Radiocarbon dating and talayots: the example of Son Ferrandell Oleza

Antiquity ◽  
1993 ◽  
Vol 67 (254) ◽  
pp. 108-116 ◽  
Author(s):  
Robert Chapman ◽  
Mark Van Strydonck ◽  
William Waldren

Like the Sardinian nuraghi, which they closely resemble, the stone-built towers on the Balearic Islands known as talayots have been the subject of considerable research in recent years. The present paper analyses a series of radiocarbon dates from the Son Ferrandell Oleza settlement and discusses the implications for Balearic prehistory.

1997 ◽  
Vol 63 ◽  
pp. 55-86 ◽  
Author(s):  
Pedro V. Castro Martínez ◽  
Sylvia Gili Suriñach ◽  
Paloma González Marcén ◽  
Vicente Lull ◽  
Rafael Micó Pérez ◽  
...  

The aim of this paper is to establish an absolute chronology for the prehistoric entities and sites of the Balearic islands. We begin with the human settlement of each island and continue with the temporalities of the most important entities and materials of the Pretalayotic period: the Beaker phenomenon, megalithic tombs, artificial burial caves, naviforms, and navetas. Then we define the chronological limits of the Talayotic period, giving special attention to its internal sequence and to the chronology of its distinctive monuments — the talayots, sanctuaries, and taulas. Finally we suggest the chronological limits of the material and sites ascribed to the Post-talayotic period. The approach adopted here is based on a detailed analysis of the radiocarbon dates corresponding to the main archaeological periods mentioned above. The information potential of each date has been evaluated critically in terms of the archaeological contexts from which samples were obtained.


1975 ◽  
Vol 41 ◽  
pp. 46-49 ◽  
Author(s):  
N. P. Stanley Price

The subject of this note is the chronology of the site of Khirokitia in Cyprus in the light of four recent radiocarbon determinations. Khirokitia has remained one of the most extensively uncovered prehistoric sites in the Levant since its initial excavation over thirty years ago (Dikaios 1953). The fourth millennium BC date then estimated for the site by Dikaios was revised markedly upwards to the mid-sixth millennium following the submission of samples for radiocarbon dating (Dikaios 1962). The fourth millennium estimate had assumed a stratigraphical continuity between the pre-dominantly aceramic occupation of the site and the appearance of well-made pottery in its upper-most levels. Since the radiocarbon samples were taken from aceramic contexts, Dikaios subsequently concluded that the pottery was the product of a re-occupation of the site in the fourth millennium bc, a date based on the ceramic parallels with and the radiocarbon dates from the site at Sotira (Dikaios 1962, 194).This conclusion is borne out by a re-examination of the published evidence and, less conclusively perhaps because of its limited nature, by the evidence of a small sounding at the site undertaken by the author in 1972 (Stanley Price and Christou 1973). The four main aims of this 2 m square sounding included further observation of the aceramic-ceramic stratigraphy and the collection of additional radiocarbon samples in an attempt to determine the duration of the aceramic occupation.


Radiocarbon ◽  
2014 ◽  
Vol 56 (02) ◽  
pp. 399-410
Author(s):  
Miguel Á Cau ◽  
Mateu Riera Rullan ◽  
Magdalena Salas ◽  
Mark Van Strydonck

Radiocarbon dates, obtained from different human bones found in several tombs of the site of Son Peretó, are presented and discussed together with the stratigraphical evidence and the study of the material culture. The calibrated dates show that the tombs were built earlier than the main phase of occupation of the West Sector, therefore belonging to a necropolis linked to the Christian building prior to the transformation of the area into a habitation nucleus. The necropolis is14C dated mainly to the 6th century AD. This is in good agreement with the chronology provided by ceramic materials.


Radiocarbon ◽  
2014 ◽  
Vol 56 (2) ◽  
pp. 399-410 ◽  
Author(s):  
Miguel Á Cau ◽  
Mateu Riera Rullan ◽  
Magdalena Salas ◽  
Mark Van Strydonck

Radiocarbon dates, obtained from different human bones found in several tombs of the site of Son Peretó, are presented and discussed together with the stratigraphical evidence and the study of the material culture. The calibrated dates show that the tombs were built earlier than the main phase of occupation of the West Sector, therefore belonging to a necropolis linked to the Christian building prior to the transformation of the area into a habitation nucleus. The necropolis is 14C dated mainly to the 6th century AD. This is in good agreement with the chronology provided by ceramic materials.


Radiocarbon ◽  
2020 ◽  
pp. 1-13
Author(s):  
C Mas Florit ◽  
M Á Cau Ontiveros ◽  
M Van Strydonck ◽  
M Boudin ◽  
F Cardona ◽  
...  

