Site types
Settlement and

Location

Coordinates (degrees)
NA
Coordinates (DMS)
NA
Country (ISO 3166)
Serbia (RS)

radiocarbon date Radiocarbon dates (253)

Lab ID Context Material Taxon Method Uncalibrated age Calibrated age References
OxA-16072 Beneath floor of building 47' Red deer molar NA NA 9850±50 BP 11393–11192 cal BP Borić & Dimitrijević 2007: Table 1, Borić 2011: 192
OxA-16076 Floor of Building 54 Red deer antler NA NA 9750±45 BP 11247–11100 cal BP Borić & Dimitrijević 2007: Table 1, Borić 2011: 192
OxA-16004 Between floors of Buildings 47 and 47' Red deer metatarsus NA NA 9730±50 BP 11245–10875 cal BP Borić & Dimitrijević 2007: Table 1, Borić 2011: 192
OxA-25092 Burial 60, adult, male? R femur Human bone Homo sapiens NA 9519±73 BP 11110–10582 cal BP Bonsall et al. 2015: 37 Table 1
OxA-11715 Burial 60 Human femur NA NA 9030±71 BP 10371–9906 cal BP Bonsall et al. 2008: 178 Table 1, Borić 2011: 192
OxA-16071 Building 26', floor Red deer modified antler NA NA 8855±40 BP 10160–9765 cal BP Borić & Dimitrijević 2007: Table 1, Borić 2011: 192
OxA-8610 Beneath floor of Building 23 Ungulate long bone NA NA 8770±60 BP 10119–9550 cal BP Whittle et al. 2002: 116, Borić 2011: 192
OxA-11703 Burial 69 Human femur NA NA 8740±67 BP 10115–9542 cal BP Bonsall et al. 2008: 178 Table 1, Borić 2011: 193
OxA-25215 Burial 69, adult, male?, L femur Human bone Homo sapiens NA 8694±63 BP 9891–9539 cal BP Bonsall et al. 2015: 37 Table 1
OxA-16074 Hearth Red deer antler NA NA 8645±40 BP 9680–9538 cal BP Borić & Dimitrijević 2007: Table 1, Borić 2011: 193
AA-57781 Burial 22, next to hearth a Human mandible NA NA 8374±75 BP 9532–9139 cal BP Borić 2011: 193
KN-405 Building 62, timber beam Charcoal (poss. Quercus sp.) NA NA 7430±160 BP 8540–7944 cal BP Quitta 1973
OxA-8725 Between floors of Buildings 20 and 33 Fish vertebra NA NA 7390±93 BP 8370–8023 cal BP Whittle et al. 2002: 116, Borić 2011: 193
OxA-11704 Burial 14 Human bone Homo sapiens NA 7390±64 BP 8342–8035 cal BP Borić & Price 2013: SI Table 1, Borić 2011: 193
KN-406 Building 27, possibly from hearth Charcoal NA NA 7210±200 BP 8390–7669 cal BP Quitta 1973, Borić 2011: 194
Bln-704a Building 36, timber beam Charcoal (Quercus sp.) NA NA 7310±100 BP 8342–7960 cal BP Quitta & Kohl 1969: 234f.
Bln-704b Building 36, timber beam Charcoal (Quercus sp.) NA NA 7360±100 BP 8370–7979 cal BP Quitta & Kohl 1969: 234f.
Bln-704a + Bln-704b Building 36, timber beam Charcoal (Quercus sp.) NA NA 7335±71 BP 8325–8014 cal BP
OxA-11705 Burial 79a, square e/4, spits 11–13 Human scapula NA NA 7340±67 BP 8325–8017 cal BP Borić 2011: 193, Borić & Price 2013: SI Table 1
OxA-11697 Burial 54e Tooth, female adult NA NA 7330±51 BP 8290–8018 cal BP Bonsall et al. 2008: 178 Table 1, Borić & Price 2013: SI Table 1, Borić 2011: 193

typological date Typological dates (6)

