Papers by María de Andrés Herrero
PLOS ONE
This paper investigates the correlation between climate, environment and human land use in the We... more This paper investigates the correlation between climate, environment and human land use in the Westernmost Mediterranean on both sides of the Strait of Gibraltar during the Late Glacial. Using a multi-proxy approach on a sample of 300 sites from the Solutrean and Magdalenian of the Iberian Peninsula and from the Iberomaurusian in Morocco, we find evidence for significant changes in settlement patterns and site density after the Last Glacial Maximum. In Southern Iberia, during Heinrich Stadial 1, hyperarid zones expanded drastically from the southeastern coast to the West through the Interior. This aridification process heavily affected Magdalenian settlement in the South and caused a strong decline of hunter-gatherer population. Southern Iberia during Heinrich Stadial 1 turned out to be a high-risk environment when compared to Northern Iberia. At the same time, the Late Iberomaurusian of Morocco, although considered to be situated in a high-risk environment as well, experiences an increase of sites and expansion of settlement area.
BOLETÍN GEOLÓGICO Y MINERO
The archaeological sequence of the Palaeolithic site of La Güelga apparently shows an interstrati... more The archaeological sequence of the Palaeolithic site of La Güelga apparently shows an interstratification of Aurignacian between the Mousterian and Châtelperronian layers, a sequence which disagrees with the stratigraphic model for the Middle to Upper Palaeolithic transition in SW-Europe. We analyzed the witness section of the interior sector in archaeological zone D using micromorphology and collected new radiocarbon dates for the Aurignacian and presumably Châtelperronian levels in order to provide detailed sediment descriptions of the site and scrutinize the presumed interstratification. Thin sections from Mousterian levels 8 and 9 show microstratification, signs of trampling and preferential sub-horizontal orientation of elongated particles. These features are less strongly developed in the Aurignacian deposit of levels 5 and 6 and are lacking in the presumably Châtelperronian ones of levels 1 and 2. The deposits of the latter show other features of reworked slope deposits such as a randomized distribution of limestone clasts. Radiocarbon dating on bone samples from level 2 places this layer to between ~41.5 and 45 ka cal BP, hence older than Aurignacian level 5, dated to between ~35.5 and 41.5 ka cal BP. Comparative dating of bones with and without ultrafiltration pretreatment conducted in two different laboratories yielded results in excellent agreement. Overall, the micromorphological observations and new radiocarbon ages strongly suggest that the few finds of presumably Châtelperronian affinity and sediments of levels 1 and 2 were transported by slope processes into the shelter.
Remote Sensing
This paper is focused on the Middle Paleolithic rock shelter called “Abrigo de San Lázaro”, place... more This paper is focused on the Middle Paleolithic rock shelter called “Abrigo de San Lázaro”, placed in the Eresma River valley (Segovia, Spain). In this area, a multisource geomatic approach is used. On the one hand, the external envelope of the shelter has been digitalized by the means of an efficient combination between aerial photogrammetry and laser scanning (static and mobile). On the other hand, the ground penetrating radar and the electric tomography were used with the aim of evaluating the inner disposition of the shelter. The combination of both digitalization (external and internal) has allowed for improving the knowledge of the site characteristics that, in turn, will facilitate the future excavation works. The results of these studies allow archaeologists to know new data for a better understanding of the site formation (geology of the site, sedimentary potential, rock shelter dimensions, etc.) and the events that took place in it (knowing its historical evolution, especi...
Quaternary Research
The timing of the late Middle Paleolithic and late disappearance of Neanderthals in the Iberian P... more The timing of the late Middle Paleolithic and late disappearance of Neanderthals in the Iberian Peninsula are hotly debated subjects in Paleolithic archeology. Several studies suggested a late survival in South and Central Iberia until about 32 ka, but were probably subject to significant age underestimation due to contamination of dating samples, undiagnostic lithic assemblages, and/or lack of stratigraphic integrity. We conducted a radiocarbon and luminescence-dating study backed by detailed sedimentological and micromorphological investigations at the newly discovered rock shelter sequence of Abrigo del Molino (Central Spain). Accumulation of the sediment sequence was rapid. It started with deposition of paleoflood slack-water deposits at around 48 ka and continued until about 41 ka with deposition of colluvial and detrital sediments. These contain two Mousterian levels, which place the latest Neanderthal occupation at around 45 to 41 ka, i.e., between Heinrich Stadials 5 and 4, ...
