DOI: 10.1016/j.epsl.2020.116183
论文题名: Analysis of geomagnetic field intensity variations in Mesopotamia during the third millennium BC with archeological implications
作者: Gallet Y. ; Fortin M. ; Fournier A. ; Le Goff M. ; Livermore P.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2020
卷: 537 语种: 英语
中文关键词: archeointensity
; archeological implications
; archeomagnetism
; Near East
; third millennium BC
; variation rates
英文关键词: Bayesian networks
; Magnetometers
; Archeointensity
; archeological implications
; Archeomagnetism
; Near East
; third millennium BC
; Geomagnetism
; archaeology
; Bayesian analysis
; Bronze Age
; data quality
; geomagnetic field
; paleomagnetism
; secular variation
; Levant
; Mediterranean Region
; Mesopotamia
; Syrian Arab Republic
; Turkey
英文摘要: We present new archeointensity results obtained at two multi-layer archeological sites, Tell Atij and Tell Gudeda (northeastern Syria), dated from the Early Bronze Period in the third millennium BC. The archeointensity data were obtained using the experimental protocol developed for the Triaxe magnetometer. In total, 68 fragments (204 specimens) of 151 fragments analyzed passed our selection criteria, allowing average intensity values to be estimated for 14 archeological layers, nine at Tell Atij and five at Tell Gudeda. Based on the available archeological constraints, the different archeological layers of Tell Atij and Tell Gudeda were dated between ∼2900 BC and ∼2600 BC and between ∼2550 BC and ∼2325 BC, respectively. The Tell Atij data show a significant increase in intensity over the dated period, while the results from Tell Gudeda exhibit a V-shape evolution. Using high-quality data available from Syria, the Levant and Turkey, a regional geomagnetic field intensity variation curve spanning the entire third millennium BC was constructed using a trans-dimensional Bayesian method. It clearly shows two intensity peaks, around 2600 BC and at ∼2300 BC, associated with variation rates of ∼0.1-0.2 μT/yr. This indicates that the occurrence of century-scale intensity peaks with rates of variation comparable to or even slightly higher than the maximum rates observed in the modern geomagnetic field is an ubiquitous feature of the geomagnetic secular variation. From an archeological point of view, the new archeointensity data strengthen the hypothesis that the successive occupation of Tell Atij and Tell Gudeda was synchronous with the two first urban phases of Mari, making possible a sustained trade network between these settlements during the third millennium BC. We further suggest that the end of Mari's first urban phase, contemporaneous with the abandonment of Tell Atij, might have been caused by a regional drought episode around 2600 BC. More generally, the Bayesian approach used to estimate the new reference intensity variation curve offers promising chronological constraints for archeological purposes. © 2020 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/164972
Appears in Collections: 气候变化与战略
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作者单位: Université de Paris, Institut de Physique du Globe de Paris, CNRS, Paris, France; Faculté des lettres et des sciences humaines, Département des sciences historiques, Université LavalQuébec, Canada; School of Earth & Environment, University of Leeds, Leeds, United Kingdom
Recommended Citation:
Gallet Y.,Fortin M.,Fournier A.,et al. Analysis of geomagnetic field intensity variations in Mesopotamia during the third millennium BC with archeological implications[J]. Earth and Planetary Science Letters,2020-01-01,537