Skip to main content
Have a personal or library account? Click to login
Peat decomposition – shaping factors, significance in environmental studies and methods of determination; a literature review Cover

Peat decomposition – shaping factors, significance in environmental studies and methods of determination; a literature review

Open Access
|Apr 2016

References

  1. Aaby, B., 1976. Cyclic climatic variations in climate over the last 5500 years reflected in raised bogs.263, 281–284.
  2. Aaby, B., 1986. Palaeoecological studies of mires. [In:] B.E. Berglund (Ed.):. John Wiley & Sons, Chichester, 145–165.
  3. Aaby, B. & Berglund B.E., 1986. Characterization of peat and lake deposits. [In:] B.E. Berglund (Ed.):. John Wiley & Sons, Chichester, 231–246.
  4. Barber, K.E., 1981.. Balkema, Rotterdam, 219 pp.
  5. Barber, K., Dumayne-Peaty, L., Hughes, P., Mauquoy, D. & Scaife, R., 1998. Replicability and variability of the recent macrofossil and proxy-climate record from raised bogs: field stratigraphy and macrofossil data from Bolton Fell Moss and Walton Moss, Cumbria, England.13, 518–528.
  6. Benner, R., Fogel, M. L., Sprague, E. K. & Hodson, R. E., 1987. Depletion of c in lignin and its implications for stable carbon isotope studies.329, 708–710.
  7. Biester, H., Knorr, K.-H., Schellekens, J., Basler, A. & Y.-M. Hermanns, Y.-M., 2014. Comparison of different methods to determine the degree of peat decomposition in peat bogs.11, 2691–2707.
  8. Birks, H.J.B. & Birks, H.H., 1980.. Edward Arnold, London, 289 pp.
  9. Blackford, J.J., 1998. Holocene climatic variability in the North Atlantic region as shown by peat bog records.46, 155–162.
  10. Blackford, J.J., 2000. Palaeoclimatic records from peat bogs.15, 193–198.
  11. Blackford, J.J. & Chambers, F.M., 1991. Proxy records of climate from blanket mires: evidence for a Dark Age (1400 BP) climatic deterioration in the British Isles.1, 63–67.
  12. Blackford, J.J. & Chambers, F.M., 1993. Determining the degree of peat decomposition in peat-based palaeoclimatic studies.5, 7–24.
  13. Botch, M.S., 1978. Niekotoryje zakonomiernosti razlozjenija rastienij na bolotach kak osnova dinamiki bolot [Some regularities of plant decomposition in mires as a base for mire dynamics]. [In:] O.L. Liss (Ed.):[]. Izdatielstwo Moskovskowo Uniwiersitjeta, Moskva, 18–24.
  14. Botch, M.S. & Masing, V.V., 1979.[]. Nauka, Leningrad, 187 pp.
  15. Broder, T., Blodau, C., Biester, H. & Knorr, K.H., 2012. Peat decomposition records in three pristine ombrotrophic bogs in southern Patagonia.9, 1479–1491.
  16. Caseldine, C.J., Baker, A., Charman, D.J. & Hendon, D., 2000. A comparative study of optical properties of NaOH peat extracts: implications for humification studies.10, 649–658.
  17. Chambers, F.M., Barber, K.E., Maddy, D. & Brew, J., 1997. A 5500-year proxy-climate and vegetation record from blanket mire at talla moss, borders, Scotland.7, 391–399.
  18. Charman, D. J., Hendon, D. & Packman, S., 1999. Multiproxy surface wetness records from replicate cores on an ombrotrophic mire: Implications for Holocene palaeoclimate records.14, 451–463.
  19. Charman, D.J., Barber, K.E., Blaauw, M., Langdon, P.G., Mauquoy, D., Daley, T.J., Hughes, P.D.M. & Karofeld, E., 2009. Climate drivers for peatland palaeoclimate records.28, 1811–1818.
  20. Chiverrell, R.C., 2001. A proxy record of late Holocene climate change from May Moss, northeast England.16, 9–29.
  21. Clymo, R.S., 1984. The limits to peat bog growth.303, 605–654.
  22. Coulson, J.C. & Butterfield, J., 1978. An investigation of biotoc factors determining the rates of plant decomposition on blanket bog.66, 631–650.
  23. Davydik, I.I., 1987. An approach to the determination of the state of decomposition pf peat and other organic substances.2, 19–27.
  24. Drzymulska D. & Zieliński, P., 2013. Developmental changes in the historical and present-day trophic status of brown water lakes. Are humic water bodies a uniform aquatic ecosystem?33, 909–919.
  25. Drzymulska D., Kłosowski, S., Pawlikowski, P. & Zieliński, P. & Jabłońska, E. 2013. The historical development of vegetation of foreshore mires beside humic lakes; different successional pathways under various environmental conditions.703, 15–31.
  26. Ellis, C.J. & Tallis, J., 2000. Climatic control of blanket mire development at Kentra Moss, north-west Scotland.88, 869–889.
  27. Frazier, B.E. & Lee, G.B. 1971. Characteristics and classification of three Wisconsin histosols.35, 776–780.
  28. Gawlik, J., 1992.[]. Wydawnictwo IMUZ, Lublin – Falenty, 86 pp.
