Pollution of Lakes and Rivers Chapter 4: Retrieving the sedimentary archive and establishing the geochronological clock: collecting and dating sediment.

Slides:



Advertisements
Similar presentations
1 Radio Maria World. 2 Postazioni Transmitter locations.
Advertisements

Trend for Precision Soil Testing % Zone or Grid Samples Tested compared to Total Samples.
AGVISE Laboratories %Zone or Grid Samples – Northwood laboratory
5.1 Rules for Exponents Review of Bases and Exponents Zero Exponents
Soil Exploration Part II
Nuclear Chemistry and Radioactivity
/ /17 32/ / /
Reflection nurulquran.com.
Worksheets.
1 Copyright © 2013 Elsevier Inc. All rights reserved. Chapter 4 Computing Platforms.
Summative Math Test Algebra (28%) Geometry (29%)
The questions will be read automatically, if you want to hear it again click on the speaker. 0.
Chapter 7: Steady-State Errors 1 ©2000, John Wiley & Sons, Inc. Nise/Control Systems Engineering, 3/e Chapter 7 Steady-State Errors.
LESSON 10 – Earth’s History: Estimating Geologic Time
Water in the West: Current Use and Future Challenges Christopher Goemans, Ph.D. Agricultural and Resource Economics 13 th Annual Farmers Cooperatives Conference.
17. Radiometric dating and applications to sediment transport William Wilcock OCEAN/ESS 410.
Dating Techniques Four Categories –Radio-isotope methods –Paleomagnetic methods –Organic/inorganic chemical methods –Biological methods.
Radiocarbon 14-C is a radioactive isotope of carbon.
Radiocarbon Dating of Groundwater
PALAEONTOLOGY The study of fossils © 2008 Paul Billiet ODWSODWS.
... or how to make sense out of Ch. 8 of the text... Prehistoric Cultures Tim Roufs section ©2009 Class Slides Set 10A Special Skills Used to Study Early.
Radiometric Dating and Half Life
Radiometric Dating Timothy G. Standish, Ph. D..
II. Why Do We Study Fossils Found in Rocks?
Chapter 8 Section 2 Handout
Earth Science Chapter 21 Section 3
Earth’s History.
Radiocarbon age-modelling I – introduction to age-models
II. Why Do We Study Fossils Found in Rocks?
Relative and Absolute Dating
Mr. Karns Biology Fossils.
Outine 17-1: The Fossil Record
21.3 – Absolute-Age Dating Objectives
THE GEOLOGIC TIME SCALE: THE HISTORY OF EARTH
Relative and Absolute Dating
College Algebra & Trigonometry
Fossil Evidence for Evolution
Exponential Growth or Decay Function
Copyright © 2010 Pearson Education Canada. 6.1 Chapter 6 Openness in Goods and Financial Markets The Short Run Power Point Presentation Brian VanBlarcom.
History of Critical Loads meetings – how have we gotten to this point? Andrzej Bytnerowicz 1, Rich Fisher 2 and Al Riebau 3 USDA Forest Service 1 Pacific.
Determining Absolute Age
2011 WINNISQUAM COMMUNITY SURVEY YOUTH RISK BEHAVIOR GRADES 9-12 STUDENTS=1021.
2011 FRANKLIN COMMUNITY SURVEY YOUTH RISK BEHAVIOR GRADES 9-12 STUDENTS=332.
Slide R - 1 Copyright © 2009 Pearson Education, Inc. Publishing as Pearson Prentice Hall Active Learning Lecture Slides For use with Classroom Response.
Resistência dos Materiais, 5ª ed.
Physics for Scientists & Engineers, 3rd Edition
Paleolimnology as a Tool for Interpreting Ecosystem Changes within Freshwater Lakes Heather Burgess1, Andrea Lini1, Milt Ostrofsky2, Suzanne Levine3, Neil.
Basic concepts (Early Diagenesis, chapters 2-3) Transport and Physical properties Sedimentation without diagenesis (reactions that alter solid composition.
Multi-Proxy Reconstructions of Environmental Change for a Small Glacial Lake in Northern Manitoba, Canada Pooja Shakya 1, Erin York 2, Mark Kruger 3 Faculty.
Dating models using man-made radionuclides Part 1: 137 Cs flux, vertical profiles and inventories Roberta Delfanti ENEA –La Spezia, Italy 1 IAEA Regional.
Reservoir Paleolimnology Paul Gremillion, Ph.D., P.E. Civil & Environmental Engineering Northern Arizona University Nelson Reservoir,
VARVE CHRONOLOGY Lakes can produce annual layers. Usually occur in glacial lakes or those that freeze over in winter. Coarser sediments are deposited in.
Soils Investigation Soil Investigation
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix.
Discovering Past Climates
Mercury Dynamics In Sub-Arctic Lake Sediments Across A Methane Ebullition Gradient Lance Erickson 1, M. Florencia Meana-Prado 2.
21.3 – Absolute Age Dating. Absolute Age Dating Enables scientists to determine the numerical age of rocks and other objects.
Climate Changes Past and Future. Defining Climate Change  Response of Earth-atmosphere system to changes in boundary conditions  What external factors.
Preserving the Scientific Record: Case Study 2 – Arctic Temperature Variability Matthew Mayernik National Center for Atmospheric Research Version 1.0 Review.
A 500- YR RECORD OF N ORTHERN P ATAGONIAN ENVIRONMENTAL CHANGES : L AGO P LOMO AND L AGO B ERTRAND N. Fagel 1,2, J. Brix 1, M. El Ouahabi 1, G. Lepoint.
Preserving the Scientific Record: Case Study 2 – Arctic Temperature Variability Data Matthew Mayernik National Center for Atmospheric Research Version.
Radiocarbon Based Paleoseismic Dating
Pollution of Lakes and Rivers Chapter 3: Sediments: an ecosystem’s memory Copyright © 2008 by DBS.
Paleoclimate Team Dr. Peter Wigand, Adam Herrera, Katie Irwin, Robert Kelty, Joseph Scott SJVRocks!! CSUBakersfield Department of Geological Sciences.
Visualizing Earth Science By Z. Merali and B. F. Skinner Chapter 10 – How Old is Old? The Rock Record and Deep Time.
SOIL MECHANICS AND FOUNDATION ENGINEERING-II (CE 311)
How old is old?. Earth Processes take a really, really, really (really) long time….. So, the question is – How do we know how old something is? Especially.
Geologic Time. The Geologic Time Scale  A summary of major events in Earth’s past that are preserved in the rock record  Divisions of Geologic Time.
Earth’s Materials and Processes-Part 3 Fossils & Relative Dating
Earth’s Materials and Processes-Part 3 Fossils & Relative Dating
Presentation transcript:

