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PROGRESS TOWARDS A BYZANTINE-MEDIEVAL HISTORIC BUILDINGS TREE-RING CHRONOLOGY FROM CYPRUS USING DENDROCHRONOLOGY AND RADIOCARBON

Published online by Cambridge University Press:  02 October 2023

Sturt W Manning*
Affiliation:
Cornell Tree Ring Laboratory, Department of Classics, and Cornell Institute for Archaeology and Material Studies, Cornell University, Ithaca NY 14853, USA The Science and Technology in Archaeology and Culture Research Center, The Cyprus Institute, 20 Konstantinou Kavafi Street, 2121 Aglantzia, Nicosia, Cyprus
Brita Lorentzen
Affiliation:
Cornell Tree Ring Laboratory, Department of Classics, and Cornell Institute for Archaeology and Material Studies, Cornell University, Ithaca NY 14853, USA Department of Anthropology, 355 South Jackson Street, Baldwin Hall, Room 250, University of Georgia, Athens GA 30602, USA
Nikolas Bakirtzis
Affiliation:
The Science and Technology in Archaeology and Culture Research Center, The Cyprus Institute, 20 Konstantinou Kavafi Street, 2121 Aglantzia, Nicosia, Cyprus
Mehmetcan Soyluoğlu
Affiliation:
The Science and Technology in Archaeology and Culture Research Center, The Cyprus Institute, 20 Konstantinou Kavafi Street, 2121 Aglantzia, Nicosia, Cyprus
*
*Corresponding author. Email: sm456@cornell.edu
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Abstract

The rich architectural heritage of Cyprus from the period of Byzantine and Latin rule includes 10 churches inscribed in the UNESCO World Heritage list. Most of these monuments preserve wooden elements: whether structural, decorative or furnishings. Many preserve wall paintings that are considered among the best examples of Byzantine and Medieval art in the Eastern Mediterranean. The dating of these paintings as well as the church buildings themselves, has been based mainly on style, with occasional dedicatory inscriptions and related historical interpretation. We report early results from a project investigating the wooden cultural heritage of Cyprus and in particular the combined use of dendrochronology with radiocarbon via tree-ring sequenced 14C wiggle-matching to help place initial tree-ring sequences. This includes a floating 264-year Pinus brutia chronology from several monuments, which, with a ca. 5-year gap, suggests prospects for >700-years of P. brutia chronology for Cyprus, and, with one gap of several decades to fill, ca. 1100 years of Pinus nigra chronology for Cyprus. Several currently floating elements from the multi-phase UNESCO-listed Timios Stravros church at Pelendri, including a terminus post quem for the celebrated liturgical wooden cross, are approximately dated across the 11th to 16th centuries AD.

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

Figure 1 (a) Map of Cyprus indicating the locations of the sites/places mentioned in the text. ANIK: Agios Nikolaos, Agios Nikolaos village; CSZ: Agios Sozomenos, Galata; GPAN: Panagia Podithou, Galata; KPAN: Panagia Chrysokourdaliatissa, Kourdali; MAIL: Monastery of Agios Ioannis Lambadistis; PAF: Pafos Gate, Nicosia; STAM: Stavros tou Agiasmati; TIMT: Timios Stavros church, Pelendri; TSAN: Agios Nikolaos, Tsakistra. Map created in OxCal 4.4.4 using USGS imagery. (b) View of the Timios Stavros church at Pelendri, north wall/entrance. (c) Balcony on its E-W support beams into/through the west wall of the Timios Stavros church, with TIMT-10 indicated. Photos: Sturt Manning.

Figure 1

Table 1 Samples and the radiocarbon dates employed in this study. The quoted GrM (Groningen) δ13C values were determined independently via IRMS; the quoted VERA (Vienna) δ13C values were as determined with the AMS system. Dates on crossdated samples placed as belonging to the identical relative years (RY) were combined into a weighted average (and tested whether consistent with this assumption) following Ward and Wilson (1978) using the R_Combine function in OxCal. Each tree-ring sample was originally measured in terms of relative years (RY) starting from RY1001. Subsequent crossdating can then lead to revised RY placement versus other samples.