Quaternary International
La Güelga cave is located at the bottom of a mountain valley in the Eastern part of Asturias (Nor... more La Güelga cave is located at the bottom of a mountain valley in the Eastern part of Asturias (Northern Spain), 186 m above sea level and 15 km far away from the coast. It currently comprises a group of caves that were occupied during the Middle and Upper Paleolithic periods (MP and UP respectively). In recent years, we have studied the levels of La Güelga cave –D Zone-proposing a sequence for the MP/UP transition: Mousterian-Aurignacian-Châtelperronian, which we review in this paper after a detailed analysis of the chronostratigraphy. We also provide new radiocarbon dates for the Mousterian, Aurignacian and Châtelperronian levels. Finally, the geoarchaeology, taphonomy, archaeological data, and chronology suggest that the interstratification -initially identified on the basis of stratigraphic observations during excavation-cannot be maintained. In any case, the stratigraphy of the internal D Zone of La Güelga cave is one of the most interesting from the Cantabrian region for analyzing the last phases of the Mousterian and the rise of the Aurignacian in the North of the Peninsula.
ISPRS International Journal of Geo-Information, 2017
The overall objective of this work is to apply GIS-based cost distance modeling (CDM) to site cat... more The overall objective of this work is to apply GIS-based cost distance modeling (CDM) to site catchment modeling and analysis of prehistoric (Solutrean) sites in Andalusia. The implementation of a GIS-method for slope-based CDM was explained in detail, so that it can be replicated easily in future studies. Additional cost components, vegetation and stream networks, were included in the method. The presented CDM approach uses slope rasters as input data, which were derived from digital elevation models (DEMs). Various DEMs that differ in cell size, accuracy and other characteristics can be applied to this method. Thus, a major goal of this work is to investigate the influence different publicly available DEMs (SRTM, ASTER GDEM, EU-DEM, official 5-m/10-m cell size DEMs) have on the results of GIS-based CDM. While the investigation was conducted on sites from different chronocultural periods, a case study was performed on Solutrean sites in order to test the CDM approach by producing actual results and then comparing and interpreting them from an archaeological perspective. The results of the DEM evaluation with resampled horizontal resolutions show a clear influence of the DEM cell size on the modeled catchment area sizes. The investigation also indicates that this influence can be superimposed by other factors, such as noise and residuals of filtered anthropogenic features, when using DEMs of different origins.
Quaternary International, 2016
The Abrigo del Molino archaeological site is located in the Eresma river valley, near Segovia cit... more The Abrigo del Molino archaeological site is located in the Eresma river valley, near Segovia city (Central Spain). It consists of a shallow cave of fluvio-karstic origin, which has been completely filled in with detrital deposits. Geoarchaeological interpretation of its genesis differentiates three groups: a lower group with sandy loams and fine sands interbedded with pebble and gravel layers deposited by palaeofloods and slope contributions respectively; a middle group with massive silts and grain-supported boulders, formed by alternating contributions from the overlying slope as well as karst mudflows and rockfall from the shelter roof; and an upper group of silt cemented by carbonates, final backfill alteration and degradation of the host rock. The techno-typological characteristics of the lithic assemblage confirm the existence of Mousterian levels at the site, and OSL dating of these levels provided an age range of 31-60 ka for the detrital deposits, presenting for the first time the occupation of Neanderthal groups in karstic contexts in the northern Iberian plateau, southern part of the Duero basin.
This paper presents a part of an archaeological research project focused on the study of the firs... more This paper presents a part of an archaeological research project focused on the study of the first human occupations between Eresma and Riaza rivers (Central Spain). In this work, we show the first results of the geoarchaeological analysis of the Abrigo del Molino karstic deposit (Eresma river, Segovia). It includes a sedimentological and geoarchaeological analysis of the site. Also, a preliminary analysis of lithics and faunal remains documented in the profile of the rockshelter was developed. It is important to highlight the presence of a flint mousterian assemblage which includes levallois knapping method. Finally, we present the results of an OSL dating collected at the top of the archaeological sequence, which lets us to asign it to Middle Paleolithic period.
