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New evidence of warm early-Holocene summers in subarctic Finland based on an enhanced regional chironomid-based temperature calibration model

Published online by Cambridge University Press:  20 January 2017

Tomi P. Luoto ,
Marjut Kaukolehto ,
Jan Weckström ,
Atte Korhola  and
Minna Väliranta
Tomi P. Luoto*
Affiliation:
Division of Geology, Department of Geosciences and Geography, University of Helsinki, P.O. Box 64, 00014, Finland
Marjut Kaukolehto
Affiliation:
Division of Atmospheric Sciences, Department of Physics, University of Helsinki, P.O. Box 48, 00014, Finland
Jan Weckström
Affiliation:
Environmental Change Research Unit (ECRU), Department of Environmental Sciences, University of Helsinki, P.O. Box 65, 00014, Finland
Atte Korhola
Affiliation:
Environmental Change Research Unit (ECRU), Department of Environmental Sciences, University of Helsinki, P.O. Box 65, 00014, Finland
Minna Väliranta
Affiliation:
Environmental Change Research Unit (ECRU), Department of Environmental Sciences, University of Helsinki, P.O. Box 65, 00014, Finland
*
*Corresponding author. E-mail address:[email protected](T.P. Luoto).
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Abstract

Paleoclimate reconstructions based on biological proxies present methodological challenges, especially during non-analog conditions, such as the early Holocene. Here, two chironomid-based training sets from Finland were amalgamated to create a more accurate transfer function of summer air temperature. The aim was to reconstruct Holocene paleoclimate in northernmost Lapland, in an area that has been either too warm or too cold for reliable reconstructions using the original calibration models. The results showed that the combined calibration model had improved performance statistics. The temperature trends inferred from the downcore chironomid record using the original and combined models were very similar. However, there were major changes in their absolute values with the combined model showing greatly improved accuracy. The chironomid-based temperature reconstruction showed significant correlation with the previous pollen-based reconstructions from northwestern Finnish Lapland. However, differences were observed in the temperature trends of the early Holocene, when the chironomid-inferred temperatures rapidly increased, but the pollen-based reconstructions lagged behind suggesting that a cool climate continued for much longer. However, similar to the chironomid record, new plant macrofossil evidence from northwestern Finland also showed warmer-than-present early Holocene temperatures. Therefore, we conclude that the early Holocene was probably warm in northern Lapland.

Keywords

ChironomidaeClimate changeLaplandPaleoclimatologyPaleolimnologyPlant macrofossilsTransfer function
Type
Research Article
Information
Quaternary Research , Volume 81 , Issue 1 , January 2014 , pp. 50 - 62
Copyright
University of Washington

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References

Bigler, C., Grahn, E., Larocque, I., Jeziorski, A., and Hall, R. Holocene environmental change at Lake Njulla (999 m a.s.l.) northern Sweden: a comparison with four small nearby lakes along an altitudinal gradient. Journal of Paleolimnology 29, (2003). 13–29.Google Scholar
Birks, H.J.B. Numerical tools in palaeolimnology: progress, potentialities and problems. Journal of Paleolimnology 20, (1998). 307–332.Google Scholar
Birks, H.H., Jones, V.J., Brooks, S.J., Birks, H.J.B., Telford, R.J., Juggins, S., and Peglar, S.M. From cold to cool in northernmost Norway: Late-glacial and early Holocene multi-proxy environmental and climate reconstructions from Jansvatnet, Hammerfest. Quaternary Science Reviews 33, (2012). 100–120.Google Scholar
Bjune, A.E., Birks, H.J.B., and Seppä, H. Holocene vegetation and climate history on a continental oceanic transect in northern Fennoscandia based on pollen and plant macrofossils. Boreas 33, (2004). 211–223.Google Scholar
