Log in

A chironomid-based salinity inference model from lakes on the Tibetan Plateau

  • Original Paper
  • Published:
Journal of Paleolimnology Aims and scope Submit manuscript

Abstract

Previous studies have shown chironomids to be excellent indicators of environmental change and training sets have been developed in order to allow these changes to be reconstructed quantitatively from subfossil sequences. Here we present the results of an investigation into the relationships between surface sediment subfossil chironomid distribution and lake environmental variables from 42 lakes on the Tibetan Plateau. Canonical correspondence analysis (CCA) revealed that of the 11 measured environmental variables, salinity (measured as total dissolved solids TDS) was most important, accounting for 10.5% of the variance in the chironomid data. This variable was significant enough to allow the development of quantitative inference models. A range of TDS inference models were developed using Weighted Averaging (WA), Partial Least Squares (PLS), Weighted Averaging–Partial Least Squares (WA–PLS), Maximum Likelihood (ML), Modern Analogues Technique (MAT) and Modern Analogues Techniques weighted by similarity (WMAT). Evaluation of the site data indicated that four lakes were major outliers, and after omitting these from the training set the models produced jack-knifed coefficients of determination (r 2) between 0.60 and 0.80, and root-mean-squared errors of prediction (RMSEP) between 0.29 and 0.44 log10 TDS. The best performing model was the two-component WA–PLS model with r 2 jack = 0.80 and RMSEPjack = 0.29 log10 TDS. The model results were similar to other chironomid-salinity models developed in different regions, and they also showed similar ecological grou**s along the salinity gradient with respect to freshwater/salinity thresholds and community diversity. These results therefore indicate that similar processes may be controlling chironomid distribution across salinity gradients irrespective of biogeographical constraints. The performance of the transfer functions illustrates that chironomid assemblages from the Tibetan Plateau lakes are clearly sensitive indicators of salinity. The models will therefore allow the quantification of long-term records of past water salinity for lacustrine sites across the Tibetan Plateau, which has important implications for future hydrological research in the region.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
EUR 32.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or Ebook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price includes VAT (United Kingdom)

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4

Similar content being viewed by others

References

  • Academica Sinica (1979) Report on the comprehensive expedition to lake Qinghai. Scientific Publishing House, Bei**g, China, pp. 44–66 (in Chinese)

  • Barnett TP, Adam JC, Lettenmaier DP (2005) Potential impacts of a warming climate on water availability in snow-dominated regions. Nature 438:303–309

    Article  CAS  Google Scholar 

  • Birks HJB (1995) Quantitative palaeoenvironmental reconstructions. In: Maddy D, Brew JS (eds) Statistical modelling of quaternary science data. Technical Guide 5, Quaternary Research Association, Cambridge, pp. 161–254

  • Birks HJB (1998) Numerical tools in palaeolimnology–progress, potentialities, and problems. J Paleolimnol 20:307–332

    Article  Google Scholar 

  • Birks HJB, Line JM, Juggins S, Stevenson AC, ter Braak CJF (1990a) Diatoms and pH reconstruction. Phil Trans Royal Soc London B 327:263–278

    Article  Google Scholar 

  • Birks HJB, Juggins S, Line JM (1990b) Lake surface-water chemistry reconstructions from palaeolimnolical data. In: Mason B (ed) The surface water acidification programme. Cambridge University Press, Cambridge, pp. 301–313

    Google Scholar 

  • Brooks SJ (2003) Chironomid analysis to interpret and quantify Holocene climate change.In: Mackay AW, Battarbee RW Birks HJB Oldfield F (eds) Global change in the holocene. Arnold, London, pp. 328–341

    Google Scholar 

  • Brooks SJ (2006) Fossil midges (Diptera: Chironomidae) as palaeoclimatic indicators for the Eurasian region. Quat Sci Rev 25:1894–1910

    Article  Google Scholar 

  • Brooks SJ, Bennion H, Birks HJB (2001) Tracing lake trophic history with a chironomid–total phosphorus inference model. Freshw Biol 46:513–533

    Article  CAS  Google Scholar 

  • Brooks SJ, Birks HJB (2001) Chironomid-inferred air temperatures from Lateglacial and Holocene sites in north-west Europe: progress and problems. Quat Sci Rev 20:1723–1741

    Article  Google Scholar 

  • Brooks SJ, Udachin V, Williamson BJ (2005) Impact of copper smelting on lakes in the southern Ural Mountains, Russia, Inferred from chironomid. J Paleolimnol 33:229–241