La Güelga cave is located at the bottom of a mountain valley in the Eastern part of Asturias (Nor... more La Güelga cave is located at the bottom of a mountain valley in the Eastern part of Asturias (Northern Spain), 186 m above sea level and 15 km far away from the coast. It currently comprises a group of caves that were occupied during the Middle and Upper Paleolithic periods (MP and UP respectively). In recent years, we have studied the levels of La Güelga cave –D Zone-proposing a sequence for the MP/UP transition: Mousterian-Aurignacian-Châtelperronian, which we review in this paper after a detailed analysis of the chronostratigraphy. We also provide new radiocarbon dates for the Mousterian, Aurignacian and Châtelperronian levels. Finally, the geoarchaeology, taphonomy, archaeological data, and chronology suggest that the interstratification -initially identified on the basis of stratigraphic observations during excavation-cannot be maintained. In any case, the stratigraphy of the internal D Zone of La Güelga cave is one of the most interesting from the Cantabrian region for analyzi...
Conference: Hugo Obermaier-Gesellschaft für Erforschung des Eizeitalters und der Steinzeit e V. 57th Annual Meeting in Heidenheim, 2015, Volume: 57th Annual Meeting in Heidenheim. Hugo Obermaier Society for Quaternary Research and Archaeology of the Stone Age, 2015
Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in ... more Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).
Coímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.
Moreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.
This work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.
"Comprendiendo el relieve: del pasado al futuro" / Juan José Durán Valsero, Manuel Montes Santiago, Alejandro Robador Moreno y Ángel Salazar Rincón, eds.- : 195-202, 2016
The upper set of the detrital filling of the fluvio-karst cavity in which the Mousterian archaeol... more The upper set of the detrital filling of the fluvio-karst cavity in which the Mousterian archaeological site of Abrigo del Molino (Segovia) is located, corresponds to sandy, loams and cobbles, which are the result of the physico-chemical weathering and the ice-wedge weathering of the roof of the shelter. It involves the final silting of the sedimentary infill of the rockshelter and its basal part contains the last remnants of Mousterian lithic industry, with datings circa 50 ka BP, close to the disappearance of the Neanderthals in the Iberian Peninsula. To estimate the required time interval for the silting of roof shelter has been taken,as current analog,the rhythm of production and accumulation of sediment that occurred on the level of excavation in the year between the end of the excavation campaign 2014 and the start of the excavation campaign of 2015. Weight and volume of the measured deposits were 101.5 kg and 72 dm3, respectively; giving an average density of 1.177 g/cm3 and an average filling, distributed on the surface of 1,275 cm that year. Assimilating the dome of the shelter to a quarter of irregular scalene ellipsoid, it has been possible to calculate the surface from which sediment is generated by weathering and ice-wedge weathering, which would be 10.09 m2, of which an average thickness of 0.4467 cm was detached this year. Finally, we have calculated the progressive average rate of silting, that is the result of the balance between the sediment detached and accumulated, which would be +0.8283 cm/year; giving thus a period of clogging, for 1.5 m height of the cavity, of about
180 years. Sources of uncertainty and error of these calculations are discussed as well as future developments, which will go through the theoretical numerical modelling of the silting process.
The Abrigo del Molino archaeological site is located in the Eresma river valley, near Segovia cit... more The Abrigo del Molino archaeological site is located in the Eresma river valley, near Segovia city (Central Spain). It consists of a shallow cave of fluvio-karstic origin, which has been completely filled in with detrital deposits. Geoarchaeological interpretation of its genesis differentiates three groups: a lower group with sandy loams and fine sands interbedded with pebble and gravel layers deposited by palaeofloods and slope contributions respectively; a middle group with massive silts and grain-supported boulders, formed by alternating contributions from the overlying slope as well as karst mudflows and rockfall from the shelter roof; and an upper group of silt cemented by carbonates, final backfill alteration and degradation of the host rock. The techno-typological characteristics of the lithic assemblage confirm the existence of Mousterian levels at the site, and OSL dating of these levels provided an age range of 31-60 ka for the detrital deposits, presenting for the first time the occupation of Neanderthal groups in karstic contexts in the northern Iberian plateau, southern part of the Duero basin.
