Mines de Gavà
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
Location
- Coordinates (degrees)
- 041.312° N, 002.001° E
- Coordinates (DMS)
- 041° 18' 00" E, 002° 00' 00" N
- Country (ISO 3166)
- Spain (ES)
Linked Data
There is no linked data available for this record.
| Lab ID | Context | Material | Taxon | Method | Uncalibrated age | Calibrated age | References |
|---|---|---|---|---|---|---|---|
| I-13099 | Mina; Mina 28A/C IV | charcoal | NA | NA | 4820±100 BP | 5845–5315 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| UBAR-363 | Mina; Mina 7/Sala B, N V | charcoal | NA | NA | 5460±850 BP | 7944–4153 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| UBAR-42 | Mina; Mina 41 | charcoal | NA | NA | 4820±100 BP | 5845–5315 cal BP | Martín 1998; Mestres et al. 1991 Hinz et al. 2012 |
| UBAR-47 | Mina; Mina 28A C IV | charcoal | NA | NA | 4610±90 BP | 5577–4985 cal BP | Martín 1998; Mestres et al. 1991 Hinz et al. 2012 |
| I-12731 | Mina; Mina 8, F1 | charcoal | NA | NA | 5350±190 BP | 6499–5658 cal BP | Villalba et al. 1986; Martín 1998 Hinz et al. 2012 |
| I-12730 | Mina; Mina 8, sala F sepulcral | charcoal | NA | NA | 4310±150 BP | 5316–4444 cal BP | Martín 1998 Hinz et al. 2012 |
| UBAR-48 | Mina; Mina 28C/C1 | charcoal | NA | NA | 4690±100 BP | 5600–5051 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| UBAR-30 | Mina; Mina 28A/C IV | charcoal | NA | NA | 4710±130 BP | 5718–4985 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| UBAR-365 | Mina; Mina 7/Sala B, N VII | charcoal | NA | NA | 5140±210 BP | 6389–5465 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| UBAR-46 | Mina; Mina 28A/C IV | charcoal | NA | NA | 4380±80 BP | 5285–4835 cal BP | Mestres et al. 1991 Hinz et al. 2012 |
| I-11786 | Mina; Mina 6, pou 1f | charcoal | NA | NA | 5070±100 BP | 6105–5591 cal BP | Martín 1998 Hinz et al. 2012 |
| UBAR-364 | Mina; Mina 7/Sala B, N VI | charcoal | NA | NA | 4930±360 BP | 6486–4654 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| Beta-72551 | Mina; Mina 70, N5 | charcoal | NA | NA | 4930±70 BP | 5895–5483 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| Beta-72552 | Mina; Mina 70, N6 | charcoal | NA | NA | 5010±60 BP | 5900–5602 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| Beta-72553 | Mina; Mina 70, N6 | charcoal | NA | NA | 5090±60 BP | 5986–5660 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| I-12158 | Mina; Mina 8, galería | charcoal | NA | NA | 4880±100 BP | 5895–5327 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| UBAR-366 | Mina; Mina 6, pou 1g | charcoal | NA | NA | 4810±60 BP | 5655–5326 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| UBAR-41 | Mina; Mina 49 | charcoal | NA | NA | 4970±110 BP | 5931–5476 cal BP | Telearchaeology 2014 ; Mestres et al. 1991 Hinz et al. 2012 |
| Beta-61491 | Mina; Mina 70, N2 | collagen, bone | Os | NA | 4660±110 BP | 5595–4987 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| CSIC-488 | Mina; Mina 7/pou, N I | charcoal | NA | NA | 4710±50 BP | 5579–5320 cal BP | Telearchaeology 2014 Hinz et al. 2012 |
| Classification | Estimated age | References |
|---|---|---|
| Mig | NA | Telearchaeology 2014 |
| Neolithikum | NA | NA |
| Mig | NA | Telearchaeology 2014 |
| Neolithikum | NA | NA |
| Mig | NA | Martín 1998; Mestres et al. 1991 |
| Neolithikum | NA | NA |
| Mig | NA | Martín 1998; Mestres et al. 1991 |
| Neolithikum | NA | NA |
| Mig | NA | Villalba et al. 1986; Martín 1998 |
| Neolithikum | NA | NA |
| Final | NA | Martín 1998 |
| Neolithikum | NA | NA |
| Mig | NA | Telearchaeology 2014 |
| Neolithikum | NA | NA |
| Mig | NA | Telearchaeology 2014 |
| Neolithikum | NA | NA |
| Mig | NA | Telearchaeology 2014 |
| Neolithikum | NA | NA |
| Mig | NA | Mestres et al. 1991 |
| Neolithikum | NA | NA |
Bibliographic references
- No bibliographic information available. [Mestres et al. 1991]
- No bibliographic information available. [Telearchaeology 2014]
- No bibliographic information available. [Martín 1998]
- No bibliographic information available. [Martín 1998; Mestres et al. 1991]
- No bibliographic information available. [Villalba et al. 1986; Martín 1998]
- No bibliographic information available. [Telearchaeology 2014 ; Mestres et al. 1991]
- 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]
@misc{Mestres et al. 1991,
}
@misc{Telearchaeology 2014,
}
@misc{Martín 1998,
}
@misc{Martín 1998; Mestres et al. 1991,
}
@misc{Villalba et al. 1986; Martín 1998,
}
@misc{Telearchaeology 2014 ; Mestres et al. 1991,
}
@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":"Mestres et al. 1991","bibtex_type":"misc"}{"bibtex_key":"Telearchaeology 2014","bibtex_type":"misc"}{"bibtex_key":"Martín 1998","bibtex_type":"misc"}{"bibtex_key":"Martín 1998; Mestres et al. 1991","bibtex_type":"misc"}{"bibtex_key":"Villalba et al. 1986; Martín 1998","bibtex_type":"misc"}{"bibtex_key":"Telearchaeology 2014 ; Mestres et al. 1991","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: Mestres et al. 1991
:bibtex_type: :misc
---
:bibtex_key: Telearchaeology 2014
:bibtex_type: :misc
---
:bibtex_key: Martín 1998
:bibtex_type: :misc
---
:bibtex_key: Martín 1998; Mestres et al. 1991
:bibtex_type: :misc
---
:bibtex_key: Villalba et al. 1986; Martín 1998
:bibtex_type: :misc
---
:bibtex_key: Telearchaeology 2014 ; Mestres et al. 1991
: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.}"