    Article  Google Scholar 

  • Clerk S, Hall R, Quinlan R, Smol JP (2000) Quantitative inferences of past hypolimnetic anoxia and nutrient levels from a Canadian Precambrian Shield lake. J Paleolimnol 23:319–336

    Article  Google Scholar 

  • Eggermont H, Heiri O, Verschuren D (2006) Fossil Chironomidae (Insecta: Diptera) as quantitative indicators of past salinity in African lakes. Quat Sci Rev 25:1966–1994

    Article  Google Scholar 

  • Flohn H (1968) Contribution to a meteorology of the Tibetan Highlands. Atmos Sci Pap 130, Colorado State University, Fort Collins, Colorado, USA

  • Gandouin E, Maasri A, Van Vliet-Lanoë B, Franquet E (2006) Chironomid (Insecta: Diptera) assemblages from a gradient of lotic and lentic waterbodies in river floodplains of France: a methodological tool for paleoecological applications. J Paleolimnol 35:149–166

    Article  Google Scholar 

  • Gao Q, Shi S (1992) Water resources in the arid zone of northwest China. J Desert Res 12:1–12

    Google Scholar 

  • Gasse F, Derbyshire E (1996) Environmental changes in the Tibetan Plateau and surrounding areas–Preface. Palaeogeogr Palaeoclim Palaeoecol 120:1–3

    Article  Google Scholar 

  • Gasse F, Fontes JC, van Campo E, Wie K (1996) Holocene environmental changes in Bangong Co basin (Western Tibet). Part 4: discussions and conclusions. Palaeogeogr Palaeoclim Palaeoecol 120:79–92

    Article  Google Scholar 

  • Greenberg AE, Clesceri LS, Eaton AD (1992) Standard methods for the examination of water and wastewater. American Public Health Association, Washington, pp. 3/34–4/138

  • Hahn DG, Manabe S (1975) The role of mountains in the south Asian monsoon circulation. J Atmos Sci 32:1515–1541

    Article  Google Scholar 

  • Heegaard E, Lotter A, Birks H (2006) Aquatic biota and the detection of climate change: Are there consistent aquatic ecotones? J Paleolimnol 35:507–518

    Article  Google Scholar 

  • Heinrichs ML, Walker IR (2006) Fossil midges and palaeosalinity: potential as indicators of hydrological balance and sea-level change. Quat Sci Rev 25:1948–1965

    Article  Google Scholar 

  • Heinrichs ML, Walker IR, Mathewes RW (2001) Chironomid-based paleosalinity records in southern British Columbia, Canada: a comparison of transfer functions. J Paleolimnol 26:147–159

    Article  Google Scholar 

  • Heiri O, Lotter AF, Hausmann S, Kienast F (2003) A chironomid-based Holocene summer air temperature reconstruction from the Swiss Alps. The Holocene 13:477–484

    Article  Google Scholar 

  • Hill MO, Gauch HG (1980) Detrended correspondence analysis: an improved ordination technique. Vegetation 42:47–58

    Article  Google Scholar 

  • Hofmann W (1998) Cladocerans and chironomids as indicators of lake level changes in north temperate lakes. J Paleolimnol 19:55–62

    Article  Google Scholar 

  • Institute of Hydrogeography and Engineering Geology, MGMR (1990) Water Quality Analysis. Geology Press, Bei**g, pp.36–200 (in Chinese)

  • Jones VJ, Juggins S (1995) The construction of a diatom-based chlorophyll a transfer function and its application at three lakes on Signy Island (maritime Antarctic) subject to differing degrees of nutrient enrichment. Freshw Biol 34:433–445

    Article  CAS  Google Scholar 

  • Juggins S (2003) C2 user guide: software for ecological and palaeoecological data analysis and visualisation. University of Newcastle, Newcastle upon Tyne, Britain

    Google Scholar 

  • Korhola A, Olander H, Blom T (2000) Cladoceran and chironomid assemblages as quantitative indicators of water depth in subarctic Fennoscandian lakes. J Paleolimnol 24:43–54

    Article  Google Scholar 

  • Lang B, Bedford A, Richardson N, Brooks SJ (2003) The use of ultra-sound in the preparation of carbonate and clay sediment for chironomid analysis. J Paleolimnol 30:451–460

    Article  Google Scholar 

  • Langdon PG, Barber KE, Lomas-Clarke SH (previously Morriss) (2004) Reconstructing climate and environmental change in Northern England through chironomid and pollen analyses: evidence from Talkin Tarn, Cumbria. J Paleolimnol 32:197–213