En este trabajo se presenta los primeros resultados de un proyecto de investigación cuyo objetivo... more En este trabajo se presenta los primeros resultados de un proyecto de investigación cuyo objetivo es estudiar la evolución del poblamiento humano y su relación con el medio natural y el paisaje en una comarca de la montaña leonesa, que se sitúa concretamente en el interfl uvio Esla-Alto Cea. Además, se pretende analizar la conexión y relación entre distintos ámbitos territoriales, conectados por zonas de tránsito natural, a lo largo de un territorio de media y alta montaña. Este territorio presenta una variedad fi siográfi ca relativamente amplia, que posibilita la existencia de distintos ecosistemas y hábitats que resultan altamente aptos para el poblamiento humano a lo largo de las distintas etapas de la Prehistoria. Esta circunstancia viene avalada por la presencia de yacimientos que abarcan desde el Paleolítico inferior a la Edad del Hierro, pasando por los distintos periodos que marcan el paso de las sociedades cazadoras-recolectoras a las
sociedades productoras-metalúrgicas.
In: Los cazadores recolectores del Pleistoceno y del Holoceno en Iberia y el Estrecho de Gibralta... more In: Los cazadores recolectores del Pleistoceno y del Holoceno en Iberia y el Estrecho de Gibraltar: estado actual del conocimiento del registro arqueológico, R. Sala Ramos (ed.). 60-63; Fundación Atapuerca.
VIII Reunión de Cuaternario Ibérico: 83-86, 2013
VIII Reunión de Cuaternario Ibérico: 34-38, 2013
Espacio, Tiempo y Forma. Serie I, Nueva época. Prehistoria y Arqueología, t. 2, 2009
This paper shows an advance of an archaeological research realised in summer of 2007 in Casa Nogu... more This paper shows an advance of an archaeological research realised in summer of 2007 in Casa Noguera site (Archivel, Caravaca de la Cruz, Murcia), with calcolithic, bronze age and iberian levels.
Espacio, Tiempo y Forma, Serie VI, Nueva época. Prehistoria y Arqueología, t. 5: 405-418, 2012
El Cierro cave (Ribadesella, Asturias, Spain) is located in a spur of limestone in a karstic plat... more El Cierro cave (Ribadesella, Asturias, Spain) is located in a spur of limestone in a karstic platform ranging
from Sardeo to Ardines, in the same place in which we also find Les Pedroses cave, with rock art assigned
to Lower Magdalenian. This site, which has provided an interesting sequence to end of the Solutrean and
Early Magdalenian, is very close to other relevant Solutrean sites, as Cova Rosa. F. Jordá Cerdá was the first
researcher who excavated in El Cierro cave in 1959. He continued his research in this site with A. Gómez
Fuentes since 1976. This paper aims to make a contextualization of Upper Cantabrian Solutrean from checking
the materials of this site.
Uploads
Papers by María de Andrés Herrero
Coímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.
Moreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.
This work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.
180 years. Sources of uncertainty and error of these calculations are discussed as well as future developments, which will go through the theoretical numerical modelling of the silting process.
sociedades productoras-metalúrgicas.
from Sardeo to Ardines, in the same place in which we also find Les Pedroses cave, with rock art assigned
to Lower Magdalenian. This site, which has provided an interesting sequence to end of the Solutrean and
Early Magdalenian, is very close to other relevant Solutrean sites, as Cova Rosa. F. Jordá Cerdá was the first
researcher who excavated in El Cierro cave in 1959. He continued his research in this site with A. Gómez
Fuentes since 1976. This paper aims to make a contextualization of Upper Cantabrian Solutrean from checking
the materials of this site.
Coímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.
Moreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.
This work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.
