Search results for "peninsula"

showing 10 items of 293 documents

The Ventian mammal age (Latest Miocene): present state

2013

[EN] The Ventian land mammal age includes most of the Spanish faunas assigned to the biochronologic unit MN 13. It is correlatable with the Messinian, although it may include, in its latest part, Early Pliocene faunas. We propose that the Ventian begins with the fi rst occurrence of the Muridae genus Stephanomys (7 Ma, paleomagnetic dating from El Bunker, Teruel basin), well recorded in Teruel basin, and ends with the appearance of Promimomys (ca. 5 Ma), also registered in the Teruel basin. We suggest a new reorganization of the Ventian. The first subdivision corresponds to the zone M (Dam et al., 2001). The second, zone N, is proposed here for the first time, being equivalent to the zone w…

PaleomagnetismCuencas continentalesMessiniensePaleontologyContinental basinsBiochronologyStructural basinPenínsula IbéricaArchaeologyQE701-760PaleontologyLa edad de mamíferos ventienses (Mioceno terminal): estado actualGeographyGenusMessinianestado actual [La edad de mamíferos ventienses (Mioceno terminal)]MammalBiocronologíabiochronology iberian peninsula continental bassin messinianIberian Peninsula
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First Early Pliocene micromammal faunas from Venta del Moro (Cabriel Basin, Spain) : new data on the Messinian dispersal of Debruijnimys

2021

The localities of La Bullana 3 and LA Bullana 2B (Valencia, E Spain) have yielded remains of Apodemusgorafensis, Paraethomys aff. abaigari, Stephanomys dubari, Apocricetus barrierei, Sciuridae indet. and Asoriculus cf. gibberodon the former, and Apodemusgorafensis, Paraethomys aff. abaigari, Stephanomys dubari, Apocricetus barrierei, Sciuridae indet., Asoriculus cf. gibberodon, Castillomysgracilis, Occitanomysbrailloni, Occitanomys sp., Paraethomys meini, Ruscinomys sp., Eliomys intermedius, Debruijnimys cf. julii and Atlantoxerussp. the latter. Based on the study of these micromammal assemblages, we propose an Early Pliocene age (MN14) for both sites. The pres-ence a gerbilid related to De…

Paleomagnetismgeographygeography.geographical_feature_categoryRange (biology)StratigraphyFaunaCordilleras IbéricasGeologyRodentiaStructural basinNeogeneNeógenoPaleontologyTaxonPeninsulaRuscinianRuscinienseBiological dispersalNeogenePenísula IbéricaIberian RangesDebruijnimysGeologyIberian Peninsula
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New bradorid arthropods from the Lower Cambrian of Spain

2007

Lower Early Cambrian rocks of the Pedroche Formation in the Sierra de Cordoba consist of well-exposed mixed facies with abundant fossil assemblages showing long stratigraphical ranges. These assemblages include diverse Ovetian archaeocyaths, trilobites, small shelly fossils, calcimicrobia, trace fossils, and stromatolites. For the ostracod-like Cambriidae it is the first record from the Iberian Peninsula. Cordubiella pedrochensis n.gen. n.sp. comes from two sections of the lower Pedroche Formation: the Arroyo de Pedroche 1 sec- tion, and the Arroyo Pedroche 2 section. The material was collected in the zone of Lemdadella perejoni, of lower Ovetian age and below the Eoredlichia FAD. It supple…

Paleontologygeographygeography.geographical_feature_categoryEoredlichiabiologyPeninsulaLemdadellaFaciesPaleontologyTrace fossilbiology.organism_classificationGeologyMicropaleontology
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Quaternary pollen analysis in the Iberian Peninsula: the value of negative results

2009

Most unsuccessful palynological work is never published. As a consequence, pollen analysts waste time re-processing sterile sediments, and the available literature exhibits a uniformly positive record of success in pollen extraction. Here we report failures with Quaternary pollen analyses in the Iberian Peninsula; that is, case studies where it was not possible to extract palynomorphs for pollen counting. Both totally sterile and partially sterile sites are considered. Sites and perspectives for future studies are suggested. The majority of the failed studies are openair archaeological and palaeontological sites, caves and rockshelters, but there are prominent cases of success. Peat bogs ha…

PalynologyArcheologygeographygeography.geographical_feature_categoryTaphonomytaphonomyarchaeologymedicine.disease_causeQuaternaryPaleontologyPeninsulaPollenmedicinelcsh:Archaeologynegative resultsIberialcsh:CC1-960QuaternarypalynologyValue (mathematics)GeologyInternet Archaeology
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Large- and small-mammal distribution patterns and chronostratigraphic boundaries from the Late Pliocene to the Middle Pleistocene of the Italian peni…

2007

Abstract Over the last 50 years the studies on terrestrial mammals of the Italian peninsula have provided a large volume of data and a more detailed knowledge of faunal events during the Late Pliocene and Quaternary. Moreover geological, sedimentological, palynological and magnetostratigraphical investigations on the Pliocene–Pleistocene continental sedimentary basins have yielded the possibility of a detailed calibration of the faunal successions. Thus, palaeontologists have been able to reconstruct faunal sequences and to propose biochronological scales based on large and small mammals, respectively. In the present contribution an integration of the two biochronological scales is proposed…

Palynologygeographygeography.geographical_feature_categoryPleistocenechronostratigraphical boundariesSmall mammalSedimentary basinIntegrated approachLate Pllioce-Middle PleistoceneLarge and small mammals; distribution patterns; chronostratigraphical boundaries; Late Pllioce-Middle Pleistocene; Italian peninsuladistribution patternsSequence (geology)PaleontologyPeninsulaPleistocene mammals bio-chronology ItalyQuaternaryGeologyLarge and small mammalsItalian peninsulaEarth-Surface Processes
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La otra cara del Dios, Patria y Rey: violencia y destrucción en Valencia durante la Guerra de la Independencia.