Classification Estimated age References
Lepenski Vir NA NA
unspec. NA Hedges et al. 1998b
unspec. NA Hedges et al. 1998b
unspec. NA Hedges et al. 1998b
unspec. NA Hedges et al. 1998b
unspec. NA Hedges et al. 1998b

Bibliographic reference Bibliographic references

@misc{Borić & Dimitrijević 2007: Table 1, Borić 2011: 192,
  
}
@misc{Bonsall et al. 2015: 37 Table 1,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Borić 2011: 192,
  
}
@misc{Whittle et al. 2002: 116, Borić 2011: 192,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Borić 2011: 193,
  
}
@misc{Borić & Dimitrijević 2007: Table 1, Borić 2011: 193,
  
}
@misc{Borić 2011: 193,
  
}
@misc{Quitta 1973,
  
}
@misc{Whittle et al. 2002: 116, Borić 2011: 193,
  
}
@misc{Borić & Price 2013: SI Table 1, Borić 2011: 193,
  
}
@misc{Quitta 1973, Borić 2011: 194,
  
}
@misc{Quitta & Kohl 1969: 234f.,
  
}
@misc{Borić 2011: 193, Borić & Price 2013: SI Table 1,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Borić & Price 2013: SI Table 1, Borić 2011: 193,
  
}
@misc{Bonsall et al. 2015: 37 Table 1, Bonsall et al. 2008: 178 Table 1, Borić 2011: 193,
  
}
@misc{Bonsall et al. 2015: 37 Table 1, Bonsall et al. 2008: 178 Table 1, Borić 2011: 195,
  
}
@misc{Bonsall et al. 2000: 123 Table 3, Bonsall et al. 2008: 178 Table 1, Borić & Price 2013: SI Table 1, Borić 2011: 194,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1, Borić 2011: 193,
  
}
@misc{Borić & Dimitrijević 2007: Table 1, Borić 2011: 194,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1, Borić 2011: 194,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1,
  
}
@misc{Whittle et al. 2002: 116, Borić 2011: 194,
  
}
@misc{Bonsall et al. 2015: 41 Table 3, Borić 2011: 194,
  
}
@misc{Bonsall et al. 2000: 123 Table 3, Bonsall et al. 2008: 178 Table 1, Borić 2011: 194,
  
}
@misc{Borić & Price 2013: SI Table 1,
  
}
@misc{Quitta & Kohl 1969: 234f., Borić 2011: 196,
  
}
@misc{Borić & Dimitrijević 2007: Table 1, Borić & Price 2013: SI Table 1,
  
}
@misc{Borić & Dimitrijević 2007: Table 1, Borić 2011: 195,
  
}
@misc{Borić & Price 2013: SI Table 1, Borić 2011: 195,
  
}
@misc{Borić & Price 2013: SI Table 1, Borić 2011: 195, Bonsall et al. 2008: 178 Table 1,
  
}
@misc{Quitta & Kohl 1969: 234f., Borić 2011: 195,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1, Borić 2011: 195,
  
}
@misc{Borić & Dimitrijević 2007: Table 1, Borić 2011: 196,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 38 Table 1, Borić 2011: 196,
  
}
@misc{Quitta 1973, Borić 2011: 196,
  
}
@misc{Bonsall et al. 2000: 123 Table 3, Bonsall et al. 2008: 178 Table 1, Borić & Price 2013: SI Table 1, Borić 2011: 196,
  
}
@misc{Bonsall et al. 2015: 41 Table 3, Borić & Price 2013: SI Table 1, Borić 2011: 195,
  
}
@misc{Borić & Price 2013: SI Table 1, Borić 2011: 196,
  
}
@misc{Bonsall et al. 2000: 123 Table 3, Bonsall 2008: Table 10.1, Borić 2011: 196,
  
}
@misc{Bonsall et al. 2015: 41 Table 3, Borić & Price 2013: SI Table 1, Borić 2011: 196,
  
}
@misc{Quitta & Kohl 1969: 234f., Bonsall et al. 2008: 178 Table 1, Borić 2011: 196,
  
}
@misc{Quitta & Kohl 1969: 234f., Bonsall et al. 2000: 123 Table 3, Bonsall 2008: Table 10.1,
  