Figure 2

Figure 2 Tree-ring sequenced 14C wiggle-match of the P. brutia Byzantine Cyprus Pine Master (BCPM). (a) Radiocarbon date ranges (68.3% highest posterior density, hpd, and 95.4% hpd) from the sets of 5 tree-rings from the crossdated Pafos Gate (PAF) and Panagia Chrysokourdaliotissa, Kourdali (KPAN) series, both parts of the crossdated BCPM chronology running from Relative Year (RY) 943–1206, wiggle-match fitted against the IntCal20 14C calibration curve (data plotted at midpoint of each 5-ring/year block). (Note: an alternative presentation of this wiggle-match is shown in the Online Supplementary Material.) (b) The calculated calendar date probability, 68.3% and 95.4% hpd ranges, and median and mean values for the last extant tree-ring, RY1206, of the current BCPM chronology. (c) The constituent elements of the BCPM chronology shown as bars representing the years included as part of each site or element with the combined tree-ring width (TRW) chronology for the BCPM chronology shown above (relative, indexed, scale).

Figure 3

Figure 3 14C wiggle-matches on elements of the Timios Stavros church, Pelendri (TIMT). (a) Dendro-sequenced 14C wiggle-match placement of the series of three 14C dates on TIMT-2 showing the modeled 68.3% hpd calendar age ranges (smaller, solid, darker histograms) and the 95.4% hpd calendar age ranges (larger, light-shaded, histograms) for the three 14C ages (Y axis ranges) given the tree-ring sequence constraints versus the IntCal20 14C calibration curve. (b) The modeled calendar probability for the last extant tree-ring, RY1113, from the chronology comprising TIMT-2+3+17+70. Since no bark or outermost tree-ring is present, this date is a TPQ for the use date. (c) Dendro-sequenced 14C wiggle-match placement of the series of three 14C dates on TIMT-5. (d) The modeled calendar probability for the last extant tree-ring, RY1131, from TIMT-5. Since no bark or outermost tree-ring is present, this date is a TPQ for the use date. (e) Dendro-sequenced 14C wiggle-match placement of the series of three 14C dates on TIMT-10. (f) The modeled calendar probability for the last extant tree-ring, RY1338, from TIMT-10. Since no bark or outermost tree-ring is present, this date is a TPQ for the use date—although, as a mature sample, and with most of part of the transverse section used, it appears likely the last extant tree-ring is not too far from the original exterior. (Note: alternative presentations of the wiggle-matches for 3a, 3c and 3e are shown in the Online Supplementary Material.)

Figure 4

Figure 4 Dendro-sequenced 14C wiggle-match placement of the series of three 14C dates on TIMT-1, the Holy Cross, from Timios Stavros church, Pelendri. (a) The modeled (solid, darker histograms) and non-modeled (light-shaded histograms) overall probability for the three 14C dates given the tree-ring sequencing versus the IntCal20 14C calibration curve. Note there are multiple plausible possible ranges. (Note: an alternative presentation of this wiggle-match is shown in the Online Supplementary Material.) (b) Detail of the fit probabilities for the RY1145-1149 sample in (a) showing the two possible ranges at 68.3% hpd and three possible ranges at 95.4% hpd. The central range (of the three possible ranges at 95.4% hpd) is clearly the most likely. (c) The modeled calendar probability for the last extant tree-ring preserved in the cross, RY1163, as derived from the wiggle-match. The most likely sub-ranges are 982–1010 Cal AD (51.5% probability from the 68.3% hpd range) or 956–1012 Cal AD (65.4% probability from the 95.4% hpd range).

Figure 5

Figure 5 (a) Tree-ring width patterns, shown as offset indexed values, comparing the (i) known-age P. nigra Troodos (Chionistra) chronology of Touchan et al. (2014a,b) versus (ii) the TIMT-75+76 iconostasis doors P. nigra chronology placed at the tentative best crossdate versus (i), and then with (iv) the GPAN early P. nigra chronology placed at the tentative best crossdate against (ii) and then with (iii) the 264-year CBPM P. brutia chronology placed at the best crossdate versus (iv)—this crossdate is also (well) within the 68.3% hpd best fit range for the chronology from the 14C wiggle-matches in Figures 2 and 5b, c (and is also consistent with a preliminary tentative crossdate versus a Cyprus Cedrus brevifolia chronology to be reported on in future work). The t (Baillie and Pilcher 1973) values cited are those from the Corina software (Harris 2007). (b) Tree-ring sequenced 14C wiggle-match of 14C dates on the BCPM chronology (PAF-6 and KPAN-3 samples) as in Figure 2 combined, via the tentative dendrochronological crossdate in (a), with the set of 14C dates on samples from the GPAN early P. nigra chronology (the latter now placed in terms of the BCPM relative years, RY). (Note: an alternative presentation of this wiggle-match is shown in the Online Supplementary Material.) (c) Calendar placement of the end of the BCPM chronology (RY1206) according to the tree-ring sequenced 14C wiggle-match shown in (b).

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