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POTTERY PRODUCTION, EXCHANGE AND CONSUMPTION IN LATE BRONZE AGE MAGNESIA (THESSALY): RESULTS OF NEUTRON ACTIVATION ANALYSIS OF POTTERY FROM DIMINI, VOLOS (NEA IONIA, KASTRO/PALAIA), PEFKAKIA AND VELESTINO

Published online by Cambridge University Press:  22 May 2023

Bartłomiej Lis*
Affiliation:
Polish Academy of Sciences
Anthi Batziou
Affiliation:
Ephorate of Antiquities of Magnesia
Vassiliki Adrymi-Sismani
Affiliation:
Ephorate of Antiquities of Magnesia
Hans Mommsen
Affiliation:
University of Bonn
Joseph Maran
Affiliation:
University of Heidelberg
Susanne Prillwitz
Affiliation:
University of Basel
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Abstract

This article presents the results of Neutron Activation Analysis (NAA) of, altogether, 145 pottery and clay samples deriving from five sites located in the Thessalian region of Magnesia: Dimini, Nea Ionia, Kastro/Palaia (Volos), Pefkakia and Velestino. Chronologically, the sampled pottery covers the entire Late Bronze Age (LBA), with a few samples dating to the Middle Bronze Age. Within this broad chronological range, Mycenaean-type pottery dominates, the majority of it being decorated, with an addition of fine unpainted pottery and such used for transport and cooking. Pottery of non-Mycenaean derivation is represented by a variety of types belonging to the early LBA as well as two classes of the early post-palatial period (i.e. after 1200 BC): Handmade Burnished Ware and Grey Ware. Importantly, samples associated with two pottery kilns at Dimini and Velestino were included in the project, although no kiln wasters were identified. Results of the analysis provide important insights into both local Thessalian pottery production and inter- and intra-regional pottery exchange. Local production utilising clay beds around Dimini is best evidenced, with a distribution of its products reaching beyond Thessaly. Two further chemical patterns appear to be associated with Velestino, while an additional two small chemical groups are likely Thessalian as well. In terms of identified imports, the Argolid stands out as the major source of non-local pottery from the beginning of the LBA until the end of the palatial period. Other regions and production localities play a significantly smaller role as sources of supply. On the basis of the study, for the first time the local production as well as importation of pottery in the region of Magnesia is documented by scientific means, opening new research perspectives and strengthening the region's standing as part of the Mycenaean world.

Αυτό το άρθρο παρουσιάζει τα αποτελέσματα της Ανάλυσης με Ενεργοποίηση Νετρονίων (NAA) συνολικά 145 δειγμάτων κεραμικής και πηλού, που προέρχονται από πέντε θέσεις από την περιοχή της Μαγνησίας στη Θεσσαλία: Διμήνι, Νέα Ιωνία, Κάστρο/Παλαιά (Βόλος), Πευκάκια και Βελεστίνο. Χρονολογικά, η κεραμική, στην οποία πραγματοποιήθηκε δειγματοληψία, καλύπτει ολόκληρη την Ύστερη Εποχή του Χαλκού, ενώ λίγα δείγματα χρονολογούνται στη Μέση Εποχή του Χαλκού. Μέσα σε αυτό το ευρύ χρονολογικό φάσμα κυριαρχεί η μυκηναϊκού τύπου κεραμική, η πλειονότητα της οποίας είναι διακοσμημένη, ενώ συμπεριλαμβάνεται λεπτή άβαφη κεραμική, καθώς και αυτή που χρησιμοποιείται για μεταφορά και μαγείρεμα. Η κεραμική που δεν συγκαταλέγεται στη μυκηναϊκή, αντιπροσωπεύεται από μια ποικιλία τύπων που ανήκουν στην πρώιμη φάση της Ύστερης εποχής του Χαλκού καθώς και σε δύο κατηγορίες της πρώιμης μεταανακτορικής περιόδου (δηλαδή μετά το 1200 π.Χ.) - χειροποίητη στιλβωμένη και τεφρή κεραμική. Είναι σημαντικό ότι στη μελέτη συμπεριλήφθηκαν δείγματα που σχετίζονται με δύο κεραμικούς κλιβάνους στο Διμήνι και στο Βελεστίνο, αλλά δεν εντοπίστηκαν απορρίματα από αυτούς. Τα αποτελέσματα της ανάλυσης παρέχουν σημαντικές γνώσεις τόσο για την τοπική θεσσαλική παραγωγή κεραμικής όσο και για τις ενδοπεριφερειακές και διαπεριφερειακές ανταλλαγές κεραμικής. Η τοπική παραγωγή που χρησιμοποιεί κοιτάσματα πηλού που εντοπίζονται γύρω από το Διμήνι τεκμηριώνεται καλύτερα, με τη διακίνηση των προϊόντων της να ξεπερνάει τα όρια της Θεσσαλίας. Δύο ακόμη χημικές ομάδες φαίνεται να συνδέονται με το Βελεστίνο, ενώ δύο επιπλέον μικρές χημικές ομάδες είναι πιθανώς επίσης Θεσσαλικές. Όσον αφορά τις προσδιοριζόμενες εισαγωγές, η Αργολίδα ξεχωρίζει ως η κύρια πηγή μη τοπικής κεραμικής από την αρχή της Ύστερης εποχής του Χαλκού μέχρι το τέλος της ανακτορικής περιόδου. Άλλες περιοχές και τόποι παραγωγής διαδραματίζουν σημαντικά μικρότερο ρόλο ως πηγές εφοδιασμού. Με βάση τη μελέτη, για πρώτη φορά τεκμηριώνεται με επιστημονικά μέσα η τοπική παραγωγή αλλά και η εισαγωγή αγγείων στην περιοχή της Μαγνησίας, ανοίγοντας νέες ερευνητικές προοπτικές και ενισχύοντας τη θέση της περιοχής ως μέρος του μυκηναϊκού κόσμου.