Pollution of Lakes and Rivers Chapter 4: Retrieving the sedimentary archive and establishing the geochronological clock: collecting and dating sediment cores Copyright © 2008 by DBS

Contents Collecting and dating sediment cores Retrieving and sampling sediment profiles Setting the time scale: geochronological methods Correlating multiple cores from the same basin The top/bottom approach: snapshots of environmental change The paleolimnologists option of setting the most appropriate scale

Retrieving the Sedimentary Archive Collecting and Dating Sediment Cores What is required? –A sedimentary sequence that is the correct length, resolution and quality –An accurate depth-time profile

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Fieldwork – what is it like? Requires planning Criteria for good recovery –No disturbance of structure –No change in water content or void ratio –No change in constituent chemistry Dealing with variable composition –Sites differ markedly in their morphology/climate etc. –Composition may vary within the lake (basin to basin)

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Commonly used approaches: Glew, J., Smol, J.P. and Last, W.M. (2001) Sediment core collection and extrusion. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Long cores: Leroy, S.A.G. and Colman, S.M. (2001) Coring and drilling equipment and procedures for recovery of long lacustrine sediment sequences. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Choosing the coring site Would like continuous, representative and undisturbed samples Single cores - take many weeks/months to analyze Not an issue since replicate cores show very good reproducibility (Charles et al., 1991) Ideal: flat, central and deep basin –Bathymetric maps –Technology (depth soundings etc.) Things to avoid –Steep morphometric gradients (slumping) –Shallow areas (prone to mixing)

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Coring platform Cores are taken through the water column From a boat, platform or ice cover Coring equipment Figure 4.1. Collecting surface lake sediments using a small diameter Glew (1991) gravity corer from the pontoons of a helicopter in Arctic Canada.