Brodersen, K.P., Pedersen, O., Lindegaard, C., and Hamburger, K. Chironomids (Diptera) and oxy-regulatory capacity: an experimental approach to paleolimnological interpretation. Limnology and Oceanography 49, (2004). 1549–1559.Google Scholar
Brodersen, K.P., Pedersen, O., Walker, I.R., and Jensen, M.R. Respiration of midges (Diptera: Chironomidae) in British Columbian lakes: oxy-regulation, temperature and their role as palaeo-indicators. Freshwater Biology 53, (2008). 593–602.Google Scholar
Brooks, S.J. Fossil midges (Diptera: Chironomidae) as palaeoclimatic indicators for the Eurasian region. Quaternary Science Reviews 25, (2006). 1894–1910.Google Scholar
Brooks, S.J., and Birks, H.J.B. Chironomid-inferred air temperatures from Lateglacial and Holocene sites in northwest Europe: progress and problems. Quaternary Science Reviews 20, (2001). 1723–1741.Google Scholar
Brooks, S.J., Langdon, P.G., and Heiri, O. The identification and use of Palaeoarctic Chironomidae larvae in palaeoecology. QRA Technical Guide No. 10. (2007). Quaternary Research Association, London.Google Scholar
Brooks, S.J., Axford, Y., Heiri, O., Langdon, P.E., and Larocque-Tobler, I. Chironomids can be reliable proxies for Holocene temperatures. A comment on Velle et al. (2010). The Holocene 22, (2012). 1495–1500.CrossRefGoogle Scholar
Carter, T.R., Fronzek, S., and Bärlund, I. FINSKEN: a framework for developing consistent global change scenarios for Finland in the 21 st century. Boreal Environment Research 9, (2004). 91–107.Google Scholar
Eggermont, H., and Heiri, O. The chironomid–temperature relationship: expressions in nature and palaeoenvironmental implications. Biological Reviews 87, (2012). 430–456.Google Scholar
Elias, S.A. Insects and climate change. BioScience 41, (1991). 552–559.Google Scholar
Engels, S., Helmens, K.F., Väliranta, M., Brooks, S.J., and Birks, H.J.B. Early Weichselian (MIS-5d and 5c) palaeoenvironmental and palaeoclimatic changes in northern Fennoscandia: a multi-proxy study on the lacustrine record of Sokli (Finland). Boreas 39, (2010). 689–704.Google Scholar
Heikkilä, M., and Seppä, H. A 11,000 yr palaeotemperature reconstruction from the southern boreal zone in Finland. Quaternary Science Reviews 22, (2003). 541–554.Google Scholar
Heiri, O., and Lotter, A.F. How does taxonomic resolution affect chironomid-based temperature reconstruction?. Journal of Paleolimnology 44, (2010). 589–601.Google Scholar
Heiri, O., Ekrem, T., Willasen, E., (2004). Larval head capsules of European Micropsectra, Paratanytarsus and Tanytarsus . (Diptera: Chironomidae: Tanytarsini) (unpublished identification guide).Google Scholar
Heiri, O., Brooks, S.J., Birks, H.J.B., and Lotter, A.F. A 274-lake calibration data-set and inference model for chironomid based summer air temperature reconstruction in Europe. Quaternary Science Reviews 30, (2011). 3445–3456.Google Scholar
Johansson, P., Kujansuu, R., (2005). Quaternary Deposits of Northern Finland — Explanation to the Maps of Quaternary Deposits 1:400 000. Espoo, Geological Survey of Finland.Google Scholar
Juggins, S. Program C2 Data Analysis. Version 1.5.0. (2007). University of Newcastle, UK.Google Scholar
Juggins, S. Quantitative reconstructions in palaeolimnology: new paradigm or sick science?. Quaternary Science Reviews 64, (2013). 20–32.Google Scholar
Kaufman, D.S., Ager, T.A., Anderson, N.J., Anderson, P.M., Andrews, J.T., Bartlein, P.T., Brubaker, L.B., Coats, L.L., Cwynar, L.C., Duvall, M.L., Dyke, A.S., Edwards, M.E., Eisner, W.R., Gajewski, K., Geirsdóttir, A., Hu, F.S., Jennings, A.E., Kaplan, M.R., Kerwin, M.W., Lozhkin, A.V., MacDonald, G.M., Miller, G.H., Mock, C.J., Oswald, W.W., Otto-Bliesner, B.L., Porinchu, D.F., Rühland, K., Smol, J.P., Steig, E.J., and Wolfe, B.B. Erratum to: Holocene thermal maximum in the western Arctic (0–180° W). Quaternary Science Reviews 23, (2004). 2059–2060.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., Weckström, J., Holmström, L., and Erästö, P. A quantitative Holocene climatic record from diatoms in northern Fennoscandia. Quaternary Research 54, (2000). 284–294.Google Scholar