}
@misc{Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 38 Table 1, Borić 2011: 197,
  
}
@misc{Borić  2011,
  
}
@misc{H.Quitta 1973,
  
}
@misc{Bonsall 2015,
  
}
@misc{Hedges et al. 1998b,
  
}
@misc{Borià & Price 2013,
  
}
@misc{Silva_VanderLinden_2017,
  
}
@misc{14SEA,
  
}
@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.}
}
@misc{Sapozhnikov I. 2005,
  
}
@misc{Quitta 1973 Boric 2011: 194,
  
}
@misc{Bonsall et al. 2008,
  
}
@misc{Bonsall et al. 2008: 178 Table 1 Boric & Price 2013: SI Table 1 Boric 2011: 193,
  
}
@misc{Bonsall et al. 2008: 178 Table 1 Boric 2011: 193,
  
}
@misc{Higham T. et al. 2007b: S33,
  
}
@misc{Boric & Dimitrijevic 2007: Table 1 Boric 2011: 196,
  
}
@misc{Boric et al. 2008: Table 1 Boric 2011: 202,
  
}
@misc{Boric & Dimitrijevic 2007: Table 1 Boric 2011: 195,
  
}
@misc{Boric et al. 2008: Table 1 Boric 2011: 201,
  
}
@misc{Whittle 1990 300 Tab. 1,
  
}
@misc{Bocquet-Appel J.P. & Demars P.Y. 2000. Antiquity 74: 544-52. Pettitt P. 1999. Oxford Journal of Archaeology 18: 217-241.,
  
}
@misc{Bonsall et al. 2015: 37 Table 1 Bonsall et al. 2008: 178 Table 1 Boric 2011: 193,
  
}
@misc{Bonsall C.  2015. Radiocarbon 57: 37,
  
}
@misc{Bicho N.F. 1999. Eraul 90: 55.,
  
}
@misc{Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 37 Table 1,
  
}
@misc{Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 37 Table 1 Boric 2011: 195,
  
}
@misc{Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 38 Table 1 Boric 2011: 196,
  
}
@misc{Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 37 Table 1 Boric 2011: 193,
  
}
@misc{Lovell 2001,
  
}
@misc{Bonsall et al. 2015: 37 Table 1 Bonsall et al. 2008: 178 Table 1 Boric 2011: 195,
  
