsOceanographybiology.organism_classificationAtmospheric sciences01 natural scienceschemistry.chemical_compoundchemistryFagus sylvaticaMeteorological observatoryDendrochronologyLigninPrecipitationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesChronologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Late Miocene remains from Venta del Moro (Iberian Peninsula) provide further insights on the dispersal of crocodiles across the late Miocene Tethys

2020

The dispersal of Crocodylus from Africa to Europe during the Miocene is not well understood. A small collection of cranial fragments and postcranial elements from the latest Miocene (6.2 Ma) site of Venta del Moro (Valencia, Spain) have previously been referred to Crocodylus cf. C. checchiai Maccagno, 1947 without accompanying descriptions. Here we describe and figure for the first time the crocodylian remains from Venta del Moro, which represent at least two individuals. Our comparisons indicate that this material clearly does not belong to Diplocynodon or Tomistoma - the only two other crocodylians described so far for the European late Miocene. The material is only tentatively referred t…

010506 paleontologybiologyPaleontologyPostcraniaLate Miocene010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesMediterranean BasinCrocodylusCretaceousPaleontologyGeographyBiological dispersalDiplocynodonGavialis0105 earth and related environmental sciencesJournal of Paleontology
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Population dynamics, social resilience strategies, and Adaptive Cycles in early farming societies of SW Central Europe

2017

Abstract Inferred European Holocene population size exhibits large fluctuations, particularly around the onset of farming. We attempt to find explanations for these fluctuations by employing the concept of cycling, especially that of the Adaptive Cycle. We base our analysis on chronologically and chorologically highly resolved ceramic and site data from the Linear Pottery culture (Germ. Linearbandkermik ) of the early Neolithic of southwestern Central Europe. Typological seriation with dendrochronological anchor dates provides the age model for these data. Ceramic motifs are analysed with respect to the temporally changing diversity in decoration. The temporal sequence of major decoration m…

010506 paleontologyeducation.field_of_study060102 archaeologyEcologymedia_common.quotation_subjectPopulation sizePopulationSeriation (archaeology)06 humanities and the artsBiology01 natural sciencesSocial dynamicsPopulation declineSocial system0601 history and archaeologyPsychological resilienceeducationhuman activities0105 earth and related environmental sciencesEarth-Surface ProcessesDiversity (business)media_commonQuaternary International
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Changing patterns of eastern Mediterranean shellfish exploitation in the Late Glacial and Early Holocene: Oxygen isotope evidence from gastropod in E…

2016

Abstract The seasonal pattern of shellfish foraging at the archaeological site of Haua Fteah in the Gebel Akhdar, Libya was investigated from the Epipaleolithic to the Neolithic via oxygen isotope (δ 18 O) analyses of the topshell Phorcus (Osilinus) turbinatus . To validate this species as faithful year-round palaeoenvironmental recorder, the intra-annual variability of δ 18 O in modern shells and sea water was analysed and compared with measured sea surface temperature (SST). The shells were found to be good candidates for seasonal shellfish forging studies as they preserve nearly the complete annual SST cycle in their shell δ 18 O with minimal slowing or stoppage of growth. During the ter…

010506 paleontologygeographyGBEpipaleolithicgeography.geographical_feature_category060102 archaeologybiologyPleistoceneArchaeological record06 humanities and the artsbiology.organism_classificationCC01 natural sciencesOceanographyRefugium (population biology)Cave13. Climate actionPhorcus0601 history and archaeology14. Life underwaterGlacial periodHoloceneGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Subglacial topography and thickness of ice caps on the Argentine Islands

2019

AbstractThis study presents the first subglacial topography and ice thickness models of the largest ice caps of the Argentine Islands, Wilhelm Archipelago, West Antarctica. During this study, ground-penetrating radar was used to map the thickness and inner structure of the ice caps. Digital surface models of all studied islands were created from aerial images obtained with a small-sized unmanned aerial vehicle and used for the construction of subglacial topography models. Ice caps of the Argentine Islands cover ~50% of the land surface of the islands on average. The maximum thickness of only two islands (Galindez and Skua) exceeds 30 m, while the average thickness of all islands is only ~5 …

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeologyGlacierOceanography01 natural sciencesGeological structureIce thicknessPrevailing windsArchipelagoIce capsDigital surfaceGeomorphologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesAntarctic Science
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Breaking the waves: Human use of marine bivalves in a microtidal range coast during the Upper Pleistocene and the Early Holocene, Vestíbulo chamber, …