Korhola, A., Vasko, K., Toivonen, H.T.T., and Olander, H. Holocene temperature changes in northern Fennoscandia reconstructed from chironomids using Bayesian modelling. Quaternary Science Reviews 21, (2002). 1841–1860.CrossRefGoogle Scholar
Korhola, A., Weckström, J., and Blom, T. Relationships between lake and land-cover features along latitudinal vegetation ecotones in arctic Fennoscandia. Archiv für Hydrobiologie 139, (2002). 203–235.Google Scholar
Kullman, L. Early Holocene appearance of mountain birch (Betula pubescens ssp. tortuosa) at unprecedented high elevations in the Swedish Scandes: megafossil evidence exposed by recent snow and ice recession. Arctic, Antarctic, and Alpine Research 36, (2004). 172–180.Google Scholar
Kultti, S., Nevalainen, L., Luoto, T.P., and Sarmaja-Korjonen, K. Subfossil chydorid (Cladocera, Chydoridae) ephippia as paleoenvironmental proxies: evidence from boreal and subarctic lakes in Finland. Hydrobiologia 676, (2011). 23–37.Google Scholar
Lampinen, R., and Lahti, T. Kasviatlas 2012. (2013). Botanical Museum, Finnish Museum of Natural History, Helsinki.Google Scholar
Larocque-Tobler, I. Reconstruction temperature at Egelsee, Switzerland, using North American and Swedish chironomid transfer functions: potential and pitfalls. Journal of Paleolimnology 44, (2010). 243–251.Google Scholar
Lehtonen, H. Does global warming threat the existence of Arctic charr, Salvelinus alpinus (Salmonidae), in northern Finland. Italian Journal of Zoology 65, (1998). 471–474.Google Scholar
Luoto, T.P. Subfossil Chironomidae (Insecta: Diptera) along a latitudinal gradient in Finland: development of a new temperature inference model. Journal of Quaternary Science 24, (2009). 150–158.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.Google 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. The relationship between water quality and chironomid distribution in Finland — a new assemblage-based tool for assessments of long-term nutrient dynamics. Ecological Indicators 11, (2011). 255–262.Google Scholar
Luoto, T.P. Spatial uniformity in depth optima of midges: evidence from sedimentary archives of shallow Alpine and boreal lakes. Journal of Limnology 71, (2012). 228–232.Google Scholar
Luoto, T.P., and Raunio, J. A comparison of chironomid-based total phosphorus training sets developed from contemporary pupal exuviae and sedimentary larval head capsules to infer lake trophic history. Fundamental and Applied Limnology 179, (2011). 93–102.CrossRefGoogle Scholar
Luoto, T.P., and Sarmaja-Korjonen, K. Midge-inferred Holocene effective moisture fluctuations in a subarctic lake, northern Lapland. Boreas 40, (2011). 650–659.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
Luoto, T.P., Nevalainen, L., Kauppila, T., Tammelin, M., and Sarmaja-Korjonen, K. Diatom-inferred total phosphorus from dystrophic Lake Arapisto, Finland, in relation to Holocene paleoclimate. Quaternary Research 78, (2012). 248–255.Google Scholar
Massaferro, J., and Brooks, S.J. Response of chironomids to Late Quaternary environmental change in the Taitao Peninsula, southern Chile. Journal of Quaternary Science 17, (2002). 101–111.Google Scholar
Nevalainen, L., Luoto, T.P., Kultti, S., and Sarmaja-Korjonen, K. Do subfossil Cladocera and chydorid ephippia disentangle Holocene climate trends?. The Holocene 22, (2012). 291–299.Google Scholar
Nyman, M., and Korhola, A. Chironomid-based classification of lakes in western Finnish Lapland. Boreal Environment Research 10, (2005). 239–254.Google Scholar
Nyman, M., Korhola, A., and Brooks, S.J. The distribution and diversity of Chironomidae (Insecta: Diptera) in western Finnish Lapland, with special emphasis on shallow lakes. Global Ecology and Biogeography 14, (2005). 137–153.Google Scholar
Nyman, M., Weckström, J., and Korhola, A. Chironomid response to environmental drivers during the Holocene in a shallow treeline lake in northwestern Fennoscandia. The Holocene 18, (2008). 215–227.Google Scholar
