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Sedimentary Cladocera as indicators of past water-level changes in shallow northern lakes

Published online by Cambridge University Press:  20 January 2017

Liisa Nevalainen ,
Kaarina Sarmaja-Korjonen  and
Tomi P. Luoto
Liisa Nevalainen*
Affiliation:
Institute for Limnology, Austrian Academy of Sciences, Mondseestraße 9, A-5310 Mondsee, Austria
Kaarina Sarmaja-Korjonen
Affiliation:
Department of Geosciences and Geography, P.O. Box 64, FI-00014 University of Helsinki, Finland
Tomi P. Luoto
Affiliation:
Institute for Limnology, Austrian Academy of Sciences, Mondseestraße 9, A-5310 Mondsee, Austria Department of Geosciences and Geography, P.O. Box 64, FI-00014 University of Helsinki, Finland
*
⁎Corresponding author. Fax: + 43 6232 3578.
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Abstract

The usability of subfossil Cladocera assemblages in reconstructing long-term changes in lake level was examined by testing the relationship between Cladocera-based planktonic/littoral (P/L) ratio and water-level inference model in a surface-sediment dataset and in a 2000-yr sediment record in Finland. The relationships between measured and inferred water levels and P/L ratios were significant in the dataset, implying that littoral taxa are primarily deposited in shallow littoral areas, while planktonic cladocerans accumulate abundantly mainly in deepwater locations. The 2000-yr water-level reconstructions based on the water-level inference model and P/L ratio corresponded closely with each other and with a previously available midge-inferred water-level reconstruction from the same core, showing a period of lower water level around AD 300–1000 and suggesting that the methods are valid for paleolimnological and -climatological use.

Keywords

Lake levelLate HoloceneSubfossil CladoceraPlanktonic/littoral ratioTransfer functionPaleoclimatology
Type
Research Article
Information
Quaternary Research , Volume 75 , Issue 3 , May 2011 , pp. 430 - 437
Copyright
University of Washington

