Pattern of large raised bog formation in the South-Eastern Baltic Region during the Holocene: the case of Kaliningrad oblast
- 作者: Napreenko-Dorokhova T.1, Napreenko M.2, Lisitzin A.3
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隶属关系:
- Shirshov Institute of Oceanology, Atlantic Branch
- Immanuel Kant Baltic Federal University
- Shirshov Institute of Oceanology
- 期: 卷 475, 编号 2 (2017)
- 页面: 900-906
- 栏目: Geography
- URL: https://journals.rcsi.science/1028-334X/article/view/190490
- DOI: https://doi.org/10.1134/S1028334X17080050
- ID: 190490
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详细
The results of complex investigations that have been carried out since 2007 in large bog ecosystems (Zehlau, Bolshoe Mokhovoe, and Koz’e) located in Kaliningrad oblast in two largest landscape areas, glaciolacustrine plains in the central part of the region and coastal lowlands of the southern coast of Curonian Lagoon and the delta of the Neman River, are presented. It is established that the intensive development of mires and their transition to the raised bog stage occurred in the territory of Kaliningrad oblast later than in most of the forest zone in European Russia, where this process was noted as early as during the Atlantic. On the glaciolacustrine flat plains in the central part of Kaliningrad oblast, where there were no deep depressions, the mire formation process was manifested weakly for a long time. A colder and more humid climate, which is a condition necessary for the raised bog peat accumulation and rapid expansion of bogs to the adjacent forest area, occurred only in the Subatlantic.
作者简介
T. Napreenko-Dorokhova
Shirshov Institute of Oceanology, Atlantic Branch
编辑信件的主要联系方式.
Email: tnapdor@gmail.com
俄罗斯联邦, Kaliningrad
M. Napreenko
Immanuel Kant Baltic Federal University
Email: tnapdor@gmail.com
俄罗斯联邦, Kaliningrad
A. Lisitzin
Shirshov Institute of Oceanology
Email: tnapdor@gmail.com
俄罗斯联邦, Moscow