OxA-4378

radiocarbon date Radiocarbon date from Schela Cladovei, c. 9545–9132 cal BP
Record created in XRONOS on 2022-12-02 00:50:45 UTC. Last updated on 2022-12-02 00:50:45 UTC. See changelog for details.
Contributors: XRONOS development team

Measurement

Age (uncal BP)
8415
Error (±)
100
Lab
NA
Method
AMS
Sample material
bone
Sample taxon
NA

Calibration

Calibration curve
IntCal20 (Reimer et al. 2020)
Calibrated age (2σ, cal BP)
  • 9545–9132

Context

Site
Schela Cladovei
Context
habitat
Sample position
NA
Sample coordinates
NA

Bibliographic reference Bibliographic references (24)

@misc{Hedges et al. 1998b,
  
}
@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}
}
@misc{Boroneant 2000: 203-204, Dinu et al. 2007: Table 2, Bonsall 2008: Table 10.4,
  
}
@misc{Boroneant 2000: 203-204, Dinu et al. 2007: Table 2,
  
}
@misc{Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table 2, Borić 2011: 199,
  
}
@misc{Dinu et al. 2007: Table 1,
  
}
@misc{Boroneanţ 1973, Groningen 14C database,
  
}
@misc{Bonsall 2008: Table 10.1, Borić 2011: 199,
  
}
@misc{Bonsall 2008: Table 10.1,
  
}
@misc{Bonsall 2008: Table 10.1, Borić 2011: 200,
  
}
@misc{Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table 2, Borić 2011: 200,
  
}
@misc{Bonsall et al. 2000: 123, Bonsall 2008: Table 10.1, Borić 2011: 200,
  
}
@misc{Bonsall et al. 2000: 124, Bonsall 2008: Table 10.1, Borić 2011: 200,
  
}
@misc{Bonsall 2008: Table 10.4,
  
}
@misc{Borić  2011,
  
}
@misc{Borić  2009, 2011,
  
}
@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{Boroneant 1973 Groningen 14C database,
  
}
@misc{Bonsall 2008: Table 10.1 Boric 2011: 199,
  
}
@misc{Bonsall 2008: Table 10.1 Boric 2011: 200,
  
}
@misc{Bonsall et al. 2000: 124 Bonsall 2008: Table 10.1 Boric 2011: 200,
  
}
@misc{Bonsall et al. 2000: 123 Bonsall 2008: Table 10.1 Boric 2011: 200,
  
}
@misc{Nalawade-Chavan et al. 2013,
  
}
@misc{Langlais M.  2015. BSPF 112: 5-58. Barshay-Szmidt C.  Quaternary International 414 (2016) 62-91.,
  
}
{"bibtex_key":"Hedges et al. 1998b","bibtex_type":"misc"}[{"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":"Boroneant 2000: 203-204, Dinu et al. 2007: Table 2, Bonsall 2008: Table 10.4","bibtex_type":"misc"}{"bibtex_key":"Boroneant 2000: 203-204, Dinu et al. 2007: Table 2","bibtex_type":"misc"}{"bibtex_key":"Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table 2, Borić 2011: 199","bibtex_type":"misc"}{"bibtex_key":"Dinu et al. 2007: Table 1","bibtex_type":"misc"}{"bibtex_key":"Boroneanţ 1973, Groningen 14C database","bibtex_type":"misc"}{"bibtex_key":"Bonsall 2008: Table 10.1, Borić 2011: 199","bibtex_type":"misc"}{"bibtex_key":"Bonsall 2008: Table 10.1","bibtex_type":"misc"}{"bibtex_key":"Bonsall 2008: Table 10.1, Borić 2011: 200","bibtex_type":"misc"}{"bibtex_key":"Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table 2, Borić 2011: 200","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 123, Bonsall 2008: Table 10.1, Borić 2011: 200","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 124, Bonsall 2008: Table 10.1, Borić 2011: 200","bibtex_type":"misc"}{"bibtex_key":"Bonsall 2008: Table 10.4","bibtex_type":"misc"}{"bibtex_key":"Borić  2011","bibtex_type":"misc"}{"bibtex_key":"Borić  2009, 2011","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":"Boroneant 1973 Groningen 14C database","bibtex_type":"misc"}{"bibtex_key":"Bonsall 2008: Table 10.1 Boric 2011: 199","bibtex_type":"misc"}{"bibtex_key":"Bonsall 2008: Table 10.1 Boric 2011: 200","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 124 Bonsall 2008: Table 10.1 Boric 2011: 200","bibtex_type":"misc"}{"bibtex_key":"Bonsall et al. 2000: 123 Bonsall 2008: Table 10.1 Boric 2011: 200","bibtex_type":"misc"}{"bibtex_key":"Nalawade-Chavan et al. 2013","bibtex_type":"misc"}{"bibtex_key":"Langlais M.  2015. BSPF 112: 5-58. Barshay-Szmidt C.  Quaternary International 414 (2016) 62-91.","bibtex_type":"misc"}
---
:bibtex_key: Hedges et al. 1998b
:bibtex_type: :misc
---
- :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: 'Boroneant 2000: 203-204, Dinu et al. 2007: Table 2, Bonsall 2008: Table
  10.4'
:bibtex_type: :misc
---
:bibtex_key: 'Boroneant 2000: 203-204, Dinu et al. 2007: Table 2'
:bibtex_type: :misc
---
:bibtex_key: 'Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table
  2, Borić 2011: 199'
:bibtex_type: :misc
---
:bibtex_key: 'Dinu et al. 2007: Table 1'
:bibtex_type: :misc
---
:bibtex_key: Boroneanţ 1973, Groningen 14C database
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall 2008: Table 10.1, Borić 2011: 199'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall 2008: Table 10.1'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall 2008: Table 10.1, Borić 2011: 200'
:bibtex_type: :misc
---
:bibtex_key: 'Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table
  2, Borić 2011: 200'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall et al. 2000: 123, Bonsall 2008: Table 10.1, Borić 2011: 200'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall et al. 2000: 124, Bonsall 2008: Table 10.1, Borić 2011: 200'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall 2008: Table 10.4'
:bibtex_type: :misc
---
:bibtex_key: Borić  2011
:bibtex_type: :misc
---
:bibtex_key: Borić  2009, 2011
: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: Boroneant 1973 Groningen 14C database
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall 2008: Table 10.1 Boric 2011: 199'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall 2008: Table 10.1 Boric 2011: 200'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall et al. 2000: 124 Bonsall 2008: Table 10.1 Boric 2011: 200'
:bibtex_type: :misc
---
:bibtex_key: 'Bonsall et al. 2000: 123 Bonsall 2008: Table 10.1 Boric 2011: 200'
:bibtex_type: :misc
---
:bibtex_key: Nalawade-Chavan et al. 2013
:bibtex_type: :misc
---
:bibtex_key: 'Langlais M.  2015. BSPF 112: 5-58. Barshay-Szmidt C.  Quaternary International
  414 (2016) 62-91.'
:bibtex_type: :misc

Changelog