Durante la primera campaña de excavaciones realizada en el año 2015 en el yacimiento tartésico de Casas del Turuñuelo (Guareña, Badajoz) se procedió a excavar la denominada estancia 100. Entre los materiales arqueológicos documentados... more
Durante la primera campaña de excavaciones realizada en el año 2015 en el yacimiento tartésico de Casas del Turuñuelo (Guareña, Badajoz) se procedió a excavar la denominada estancia 100. Entre los materiales arqueológicos documentados sobre el pavimento de la habitación se recuperaron cuatro placas que por la posición que presentaban decoraban las cuatro caras de una caja de madera perdida por el incendio que puso fin a la vida del edificio. Este trabajo reúne la información referente a su hallazgo y contexto arqueológico, el estudio de las piezas y su iconografía, los resultados de los análisis realizados tanto de las placas como de los clavos conservados, así como el proceso de restauración y conservación al que las piezas han sido sometidas. Su estudio nos ha permitido abrir nuevas líneas de investigación en torno al comercio fenicio con Occidente y la existencia de un artesanado especializado en el trabajo del hueso y el marfil en los enclaves peninsulares.
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Se recogen en el presente trabajo los resultados obtenidos tras la ejecución de cinco campañas de excavación en el yacimiento de Cerro Borreguero (Zalamea de la Serena, Badajoz). Estos trabajos han permitido documentar la existencia de... more
Se recogen en el presente trabajo los resultados obtenidos tras la ejecución de cinco campañas de excavación en el yacimiento de Cerro Borreguero (Zalamea de la Serena, Badajoz). Estos trabajos han permitido documentar la existencia de tres momentos de ocupación que se extienden entre el siglo IX ane y I ane con un hiatus pronunciado entre las etapas protohistórica y romana. La aparición de una cabaña oval en convivencia con una construcción de planta rectangular nos sitúa ante el primer yacimiento de transición entre el Bronce Final y la I Edad del Hierro en el valle medio del Guadiana
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this work summarizes the results yielded after five excavation campaigns where undertaken at the Cerro Borreguero (Borreguero Hill) Archaeological Site (Zalamea de la Serena, Badajoz). Said excavation campaigns have allowed us to... more
this work summarizes the results yielded after five excavation campaigns where undertaken at the Cerro Borreguero (Borreguero Hill) Archaeological Site (Zalamea de la Serena, Badajoz). Said excavation campaigns have allowed us to document the existence of three moments of occupation between the ninth century BCE and the first century BCE, with a noticeable hiatus between the Protohistoric Period and Roman Period. The appearance of an oval hut along with a rectangular construction indicates that this is the first transition archaeological site in the Middle Valley of the Guadiana River which dates between the Late Bronze Age and Iron Age I.
Resumen Se presentan en este trabajo los resultados obtenidos durante la excavación de la estancia 100 del yacimiento de 'Casas del Turuñuelo' (Guareña, Badajoz). Para ello realizamos un recorrido a través de su arquitectura y de los... more
Resumen Se presentan en este trabajo los resultados obtenidos durante la excavación de la estancia 100 del yacimiento de 'Casas del Turuñuelo' (Guareña, Badajoz). Para ello realizamos un recorrido a través de su arquitectura y de los ele-mentos materiales documentados durante las excavaciones. A partir de su análisis planteamos una primera lectura del espacio, donde incluimos su funcionalidad y comparativa con otros ejemplos documentados tanto en el núcleo de Tarteso como en su periferia geográfica, el valle medio del Guadiana.
