Diatom inferred acidity history of 32 lakes on the Kola Peninsula, Russia

被引:18
|
作者
Weckström, J
Snyder, JA
Korhola, A
Laing, TE
MacDonald, GM
机构
[1] Univ Helsinki, Div Hydrobiol, Dept Systemat & Ecol, ECRU, FIN-00014 Helsinki, Finland
[2] Bowling Green State Univ, Dept Geol, Bowling Green, OH 43403 USA
[3] Queens Univ, Dept Biol, PEARL, Kingston, ON K7L 3N6, Canada
[4] Univ Calif Los Angeles, Dept Geog, Los Angeles, CA 90024 USA
[5] Univ Calif Los Angeles, Dept Organism Biol Ecol & Evolut, Los Angeles, CA USA
来源
WATER AIR AND SOIL POLLUTION | 2003年 / 149卷 / 1-4期
基金
芬兰科学院;
关键词
acidification; diatoms; Kola Peninsula; lakes; smelters; sulphur emission;
D O I
10.1023/A:1025682801187
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Kola Peninsula is characterised by vast environmental contrasts. Large areas are almost in pristine condition. However, mining and associated industrial activity generate one of the largest sources of heavy metal and sulphur emissions in the world and create 'technogenic wastelands' around smelters. Due to the lack of monitoring data, insufficient knowledge is available regarding the acidification history of lakes on the peninsula. In this study, palaeolimnological techniques were used to reveal the pre-industrial pH status of 32 small lakes in order to evaluate the role of human impacts on freshwater ecosystems. Diatom-inferred pH reconstructions demonstrated that for 22 (68.75%) of the lakes, the pH was below 6.5 and in eight (25%) below 6.0 during the pre-industrial period; signs of recent acidification could be detected only in seven lakes of which five are located relatively close to current pollution sources. Furthermore, no substantial changes between the pre-industrial and modern species richness and composition were observed, indicating relatively stable environmental conditions. Most of the lakes seem to have undergone long-term acidification and are mainly affected by natural acidifying factors (e.g., vegetation, bedrock, climate, sea salt). The effect of anthropogenic emissions seems to be surprisingly geographically restricted and controlled mainly by the surrounding topography and prevailing winds. However, although many lakes seem to be in relatively pristine condition, only a significant reduction in heavy metal and sulphur emissions will prevent the lakes from acidifying in the future.
引用
收藏
页码:339 / 361
页数:23
相关论文
共 50 条
  • [1] Diatom Inferred Acidity History Of 32 Lakes On The Kola Peninsula, Russia
    Jan Weckström
    Jeffrey A. Snyder
    Atte Korhola
    Tamsin E. Laing
    Glen M. Macdonald
    Water, Air, and Soil Pollution, 2003, 149 : 339 - 361
  • [2] Holocene history of Lake Soldatskoje (Kola Peninsula, Russia) inferred from sedimentary diatom assemblages
    Grönlund, T
    Kauppila, T
    BOREAS, 2002, 31 (03) : 273 - 284
  • [3] Postglacial relative sea-level history: sediment and diatom records of emerged coastal lakes, north-central Kola Peninsula, Russia
    Snyder, JA
    Forman, SL
    Mode, WN
    Tarasov, GA
    BOREAS, 1997, 26 (04) : 329 - 346
  • [4] LEPIDOPTERA OF THE KOLA PENINSULA, NORTHWESTERN RUSSIA
    KOZLOV, MV
    JALAVA, J
    ENTOMOLOGICA FENNICA, 1994, 5 (02) : 65 - 85
  • [5] Diamond potential of the Kola Peninsula (Russia)
    Chashchin, VV
    GEOLOGY OF ORE DEPOSITS, 1997, 39 (06) : 489 - 493
  • [6] Burbankite from Kola Peninsula, Russia
    Gravier, Denis
    Laurs, Brendan M.
    JOURNAL OF GEMMOLOGY, 2024, 39 (03)
  • [7] Diatom assemblages from Holocene sediments of the Kola Peninsula
    O. S. Olyunina
    E. I. Polyakova
    F. A. Romanenko
    Doklady Earth Sciences, 2008, 423 : 1343 - 1347
  • [8] Diatom assemblages from Holocene sediments of the Kola Peninsula
    Olyunina, O. S.
    Polyakova, E. I.
    Romanenko, F. A.
    DOKLADY EARTH SCIENCES, 2008, 423 (02) : 1343 - 1347
  • [9] Postglacial climate and vegetation history, north-central Kola Peninsula, Russia: pollen and diatom records from Lake Yarnyshnoe-3
    Snyder, JA
    Macdonald, GM
    Forman, SL
    Tarasov, GA
    Mode, WN
    BOREAS, 2000, 29 (04) : 261 - 271
  • [10] The Kovdor phlogopite deposit, Kola Peninsula, Russia
    Krasnova, NI
    CANADIAN MINERALOGIST, 2001, 39 (01): : 33 - 44