    Google Scholar 

  • Langdon PG, Ruiz Z, Brodersen KP, Foster IDL (2006) Assessing lake eutrophication using chironomids: understanding the nature of community response in different lake types. Freshw Biol 51:562–577

    Article  CAS  Google Scholar 

  • Lau K, Li M (1984) The monsoon of East Asia and its global association–a survey. Bull Am Meteorol Soc 65:114–125

    Article  Google Scholar 

  • Lotter AF, Birks HJB, Hofmann W, Marchetto A (1997) Modern diatom, cladocera, chironomid, and chrysophyte cyst assemblages as quantitative indicators for the reconstruction of past environmental conditions in the Alps.Ι. Climate. J Paleolimnol 18:395–420

    Article  Google Scholar 

  • Martens H, Naes T (1989) Multivariate calibration. Wiley, Chichester

    Google Scholar 

  • Oliver DR, Roussel ME (1983) The insects and arachnids of Canada. Part 11. The genera of larval midges of Canada. Diptera: chironomidae. Agriculture Canada, Ottawa, pp 1–263

  • Pinder LCV, Morley DJ (1995) Chironomidae as indicators of water quality-with a comparison of the chironomid faunas of a series of contrasting Cumbrian tarns. In: Harrington R, Stork NE (eds) Insects in a changing environment. Academic Press, London, pp. 272–290

    Google Scholar 

  • Quinlan R, Smol JP (2001) Setting minimum head capsule abundance and taxa deletioncriteria in chironomid-based inference models. J Paleolimnol 26:327–342

    Article  Google Scholar 

  • Rieradevall M, Brooks SJ (2001) An identification guide to subfossil Tanypodinae larvae (Insecta: Diptera: Chironomidae) based on cephalic setation. J Paleolimnol 25:81–99

    Article  Google Scholar 

  • Shao XM, Huang L, Liu HB, Liang EY, Fang XQ, Wang LL (2005) Reconstruction of precipitation variation from tree rings in recent 1,000 years in Delingha, Qinghai. Sci China Ser D 48:939–949

    Article  Google Scholar 

  • Singh P, Kumar N (1997) Impact assessment of climate change on the hydrological response of a snow and glacier melt runoff dominated Himalayan river. J Hydrol 93:316–350

    Article  Google Scholar 

  • Singh P (2003) Effect of warmer climate on the depletion of snow covered area in the Satluj basin in the western Himalayan region. Hydrol Sci J 48:413–425

    Article  Google Scholar 

  • ter Braak CJF (1987) The analysis of vegetation-environment relationships by canonical correspondence analysis. Vegetatio 69:69–77

    Article  Google Scholar 

  • ter Braak CJF (1990) Update notes: CANOCO version 3.10.Agricultural Mathematics Group, Wageningen

  • ter Braak CJF, Prentice IC (1988) A theory of gradient analysis. Advances in Ecol Res 18:271–317

    Article  Google Scholar 

  • ter Braak CJF, Juggins S (1993) Weighted averaging partial least squares regression (WA–PLS): an improved method for reconstructing environmental variables from species assemblages. Hydrobiologia 269/270:485–502

    Article  Google Scholar 

  • ter Braak CJF, Šmilauer P (1998) CANOCO reference manual and user’s guide to Canoco for Windows (version 4). Centre for Biometry Wageningen, New York

  • Velle G, Brooks SJ, Birks HJB, Willassen E (2005) Chironomids as a tool for inferring Holocene climate: an assessment based on six sites in southern Scandinavia. Quat Sci Rev 24:1429–1462

    Article  Google Scholar 

  • Verschuren D (2003) Lake-based climate reconstruction in Africa: progress and challenges. Hydrobiologia 500:315–330

    Article  Google Scholar 

  • Verschuren D, Tibby J, Sabbe K, Roberts CN (2000) Effects of lake level, salinity and substrate on the invertebrate community of a fluctuating tropical lake. Ecology 81:164–182

    Article  Google Scholar 

  • Verschuren D, Cumming BF, Laird KR (2004) Quantitative reconstruction of past salinity variations in African lakes: assessment of chironomid-based inference models (Insecta: Diptera) in space and time. Can J Fish Aquat Sci 61:986–998

    Article  Google Scholar 

  • Walker IR (1987) Chironomidae (Diptera) in paleoecology. Quat Sci Rev 6:29–40

    Article  Google Scholar 

  • Walker IR (2001) Midges:Chironomidae and related Diptera. In: Smol JP, Birks HJB, Last WM (eds) Tracking environmental change using late sediments. Vol. 4. Zoological Indicators, Kluwer Academic Publishers, Dordrecht, pp. 43–66