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Hacia mediados del siglo VI a. C. se detecta en el núcleo de Tarteso un profundo cambio del que seguimos ignorando sus verdaderas causas; así, en muchos de los yacimientos del valle del Guadalquivir y de la provincia de Huelva, se... more
Hacia mediados del siglo VI a. C. se detecta en el núcleo de Tarteso un profundo cambio del que seguimos ignorando sus verdaderas causas; así, en muchos de los yacimientos del valle del Guadalquivir y de la provincia de Huelva, se manifiesta un momento de decadencia y abandono que ha sido definido como la crisis de Tarteso. Sin embargo, y frente a lo que algunos defienden, la cultura tartésica aún tendrá un largo recorrido pues, si bien es cierto que se difumina en el sur peninsular, su esencia se proyecta hacia las tierras del interior, en concreto al valle del Guadiana, una región entendida desde los años 80 del pasado siglo como la periferia y la frontera de Tarteso. De ese modo, entre finales del siglo VII y principios del VI a. C. el valle medio del Guadiana fue testigo de un fuerte crecimiento demográfico que supuso el desarrollo de un patrón territorial propio. Se rompía así con la escasa información que teníamos sobre el poblamiento de este territorio durante el Bronce Final, a la vez que se inauguraba un modelo de asentamiento que, a pesar de su originalidad, hundía sus raíces en la cultura tartésica. En este artículo se analizan los principales túmulos tartésicos conocidos, y se incluye un mapa con la ubicación de los hasta ahora localizados, así como una magnífica ilustración a doble página realizada por Josep R. Casals en el que se reconstruye el famoso santuario de Cancho Roano en su fase A.
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There are reasons other than biological and environmental to argue for the preservation of Doñana National Park—reasons which are geological, archaeological, and anthropological. Up until the establishment of Estación Biológica of CSIC,... more
There are reasons other than biological and environmental to argue for the preservation of Doñana National Park—reasons which are geological, archaeological, and anthropological. Up until the establishment of Estación Biológica of CSIC, the lower Guadalquivir River basin was home to a human community adapted to the rich, varied resources of a marshland milieu. Early in the 20th century, the construction of Palacio de la Marismilla led to the unexpected discovery of a yet older settlement: one by Cerro del Trigo, dated to the 2nd to the 6th century AD, which archaeologist G. Bonsor and philologist A. Schulten excavated in the 1920s. Their project confirmed such occupation, and, in the process, revealed an earlier, prehistoric one, along with clear signs of subsidence of the ground during the Holocene. In effect, Doñana National Park is a setting for relatively rapid geomorphological processes of scientific interest, which can be compared with those that climate oscillations and neo-tectonics have generated elsewhere in the planet over the past millennia. Since 2005 the interdisciplinary Hinojos Project has brought the relevance of these scientific accomplishments to bear on its own results—mainly, on the one hand, the evidence of settlement and cultural development that goes back to at least Neolithic times and, on the other, the traces of a rapid geomorphological dynamics that combines long phases of alluvial sedimentation and subsidence of the ground with short, periodic events of high-energy marine transgression.
KEY WORDS: Doñana, Guadalquivir paleo-estuary, Middle Holocene, Late Holocene, Geomorphological evolution, Neo-tectonics, Extreme Wave Events, Subsidence, Settlement changes, Neolithic, Copper Age, Bronze Age, Roman period, Islamic period.
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http://editorial.csic.es/publicaciones/libros/12647/978-84-00-10101-5/donana-50-anos-de-investigaciones-cientificas.html
RESUMEN: Hay más razones que las biológicas y medioambientales para conservar Doñana: son razones geológicas, arqueológicas y antropológicas. Hasta la constitución de la Estación Biológica del CSIC en 1964, la comarca del bajo Guadalquivir estuvo habitada durante siglos por una comunidad humana adaptada al aprovechamiento de los muchos recursos que el medio marismeño ofrece. A comienzos del siglo XX, la construcción del Palacio de La Marismilla tuvo por efecto inesperado el descubrimiento de los restos de un poblamiento más antiguo aún: el del yacimiento de El Cerro del Trigo, de los siglos II a VI de nuestra era, que el arqueólogo G. Bonsor y el filólogo A. Schulten excavarían en la década de 1920. Su proyecto confirmó este poblamiento y, además, reveló indicios de otro, más remoto todavía, de la prehistoria, así como señales de una subsidencia general del terreno durante el Holoceno. El Espacio Natural es, en efecto, escenario de procesos geomorfológicos de duración relativamente rápida que tienen un gran interés científico; son comparables a los que generan en otras zonas del planeta las fluctuaciones climáticas y la neo-tectónica de los últimos milenios. El pluridisciplinar Proyecto Hinojos, iniciado en 2005, ha puesto en valor estos referentes para la ciencia sobre Doñana a la luz de sus propios resultados: principalmente, de un lado, evidencias de poblamiento y tradiciones culturales que se remontan al menos al Neolítico y, de otro, claros signos de una rápida dinámica geomorfológica de fases sedimentarias aluviales y de subsidencia, interrumpidas periódicamente por episodios erosivos de origen oceánico de alta energía.
