# Towards an Absolute Chronology for the Aegean Iron Age: New Radiocarbon Dates from Lefkandi, Kalapodi and Corinth

Michael Toffolo, Alexander Fantalkin, Irene Lemos, Rainer Felsch, Wolf-Dietrich Niemeier, Guy Sanders, Israel Finkelstein, Elisabetta Boaretto, Roberto Macchiarelli

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Michael Toffolo, Alexander Fantalkin, Irene Lemos, Rainer Felsch, Wolf-Dietrich Niemeier, et al. "Towards an Absolute Chronology for the Aegean Iron Age: New Radiocarbon Dates from Lefkandi, Kalapodi and Corinth." PLoS ONE, 2013, 8 (12), e0083117. [DOI: 10.1371/journal.pone.0083117](https://doi.org/10.1371/journal.pone.0083117). [HAL Id: hal-01877870](https://hal.science/hal-01877870v1)

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<figure><img src="image_1.png" /></figure>
# Towards an Absolute Chronology for the Aegean Iron Age: New Radiocarbon Dates from Lefkandi, Kalapodi and Corinth

Michael B. Toffolo<sup>1,2*</sup>, Alexander Fantalkin<sup>2</sup>, Irene S. Lemos<sup>3</sup>, Rainer C. S. Felsch<sup>4</sup>,
Wolf-Dietrich Niemeier<sup>5</sup>, Guy D. R. Sanders<sup>6</sup>, Israel Finkelstein<sup>2</sup>, Elisabetta Boaretto<sup>1,7</sup>

1 Kimmel Center for Archaeological Science, Weizmann Institute of Science, Rehovot, Israel, 2 Sonia and Marco Nadler Institute of Archaeology, Tel Aviv University, Tel Aviv, Israel, 3 Merton College, University of Oxford, Oxford, United Kingdom, 4 Haferkamp 3c, Isernhagen, Germany, 5 German Archaeological Institute at Athens, Athens, Greece, 6 American School of Classical Studies at Athens, Corinth Excavations, Ancient Corinth, Greece, 7 Weizmann Institute-Max Planck Center for Integrative Archaeology, D-REAMS Radiocarbon Laboratory, Weizmann Institute of Science, Rehovot, Israel

## Abstract

The *relative* chronology of the Aegean Iron Age is robust. It is based on minute stylistic changes in the Submycenaean, Protogeometric and Geometric styles and their sub-phases. Yet, the *absolute* chronology of the time-span between the final stages of Late Helladic IIIC in the late second millennium BCE and the archaic colonization of Italy and Sicily toward the end of the 8th century BCE lacks archaeological contexts that can be *directly* related to events carrying absolute dates mentioned in Egyptian/Near Eastern historical sources, or to well-dated Egyptian/Near Eastern rulers. The small number of radiocarbon dates available for this time span is not sufficient to establish an absolute chronological sequence. Here we present a new set of short-lived radiocarbon dates from the sites of Lefkandi, Kalapodi and Corinth in Greece. We focus on the crucial transition from the Submycenaean to the Protogeometric periods. This transition is placed in the late 11th century BCE according to the Conventional Aegean Chronology and in the late 12th century BCE according to the High Aegean Chronology. Our results place it in the second half of the 11th century BCE.

**Citation:** Toffolo MB, Fantalkin A, Lemos IS, Felsch RCS, Niemeier W-D, et al. (2013) Towards an Absolute Chronology for the Aegean Iron Age: New Radiocarbon Dates from Lefkandi, Kalapodi and Corinth. PLoS ONE 8(12): e83117. doi:10.1371/journal.pone.0083117

**Editor:** Roberto Macchiarelli, Université de Poitiers, France

**Received:** July 4, 2013; **Accepted:** October 30, 2013; **Published:** December 26, 2013

**Copyright:** © 2013 Toffolo et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

**Funding:** The research leading to these results has received funding from the European Research Council under the European Community's Seventh Framework Program (FP7/2007–2013)/ERC grant agreement number 229418. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

**Competing Interests:** The authors have declared that no competing interests exist.

* E-mail: michael.toffolo@weizmann.ac.il

## Introduction

The absolute chronology of the different phases of the Iron Age in the Aegean has been debated during the last decade [1–9]. This is not surprising since any significant change in the dates would affect the entire Mediterranean basin, far beyond the Greek shores.

The disagreement regarding the chronology of the Aegean Iron Age is a result of an inherent problem in the archaeology of this region. The strength of the Greek painted pottery is in its robust *relative* sequence, including rapid stylistic changes. Yet, it is difficult to tie this relative scheme into an *absolute* dating system. This is so because the period between the final stages of the Late Helladic IIIC (LH IIIC) in the late second millennium BCE and the archaic colonization of Italy and Sicily toward the end of the 8th century BCE lacks archaeological contexts that can be *directly* related to events carrying absolute dates, such as layers with Egyptian items bearing names of well-dated pharaohs. Scholars of the Aegean Iron Age who tried to resolve the problem have therefore been forced to resort to comparative material from the East, that is, to Levantine sites which yielded Greek Protogeometric (PG) and Geometric (G) items, such as the old excavations at Samaria, Megiddo and Tell Abu Hawam [10]. Yet, this too did not save the

day, because: a) the Aegean items found in these sites did not come from stratigraphically secure contexts; b) the date of the relevant layers in the Levant was also debated [11,12], mainly because it was founded on biblical texts whose historicity has been challenged [13–16].

This resulted in two contrasting systems for the PG and G phases in the Greek world: the Conventional Aegean Chronology, which followed the Samaria-based Low Palestinian Chronology of Crowfoot-Kenyon, and the Aegean High Chronology based on the traditional High (biblical-based) Palestinian Chronology [17]. The appearance of the new Low Chronology for the Levant [14,18,19], which roughly corresponds to the old Low Palestinian Chronology of Crowfoot-Kenyon and therefore to the Conventional Aegean Chronology, has been embraced by the scholars working in the Aegean [12]. However, the debate is far from being resolved, because of recent attempts, based on radiometric dates from Italy, Spain and Tunisia [4], to raise the Aegean Chronology by more than a century. This would be in line with the High Palestinian Chronology, although the latter appears obsolete even according to the Modified Conventional Chronology for the Levant proposed by Mazar [20,21], which differs from the Low Chronology of Levant by only a few decades. The renewed High Chronology for the Aegean has been criticized regarding
<figure><img src="image_2.png" /></figure>

**Figure 1.** *High and Low absolute chronologies for the ceramic phases of the Aegean Iron Age, based on [12,17]. LH IIIC: Late Helladic IIIC; SM: Sub-Mycenaean; EPG: Early Proto-Geometric; MPG: Middle Proto-Geometric; LPG: Late Proto-Geometric; EG: Early Geometric; MG: Middle Geometric; LG: Late Geometric.*

doi:10.1371/journal.pone.0083117.g001

unreliable contexts and problematic interpretation of the data [7],
and the dispute continues [6] (Fig. 1).