}
@misc{Boric & Dimitrijevic 2007: Table 1 Boric 2011: 193,
  
}
@misc{14SEA,
  url = {http://www.14sea.org/},
  note = {Reingruber, A., and Thissen, L. (2017). The 14SEA Project: A 14C database for Southeast Europe and Anatolia (10,000–3000 calBC). Updated 2017-01-31. http://www.14sea.org/index.html}
}
@misc{CalPal,
  title = {CalPal Edition 2022.9},
  author = {Weninger, Bernie},
  year = {2022},
  month = {sep},
  doi = {1010.5281/zenodo.7422618},
  url = {https://zenodo.org/record/7422618},
  abstract = {CalPal is scientific freeware for 14C-based chronological research for Holocene and Palaeolithic Archaeology.},
  copyright = {Creative Commons Attribution 4.0 International, Open Access},
  howpublished = {Zenodo},
  month_numeric = {9}
}
@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.}
}
@article{dErricoEtAl2011,
  title = {PACEA Geo-Referenced Radiocarbon Database},
  author = {},
  date = {2011},
  journaltitle = {PaleoAnthropology},
  volume = {2011},
  pages = {1–12},
  abstract = {Numerous Paleolithic radiocarbon databases exist, but their geographic and temporal scopes are diverse and their availability variable. With this paper we make available to the scientific community a georeferenced database of radiocarbon ages for the late Middle Paleolithic, Upper Paleolithic, and initial Holocene in Europe. The PACEA radiocarbon database consists of conventional and AMS 14C age determinations from archaeological sites in Europe that fall within Marine Isotope Stages (MIS) 3–1. In all, we have assembled 6,019 radiocarbon ages (conventional=3,820, AMS=2,176, unspecified=23) from a total of 1,208 sites, along with comprehensive contextual information on the dated samples.},
  keywords = {⛔ No DOI found},
  file = {/home/joeroe/g/work/library/2011/d’Errico_et_al_2011.pdf}
}
@article{p3k14c,
  title = {P3k14c, a Synthetic Global Database of Archaeological Radiocarbon Dates},
  author = {Bird, Darcy and Miranda, Lux and Vander Linden, Marc and Robinson, Erick and Bocinsky, R. Kyle and Nicholson, Chris and Capriles, José M. and Finley, Judson Byrd and Gayo, Eugenia M. and Gil, Adolfo and d’Alpoim Guedes, Jade and Hoggarth, Julie A. and Kay, Andrea and Loftus, Emma and Lombardo, Umberto and Mackie, Madeline and Palmisano, Alessio and Solheim, Steinar and Kelly, Robert L. and Freeman, Jacob},
  year = {2022},
  month = {jan},
  journal = {Scientific Data},
  volume = {9},
  number = {1},
  pages = {27},
  publisher = {Nature Publishing Group},
  issn = {2052-4463},
  doi = {10.1038/s41597-022-01118-7},
  abstract = {Archaeologists increasingly use large radiocarbon databases to model prehistoric human demography (also termed paleo-demography). Numerous independent projects, funded over the past decade, have assembled such databases from multiple regions of the world. These data provide unprecedented potential for comparative research on human population ecology and the evolution of social-ecological systems across the Earth. However, these databases have been developed using different sample selection criteria, which has resulted in interoperability issues for global-scale, comparative paleo-demographic research and integration with paleoclimate and paleoenvironmental data. We present a synthetic, global-scale archaeological radiocarbon database composed of 180,070 radiocarbon dates that have been cleaned according to a standardized sample selection criteria. This database increases the reusability of archaeological radiocarbon data and streamlines quality control assessments for various types of paleo-demographic research. As part of an assessment of data quality, we conduct two analyses of sampling bias in the global database at multiple scales. This database is ideal for paleo-demographic research focused on dates-as-data, bayesian modeling, or summed probability distribution methodologies.},
  copyright = {2022 The Author(s)},
  langid = {english},
  keywords = {Archaeology,Chemistry},
  month_numeric = {1}
}
{"bibtex_key":"Borić & Dimitrijević 2007: Table 1, Borić 2011: 192","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 37 Table 1","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Borić 2011: 192","bibtex_type":"misc"}{"bibtex_key":"Whittle et al. 2002: 116, Borić 2011: 192","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Borić & Dimitrijević 2007: Table 1, Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Quitta 1973","bibtex_type":"misc"}{"bibtex_key":"Whittle et al. 2002: 116, Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Borić & Price 2013: SI Table 1, Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Quitta 1973, Borić 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Quitta & Kohl 1969: 