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Lake and catchment response to Holocene environmental change: spatial variability along a climate gradient in southwest Greenland

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Abstract

The Kangerlussuaq area of southwest Greenland is a lake-rich landscape that covers a climate gradient: a more maritime, cooler and wetter coastal zone contrasts with a dry, continental interior. Radiocarbon-dated sediment sequences (covering ~11,200–8,300 cal year) from paired lakes at the coast and the head of the fjord were analysed for lithostratigraphic variables (organic-matter content, bulk density, Ti, Ca). Minerogenic and carbon accumulation rates from the four lakes were compared to determine catchment and lake response to Holocene climatic variability. Catchment erosion at the coast was dominated by cryonival processes, with considerable sediment production due to the limited vegetation cover and exposed rock faces. Input of minerogenic sediment at one site (AT4) was high (>1 gDW cm−2 year−1) during the period 5,800–4,000 cal year BP, perhaps reflecting intensification of cryogenic processes on northeast-facing slopes and rapid delivery to the lake. This period of erosional activity was not observed at the nearby, higher elevation site (AT1) due to the lower catchment relief; instead, there was an abrupt decline in carbon and minerogenic accumulation rates at ~5,800 cal year BP. Sediment accumulation rates at the inland sites were much lower (<0.005 gDW cm−2 year−1) reflecting greater catchment stability (more extensive vegetation cover), lower relief and substantially lower precipitation, but synchronous increases in mineral accumulation rates from ~1,200 to 1,000 cal year BP may reflect wind erosion associated with regional cooling and local aridity. Carbon-accumulation-rate profiles were similar at the two inland sites, with higher-than-average accumulation (~6–8 g C m−2 year−1) during the early Holocene and a subsequent decline after ~6,000 cal year BP. At the inland lakes, both mineral and carbon accumulation rates exhibited a stronger link to climate, driven by trends in effective precipitation and regional aeolian activity. Catchment differences (relief, altitude) lead to more individualistic records in both erosion history and lake productivity at the coast.

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References

  • Abbott MB, Stafford TW (1996) Radiocarbon geochemistry of modern and ancient Arctic lake systems, Baffin Island, Canada. Quat Res 45:300–311

    Article  Google Scholar 

  • ACIA (2005) Arctic Climate Impact Assessment. Cambridge University Press, Cambridge, p 1042

    Google Scholar 

  • Aebly FA, Fritz SC (2009) Palaeohydrology of Kangerlussuaq (Søndre Strømfjord), west Greenland during the last ~8000 years. Holocene 19:91–104

    Article  Google Scholar 

  • AMAP (2006) Assessment report: Arctic Monitoring and Assessment Programme. AMAP, Oslo

    Google Scholar 

  • Anderson NJ, Leng MJ (2004) Increased aridity during the early Holocene in west Greenland inferred from stable isotopes in laminated-lake sediments. Quat Sci Rev 23:841–849

    Article  Google Scholar 

  • Anderson NJ, Stedmon CA (2007) The effect of evapoconcentration on dissolved organic carbon concentration and quality in lakes of SW Greenland. Freshwat Biol 52:280–289

    Article  Google Scholar 

  • Anderson L, Abbott MB, Finney BP (2001a) Holocene climate inferred from oxygen isotope ratios in lake sediments, central Brooks Range, Alaska. Quat Res 55:313–321

    Article  Google Scholar 

  • Anderson NJ, Harriman R, Ryves DB, Patrick ST (2001b) Dominant factors controlling variability in the ionic composition of west Greenland lakes. Arct Antarct Alp Res 33:418–425

    Article  Google Scholar 

  • Anderson NJ, Brodersen KP, Ryves DB, McGowan S, Johansson LS, Jeppesen E, Leng MJ (2008) Climate versus in-lake processes as controls on the development of community structure in a low-arctic lake (south-west Greenland). Ecosystems 11:307–324

    Article  Google Scholar 

  • Anderson NJ, D’Andrea W, Fritz SC (2009) Holocene carbon burial by lakes in SW Greenland. Global Change Biol 15:2590–2598

    Article  Google Scholar 

  • Andresen CS, Bjorck S, Bennike O, Bond G (2004) Holocene climate changes in southern Greenland: evidence from lake sediments. J Quat Sci 19:783–795

    Article  Google Scholar 

  • Bennike O (2000) Palaeoecological studies of Holocene lake sediments from west Greenland. Palaeogeog Palaeoclimat Palaeoecol 155:285–304

    Article  Google Scholar 

  • Bennike O, Anderson NJ, McGowan S (2010) Holocene palaeoecology of southwest Greenland inferred from macrofossils in sediments of an oligosaline lake. J Paleolimnol 43:787–798

