Persona: Jordá Pardo, Jesús Francisco
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0000-0002-3937-9199
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Jordá Pardo
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Jesús Francisco
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Publicación Geoarchaeology and Chronostratigraphy of the Middle-Upper Palaeolithic transition at the cave of La Güelga (Cangas de Onis, Asturias, Spain).(A. Pastoors y B. Auffermann, 2013-05-16) Carral Gonzalez, Pilar; Wood, Rachel; Jordá Pardo, Jesús Francisco; Menéndez Fernández, Mario; Quesada López, José Manuel; https://orcid.org/0000-0002-6289-691XThe cave of La Güelga (Asturias, Spain) is located in the eastern region of the Asturian Massif within the carboniferous limestones of the Calizas de Montaña. A small river runs through the cave, and this has formed several marks on the walls and terraces at the cave entrance. This cavity is large and has the morphology of a rock shelter. In one terrace, an Upper Pleistocene deposit containing archaeological and palaeontological remains from the Middle to Upper Palaeolithic transition has been excavated. These deposits have been AMS dated at the Oxford Radiocarbon Accelerator Unit (ORAU). Bones were pretreated using the ultrafiltration protocol, which aims to purify the collagen selected for dating by removing contaminants. In many cases, dates on collagen processed in this way are significantly older than those where collagen has not been ultrafiltered. The new dates place the lower deposits from zone D between 55,710 – 44,940 years cal BP, during OIS 3c.Publicación Excavaciones arqueológicas en la Cueva de La Güelga.(Cangas de Onís. Asturias).(2011-11-30) Carral Gonzalez, Pilar; Trancho, Gonzalo; Álvarez Alonso, David; Rojo Hernández, Julio Antonio; Wood, Rachel; Menéndez Fernández, Mario; Quesada López, José Manuel; Jordá Pardo, Jesús Francisco; Gómez García, Eduardo; https://orcid.org/0000-0002-6289-691XPublicación Procesos sedimentarios y diagenéticos en el registro arqueológico del yacimiento pleistoceno de la cueva de El Esquilleu (Picos de Europa, Norte de España).(2008) Baena Preysler, Javier; Carral Gonzalez, Pilar; García Guinea, Javier; Correcher, V.; Yravedra Sainz de los Terreros, José; Jordá Pardo, Jesús Francisco; https://orcid.org/0000-0002-6289-691XJordá Pardo, J.F., Baena Preysler, J., Carral González, P., García-Guinea, J., Correcher Delgado, V. e Yravedra Sainz de los Terreros, J. (2008): Procesos sedimentarios y diagenéticos en el registro arqueológico del yacimiento pleistoceno de la cueva de El Esquilleu (Picos de Europa, Norte de España). Cuaternario y Geomorfología, 22 (3-4), 2008, 31-46. I.S.S.N.: 0214-1744Publicación Retorno a Cova Rosa. Nuevas investigaciones geoarqueológicas en el yacimiento del Pleistoceno superior de Cova Rosa(Universidad el Pais Vasco, 2021-07-05) Jordá Pardo, Jesús Francisco; Álvarez Alonso, David; Alvarez-Fernandez, Esteban; Andrés Herrero, María de ; Arias, Pablo; Bécares Pérez, Julián; Carral Gonzalez, Pilar; et al.; López González, Nieves; Pérez López, Alberto; Cambeses Torres, Aitor; https://orcid.org/0000-0003-0481-7563; https://orcid.org/0000-0002-6289-691XLa cavidad kárstica de Cova Rosa (Sardéu, Ribadesella, Asturias), abierta en las calizas de La Escalada (Moscoviense, Carbonífero), contiene una importante secuencia arqueosedimentaria excavada durante la segunda mitad del siglo XX por Jordá Cerdá y Gómez Fuentes (1982) con niveles del Solutrense, Magdaleniense y Mesolítico, estudiada sedimentológicamente por Hoyos Gómez (1979). En los últimos años los miembros de un amplio equipo de investigación estamos trabajando de nuevo sobre este yacimiento y sus materiales (Álvarez-Fernández y Jordá Pardo, 2018) y en este trabajo presentamos la secuencia estratigráfica que ha sido estudiada de nuevo con metodología geoarqueológica.Publicación Geomorphology, Geoarchaeology, and Geochronology of the Upper Pleistocene Archaeological Site of El Olivo Cave (Llanera, Asturias, Northern Spain)(MDPI, 0023-10-07) Jordá Pardo, Jesús Francisco; Álvarez Alonso, David; Andrés Herrero, María de; Ballesteros, Daniel; Carral Gonzalez, Pilar; Hevia Carrillo, Aitor; Sanjurjo, Jorge; Giralt, Santiago; Jiménez Sánchez, Montserrat; https://orcid.org/0000-0002-6289-691XEl Olivo Cave (Pruvia de Arriba, Llanera, Asturias, Spain) is a small karst cave located in the Aboño River basin and formed in the Cretaceous limestone of the Mesozoic cover of the Cantabrian Mountains (north of the Iberian Peninsula). It contains an important upper Pleistocene sedimentary, archaeological, and paleontological record, with abundant technological evidence and faunal remains. The archaeological record shows a first occupation that could correspond to the Middle Paleolithic and a second occupation in the Middle Magdalenian. The stratigraphic sequence inside and outside the cave was studied with geoarchaeological methodology. In this paper, the lithostratigraphic sequence is analyzed, and the data from the granulometric, mineralogical, edaphological, and radiometric analyses are presented. The results of these analyses enable an accurate interpretation of both the lithostratigraphy of the deposit and the processes responsible for its formation and subsequent evolution. The available numerical dates allow us to locate the first sedimentation episode in the cave in OIS 7a, in the Middle Pleistocene, the base of the outer fluvial sedimentation in the cold OIS 3a stage of the Upper Pleistocene and the Magdalenian occupation in the Last Glacial Maximum (OIS 2) at the end of the Late PleistocenePublicación Cova Rosa revisited. New geoarchaeological research at the Upper Pleistocene – Lower Holocene site of Cova Rosa (Sardéu, Ribadesella, Asturias, Spain)(2022-09-12) Jordá Pardo, Jesús Francisco; Carral Gonzalez, Pilar; Duarte, Carlos; Maestro, Adolfo; Maximiano, Alfredo; Molina, Juana; Obeso, Ramón; Colectivo Espeleológico L´Esperteyu Cavernícola Espeleo Club; Alvarez-Fernandez, Esteban; https://orcid.org/0000-0002-6289-691XThe karstic cavity of Cova Rosa (Sardéu, Ribadesella, Asturias), developed in the La Escalada limestones (Moscovien, Carboniferous), contains an important archaeosedimentary sequence covering the Late Upper Pleistocene and the Lower Holocene. This sequence, excavated during the second half of the 20th century by Jordá Cerdá and Gómez Fuentes (1982), presents levels of Solutrense, Lower and Upper Magdalenian and Mesolithic. The sequence was studied sedimentologically by Hoyos Gómez (1979). In the last years members of a large research team are working again on this site and its materials (Álvarez-Fernández and Jordá Pardo, 2018) and in this contribution we present the new lithostratigraphic sequence that has been studied again with geoarchaeological methodology. In addition, thanks to the 22 radiocarbon dates obtained (Álvarez-Alonso et al., 2021), we can place the sequence on the Quaternary chronostratigraphic scale