The debate in the Levant involved approximately the same time-frame as in the Aegean – between the collapse of Egyptian rule in Canaan in the late 12th century and the beginning of Assyrian domination in the late 8th century [14]. In order to resolve it, starting in the late 1990s scholars turned to radiocarbon dating, with impressive success [19,22,23]. Though the results have been interpreted in different and sometimes contrasting ways, a general trend toward the Low Chronology is well-established by now [18,20]. Dates for some Aegean Iron Age sites, mostly peripheral, have also been published [1,2,24–27], but so far a *systematic* attempt to date the PG and G sequence in Greece by means of radiocarbon analyses has not been attempted.

Establishing a reliable radiocarbon-based chronological system
for the Iron Age phases in the Aegean depends on: a) secure

stratigraphic contexts; b) with good pottery assemblages (which
provide the basis for the *relative* Greek system); c) which can be
dated by short-lived samples. This has been the goal of the
radiocarbon track-team working in the framework of a European
Research Council-funded project on Iron Age Levantine archae-
ology and the exact and life sciences. Here we report the results of
our work in the last four years in three sites in Greece: Lefkandi
[28], Kalapodi [29,30], and Corinth [31] (Fig. 2).

**Materials and Methods**

Selection of sites and focus of research

The three sites discussed here were conceived as suitable for our
purpose for a number of reasons:

1. They feature a stratigraphic sequence that covers a long time range from the LH IIIC through to the G period; the possibility
<figure><img src="image_3.png" /><figcaption>Figure 2. Map of the Aegean showing the locations of the sites mentioned in the article.</figcaption></figure>

doi:10.1371/journal.pone.0083117.g002

of dating a full sequence is a key factor in the establishment of a
solid absolute chronology, because this is the only way to
determine transitions between phases and their duration using
Bayesian analysis [32,33].

2. They are located in the central part of Greece and represent the relative chronological sequence of three important regions, namely Euboea (Lefkandi), Phocis (Kalapodi) and Corinthia (Corinth). The links between the ceramic assemblages of these areas are well known, as well as those with neighboring regions, thus allowing a good control over the accuracy of the radiocarbon measurements vis-à-vis the relative system of the Aegean PG and G periods.

3. They have been carefully excavated and studied for decades and the given expeditions are still operating in the field, a situation that facilitated the retrieval of samples from museums, storage facilities and the field, and provided access to the relevant documentation.

The characteristics mentioned above are essential in order to
obtain a reliable set of radiocarbon dates, but they are not enough.
Samples should come from primary contexts which did not
undergo any type of disturbance after their deposition, such as
hearths and cooking installations, occupational accumulations on
floors and single-burial inhumations. These contexts should
feature well-defined ceramic assemblages, which provide the basis
for the entire discussion. Destruction layers are especially
important in this sense, as they represent short events in time and usually seal assemblages of complete vessels and clusters of short-lived samples, such as charred seeds, which are less likely to bear the “old wood” effect.

Some of these “ideal” criteria could not be applied in the sites under investigation. First, no destruction layers were found (they are not easy to come by in Greek sites), and therefore we were not able to collect samples from contexts with rich assemblages of complete vessels (e.g. Lefkandi and Kalapodi). As a result, in most cases we did not work with clusters of short-lived samples, such as olive pits and grain seeds. Also, when a good pottery assemblage was available, in several cases we could not find preserved collagen in bones. This is so for the horse bone from the famous Toumba in Lefkandi [28] and for some of the graves that were tested in Corinth [34–36] (results not included in this study). Still, we were able to collect a substantial amount of material, representing the LH IIIC, Submycenaean (SM) and PG periods (16 samples; Table 1). Evidently, they are not enough for a comprehensive dating of all the phases of the Iron Age. For instance, the PG/G transition could not be determined with precision, as only three dates (in addition to the 16 mentioned above) are available for the G period. Yet, what we did obtain allows the calculation of the highly important SM/PG transition using Bayesian analysis [32,33] (this transition is labeled as LH IIIC Late-SM/EPG in the Bayesian models, Fig. 3–6). Good results for this transition can serve as a crucial peg for the Aegean Iron Age chronology. This is the focus of our article.

## Sampling and measurement strategy

The original idea was to collect samples from the field, but the strict quality-control criteria employed in screening the archaeological contexts [4,19,37,38] left no suitable items. Nevertheless, it was possible to choose samples collected during past excavation seasons. As shown in [39], it is inappropriate to average dates obtained from different single short-lived samples even if they are found within the same layer and sometime even specific context; since the relationship between single samples is often unknown, they might have been deposited in different events in the history of a given layer, which can be decades apart. Therefore, we opted for clusters of seeds and/or bones where possible. Also, we decided to measure more than once all the samples for which we had enough material, in order to increase the precision of the dates. We believe that this is an essential step when dealing with many time-spans such as the phases of the Aegean Iron Age, which could have been shorter than a typical AMS uncertainty in the measurement (±50 years). In one case – the Toumba of Lefkandi – we decided to sample long-lived material (wood), taking into account the paucity of short-lived samples within this context, which we consider “sealed” and hence very reliable. This date will be considered as a *terminus post quem*.

Samples were thus collected in 2009, 2010 and 2012 from the excavations' storages and from museums, and their provenience was carefully checked with the excavators. Samples were taken in cooperation with the directors of the excavations (among the authors) and with the necessary permits from the Greek Ministry of Culture. Not working in the field, it was impossible to analyze the sediments associated with the samples in order to get more information about site-formation and post-depositional processes which could have affected the contexts [38,40]. Only the context of sample RTT-6104 was analyzed using the microarchaeological approach of [39]. The sediment associated with this charcoal sample turned out to be in secondary deposition (see below), and therefore not reliable from a stratigraphic point of view. Nevertheless, it was dated in order to get an idea of the degree

of “noise” from residual material within the stratigraphic/ceramic sequence. Bone samples were pre-screened at the sampling location in Greece in order to have a first glimpse regarding the preservation of collagen. In the case of Corinth, for instance, 13 samples were pre-screened, but only 7 yielded an insoluble fraction. About 200 mg of bone powder (ca. a full teaspoon) obtained by manually grinding clean bone fragments with an agate mortar and pestle were dissolved with ~20 ml of 1N HCl inside a plastic ziplock bag. The occurrence of an insoluble fraction, floating within the solution and resembling gel, was a good hint for the presence of collagen [40].

