Persona: Jordá Pardo, Jesús Francisco
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Jordá Pardo
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Jesús Francisco
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Publicación Un asentamiento neolítico de superficie en el interior de una cueva: Torca l’Arroyu (Llanera, Asturias, España)(Museo Arqueológico de Alicante- MARQ, 2008-09-04) Jordá Pardo, Jesús Francisco; Estrada García, Rogelio; Mestres Torres, Joan S.; Yraveda Sainz de los Terreros, José; Marín Suárez, CarlosEl yacimiento de la Torca L’Arroyu fue descubierto durante las obras de realización de la red de saneamiento del municipio de Llanera (Asturias, N de España). Es una pequeña cueva desarrollada en las calizas y margas del Cretácico superior rellena por sedimentos cuyo techo presenta una abertura tipo torca. El depósito tiene forma de cono cuyo vértice se encuentra bajo la torca y está formado por capas inclinadas depositadas a partir de los arrastres producidos en la ladera exterior, donde existió un asentamiento holoceno. En estos niveles se recogieron materiales cerámicos muy rodados, dos piezas líticas pulimentadas, abundantes restos óseos de animales consumidos y fragmentos carbonosos. Para situar los depósitos en el tiempo con precisión se dataron mediante radiocarbono dos muestras signifi cativas de los restos óseos asociados a las cerámicas y piezas pulimentadas y varios fragmentos de carbones de ese mismo nivel, así como carbones de un nivel superior. Las fechas ofrecidas por las muestras óseas del nivel inferior son: UBAR-803 4930+70 BP y UBAR-804 4240+60 BP. Las fechas proporcionadas por los carbones son: nivel inferior, UBAR-745 3190+150 BP, y nivel superior UBAR-746 2050+120 BP. Las dataciones de los huesos asociados a cerámicas nos indican la existencia en la ladera exterior de un asentamiento neolítico que pudo tener continuidad en el Calcolítico, cuyos materiales fueron arrastrados por la ladera y depositados en la cueva en una fecha muy posterior, como consecuencia del desarrollo de un incendio, proceso este que se repitió años después como atestigua la fecha más reciente. Las fechas obtenidas fueron sometidas a calibración dendrocronológica y se han comparado con las de otros yacimientos cantábricos de similar cronología.Publicación New data about the shellfish gathering during the Late Pleistocene in the Sella Valley(European Association of Archaeologists, 2023-08-30) Marchán, Alberto; Uribesalgo, Amaia; Cueto, Marián; Jordá Pardo, Jesús Francisco; Martínez Villa, Alberto; Tapia, Jesús; Álvarez Fernández, EstebanThis communication presents the results of the analysis of archaeomalacological remains from archaeological excavations in the Sella valley (Asturias, Spain). Shells from Tito Bustillo (Dwelling Area, SUs 101 to 104), Cova Rosa (Layers A0 to B11), La Lloseta (Clark Sector, Level VI) and El Cierro (Sala de la Natividad, Levels 3 and 4) have been studied. This analysis has been performed from a taxonomic, quantitative, taphonomic and biometric point of view. In the selected sample, species collected for their bromatological interest prevail (mainly Patella vulgata and Littorina littorea), although taxa of no food value have also been documented. Anthropic alterations have been detected in the shells, ranging from thermoalteration to fractures caused by limpet collection. The latter alteration has been identified by experimentation with current specimens. The results obtained in this study are compared with existing information on nearby sites, reflecting on the mobility of shellfishing groups in the Sella valley during the Magdalenian periodPublicación Antler management in the Sella Valley: an example through the osseous industry from the site of Cova Rosa(European Association of Archaeologists, 2023) Cerezo Fernández, R.; Pétillon, Jean-Marc; Cueto, Marian; Panero, Lucia; Portero,Rodrigo; Tapia, Jesús; Jordá Pardo, Jesús Francisco; Álvarez Fernández, EstebanThis communication introduces aspects of the management and transformation of deer antler by hunter-gatherer groups during the Cantabrian Magdalenian (17-14 Ka cal BP), and specifically in the Sella valley. Numerous Magdalenian sites are concentrated in this region, making the study of their material remains interesting to determine the potential particularities of a specific territory inhabited by human groups. To this end, more than a hundred remains of this raw material from the archaeological site of Cova Rosa (Asturias, Northern Spain) have been analyzed. The examination of these antler