    Article  Google Scholar 

  • Bennike O, Wagner B, Richter A (2011) Relative sea level changes during the Holocene in the Sisimiut area, south-western Greenland. J Quat Sci 26:353–361

    Article  Google Scholar 

  • Callaghan TV, Bergholm F, Christensen TR, Jonasson C, Kokfelt U, Johansson M (2010) A new climate era in the sub-arctic: accelerating climate changes and multiple impacts. Geophys Res Letts 37:L14705

    Article  Google Scholar 

  • Cockburn JMH, Lamoureux SF (2008a) Hydroclimate controls over seasonal sediment yield in two adjacent high arctic watersheds. Hydrol Proc 22:2013–2027

    Article  Google Scholar 

  • Cockburn JMH, Lamoureux SF (2008b) Inflow and lake controls on short-term mass accumulation and sedimentary particle size in a high arctic lake: Implications for interpreting varved lacustrine sedimentary records. J Paleolimnol 40:923–942

    Article  Google Scholar 

  • D’Andrea WJ, Huang Y, Fritz SC, Anderson NJ (2011) Abrupt Holocene climate change as an important factor for human migration in west Greenland. Proc Nat Acad Sci 108:9765–9769

    Article  Google Scholar 

  • Dean WE (1974) Determination of carbonate and organic-matter in calcareous sediments and sedimentary rocks by loss on ignition: comparison with other methods. J Sediment Petrol 44:242–248

    Google Scholar 

  • Dearing JA (1991) Lake sediment records of erosional processes. Hydrobiol 214:99–106

    Article  Google Scholar 

  • Dugan HA, Lamoureux SF, Lafreniere MJ, Lewis T (2009) Hydrological and sediment yield response to summer rainfall in a small high arctic watershed. Hydrol Process 23:1514–1526

    Article  Google Scholar 

  • Eisner WR, Törnqvist TE, Koster EA, Bennike O, Vanleeuwen JFN (1995) Paleoecological studies of a Holocene lacustrine record from the Kangerlussuaq (Søndre Strømfjord) region of west Greenland. Quat Res 43:55–66

    Article  Google Scholar 

  • Francis JA, White DM, Cassano JJ, Gutowski WJ Jr, Hinzman LD, Holland MM, Steele MA, Voeroesmarty CJ (2009) An Arctic hydrologic system in transition: feedbacks and impacts on terrestrial, marine, and human life. J Geophys Res 114:G04019

    Article  Google Scholar 

  • Fredskild B (1991) The genus Betula in Greenland: Holocene history, present distribution and synecology. Nord J Bot 11:393–412

    Article  Google Scholar 

  • Geirsdottir A, Miller GH, Thordarson T, Olafsdottir KB (2009) A 2000 year record of climate variations reconstructed from Haukadalsvatn, west Iceland. J Paleolimnol 41:95–115

    Article  Google Scholar 

  • Hasholt B, Søgaard H (1978) Et forsøg på en klimatisk-hydrologisk regionsinddeling af Holsteinborgs kommune (Sisimiut). Geogr Tidsskr 77:72–92

    Google Scholar 

  • Heggen MP, Birks HH, Anderson NJ (2010) Long-term ecosystem dynamics of a small lake and its catchment in west Greenland. Holocene 20:1207–1222

    Article  Google Scholar 

  • Lamoureux SF, Gilbert R (2004) A 750-year record of autumn snowfall and temperature variability and winter storminess recorded in the varved sediments of Bear Lake, Devon Island, Arctic Canada. Quat Res 61:134–147

    Article  Google Scholar 

  • Lamoureux SF, Gilbert R, Lewis T (2002) Lacustrine sedimentary environments in high arctic proglacial Bear Lake, Devon Island, Nunavut, Canada. Arct Antarct Alp Res 34:130–141

    Article  Google Scholar 

  • Leavitt PR, Fritz SC, Anderson NJ, Baker PA, Blenckner T, Bunting L, Catalan J, Conley DJ, Hobbs WO, Jeppesen E, Korhola A, McGowan S, Rühland K, Rusak JA, Simpson GL, Solovieva N, Werne J (2009) Paleolimnological evidence of the effects on lakes of energy and mass transfer from climate and humans. Limnol Oceanogr 54:2330–2348

    Article  Google Scholar 

  • Leng MJ, Wagner B, Anderson NJ, Bennike O, Woodley E, Kemp S (2012) Deglaciation and catchment ontogeny in coastal southwest Greenland: Implications for terrestrial and aquatic carbon cycling. J Quat Sci (in press)

  • McGowan S, Ryves DB, Anderson NJ (2003) Holocene records of effective precipitation in west Greenland. Holocene 13:239–249

    Article  Google Scholar 

  • McGowan S, Grauert M, Anderson NJ (2008) A late Holocene record of landscape degradation from Heygsvatn, the Faroe Islands. Palaeogeog Palaeoclimat Palaeoecol 264:11–24