2016

Abstract This paper presents the results obtained from the study of the bivalves recovered during the archaeological excavations in the Vestibulo chamber of Nerja Cave (Malaga, southern Spain) carried out by Professor Francisco Jorda Cerda between 1983 and 1987. These excavations recovered the archaeological record of the sequence from the Gravettian to the Neolithic. The mollusc remains from the Vestibulo chamber of Nerja Cave record constitute an extraordinary collection, composed of more than 136000 specimens which correspond to more than 78 kg. In this work, only marine bivalves were studied. The bivalve remains are more than 124000 specimens, corresponding to more than 65 kg from 31 ta…

010506 paleontologygeographygeography.geographical_feature_category060102 archaeologyPleistoceneRange (biology)Archaeological recordExcavation06 humanities and the arts01 natural sciencesArchaeologyMiddenPaleontologyHuman useCave0601 history and archaeologyHoloceneGeology0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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Sea–land geology of Marettimo (Egadi Islands, central Mediterranean sea)

2016

We present a 1:10,000 scale geological map of Marettimo Island and its offshore (Egadi Archipelago, central Mediterranean Sea). The map was achieved by integrating a new geological survey with data from recent, marine, geological and geophysical surveys acquired along the adjacent continental shelf. The island is composed of a Mesozoic, mostly carbonate platform succession, which is overlain by continental to coastal marine Quaternary deposits. Extensional tectonics have affected the carbonate platform since the Late Triassic producing an initial increase of accommodation space that was filled by interbed breccias, marls and calcareous marls. During the Jurassic, a NE-SW-directed normal fau…

010506 paleontologygeographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaContinental shelfCarbonate platformSettore GEO/03 - Geologia StrutturaleGeography Planning and Developmentstratigraphy010502 geochemistry & geophysics01 natural sciencestectonicPaleontologyTectonicsMediterranean seaArchipelagoMarlEarth and Planetary Sciences (miscellaneous)Egadi IslandExtensional tectonicsGeological surveyGeological Map geological survey stratigraphy tectonics Egadi IslandsQuaternaryGeology0105 earth and related environmental sciences
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Regional Tectonic Setting and Geological Structure of the Rhenish Massif

1983

This chapter contains an outline of the geological history of the Rhenish Massif and the development of its margins and surrounding areas. Section 2.2 gives some main aspects of the development of the Variscan geosyncline and orogeny and a short description of the pre-Variscan geological history of this region. Since the end of the Variscan orogeny many different epeirogenetic processes have occurred here (Sect. 2.3). During these long geological times uplift and subsidence changed in the different parts of the Massif and in the surrounding areas.

010506 paleontologygeographygeography.geographical_feature_categorySubsidenceOrogenyMassifGeosyncline010502 geochemistry & geophysics01 natural sciencesCoast lineGeological structurePaleontologyTectonicsSection (archaeology)PetrologyGeology0105 earth and related environmental sciences
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Soil physicochemical and microbial drivers of temperature sensitivity of soil organic matter decomposition under boreal forests

2020

Abstract Soil organic matter (SOM) in boreal forests is an important carbon sink. The aim of this study was to assess and to detect factors controlling the temperature sensitivity of SOM decomposition. Soils were collected from Scots pine, Norway spruce, silver birch, and mixed forests (O horizon) in northern Finland, and their basal respiration rates at five different temperatures (from 4 to 28 °C) were measured. The Q10 values, showing the respiration rate changes with a 10 °C increase, were calculated using a Gaussian function and were based on temperature-dependent changes. Several soil physicochemical parameters were measured, and the functional diversity of the soil microbial communit…

0106 biological sciences$Q_{10}$ metabolic coefficientQ10Soil ScienceSoil scienceglobal warmingcomplex mixtures010603 evolutionary biology01 natural sciences$CO_{2}$ evolutionbiologySoil organic matterTaigaScots pineCarbon sink$MicroResp^{TM}$04 agricultural and veterinary sciencesbiology.organism_classificationEnvironmental chemistrySoil watermicrobial functional diversity040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSoil horizonMicroResp™Q10 metabolic coefficientRespiration rateCO2 evolutionPedosphere
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