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Peat

  • Richard Lindsay
  • Roxane Andersen
Reference work entry

Abstract

Peat is a soil consisting of semi-decomposed plant material which accumulates in situ as a result of waterlogging. The percentage of mineral matter contained within such soils can vary from as little as 2% by weight to as much as 30%, though even this upper limit is more an agreed convention than any strict biological threshold. Peat can be generated from a wide range of plant materials under various forms of waterlogging. The orderly nature of peat layers, which may attain depths of 40 m or more and which may have accumulated over periods as long as 100,000 years, offer much of interest to palaeobotanists and archaeologists, particularly as the processes which result in the preservation of plant material also preserve other objects, such as human remains. The carbon stored in the world’s peatlands exceeds that which is stored in all the world’s vegetation.

Keywords

Bog Bog butter Carbon Fen Histosol Mire Mosses Peat Peatland Plants Pollen Preservation Soil Tollund Man Von Post Waterlogging 

References

  1. Clymo RS. Peat. In: Gore AJP, editor. Ecosystems of the world 4A. Mires: swamp, bog, fen and moor. Amsterdam: Elsevier; 1983. p. 159–224.Google Scholar
  2. Davidson NC. How much wetland has the world lost? Long-term and recent trends in global wetland area. Mar Freshw Res. 2014;65:934–41.CrossRefGoogle Scholar
  3. Fischer C. Tollund man – gift to the gods [English edition]. Stroud: The History Press; 2012.Google Scholar
  4. Glob PV. The bog people: iron age man preserved [English edition]. London: Faber and Faber; 1969.Google Scholar
  5. Hobbs NB. Mire morphology and the properties and behaviour of some British and foreign peats. Q J Eng Geol. 1986;19:7–80.CrossRefGoogle Scholar
  6. Joosten H, Clarke D. Wise use of mires and peatlands. Totness/Devon: NHBS/International Mire Conservation Group and International Peat Society; 2002.Google Scholar
  7. Pennington W. Vegetation history in the North West of England: a regional synthesis. In: Walker D, West RG, editors. Studies in the vegetational history of the British Isles. Cambridge: Cambridge University Press; 1970. p. 41–80.Google Scholar
  8. Ramsar website for Nakaikemi-shicchi. https://rsis.ramsar.org/ris/2057. Accessed 9 Mar 2015.
  9. Santos L, Romani JRV, Jalut G. History of vegetation during the Holocene in the Courel and Queixa Sierras, Galicia, northwest Iberian Peninsula. J Quat Sci. 2000;15(6):621–32.CrossRefGoogle Scholar
  10. Scharlemann JPW, Tanner EVJ, Heiderer R, Kapos V. Global soil carbon: understanding and managing the terrestrial carbon pool. Carbon Manag. 2014;5(1):81–91. doi:10.4155/cmt.13.77.CrossRefGoogle Scholar
  11. Troels-Smith J. Characterisation of unconsolidated sediments. Geological Survey of Denmark. IV. Series Vol. 3, No. 10. København: Forlag and Sandal; 1955.Google Scholar

Copyright information

© Springer Science+Business Media B.V., part of Springer Nature 2018

Authors and Affiliations

  1. 1.Sustainability Research InstituteUniversity of East LondonLondonUK
  2. 2.Environmental Research InstituteUniversity of the Highlands and IslandsThursoUK

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