Resilience, rapid transitions and regime shifts: Fingerprinting the responses of Lake Żabińskie (NE Poland) to climate variability and human disturbance since AD 1000
Abstract
Rapid ecosystem transitions and adverse effects on ecosystem services as responses to combined climate and human impacts are of major concern. Yet few long-term (i.e. >60 years) quantitative observational time series exist, particularly for ecosystems that have a long history of human intervention. Here, we combine three major environmental pressures (land use, nutrients and erosion) with quantitative summer and winter climate reconstructions and climate model simulations to explore the system dynamics, resilience and the role of disturbance regimes in varved eutrophic Lake Żabińskie (NE Poland) since AD 1000. The comparison between these independent sources of information allows us to establish the coherence and points of disagreements between such data sets. We find that climate reconstructions capture noticeably natural forced climate variability, while internal variability is the dominant source of variability during most parts of the last millennium at the regional scale, precisely at which climate models seem to underestimate forced variability. Using different multivariate analyses and change point detection techniques, we identify ecosystem changes through time and shifts between rather stable states and highly variable ones. Prior to AD 1600, the lake ecosystem was characterised by high stability and resilience against observed natural climate variability. During this period, the anthropogenic fingerprint was small; the lake ecosystem was buffered against the combined human and natural disturbance. In contrast, lake–ecosystem conditions started to fluctuate across a broad range of states after AD 1600. The period AD 1745–1886 represents the phase with the strongest human disturbance of the catchment–lake ecosystem. During that time, the range of natural climate variability did not increase. Analyses of the frequency of change points in the multi-proxy data set suggest that the last 400 years were highly variable and increased vulnerability of the ecosystem to the anthropogenic disturbances. This led to significant rapid ecosystem transformations.
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References
Amann B, Lobsiger S, Fischer D, et al. (2014) Spring temperature variability and eutrophication history inferred from sedimentary pigments in the varved sediments of Lake Żabińskie, north-eastern Poland, AD 1907–2008. Global and Planetary Change 123: 86–96.
Anderson NJ (1993) Natural versus anthropogenic charge in lakes: The role of the sediment record. Trends in Ecology & Evolution 8: 356–361.
Anderson NJ, Odgaard BV, Segerström U, et al. (1996) Climate-lake interactions recorded in varved sediments from a Swedish boreal forest lake. Global Change Biology 2: 399–403.
Battarbee RW (1986) Diatom analysis. In: Berglund BE (ed.) Handbook of Holocene Palaeoecology and Palaeohydrology. New-York: Wiley-Interscience, pp. 527–570.
Berglund BE, Ralska-Jasiewiczowa M (1986) Pollen analysis and pollen diagrams. In: Berglund BE (ed.) Handbook of Holocene Palaeoecology and Palaeohydrology. New York: Wiley-Interscience, pp. 455–484.
Bonk A, Tylmann W, Amann B, et al. (2015a) Modern limnology and varve-formation processes in lake Żabińskie, northeastern Poland: Comprehensive process studies as a key to understand the sediment record. Journal of Limnology 74: 358–370.
Bonk A, Tylmann W, Goslar T, et al. (2015b) Comparing varve counting and 14C-AMS chronologies in the sediments of Lake Żabińskie, northeastern Poland: Implications for accurate 14C dating of lake sediments. Geochronometria 42: 159–171.
Brown A, Pluskowski A (2011) Detecting the environmental impact of the Baltic Crusades on a late-medieval (13th–15th century) frontier landscape: Palynological analysis from Malbork Castle and hinterland, Northern Poland. Journal of Archaeological Science 38: 1957–1966.
Conley DJ, Schelske CL (2001) Biogenic silica. In: Smol JP, Birks HJB, Last WM, et al. (eds) Tracking Environmental Change using Lake Sediments: Terrestrial, Algal, and Siliceous Indicators. Kluwer Academic Press, pp. 281–293.
Crowley TJ (2000) Causes of climate change over the past 1000 years. Science 289: 270–277.
Cwynar LC, Rees ABH, Pedersen CR, et al. (2012) Depth distribution of chironomids and an evaluation of site-specific and regional lake-depth inference models: A good model gone bad? Journal of Paleolimnology 48: 517–533.
D’Anjou RM, Bradley RS, Balascio NL, et al. (2012) Climate impacts on human settlement and agricultural activities in northern Norway revealed through sediment biogeochemistry. Proceedings of the National Academy of Sciences of the United States of America 109: 20332–20337.