PALABRAS CLAVE: Doñana, paleo-estuario del Guadalquivir, Holoceno Medio, Holoceno Superior, evolución geomorfológica, neo-tectónica, episodios de transgresión oceánica extrema, subsidencia, cambios en poblamiento, Neolítico, Calcolítico, Edad del Bronce, época romana, época andalusí.
KEY WORDS: Doñana, Guadalquivir paleo-estuary, Middle Holocene, Late Holocene, Geomorphological evolution, Neo-tectonics, Extreme Wave Events, Subsidence, Settlement changes, Neolithic, Copper Age, Bronze Age, Roman period, Islamic period.
Full text in:
http://editorial.csic.es/publicaciones/libros/12647/978-84-00-10101-5/donana-50-anos-de-investigaciones-cientificas.html
RESUMEN: Hay más razones que las biológicas y medioambientales para conservar Doñana: son razones geológicas, arqueológicas y antropológicas. Hasta la constitución de la Estación Biológica del CSIC en 1964, la comarca del bajo Guadalquivir estuvo habitada durante siglos por una comunidad humana adaptada al aprovechamiento de los muchos recursos que el medio marismeño ofrece. A comienzos del siglo XX, la construcción del Palacio de La Marismilla tuvo por efecto inesperado el descubrimiento de los restos de un poblamiento más antiguo aún: el del yacimiento de El Cerro del Trigo, de los siglos II a VI de nuestra era, que el arqueólogo G. Bonsor y el filólogo A. Schulten excavarían en la década de 1920. Su proyecto confirmó este poblamiento y, además, reveló indicios de otro, más remoto todavía, de la prehistoria, así como señales de una subsidencia general del terreno durante el Holoceno. El Espacio Natural es, en efecto, escenario de procesos geomorfológicos de duración relativamente rápida que tienen un gran interés científico; son comparables a los que generan en otras zonas del planeta las fluctuaciones climáticas y la neo-tectónica de los últimos milenios. El pluridisciplinar Proyecto Hinojos, iniciado en 2005, ha puesto en valor estos referentes para la ciencia sobre Doñana a la luz de sus propios resultados: principalmente, de un lado, evidencias de poblamiento y tradiciones culturales que se remontan al menos al Neolítico y, de otro, claros signos de una rápida dinámica geomorfológica de fases sedimentarias aluviales y de subsidencia, interrumpidas periódicamente por episodios erosivos de origen oceánico de alta energía.
PALABRAS CLAVE: Doñana, paleo-estuario del Guadalquivir, Holoceno Medio, Holoceno Superior, evolución geomorfológica, neo-tectónica, episodios de transgresión oceánica extrema, subsidencia, cambios en poblamiento, Neolítico, Calcolítico, Edad del Bronce, época romana, época andalusí.
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A multidisciplinary analysis of cores and geomorphic patterns in the marshes of Doñana National Park (SW Spain) has yielded new evidence regarding the sedimentary infilling and geomorphological evolution of the Guadalquivir estuary... more
A multidisciplinary analysis of cores and geomorphic patterns in the marshes of Doñana National Park (SW
Spain) has yielded new evidence regarding the sedimentary infilling and geomorphological evolution of the
Guadalquivir estuary during the Holocene. The sedimentation and geomorphological disposition have been
strongly conditioned by neotectonic activity along a set of SW-NE alignments, interrupted by other alignments
that follow E-W and NW-SE directions. The most conspicuous of the SW-NE alignments is the Torre
Carbonero-Marilópez Fault (TCMF). South of this fault, the estuary experienced a marked subsidence from
about 4000 to 2000 cal. yr BP through a series of sedimentary sequences of retrogradation and aggradationwithin
the context of relative sea-level rise. From c. 2000 cal. yr BP to the present the subsidence has remained relatively
dormant, with progradation of the littoral systems and infilling of the marshland progressing within a context of
sea-level stability. Our results reveal that neotectonic activity is a critical factor that must also be reckonedwith in
any attempt to understand the Holocene geomorphological evolution in the Guadalquivir estuary.