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References

Alhonen, P. On the significance of the planktonic/littoral ratio in the cladoceran stratigraphy of lake sediments. Commentationes Biologicae 35, (1970). 1–9.Google Scholar
Alhonen, P. The paleolimnology of four lakes in south-western Finland. Academiae Scientiarum Fennicae Series A III. Geologica-Geographica 105, (1970). 1–39.Google Scholar
Alhonen, P. The Flandrian development of the pond Hyrynlampi, southern Finland, with special reference to the pollen and cladoceran stratigraphy. Acta Botanica Fennica 95, (1971). 1–19.Google Scholar
Alhonen, P. Gallträsket: the geological development and paleolimnology of a small polluted lake in Southern Finland. Commentationes Biologicae 57, (1972). 1–34.Google Scholar
Amsinck, S.L., Jeppesen, E., and Landkildehus, F. Relationship between environmental variables and zooplankton subfossils in the surface sediments of 36 shallow coastal brackish lakes with special emphasis on the role of fish. Journal of Paleolimnology 33, (2005). 39–51.Google Scholar
Amsinck, S.L., Strzelczak, A., Bjerring, R., Landkildehus, F., Lauridsen, T.L., Christofferssen, K., and Jeppesen, E. Lake depth rather than planktivory determines cladoceran community structure in Faroese lakes—evidence from contemporary data and sediments. Freshwater Biology 51, (2006). 2124–2142.Google Scholar
Benestad, R.E. Tentative probabilistic temperature scenarios for northern Europe. Tellus. Series A: Dynamic Meteorology and Oceanography 56, (2004). 89–101.Google Scholar
Christensen, J.H., Räinsänen, J., Iversen, T., Bjørge, D., Christensen, O.B., and Rummukainen, M. A synthesis of regional climate change simulations—a Scandinavian perspective. Geophysical Research Letters 28, (2001). 1003–1006.Google Scholar
Davidson, T.A., Sayer, C.D., Perrow, M.R., Bramm, M., and Jeppesen, E. Are the controls of species composition similar for contemporary and sub-fossil cladoceran assemblages? A study of 39 shallow lakes of contrasting trophic status. Journal of Paleolimnology 38, (2007). 117–134.Google Scholar
Davidson, T.A., Sayer, C.D., Perrow, M.R., Bramm, M., and Jeppesen, E. The simultaneous inference of zooplanktivorous fish and macrophyte density from sub-fossil cladoceran assemblages: a multivariate regression tree approach. Freshwater Biology 55, (2010). 546–564.Google Scholar
Davidson, T.A., Sayer, C.D., Langdon, P.G., Burgess, A., and Jackson, M. Inferring past zooplanktivorous fish and macrophyte density in a shallow lake: application of a new regression tree model. Freshwater Biology 55, (2010). 584–599.Google Scholar
DeSellas, A.M., Paterson, A.M., Sweetman, J.N., and Smol, J.P. Cladocera assemblages from the surface sediments of south-central Ontario (Canada) lakes and their relationships to measured environmental variables, 2008. Hydrobiologia 600, (2008). 105–119.Google Scholar
Frey, D.G. The non-cosmopolitanism of chydorid Cladocera: implications for biogeography and evolution. Gore, R.H., and Heck, K.L. Crustacean Biogeography. (1986). Balkema, Rotterdam. 237–356.Google Scholar
Frey, D.G. Littoral and offshore communities of diatoms, cladocerans and dipterous larvae, and their interpretation in paleolimnology. Journal of Paleolimnology 1, (1988). 179–191.Google Scholar
Heikkilä, M., Edwards, T., Seppä, H., and Sonninen, E. Sediment isotope tracers from Lake Saarikko, Finland, and implications for Holocene hydroclimatology. Quaternary Science Reviews 29, (2010). 2146–2160.Google Scholar
Helama, S., Meriläinen, J., and Tuomenvirta, H. Multicentennial megadrought in northern Europe coincided with a global El Niño–Southern Oscillation drought pattern during the Medieval Climate Anomaly. Geology 37, (2009). 175–178.Google Scholar
Hill, M.O. Diversity and evenness: a unifying notation and its consequences. Ecology 54, (1973). 427–432.Google Scholar
Hofmann, W. Cladocerans and chironomids as indicators of lake level changes in north temperate lakes. Journal of Paleolimnology 19, (1998). 55–62.Google Scholar
Hurrell, J.W. Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitation. Science 269, (1995). 676–679.Google Scholar
Hyvärinen, H., and Alhonen, P. Holocene lake-level changes in the Fennoscandian tree-line region, western Finnish Lapland: diatom and cladoceran evidence. Holocene 4, (1994). 251–258.Google Scholar
Jeppesen, E., Jensen, J.P., Lauridsen, T.I., Amsinck, S.L., Christoffersen, K., Søndergaard, M., and Mitchell, S. Sub-fossils of cladocerans in the surface sediments of 135 lakes as proxies for community structure of zooplankton, fish abundance and lake temperature. Hydrobiologia 491, (2003). 321–330.Google Scholar
Juggins, S., (2007). Program C2 data analysis. Version 1.5.0. University of Newcastle, UK.Google Scholar
Jylhä, K., Tuomenvirta, H., and Ruosteenoja, K. Climate change projections for Finland during the 21st century. Boreal Environment Research 9, (2004). 127–152.Google Scholar
Kansanen, P.H., Jaakkola, T., Kulmala, S., and Suutarinen, R. Sedimentation and distribution of gamma emitting radionuclides in bottom sediments of southern Lake Päijänne, Finland, after the Chernobyl accident. Hydrobiologia 222, (1991). 121–140.Google Scholar