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Coring equipment Last 100 years contained in 50 cm (N. America) (cf. fast accumulation) More ancient histories contained in cores 2 m or longer Recent sediments are unconsolidated > 90 % water Short Cores (Surface Sediments) Open-barrel gravity corers (plastic tubes) –Close-on-contact type (line tension) –Messenger-operated

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Surface sediments Freeze-crust samplers (Renberg, 1981, Verchuren, 2000) Designed to preserve chemistry of the sediment-water interface Figure 4.3. General operation of a freeze- crust sampler. Inset: Corer chamber is filled with dry ice and a coolant, such as alcohol. The corer top is secured. A: Corer is lowered through the water column B: Corer is lowered into the sediment, sediment freezes to the corer C: Sediment-encrusted corer brought to the surface.

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Long Cores Livingstone corer –Rod driven piston corer Figure 4.4. Simplified diagram showing the basic principles used in piston coring. A) To recover an undisturbed core sample, the corer is positioned at the sediment surface B) The piston held stationary, while the core tube is pushed past it into the sediment using the coring rod. C) The core section is recovered to the surface, with the core tube and piston locked together. The sealing of the piston in the core tube prevents any tendency for the sample to slide out or for the core material to be deformed.

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Kullenberg –Cable-operated Livingstone corer –For deep water Figure 4.5. General operation of a Livingstone-type piston corer, showing the lowering (A), sampling (B), and withdrawal (C) of a sediment sequence. The operator uses the drive rods to push the corer into the sediment to the desired depth. A cable, also held by the operator, keeps the piston in place. From Glew et al. (2001); used with permission.

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Long Cores Mackereth compressed air piston corer (Mackereth, 1958; 1969) See Glew et al., 2001

Retrieving the Sedimentary Archive Retrieving and Sampling Sediment Profiles Sediment Sectioning Photography Choice of division may be based on visible mixing Should be sectioned lake-side / ASAP

Retrieving the Sedimentary Archive Setting the Time Scale: Geochronological methods Radioisotopic techniques –Measure decay of naturally occurring radioisotopes – 210 Pb (t 1/2 = 22.3 yrs) most commonly used (for recent sediments ~150 yrs) 210 Pb Dating –Supported 210 Pb (in-situ decay of 238 U) –Unsupported 210 Pb (from atmosphere) (= total 210 Pb – Supported 210 Pb) Assumptions: Rate of deposition of unsupported 2 10 Pb is constant Transfer of 210 Pb from the water column to sediments No disturbances: mixing/additions from catchment inflows

Retrieving the Sedimentary Archive Setting the Time Scale: Geochronological methods

210 Pb dating example ln (unsupported 210 Pb activity) Depth (cm) 0 Pb x x Pb 0 t = 1 ln( 210 Pb 0 / 210 Pb x ) λ Slope; m = - λ / a Where a = sedimentation rate

Retrieving the Sedimentary Archive Setting the Time Scale: Geochronological methods Other radioisotopic indicators – 137 Cs from bomb tests and Chernobyl (also 241 Am) –Peaks in 1954, 1958, 1962 (Test ban treaty, 1986) Appleby, 2001

Retrieving the Sedimentary Archive Setting the Time Scale: Geochronological methods 14 C used for longer sequences production via cosmic rays 1 0 n N 14 6 C H Atmospheric 14 C is found in 14 CO 2 Incorporated into plants where it decays –Whilst alive 14 C/ 12 C ratio is constant –After death 14 C no longer replaced from environment –Useful for about 7 half-lives t 1/2 = 5,730 yr

Retrieving the Sedimentary Archive Setting the Time Scale: Geochronological methods Pollen chronologies –Introduction, proliferation and demise of plant species –e.g. Ambrosia (ragweed) ~ European settlement Episodic events –e.g. volcanic ash from known eruptions (Tephrachronology) –e.g. Charcoal from forest fires Other anthropogenic time markers –Chemicals from anthropogenic activity

Retrieving the Sedimentary Archive Setting the Time Scale: Geochronological methods Annually laminated sediments (varves) –Similar to tree rings –Very few varve forming lakes Figure 4.9. Annual couplets (varves) of sediment from Nicolay Lake, Nunavut, Arctic Canada. Photograph taken by S. Lamoureux.