## Laboratory procedures

The selected bones were further analyzed by means of Fourier-Transform infrared spectrometry (FTIR) in the Radiocarbon Laboratory at the Weizmann Institute of Science [41]. A total of 19 samples (Table 1) were processed for radiocarbon dating. Charred seeds, charcoal, bones, wood and textile were pre-treated at the Weizmann Institute of Science following [41,42] in order to remove all contaminants. The procedure for charred remains is based on the acid-base-acid (ABA) method as in [41,42], whereas bones were further subjected to ultra-filtration as in [41]. After the pre-treatment, the degree of purity of the charcoal and collagen was determined using FTIR spectrometry. Then, the samples were oxidized in vacuum with CuO at 900°C and prepared as graphite for ¹⁴C determination using accelerator mass spectrometry (AMS). The amount of carbon obtained was enough (40% or more) for the AMS measurements. Measurements were performed at the NSF-AMS Radiocarbon Laboratory at University of Arizona, Tucson. Radiocarbon dates are reported in conventional ¹⁴C years before present (BP) following the international convention [43]. All calculated ¹⁴C ages have been corrected for isotopic fractionation based on the stable carbon isotope ratio (δ¹³C value). Calibrated ages in calendar years have been obtained from the calibration tables of [44] using OxCal v 4.1.7 [33,45]. The same software was used for the Bayesian analysis of the radiocarbon dates [32,33,45]. Carbon and nitrogen isotopic values were obtained using a Thermo Scientific EA1112 analyzer linked to a DELTA V isotope ratio mass spectrometer.

## Bayesian analysis

Groups of radiocarbon dates can be analyzed using Bayesian statistics [32,33,45]. This methodology allows the identification of outliers and their rejection based on a number of constraints provided by stratigraphic and contextual information. As a result, absolute chronological sequences become more precise and accurate.

When possible, the samples were collected from contexts which feature a single Aegean ceramic phase assemblage. Sometimes the ceramic evidence was less than ideal, forcing the excavators to label the context as belonging to a longer period, encompassing more than one relative ceramic phase, for instance “LH IIIC Late to SM”. In such a case, in the Bayesian models we maintained the excavators’ affiliation and classified the two phases as belonging to one block. This procedure allowed us to check constraints which originate from the pottery sequence of the given sample: according to this method, a date that shows poor agreement in, e.g., the LH IIIC Late to SM phase might fit the model better if placed in the LH IIIC Late only, that is, with the phase labeled in the model LH IIIC Middle to Late. Similarly, samples labeled by the excavators as “PG” or “G”, with no further subdivision to early, middle or late, were considered as contemporary with the entire block (e.g. sample RTK-6697 is contemporary to other samples belonging to
<table><caption>**Table 1.** ¹⁴C results obtained for the samples from Kalapodi, Lefkandi and Corinth with ceramic phase, laboratory number, material identification, context description, sample ID, ¹⁴C age in yr BP, calibrated ranges for ±1σ and ±2σ, and ‰ δ¹³C.</caption><thead><tr><th>Ceramic phase</th><th>Lab #</th><th>Type</th><th>Context</th><th>Site and sample ID</th><th>¹⁴C age ±yr BP</th><th>Calibrated range ±1σ (BCE)</th><th>Calibrated range ±2σ (BCE)</th><th>δ¹³C (‰)</th></tr></thead><tbody><tr><td>LH IIIC early to middle</td><td>RTK-6370</td><td>Charred wheat</td><td>Pit</td><td>Lefkandi, Basket 879, Area T North</td><td>2880±55</td><td>1187-1183 (1.1%), 1154-1146 (2.0%), 1130-976 (63.9%), 952-947 (1.2%)</td><td>1258-1233 (2.9%), 1217-916 (92.5%)</td><td>-22.7</td></tr><tr><td>LH IIIC middle to late</td><td>RTT-6104</td><td>Charcoal</td><td>Layer of burnt debris in standing section</td><td>Lefkandi, Area M, section 367</td><td>2980±55</td><td>1305-1126 (68.2%)</td><td>1388-1047 (95.4%)</td><td>-23.3</td></tr><tr><td>LH IIIC middle to late</td><td>RTK-6372 and RTK 6373</td><td>Charred wheat and chickpeas</td><td>Burnt debris</td><td>Kalapodi, KAL08 363 5035/4975</td><td>2930±25*<sup>a</sup> (6)</td><td>1208-1202 (2.6%), 1195-1140 (34.3%), 1135-1111 (14.5%), 1103-1076 (12.6%), 1065-1056 (4.2%)</td><td>1259-1232 (6.0%), 1218-1041 (89.4%)</td><td>-23.4 (RTK6372), -22.4 (RTK6373)</td></tr><tr><td>LH IIIC late to late</td><td>RTK-6374 and RTK 6375</td><td>Charred chickpeas and wheat</td><td>Hearth</td><td>Kalapodi, KAL08 368 5035/4975</td><td>2913±17*<sup>b</sup> (8)</td><td>1129-1051 (68.2%)</td><td>1195-1142 (18.4%), 1134-1021 (77.0%)</td><td>-22.8 (RTK6374), -23.8 (RTK6375)</td></tr><tr><td>LH IIIC late to SM</td><td>RTK-6123</td><td>Animal bone</td><td>Pit</td><td>Lefkandi, Area M, Pit 47, basket 5359</td><td>2975±30* (4)</td><td>1263-1190 (47.7%), 1180-1158 (11.9%), 1145-1131 (8.5%)</td><td>1369-1359 (0.7%), 1315-1113 (93.7%), 1099-1088 (0.8%), 1063-1059 (0.3%)</td><td>-19.0</td></tr><tr><td>LH IIIC late to SM</td><td>RTK-6124</td><td>Animal bone</td><td>Pit</td><td>Lefkandi, Area M, Pit 48, basket 5366 (top)</td><td>2850±30* (4)</td><td>1052-973 (57.7%), 958-939 (10.5%)</td><td>1116-925 (95.4%)</td><td>-19.4</td></tr><tr><td>LH IIIC late to SM</td><td>RTK-6127</td><td>Animal bone</td><td>Pit</td><td>Lefkandi, Area M, Pit 48, basket 5374 (bottom)</td><td>2920±30* (4)</td><td>1193-1174 (9.5%), 1166-1143 (11.6%), 1133-1051 (47.1%)</td><td>1256-1237 (3.7%), 1215-1014 (91.7%)</td><td>-19.6</td></tr><tr><td>LH IIIC late to SM</td><td>RTK-6156</td><td>Animal bone</td><td>Pit</td><td>Lefkandi, Area M, Pit 47, basket 5359</td><td>2855±50</td><td>1114-1097 (6.0%), 1092-972 (53.1%), 959-936 (9.1%)</td><td>1209-901 (95.4%)</td><td>-20.4</td></tr><tr><td>SM</td><td>RTK-6699</td><td>Human bone</td><td>Single burial [32-34]</td><td>Corinth, COR1969-33</td><td>2805±55</td><td>1042-897 (68.2%)</td><td>1118-833 (95.4%)</td><td>-19.7</td></tr><tr><td>EPG</td><td>RTK-6371</td><td>Charred wheat</td><td>Burnt debris, possibly of a hearth</td><td>Kalapodi, KAL08 322 5035/4975</td><td>2850±40* (2)</td><td>1109-1104 (1.8%), 1072-1066 (2.3%), 1056-970 (50.3%), 962-932 (13.8%)</td><td>1187-1184 (0.3%), 1153-1149 (0.3%), 1130-906 (94.8%)</td><td>-22.5</td></tr><tr><td>(E?)PG</td><td>RTK-6697</td><td>Human bone</td><td>Single burial [32-34]</td><td>Corinth, COR1973-4</td><td>2835±55</td><td>1110-1104 (1.8%), 1074-1065 (2.5%), 1056-913 (63.9%)</td><td>1192-1176 (1.4%), 1163-1143 (1.7%), 1132-843 (92.3%)</td><td>-19.5</td></tr><tr><td>(E?)PG</td><td>RTK-6698</td><td>Human bone</td><td>Single burial [32-34]</td><td>Corinth, COR1973-5</td><td>2520±60</td><td>790-731 (19.9%), 692-660 (11.2%), 651-544 (37.2%)</td><td>800-486 (90.4%), 463-448 (1.7%), 443-416 (3.3%)</td><td>nd</td></tr><tr><td>MPG to LPG</td><td>RTK-6384</td><td>Textile</td><td>Toumba [28]</td><td>Lefkandi, LEFT9</td><td>2880±40* (2)</td><td>1126-1001 (68.2%)</td><td>1209-969 (89.8%), 963-930 (5.6%)</td><td>-26.0</td></tr><tr><td>MPG to LPG</td><td>RTK-6385</td><td>Decayed wood</td><td>Toumba [28]</td><td>Lefkandi, LEFT10</td><td>2600±55</td><td>833-753 (55.3%), 686-668 (7.5%), 632-626 (1.3%), 612-596 (4.2%)</td><td>896-731 (65.5%), 692-660 (9.5%), 651-544 (20.3%)</td><td>-24.6</td></tr><tr><td>LPG</td><td>RTK-6397</td><td>Animal bone</td><td>Fill with ceramics</td><td>Kalapodi, KAL05 146 5030/4965</td><td>2742±29* (4)</td><td>908-841 (68.2%)</td><td>972-959 (3.0%), 936-819 (92.4%)</td><td>-22.4</td></tr></tbody></table>
<table><caption>Table 1. Cont.</caption><thead><tr><th>Ceramic phase</th><th>Lab#</th><th>Type</th><th>Context</th><th>Site and sample ID</th><th><sup>14</sup>C age ± yr BP</th><th>Calibrated range ±1σ (BCE)</th><th>Calibrated range ±2σ (BCE)</th><th>δ<sup>13</sup>C (%)</th></tr></thead><tbody><tr><td>SPG</td><td>RTK 6396</td><td>Animal bone</td><td>Sacrifice place related to altar</td><td>Kalapodi, KAL05 131 5030/4965-70</td><td>2888±28* (4)</td><td>1116-1021 (68.2%)</td><td>1194-1142 (7.9%), 1133-979 (87.5%)</td><td>-19.7</td></tr><tr><td>(E?)G</td><td>RTK-6701</td><td>Human bone</td><td>Single burial [32-34]</td><td>Corinth, COR1969-29</td><td>2760±60</td><td>976-952 (10.4%), 946-833 (57.8%)</td><td>1049-805 (95.4%)</td><td>-19.4</td></tr><tr><td>MG</td><td>RTK-6702</td><td>Human bone</td><td>Single burial [32-34]</td><td>Corinth, COR1971-2</td><td>2855±55</td><td>1115-971 (58.7%), 960-935 (9.5%)</td><td>1252-1241 (0.7%), 1213-897 (94.7%)</td><td>-19.6</td></tr><tr><td>MG to LG</td><td>RTK-6395</td><td>Animal bone</td><td>Fill with ceramics</td><td>Kalapodi, KAL05 70 5030/4965</td><td>2445±55</td><td>746-689 (18.3%), 664-646 (5.7%), 552-412 (44.2%)</td><td>761-682 (22.3%), 671-405 (73.1%)</td><td>-19.2</td></tr></tbody></table>