2016

There are so many reasons why the Peninsular War (1808-1814) is one of a kind chapter of our history. The deep politicization of the city of Valencia during this conflict explains the existence of cruel and violent episodes. These ones weren’t forgotten, but of course they were properly overcome through the years by other expressions of patriotism and heroism. So, the goal of this paper is to examine and think about the artistic expression of these violent events, their functions, evolution and, in conclusion, their lives. Son diversos y pródigos los factores que contribuyen a definir la Guerra de la Independencia española (1808-1814) como uno de los episodios más únicos de nuestra historia…

Peninsular War Valencia engraving violence architecture painting.Guerra Independencia Valencia estampa violencia arquitectura pintura.Settore L-ART/03 - Storia Dell'Arte Contemporanea
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Pleistocene Calabrian and Sicilian bioprovinces

2002

During the Pleistocene, southern Calabria was the area through which several mammalian taxa dispersed into the Sicilian island via the Straits of Messina. The rich fossil record of Sicily allowed for the construction of a fairly detailed bio-chronological frame that is dated by correlation of vertebrate bearing deposits with marine deposits. At present five Faunal Complexes (F.C.), characterised by the occurrence of different taxa, have been recognised. The two older Faunal Complexes (Monte Pellegrino F.C.'xes Elephas falconeri F.C.) include taxa with differently marked endemic features denoting the occurrence of an insular system made up of geographically isolated small islands, with very …

PleistoceneStratigraphyFaunaPopulationPaleobiogeographyElephasPeninsulaeducationSicilyEndemic faunaeducation.field_of_studygeographygeography.geographical_feature_categorybiologyEcologyPaleontologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationPleistocene vertebratelanguage.human_languageSpace and Planetary SciencelanguageBiological dispersalMammalSicilianGeologyGeobios
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Late Pliocene and Pleistocene small mammal chronology in the Italian peninsula

2007

The abundant documentation of small mammals in the Italian peninsula, collected over recent years, furnishes a detailed biochronological sequence mainly from the Late Pliocene onwards. An updated stratigraphic framework is here presented, based on the European small mammal biozonation. The Early Villanyian is characterized by Mimomys hassiacus, M. stehlini, and, later, poorly documented M. polonicus. The Late Villanyian localities are well characterized with M. pliocaenicus, M. pitymyoides and M. tigliensis. The older part of the Early Biharian is documented by assemblages containing Microtus (Allophaiomys) ex gr. pliocaenicus, M. pusillus, M. cf. ostramosensis and M. tornensis, while the l…

PliocenePleistoceneRodentbiochronologyEcological successionSmall mammals; Italy; Pliocene; PleistoceneSmall mammals; Late Plioce-Pleistocene; biochronology; Italian peninsulaSmall mammalLate Plioce-PleistoceneSequence (geology)Peninsulabiology.animalPliomysSmall mammalsMicrotusEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyEcologybiology.organism_classificationPleistoceneItalyItalian peninsulaGeologyChronologyQuaternary International
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THE PLEISTOCENE–HOLOCENE TRANSITION IN THE IBERIAN PENINSULA: CONTINUITY AND CHANGE IN HUMAN ADAPTATIONS

1998

Abstract Data obtained from recent excavations (as well as from selected older excavations) are used to outline the principal environmental, technological and economic aspects of the Pleistocene–Holocene transition in three distinct regions of the Iberian Peninsula: Portugal, Cantabrian and Mediterranean Spain. The period covered extends from the terminal Paleolithic Magdalenian period to the initial Neolithic. Despite proximity to SW France and many similarities with that classic prehistoric culture area in terms of artistic/symbolic expression and technology, the Iberian regions show significant differences, especially in terms of subsistence strategies and their development during the Ta…

PrehistoryReinterpretationGeographygeography.geographical_feature_categoryPleistocenePeninsulaPeriod (geology)Subsistence agricultureMagdalenianArchaeologyHoloceneEarth-Surface ProcessesQuaternary International
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Roman quarries of the Iberian Peninsula: "Anasol" and "Anasol-type".

2007

The Iberian peninsula is rich in marble, both white and coloured, of excellent quality, used in the past (Pliny NH, XXXVI, II) and also at the present time as material for building and decoration. Many types of these marbles are similar to some, better known, Greek, Italian, Egyptian and Asian marbles. During the Roman Empire “ marmor carystium ” was extensively used. Taking into account the great similarity of this marble with the “ anasol ” and “ anasol ”-types mined in Spain and Portugal, this work presents a minero-petrographic, chemical and geochemical characterisation of these lithotypes, aiming at finding parameters to distinguish them from the better-known Greek and Italian “ cipoll…

ProvenanceDolomitearchaeometric implicationspetrographyAnasol Archeometric implications Geochemistry Petrography Potugal Roman quarry SpainPetrographyType (biology)Mining engineeringGeochemistry and PetrologyPeninsulaspainanasolMetamorphic faciesgeochemistrygeographygeography.geographical_feature_categorypotugalanasol; archaeometric implications.; archeometric implications; geochemistry; petrography; portugal; potugal; roman quarry; spainportugalroman quarryArchaeologylanguage.human_languageRoman Empirearcheometric implicationslanguagePortugueseGeology
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