OxA-4378
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
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 references (24)
- No bibliographic information available. [Hedges et al. 1998b]
- PACEA Geo-Referenced Radiocarbon Database. (2011). PaleoAnthropology, 2011, 1–12. [PACEA]
- No bibliographic information available. [Boroneant 2000: 203-204, Dinu et al. 2007: Table 2, Bonsall 2008: Table 10.4]
- No bibliographic information available. [Boroneant 2000: 203-204, Dinu et al. 2007: Table 2]
- No bibliographic information available. [Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table 2, Borić 2011: 199]
- No bibliographic information available. [Dinu et al. 2007: Table 1]
- No bibliographic information available. [Boroneanţ 1973, Groningen 14C database]
- No bibliographic information available. [Bonsall 2008: Table 10.1, Borić 2011: 199]
- No bibliographic information available. [Bonsall 2008: Table 10.1]
- No bibliographic information available. [Bonsall 2008: Table 10.1, Borić 2011: 200]
- No bibliographic information available. [Boroneant et al. 1999, Boroneanţ 2000: 203-204, Dinu et al. 2007: Table 2, Borić 2011: 200]
- No bibliographic information available. [Bonsall et al. 2000: 123, Bonsall 2008: Table 10.1, Borić 2011: 200]
- No bibliographic information available. [Bonsall et al. 2000: 124, Bonsall 2008: Table 10.1, Borić 2011: 200]
- No bibliographic information available. [Bonsall 2008: Table 10.4]
- No bibliographic information available. [Borić 2011]
- No bibliographic information available. [Borić 2009, 2011]
- Hinz, M., Furholt, M., Müller, J., Raetzel-Fabian, D., Rinne, C., Sjögren, K.-G., & Wotzka, H.-P. (2012). RADON - Radiocarbon Dates Online 2012. Central European Database of 14C Dates for the Neolithic and the Early Bronze Age. Journal of Neolithic Archaeology, 14, 1–4. https://www.jna.uni-kiel.de/index.php/jna/article/view/65/116 [RADON]
- No bibliographic information available. [Boroneant 1973 Groningen 14C database]
- No bibliographic information available. [Bonsall 2008: Table 10.1 Boric 2011: 199]
- No bibliographic information available. [Bonsall 2008: Table 10.1 Boric 2011: 200]
- No bibliographic information available. [Bonsall et al. 2000: 124 Bonsall 2008: Table 10.1 Boric 2011: 200]
- No bibliographic information available. [Bonsall et al. 2000: 123 Bonsall 2008: Table 10.1 Boric 2011: 200]
- No bibliographic information available. [Nalawade-Chavan et al. 2013]
- No bibliographic information available. [Langlais M. 2015. BSPF 112: 5-58. Barshay-Szmidt C. Quaternary International 414 (2016) 62-91.]
@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