    Article  Google Scholar 

  • Perren BB, Anderson NJ, Douglas MSV, Fritz SC (2012) The influence of temperature, moisture, and eolian activity on Holocene lake development in West Greenland. J Paleolimnol. doi:10.1007/s10933-012-9613-6

  • Petterson G, Renberg I, Sjostedt-de Luna S, Arnqvist P, Anderson NJ (2010) Climatic influence on the inter-annual variability of late-Holocene minerogenic sediment supply in a boreal forest catchment. Earth Surf Proc Landforms 35:390–398

    Google Scholar 

  • Post E, Forchhammer MC, Bret-Harte MS, Callaghan TV, Christensen TR, Elberling B, Fox AD, Gilg O, Hik DS, Hoye TT, Ims RA, Jeppesen E, Klein DR, Madsen J, McGuire AD, Rysgaard S, Schindler DE, Stirling I, Tamstorf MP, van der Tyler NJC, Wal R, Welker J, Wookey PA, Schmidt NM, Aastrup P (2009) Ecological dynamics across the Arctic associated with recent climate change. Science 325:1355–1358

    Article  Google Scholar 

  • Ramsey CB (2008) Deposition models for chronological records. Quat Sci Rev 27:42–60

    Article  Google Scholar 

  • Ramsey CB (2009) Bayesian analysis of radiocarbon dates. Radiocarbon 51:337–360

    Google Scholar 

  • Reimer PJ, Baillie MGL, Bard E, Bayliss A, Beck TW, Blackwell PG, Ramsey CB, Buck CE, Burr GS, Edwards RL, Friedrich M, Grootes PM, Guilderson TP, Hajdas I, Heaton TJ, Hogg AG, Hughen KA, Kaiser KF, Kromer B, McCormac FG, Manning SW, Reimer RW, Richards DA, Southon JR, Talamo S, Turney CSM, van der Plicht J, Weyhenmeyer CE (2009) Intcal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51:1111–1150

    Google Scholar 

  • Rubensdotter L, Rosqvist G (2003) The effect of geomorphological setting on Holocene lake sediment variability, northern Swedish Lapland. J Quat Sci 18:757–767

    Article  Google Scholar 

  • Schofield JE, Edwards KJ, Mighall TM, Martinez Cortizas A, Rodriguez-Racedo J, Cook G (2010) An integrated geochemical and palynological study of human impacts, soil erosion and storminess from southern Greenland since c. AD 1000. Palaeogeogr Palaeoclimat Palaeoecol 295:19–30

    Article  Google Scholar 

  • van Tatenhove FGM, van der Meer JJM, Koster RD (1996) Implications for deglaciation chronology from new AMS age determinations in central west Greenland. Quat Res 45:245–253

    Article  Google Scholar 

  • Wagner B, Bennike O (2012) Chronology of the last deglaciation and Holocene environmental changes in the Sisimiut area, south-west Greenland based on lacustrine records. Boreas (in press)

  • Willemse NW, Törnqvist TE (1999) Holocene century-sale temperature variability from west Greenland lake records. Geology 27:580–584

    Article  Google Scholar 

  • Willemse NW, Koster EA, Hoogakker B, van Tatenhove FGM (2003) A continuous record of Holocene eolian activity in west Greenland. Quat Res 59:322–334

    Article  Google Scholar 

  • Wookey PA, Aerts R, Bardgett RD, Baptist F, Brathen KA, Cornelissen JHC, Gough L, Hartley IP, Hopkins DW, Lavorel S, Shaver GR (2009) Ecosystem feedbacks and cascade processes: understanding their role in the responses of arctic and alpine ecosystems to environmental change. Global Change Biol 15:1153–1172

    Article  Google Scholar 

Download references

Acknowledgments

We thank William D’Andrea, Tessa Needham and Kent Joensen for help with fieldwork, Jesper Olsen for the 14C chronologies, and Mike Marshall for help with the XRF analyses. Dating was funded by NERC (awards to NJA and SMcG), thanks to Charlotte Bryant at the NERC radiocarbon laboratory. Fieldwork was funded by a University of Nottingham New Lecturer’s Award to SMcG and a Royal Geographical Society Postgraduate Travel Bursary to ACL. Three anonymous reviewers provided helpful comments on an earlier draft.

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Correspondence to N. J. Anderson.

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This is one of 18 papers published in a special issue edited by Darrell Kaufman, and dedicated to reconstructing Holocene climate and environmental change from Arctic lake sediments.

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Anderson, N.J., Liversidge, A.C., McGowan, S. et al. Lake and catchment response to Holocene environmental change: spatial variability along a climate gradient in southwest Greenland. J Paleolimnol 48, 209–222 (2012). https://doi.org/10.1007/s10933-012-9616-3

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