Journal of Paleolimnology

, Volume 58, Issue 4, pp 551–569 | Cite as

Trends in catchment processes and lake evolution during the late-glacial and early- to mid-Holocene inferred from high-resolution XRF data in the Yellowstone region

  • Yanbin Lu
  • Sherilyn C. Fritz
  • Jeffery R. Stone
  • Teresa R. Krause
  • Cathy Whitlock
  • Erik T. Brown
  • James V. Benes
Original paper


High-resolution records of geochemical data from four lakes in the Greater Yellowstone region were used to investigate watershed and lake history during the late-glacial and early-Holocene periods. Clastic input to regional lakes was high and variable during the early stages of lake development, when the surrounding landscape was geomorphically unstable and sparsely vegetated, and it decreased as vegetation gradually developed in each catchment. The decrease of clastic input was not regionally synchronous but occurred in a time-transgressive pattern from south to north. Long-term organic matter concentration and diatom production were inversely related to catchment erosion during the early stages of lake development and increased as temperatures warmed and in-lake nutrient concentrations increased. Similarly, calcite production usually was low following lake formation and increased over time, driven by climate change and its associated influences on lake-level, algal production, and lake thermal structure. Overall differences in the timing and pattern of geochemical change indicate that once the landscape had stabilized following deglaciation, changes in the geochemical character of the sediments were strongly influenced by local factors.


X-ray fluorescence Paleoenvironments Western North America Watershed history 



This research was supported by National Science Foundation Grants EAR-0816576 to S. Fritz and EAR-0818467 to C. Whitlock, as well as a GSA Graduate Student Research grant to Y. Lu. We thank C. Hendrix and S. Gunther (Yellowstone National Park) for logistical support, and T. Spanbauer, D. Navarro, and J. Giskaas for field assistance.


