Holocene Development and Permafrost History of the Usinsk Mire, Northeast European Russia

• Published in: Géographie physique et Quaternaire
• Main Authors: Oksanen, Pirita O., Kuhry, Peter, Alekseeva, Rimma N.
• Format: Text
• Language: English
• Published: Les Presses de l'Université de Montréal 2003
• Subjects: Usinsk; palsa; palsas; Peat; Pechora; permafrost; taiga; pergélisol
• Online Access: http://id.erudit.org/iderudit/011312ar; https://doi.org/10.7202/011312ar

This study discusses Holocene vegetation succession, permafrost dynamics and peat accumulation in the Usinsk mire, located in the Pechora lowlands of Northeast European Russia. At present, the area is situated in the extreme northern taiga subzone near the southern limit of permafrost. Reconstructions are based on plant macrofossil analysis, physico-chemical analysis and AMS (accelerator mass spectrometry) radiocarbon dating of two peat profiles investigated in detail. Additional information is available from seven other sites. Organic accumulation started at ca. 11 350 BP (14C yrs). Terrestrialization of ponds was the most common pathway for mire initiation. During a large part of their history, the sites have been Cyperaceae-dominated fens. A change into Sphagnum-dominated ecosystems is recorded at 3700-3000 BP. Permafrost became established around 2300 BP, although first signs of embryonic palsa formation can be tentatively traced back to about 2900 BP. Palsas and peat plateaus have experienced several periods of freezing and entire or partial thawing. The extant permafrost stages are young. The long-term carbon accumulation rate in the investigated sites is 19 g/m2/yr. The average rate of carbon accumulation in the dynamic permafrost stage is 23 g/m2/yr. Cette étude discute de la succession de la végétation, de la dynamique du pergélisol et de l'accumulation de la tourbe à l'Holocène dans la tourbière d'Usinsk, située dans les basses terres de Pechora, au nord-est de la Russie d’Europe. La région se trouve dans l'extrême nord de la taïga actuelle, près de la limite méridionale du pergélisol. Les reconstitutions sont fondées sur l'analyse macrofossile des plantes, l'analyse physico-chimique et les dates au radiocarbone déterminées par spectrométrie de masse à l’aide d’un accélérateur de particules (SMA) de deux profils de tourbe étudiés en détail. De l'information additionnelle provient de sept autres sites. L'accumulation de matière organique a commencé vers 11 350 BP (années 14C). L’accumulation de tourbe ...