0000000001092594

AUTHOR

Luis Gibert

showing 7 related works from this author

Chronology for the Cueva Victoria fossil site (SE Spain): Evidence for Early Pleistocene Afro-Iberian dispersals

2014

Cueva Victoria has provided remains of more than 90 species of fossil vertebrates, including a hominin phalanx, and the only specimens of the African cercopithecid Theropithecus oswaldi in Europe. To constrain the age of the vertebrate remains we used paleomagnetism, vertebrate biostratigraphy and (230)Th/U dating. Normal polarity was identified in the non-fossiliferous lowest and highest stratigraphic units (red clay and capping flowstones) while reverse polarity was found in the intermediate stratigraphic unit (fossiliferous breccia). A lower polarity change occurred during the deposition of the decalcification clay, when the cave was closed and karstification was active. A second polarit…

Theropithecus010506 paleontologyEarly PleistocenePleistoceneved/biology.organism_classification_rank.speciesBiostratigraphy010502 geochemistry & geophysics01 natural sciencesTheropithecusPaleontologyAfrica NorthernCaveAnimalsEcology Evolution Behavior and SystematicsMagnetostratigraphy0105 earth and related environmental sciencesMammalsgeographygeography.geographical_feature_categoryFossilsved/biologyHominidaeBiological EvolutionCavesSpainAnthropologyAnimal MigrationTheropithecus oswaldiGeologyAcheuleanJournal of Human Evolution
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Speleothem δ13C record suggests enhanced spring/summer drought in south-eastern Spain between 9.7 and 7.8 ka – A circum-Western Mediterranean anomaly?

2019

South-eastern Spain is one of the driest regions in Europe and thus, prone to drought. Terrestrial climate records covering the late Glacial and Holocene from this area are sparse. Here, we present a flowstone record from Cueva Victoria, south-eastern Spain, which covers the late Glacial (15 ka) to the mid-Holocene (7 ka) including the Younger Dryas (YD). Between the onset of the Bølling/Allerød (B/A) and the early Holocene, flowstone δ18O values progressively decrease in accordance with sea-surface temperatures in the Alboran Sea, indicating an increase in precipitation in south-eastern Spain and a supra-regional signal of North Atlantic temperature change. At the same time, decreasing δ13…

Mediterranean climateArcheologyGlobal and Planetary Changegeographygeography.geographical_feature_categoryEcologyδ13CAnomaly (natural sciences)PaleontologySpeleothemOceanographySpring (hydrology)Glacial periodGeologySouth easternHoloceneEarth-Surface ProcessesThe Holocene
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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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Western Mediterranean Climate Response to Dansgaard/Oeschger Events: New Insights From Speleothem Records

2019

The climate of the western Mediterranean was characterized by a strong precipitation gradient during the Holocene driven by atmospheric circulation patterns. The scarcity of terrestrial paleoclimate archives has precluded exploring this hydroclimate pattern during Marine Isotope Stages 5 to 3. Here we present stable carbon and oxygen isotope records from three flowstones from southeast Iberia, which show that Dansgaard/Oeschger events were associated with more humid conditions. This is in agreement with other records from the Iberian Peninsula, the Mediterranean, and western Europe, which all responded in a similar way to millennial‐scale climate variability in Greenland. This general incre…

Mediterranean climategeographygeography.geographical_feature_categoryIsòtopsPrecipitacions (Meteorologia)Speleothem550 GeowissenschaftenPrecipitations (Meteorology)GeophysicsOceanography550 Earth sciencesIsotopesClima mediterraniGeneral Earth and Planetary SciencesMediterranean climateGeology
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Architecture and tectono-stratigraphic evolution of the intramontane Baza Basin (Bétics, SE-Spain): Constraints from seismic imaging

2017

The Baza basin is a large Neogene intramontane basin in the Bétic Cordillera of southern Spain that formed during the Tortonian (late Miocene). The Bétic Cordillera was produced by NW–SE oblique convergence between the Eurasian and African Plates. Three seismic reflection lines (each 18 km long; vibroseis method) were acquired across the Baza basin to reveal the architecture of the sedimentary infill and faulting during basin formation. We applied rather conventional CDP data processing followed by first arrival P-wave tomography to provide complementary structural information and establish velocity models for the post-stack migration. These images show a highly asymmetric structure for the…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesOutcropBaza BasinLate MioceneStructural basinFault (geology)010502 geochemistry & geophysicsNeogene01 natural sciencesBack-strippingBasin structurePaleontologyGeophysicsBasement (geology)Betic CordilleraReflection seismic imagingSedimentary rockNeogeneGeologySeismology0105 earth and related environmental sciencesEarth-Surface ProcessesFault system
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Evidence for an African-Iberian mammal dispersal during the pre-evaporitic Messinian

2013

The accurate timing of biogeographic dispersal can be determined by examining the age of fossiliferous strata on either side of a physical barrier. Here we show that African mammals migrated to Iberia and European mammals migrated to North Africa at the same time before isolation of the Mediterranean Sea during the Messinian. The fossil site of Venta del Moro (Spain) exhibits western Europe’s most complete vertebrate fauna for the latest Miocene. Its uniquely cosmopolitan assemblage is evidence of faunal dispersals from Africa and Asia to Europe during the latest Miocene glaciation. A preliminary paleomagnetic study suggested an age of 5.8 Ma for this site, but our expanded magnetostratigra…

Mediterranean climatePaleontologyPaleomagnetismMediterranean seaEphemeral keyBiological dispersalGeologyGlacial periodNeogeneGeologyMagnetostratigraphyGeology
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Supplement_Budsky – Supplemental material for Speleothem δ13C record suggests enhanced spring/summer drought in south-eastern Spain between 9.7 and 7…

2019

Supplemental material, Supplement_Budsky for Speleothem δ13C record suggests enhanced spring/summer drought in south-eastern Spain between 9.7 and 7.8 ka – A circum-Western Mediterranean anomaly? by Alexander Budsky, Denis Scholz, Jasper A Wassenburg, Regina Mertz-Kraus, Christoph Spötl, Dana FC Riechelmann, Luis Gibert, Klaus Peter Jochum and Meinrat O Andreae in The Holocene

HistoryGeography
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