Dean WE, Gorham E (1998) Magnitude and significance of carbon burial in lakes, reservoirs, and peatlands. Geology 26: 535–538.
Dean WE, Megard RO (1993) Environment of deposition of CaCO3 in Elk Lake, Minnesota. Geological Society of America Special Papers 276: 97–114.
Dearing JA, Zolitschka B (1999) System dynamics and environmental change: An exploratory study of Holocene lake sediments at Holzmaar, Germany. The Holocene 9: 531–540.
Dearing JA, Battarbee RW, Dikau R, et al. (2006) Human–environment interactions: Learning from the past. Regional Environmental Change 6: 1–16.
Filipkowski T (1983) Dzieje Warmii i Mazur w zarysie. Od 1871 do 1975 roku [History of Warmia and Mazuria. From 1871 to 1975]. Warszawa: Państwowe Wydawn. Naukowe.
Fritz S (2008) Deciphering climatic history from lake sediments. Journal of Paleolimnology 39: 5–16.
Gałka M, Miotk-Szpiganowicz G, Marczewska M, et al. (2014a) Palaeoenvironmental changes in Central Europe (NE Poland) during the last 6200 years reconstructed from a high-resolution multi-proxy peat archive. The Holocene 25: 421–434.
Gałka M, Tobolski K, Górska A, et al. (2014b) Disentangling the drivers for the development of a Baltic bog during the Little Ice Age in northern Poland. Quaternary International 328: 323–337.
Gałka M, Tobolski K, Zawisza E, et al. (2014c) Postglacial history of vegetation, human activity and lake-level changes at Jezioro Linówek in northeast Poland, based on multi-proxy data. Vegetation History and Archaeobotany 23: 123–152.
Gómez-Navarro J, Bothe O, Wagner S, et al. (2015) A regional climate palaeosimulation for Europe in the period 1501–1990 – Part 2: Comparison with gridded reconstructions. Climate of the Past 11: 1077–1095.
Gómez-Navarro J, Montávez J, Wagner S, et al. (2013) A regional climate palaeosimulation for Europe in the period 1500–1990 – Part 1: Model validation. Climate of the Past 9: 1667–1682.
Goslar T, Ralska-Jasiewiczowa M, van Geel B, et al. (1999) Anthropogenic changes in the sediment composition of Lake Gościąż (central Poland), during the last 330 yrs. Journal of Paleolimnology 22: 171–185.
Hall RI, Smol JP (1999) Diatoms as indicators of lake eutrophication. In: Stoermer EF, Smol JP (eds) The Diatoms: Applications for the Environmental and Earth Sciences. Cambridge: Cambridge University Press.
Hausmann S, Lotter AF, van Leeuwen JFN, et al. (2002) Interactions of climate and land use documented in the varved sediments of Seebergsee in the Swiss Alps. The Holocene 12: 279–289.
Heiri O, Lotter AF, Lemcke G (2001) Loss on ignition as a method for estimating organic and carbonate content in sediments: Reproducibility and comparability of results. Journal of Paleolimnology 25: 101–110.
Hernández-Almeida I, Grosjean M, Przybylak R, et al. (2015a) A chrysophyte-based quantitative reconstruction of winter severity from varved lake sediments in NE Poland during the past millennium and its relationship to natural climate variability. Quaternary Science Reviews 122: 74–88.
Hernández-Almeida I, Grosjean M, Tylmann W, et al. (2015b) Chrysophyte cyst-inferred variability of warm season lake water chemistry and climate in northern Poland: Training set and downcore reconstruction. Journal of Paleolimnology 53: 123–138.
Hodell DA, Schelske CL, Fahnenstiel GL, et al. (1998) Biologically induced calcite and its isotopic composition in Lake Ontario. Limnology and Oceanography 43: 187–199.
Intergovernmental Panel on Climate Change (IPCC) (2014) Climate Change 2013: The Physical Science Basis – Working Group I Contribution to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press.
Jansen E, Overpeck J, Briffa KR, et al. (2007) Paleoclimate. In: Solomon S, Qin D, Manning M, et al. (eds) Climate Change 2007: The Physical Science Basis – Contribution of Working Group I to the Fourth Assessment – Report of the IPCC. New York: Cambridge University Press, 996 pp.