Spain) has yielded new evidence regarding the sedimentary infilling and geomorphological evolution of the
Guadalquivir estuary during the Holocene. The sedimentation and geomorphological disposition have been
strongly conditioned by neotectonic activity along a set of SW-NE alignments, interrupted by other alignments
that follow E-W and NW-SE directions. The most conspicuous of the SW-NE alignments is the Torre
Carbonero-Marilópez Fault (TCMF). South of this fault, the estuary experienced a marked subsidence from
about 4000 to 2000 cal. yr BP through a series of sedimentary sequences of retrogradation and aggradationwithin
the context of relative sea-level rise. From c. 2000 cal. yr BP to the present the subsidence has remained relatively
dormant, with progradation of the littoral systems and infilling of the marshland progressing within a context of
sea-level stability. Our results reveal that neotectonic activity is a critical factor that must also be reckonedwith in
any attempt to understand the Holocene geomorphological evolution in the Guadalquivir estuary.
A detailed pollen analysis has been carried out on two sediment cores taken from a marsh area located in the Doñana National Park, southwestern Spain. The studied sedimentary sequences contain a similar late Holocene record of vegetation... more
A detailed pollen analysis has been carried out on two sediment cores taken from a marsh area located in the Doñana National Park, southwestern Spain.
The studied sedimentary sequences contain a similar late Holocene record of vegetation and climate and show a progressive aridification trend since at
least 5000 cal. yr BP, through a decrease in forest cover in this area. Long-term vegetation changes shown here (semi-desert expansion and Mediterranean
forest decline) paralleled declining summer insolation. Decreasing summer insolation most likely impacted negatively on tree growing season as well as on
winter precipitation in the area. Superimposed on the long-term aridification trend were multi-centennial scale periods characterized by forest reductions
or increases in arid and halophytic plants that can be interpreted as produced by enhanced droughts and/or by local geodynamic processes. These are
centered at ca. 4000, 3000–2500, and 1000 cal. yr BP, coinciding in timing and duration with well-known dry events in the western Mediterranean and
other areas but could have also been generated by local sedimentary or geodynamic processes such as a marine transgression in a subsidence context
and extreme wave events (EWEs). The alternation of persistent North Atlantic Oscillation modes probably played an important role in controlling these
relatively humid–arid cycles.
The studied sedimentary sequences contain a similar late Holocene record of vegetation and climate and show a progressive aridification trend since at
least 5000 cal. yr BP, through a decrease in forest cover in this area. Long-term vegetation changes shown here (semi-desert expansion and Mediterranean
forest decline) paralleled declining summer insolation. Decreasing summer insolation most likely impacted negatively on tree growing season as well as on
winter precipitation in the area. Superimposed on the long-term aridification trend were multi-centennial scale periods characterized by forest reductions
or increases in arid and halophytic plants that can be interpreted as produced by enhanced droughts and/or by local geodynamic processes. These are
centered at ca. 4000, 3000–2500, and 1000 cal. yr BP, coinciding in timing and duration with well-known dry events in the western Mediterranean and
other areas but could have also been generated by local sedimentary or geodynamic processes such as a marine transgression in a subsidence context
and extreme wave events (EWEs). The alternation of persistent North Atlantic Oscillation modes probably played an important role in controlling these
relatively humid–arid cycles.
