Environmental footprint of small-scale, historical mining and metallurgy in the Swedish boreal forest landscape: The Moshyttan blast furnace as microcosm/ (Record no. 12808)

MARC details
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fixed length control field 03113nab a2200337 4500
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control field 20220816163159.0
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Personal name Myrstener, Erik
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Title Environmental footprint of small-scale, historical mining and metallurgy in the Swedish boreal forest landscape: The Moshyttan blast furnace as microcosm/
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Name of publisher, distributor, etc Sage,
Date of publication, distribution, etc 2019.
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Pages Vol 29, issue 4, 2019 : (578-591 p.).
520 ## - SUMMARY, ETC.
Summary, etc The history of mining and smelting and the associated pollution have been documented using lake sediments for decades, but the broader ecological implications are not well studied. We analyzed sediment profiles covering the past ~10,000 years from three lakes associated with an iron blast furnace in central Sweden, as an example of the many small-scale furnaces with historical roots in the medieval period. With a focus on long-term lake-water quality, we analyzed multiple proxies including geochemistry, pollen and charcoal, diatom composition and inferred pH, biogenic silica (bSi), visible near-infrared spectroscopy (VNIRS)-inferred lake-water total organic carbon (LW-TOC), and VNIRS-inferred sediment chlorophyll (sed-Chl). All three lakes had stable conditions during the middle Holocene (~5000 BCE to 1110 CE) typical of oligo-dystrophic lakes: pH 5.4–5.6, LW-TOC 15–18 mg L−1. The most important diatom taxa include, for example, Aulacoseira scalaris, Brachysira neoexilis, and Frustulia saxonica. From ~1150 CE, decreases in LW-TOC, bSi, and sed-Chl in all three lakes coincide with a suite of proxies indicating disturbance associated with local, small-scale agriculture, and the more widespread use of the landscape in the past (e.g. forest grazing, charcoal production). Most important was a decline in LW-TOC by 30–50% in the three lakes prior to the 20th century. In addition, the one lake (Fickeln) downstream of the smelter and main areas of cultivation experienced a shift in diatom composition (mainly increasing Asterionella formosa) and a 0.6 pH increase coinciding with increasing cereal pollen and signs of blast furnace activity. The pH did not change in the other two lakes in response to disturbance; however, these lakes show a slight increase (0.3–0.5 pH units) because of modern liming. LW-TOC has returned to background levels in the downstream lake and remains lower in the other two.
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Subject diatoms,
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Subject environmental change,
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Subject geochemistry,
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Subject human impacts,
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Subject lake-water carbon,
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Subject sediment,
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Subject total organic carbon
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Added Entry Personal Name Harald Biester,
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Added Entry Personal Name Bigler, Christian
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Added Entry Personal Name Lidberg, William
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Added Entry Personal Name Meyer-Jacob, Carsten
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Added Entry Personal Name Rydberg, Johan
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Added Entry Personal Name Bindler, Richard
773 0# - HOST ITEM ENTRY
Host Biblionumber 12756
Host Itemnumber 16504
Place, publisher, and date of publication London: Sage Publication Ltd, 2019.
Title Holocene/
International Standard Serial Number 09596836
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Uniform Resource Identifier https://doi.org/10.1177/0959683618824741
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Koha item type Articles
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