remains, from an anatomical, taxonomic, typological and technological point of view, has allowed us to distinguish several strategies for the collection and selection of the antler, as well as to reconstruct part of the "chaîne opératoire" of the manufacture of tools at this site. This study has also enabled us to introduce aspects of the use and recycling of the tools. Finally, through a bibliographical review of studies of the osseous industry in the Sella valley, we can confirm a relative homogeneity, at least topologically, of osseous tools in the archaeological record. Ultimately, this communication highlights the need for the inclusion of these methodological approaches in research on deer antler working during the Magdalenian period in the studied territoryPublicación 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, Pilar; Duarte, Carlos; Maestro, Adolfo; Maximiano, Alfredo; Molina, Juana; Obeso, Ramón; Colectivo Espeleológico L´Esperteyu Cavernícola Espeleo Club; Álvarez Fernández, EstebanThe 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 scalePublicación Geoarchaeology, chronostratigraphy and human occupation of the cental sector of the Cantabrian coast (North Iberia) during the Late Upper Pleistocene and Lower Holocene: The prehistoric sites of the Sella River estuary (Ribadesella,Asturias, Spain)(Sapienza University of Rome, 2023-07-14) Jordá Pardo, Jesús Francisco; Cabello Ligero, Lidia; Cueto, Marian; López Tascón, Cristina; Maestro, Adolfo; Martínez-VBilla, Alberto; Molina Salido, Juana; Tapia, Jesús; Álvarez Fernández, EstebanThe archaeological researchs that have been carried out in the last decade in the Sella river valley (central sector of the Cantabrian coast, North Iberia), in general, and in its stuary, in particular, are making it possible to specify the occupations of the groups of hunter-gatherers-shellsh gatherers who lived in southwestern Europe during the Upper Pleistocene and Lower Holocene. Thus, the review of the stratigraphies and archaeological materials from ancient excavations and the performance of new research projects at the classic sites located at the West bank of the stuary of Sella River (Cova Rosa, El Cierro, Les Pedroses, La Lloseta and Tito Bustillo) have made it possible to obtain new radiocarbon dating that allows us to specify the chronostratigraphic position of the dierent sequences while achieving a better understanding of the geological processes involved in the formation of these karstic deposits. In addition, the results of these investigations have made it possible to carry out a paleogeographic reconstruction of the coastline throughout the period between OIS 3 and OIS 1Publicación Arqueología y gas natural: el Paleolítico medio de El Barandiallu (Villabona, Llanera, Asturias central)(Array, 2004) Estrada García, Rogelio; Jordá Pardo, Jesús FranciscoSituado en el centro de Asturias, El Barandiallu (Villabona, Llanera) es un nuevo yacimiento al aire libre desarrollado en los depósitos de la terraza fluvial de +26/27 m del río Aboño, que ha proporcionado una colección de artefactos líticos atribuida tecnológicamente al Paleolítico Medio. Su localización fue posible gracias a los trabajos de seguimiento arqueológico realizados durante la construcción de un gasoducto de gas natural en los años 1.987-88. Presenta un gran interés, dado que en el contexto regional de la cornisa cantábrica no son frecuentes los sitios con materiales mesopaleolíticos incluidos en estratigrafías al aire libre.Publicación Torca l’Arroyu: A new holocene site in the centre of Asturias (North of Spain)(B.A.R., 2008-12-10) Estrada García, Rogelio; Jordá Pardo, Jesús Francisco; Mestres Torres, Joan S.; Yravedra Sainz de los Terreros, JoséThe archaeological site of Torca L’Arroyu was discovered in 2002 during the works of construction of the new net of sewer of Llanera’s municipality (province of Asturias, N of Spain). The archaeological deposit is placed inside a small cave and it has provided some ceramic fragments very rolled, two polished lithic pieces, abundant bones of animals consumed by man and charcoals. The archaeological materials and the 14C dates of the bones associated with the ceramics (UBAR-803 4930 ± 70 BP y UBAR-804 4240 ± 60 BP) indicate the existence of an settlement of certain duration that would correspond to the chronological frame of the regional Neolithic. Sites of this chronology are very scanty in the Cantabrian area, therefore, this new deposit will contribute to a better knowledge of the Neolithic in this zone of the Iberian Peninsula.