Amultidisciplinary study froma number of drilled cores in theGuadalquivir estuary hasmade possible to identify as many as three extreme wave events and their facies in the 4th millennium BP (A: ~4000 cal yr BP, B: ~3550 cal yr BP, and... more
Amultidisciplinary study froma number of drilled cores in theGuadalquivir estuary hasmade possible to identify as
many as three extreme wave events and their facies in the 4th millennium BP (A: ~4000 cal yr BP, B: ~3550 cal yr
BP, and C: ~3150 cal yr BP). These events,which caused strong erosion in the Guadalquivir sandy barrier and in the
neighboring aeolian systems of El Abalario, brought about significant paleogeographical changes that may have
affected human settlements established in the area during the Neolithic and Copper Age periods and during the
Middle Bronze Age. The three events can be spatially correlated and their facies differentiated frommore proximal
to more distal from the coastline. The most proximal facies is characterized by a massive accumulation of shells, a
sandy or sandy–muddy matrix, an erosive base, a highly diverse mixture of species (marine and estuarine), and
lithoclasts. The most distal facies presents a muddy–sandy matrix, dominance of estuarine fauna, shell accumulation,
presence of terrestrial species, mudpebbles, pebbles in a clayey matrix, and bioturbation. The evidence
presented will further advance scientific knowledge about the impact of extreme wave events on coastal areas
in SW Iberia and NWAfrica.
many as three extreme wave events and their facies in the 4th millennium BP (A: ~4000 cal yr BP, B: ~3550 cal yr
BP, and C: ~3150 cal yr BP). These events,which caused strong erosion in the Guadalquivir sandy barrier and in the
neighboring aeolian systems of El Abalario, brought about significant paleogeographical changes that may have
affected human settlements established in the area during the Neolithic and Copper Age periods and during the
Middle Bronze Age. The three events can be spatially correlated and their facies differentiated frommore proximal
to more distal from the coastline. The most proximal facies is characterized by a massive accumulation of shells, a
sandy or sandy–muddy matrix, an erosive base, a highly diverse mixture of species (marine and estuarine), and
lithoclasts. The most distal facies presents a muddy–sandy matrix, dominance of estuarine fauna, shell accumulation,
presence of terrestrial species, mudpebbles, pebbles in a clayey matrix, and bioturbation. The evidence
presented will further advance scientific knowledge about the impact of extreme wave events on coastal areas
in SW Iberia and NWAfrica.
The recent archaeological findings in the city of Huelva have supposed an important turn in the investigation on the first contacts of the Phoenicians in the Iberian Peninsula, now dated in the last years from century X a.n.e. This... more
The recent archaeological findings in the city of Huelva have
supposed an important turn in the investigation on the first contacts of the
Phoenicians in the Iberian Peninsula, now dated in the last years from century
X a.n.e. This circumstance allows us to consider a fluid commercial relation
between the Atlantic and the Mediterranean, through Straits of Gibraltar,
before which until now it was possible to be defended. Nevertheless, in some
areas of the interior of the peninsular southwest objects and cultural manifestations
of clear Eastern origin are detected previous to the Phoenician presence
in the south of the Iberian Peninsula, which takes to us to propose a
route of continental penetration previous to the Phoenician colonization from
the south-east French, where some products of clear Cypriot origin would be
introduced, case of the found ones in some deposits of the Portuguese Beira
or the represented ones in the stelae of warrior. After the Phoenician colonization
of the peninsular southwestern coast a territory of more or less homogenous
culture will be formed that the Greeks denominated Tartessos, and
that must be understood as the amalgam arisen between the powerful original
culture of the Eastern Mediterranean introduced by the Phoenicians and the
native, of Atlantic origin.
supposed an important turn in the investigation on the first contacts of the
Phoenicians in the Iberian Peninsula, now dated in the last years from century
X a.n.e. This circumstance allows us to consider a fluid commercial relation
between the Atlantic and the Mediterranean, through Straits of Gibraltar,
before which until now it was possible to be defended. Nevertheless, in some
areas of the interior of the peninsular southwest objects and cultural manifestations
of clear Eastern origin are detected previous to the Phoenician presence
in the south of the Iberian Peninsula, which takes to us to propose a
route of continental penetration previous to the Phoenician colonization from
the south-east French, where some products of clear Cypriot origin would be
introduced, case of the found ones in some deposits of the Portuguese Beira
or the represented ones in the stelae of warrior. After the Phoenician colonization
of the peninsular southwestern coast a territory of more or less homogenous
culture will be formed that the Greeks denominated Tartessos, and
that must be understood as the amalgam arisen between the powerful original
culture of the Eastern Mediterranean introduced by the Phoenicians and the
native, of Atlantic origin.