The samples are ordered according to the relative chronological sequence. LH: IIIC; Late Helladic; IIIC: SM: Sub-Mycenaean; EPG: Early Proto-Geometric; MPG: Middle Proto-Geometric; LPG: Late Proto-Geometric; SPG: Sub-Proto-

Geometric; EG: Early Geometric; MG: Middle Geometric; LG: Late Geometric;

*: the date is the average of multiple measurements on the same sample (the number of measurements is indicated between brackets);

a: RTK6372 and RTK6373 are parts of the same assemblage of seeds, and therefore dates were averaged;

b: RTK6374 and RTK6375 are parts of the same assemblage of seeds, and therefore dates were averaged.

All the charred seeds come from clusters. References for published contexts are included within the "Context" column; all the other contexts are yet unpublished. δ¹³C values were obtained using an isotope ratio mass spectrometer.

doi:10.1371/journal.pone.0083117.t001

the Early Protogeometric, EPG or to the Middle Protogeometric, MPG).

The results of the analyses presented here as "transition" and reported as a time range should be regarded as calculated probability distributions of the transition timing; they do not represent the actual (historical) length of the transition [33,45].

## Results

### Radiocarbon dating

The ¹⁴C calibrated ages are presented in Table 1, with the dates ordered according to the relative chronological sequence determined for the contexts from which the samples were collected. All the dates that were averaged (i.e. the dates of the samples measured more than once, Table 1) passed the $\chi^2$ test. Table 2 shows the C and N isotopic values of the human bones from Corinth. The δ¹³C and δ¹⁵N values were determined in order to check whether the bones are affected by a marine reservoir age effect dependent on a marine fish diet. Marine reservoir age can increase the apparent age of humans/animals by up to 400 years BP [46,47]. Values lower than ca. -19‰ and 10‰ for the δ¹³C and the δ¹⁵N, respectively, are not compatible with a diet based on marine fish [48]. Therefore, based on the data reported in Table 2, we conclude that the individuals from Corinth are not affected by a marine reservoir age effect. Even if one takes the δ¹⁵N value of RTK-6702, which is slightly above 10‰, as an indicator for a possible input of marine fish in the diet of that specific individual, the reservoir age effect would increase the age of the sample by less than 20 radiocarbon years [48], with no substantial effect on the resolution of the chronological sequence that we propose in the present study. It was not possible to measure the δ¹⁵N value for RTK-6698, since the size of the collagen sample was very small and priority was given to the ¹⁴C determination. However its radiocarbon age, which is much younger than what was expected according to the ceramic phase attribution, clearly excludes the possibility of a reservoir age effect. The archaeological contexts of the animal bones from Lefkandi and Kalapodi are not published yet, therefore we are not able to provide precise taxonomic classifications. However, all the bones belong to large terrestrial mammals, which are unlikely to be fed on marine fish. The δ¹³C values for the animal bones (Table 1) support this assumption. Moreover, Kalapodi is located inland, not on the coast.

Four samples were not used in the Bayesian analysis. Sample RTT-6104 was found in secondary deposition. The charcoal fragments were embedded in an ashy layer, but no combustion feature was visible by naked eye. FTIR analysis confirmed this observation, as no heat-altered clay minerals were detected within the same sample [49]. We conclude that the ash (and therefore the charcoal) is the product of a fire-related activity which took place elsewhere.

Sample RTK-6385 is ~200 yr BP younger than expected, and this is probably related to poor preservation state or to its contamination during storage. FTIR analysis showed that this material does not contain cellulose as it would be expected for wood; rather, the FTIR spectrum resembles charcoal [41]. It is unlikely that the wood was found out of context, as it came together with other items from the well-defined Toumba context in Lefkandi.

Samples RTK-6395 and RTK-6698 are of little importance, as their radiocarbon dates fall within the "Hallstatt plateau" and the probability distribution covers a wide time span. Remarkably, RTK-6698 shows a date which is very late compared to the expected age provided by the ceramic assemblage. This might be related to a problematic context characterization at the time of the
OxCal v4.1.7 Bronk Ramsey (2010); r5 Atmospheric data from Reimer et al. (2009);

<figure><img src="image_4.png" /><figcaption>**Figure 3. Model A, including all the dates.** The label “L” after the laboratory number stands for Lefkandi; similarly, “K” stands for Kalapodi and “C” marks the samples from Corinth. Note that RTK-6372-73K, RTK-6374-75K, RTK-6123L, RTK-6124L, RTK-6127L, RTK-6371K, RTK-6384L, RTK-6397K and RTK-6396K are radiocarbon dates obtained by averaging multiple measurements of the same sample using the R_Combine command of OxCal. doi:10.1371/journal.pone.0083117.g003</figcaption></figure>

excavation. These four samples are therefore irrelevant for the
purposes of the following discussion and were not included in the
Bayesian analysis. All the absolute ranges presented in the text
refer to ±1σ (68.2% probability).

Bayesian models

The information regarding the relative pottery phases summa-
rized in Table 1 was used as a constraint in our Bayesian analysis
 lines of codes for each model are provided in Figure S1). Note that
 “Modelled date (BC)” notation at the end of each model relates to
 calendar years BCE. The modeled age probability distributions
 are presented as black areas, whereas the measured un-modeled
 age probability distributions appear as empty areas. Under each
 modeled distribution the upper segment refers to 68.2% proba-
bility, whereas the lower segment refers to 95.4% probability.
 After modeling some samples showed low agreement within the
 model (below 60% the date is considered to be in poor agreement
 [33,45]). These samples were checked again to detect possible
 archaeological or analytical errors to justify their exclusion from
 the model. In the absence of evident errors the samples were
 excluded from the model once at a time until the general
 agreement of the model was above 60%. Each of the samples

excluded is pointed out and justified. Model A (Fig. 3) presents 15
dates organized in a sequence of contiguous phases (i.e. one phase
starts as the previous one ends, and from the oldest period of the
relative chronology to the youngest). Within the PG phase was
included a sub-sequence with dates organized according to the
relative sub-phasing, where RTK-6371 belongs to the EPG, RTK-
6384 to the Middle-Late Protogeometric (M-LPG), RTK-6397 to
the LPG and RTK-6396 to the Sub-Protogeometrci (SPG). The
only undivided PG date – RTK-6697 – was considered as
contemporary with the entire block; in other words, it might be
contemporary with any of the other samples. The agreement of
the model is low (16%), and this is due mainly to sample RTK-
6123 (too old for the LH IIIC Late to SM phase) and sample
RTK-6397 (too young to be placed before RTK-6396, which
comes from a SPG horizon and shows an older date). The SM/PG
transition is placed between 1050 and 1000 BCE.

In Model B (Fig. 4) we decided to test another possibility, by
placing samples RTK-6123 and RTK-6127 of the LH IIIC Late
to SM in the LH IIIC Middle to Late phase, as explained above;
this is still in line with the relative chronology sequence. As
mentioned previously for Model A, RTK-6396 (SPG) and RTK-
6397 (LPG) provided dates in an opposite order compared to the
<figure><img src="image_5.png" /><figcaption>**Figure 4. Model B.** Note that two dates were labeled as outliers (RTK-6396 and RTK-6397), whereas RTK-6123 and RTK-6127 were placed within the LH IIIC Middle to Late phase.
doi:10.1371/journal.pone.0083117.g004</figcaption></figure>

relative chronology of the ceramic phases they belong to (RTK-6396 older than RTK-6397). This is the reason for their exclusion by the model (i.e. by OxCal) on the ground of poor agreement (i.e. <60%). Considering that each of these two samples was measured four times and that the combined dates passed the χ² test, we believe that the problem is in their ceramic-phase attribution; therefore they were labeled as outliers in OxCal. Also note that RTK-6396 is too old to be included within the SPG (Table 1). After these changes, the agreement increased to 81% and the SM/PG transition occurs between 1050 and 1000 BCE, which is similar to the result of Model A. The transition between PG and G ranges between 1030 and 970 BCE, but this value has little meaning, considering that there are only two dates for the G period. Moreover, one of these two samples (RTK-6702) shows a radiocarbon date that could fit also into the SM period. This explains the high range for the PG/G transition. In order to have a better control on this transition, more dates for the LPG, Early Geometric (EG) and Middle Geometric (MG) are needed. This we hope to achieve in next phase of our research.

