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Becker, Fabian; Eser, Raphael; Hoelzmann, Philipp; Schütt, Brigitta (2018): Geochemistry of five sediment sequences obtained in the Campo coastal plain on Elba Island (Tuscany, Italy) [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.891242, Supplement to: Becker, F et al. (2019): Reconstructing human–landscape interactions in the context of ancient iron smelting on Elba Island, Italy, using sedimentological evidence. Geoarcheology, 34(3), 336-359, https://doi.org/10.1002/gea.21726

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Published: 2018-06-20DOI registered: 2018-08-02

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Abstract:
We obtained five sediment sequences by percussion drilling in order to reconstruct human-landscape interactions in the context of ancient bloomery smelting on Elba Island, Tyrrhenian Sea, based on sedimentological evidences; Elba was, together with Populonia, the centre of iron production in antiquity (mid-6th century B.C.E. to 2nd century C.E.). The aim of the analysis is an assessment of (1) palaeolandscape site conditions, (2) morphodynamics triggered by human land use change (especially charcoal production to run the bloomeries); and (3) to characterize a sediment smelting signature. We described the sediments macroscopically and measured basic bulk geochemical parameters, including pH, electric conductivity, total organic and inorganic carbon contents (estimated using LOI at 560 °C and 900 °C), magnetic susceptibility, and sediment colour. The element composition of the sediment sequences was obtained by ICP-OES, portable ED-XRF, and a CHN+S analyser. Geochemical units ('chemofazies') were grouped by cluster analysis in a compositional-data framework.
Coverage:
Median Latitude: 42.761950 * Median Longitude: 10.232009 * South-bound Latitude: 42.741160 * West-bound Longitude: 10.216650 * North-bound Latitude: 42.770870 * East-bound Longitude: 10.237080
Size:
11 datasets

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Datasets listed in this publication series

  1. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Bulk geochemical parameters in Elba_F-I sediment core from the Campo coastal plain on Elba Island. https://doi.org/10.1594/PANGAEA.891231
  2. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Elemental composition of Elba_F-I sediment core from the Campo coastal plain on Elba Island determined by ICP-OES. https://doi.org/10.1594/PANGAEA.891234
  3. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Elemental composition of Elba_F-I sediment core from the Campo coastal plain on Elba Island determined by portable ED-XRF. https://doi.org/10.1594/PANGAEA.891236
  4. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Elemental composition of Elba_F-II sediment core from the Campo coastal plain on Elba Island determined by portable ED-XRF. https://doi.org/10.1594/PANGAEA.891237
  5. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Bulk geochemical parameters in Elba_F-III sediment core from the Campo coastal plain on Elba Island. https://doi.org/10.1594/PANGAEA.891232
  6. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Elemental composition of Elba_F-III sediment core from the Campo coastal plain on Elba Island determined by ICP-OES. https://doi.org/10.1594/PANGAEA.891235
  7. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Elemental composition of Elba_F-III sediment core from the Campo coastal plain on Elba Island determined by portable ED-XRF. https://doi.org/10.1594/PANGAEA.891238
  8. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Magnetic susceptibility in Elba_F-III sediment core from the Campo coastal plain on Elba Island. https://doi.org/10.1594/PANGAEA.891241
  9. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Bulk geochemical parameters in Elba_S-I sediment core from the Campo coastal plain on Elba Island. https://doi.org/10.1594/PANGAEA.891233
  10. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Elemental composition of Elba_S-I sediment core from the Campo coastal plain on Elba Island determined by portable ED-XRF. https://doi.org/10.1594/PANGAEA.891239
  11. Becker, F; Eser, R; Hoelzmann, P et al. (2018): Elemental composition of Elba_S-II sediment core from the Campo coastal plain on Elba Island determined by portable ED-XRF. https://doi.org/10.1594/PANGAEA.891240