ABSTRACT The excavation of a building in the village of Felanitx in the eastern part of the island of Mallorca (Balearic Islands) has revealed the existence of a small necropolis. The inhumations did not provide grave goods except for a bronze belt buckle for which the typological study suggests a Late Antique chronology. The stratigraphical sequence however seems to suggest a possible evolution of the space across time since some graves are cut by others. In order to obtain an absolute date for the necropolis and to verify if there are chronological differences between the graves, a total of 6 human bones samples have been 14C dated by AMS. The results of the radiocarbon dating confirm a Late Antique chronology (4th to 7th century AD) for the graves but do not suggest a chronological evolution. Despite the fact that the knowledge of the necropolis is still fragmentary, the results are extremely important because they provide an absolute date for a Late Antique necropolis in the Mallorcan rural area.


2003 ◽  
Vol 68 (4) ◽  
pp. 719-735 ◽  
Author(s):  
William C. Prentiss ◽  
Michael Lenert ◽  
Thomas A. Foor ◽  
Nathan B. Goodale ◽  
Trinity Schlegel

This paper provides an analysis of radiocarbon dates acquired during earlier and recent field seasons at the Keatley Creek site, southern British Columbia. Results indicate that early occupations predating 1900 cal. B.P. occurred, but were not likely associated with population aggregation and large housepits. The aggregated village appears to have emerged by approximately 1700 cal. B.P. and was abandoned at approximately 800 cal. B.P. A break in the occupational sequence is recognized at 1450-1350 cal. B.P. and one other short break may have occurred shortly after 1250 cal. B.P. Peak socioeconomic complexity appears to have been achieved between 1350 and 800 cal B.P. Climatic warming may have provided a selective environment favoring population aggregation and intensification during this time. The final abandonment of the Keatley Creek village appears to have been part of a regional phenomenon suggesting the possibility that climatic factors were important in this case as well.


2004 ◽  
Vol 31 (3) ◽  
pp. 177-180 ◽  
Author(s):  
HENRY P. HUNTINGTON ◽  
ROBERT S. SUYDAM ◽  
DANIEL H. ROSENBERG

The integration or co-application of traditional knowledge and scientific knowledge has been the subject of considerable research and discussion (see Johannes 1981; Johnson 1992; Stevenson 1996; McDonald et al. 1997; Huntington et al. 1999, 2002), with emphasis on various specific topics including environmental management and conservation (see Freeman & Carbyn 1988; Ferguson & Messier 1997; Ford & Martinez 2000; Usher 2000; Albert 2001). In most cases, examples of successful integration compare traditional and scientific observations at similar spatial scales to increase confidence in understanding or to fill gaps that appear from either perspective. We present a different approach to integration, emphasizing complementarity rather than concordance in spatial perspective, using two migratory species as examples.


Radiocarbon ◽  
1995 ◽  
Vol 37 (2) ◽  
pp. 103-110 ◽  
Author(s):  
Anna Pazdur ◽  
Mieczysław F. Pazdur ◽  
Jacek Pawlyta ◽  
Andrzej Górny ◽  
Michał Olszewski

We report preliminary results of a long-term systematic study intended to gather paleoclimatic records from precisely dated speleothems. The research project is limited to speleothems deposited in caves of the Cracow-Wieluń Upland, the largest and best-explored karst region in Poland, covering ca. 2900 km2 with >1000 caves. Speleothem samples were selected from collections of the Geological Museum of the Academy of Mining and Metallurgy in Cracow. Radiocarbon dates of these samples from ca. 45–20 ka bp almost exactly coincide with age range of the Interplenivistulian. A break in speleothem formation between ca. 20 and 10 ka bp may be interpreted as a result of serious climatic deterioration associated with the maximum extent of the last glaciation. We observed differences among 14C, U/Th and AAR dating results. Changes of δ13C and δ18O in speleothems that grew between ca. 30 and 20 ka bp may be interpreted as changes of paleoclimatic conditions.


2002 ◽  
Vol 33 ◽  
pp. 9-19 ◽  
Author(s):  
David Mattingly ◽  
David Edwards ◽  
John Dore

AbstractThis short paper presents a full list of the currently available radiocarbon dates from the work of Charles Daniels in the 1960s-1970s and the Fazzan Project (1997-2001). The dates can be grouped into several categories, by site or area, and demonstrate the potential of radiocarbon dating being applied to historic-period archaeology in the Sahara. This complements earlier Italian work on later prehistory. One of the most important conclusions to emerge is that the construction of castle-like buildings in Fazzan began within the Garamantian period and that some of the numerous well-preserved mudbrick fortified sites are thus rather earlier than has previously been envisaged. A second important conclusion is that the use of AMS dating can help to identify and confirm activity of the post-Garamantian and early Islamic phases, which has hitherto been elusive.


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