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The findings of the first southwestern warrior stelae and other treasures like the one from Aliseda, the bronze jugs or the orientalazing jewellery, have emphasize the importance of the Phoenician presence inside the Iberian Peninsula.... more
The findings of the first southwestern warrior stelae and other treasures like the one from Aliseda,
the bronze jugs or the orientalazing jewellery, have emphasize the importance of the Phoenician
presence inside the Iberian Peninsula. The appearance of cemeteries with elements of the Phoenician
world, such as Medellín, as well as the proliferation of singular buildings of eastern plant, has increased
this idea. However, a greater interest offers the change of economic strategy that is appraised in
this ample territory in the Orientalizing Period, where is evident the development of agriculture and
the detriment of the cattle economical base of the Final Bronze Age. These circumstances have allowed
elaborating some hypotheses that assert land colonization by Phoenician agents. Nevertheless,
it has been impossible to ratify this fact in any case, that rather seems to respond to a Tartesic colonization
of the inland territories that would contribute with manpower bringing the inherited cultural
features of the Phoenician colonization within the Tartesic nucleus. Therefore, it will be through the
Tartesic culture when objects or techniques of Eastern origin are introduced in inland Iberia, attached
to a change in the social, religious or economic organization that would alter the system implanted
since the beginnings of the Bronze Age, that at the end would determine a change in the commercial
relations around the Guadiana river.
the bronze jugs or the orientalazing jewellery, have emphasize the importance of the Phoenician
presence inside the Iberian Peninsula. The appearance of cemeteries with elements of the Phoenician
world, such as Medellín, as well as the proliferation of singular buildings of eastern plant, has increased
this idea. However, a greater interest offers the change of economic strategy that is appraised in
this ample territory in the Orientalizing Period, where is evident the development of agriculture and
the detriment of the cattle economical base of the Final Bronze Age. These circumstances have allowed
elaborating some hypotheses that assert land colonization by Phoenician agents. Nevertheless,
it has been impossible to ratify this fact in any case, that rather seems to respond to a Tartesic colonization
of the inland territories that would contribute with manpower bringing the inherited cultural
features of the Phoenician colonization within the Tartesic nucleus. Therefore, it will be through the
Tartesic culture when objects or techniques of Eastern origin are introduced in inland Iberia, attached
to a change in the social, religious or economic organization that would alter the system implanted
since the beginnings of the Bronze Age, that at the end would determine a change in the commercial
relations around the Guadiana river.
Research Interests:
In recent fieldworks carried out at the archaeological site of Cancho Roano, a boundary pit full-up with a big amount of animal bones and pottery have been discovered surrounding the building. The analysis of these remains allow us to... more
In recent fieldworks carried out at the archaeological site of Cancho Roano, a boundary pit
full-up with a big amount of animal bones and pottery have been discovered surrounding
the building. The analysis of these remains allow us to infer the celebration of a communal
banquet during the last moments of occupation of the complex, similar to those well-know
in other sites of the Iberian Peninsula and Central Europe. In opposition, the presence of
banquet tools with a more restricted use such as spits or tools related to the manoeuvring of
wine inside the building, implies another kind of commensality practices with a exclusively
private character.
full-up with a big amount of animal bones and pottery have been discovered surrounding
the building. The analysis of these remains allow us to infer the celebration of a communal
banquet during the last moments of occupation of the complex, similar to those well-know
in other sites of the Iberian Peninsula and Central Europe. In opposition, the presence of
banquet tools with a more restricted use such as spits or tools related to the manoeuvring of
wine inside the building, implies another kind of commensality practices with a exclusively
private character.
