Article

Article name LATE-HOLOCENE MIRE HYDROLOGY RECONSTRUCTION: CHALLENGES IN APPLYING PROXIES OF SURFACE WETNESS FOR NON-SPHAGNUM PEAT DEPOSITS
Authors

Natalia G. Mazei, PhD, Senior Researcher, Department of Physical Geography and Landscape Science, Faculty of Geography, Lomonosov Moscow State University (119991, Russia, Moscow, Leninskie Gory 1); iD ORCID: https://orcid.org/0000-0002-4759-8703; e-mail: natashamazei@mail.ru
Andrey N. Tsyganov, PhD, Leading Researcher, Department of General Ecology and Hydrobiology, Faculty of Biology, Lomonosov Moscow State University (119991, Russia, Moscow, Leninskie Gory 1, building 12); iD ORCID: https://orcid.org/0000-0002-5660-8432; e-mail: tsyganovan@my.msu.ru
Elena Y. Novenko, Dr.Sc., Main Researcher, Department of Quaternary Paleogeography, Institute of Geography of RAS (119017, Russia, Moscow, Staromonetny Lane, 29); Professor, Faculty of Geography and Geoinformation Technology, Higher School of Economics University (101000, Russia, Moscow, Myasnitskaya str., 20); iD ORCID: https://orcid.org/0000-0003-2174-8467; e-mail: lenanov@mail.ru
Daria A. Avdeeva, MSc Student, Department of Physical Geography and Landscape Science, Faculty of Geography, Lomonosov Moscow State University (119991, Russia, Moscow, Leninskie Gory 1); iD ORCID: https://orcid.org/0000-0002-5885-6683; e-mail: avdeevadasha1804@yandex.ru
Kirill V. Babeshko, PhD, Senior Researcher, Department of General Ecology and Hydrobiology, Faculty of Biology, Lomonosov Moscow State University (119991, Russia, Moscow, Leninskie Gory 1, building 12); Senior Researcher, Faculty of Biology, Shenzhen MSU-BIT University, (518172, China, Shenzhen, International University Park Road, 1); iD ORCID: https://orcid.org/0000-0003-4557-4908; e-mail: fytark@yandex.ru
Dmitry A. Kupriyanov, Junior Researcher, Department of Quaternary Paleogeography, Institute of Geography of RAS (119017, Russia, Moscow, Staromonetny Lane, 29); iD ORCID: https://orcid.org/0000-0003-1441-4039; e-mail: dmitriykupriyanov1994@yandex.ru
Mikhail S. Paramonov, PhD student, Department of General Ecology and Hydrobiology, Faculty of Biology, Lomonosov Moscow State University (119991, Russia, Moscow, Leninskie Gory 1, building 12); iD ORCID: https://orcid.org/0000-0003-3916-4849; e-mail: paramis00@mail.ru
Damir A. Saldaev, PhD, Senior Researcher, Department of General Ecology and Hydrobiology, Faculty of Biology, Lomonosov Moscow State University (119991, Russia, Moscow, Leninskie Gory 1, building 12); Professor, Faculty of Biology, Shenzhen MSU-BIT University, (518172, China, Shenzhen, International University Park Road, 1); iD ORCID: https://orcid.org/0000-0002-4044-2562; e-mail: k-brom@yandex.ru
Ping Ding, Senior Engineer, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou (510640, China, Guangzhou, Kehua str. 511); iD ORCID: https://orcid.org/0000-0003-3018-4720; e-mail: pingding0915@163.com
Yuri A. Mazei, Dr.Sc., Corresponding member of Russian Academy of Sciences, Professor, Department of General Ecology and Hydrobiology, Faculty of Biology, Lomonosov Moscow State University (119991, Russia, Moscow, Leninskie Gory 1, building 12); iD ORCID: https://orcid.org/0000-0002-5443-8919; e-mail: yurimazei@mail.ru

Reference to article

Mazei N.G., Tsyganov A.N., Novenko E.Y., Avdeeva D.A., Babeshko K.V., Kupriyanov D.A., Paramonov M.S., Saldaev D.A., Ding P., Mazei Y.A. 2026. Late-Holocene mire hydrology reconstruction: challenges in applying proxies of surface wetness for non-Sphagnum peat deposits. Nature Conservation Research 11(2): 67–81. https://dx.doi.org/10.24189/ncr.2026.013

Electronic Supplement 1. Additional information to the paper by Mazei et al. (2026) (Link)

Section Research articles
DOI https://dx.doi.org/10.24189/ncr.2026.013
Abstract

Understanding the long-term dynamics of hydrological changes in mire ecosystems is critical for predicting their responses to climate changes and managing carbon-rich peat deposits. This study reconstructs the late-Holocene hydrological dynamics of a mire at the southern boundary of the mixed forests of the East European Plain, with a focus on non-Sphagnum (consisting of wood and grass remains) peats. We apply a multiproxy approach, utilising plant macrofossil analysis, testate amoeba assemblages, and peat humification measurements as proxies of past moisture conditions. The data reveal that the main changes in vegetation cover over the last 3000 years correspond well to climatic variation. However, the agreement among the hydrological reconstructions based on three proxies was good only at the initial stage of peat accumulation and greatly reduced with the predominance of trees in vegetation cover. Moreover, our findings show that Sphagnum-dominated peats of an adjacent mire were characterised by a better agreement among hydrological proxies. Overall, despite the agreement among various proxies can vary depending on the type of peat deposits, an application of a multi-proxy approach can reveal complimentary aspects of the hydrological regime variation in mires.

Keywords

forest fires, Mordovia State Nature Reserve, palaeoecological proxies, Pavlovskoe mire, peat humification, peatland, plant macrofossils, testate amoebae

Artice information

Received: 12.08.2025. Revised: 15.12.2025. Accepted: 17.02.2026.

The full text of the article
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