  29. Grosse-Brauckmann, G., 1986. Analysis of vegetative plant macrofossils. [In:] B.E. Berglund (Ed.):. John Wiley & Sons, Chichester, 591–618.
  30. Grosse-Brauckmann, G., 1990. Ablagerungen der Moore. [In:] K. Göttlich (Ed.):. Schweizerbart’sche Verlagsbuchhandlung, Stuttgart, 145–165.
  31. Grosse-Brauckmann, G., 1996. Classification of peat and peatbogs in Germany and its botanical, ecological and pedological foundations. [In:] G.W. Lüttig (Ed.):Proceedings of the 10International Peat Congress, Bremen, Vol. 2. E. Schweizerbart’sche Verlagsbuchhandlung, Stuttgart, 21–38.
  32. Hornibrook, E.R.C., Longstaffe, F.J., Fyfe, W.S. & Bloom, Y., 2000. Carbon-isotope ratios and carbon, nitrogen and sulfur abundances in flora and soil organic matter from a temperate-zone bog and marsh.34, 237–245.
  33. Jasnowski, M., 1957.Kindb. w układzie stratygraficznym i florze torfowisk holoceńskich Polski [Kindb. in startygraphy and flora of the Holocene mires of Poland].26, 701–718.
  34. Jones, M.C., Peteet, D.M. & Sambrotto, R., 2010. Late-Glacial and Holocene δ15n and δ13c variation from a Kenai Peninsula, Alaska peatland.293, 132–143.
  35. Klavins, M., Sire, J., Purmalis, O. & Melecis, V., 2008. Approaches to estimating humification indicators for peat.3, 1–15.
  36. Kuhry, P. & Vitt, D.H., 1996. Fossil carbon/nitrogen ratios as a measure of peat decomposition.77, 271–275.
  37. Lubliner-Mianowska, K., 1951.[]. Państwowe Wydawnictwo Techniczne, Katowice, 88 pp.
  38. Maciak, F. & Liwski, S., 1979.[]. Skrypty SGGW, Akademii Rolniczej w Warszawie, Warszawa, 159 pp.
  39. Maksimow, A., 1965.[]. PWRiL, Warszawa, 395 pp.
  40. Malmer, N. & Wallén, B., 2004. Input rates, decay losses and accumulation rates of carbon in bogs during the last millennium: Internal processes and environmental changes.14, 111–117.
  41. Mathur, S.P. & Farnham, R.S., 1985. Geochemistry of humic substances in natural and cultivated peatlands. [In:] G.R. Aiken, D.M. McKnight, R.L. Wershaw & P. MacCarthy (Eds):. John Wiley & Sons, New York, 53–86.
  42. Mauquoy, D. & Barber, K., 2002. Testing the sensitivity of the palaeoclimatic signal from ombrotrophic peat bogs in northern England and the Scottish Borders.119, 219–240.
  43. Nilssen, E. & Vorren, K.D., 1991. Peat humification and climate history.71, 215–217.
  44. Obidowicz, A., 1975. Entstehung und Alter einiger Moore im nördlichen Teil der Hohen Tatra.21, 3, 289–466.
  45. Obidowicz, A., 1990. Eine Pollenanalytische und Moorkundliche Studie zur Vegetationsgeschichte des Podhale-Gebietes (West-Karpaten).30, 147–219.
  46. Oświt, J., 1977. Naturalne siedliska torfotwórcze jako podstawa wyróżniania jednostek przyrodniczych [Natural peat-forming habitats].79, 29–50.
  47. Oświt, J. & Żurek, S., 1981. Rekonstrukcja rozwoju zabagnień w pradolinie Biebrzy.134, 59–70.
  48. Rydin, H. & Jeglum, J., 2008.. Oxford University Press, Oxford, 343 pp.
  49. Skrzypek, G., Kałużny, A., Wojtuń, B. & Jędrysek, M.-O., 2007. The carbon stable isotopic composition of mosses: A record of temperature variation.38, 1770–1781.
  50. Stanek, W. & Silc, T., 1977. Comparisons of four methods for determination of degree of peat humification (decomposition) with emphasis on the von Post method.57, 109–117.
  51. Tobolski, K., 2000.[]. Wydawnictwo Naukowe PWN, Warszawa, 508 pp.
  52. Troels-Smith, J., 1955. Karakterisering af løse jordarter [Characterization of loose soils].IV, Reakke 3,10, 1–73.
  53. Yeloff, D. & Mauquoy, D., 2006. The influence of vegetation composition on peat humification: Implications for palaeoclimatic studies.35, 662–673.
  54. van der Linden, M. & van Geel, B., 2006. Late Holocene climate change and human impact recorded in a south Swedish ombrotrophic peat bog.240, 649–667.
  55. Varlygin, P. D. & Minkina, C.I., 1949. Polevoj sposób opredelenija stepeni razlozienija torfa – syrca posredstvom mazkov [Field method of determination of peat decomposition degree by smears].3, 21–23.
  56. Żurek, S., Michczyńska, D.J. & Pazdur, A., 2002. Time record of palaeohydrologic changes in the development of mires during the Late Glacial and Holocene, North Podlasie Lowland and Holy Cross Mts.21, 109–118.
DOI: https://doi.org/10.1515/logos-2016-0005 | Journal eISSN: 2080-6574 | Journal ISSN: 1426-8981
Language: English
Page range: 61 - 69
Submitted on: Mar 6, 2015
Accepted on: Feb 1, 2016
Published on: Apr 18, 2016
Published by: Adam Mickiewicz University
In partnership with: Paradigm Publishing Services

© 2016 Danuta Drzymulska, published by Adam Mickiewicz University
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.