234f.","bibtex_type":"misc"}{"bibtex_key":"Borić 2011: 193, Borić & Price 2013: SI Table 1","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Borić & Price 2013: SI Table 1, Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 37 Table 1, Bonsall et al. 2008: 178 Table 1, Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 37 Table 1, Bonsall et al. 2008: 178 Table 1, Borić 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 123 Table 3, Bonsall et al. 2008: 178 Table 1, Borić & Price 2013: SI Table 1, Borić 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1, Borić 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Borić & Dimitrijević 2007: Table 1, Borić 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1, Borić 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1","bibtex_type":"misc"}{"bibtex_key":"Whittle et al. 2002: 116, Borić 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 41 Table 3, Borić 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 123 Table 3, Bonsall et al. 2008: 178 Table 1, Borić 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Borić & Price 2013: SI Table 1","bibtex_type":"misc"}{"bibtex_key":"Quitta & Kohl 1969: 234f., Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Borić & Dimitrijević 2007: Table 1, Borić & Price 2013: SI Table 1","bibtex_type":"misc"}{"bibtex_key":"Borić & Dimitrijević 2007: Table 1, Borić 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Borić & Price 2013: SI Table 1, Borić 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Borić & Price 2013: SI Table 1, Borić 2011: 195, Bonsall et al. 2008: 178 Table 1","bibtex_type":"misc"}{"bibtex_key":"Quitta & Kohl 1969: 234f., Borić 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 37 Table 1, Borić 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Borić & Dimitrijević 2007: Table 1, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 38 Table 1, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Quitta 1973, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 123 Table 3, Bonsall et al. 2008: 178 Table 1, Borić & Price 2013: SI Table 1, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 41 Table 3, Borić & Price 2013: SI Table 1, Borić 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Borić & Price 2013: SI Table 1, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 123 Table 3, Bonsall 2008: Table 10.1, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 41 Table 3, Borić & Price 2013: SI Table 1, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Quitta & Kohl 1969: 234f., Bonsall et al. 2008: 178 Table 1, Borić 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Quitta & Kohl 1969: 234f., Bonsall et al. 2000: 123 Table 3, Bonsall 2008: Table 10.1","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1, Bonsall et al. 2015: 38 Table 1, Borić 2011: 197","bibtex_type":"misc"}{"bibtex_key":"Borić  2011","bibtex_type":"misc"}{"bibtex_key":"H.Quitta 1973","bibtex_type":"misc"}{"bibtex_key":"Bonsall 2015","bibtex_type":"misc"}{"bibtex_key":"Hedges et al. 1998b","bibtex_type":"misc"}{"bibtex_key":"Borià & Price 2013","bibtex_type":"misc"}{"bibtex_key":"Silva_VanderLinden_2017","bibtex_type":"misc"}{"bibtex_key":"14SEA","bibtex_type":"misc"}[{"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":"Sapozhnikov I. 2005","bibtex_type":"misc"}{"bibtex_key":"Quitta 1973 Boric 2011: 194","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1 Boric & Price 2013: SI Table 1 Boric 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1 Boric 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Higham T. et al. 2007b: S33","bibtex_type":"misc"}{"bibtex_key":"Boric & Dimitrijevic 2007: Table 1 Boric 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Boric et al. 2008: Table 1 Boric 2011: 202","bibtex_type":"misc"}{"bibtex_key":"Boric & Dimitrijevic 2007: Table 1 Boric 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Boric et al. 2008: Table 1 Boric 2011: 201","bibtex_type":"misc"}{"bibtex_key":"Whittle 1990 300 Tab. 1","bibtex_type":"misc"}{"bibtex_key":"Bocquet-Appel J.P. & Demars P.Y. 2000. Antiquity 74: 544-52. Pettitt P. 1999. Oxford Journal of Archaeology 18: 217-241.","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 37 Table 1 Bonsall et al. 2008: 178 Table 1 Boric 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Bonsall C.  2015. Radiocarbon 57: 37","bibtex_type":"misc"}{"bibtex_key":"Bicho N.F. 1999. Eraul 90: 55.","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 37 Table 1","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 37 Table 1 Boric 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 38 Table 1 Boric 2011: 196","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 