  1. Aguilar C, Nealson KH (1998) Biogeochemical cycling of manganese in Oneida Lake, New York: whole lake studies of manganese. J Gt Lakes Res 24:93–104CrossRefGoogle Scholar
  2. Alley RB, Clark PU (1999) The deglaciation of the northern hemisphere: a global perspective. Annu Rev Earth Planet Sci 27:149–182CrossRefGoogle Scholar
  3. Battarbee RW (2000) Palaeolimnological approaches to climate change with special regard to the biological record. Quat Sci Rev 19:107–124CrossRefGoogle Scholar
  4. Berger AL (1978) Long-term variations of caloric insolation resulting from Earth’s orbital elements. Quat Res 9:139–167CrossRefGoogle Scholar
  5. Bigler C, Larocque I, Peglar SM, Birks HJB, Hall RI (2002) Quantitative multi-proxy assessment of long-term patterns of Holocene environmental change from a small lake near Abisko, northern Sweden. Holocene 12:481–496CrossRefGoogle Scholar
  6. Bigler C, Grahn E, Larocque I, Jeziorski A, Hall R (2003) Holocene environmental change at Lake Njulla (999 m asl), northern Sweden: a comparison with four small nearby lakes along an altitudinal gradient. J Paleolimnol 29:13–29CrossRefGoogle Scholar
  7. Birks HH, Battarbee RW, Birks HJB (2000) The development of the aquatic ecosystem at Krakenes Lake, western Norway, during the late-glacial and early-Holocene—a synthesis. J Paleolimnol 23:91–114CrossRefGoogle Scholar
  8. Blaauw M, Christen A (2011) Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Anal 6:457–474Google Scholar
  9. Bradshaw EG, Jones VJ, Birks HJB, Birks HH (2000) Diatom responses to late-glacial and early-Holocene environmental changes at Kråkenes, western Norway. J Paleolimnol 23:21–34CrossRefGoogle Scholar
  10. Brown ET (2015) Estimation of biogenic silica concentrations using scanning XRF: insights from studies of Lake Malawi sediments. In: Croudace IW, Rothwell RG (eds) Micro-XRF studies of sediment cores-applications of a non-destructive tool for the environmental sciences. Developments in paleoenvironmental research, vol 17. Springer, Dordrecht, pp 267–277CrossRefGoogle Scholar
  11. Cohen AS (2003) Paleolimnology: the history and evolution of lake systems. Oxford University Press, New YorkGoogle Scholar
  12. Croudace IW, Rothwell RG (eds) (2015) Micro-XRF studies of sediment cores—applications of a non-destructive tool for the environmental sciences. Developments in paleoenvironmental research, vol 17. Springer, Dordrecht, p 656Google Scholar
  13. Croudace IW, Rindby A, Rothwell RG (2006) ITRAX: description of evaluation of a new multi-functional X-ray core scanner. In: Rothwell RG (ed) New techniques in sediment core analysis. The Geological Society of London, LondonGoogle Scholar
  14. Das BK, Haake B-G (2003) Geochemistry of Rewalsar Lake sediment, Lesser Himalaya, India: implications for source-area weathering, provenance and tectonic setting. Geosci J 7:299–312CrossRefGoogle Scholar
  15. Das SK, Routh J, Roychoudhury AN, Klump JV, Ranjan RK (2009) Phosphorus dynamics in shallow eutrophic lakes: an example from Zeekoevlei, South Africa. Hydrobiologia 619:55–66CrossRefGoogle Scholar
  16. Davison W (1993) Iron and manganese in lakes. Earth Sci Rev 34:119–163CrossRefGoogle Scholar
  17. Dean WE, Megard RO (1993) Environment of deposition of CaCO3 in Elk Lake, Minnesota. In: Bradbury JP, Dean WE (eds) Elk Lake, Minnesota: evidence for rapid climate change in the North-Central United States. Geological Society of America, Boulder, Special Paper 276, pp 97–114Google Scholar
  18. Engstrom DR, Fritz SC, Almendinger JE, Juggins S (2000) Chemical and biological trends during lake evolution in recently deglaciated terrain. Nature 408:161–166CrossRefGoogle Scholar
  19. Fritz SC, Anderson NJ (2013) The relative influences of climate and catchment processes on Holocene lake development in glaciated regions. J Paleolimnol 49:349–362CrossRefGoogle Scholar
  20. Grimm EC, Donovan JJ, Brown KJ (2011) A high-resolution mineral, pollen, and charcoal record of climatic variability and landscape response from Kettle Lake in the Northern Great Plains of North America. Quat Sci Rev 30:2626–2650CrossRefGoogle Scholar
  21. Hammer Ø, Harper DAT, Ryan PD (2001) PAST: paleontological statistics software package for education and data analysis. Palaeontol Electron 4:9Google Scholar
  22. Higuera PE, Brubaker LB, Anderson PM, Brown TA, Kennedy AT, Hu FS (2008) Frequent fires in ancient shrub tundra: implication of paleo-records for arctic environmental change. PLoS ONE 3:e0001744CrossRefGoogle Scholar
  23. Hobbs WO, Fritz SC, Stone JR, Donovan JJ, Grimm EC, Almendinger JE (2011) Environmental history of a closed-basin lake in the US Great Plains: diatom response to variations in groundwater flow regimes over the last 8500 cal yr BP. Holocene 21:1203–1216CrossRefGoogle Scholar
  24. Jacobs K, Whitlock C (2008) A 2000-year environmental history of Jackson Hole, Wyoming, inferred from lake-sediment records. West N Am Nat 68:350–364CrossRefGoogle Scholar
  25. Jin Z, Li F, Cao J, Wang S, Yu J (2006) Geochemistry of Daihai Lake sediments, Inner Mongolia, north China: implications for provenance, sedimentary sorting, and catchment weathering. Geomorphology 80:147–163CrossRefGoogle Scholar
  26. Koinig KA, Shotyk W, Lotter AF, Ohlendorf C, Sturm M (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. J Paleolimnol 30:307–320CrossRefGoogle Scholar
  27. Krause TR, Whitlock C (2013) Climate and vegetation change during the late-glacial/early-Holocene transition inferred from multiple proxy records from Blacktail Pond, Yellowstone National Park, USA. Quat Res 79:391–402CrossRefGoogle Scholar