Jenny J-P, Francus P, Normandeau A, et al. (2016) Global spread of hypoxia in freshwater ecosystems during the last three centuries is caused by rising local human pressure. Global Change Biology 22: 1481–1489.
Juggins S (2009) Rioja: An R package for the analysis of Quaternary science data. Available at: https://cran.r-project.org/web/packages/rioja/index.html.
Kamenik C, Schmidt R, Koinig K, et al. (2001) The chrysophyte stomatocyst composition in a high alpine lake (Gossenkollesee, Tyrol, Austria) in relation to seasonality, temperature and land-use. Nova Hedwigia 122: 1–22.
Kienel U, Vos H, Dulski P, et al. (2013) Modification of climate signals by human activities recorded in varved sediments (AD 1608–1942) of Lake Holzmaar (Germany). Journal of Paleolimnology 50: 561–575.
Killick R, Eckley I (2014) changepoint: An R package for changepoint analysis. Journal of Statistical Software 58: 1–19.
Koinig KA, Shotyk W, Lotter AF, et al. (2003) 9000 years of geochemical evolution of lithogenic major and trace elements in the sediment of an alpine lake – The role of climate, vegetation, and land-use history. Journal of Paleolimnology 30: 307–320.
Lamentowicz M, Cedro A, Gałka M, et al. (2008a) Last millennium palaeoenvironmental changes from a Baltic bog (Poland) inferred from stable isotopes, pollen, plant macrofossils and testate amoebae. Palaeogeography, Palaeoclimatology, Palaeoecology 265: 93–106.
Lamentowicz M, Gałka M, Lamentowicz Ł, et al. (2015) Reconstructing climate change and ombrotrophic bog development during the last 4000 years in northern Poland using biotic proxies, stable isotopes and trait-based approach. Palaeogeography, Palaeoclimatology, Palaeoecology 418: 261–277.
Lamentowicz M, Gałka M, Milecka K, et al. (2013) A 1300-year multi-proxy, high-resolution record from a rich fen in northern Poland: Reconstructing hydrology, land use and climate change. Journal of Quaternary Science 28: 582–594.
Lamentowicz M, Gałka M, Pawlyta J, et al. (2011) Climate change and human impact in the southern Baltic during the last millennium reconstructed from an ombrotrophic bog archive. Studia Quaternaria 28: 3–16.
Lamentowicz M, Milecka K, Gałka M, et al. (2009) Climate and human induced hydrological change since AD 800 in an ombrotrophic mire in Pomerania (N Poland) tracked by testate amoebae, macro-fossils, pollen and tree rings of pine. Boreas 38: 214–229.
Lamentowicz M, Obremska M, Mitchell EAD (2008b) Autogenic succession, land-use change, and climatic influences on the Holocene development of a kettle-hole mire in Northern Poland. Review of Palaeobotany and Palynology 151: 21–40.
Larocque I, Hall R, Grahn E (2001) Chironomids as indicators of climate change: A 100-lake training set from a subarctic region of northern Sweden (Lapland). Journal of Paleolimnology 26: 307–322.
Larocque-Tobler I, Filipiak J, Tylmann W, et al. (2015) Comparison between chironomid-inferred mean-August temperature from varved Lake Żabińskie (Poland) and instrumental data since 1896 AD. Quaternary Science Reviews 111: 35–50.
Larocque-Tobler I, Filipiak J, Tylmann W, et al. (2016) Corrigendum to ‘Comparison between chironomid-inferred mean-August temperature from varved Lake Żabińskie (Poland) and instrumental data since 1896 AD’. Quaternary Science Reviews 140: 163–167.
Leavitt PR, Fritz SC, Anderson N, et al. (2009) Paleolimnological evidence of the effects on lakes of energy and mass transfer from climate and humans. Limnology and Oceanography 54: 2330–2348.
Leng MJ, Roberts N, Reed JM, et al. (1999) Late Quaternary palaeohydrology of the Konya Basin, Turkey, based on isotope studies of modern hydrology and lacustrine carbonates. Journal of Paleolimnology 22: 187–204.
Lindegren M, Dakos V, Gröger JP, et al. (2012) Early detection of ecosystem regime shifts: A multiple method evaluation for management application. PLoS ONE 7: E38410.
Lorenc H (2005) Atlas klimatu Polski [Climatic Atlas of Poland]. Warszawa: Instytut Meteorologii i Gospodarki Wodnej.