Kattel, G.R., Battarbee, R.W., Mackay, A., and Birks, H.J.B. Are cladoceran fossils in lake sediment samples a biased reflection of the communities from which they are derived?. Journal of Paleolimnology 38, (2007). 157–181.Google Scholar
Kattel, G.R., Battarbee, R.W., Mackay, A., and Birks, H.J.B. Recent ecological change in a remote Scottish mountain loch: an evaluation of a Cladocera-based temperature transfer-function. Palaeogeography, Palaeoclimatology, Palaeoecology 259, (2008). 51–76.Google Scholar
Korhola, A. Distribution patterns of Cladocera in subarctic Fennoscandian lakes and their potential in environmental reconstruction. Ecography 22, (1999). 357–373.Google Scholar
Korhola, A., Olander, H., and Blom, T. Cladoceran and chironomid assemblages as quantitative indicators of water depth in subarctic Fennoscandian lakes. Journal of Paleolimnology 24, (2000). 43–53.Google Scholar
Korhola, A., Tikkanen, M., and Weckström, J. Quantification of Holocene lake-level changes in Finnish Lapland using a cladoceara–lake depth model. Journal of Paleolimnology 34, (2005). 175–190.Google Scholar
Kurek, J., and Cwynar, L.C. The potential of site-specific and local chironomid-based inference models for reconstructing lake levels. Journal of Paleolimnology 42, (2009). 37–50.Google Scholar
Lamb, P., and Peppler, R.A. North Atlantic Oscillation: concept and an application. Bulletin of the American Meteorological Society 68, (1987). 1218–1225.Google Scholar
Lotter, A.F., Birks, H.J.B., Hofmann, W., and Marchetto, A. Modern diatom, cladocera, chironomid, and chrysophyte cyst assemblages as quantitative indicators for the reconstruction of past environmental conditions in the Alps: I. Climate. Journal of Paleolimnology 18, (1997). 395–420.Google Scholar
Luoto, T.P. A Finnish chironomid- and chaoborid-based inference model for reconstructing past lake levels. Quaternary Science Reviews 28, (2009). 1481–1489.CrossRefGoogle Scholar
Luoto, T.P. Hydrological change in lakes inferred from midge assemblages through use of an intralake calibration set. Ecological Monographs 80, (2010). 303–329.Google Scholar
Luoto, T.P. Spatial and temporal variability in midge (nematocera) assemblages in shallow Finnish lakes (60–70°N): community-based modelling of past environmental change. Publications of the Department of Geosciences and Geography A4. (2010). 62 pp.Google Scholar
Luoto, T.P., Kultti, S., Nevalainen, L., and Sarmaja-Korjonen, K. Temperature and effective moisture variability in southern Finland during the Holocene quantified with midge-based calibration models. Journal of Quaternary Science 25, (2010). 1317–1326.Google Scholar
Manca, M., and Comoli, P. Temporal variations of fossils Cladocera in the sediments of Lake Orta (N. Italy) over the last 400 years. Journal of Paleolimnology 14, (1995). 113–122.Google Scholar
Nevalainen, L., Luoto, T., and Sarmaja-Korjonen, K. Late Holocene water-level changes in Lake Iso Lehmälampi, southern Finland, reflected in subfossil cladocerans and chironomids. Studia Quaternaria 25, (2008). 33–42.Google Scholar
Sarmaja-Korjonen, K. Correlation of fluctuations in cladoceran planktonic:littoral ratio between three cores from a small lake in southern Finland: Holocene water-level changes. Holocene 11, (2001). 53–63.Google Scholar
Sarmaja-Korjonen, K., and Alhonen, P. Cladoceran and diatom evidence of lake-level fluctuations from a Finnish lake and the effect of aquatic moss layers on microfossil assemblages. Journal of Paleolimnology 22, (1999). 277–290.Google Scholar
Sarmaja-Korjonen, K., and Hyvärinen, H. Cladoceran and diatom stratigraphy of calcareous lake sediments from Kuusamo, NE Finland. Indications of Holocene lake-level changes. Fennia 177, (1999). 55–70.Google Scholar
Seppä, H., and Birks, H.J.B. July mean temperature and annual precipitation trends during the Holocene in the Fennoscandian tree-line area: pollen-based climate reconstructions. Holocene 11, (2001). 527–539.Google Scholar
Seppä, H., and Hammarlund, D. Pollen-stratigraphical evidence of Holocene hydrological change in the Fennoscandia supported by independent isotopic data. Journal of Paleolimnology 24, (2000). 69–79.Google Scholar
Sweetman, J., and Smol, J. Patterns in the distribution of cladocerans (Crustacea, Branchiopoda) in lakes across a north–south transect in Alaska, USA. Hydrobiologia 553, (2006). 277–291.Google Scholar
Szeroczyńska, K., and Sarmaja-Korjonen, K. Atlas of Subfossil Cladocera from Central and Northern Europe. (2007). Friends of the Lower Vistula Society, Świecie.Google Scholar
ter Braak, C.J.F. Program CANOCO, Version 4.52. Biometris—Quantitative Methods in the Life and Earth Sciences. (2003). Plant Research International, Wageningen University and Research Centre, the Netherlands.Google Scholar
ter Braak, C.J.F., and Juggins, S. Weighted averaging partial least squares regression (WA-PLS): an important method for reconstructing environmental variables from species assemblages. Hydrobiologia 269, 270 (1993). 485–502.Google Scholar
Yu, G., and Harrision, S.P. Holocene changes in atmospheric circulation patterns as shown by lake status in northern Europe. Boreas 24, (1995). 260–268.Google Scholar