Research Interests:
The Castejón de las Merchanas is a fortified settlement located in the Guadamez valley in the margins of the Serena region (Don Benito, Badajoz, Spain). Its good state of preservation and the monumentality of the visible remains made... more
The Castejón de las Merchanas is a fortified settlement
located in the Guadamez valley in the margins of the Serena
region (Don Benito, Badajoz, Spain). Its good state of preservation
and the monumentality of the visible remains made
it worthwhile to develop a thorough recording effort in order
to improve our knowledge of the structure, functionality and
chronology of the site. The results of said effort are confronted
with the knowledge we currently have of the fortifications in
a regional framework, analyzing their locational criteria, design,
building techniques and archaeological finds. We propose
a model of strategic control of the territory and its contextualization
in the process of «Romanization» in southwestern
Spain.
located in the Guadamez valley in the margins of the Serena
region (Don Benito, Badajoz, Spain). Its good state of preservation
and the monumentality of the visible remains made
it worthwhile to develop a thorough recording effort in order
to improve our knowledge of the structure, functionality and
chronology of the site. The results of said effort are confronted
with the knowledge we currently have of the fortifications in
a regional framework, analyzing their locational criteria, design,
building techniques and archaeological finds. We propose
a model of strategic control of the territory and its contextualization
in the process of «Romanization» in southwestern
Spain.
Research Interests:
In this paper we analyze the peculiar colonization strategy developed by Rome in a peripheral territory such as La Serena region (Extremadura, Spain). This is a large territory that after showing a considerable importance in the... more
In this paper we analyze the peculiar colonization strategy developed by Rome in a peripheral territory such as La Serena region (Extremadura, Spain). This is a large territory that after showing a considerable importance in the Orientalizing period, only recovers its vitality gradually and parallel to the advance of the roman presence in the area. The settlement strategy in La Serena is strongly characterized by the multiplication of the so-called "fortified -or cyclopean- enclosures". The roman strategy proved to be effective and valid under different periods and so these sites emerged in the republican times and lasted during the early Roman Empire. Their functionality also appears to be diverse depending on its timing and location, related either to the control of the territory or to the economic exploitation of the resources of this area, both mining and agricultural. These sites and their constructive characteristics have some coincidences with what we know in other regions of the Iberian Peninsula, such as the portuguese Alentejo or the High Guadalquivir (Andalusia, Spain). The singularity in the formation of La Serena territory, mainly rural, is enhanced by the presence of a rock sanctuary such as the “Cueva del Valle”, which must have worked as a gathering place for the surrounding villages, thus contributing to the consolidation of the Roman occupation.
Research Interests:
The aim of this paper is to show the survey methods developed in the framework of a research project carried out in the Serena region (Badajoz Province, Spain). We start from a critical use of the notion of archaeological site and an... more
The aim of this paper is to show the survey methods
developed in the framework of a research project carried
out in the Serena region (Badajoz Province, Spain). We
start from a critical use of the notion of archaeological
site and an assessment of the meaning of intensive surface
collection in the context of the study of the structure
of preindustrial agrarian landscapes. We offer a detailed
exposition of the survey planning, data capture and spatial
analysis. In a first stage we make a global estimate of
density of surface finds, locating possible areas of interest.
In a second phase detected dispersions are qualified
by systematic sampling. Its main purpose is to dismiss selective
procedures leading to remarkable biases in surface
record. We emphasize the balance achieved between
data resolution and effort invested. This method has
shown its effectiveness to characterize archaeological
entities often not considered in Peninsular regional projects.
Other factors affecting the recognition of sherd
scatters are discussed, like the so-called “background
noise”.
developed in the framework of a research project carried
out in the Serena region (Badajoz Province, Spain). We
start from a critical use of the notion of archaeological
site and an assessment of the meaning of intensive surface
collection in the context of the study of the structure
of preindustrial agrarian landscapes. We offer a detailed
exposition of the survey planning, data capture and spatial
analysis. In a first stage we make a global estimate of
density of surface finds, locating possible areas of interest.
In a second phase detected dispersions are qualified
by systematic sampling. Its main purpose is to dismiss selective
procedures leading to remarkable biases in surface
record. We emphasize the balance achieved between
data resolution and effort invested. This method has
shown its effectiveness to characterize archaeological
entities often not considered in Peninsular regional projects.
Other factors affecting the recognition of sherd
scatters are discussed, like the so-called “background
noise”.