Lotter AF (2001) The palaeolimnology of Soppensee (Central Switzerland), as evidenced by diatom, pollen, and fossil-pigment analyses. Journal of Paleolimnology 25: 65–79.
Lotter A, Birks HJ, Hofmann W, et al. (1997) 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: 395–420.
Luterbacher J, Dietrich D, Xoplaki E, et al. (2004) European seasonal and annual temperature variability, trends, and extremes since 1500. Science 303: 1499–1503.
Luterbacher J, Xoplaki E, Küttel M, et al. (2010) Climate change in Poland in the past centuries and its relationship to European climate: Evidence from reconstructions and coupled climate models. In: Przybylak R, Majorowicz J, Brázdil R, et al. (eds) The Polish Climate in the European Context: An Historical Overview. Berlin: Springer, pp. 3–39.
McCrea JM (1950) On the isotopic chemistry of carbonates and a paleotemperature scale. The Journal of Chemical Physics 18: 849–857.
McKenzie J (1985) Carbon isotopes and productivity in the lacustrine and marine environment. In: Stumm W (ed.) Chemical Processes in Lakes. New York: Wiley, pp. 99–118.
Madeja J (2013) Vegetation changes and human activity around Lake Łańskie (Olsztyn Lake District, NE Poland) from the mid-Holocene, based on palynological study. Acta Palaeobotanica 53: 235–262.
Makohonienko M, Gaillard M-J, Tobolski K (1998) Modern pollen/land-use relationships in ancient cultural landscapes of north-western Poland, with an emphasis on mowing, grazing, and crop cultivation. In: Gaillard M-J, Berglund BE (eds) Quantification of Land Surfaces Cleared of Forests during the Holocene – Modern Pollen/Vegetation/Landscape Relationships as an Aid to the Interpretation of Fossil Pollen Sata. Stuttgart: Gustav Fischer Verlag, pp. 85–98.
Marcisz K, Tinner W, Colombaroli D, et al. (2015) Long-term hydrological dynamics and fire history over the last 2000 years in CE Europe reconstructed from a high-resolution peat archive. Quaternary Science Reviews 112: 138–152.
May RM (1977) Thresholds and breakpoints in ecosystems with a multiplicity of stable states. Nature 269: 471–477.
Messerli B, Grosjean M, Hofer T, et al. (2000) From nature-dominated to human-dominated environmental changes. Quaternary Science Reviews 19: 459–479.
Nicholson E, Mace GM, Armsworth PR, et al. (2009) Priority research areas for ecosystem services in a changing world. Journal of Applied Ecology 46: 1139–1144.
Oldfield F, Alverson K (2003) The societal relevance of paleoenvironmental research. In: Alverson K, Pedersen T, Bradley R (eds) Paleoclimate, Global Change and the Future. Berlin, Heidelberg: Springer, pp. 1–11.
PAGES 2k Consortium (2013) Continental-scale temperature variability during the past two millennia. Nature Geoscience 6: 339–346.
Pazdur A (2005) Archaeological cultures on the background of climatic changes in the Holocene, Poland. In: Marian Scott E, Alekseev A, Zaitseva G (eds) Impact of the Environment on Human Migration in Eurasia. Dordrecht: Springer, pp. 309–321.
Quinlan R, Smol JP, Hall RI (1998) Quantitative inferences of past hypolimnetic anoxia in south-central Ontario lakes using fossil midges (Diptera: Chironomidae). Canadian Journal of Fisheries and Aquatic Sciences 55: 587–596.
R Development Core Team (2009) R Project for Statistical Computing, version 2.9. 2. Vienna: R Foundation for Statistical Computing.
Ralska-Jasiewiczowa M, Starkel L (1988) Record of the hydrological changes during the Holocene in the lake, mire and fluvial deposits of Poland. Folia Quaternaria 57: 91–127.
Scheffer M, Carpenter S, Foley JA, et al. (2001) Catastrophic shifts in ecosystems. Nature 413: 591–596.
Schmidt R, Koinig KA, Thompson R, et al. (2002) A multi proxy core study of the last 7000 years of climate and alpine land-use impacts on an Austrian mountain lake (Unterer Landschitzsee, Niedere Tauern). Palaeogeography, Palaeoclimatology, Palaeoecology 187: 101–120.
Schoonmaker PK, Foster DR (1991) Some implications of paleoecology for contemporary ecology. The Botanical Review 57: 204–245.
