Large shallow lake response to anthropogenic stressors and climate change: Missing macroinvertebrate recovery after oligotrophication (Lake Balaton, East-Central Europe)

被引:3
作者
Magyari, E. K. [1 ,2 ]
Szabo, Z. [1 ]
Falus, Gy. [3 ]
Mora, A. [4 ]
Szalai, Z. [1 ,5 ]
Hamerlik, L. [6 ,7 ]
Toth, M.
Farkasi, A. [8 ]
Pomogyi, P. [9 ]
Somogyi, B.
Voros, L.
Korponai, J. [1 ]
机构
[1] Eotvos Lorand Univ, Dept Environm & Landscape Geog, Pazmany Peter Str 1-C, H-1117 Budapest, Hungary
[2] HUN REN MTM ELTE Res Grp Palaeontol, Pazmany Peter Str 1-C, H-1117 Budapest, Hungary
[3] Min & Geol Survey Hungary, Columbus Str 17-23, H-1145 Budapest, Hungary
[4] Univ Pecs, Dept Hydrobiol, Ifjusag Utja 6, H-7624 Pecs, Hungary
[5] Res Ctr Astron & Earth Sci, Geog Inst, Budaors Ut 45, H-1112 Budapest, Hungary
[6] Matej Bel Univ, Fac Nat Sci, Tajovskeho 40, Banska Bystrica 97401, Slovakia
[7] Slovak Acad Sci, Inst Zool, Dubravska Cesta 9, Bratislava, Slovakia
[8] Balaton Limnol Res Inst, Klebelsberg Kuno Utca 3, H-8237 Tihany, Hungary
[9] HUN REN ATOMK, Bem Ter 18-c, H-4026 Debrecen, Hungary
基金
芬兰科学院;
关键词
Chironomid paleoecology; Lake Balaton; Pollen; Geochemistry; Restoration targets; TOP-DOWN CONTROL; QUANTITATIVE RECONSTRUCTION; TEMPERATURE RECONSTRUCTION; CHIRONOMID COMMUNITIES; COMBINING LIMNOLOGY; PHOSPHORUS RELEASE; NUTRIENT STATE; KIS-BALATON; LONG-TERM; PATTERNS;
D O I
10.1016/j.scitotenv.2024.174191
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
East-Central Europe 's largest shallow lake, Balaton, experienced strong eutrophication in the 1970 -80s, followed by water quality improvement and oligotrophication by 2010 CE. Recently however, repeated cyanobacterial blooms occurred and warned that internal P-recycling can act similarly to external P load, therefore we need a better understanding of past water level (WL) and trophic changes in the lake. In this study we discuss the last 500-yr trophic, WL and habitat changes of the lake using paleoecological (chironomids, pollen) and geochemical (sediment chlorophyll, TOC, TS, TN, C/H ratio, major and trace element) methods. We demonstrate that the most intensive and irreversible change in the macroinvertebrate fauna occurred during the period of economic boom between the First and Second World War (similar to 1925 -1940 CE), when large-scale built-in and leisure use of the lake has intensified. At that time, the Procladius-Microchironomus-Stempellina dominated community transformed to Procladius- Chironomus plumosus- type- Microchironomus community that coincided with land use changes, intensified erosion and water-level regulation in the lake with the maintenance of year-round high WL. This was followed by the impoverishment and population size decrease of the chironomid fauna and Procladius dominance since 1940 CE, without any recovery after 1994 CE despite the ongoing oligotrophication. Accelerated rate of change and turnover of the fauna was connected to an increase in the benthivorous fish biomass and eutrophication. The basin lost almost completely its once characteristic Stempellina species between 1927 and 1940 CE due to trophic level increase and seasonal anoxia in the Szemes Basin. Reference conditions for ecosystem improvement were assigned to 1740 -1900 CE. We conclude that in spite of the ongoing oligotrophication, the re establishment of the Procladius-Microchironomus-Stempellina assemblage is hampered, and requires fish population regulation.
引用
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页数:18
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