  28. Krause TR, Lu Y, Whitlock C, Fritz S, Pierce KL (2015) Patterns of terrestrial and limnologic development in the northern Greater Yellowstone Ecosystem (USA) during the late-glacial/early-Holocene transition. Palaeogeogr Palaeoclimatol Palaeoecol 422:46–56CrossRefGoogle Scholar
  29. Kuehn SC, Froese DG, Carrara PE, Foit F, Pearce NJG, Rotheisler P (2009) Major and trace-element characterization, expanded distribution, and a new chronology for the latest Pleistocene Glacier Peak tephras in western North America. Quat Res 71:201–216CrossRefGoogle Scholar
  30. Kylander ME, Ampel L, Wohlfarth B, Veres D (2011) High-resolution X-ray fluorescence core scanning analysis of Les Echets (France) sedimentary sequence: new insights from chemical proxies. J Quat Sci 26:109–117CrossRefGoogle Scholar
  31. Licciardi JM, Pierce KL (2008) Cosmogenic exposure-age chronologies of Pinedale and Bull Lake glaciations in greater Yellowstone and the Teton Range, USA. Quat Sci Rev 27:814–831CrossRefGoogle Scholar
  32. Licciardi JM, Clark PU, Brook EJ, Elmore D, Sharma P (2004) Variable responses of western US glaciers during the last deglaciation. Geology 32:81–84CrossRefGoogle Scholar
  33. Lu Y (2014) Watershed and aquatic ecosystem evolution during the late-glacial and early-holocene inferred from high-resolution diatom and geochemical records in the Yellowstone Region. Ph.D. Thesis, University of Nebraska-LincolnGoogle Scholar
  34. Meyers PA, Teranes JL (2001) Sediment organic matter. In: Last WM, Smol JP (eds) Tracking environmental change using lake sediments, vol 2. Physical and geochemical methods. Kluwer Academic Publishers, Dordrecht, pp 239–269CrossRefGoogle Scholar
  35. Moreno A, Giralt S, Valero-Garces B, Saezc A, Baod R, Pregoe R, Pueyoc JJ, Gonzalez-Samperiza L, Tabernerb C (2007) A 14 kyr record of the tropical Andes: the Lago Chungará sequence (18°S, northern Chilean Altiplano). Quat Int 161:4–21CrossRefGoogle Scholar
  36. Morgan LA, Shanks WC III, Pierce KL (2009) Hydrothermal processes above a large magma chamber: large hydrothermal systems and hydrothermal explosions in Yellowstone National Park. Geol Soc Am Spec Pap 459:1–95Google Scholar
  37. Peinerud EK (2000) Interpretation of Si concentrations in lake sediments: three case studies. Environ Geol 40:64–72CrossRefGoogle Scholar
  38. Pierce KL (1979) History and dynamics of glaciations in the northern Yellowstone National Park area. US Geol Surv Prof Pap 729F:91Google Scholar
  39. Pierce KL (2004) Pleistocene glaciations of the Rocky Mountains. In: Gillespie A, Porter SC (eds) Developments in quaternary science, vol 1. Elsevier, Amsterdam, pp 63–76Google Scholar
  40. Pierce KL, Good JM (1990) Quaternary geology of Jackson Hole, Wyoming. In: Roberts SM (ed) Geologic field tours of western Wyoming and parts of adjacent Idaho, Montana, and Utah. Public Information Circular, number 29, Geological Survey of Wyoming, Laramie, Wyoming, USA, pp 127–138Google Scholar
  41. Reimer PJ, Bard E, Bayliss A, Beck JW, Blackwell PG, Ramsey CB, Buck CE, Cheng H, Edwards RL, Friedrich M, Grootes PM, Guilderson TP, Haflidason H, Hajdas I, Hatté C, Heaton TJ, Hoffmann DL, Hogg AG, Hughen KA, Kaiser KF, Kromer B, Manning SW, Niu M, Reimer RW, Richards DA, Scott EM, Southon JR, Staff RA, Turney CSM, van der Plicht J (2013) IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55:1869–1887CrossRefGoogle Scholar
  42. Saros JE, Anderson NJ (2015) The ecology of the planktonic diatom Cyclotella and its implications for global environmental change studies. Biol Rev 90:522–541CrossRefGoogle Scholar
  43. Shakun JD, Carlson AD (2010) A global perspective on Late Glacial Maximum to Holocene climate change. Quat Sci Rev 29:1801–1816CrossRefGoogle Scholar
  44. Thackray GD (2008) Varied climatic and topographic influences on Late Pleistocene glaciation in the western United States. J Quat Sci 23:671–681CrossRefGoogle Scholar
  45. Waddington JCB, Wright HE Jr (1974) Late Quaternary vegetational changes on the east side of Yellowstone Park, Wyoming. Quat Res 4:175–184CrossRefGoogle Scholar
  46. Westover KS, Fritz SC, Blyakharchuk TA, Wright HE Jr (2006) Diatom paleolimnological record of environmental change in the Altai Mountains, Siberia. J Paleolimnol 35:519–541CrossRefGoogle Scholar
  47. Wetzel RG (2001) Limnology of lake and river ecosystems, 3rd edn. Academic Press, San DiegoGoogle Scholar
  48. Whitlock C (1993) Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecol Monogr 63:173–198CrossRefGoogle Scholar
  49. Whitlock C, Bartlein PJ (1993) Spatial variations of Holocene climatic change in the Yellowstone region. Quat Res 39:231–238CrossRefGoogle Scholar
  50. Whitlock C, Dean WE, Fritz SC, Stevens LR, Stone JR, Power MJ, Rosenbaum JR, Pierce KL, Bracht-Flyr BB (2012) Holocene seasonal variability inferred from multiple proxy records from Crevice Lake, Yellowstone National Park, USA. Palaeogeogr Palaeoclimatol Palaeoecol 331–332:90–103CrossRefGoogle Scholar
  51. Wright HE Jr, Mann DH, Glaser PH (1983) Piston corers for peat and lake sediments. Ecology 65:657–659CrossRefGoogle Scholar
  52. Zeeb BA, Smol JP (2001) Chrysophyte scales and cysts. In: Smol JP, Birks HJB, Last WM (eds) Tracking environmental change using lake sediments. Algal and siliceous indicators, vol 3. Terrestrial. Kluwer Academic Publishers, Dordrecht, pp 203–223CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media B.V. 2017

Authors and Affiliations

  1. 1.Department of Earth and Atmospheric SciencesUniversity of Nebraska-LincolnLincolnUSA
  2. 2.Department of Earth and Environmental SystemsIndiana State UniversityTerre HauteUSA
  3. 3.Department of Earth SciencesMontana State UniversityBozemanUSA
  4. 4.Large Lakes ObservatoryUniversity of Minnesota-DuluthDuluthUSA

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