Skwierawski A (2011) The Causes, Extent and Consequences of Lake Drainage in the Olsztyn Lakeland in the 19th and Early 20th Century. Environment Alterations-Research and Protection Methods. Olsztyn: University of Warmia and Mazury, pp. 33–52.
Spanbauer TL, Allen CR, Angeler DG, et al. (2014) Prolonged instability prior to a regime shift. PloS ONE 9: e108936.
Srokowski S (1930) Jeziora i moczary Prus wschodnich [Lakes and swamps of East Prussia]. Warsaw: Wojskowy Instytut Naukowo-Wydawniczy.
Stewart MM, Larocque-Tobler I, Grosjean M (2011) Quantitative inter-annual and decadal June–July–August temperature variability ca. 570 BC to AD 120 (Iron Age–Roman Period) reconstructed from the varved sediments of Lake Silvaplana, Switzerland. Journal of Quaternary Science 26: 491–501.
Szumański A (2000) Objaśnienia do Szczegółowej Mapy Geologicznej w skali 1:50000 [Detailed explanation of the Geological Map of Poland in scale 1:50000]. Warsaw: Panstwowy Instytut Geologiczny.
Taranu ZE, Gregory-Eaves I, Leavitt PR, et al. (2015) Acceleration of cyanobacterial dominance in north temperate-subarctic lakes during the Anthropocene. Ecology Letters 18: 375–384.
Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5 and the experiment design. Bulletin of the American Meteorological Society 93: 485–498.
Thevenon F, de Alencastro LF, Loizeau J-L, et al. (2013) A high-resolution historical sediment record of nutrients, trace elements and organochlorines (DDT and PCB) deposition in a drinking water reservoir (Lake Brêt, Switzerland) points at local and regional pollutant sources. Chemosphere 90: 2444–2452.
Tinner W, Hubschmid P, Wehrli M, et al. (1999) Long-term forest fire ecology and dynamics in southern Switzerland. Journal of Ecology 87: 273–289.
Trouet V, Esper J, Graham NE, et al. (2009) Persistent positive North Atlantic oscillation mode dominated the Medieval Climate Anomaly. Science 324: 78–80.
Tylmann W (2005) Lithological and geochemical record of anthropogenic changes in recent sediments of a small and shallow lake (Lake Pusty Staw, northern Poland). Journal of Paleolimnology 33: 313–325.
Tylmann W, Bonk A, Goslar T, et al. (2016) Calibrating 210Pb dating results with varve chronology and independent chronostratigraphic markers: Problems and implications. Quaternary Geochronology 32: 1–10.
Wacnik A (2009) From foraging to farming in the Great Mazurian Lake District: Palynological studies on Lake Miłkowskie sediments, northeast Poland. Vegetation History and Archaeobotany 18: 187–203.
Wacnik A, Goslar T, Czernik J (2012) Vegetation changes caused by agricultural societies in the Great Mazurian Lake District. Acta Palaeobotanica 52: 59–104.
Wacnik A, Tylmann W, Bonk A, et al. (2016) Determining the responses of vegetation to natural processes and human impacts in north-eastern Poland during the last millennium: Combined pollen, geochemical and historical data. Vegetation History and Archaeobotany. Epub ahead of print 17 March.
Wakar A, Wilamowski B (1968) Węgorzewo z Dziejów Miasta i Powiatu [Węgorzewo: The History of the Town and County]. Olsztyn: Pojezierze, 312 pp.
Wersin P, Höhener P, Giovanoli R, et al. (1991) Early diagenetic influences on iron transformations in a freshwater lake sediment. Chemical Geology 90: 233–252.
Whitlock C, Larsen C (2001) Charcoal as a Fire Proxy: Tracking Environmental Change using Lake Sediments. Berlin: Springer, pp. 75–97.
Witak M, Hernandez-Almeida I, Grosjean M, et al. (in press) Diatom-based reconstruction of past trophic status changes recorded in varved sediments of Lake Żabińskie, northeastern Poland, AD 1888–2010. Oceanological and Hydrobiological Studies.
Zolitschka B (1998) A 14,000 year sediment yield record from western Germany based on annually laminated lake sediments. Geomorphology 22: 1–17.
Zolitschka B, Francus P, Ojala AEK, et al. (2015) Varves in lake sediments – A review. Quaternary Science Reviews 117: 1–41.
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