Small peatland with a big story: 600-year paleoecological and historical data from a kettle-hole peatland in Western Russia

Author:

Mroczkowska Agnieszka12ORCID,Kittel Piotr2ORCID,Marcisz Katarzyna3ORCID,Dolbunova Ekaterina4,Gauthier Emilie5,Lamentowicz Mariusz3,Mazurkevich Andrey4,Obremska Milena6,Płóciennik Mateusz7,Kramkowski Mateusz8,Łuców Dominika13ORCID,Kublitskiy Yuriy9,Słowiński Michał1ORCID

Affiliation:

1. Past Landscape Dynamics Laboratory, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Poland

2. University of Lodz, Faculty of Geographical Sciences, Department Geology and Geomorphology, Poland

3. Climate Change Ecology Research Unit, Adam Mickiewicz University, Poland

4. The State Hermitage Museum, Russia

5. UMR CNRS 6249, Laboratoire de Chrono-Environnement, Université Bourgogne Franche-Comté, France

6. Institute of Geological Sciences, Polish Academy of Sciences, Poland

7. Department of Invertebrate Zoology and Hydrobiology, University of Lodz, Poland

8. Department of Environmental Resources and Geohazards, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Poland

9. Herzen State Pedagogical University of Russia, Russia

Abstract

Peatlands are important records of past environmental changes. Based on a multiproxy analysis, the main factors influencing the evolution of a peatland can be divided into autogenic and allogenic. Among the important allogenic factors, apart from climate change, are deforestation and drainage, which are directly associated with human impact. Numerous consequences arise from these processes, the most important of which are physical and chemical denudation in the catchment and the related hydrological disturbances in the catchment and peatland. The present study determined how human activities and the past climatic variability mutually influenced the development of a small peatland ecosystem. The main goals of the study were: (1) to trace the local changes of the peatland history over the past 600 years, (2) to investigate their relationship with changes in regional hydroclimate patterns, and (3) to estimate the sensitivity of a small peatland to natural and human impact. Our reconstructions were based on a multiproxy analysis, including the analysis of pollen, macrofossils, Chironomidae, Cladocera, and testate amoebae. Our results showed that, depending on the changes in water level, the history of peatland can be divided into three phases as follows: 1/the phase of stable natural conditions, 2/phase of weak changes, and 3/phase of significant changes in the catchment. Additionally, to better understand the importance of the size of catchment and the size of the depositional basin in the evolution of the studied peatland ecosystem, we compared data from two peatlands – large and small – located close to each other. The results of our study indicated that “size matters,” and that larger peatlands are much more resilient and resistant to rapid changes occurring in the direct catchment due to human activities, whereas small peatlands are more sensitive and perfect as archives of environmental changes.

Funder

Narodowe Centrum Nauki

Publisher

SAGE Publications

Subject

Paleontology,Earth-Surface Processes,Ecology,Archeology,Global and Planetary Change

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