In Model C (Fig. 5) the standard deviation error of all the dates of Model B was arbitrarily reduced by us to ±20 yr BP in order to check whether an increased precision might enhance the

agreement of the model. We obtained the opposite effect, because the first five dates fall within the Late Bronze Age plateau of the calibration curve (approximately between 1300 and 1150 BCE); no matter how small the uncertainty in the measurement, these dates will always show a wide probability distribution. Also, the dates which do not fall in the region of the plateau (from the LH IIIC Late onwards), cluster in a shorter period of time, with no overlap with the older dates (those located in the plateau), thus resulting in a low agreement of the model. Yet, even in this case the SM/PG transition is located at the end of the 11th century (1030-990 BCE). Remarkably, this happens also if we consider only the dates from Lefkandi, as shown in Model D (Fig. 6). In this case the SM/PG transition occurs between 1065 and 980 BCE. Therefore, even taking into account one specific site for which we have enough dates to calculate the transition, the range of the transition would not change.

It is clear that all the models presented above point towards the same result, i.e. they place the SM/PG transition in the second half of the 11th century, approximately centered on 1025 BCE.
OxCal v4.1.7 Bronk Ramsey (2010); r.5 Atmospheric data from Reimer et al. (2009);

<figure><img src="image_6.png" /></figure>

**Figure 5. Model C.** Note that the standard deviation of all the dates was reduced to ±20 yr BP.
doi:10.1371/journal.pone.0083117.g005

OxCal v4.1.7 Bronk Ramsey (2010); r.5 Atmospheric data from Reimer et al. (2009);

<figure><img src="image_7.png" /></figure>

**Figure 6. Model D.** The plot shows the radiocarbon dates of Lefkandi only.
doi:10.1371/journal.pone.0083117.g006
<table><caption>**Table 2.** Isotopic values of human bones from Corinth.</caption><thead><tr><th>Lab #</th><th>%C</th><th>%N</th><th>C/N</th><th>δ<sup>13</sup>C (‰)</th><th>δ<sup>15</sup>N (‰)</th></tr></thead><tbody><tr><td>RTK6697</td><td>40.0</td><td>16.8</td><td>2.7</td><td>-19.5±0.2</td><td>9.5±0.3</td></tr><tr><td>RTK6698</td><td>42.6</td><td>nd</td><td>nd</td><td>nd</td><td>nd</td></tr><tr><td>RTK6699</td><td>42.0</td><td>17.5</td><td>2.8</td><td>-19.7±0.3</td><td>9.7±0.5</td></tr><tr><td>RTK6701</td><td>42.0</td><td>18.8</td><td>2.6</td><td>-19.4±0.3</td><td>8.1±0.2</td></tr><tr><td>RTK6702</td><td>40.7</td><td>19.8</td><td>2.4</td><td>-19.6±0.1</td><td>10.4±0.5</td></tr></tbody></table>

doi:10.1371/journal.pone.0083117.t002

## Discussion

Adherents of the Conventional Aegean Chronology put the SM/PG transition in the mid-to-late 11th century BCE, while those who accept the High Chronology place it close to the end of the 12th century BCE. Accepting the latter would force one to stretch the MG over two centuries at the expense of the EG, the entire PG, the SM and even part of the LH IIIC [12] (Fig. 1). Our results support the Conventional Aegean Chronology [17] and shed light on the duration of the SM phase in the Aegean sequence, a phase that is still being considered as somewhat elusive [27].

Despite a plea to abandon the term [50], the SM represents a definable chronological stage, at least in Attica, Boeotia and the Argolid, even if from an interregional perspective it may overlap with the final stages of the LH IIIC Late and the beginning of the EPG (e.g., the LH IIIC Late in the Argolid is contemporary with the beginning of the SM in Attica). Moreover, even if one follows Rutter [50] and argues that the style referred to as SM represents tombs' repertoire, chronologically parallel to the LH IIIC Late in settlement sites (see Lemos [51] against this notion), it is not necessarily crucial for the purpose of establishing the absolute chronology for this stylistic phenomenon. From the perspective of relative chronology, given the paucity of the SM material and the dense sequence of styles in the Late Bronze and early Iron Ages, the SM phase could not have been long-lived. It is generally allowed two generations, that is, some 50 years of existence [52,53] at the most [27]. Lemos' suggestion [51], which allows it two generations of twenty-five years long, with an additional generation for the transition from SM to the EPG may be too generous, since it turns a relatively short-lived, local phenomenon, without much internal variety [12,54], into one of the longest phases in Iron Age Greece. The same holds true for the more maximalist reconstruction of Ruppenstein [55], according to whom the SM period covers most of the 11th century BCE.

The absolute chronology of the SM period is difficult to establish [27]. The upper anchor is not clear enough, due to the lack of genuine LH IIIC Late imports in well-dated strata in the Levant [56]. The lower anchor, i.e. the transition to the EPG, is no less problematic. Desborough [57] suggested that the Attic PG started at ca. 1025 BCE; later on, he hesitantly opted for a slightly earlier date of ca. 1050 BCE [58–61]. This date was in fact based

on Gjerstad's calculations [62] regarding the presence of a Cypriot White Painted I bowl (contemporary to the EPG in Greece) in Stratum VIA at Megiddo in the Levant, dated by Albright, on the basis of biblical references, to ca. 1050-1000 BCE [5]. A large number of ¹⁴C determinations now puts the beginning of Megiddo VIA in the second half of the 11th century and its end in the range 985-935 BCE [63]. Thus, it seems that even before one applies the radiocarbon dates reported here, the initial date of ca. 1050 BCE for the SM/PG transition is probably too high [5]. A date closer to ca. 1020/1000 BCE, which would fit better the Low Chronology in the Levant would be in line with Desborough's initial guess and Mountjoy and Hankey's lowering of the beginning of the Protogeometric period [51,64]. No less important, it fits the dates reported here. The recent revival of the High Aegean Chronology, based on radiometric dates from sites such as Assiros, Carthage and Huelva [1–4,6], apart from being based on problematic interpretations [5,65] and dubious contexts [7], would push the SM/PG transition toward the end of the 12th century BCE, a date which is far from the range reported here.

According to Weninger and Jung [65], the SM/EPG transition should be set around 1070/40 BCE. We prefer to consider this datum as reflecting the beginning of the SM phase [7]. Based on the radiocarbon measurements reported here and the considerations detailed above, we suggest to put its end—and the transition to the EPG—around 1020/1000 BCE.

## Conclusions

The absolute dates of the relative ceramic phases of the Iron Age in the Aegean Basin have been disputed for many decades. In this article we report the results of the first systematic attempt to radiocarbon date these phases with samples taken from the key sites of Lefkandi, Kalapodi and Corinth. The data at hand enable to tackle the important transition between the SM and PG periods. This transition is placed by adherents of the Conventional Aegean Chronology in the mid-to-late 11th century and by supporters of the High Aegean Chronology in the late 12th century BCE. Our results put it in the second half of the 11th century BCE.

