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Long-term development and trajectories of inferred lake-water organic carbon and pH in naturally acidic boreal lakes

Myrstener, Erik (författare)
Umeå universitet,Institutionen för ekologi, miljö och geovetenskap,Arcum
Ninnes, Sofia (författare)
Umeå universitet,Institutionen för ekologi, miljö och geovetenskap
Meyer-Jacob, Carsten, 1984- (författare)
Umeå universitet,Institutionen för ekologi, miljö och geovetenskap,Paleoecological Environmental Assessment and Research Laboratory (PEARL), Department of Biology, Queen's University, ON, Kingston, Canada,Arcum
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Mighall, Tim (författare)
Department of Geography and Environment, School of Geosciences, University of Aberdeen, Aberdeen, United Kingdom
Bindler, Richard, 1963- (författare)
Umeå universitet,Institutionen för ekologi, miljö och geovetenskap,Arcum
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 (creator_code:org_t)
2021-05-04
2021
Engelska.
Ingår i: Limnology and Oceanography. - : John Wiley & Sons. - 0024-3590 .- 1939-5590. ; 66:6, s. 2408-2422
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • Monitoring of surface waters in the boreal region over the last decades shows that waters are becoming browner. This timeframe may not, however, be sufficient to capture underlying trajectories and driving mechanisms of lake-water quality, important for prediction of future trajectories. Here we synthesize data from seven lakes in the Swedish boreal landscape, with contemporary lake-water total organic carbon (TOC) concentrations of 1.4–14.4 mg L−1, to conceptualize how natural and particularly human-driven processes at the landscape scale have regulated lake-water TOC levels over the Holocene. Sediment-inferred trends in TOC are supported by several proxies, including diatom-inferred pH. Before ~ 700 ce, all lakes were naturally acidic (pH 4.7–5.4) and the concentrations of inferred lake-water TOC were high (10–23 mg L−1). The introduction of traditional human land use from ~ 700 ce led to a decrease in lake-water TOC in all lakes (to 5–14 mg L−1), and in four poorly buffered lakes, also to an increase in pH by > 1 unit. During the 20th century, industrial acid deposition was superimposed on centuries of land use, which resulted in unprecedentedly low lake-water TOC in all lakes (3–11 mg L−1) and severely reduced pH in the four poorly buffered lakes. The other lakes resisted pH changes, likely due to close connections to peatlands. Our results indicate that an important part of the recent browning of boreal lakes is a recovery from human impacts. Furthermore, on a conceptual level we stress that contemporary environmental changes occur within the context of past, long-term disturbances.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)

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