Bayesian spatiotemporal analysis of radiocarbon dates from Eastern Fennoscandia

Research output: Contribution to journalArticleScientificpeer-review

Abstract

Archaeological phenomena, especially those that have been radiocarbon dated, can be utilized as indications of human activity and occupancy in space and time. 14C dates from archaeological contexts have been used as proxies for population history events in several recent studies (e.g. Gamble et al. 2005; Shennan and Edinborough 2007; Oinonen et al. 2010; Tallavaara et al. 2010; Pesonen et al. 2011). As a step towards a larger spatiotemporal modeling effort, we present examples of spatial distributions obtained using Bayesian methodology, analyzing all available archaeological 14C dates from the Stone Age (9000–1500 cal BC) in eastern Fennoscandia. The resulting maps follow the patterns of pioneer settlement in Finland beginning at ~9000 cal BC and provide supporting evidence for the postulated population peak around 4000–3500 cal BC in Finland and the subsequent population decline.

Original languageEnglish
JournalRadiocarbon
Volume54
Issue number3-4
Pages (from-to)649-659
Number of pages11
ISSN0033-8222
Publication statusPublished - 2012
MoE publication typeA1 Journal article-refereed

Fields of Science

  • 114 Physical sciences

Cite this

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title = "Bayesian spatiotemporal analysis of radiocarbon dates from Eastern Fennoscandia",
abstract = "Archaeological phenomena, especially those that have been radiocarbon dated, can be utilized as indications of human activity and occupancy in space and time. 14C dates from archaeological contexts have been used as proxies for population history events in several recent studies (e.g. Gamble et al. 2005; Shennan and Edinborough 2007; Oinonen et al. 2010; Tallavaara et al. 2010; Pesonen et al. 2011). As a step towards a larger spatiotemporal modeling effort, we present examples of spatial distributions obtained using Bayesian methodology, analyzing all available archaeological 14C dates from the Stone Age (9000–1500 cal BC) in eastern Fennoscandia. The resulting maps follow the patterns of pioneer settlement in Finland beginning at ~9000 cal BC and provide supporting evidence for the postulated population peak around 4000–3500 cal BC in Finland and the subsequent population decline.",
keywords = "114 Physical sciences",
author = "P{\"a}ivi Onkamo and Juhana Kammonen and Petro Pesonen and Tarja Sundell and Elena Moltchanova and Markku Oinonen and Miikka Haimila and Elja Arjas",
year = "2012",
language = "English",
volume = "54",
pages = "649--659",
journal = "Radiocarbon",
issn = "0033-8222",
publisher = "UNIV ARIZONA DEPT GEOSCIENCES",
number = "3-4",

}

Bayesian spatiotemporal analysis of radiocarbon dates from Eastern Fennoscandia. / Onkamo, Päivi; Kammonen, Juhana; Pesonen, Petro; Sundell, Tarja; Moltchanova, Elena; Oinonen, Markku; Haimila, Miikka; Arjas, Elja.

In: Radiocarbon, Vol. 54, No. 3-4, 2012, p. 649-659.

Research output: Contribution to journalArticleScientificpeer-review

TY - JOUR

T1 - Bayesian spatiotemporal analysis of radiocarbon dates from Eastern Fennoscandia

AU - Onkamo, Päivi

AU - Kammonen, Juhana

AU - Pesonen, Petro

AU - Sundell, Tarja

AU - Moltchanova, Elena

AU - Oinonen, Markku

AU - Haimila, Miikka

AU - Arjas, Elja

PY - 2012

Y1 - 2012

N2 - Archaeological phenomena, especially those that have been radiocarbon dated, can be utilized as indications of human activity and occupancy in space and time. 14C dates from archaeological contexts have been used as proxies for population history events in several recent studies (e.g. Gamble et al. 2005; Shennan and Edinborough 2007; Oinonen et al. 2010; Tallavaara et al. 2010; Pesonen et al. 2011). As a step towards a larger spatiotemporal modeling effort, we present examples of spatial distributions obtained using Bayesian methodology, analyzing all available archaeological 14C dates from the Stone Age (9000–1500 cal BC) in eastern Fennoscandia. The resulting maps follow the patterns of pioneer settlement in Finland beginning at ~9000 cal BC and provide supporting evidence for the postulated population peak around 4000–3500 cal BC in Finland and the subsequent population decline.

AB - Archaeological phenomena, especially those that have been radiocarbon dated, can be utilized as indications of human activity and occupancy in space and time. 14C dates from archaeological contexts have been used as proxies for population history events in several recent studies (e.g. Gamble et al. 2005; Shennan and Edinborough 2007; Oinonen et al. 2010; Tallavaara et al. 2010; Pesonen et al. 2011). As a step towards a larger spatiotemporal modeling effort, we present examples of spatial distributions obtained using Bayesian methodology, analyzing all available archaeological 14C dates from the Stone Age (9000–1500 cal BC) in eastern Fennoscandia. The resulting maps follow the patterns of pioneer settlement in Finland beginning at ~9000 cal BC and provide supporting evidence for the postulated population peak around 4000–3500 cal BC in Finland and the subsequent population decline.

KW - 114 Physical sciences

M3 - Article

VL - 54

SP - 649

EP - 659

JO - Radiocarbon

JF - Radiocarbon

SN - 0033-8222

IS - 3-4

ER -