Peat multi-proxy data from Männikjärve bog as indicators of Late Holocene climate changes in Estonia

U. Sillasoo, Dmitri Mauquoy, A. Blundell, D. Charman, M. Blaauw, J. R. G. Daniell, P. Toms, J. Newberry, F. M. Chambers, E. Karofeld

Research output: Contribution to journalArticle

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Abstract

As part of a wider project on European climate change over the past 4500 years, a 4.5-m peat core was taken from a lawn microform on Mannikjarve bog, Estonia. Several methods were used to yield proxy-climate data: (i) a quadrat and leaf-count method for plant macrofossil data, (ii) testate amoebae analysis, and (iii) colorimetric determination of peat humification. These data are provided with an exceptionally high resolution and precise chronology. Changes in bog surface wetness were inferred using Detrended Correspondence Analysis (DCA) and zonation of macrofossil data, particularly concerning the occurrence of Sphagnum balticum, and a transfer function for water-table depth for testate amoebae data. Based on the results, periods of high bog surface wetness appear to have occurred at c. 3100, 3010-2990, 2300, 1750-1610, 1510, 14 10, 1110, 540 and 3 10 cal. yr BP, during four longer periods between c. 3170 and 2850 cal. yr BP, 2450 and 2000 cal. yr BP, 1770 and 1530 cal. yr BP and in the period from 880 cal. yr BP until the present. In the period between 1770 and 1530 cal. yr BP. the extension or initiation of a hollow microtope occurred, which corresponds with other research results from Mannikjarve bog. This and other changes towards increasing bog surface wetness may be the responses to colder temperatures and the predominance of a more continental climate in the region, which favoured the development of bog microdepressions and a complex bog microtopography. Located in the border zone of oceanic and continental climatic sectors, in an area almost without land uplift, this study site may provide valuable information about changes in palaeohydrological and palaeoclimatological conditions in the northern parts of the eastern Baltic Sea region.

Original languageEnglish
Pages (from-to)20-37
Number of pages17
JournalBoreas
Volume36
Issue number1
DOIs
Publication statusPublished - Jan 2007

Keywords

  • atmospheric circulation
  • environmental-change
  • raised bogs
  • record
  • moss
  • temperature
  • macrofossil
  • deposits
  • hollows
  • England

Cite this

Sillasoo, U., Mauquoy, D., Blundell, A., Charman, D., Blaauw, M., Daniell, J. R. G., ... Karofeld, E. (2007). Peat multi-proxy data from Männikjärve bog as indicators of Late Holocene climate changes in Estonia. Boreas, 36(1), 20-37. https://doi.org/10.1111/j.1502-3885.2007.tb01177.x

Peat multi-proxy data from Männikjärve bog as indicators of Late Holocene climate changes in Estonia. / Sillasoo, U.; Mauquoy, Dmitri; Blundell, A.; Charman, D.; Blaauw, M.; Daniell, J. R. G.; Toms, P.; Newberry, J.; Chambers, F. M.; Karofeld, E.

In: Boreas, Vol. 36, No. 1, 01.2007, p. 20-37.

Research output: Contribution to journalArticle

Sillasoo, U, Mauquoy, D, Blundell, A, Charman, D, Blaauw, M, Daniell, JRG, Toms, P, Newberry, J, Chambers, FM & Karofeld, E 2007, 'Peat multi-proxy data from Männikjärve bog as indicators of Late Holocene climate changes in Estonia', Boreas, vol. 36, no. 1, pp. 20-37. https://doi.org/10.1111/j.1502-3885.2007.tb01177.x
Sillasoo, U. ; Mauquoy, Dmitri ; Blundell, A. ; Charman, D. ; Blaauw, M. ; Daniell, J. R. G. ; Toms, P. ; Newberry, J. ; Chambers, F. M. ; Karofeld, E. / Peat multi-proxy data from Männikjärve bog as indicators of Late Holocene climate changes in Estonia. In: Boreas. 2007 ; Vol. 36, No. 1. pp. 20-37.
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abstract = "As part of a wider project on European climate change over the past 4500 years, a 4.5-m peat core was taken from a lawn microform on Mannikjarve bog, Estonia. Several methods were used to yield proxy-climate data: (i) a quadrat and leaf-count method for plant macrofossil data, (ii) testate amoebae analysis, and (iii) colorimetric determination of peat humification. These data are provided with an exceptionally high resolution and precise chronology. Changes in bog surface wetness were inferred using Detrended Correspondence Analysis (DCA) and zonation of macrofossil data, particularly concerning the occurrence of Sphagnum balticum, and a transfer function for water-table depth for testate amoebae data. Based on the results, periods of high bog surface wetness appear to have occurred at c. 3100, 3010-2990, 2300, 1750-1610, 1510, 14 10, 1110, 540 and 3 10 cal. yr BP, during four longer periods between c. 3170 and 2850 cal. yr BP, 2450 and 2000 cal. yr BP, 1770 and 1530 cal. yr BP and in the period from 880 cal. yr BP until the present. In the period between 1770 and 1530 cal. yr BP. the extension or initiation of a hollow microtope occurred, which corresponds with other research results from Mannikjarve bog. This and other changes towards increasing bog surface wetness may be the responses to colder temperatures and the predominance of a more continental climate in the region, which favoured the development of bog microdepressions and a complex bog microtopography. Located in the border zone of oceanic and continental climatic sectors, in an area almost without land uplift, this study site may provide valuable information about changes in palaeohydrological and palaeoclimatological conditions in the northern parts of the eastern Baltic Sea region.",
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AU - Blundell, A.

AU - Charman, D.

AU - Blaauw, M.

AU - Daniell, J. R. G.

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AB - As part of a wider project on European climate change over the past 4500 years, a 4.5-m peat core was taken from a lawn microform on Mannikjarve bog, Estonia. Several methods were used to yield proxy-climate data: (i) a quadrat and leaf-count method for plant macrofossil data, (ii) testate amoebae analysis, and (iii) colorimetric determination of peat humification. These data are provided with an exceptionally high resolution and precise chronology. Changes in bog surface wetness were inferred using Detrended Correspondence Analysis (DCA) and zonation of macrofossil data, particularly concerning the occurrence of Sphagnum balticum, and a transfer function for water-table depth for testate amoebae data. Based on the results, periods of high bog surface wetness appear to have occurred at c. 3100, 3010-2990, 2300, 1750-1610, 1510, 14 10, 1110, 540 and 3 10 cal. yr BP, during four longer periods between c. 3170 and 2850 cal. yr BP, 2450 and 2000 cal. yr BP, 1770 and 1530 cal. yr BP and in the period from 880 cal. yr BP until the present. In the period between 1770 and 1530 cal. yr BP. the extension or initiation of a hollow microtope occurred, which corresponds with other research results from Mannikjarve bog. This and other changes towards increasing bog surface wetness may be the responses to colder temperatures and the predominance of a more continental climate in the region, which favoured the development of bog microdepressions and a complex bog microtopography. Located in the border zone of oceanic and continental climatic sectors, in an area almost without land uplift, this study site may provide valuable information about changes in palaeohydrological and palaeoclimatological conditions in the northern parts of the eastern Baltic Sea region.

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KW - environmental-change

KW - raised bogs

KW - record

KW - moss

KW - temperature

KW - macrofossil

KW - deposits

KW - hollows

KW - England

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