Multi-proxy analyses of a minerotrophic fen to reconstruct prehistoric periods of human activity associated with salt mining in the Hallstatt region (Austria)
Bibliographic Data
| ID | 13097031 |
|---|---|
| Authors | Wolfgang Knierzinger (0000-0001-8944-1213, University of Vienna, corresponding author), Daniela Festi (0000-0003-1250-4815, Institute for Interdisciplinary Mountain Research), Andreas Limbeck (0000-0001-5042-2445, TU Wien), Felix Horak (0000-0002-0089-4134, TU Wien), Lukas Brunnbauer (0000-0001-7423-4668, TU Wien), Simon Drollinger (0000-0002-4912-2629, University of Göttingen), Michael Wagreich (0000-0002-8828-0857, University of Vienna), Jyh‐jaan Steven Huang (0000-0001-8815-3957, Universität Innsbruck), Michael Strasser (0000-0003-3991-2405, Universität Innsbruck), Klaus‐holger Knorr (0000-0003-4175-0214), Hans Reschreiter (0000-0003-0337-5660, Natural History Museum Vienna), Susanne Gier (0000-0002-7926-7714, University of Vienna), Werner Kofler (0000-0001-7310-7819, Universität Innsbruck), Christopher Herzig (0000-0002-6904-5739, TU Wien), Kerstin Kowarik (0000-0003-0497-3419, Natural History Museum Vienna) |
| Year | 2021 |
| Volume | 36 |
| Pages | 102813-102813 |
| Publication date | 2021-02-01 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Journal of Archaeological Science Reports (JOURNAL) |
| Journal identifiers | ISSN: 2352-409X • E-ISSN: 2352-4103 |
| Publisher | Elsevier BV (PUBLISHER) |
| DOI | 10.1016/j.jasrep.2021.102813 |
| OpenAlex | W3127792415 |
| Language | EN |
| Citations received | 2 |
| References cited | 82 |
In this study, periods of prehistoric anthropogenic activity in the Hallstatt salt mining area (Upper Austria) are reconstructed from elemental (XRF-scanning, Q-ICP-MS) and Pb isotopic analyses (206Pb,207Pb,208Pb) of a radiocarbon-dated, 137-cm-long peat core covering the past ~7,000 years. The peat core was retrieved from a minerotrophic fen in the Hallstatt High Valley. Distinct metal enrichments attributed to low anthropogenic impact in Hallstatt can be traced back to a time around 2350 cal BCE and to another period around 1800 cal BCE. The period from the Late Bronze Age to the Early Iron Age (~1300 cal BCE to ~500 cal BCE) is characterised by increased anthropogenic activity. Relatively high Sn concentrations between ~1210 cal BCE and ~540 cal BCE) point towards intensive bronze casting processes, probably associated with the production of bronze picks that were used for local salt mining during this time. Intense human impact was also determined for the early Roman imperial period (1st century BCE – 2nd century CE). Increasing Pb and Sb concentrations and a marked decrease of 206Pb/207Pb ratios in the uppermost fen layers are attributed to rising industrialization processes in the modern period. Even though peaks of the trace elements Pb, Sb, Cu and Sn do not always correspond directly to anthropogenic activity, a combination with erosional, archaeological and palaeovegetational records enables a relatively accurate and reliable interpretation of prehistoric human impact at Hallstatt
Archaeology · Art · Bronze · Bronze Age · Chalcolithic · Chronology · Geography · Peat · Period (music · Prehistory · Radiocarbon dating · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Heavy metals in environment · Geology
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| Unique citing works | 2 |
|---|---|
| Citations per year | 0,33 |
| Citation span | 2020 - 2023 (4) |
| Citation velocity | historical |
| Highly cited | No |
| Citation types | Neutral: 2 |