Olander, H., Birks, H.J.B., Korhola, A., and Blom, T. An expanded calibration model for inferring lakewater and air temperatures from fossil chironomid assemblages in northern Fennoscandia. The Holocene 9, (1999). 279–294.Google Scholar
R Development Core Team, R: A Language and Environment for Statistical Computing. (2009). R Foundation for Statistical Computing, Vienna.Google Scholar
Renssen, H., Seppä, H., Crosta, X., Goosse, H., and Roche, D.M. Global characterization of the Holocene Thermal Maximum. Quaternary Science Reviews 48, (2012). 7–19.Google Scholar
Rieradevall, M., and Brooks, S.J. An identification guide to subfossil Tanypodinae larvae (Insecta: Diptera: Chironomidae) based on cephalic setation. Journal of Paleolimnology 25, (2001). 81–99.Google Scholar
Salonen, J.S., Seppä, H., Väliranta, M., Jones, V.J., Self, A., Heikkilä, M., Kultti, S., and Yang, H. The Holocene thermal maximum and late-Holocene cooling in the tundra of NE European Russia. Quaternary Research 75, (2011). 501–511.Google Scholar
Salonen, J.S., Helmens, K.F., Seppä, H., and Birks, H.J.B. Pollen-based palaeoclimate reconstructions over long glacial–interglacial timescales: methodological tests based on the Holocene and MIS 5d–c deposits at Sokli, northern Finland. Journal of Quaternary Science 28, (2013). 271–282.Google Scholar
Sarmaja-Korjonen, K., Nyman, M., Kultti, K., and Väliranta, M. Palaeolimnological development of Lake Njargajavri, northern Finnish Lapland, in a changing Holocene climate and environment. Journal of Paleolimnology 35, (2006). 65–81.Google Scholar
Schnell, Ø.A., Rieradevall, M., Granados, I., and Hanssen, O. A chironomid taxa coding system for use in ecological and palaeoecological databases. NIVA Report SNO. (1999). 3710–3797.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. The Holocene 11, (2001). 527–537.Google Scholar
Seppä, H., and Birks, H.J.B. Holocene climate reconstructions from the Fennoscandian tree-line area based on pollen data from Toskaljavri. Quaternary Research 57, (2002). 191–199.Google Scholar
Seppä, H., and Weckström, J. Holocene vegetational and limnological changes in the Fennoscandian tree-line area as documented by pollen and diatom records from Lake Tsuolbmajavri, Finland. Ecoscience 6, (1999). 621–635.Google Scholar
Seppä, H., Nyman, M., Korhola, A., and Weckström, J. Changes of treelines and alpine vegetation in relation to post-glacial climate dynamics in northern Fennoscandia based on pollen and chironomid records. Journal of Quaternary Science 17, (2002). 287–301.Google Scholar
Shemesh, A., Rosqvist, G., Rietti-Shati, M., Rubensdotter, L., Bigler, C., Yam, R., and Karlén, W. Holocene climatic change in Swedish Lapland inferred from an oxygen-isotope record of lacustrine biogenic silica. The Holocene 11, (2001). 447–454.Google Scholar
Siitonen, S., Väliranta, M., Weckström, J., Juutinen, S., and Korhola, A. Comparison of Cladocera-based water-depth reconstruction against other types of proxy data in Finnish Lapland. Hydrobiologia 676, (2011). 155–172.CrossRefGoogle Scholar
Smol, J.P. Pollution of Lakes and Rivers: A Paleoenvironmental Perspective. 2nd ed. (2008). Blackwell Pub., Malden, MA.Google Scholar
Solanki, S.K., Usoskin, I.G., Kromer, B., Schüssler, M., and Beer, J. An unusually active Sun during recent decades compared to the previous 11,000 years. Nature 431, (2004). 1084–1087.Google Scholar
Solovieva, N., Tarasov, P.E., and MacDonald, G. Quantitative reconstruction of Holocene climate from the Chuna Lake pollen record, northwest Russia. The Holocene 15, (2005). 141–148.Google Scholar
Szeroczyńska, K., Tatur, A., Weckström, J., Gąsiorowski, M., Noryśkiewicz, A.M., and Sienkiewicz, E. Holocene environmental history in northwest Finnish Lapland reflected in the multi-proxy record of a small subarctic lake. Journal of Paleolimnology 38, (2007). 25–47.Google Scholar
