4.7 Article

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

期刊

LIMNOLOGY AND OCEANOGRAPHY
卷 66, 期 6, 页码 2408-2422

出版社

WILEY
DOI: 10.1002/lno.11761

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资金

  1. Swedish Research Council (Vetenskapsradet) [2008-03741, 2011-03638, 2014-05219]
  2. Vinnova [2014-05219] Funding Source: Vinnova
  3. Swedish Research Council [2014-05219, 2011-03638, 2008-03741] Funding Source: Swedish Research Council

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Monitoring of surface waters in the boreal region over the last decades has shown that waters are becoming browner due to human impacts. Human land use since around 700 AD and industrial acid deposition in the 20th century have led to a decrease in lake-water TOC levels, resulting in unprecedentedly low levels. The study highlights the importance of considering past, long-term disturbances in understanding contemporary environmental changes.
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 similar to 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 similar to 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 20(th) 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.

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