## Supporting Information

**Figure S1** Lines of codes for the Bayesian models. (TXT)

## Acknowledgments

MBT wishes to thank Eugenia Mintz (D-REAMS Radiocarbon Laboratory, Weizmann Institute of Science) for her assistance during the preparation of the samples for radiocarbon dating.

## Author Contributions

Conceived and designed the experiments: MBT AF ISL RCSF WDN GDRS IF EB. Performed the experiments: MBT EB. Analyzed the data: MBT AF ISL RCSF WDN GDRS IF EB. Contributed reagents/materials/analysis tools: MBT AF ISL RCSF WDN GDRS IF EB. Wrote the paper: MBT AF ISL RCSF WDN GDRS IF EB.

## References

1. Newton MW, Kuniholm PI, Wardle KA (2005) A Dendrochronological ¹⁴C Wiggle-match for the Early Iron Age of North Greece. In: Levy TE, Higham T, editors. The Bible and Radiocarbon Dating Archaeology, Text and Science. London. pp. 104–113.

2. Newton MW, Kuniholm PI, Wardle KA (2007) Troy VIIB₂ Revisited: The Date of the Transition from Bronze to Iron Age in the Northern Aegean. In: Todorova H, Stefanovich M, Ivanov G, editors. The Struma/Strymon River Valley in Prehistory. Sofia. pp. 481–497.

3. Nijboer AJ (2005) The Iron Age in the Mediterranean: A Chronological Mess or 'Trade before the Flag', Part II. Ancient West and East 4: 254–277.

4. van der Plicht H, Bruins HJ, Nijboer AJ (2009) The Iron Age around the Mediterranean: a high chronology perspective from the Groningen radiocarbon database. Radiocarbon 51: 213–242.

5. Maeir AM, Fantalkin A, Zuckerman A (2009) The Earliest Greek Import in the Iron Age Levant: New Evidence from Tell es-Safi/Gath, Israel. Ancient West and East 8: 57–80.
6. Bruins HJ, Nijboer AJ, van der Plicht H (2011) Iron Age Mediterranean chronology: a reply. Radiocarbon 53: 199-220.

7. Fantalkin A, Finkelstein I, Piasetzky E (2011) Iron Age Mediterranean chronology: a rejoinder. Radiocarbon 53: 179-198.

8. Bartoloni G, Delpino F, editors(2005) Oriente e Occidente: metodi e discipline a confronto. Riflessioni sulla cronologia dell'età del ferro in Italia. Atti dell'incontro di studi, Roma 30-31 ottobre 2003. Pisa: Istituti Editoriali e Poligrafici Internazionali.

9. Brandherm D, Trachsel M, editors(2008) A New Dawn for the Dark Age? Shifting Paradigms in Mediterranean Iron Age Chronology. Oxford: Archaeopress.

10. Desborough VRdA (1957) A Group of Vases from Amathus. Journal of Hellenic Studies 77: 212-219.

11. Fantalkin A (2001) Low Chronology and Greek Protogeometric and Geometric Pottery in the Southern Levant. Levant 33: 117-125.

12. Coldstream N (2003) Some Aegean reactions to the chronological debate in the southern Levant. Tel Aviv 30: 247-258.

13. Van Seters J (1983) In Search of History. New Haven: Yale University.

14. Finkelstein I (1996) The Archaeology of the United Monarchy: An Alternative View. Levant 28: 177-187.

15. Miller MJ (1997) Separating the Solomon of History from the Solomon of Legend. In: Handy LK, editor. The Age of Solomon: Scholarship at the Turn of the Millennium. Leiden: Brill. pp. 1-24.

16. Niemann HM (1997) The Socio-Political Shadow Cast by the Biblical Solomon. In: Handy LK, editor. The Age of Solomon: Scholarship at the Turn of the Millennium. Leiden: Brill. pp. 252-299.

17. Coldstream N (1968) Greek Geometric Pottery: A Survey of Ten Local Styles and Their Chronology. London.

18. Finkelstein I, Piasetzky E (2011) The Iron Age Chronology Debate: Is the Gap Narrowing? NEA 74: 50-54.

19. Sharon I, Gilboa A, Jull TAj, Boaretto E (2007) Report on the first stage of the Iron Age dating project in Israel: supporting a low chronology. Radiocarbon 49: 1-46.

20. Mazar A (2011) The Iron Age Chronology Debate: Is the Gap Narrowing? Another Viewpoint. NEA 74: 105-111.

21. Mazar A (2005) The Debate over the Chronology of the Iron Age in the Southern Levant: Its History, the Current Situation, and a Suggested Resolution. In: Levy TE, Higham T, editors. The Bible and Radiocarbon Dating: Archaeology, Text and Science. London. pp. 15-30.

22. Mazar A, Bronk Ramsey C (2008) ¹⁴C dates and the Iron Age chronology of Israel: a response. Radiocarbon 50: 159-180.

23. Finkelstein I, Piasetzky E (2010) Radiocarbon dating the Iron Age in the Levant: a Bayesian model for six ceramic phases and six transitions. Antiquity 84: 374-385.

24. Wells B (1983) Asine II: Results of the Excavations East of the Acropolis 1970-1974, Vol. 4: The Protogeometric Period, Part 2. Stockholm.

25. Manning SW, Weninger B (1992) A Light in the Dark: Archaeological Wiggle Matching and the Absolute Chronology of the Close of the Aegean Late Bronze Age. Antiquity 66: 636-663.

26. Luce J-M (1993) Delphes: 1. Fouille de l'aire du pilier des Rhodiens. Bulletin de correspondance hellénique 117: 619-631.

27. Papadopoulos JK, Damiata BN, Marston JM (2011) Once More with Feeling: Jeremy Rutter's Plea for the Abandonment of the Term Submycenaean Revisited. In: Gauss W, Lindblom M, Smith A, Wright J, editors. Our Cups are Full Pottery and Society in the Aegean Bronze Age. Oxford: BAR Int. Series 2227. pp. 187-202.

28. Popham MR, Lemos IS (1996) Lefkandi III: the Toumba Cemetery. The Excavations of 1981, 1984, 1986 and 1992-4. Oxford.

29. Felsch R, editor(2007) Kalapodi II. Ergebnisse der Ausgrabungen im Heiligtum der Artemis und des Apollon von Hyampolis in der antiken Phokis. Mainz am Rhein: Philipp von Zabern.

30. Felsch R, editor(1996) Kalapodi I. Ergebnisse der Ausgrabungen im Heiligtum der Artemis und des Apollon von Hyampolis in der antiken Phokis. Mainz am Rhein: Philipp von Zabern.

31. Williams CK, Bookidis N, editors(2003) Corinth, the Centenary: 1896-1996. Athens: The American School of Classical Studies at Athens.