180 years. Sources of uncertainty and error of these calculations are discussed as well as future developments, which will go through the theoretical numerical modelling of the silting process.
sociedades productoras-metalúrgicas.
from Sardeo to Ardines, in the same place in which we also find Les Pedroses cave, with rock art assigned
to Lower Magdalenian. This site, which has provided an interesting sequence to end of the Solutrean and
Early Magdalenian, is very close to other relevant Solutrean sites, as Cova Rosa. F. Jordá Cerdá was the first
researcher who excavated in El Cierro cave in 1959. He continued his research in this site with A. Gómez
Fuentes since 1976. This paper aims to make a contextualization of Upper Cantabrian Solutrean from checking
the materials of this site.
Coímbre cave (142 meters asl) is located on the southwestern slope of Mount Pendendo (529 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).
Coímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.
Moreover, Coímbre cave presents an interesting set of Magdalenian engravings, locatedin different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.
This work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.
The poster presents results of the archaeological research in La Güelga cave, carried out between 1989 and 2012. They comprise interesting data (faunal, lithics and mobile art) of the late hunter-gatherer groups in northern Spain and important data on the MP to UP transition in the northern Iberian Peninsula (Menéndez et al. 2014).
This site has been known since 1971, when a series of parietal engravings attributed to the initial and recent Magdalenian were discovered, as well as a large archaeological deposit, although this was not excavated (Moure and Gil, 1974; Álvarez-Alonso et al., 2014). However, from 2008 to 2012 the present team has excavated a total surface area of 4m2 in the innermost part of the main chamber -called Zone B-, which has yielded an interesting full Magdalenian sequence in addition to a Gravettian level, which is presented here (Álvarez Alonso et al., 2009, 2013, 2015; Yravedra et al., 2016). The Co.B.6 level of Coímbre has been dated between 29.660 and 28.560 Cal BP, coinciding with the warm event of the Greenland Interstadial 4, in one of the warm phases of the MIS3a.
Coímbre’s Gravettian and Magdalenian occupations differ widely, mainly concerning the space occupation and management and the resources catchment patterns. Thus, during the Gravettian can be appreciated a dominant local procurement with an important dependence on the closest lithic raw materials -mainly quartzites-, as well as a low technical requirements and a great immediacy in the management of the different chaînes opératoires. In contrast, related to the hunted faunas the Gravettian groups were not limited to the most abundant species in the immediate environment -considering the mountainous area- as happened during the Magdalenian, where Coímbre highlighted as an ibex’s kill-site. In this way, in the Co.B.6 level, the identified fauna includes large species like Bos/Bison, Equus ferus and Cervus elaphus, but also Capra pyrenaica.
Considering these features and the results of the spatial analysis (GIS) of the economic territory and the subsistential mobility, we can interpret this such as a sporadic occupation, which responds to a high degree of immediacy, probably within an east-west high mobility context. The palaeobotanical data and the use of bone as fuel (Yravedra et al., 2016), underpin this hypothesis.
Due to its large and varied archaeological record, Coímbre is one of the most outstanding sites to study the characteristics of Gravettian human occupations in one of the most western ends of the expansion of this technocomplex on the European continent.
References
Álvarez Alonso, D., Yravedra, J., Arrizabalaga, A., Jordá Pardo, J., Heredia, N., 2009. La cueva de Coímbre (Peñamellera Alta, Asturias, España): su yacimiento arqueológico y su santuario rupestre. Un estado de la cuestión en 2008. Munibe 60, 139-155
Álvarez Alonso, D., Yravedra, J., Arrizabalaga, A., Jordá, J. F., 2013. Excavaciones arqueológicas en la cueva de Coímbre (Besnes, Peñamellera Alta). Cam¬pañas 2008-2012, In: Excavaciones Arqueológicas en Asturias 2007-2012, Asturias, pp. 109-120.
Álvarez Alonso, D., Yravedra, J., Andrés Herrero, M. de., Arrizabalaga, A., García Díez, M., Garrido, D., Jordá Pardo, J. F., 2014. La cueva de Coímbre (Asturias, España): artistas y cazadores durante el Magdaleniense en la región cantábrica. In: Corchón, Mª S. and Menéndez Fernández, M. (Eds.), Cien Años de arte rupestre paleolítico. Centenario del descubrimiento de la cueva de la Peña de Candamo (1914-2014). Acta salmanticensia. Estudios históricos y geográficos 106, pp. 101-108.