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Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
Copyright © The Author(s), 2023. Published by Cambridge University Press on behalf of The Council, British School at Athens
Figure 0

Fig. 1. Map of Greece showing sites and regions mentioned in the text.

Figure 1

Fig. 2. View of the Bay of Volos with location of sites (except for Velestino) that were included in sampling. Base map: Google Earth.

Figure 2

Fig. 3. Plan of Dimini showing contexts from which samples were selected.

Figure 3

Fig. 4. Plan of Kastro/Palaia showing locations of rescue excavations from which samples were selected, as well as the excavations of Theocharis with substantial Mycenaean structures (© plan by T. Ross).

Figure 4

Fig. 5. Plan of Pefkakia Magoula with highlighted contexts from which samples were selected. Modified after Maran 1992, plan I.

Figure 5

Fig. 6. Photograph of excavations at the site of Mycenaean Pefkakia, south of Magoula, with highlighted context (Room 1) from which samples were selected. North at the bottom of the photograph. Modified after Batziou-Efstathiou 2015a, fig. 6.

Figure 6

Fig. 7. View of Velestino with location of kiln in relation to the site of Magoula Bakali. Base map: Google Earth, photograph of the kiln after Batziou-Efstathiou 1994, fig. 2.

Figure 7

Table 1. Average concentration values M in μg/g (ppm), if not indicated otherwise, of groups of samples in the Thessaly dataset of this project. σ is the standard deviation (root mean square deviation) in %. All member samples of the groups in the Bonn databank are shown. The individual samples have been corrected with a best relative factor with respect to the grouping values (given in Table 2).

Figure 8

Table 2. Dilution or elutriation factors of the individual samples of the groups applied to the raw NAA concentration data forming the groups (w = repetition measurement).

Figure 9

Fig. 8. Result of a discriminant analysis (DA) of 74 samples, corrected for dilution, assuming the six clusters given in Table 1 using all elements shown there except As, Ba, Ca, Na, Ti. Plotted are the discriminant functions W1 and W2, which cover 76.3% and 11.1% of the between-group variance. The ellipses drawn are the 2σ boundaries of the groups.

Figure 10

Fig. 9. Result of a discriminant analysis (DA) as in Fig. 8, including now three additional clusters (MYBE, EuA, TheB). Plotted are the discriminant functions W1 and W3, which cover 92.1% and 2.7% of the between-group variance. The groups MYBE and X119 overlap here, but are resolved in other projections (group centres of MYBE: W1 = -163.8, W2 = 1.48, W3 = -41.6 and of X119: W1 = -163.2, W2 = -7.2, W3 = -41.2): all groups are well separated in the multidimensional concentration space.

Figure 11

Table 3. Provenance as determined by NAA of different pottery groups analysed in the project.

Figure 12

Table 4. Share of samples with particular/without provenance determined by NAA at the sites included in the project

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