  • Walker IR, Paterson CG (1985) Efficient separation of subfossil Chironomidae from lake sediments. Hydrobiologia 122:189–192

    Article  Google Scholar 

  • Walker IR, MacDonald GM (1995) Distributions of Chironomidae (Insecta: Diptera) and other freshwater midges with respect to treeline, Northwest Territories, Canada. Arct Alp Res 27:258–263

    Article  Google Scholar 

  • Walker IR, Smol JP, Engstrom DR, Birks HJB (1991) An assessment of Chironomidae as quantitative indicators of past climatic change. Can J Fish Aquat Sci 48:975–987

    Google Scholar 

  • Walker IR, Wilson SE, Smol JP (1995) Chironomidae (Diptera): quantitative palaeosalinity indicators for lakes of western Canada. Can J Fish Aquat Sci 52:950–960

    Article  Google Scholar 

  • Walker IR, Cwynar LC (2006) Midges and palaeotemperature reconstruction—the North American experience. Quat Sci Rev 25:1911–1925

    Article  Google Scholar 

  • Wetzel BG (2001) Limnology. Academic Press, San Diego, USA

    Google Scholar 

  • Wiederholm T (ed) (1983) Chironomidae of the Holarctic region. Keys and Diagnoses. Part I. Larvae. Entomologica Scandinavica Supplement 19, pp. 1–457

  • Williams WD, Boulton AJ, Taaffe RG (1990) Salinity as a determinant of salt lake fauna: a question of scale. Hydrobiologia 197:257–266

    Article  CAS  Google Scholar 

  • Woodward CA, Shulmeister J (2005) A Holocene record of human induced and natural environmental change from Lake Forsyth (Te Wairewa), New Zealand. J Paleolimnol. 34:481–501

    Article  Google Scholar 

  • Yang X, Kamenik C, Schmidt R, Wang S (2003) Diatom-based conductivity and water-level inference models from eastern Tibetan (Qinghai-**zang) Plateau lakes. J Paleolimnol 30:1–19

    Article  CAS  Google Scholar 

  • Yang X, Wang S, Kamenik C, Schmidt R, Shen J, Zhu L, Li S (2004) Diatom assemblages and quantitative reconstruction for palaeo-salinity from a sediment core of Chencuo Lake, southern Tibet. Sci China Ser D 47:522–528.

    Article  Google Scholar 

  • Yao TD, Guo XJ, Thompson L, Duan KQ, Wang NL, Pu JC, Xu BQ,Yang XX, Sun WZ (2006). Delta O-18 record and temperature change over the past 100 years in ice cores on the Tibetan Plateau. Sci China Ser D 49:1–9

    Article  CAS  Google Scholar 

  • Zhang EL, Shen J, Wang SM, Yin Y, Zhu YX, **a WL (2004) Quantitative reconstruction of thepaleosalinity at Qinghai Lake in the past 900 years. Chinese Sci Bull 49:730–734

    Article  CAS  Google Scholar 

  • Zhang EL, Bedford A, Jones RT, Shen J, Wang SM, Tang HQ (2006) A subfossil chironomid-total phosphorus inference model for lakes in the middle and lower reaches of the Yangtze River. Chinese Sci Bull 51:2125–2132

    Article  CAS  Google Scholar 

Download references

Acknowledgements

We gratefully acknowledge Prof. **angdong Yang for the samples and providing the chemistry data as well as constructive suggestions regarding this paper. Prof. Ji Shen, Prof. John Dearing, Prof. Wang Sumin, Dr. Enfeng Liu, Mr. Xuhui Dong, Dr. Barbara Lang, Prof. Houyuan Lü and Prof. **nhua Wang, are also acknowledged for their help during the preparation of this paper. Prof. Ian Walker is acknowledged for providing references and Bob Smith of the Southampton University Geography Cartographic Department is thanked for preparing the figures. We are very grateful to Drs Hilde Eggermont and Markus Heinrichs whose comments greatly improved the manuscript. This study is supported by the State Key Basic Research and Development Plan of China (2005CB422002), NSFC (Grant No.:40402015), and the Knowledge Innovation Program of the CAS (KZCX3-SW-339).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Enlou Zhang.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Zhang, E., Jones, R., Bedford, A. et al. A chironomid-based salinity inference model from lakes on the Tibetan Plateau. J Paleolimnol 38, 477–491 (2007). https://doi.org/10.1007/s10933-006-9080-z

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10933-006-9080-z

Keywords

Navigation