37 Table 1 Boric 2011: 193","bibtex_type":"misc"}{"bibtex_key":"Lovell 2001","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2015: 37 Table 1 Bonsall et al. 2008: 178 Table 1 Boric 2011: 195","bibtex_type":"misc"}{"bibtex_key":"Boric & Dimitrijevic 2007: Table 1 Boric 2011: 193","bibtex_type":"misc"}[{"bibtex_key":"14SEA","bibtex_type":"misc","url":"{http://www.14sea.org/}","note":"{Reingruber, A., and Thissen, L. (2017). The 14SEA Project: A 14C database for Southeast Europe and Anatolia (10,000–3000 calBC). Updated 2017-01-31. http://www.14sea.org/index.html}"}][{"bibtex_key":"CalPal","bibtex_type":"misc","title":"{CalPal Edition 2022.9}","author":"{Weninger, Bernie}","year":"{2022}","month":"{sep}","doi":"{1010.5281/zenodo.7422618}","url":"{https://zenodo.org/record/7422618}","abstract":"{CalPal is scientific freeware for 14C-based chronological research for Holocene and Palaeolithic Archaeology.}","copyright":"{Creative Commons Attribution 4.0 International, Open Access}","howpublished":"{Zenodo}","month_numeric":"{9}"}][{"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":"dErricoEtAl2011","bibtex_type":"article","title":"{PACEA Geo-Referenced Radiocarbon Database}","author":"{}","date":"{2011}","journaltitle":"{PaleoAnthropology}","volume":"{2011}","pages":"{1–12}","abstract":"{Numerous Paleolithic radiocarbon databases exist, but their geographic and temporal scopes are diverse and their availability variable. With this paper we make available to the scientific community a georeferenced database of radiocarbon ages for the late Middle Paleolithic, Upper Paleolithic, and initial Holocene in Europe. The PACEA radiocarbon database consists of conventional and AMS 14C age determinations from archaeological sites in Europe that fall within Marine Isotope Stages (MIS) 3–1. In all, we have assembled 6,019 radiocarbon ages (conventional=3,820, AMS=2,176, unspecified=23) from a total of 1,208 sites, along with comprehensive contextual information on the dated samples.}","keywords":"{⛔ No DOI found}","file":"{/home/joeroe/g/work/library/2011/d’Errico_et_al_2011.pdf}"}][{"bibtex_key":"p3k14c","bibtex_type":"article","title":"{P3k14c, a Synthetic Global Database of Archaeological Radiocarbon Dates}","author":"{Bird, Darcy and Miranda, Lux and Vander Linden, Marc and Robinson, Erick and Bocinsky, R. Kyle and Nicholson, Chris and Capriles, José M. and Finley, Judson Byrd and Gayo, Eugenia M. and Gil, Adolfo and d’Alpoim Guedes, Jade and Hoggarth, Julie A. and Kay, Andrea and Loftus, Emma and Lombardo, Umberto and Mackie, Madeline and Palmisano, Alessio and Solheim, Steinar and Kelly, Robert L. and Freeman, Jacob}","year":"{2022}","month":"{jan}","journal":"{Scientific Data}","volume":"{9}","number":"{1}","pages":"{27}","publisher":"{Nature Publishing Group}","issn":"{2052-4463}","doi":"{10.1038/s41597-022-01118-7}","abstract":"{Archaeologists increasingly use large radiocarbon databases to model prehistoric human demography (also termed paleo-demography). Numerous independent projects, funded over the past decade, have assembled such databases from multiple regions of the world. These data provide unprecedented potential for comparative research on human population ecology and the evolution of social-ecological systems across the Earth. However, these databases have been developed using different sample selection criteria, which has resulted in interoperability issues for global-scale, comparative paleo-demographic research and integration with paleoclimate and paleoenvironmental data. We present a synthetic, global-scale archaeological radiocarbon database composed of 180,070 radiocarbon dates that have been cleaned according to a standardized sample selection criteria. This database increases the reusability of archaeological radiocarbon data and streamlines quality control assessments for various types of paleo-demographic research. As part of an assessment of data quality, we conduct two analyses of sampling bias in the global database at multiple scales. This database is ideal for paleo-demographic research focused on dates-as-data, bayesian modeling, or summed probability distribution methodologies.}","copyright":"{2022 The Author(s)}","langid":"{english}","keywords":"{Archaeology,Chemistry}","month_numeric":"{1}"}]
---
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---
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---
:bibtex_key: Silva_VanderLinden_2017
:bibtex_type: :misc
---
:bibtex_key: 14SEA
:bibtex_type: :misc
---
- :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: Sapozhnikov I. 2005
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---
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---