Telford, R.J., and Birks, H.J.B. A novel method for assessing the statistical significance of quantitative reconstructions inferred from biotic assemblages. Quaternary Science Reviews 30, (2011). 1272–1278.Google Scholar
ter Braak, C.J.F., and Juggins, S. Weighted averaging partial least squares regression (WA-PLS): an improved method for reconstructing environmental variables from species assemblages. Hydrobiologia 269, 270 (1993). 485–502.Google Scholar
ter Braak, C.J.F., and Šmilauer, P. CANOCO — Software for Multivariate Data Exploration, Testing, and Summarization (Version 5.00). (2012). Biometris, Plant Research International, the Netherlands/Czech Republic.Google Scholar
Tiljander, M., Saarnisto, M., Ojala, A.E.K., and Saarinen, T. A 3000-year palaeoenvironmental record from annually laminated sediment of Lake Korttajärvi, central Finland. Boreas 26, (2003). 566–577.Google Scholar
Tolonen, K.T., Hämäläinen, H., Holopainen, I.J., and Karjalainen, J. Influences of habitat type and environmental variables on littoral macroinvertebrate communities in a large lake system. Archiv für Hydrobiologie 152, (2001). 39–67.Google Scholar
Väliranta, M. Long-term changes in aquatic plant species composition in North-eastern European Russia and Finnish Lapland, as evidenced by plant macrofossil analysis. Aquatic Botany 85, (2006). 224–232.Google Scholar
Väliranta, M., Kultti, S., Nyman, M., and Sarmaja-Korjonen, K. Holocene development of aquatic vegetation in a shallow Lake Njargajavri, Finnish Lapland with evidence of water level fluctuations and drying. Journal of Paleolimnology 34, (2005). 203–215.Google Scholar
Väliranta, M., Birks, H.H., Helmens, K., Engels, S., and Piirainen, M. Early Weichselian interstadial (MIS 5c) summer temperatures were higher than today in northern Fennoscandia. Quaternary Science Reviews 28, (2009). 777–782.CrossRefGoogle Scholar
Väliranta, M., Kaakinen, A., Kuhry, P., Kultti, S., Salonen, S., and Seppä, H. Scattered late-glacial and early-Holocene tree populations as dispersal nuclei for forest development in NE European Russia. Journal of Biogeography 38, (2011). 922–932.CrossRefGoogle Scholar
Väliranta, M., Weckström, J., Siitonen, S., Seppä, H., Alkio, J., Juutinen, S., and Tuittila, E.-S. Holocene aquatic ecosystem change in the boreal vegetation zone of northern Finland. Journal of Paleolimnology 45, (2011). 339–352.Google Scholar
Velle, G., Brodersen, K.P., Birks, H.J.B., and Willassen, E. Midges as quantitative temperature indicator species: lessons for palaeoecology. The Holocene 20, (2010). 989–1002.Google Scholar
Velle, G., Brodersen, K.P., Birks, H.J.B., and Willassen, E. Inconsistent results should not be overlooked: a reply to Brooks et al. (2012). The Holocene 22, (2012). 1501–1508.Google Scholar
Venäläinen, A., Tuomenvirta, H., Pirinen, P., and Drebs, A. A Basic Climate Data Set 1961–2000 — Description and Illustrations. (2005). Finnish Meteorological Institute, 5 (Reports) Google Scholar
Vesajoki, H., and Holopainen, J. The early temperature records of Turku (Åbo), south-west Finland 1749–1800. Paläoklimaforschung — Palaeoclimate Research 23, (1998). 151–161.Google Scholar
Walker, I.R., and Cwynar, L.C. Midges and palaeotemperature reconstruction—the North American experience. Quaternary Science Reviews 25, (2006). 1911–1925.Google Scholar
Wanner, H., Beer, J., Butikofer, J., Crowley, T.J., Cubasch, U., Fluckiger, J., Goosse, H., Grosjean, M., Joos, F., Kaplan, J.O., Kuttel, M., Muller, S.A., Prentice, I.C., Solomina, O., Stocker, T.F., Tarasov, P., Wagner, M., and Widmann, M. Mid- to Late Holocene climate change: an overview. Quaternary Science Reviews 27, (2008). 1791–1828.Google Scholar
Weckström, J., and Korhola, A. Patterns in the distribution, composition and diversity of diatom assemblages in relation to ecoclimatic factors in Arctic Lapland. Journal of Biogeography 28, (2001). 31–45.Google Scholar
Wiederholm, T. Chironomidae of the Holarctic Region: Keys and Diagnoses. Part 1. Larvae. Entomologica Scandinavica Supplement (1983). Borgströms Tryckeri AB, Motala, Sweden.Google Scholar