Retrieving the Sedimentary Archive The Top/Bottom Approach: Snapshots of Environmental Change Time consuming to analyze every layer With multiple lakes + cores the no. of samples increases before and after type questions do not require entire core e.g. are lakes currently more acidic than 1850s? Cumming et al., 1992

Retrieving the Sedimentary Archive The Paleolimnologists Option of Setting the Most Appropriate Time Scale Ecosystems change and respond to stress over varying time-scales Paleolimnology allows the scientists to set their own time-scale

Retrieving the Sedimentary Archive Summary Collection and dating is a crucial first part of any study 210 Pb most common dating technique for recent sediments Top/bottom approach may be used if detailed analysis not required

References Anderson, T.W. (1974) The chestnut pollen decline as a time horizon in lake sediments in eastern North America. Canadian Journal of Earth Sciences, Vol. 11, pp Appleby, P.G. (1993) Foreward to the lead-210 dating anniversary series. Journal of Paleolimnology, Vol. 9, pp Appleby, P.G. (2001) Chronostratigraphic techniques in recent sediments. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Appleby, P.G. and Oldfield, F. (1978) The calculation of 210 Pb dates assuming a constant rate of supply of unsupported 210 Pb to the sediment. Catena, Vol. 5, pp Appleby, P.G., Richardson, N. and Nolan, P.J. (1991) 241 Am dating of lake sediments. Hydrobiolgia, Vol. 214, pp Bennett, K.D. and Willis, K.J. (2001) Pollen. In Smol, J.P., Birks, H.J.B. and Last, W.M. (eds.) Tracking Environmental Change using Lake Sediments, Volume 3, Terrestrial, Algal, and Silaceous Indicators. Kluwer Academic Publishers, Dordrecht, pp Birks, H.H. (2001) Plant macrofossils. In Smol, J.P., Birks, H.J.B. and Last, W.M. (eds.) Tracking Environmental Change using Lake Sediments, Volume 3, Terrestrial, Algal, and Silaceous Indicators. Kluwer Academic Publishers, Dordrecht, pp

References Björck, S. and Wohlfarth, B. (2001) 14 C chronostratigraphic techniques in paleolimnology. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Blais, J.M., Kalff, J., Cornett, R.J. and Evans R.D. (1995) Evaluation of 210 Pb dating in lake sediments using stable Pb, Ambrosia pollen, and 137 Cs. Journal of Paleolimnology, Vol. 13, pp Boyle, J.F. (1995) A simple closure mechanism for a compact, large-diameter gravity corer. Journal of Paleolimnology, Vol. 13, pp Brinkhurst, R.O., Chua, K.E. and Batoosingh, E. (1969) Modifications in sampling procedures applied to studies on the bacteria and tubified oligochaetes inhabiting aquatic sediments. Journal of the Fisheries Research Board of Canada, Vol. 26, pp Charles, D.F., Dixit, S.S., Cumming, B.F. and Smol, J.P. (1991) Variability in diatom and chrysophyte assemblages and inferred pH: paleolimnological studies of Big Moose L., N.Y. Journal of Paleolimnology, Vol. 5, pp Cumming, B.F., Smol, J.P., kingston, J.C., Charles, D.F., Birks, H.J.B., Camburn, K.E., Dixit, S.S., Uutala, A.J. and Selle, A.R. (1992) How much acidification has occurred in Adriondack region (New York, USA) lakes since preindustrial times? Canadian Journal of Fisheries and Aquatic Sciences, Vol. 49, pp Cumming, B.F., Glew, J.R., Smol, J.P. and Norton, S.A. (1993) Comment on Core compression and surficial sediment loss of lake sediments of high porosity caused by gravity coring (Crusius and Anderson). Limnology and Oceanography, Vol. 38, pp

