@article{RADON,
title = {RADON - Radiocarbon Dates Online 2012. Central European Database of 14C Dates for the Neolithic and the Early Bronze Age.},
author = {Hinz, Martin and Furholt, Martin and Müller, Johannes and Raetzel-Fabian, Dirk and Rinne, Christophe and Sjögren, Karl-Göran and Wotzka, Hans-Peter},
date = {2012},
journaltitle = {Journal of Neolithic Archaeology},
volume = {14},
pages = {1–4},
url = {https://www.jna.uni-kiel.de/index.php/jna/article/view/65/116},
abstract = {In order to understand the dynamics of cultural phenomena, scientific dating in archaeology is an increasingly indispensable tool. Only by dating independently of typology is it possible to understand typological development itself (Müller 2004). Here radiometric dating methods, especially those based on carbon isotopy, still play the most important role. For evaluations exceeding the intra-site level, it is particularly important that such data is collected in large numbers and that the dates are easily accessible. Also, new statistical analyses, such as sequential calibration based on Bayesian methods, do not require single dates, but rather demand a greater number. By their combination significantly more elaborate results can be achieved compared to the results from conventional evaluation (e. g. Whittle et al. 2011). A second premise of RADON is that of „Open Access“. This approach continues to be applied in the international research community, which we welcome as a highly positive development. The radiocarbon database RADON has been committed to this principle for more than 12 years. In this database 14C data – primarily of the Neolithic of Central Europe and Southern Scandinavia – is collected and successively augmented.}
}
[{"bibtex_key":"RADON","bibtex_type":"article","title":"{RADON - Radiocarbon Dates Online 2012. Central European Database of 14C Dates for the Neolithic and the Early Bronze Age.}","author":"{Hinz, Martin and Furholt, Martin and Müller, Johannes and Raetzel-Fabian, Dirk and Rinne, Christophe and Sjögren, Karl-Göran and Wotzka, Hans-Peter}","date":"{2012}","journaltitle":"{Journal of Neolithic Archaeology}","volume":"{14}","pages":"{1–4}","url":"{https://www.jna.uni-kiel.de/index.php/jna/article/view/65/116}","abstract":"{In order to understand the dynamics of cultural phenomena, scientific dating in archaeology is an increasingly indispensable tool. Only by dating independently of typology is it possible to understand typological development itself (Müller 2004). Here radiometric dating methods, especially those based on carbon isotopy, still play the most important role. For evaluations exceeding the intra-site level, it is particularly important that such data is collected in large numbers and that the dates are easily accessible. Also, new statistical analyses, such as sequential calibration based on Bayesian methods, do not require single dates, but rather demand a greater number. By their combination significantly more elaborate results can be achieved compared to the results from conventional evaluation (e. g. Whittle et al. 2011). A second premise of RADON is that of „Open Access“. This approach continues to be applied in the international research community, which we welcome as a highly positive development. The radiocarbon database RADON has been committed to this principle for more than 12 years. In this database 14C data – primarily of the Neolithic of Central Europe and Southern Scandinavia – is collected and successively augmented.}"}]
---
- :bibtex_key: RADON
:bibtex_type: :article
:title: "{RADON - Radiocarbon Dates Online 2012. Central European Database of 14C
Dates for the Neolithic and the Early Bronze Age.}"
:author: "{Hinz, Martin and Furholt, Martin and Müller, Johannes and Raetzel-Fabian,
Dirk and Rinne, Christophe and Sjögren, Karl-Göran and Wotzka, Hans-Peter}"
:date: "{2012}"
:journaltitle: "{Journal of Neolithic Archaeology}"
:volume: "{14}"
:pages: "{1–4}"
:url: "{https://www.jna.uni-kiel.de/index.php/jna/article/view/65/116}"
:abstract: "{In order to understand the dynamics of cultural phenomena, scientific
dating in archaeology is an increasingly indispensable tool. Only by dating independently
of typology is it possible to understand typological development itself (Müller
2004). Here radiometric dating methods, especially those based on carbon isotopy,
still play the most important role. For evaluations exceeding the intra-site level,
it is particularly important that such data is collected in large numbers and
that the dates are easily accessible. Also, new statistical analyses, such as
sequential calibration based on Bayesian methods, do not require single dates,
but rather demand a greater number. By their combination significantly more elaborate
results can be achieved compared to the results from conventional evaluation (e.
g. Whittle et al. 2011). A second premise of RADON is that of „Open Access“. This
approach continues to be applied in the international research community, which
we welcome as a highly positive development. The radiocarbon database RADON has
been committed to this principle for more than 12 years. In this database 14C
data – primarily of the Neolithic of Central Europe and Southern Scandinavia –
is collected and successively augmented.}"
There are 11455 records in XRONOS that cite this reference.
| Site | Lab ID | Context | Material | Taxon | Method | Uncalibrated age | Calibrated age | References |
|---|---|---|---|---|---|---|---|---|
| Pupičina peč | Beta-131624 | NA | NA | NA | 14C | 6270±120 BP | 7425–6890 cal BP | Hinz et al. 2012 Weninger 2022 |
| Pupičina peč | Beta-131625 | NA | NA | NA | 14C | 6680±100 BP | 7705–7338 cal BP | Hinz et al. 2012 Weninger 2022 |
| Pupičina peč | OxA-8471 | NA | NA | NA | 14C | 6495±60 BP | 7555–7280 cal BP | Hinz et al. 2012 Weninger 2022 |
| Ayios Dimitrios | OxA-120 | NA | charcoal | NA | 14C | 2860±150 BP | 3381–2725 cal BP | Hinz et al. 2012 Weninger 2022 |
| Kissonerga-Mylouthkia | OxA-7462 | NA | seed/fruit | Pistacia | 14C | 4650±50 BP | 5570–5294 cal BP | Hinz et al. 2012 Weninger 2022 |
| Kissonerga-Mylouthkia | OxA-7463 | NA | seed/fruit | Pistacia | 14C | 4710±50 BP | 5579–5320 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8264 | NA | charcoal | NA | 14C | 3060±35 BP | 3361–3175 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8265 | NA | olive stone | Olea | 14C | 2960±35 BP | 3219–3000 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8266 | NA | olive stone | Olea | 14C | 2985±35 BP | 3328–3009 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8267 | NA | olive stone | Olea | 14C | 2940±35 BP | 3207–2968 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8321 | NA | charcoal | NA | 14C | 3020±45 BP | 3349–3075 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8322 | NA | olive stone | Olea | 14C | 2935±45 BP | 3212–2960 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8323 | NA | charcoal | NA | 14C | 3055±45 BP | 3372–3084 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8324 | NA | olive stone | Olea | 14C | 2930±40 BP | 3206–2962 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8325 | NA | charcoal | NA | 14C | 3030±40 BP | 3355–3079 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8326 | NA | charcoal | NA | 14C | 3025±40 BP | 3351–3077 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8327 | NA | charcoal | NA | 14C | 3130±45 BP | 3448–3235 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8348 | NA | charcoal | NA | 14C | 3090±40 BP | 3386–3184 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8349 | NA | charcoal | NA | 14C | 3060±40 BP | 3364–3170 cal BP | Hinz et al. 2012 Weninger 2022 |
| Maroni-Tsaroukkas | OxA-8350 | NA | seed/fruit | Prunus | 14C | 3080±40 BP | 3378–3177 cal BP | Hinz et al. 2012 Weninger 2022 |