2022
DOI: 10.1016/j.scitotenv.2022.156083
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The forest effect: Biosphere 87Sr/86Sr shifts due to changing land use and the implications for migration studies

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Cited by 12 publications
(15 citation statements)
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“…The plant samples collected from location 6 (old mining site) on the Pennine Lower Coal Measures range from 0.7145 to 0.7151, and are higher in comparison to the plant 87 Sr/ 86 Sr based on the same geological bedrock, albeit c. 50km north of the site [ 28 ], with a difference of approximately 0.0030. They also contrast with data collected by Johnson [ 29 , 30 ] from the Pennine Coal Measures around Nuneaton, at 0.7103 and 0.7106, immediately south of the 25km catchment border. A further 12 plant samples based on the Precambrian Charnian Supergroup and the Charnwood Diorites southeast of Heath Wood range between 0.7104 and 0.7112, whilst a singular plant at 0.7110 is found on the Ordovician Mountsorrel Igneous Complex [ 29 ] ( Fig 5 ; SI.3—S1 Table S1 File ).…”
Section: Resultscontrasting
confidence: 88%
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“…The plant samples collected from location 6 (old mining site) on the Pennine Lower Coal Measures range from 0.7145 to 0.7151, and are higher in comparison to the plant 87 Sr/ 86 Sr based on the same geological bedrock, albeit c. 50km north of the site [ 28 ], with a difference of approximately 0.0030. They also contrast with data collected by Johnson [ 29 , 30 ] from the Pennine Coal Measures around Nuneaton, at 0.7103 and 0.7106, immediately south of the 25km catchment border. A further 12 plant samples based on the Precambrian Charnian Supergroup and the Charnwood Diorites southeast of Heath Wood range between 0.7104 and 0.7112, whilst a singular plant at 0.7110 is found on the Ordovician Mountsorrel Igneous Complex [ 29 ] ( Fig 5 ; SI.3—S1 Table S1 File ).…”
Section: Resultscontrasting
confidence: 88%
“… Location 6 samples from this study not included. Additional samples from Johnson [ 29 , 30 ] from the Charnwood area (see Fig 4 ). For information on lithology and sample location see Fig 4 and SI.3—S1 Table in S1 File .…”
Section: Resultsmentioning
confidence: 99%
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“…Biosphere mapping of southwest England, guided by geochemical soil profiles [ 34 ], has highlighted areas around the granite intrusions in Devon and Cornwall where Sr in plants reaches values of 87 Sr/ 86 Sr = 0.72 [ 28 ] and Roman and Medieval sheep from this region record 87 Sr/ 86 Sr ratios up to 0.717 [ 35 , 36 ]. In addition, it has been shown [ 37 , 38 ] that well-established forest on certain terrains, typically those with soils derived from both siliceous and carbonate bedrock, will leach out the carbonate component over time, resulting in a more radiogenic signature for the forest area. These developments mean there are now areas of England that can be considered as a possible source region as well as parts of Scotland.…”
Section: Introductionmentioning
confidence: 99%