32. Bayes T (1763) An essay towards solving a Problem in the Doctrine of Chances. Philosophical Transactions of the Royal Society of London 53: 370-418.

33. Bronk Ramsey C (2009) Bayesian analysis of radiocarbon dates. Radiocarbon 51: 337-360.

34. Williams CK (1970) Corinth, 1969: Forum Area. Hesperia 39: 1-39.

35. Williams CK, Fisher JE (1972) Corinth, 1971: Forum Area. Hesperia 41: 143-184.

36. Williams CK, MacIntosh J, Fisher JE (1974) Excavation at Corinth, 1973. Hesperia 43: 1-76.

37. Sharon I (2001) 'Transition dating' - A heuristic mathematical approach to the collation of radiocarbon dates from stratified sequences. Radiocarbon 43: 345-354.

38. Boaretto E (2009) Dating materials in good archaeological contexts: the next challenge for radiocarbon analysis. Radiocarbon 51: 275-281.

39. Toffolo MB, Maeir AM, Chadwick JR, Boaretto E (2012) Characterization of contexts for radiocarbon dating: results from the early Iron Age at Tel es-Safi/ Gath, Israel. Radiocarbon 54: 371-390.

40. Boaretto E (2007) Determining the chronology of an archaeological site using radiocarbon: Minimizing uncertainty. Israel Journal of Earth Sciences 56: 207-216.

41. Yizhaq M, Mintz G, Cohen I, Khalaily H, Weiner S, et al. (2005) Quality controlled radiocarbon dating of bones and charcoal from the early Pre-Pottery Neolithic B (PPNB) of Motza (Israel). Radiocarbon 47: 193-206.

42. Rebollo NR, Cohen-Ofri I, Popovitz-Biro R, Bar-Yosef O, Meignen L, et al. (2008) Structural characterization of charcoal exposed to high and low pH: implications for ¹⁴C sample preparation and charcoal preservation. Radiocarbon 50: 289-307.

43. Stuiver M, Polach HA (1977) Discussion: reporting of ¹⁴C data. Radiocarbon 19: 355-363.

44. Reimer PJ, Baillie MGL, Bard E, Bayliss A, Beck JW, et al. (2009) IntCal09 and Marine09 radiocarbon age calibration curves, 0-50,000 years cal BP. Radiocarbon 51: 1111-1150.

45. Bronk Ramsey C, Dee M, Lee S, Nakagawa T, Staff R (2010) Developments in the calibration and modelling of radiocarbon dates. Radiocarbon 52: 953-961.

46. Stuiver M, Braziunas TF (1993) Modelling atmospheric ¹⁴C influences and ¹⁴C ages of marine samples to 10,000 BC. Radiocarbon 35: 137-189.

47. Ascough PL, Cook GT, Dugmore AJ (2005) Methodological approaches to determining the marine radiocarbon reservoir effect. Progress in Physical Geography 29: 523-547.

48. Craig OE, Bondioli L, Fattore L, Higham T, Hedges R (2013) Evaluating Marine Diets Through Radiocarbon Dating and Stable Isotope Analysis of Victims of the AD79 Eruption of Vesuvius. American Journal of Physical Anthropology.

49. Berna F, Behar A, Shahack-Gross R, Berg J, Boaretto E, et al. (2007) Sediments exposed to high temperatures: reconstructing pyrotechnological processes in Late Bronze and Iron Age Strata at Tel Dor (Israel). Journal of Archaeological Science 34: 358-373.

50. Rutter JB (1978) A Plea for the Abandonment of the Term 'Submycenaean'. In: Betancourt PP, editor. Studies of New and Little Known Materials from the Aegean Bronze Age. Philadelphia: Temple University Aegean Symposium 3. pp. 58-65.

51. Lemos IS (2002) The Protogeometric Aegean. The Archaeology of the Late Eleventh and Tenth Centuries B.C. Oxford: Oxford University Press.

52. Warren PM, Hankey V (1989) Aegean Age Chronology. Bristol.

53. Whitley J (1991) Style and Society in Dark Age Greece: The Changing Face of a Pre-literate Society, 1100-700 BC. Cambridge.

54. Dickinson OTPK (2006) The Aegean from Bronze Age to Iron Age: continuity and change between the twelfth and eighth centuries B.C. New York: Routledge.

55. Ruppenstein F (2007) Die submykenische Nekropole. Neufunde und Neubewertung (Kerameikos XVIII). München: Hirmer.

56. Yasur-Landau A (1993) The Absolute Chronology of the Late Helladic IIIC Period: A View from the Levant. In: Deger-Jalkotzy S, Zavadil M, editors. LH IIIC Chronology and Synchronisms Proceedings of the Internation Workshop Held at the Austrian Academy of Sciences at Vienna, May 7th and 8th, 2001. Vienna. pp. 235-244.

57. Desborough VRdA (1952) Protogeometric Pottery. Oxford.

58. Desborough VRdA (1972) The Greek Dark Ages. London.

59. Snodgrass AM (1971) The Dark Age of Greece: An Archaeological Survey of the Eleventh to the Eighth Centuries B.C. Edinburgh.

60. Sherratt S (2006) The Chronology of the Philistine Monochrome Pottery: An Outsider's View. In: Maeir AM, de Miroshedji P, editors. I Will Speak the Riddles of Ancient Times: Archaeological and Historical Studies in Honor of Amihai Mazar on the Occasion of his Sixtieth Birthday. Winona Lake. pp. 261-274.

61. French EB (2007) The Impact on Correlations to the Levant of the recent Stratigraphic Evidence from the Argolid. In: Bietak M, Czerny E, editors. The Synchronisation of Civilization in the Eastern Mediterranean in the Second Millennium BC III: Proceedings of the SCIEM 2000 - 2nd EuroConference, Vienna 28th of May-1st of June 2003. Vienna. pp. 525-536.

62. Gjerstad E (1944) The Initial Date of the Cypriot Iron Age. OpArch 3: 73-106.

63. Toffolo MB, Arie E, Martin MAS, Boaretto E, Finkelstein I (in press) The absolute chronology of Megiddo, Israel in the Late Bronze and Iron Ages: high-resolution radiocarbon dating. Radiocarbon.

64. Mountjoy PA, Henkey V (1988) LH IIIC Late versus Submycenaean: The Kerameikos Pompeion Cemetery Reviewed. Jdl 103: 1-33.

65. Weninger B, Jung R (2009) Absolute Chronology of the End of the Aegean Bronze Age. In: Deger-Jalkotzy S, Bächle AE, editors. LH III C Chronology and Synchronisms III: LH III C Late and the Transition to the Early Iron Age. Wien. pp. 373-416.