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---
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:bibtex_type: :misc
---
:bibtex_key: 'Bonsall et al. 2008: 178 Table 1 Bonsall et al. 2015: 38 Table 1 Boric
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:bibtex_type: :misc
---
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---
:bibtex_key: Lovell 2001
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---
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:bibtex_type: :misc
---
- :bibtex_key: 14SEA
  :bibtex_type: :misc
  :url: "{http://www.14sea.org/}"
  :note: "{Reingruber, A., and Thissen, L. (2017). The 14SEA Project: A 14C database
    for Southeast Europe and Anatolia (10,000–3000 calBC). Updated 2017-01-31. http://www.14sea.org/index.html}"
---
- :bibtex_key: CalPal
  :bibtex_type: :misc
  :title: "{CalPal Edition 2022.9}"
  :author: "{Weninger, Bernie}"
  :year: "{2022}"
  :month: "{sep}"
  :doi: "{1010.5281/zenodo.7422618}"
  :url: "{https://zenodo.org/record/7422618}"
  :abstract: "{CalPal is scientific freeware for 14C-based chronological research
    for Holocene and Palaeolithic Archaeology.}"
  :copyright: "{Creative Commons Attribution 4.0 International, Open Access}"
  :howpublished: "{Zenodo}"
  :month_numeric: "{9}"
---
- :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: dErricoEtAl2011
  :bibtex_type: :article
  :title: "{PACEA Geo-Referenced Radiocarbon Database}"
  :author: "{}"
  :date: "{2011}"
  :journaltitle: "{PaleoAnthropology}"
  :volume: "{2011}"
  :pages: "{1–12}"
  :abstract: "{Numerous Paleolithic radiocarbon databases exist, but their geographic
    and temporal scopes are diverse and their availability variable. With this paper
    we make available to the scientific community a georeferenced database of radiocarbon
    ages for the late Middle Paleolithic, Upper Paleolithic, and initial Holocene
    in Europe. The PACEA radiocarbon database consists of conventional and AMS 14C
    age determinations from archaeological sites in Europe that fall within Marine
    Isotope Stages (MIS) 3–1. In all, we have assembled 6,019 radiocarbon ages (conventional=3,820,
    AMS=2,176, unspecified=23) from a total of 1,208 sites, along with comprehensive
    contextual information on the dated samples.}"
  :keywords: "{⛔ No DOI found}"
  :file: "{/home/joeroe/g/work/library/2011/d’Errico_et_al_2011.pdf}"
---
- :bibtex_key: p3k14c
  :bibtex_type: :article
  :title: "{P3k14c, a Synthetic Global Database of Archaeological Radiocarbon Dates}"
  :author: "{Bird, Darcy and Miranda, Lux and Vander Linden, Marc and Robinson, Erick
    and Bocinsky, R. Kyle and Nicholson, Chris and Capriles, José M. and Finley, Judson
    Byrd and Gayo, Eugenia M. and Gil, Adolfo and d’Alpoim Guedes, Jade and Hoggarth,
    Julie A. and Kay, Andrea and Loftus, Emma and Lombardo, Umberto and Mackie, Madeline
    and Palmisano, Alessio and Solheim, Steinar and Kelly, Robert L. and Freeman,
    Jacob}"
  :year: "{2022}"
  :month: "{jan}"
  :journal: "{Scientific Data}"
  :volume: "{9}"
  :number: "{1}"
  :pages: "{27}"
  :publisher: "{Nature Publishing Group}"
  :issn: "{2052-4463}"
  :doi: "{10.1038/s41597-022-01118-7}"
  :abstract: "{Archaeologists increasingly use large radiocarbon databases to model
    prehistoric human demography (also termed paleo-demography). Numerous independent
    projects, funded over the past decade, have assembled such databases from multiple
    regions of the world. These data provide unprecedented potential for comparative
    research on human population ecology and the evolution of social-ecological systems
    across the Earth. However, these databases have been developed using different
    sample selection criteria, which has resulted in interoperability issues for global-scale,
    comparative paleo-demographic research and integration with paleoclimate and paleoenvironmental
    data. We present a synthetic, global-scale archaeological radiocarbon database
    composed of 180,070 radiocarbon dates that have been cleaned according to a standardized
    sample selection criteria. This database increases the reusability of archaeological
    radiocarbon data and streamlines quality control assessments for various types
    of paleo-demographic research. As part of an assessment of data quality, we conduct
    two analyses of sampling bias in the global database at multiple scales. This
    database is ideal for paleo-demographic research focused on dates-as-data, bayesian
    modeling, or summed probability distribution methodologies.}"
  :copyright: "{2022 The Author(s)}"
  :langid: "{english}"
  :keywords: "{Archaeology,Chemistry}"
  :month_numeric: "{1}"

Changelog