The findings of the first southwestern warrior stelae and other treasures like the one from Aliseda, the bronze jugs or the orientalazing jewellery, have emphasize the importance of the Phoenician presence inside the Iberian Peninsula.... more
The findings of the first southwestern warrior stelae and other treasures like the one from Aliseda,
the bronze jugs or the orientalazing jewellery, have emphasize the importance of the Phoenician
presence inside the Iberian Peninsula. The appearance of cemeteries with elements of the Phoenician
world, such as Medellín, as well as the proliferation of singular buildings of eastern plant, has increased
this idea. However, a greater interest offers the change of economic strategy that is appraised in
this ample territory in the Orientalizing Period, where is evident the development of agriculture and
the detriment of the cattle economical base of the Final Bronze Age. These circumstances have allowed
elaborating some hypotheses that assert land colonization by Phoenician agents. Nevertheless,
it has been impossible to ratify this fact in any case, that rather seems to respond to a Tartesic colonization
of the inland territories that would contribute with manpower bringing the inherited cultural
features of the Phoenician colonization within the Tartesic nucleus. Therefore, it will be through the
Tartesic culture when objects or techniques of Eastern origin are introduced in inland Iberia, attached
to a change in the social, religious or economic organization that would alter the system implanted
since the beginnings of the Bronze Age, that at the end would determine a change in the commercial
relations around the Guadiana river.
the bronze jugs or the orientalazing jewellery, have emphasize the importance of the Phoenician
presence inside the Iberian Peninsula. The appearance of cemeteries with elements of the Phoenician
world, such as Medellín, as well as the proliferation of singular buildings of eastern plant, has increased
this idea. However, a greater interest offers the change of economic strategy that is appraised in
this ample territory in the Orientalizing Period, where is evident the development of agriculture and
the detriment of the cattle economical base of the Final Bronze Age. These circumstances have allowed
elaborating some hypotheses that assert land colonization by Phoenician agents. Nevertheless,
it has been impossible to ratify this fact in any case, that rather seems to respond to a Tartesic colonization
of the inland territories that would contribute with manpower bringing the inherited cultural
features of the Phoenician colonization within the Tartesic nucleus. Therefore, it will be through the
Tartesic culture when objects or techniques of Eastern origin are introduced in inland Iberia, attached
to a change in the social, religious or economic organization that would alter the system implanted
since the beginnings of the Bronze Age, that at the end would determine a change in the commercial
relations around the Guadiana river.
Research Interests:
Research Interests:
The famous stelae from the Tartessos region of southern Iberia are compared with new discoveries from the Levant. Similarities of theme and iconography endorse the Phoenician connection, but show it to be more a cultural dialogue... more
The famous stelae from the Tartessos region of southern Iberia are compared with new discoveries
from the Levant. Similarities of theme and iconography endorse the Phoenician connection, but
show it to be more a cultural dialogue between east and west than an imposition by colonists.
from the Levant. Similarities of theme and iconography endorse the Phoenician connection, but
show it to be more a cultural dialogue between east and west than an imposition by colonists.
El presente volumen es el colofón de un proyecto que comenzó en el año 2015 tras el hallazgo en el yacimiento de Cerro Borreguero (Zalamea de la Serena, Badajoz) de una cazuela a mano pintada postcocción, de las denominadas comúnmente... more
El presente volumen es el colofón de un proyecto que comenzó en el año 2015 tras el hallazgo en el yacimiento de Cerro Borreguero (Zalamea de la Serena, Badajoz) de una cazuela a mano pintada postcocción, de las denominadas comúnmente como 'tipo Medellín'. A partir de este hallazgo se inició la búsqueda de ejemplares análogos depositados en varios museos arqueológicos españoles con la finalidad de seleccionar, analizar y estudiar un conjunto amplio de este tipo de producciones. De este trabajo de recopilación surge esta edición en la que se recogen las aportaciones de diferentes especialistas en el estudio de este tipo de cerámicas que, hasta ahora, siempre habían sido analizadas de forma aislada dentro de sus propios contextos territoriales. Así, el objetivo de este trabajo era reunir conjuntos de distintas regiones de la vertiente atlántica con la finalidad de hallar concomitancias y diferencias que nos permitan crear grupos homogéneos y establecer las relaciones que existen entre las diversas áreas geográficas donde han sido localizadas estas cerámicas, acotando las zonas de producción, la cronología de las piezas y la técnica empleada para su fabricación y posterior decoración.