References Damon, E., Donahue, D.J., Gore, B.H., Hatheway, A.L., Jull, A.J.T., Linick, W., Sercel, P.J., Toolin, A.J., Bronk, C.R., Hall, E.T., Hedges, E.M., Housley, R., Law, I.A., perry, C., Bonani, G., Trumbore, S., Woelfli, W., Ambers, J.C., Bowman, G.E., Leese, M.N. and Tite, M.S. (1989) Radiocarbon dating of the Shroud of Turin. Nature, Vol. 337, pp Davidson, G.A. (1988) A modified tape-peel technique for preparing permanent qualitative microfossil slides. Journal of Paleolimnology, Vol. 1, pp Davis, R.B., Hess, C.T., Norton, S.A., hanson, D.W., Hoagland, K.D. and Andreson, D.S. (1984) 137 Cs and 210 Pb dating of sediments from soft-water lakes in New England (U.S.A.) and Scandinavia, a failure of 137Cs dating. Chemical Geology, Vol. 44, pp Dixit, S.S., Dixit, A.S. and Smol, J.P. (1992) Assessment of changes in lake water chemistry in Sudbury area lakes since preindustrial times. Canadian Journal of Fisheries and Aquatic Sciences, Vol. 49, pp Foster, D.L., Mighall, T.M., Proffitt, H., Walling, D.W. and Owens, P.N. (2006) Post- depositional 137Cs mobility in the sediments of three shallow coastal lagoons, SW England. Journal of Paleolimnology, Vol. 35, pp Glew, J. (1988) A portable extruding device for close interval sectioning of unconsolidated core samples. Journal of Paleolimnology, Vol. 1, pp Glew, J. (1989) A new trigger mechanism for sediment samplers. Journal of Paleolimnology, Vol. 2, pp Glew, J. (1991) Miniature gravity corer for recovering short sediment cores. Journal of Paleolimnology, Vol. 5, pp

References Glew, J. (1995) Conversion of shallow water gravity coring equipment for deep water operation. Journal of Paleolimnology, Vol. 14, pp Glew, J., Smol, J.P. and Last, W.M. (2001) Sediment core collection and extrusion. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Hvorslev (1949) Subsurface Exploration and Sampling Soils for Civil Engineering Purposes. Vicksburg, MI: American Society of Civil Engineers. Waterways Experiment Station, Corps of Engineering Purposes, U.S. Army. Kajak, Z., Kacprzak, K. and Polowski, R. (1965) Chwytacz rurowy do pobierania préb dna. Ekologia Polska Seria B, Vol. 11, pp Kansanen, P.H., Jaakkola, T., Kulmala, S. and Suutarinen, R. (1991) Sedimentation and distribution of gamma-emitting radionuclides in bottom sediments of southern lake Päijänne, Finalnd after the Chernobyl accident. Hydrobiologia, Vol. 222, pp Kemp, A.E.S., Dean, J., Pearce, R.B. and Pike, J. (2001) Recognition and analysis of bedding and sediment fabric features. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 2, Physical and Geochemical Methods. Kluwer Academic Publishers, Dordrecht, pp Kilby, G.W. and Batley, G.E. (1993) Chemical indicators of sediment chronology. Australian Journal of marine and Freshwater Research, Vol. 44, pp

References Krisnaswami, S., Lal, D., Martin, J.M. and Meybeck, M. (1971) Geochronology of lake sediments. Earth and Planetary Science Letters, Vol. 11, pp Kullenberg, B. (1947) The piston core sampler. Svenska Hydrografisk-Biologiska Kommissionens, Skrifter III, Hydrograpfi, Vol. 1, pp Lamoureux, S. (2001) Varve chronology techniques. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Last, W.M. and Smol, J.P. (eds.) (2001) Tracking Environmental Change using Lake Sediments, Volume 2, Physical and Geochemical Methods. Kluwer Academic Publishers, Dordrecht. Leroy, S.A.G. and Colman, S.M. (2001) Coring and drilling equipment and procedures for recovery of long lacustrine sediment sequences. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Livingstone, D.A. (1955) A lightweight piston sampler for lake deposits. Ecology, Vol. 36, pp MacDonald, G.M., Beukens, R.P., Kieser, W.E. and Vitt, D.H. (1991) Comparative radiocarbon dating of terrestrial plant macrofossils and aquatic moss from the ice-free corridor of western Canada. Geology, Vol. 15, pp

References Mackereth, F.J.H. (1958) A portable core sampler for lake deposits. Limnology and Oceanography, Vol. 3, pp Mackereth, F.J.H. (1969) A short core sampler for subaqueous deposits. Limnology and Oceanography, Vol. 14, pp Oldfield. F. and Appleby, P.G. (1984) Empirical testing of 210 Pb-dating models for lake sediments. In Haworth, E.Y. and Lund, J.W.G. (eds.), Lake Sediments and Environmental History. University of Minnesota Press, Minneapolis, pp Pennington, W., Cambray, R.S. and Fisher, E.M. (1973) Observations on lake sediments using fallout 137 Cs as a tracer. Nature, Vol. 242, pp Renberg, I. (1981) Improved methods for sampling, photographing and varve-counting of varved lake sediments. Boreas, Vol. 10, pp Renberg, I. and Wik, M. (1984) Dating of recent lake sediments by soot article counting. Verhandlungen der Internationalen Vereinigung von Limnologen, Vol. 22, pp Renberg, I. (1991) The HON-Kajak sediment corer. Journal of Paleolimnology, Vol. 6, pp

References Robins, J.A. (1978) Geochemical and geophysical applications of radioactive lead. In Nriagu, J.O. (ed.), Biogeochemistry of Lead in the Environment. Elsevier Scientific, Amsterdam, pp Rose. N. (2001) Fly-ash particles. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 2, Physical and Geochemical Methods. Kluwer Academic Publishers, Dordrecht, pp Saarinen, T. and Petterson, G. (2001) Image analysis techniques. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 2, Physical and Geochemical Methods. Kluwer Academic Publishers, Dordrecht, pp Scholz, C.A. (2001) Applications of seismic sequence stratigraphy in lacustrine basins. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Simola, H. (1977) Diatom succession in the formation of annually laminated sediment in Lovojärvi, a small eutrophicated lake. Annals Botanica Fennici, Vol. 18, pp Simola, H., Hanski, I. and Liukkonen, M. (1990) Stratigraphy, species richness and seasonal dynamics of planktonic diatoms during 418 years in Lake Lovojärvi,, South Finalnd. Annals Botanica Fennici, Vol. 27, pp Smol, J.P. and Dickman, M.D. (1981) The recent histories of three Canadian Shield lakes: a paleolimnological experiment. Archiv für Hydrobiologie, Vol. 93, pp

References Stephenson, M., Klaverkamp, J., Motycka, M., baron, C. and Schwartz, W. (1996) Coring artifacts and contaminant inventories in lake sediment. Journal of Paleolimnology, Vol. 15, pp Stuiver, M., Reimer, P.J., Bard, E. et al. (1998) INTCAL98 radiocarbon age calibration, 24,000-0 cal BP. Radiocarbon, Vol. 40, pp Turney, C.S.M. and Lowe, J.J. (2001) Teprochronology. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp Verschuren, D. (2000) Freeze coring soft sediments in tropical lakes. Journal of Paleolimnology, Vol. 24, pp Whitlock, C. and Larsen, C.P.S. (2001) Charcoal as a fire proxy. In Smol, J.P., Birks, H.J.B. and Last, W.M. (eds.) Tracking Environmental Change using Lake Sediments, Volume 3, Terrestrial, Algal, and Silaceous Indicators. Kluwer Academic Publishers, Dordrecht, pp Wright, H.E. Jr. (1990) An improved Hongve sampler for surface sediments. Journal of Paleolimnology, Vol. 4, pp Wright, H.E. Jr. (1991) Coring tips. Journal of Paleolimnology, Vol. 6, pp Zolitschka, B., Mingram, J., van der Gaast, S., Jansen, J.H.F. and Naumann, R. (2001) Sediment logging techniques. In Last, W.M. and Smol, J.P. (eds.), Tracking Environmental Change using Lake Sediments, Volume 1, Basin Analysis, Coring, and Chronological Techniques. Kluwer Academic Publishers, Dordrecht, pp