Hydrological changes in the Rzecin peatland (Puszcza Notecka, Poland) induced by anthropogenic factors: Implications for mire development and carbon sequestration
| Autor: | Mariusz Lamentowicz, Krystyna Milecka, Jan Barabach, Tomasz Goslar, Barbara Fiałkiewicz-Kozieł, Bogdan H. Chojnicki, Grzegorz Kowalewski, Mariusz Gałka |
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| Rok vydání: | 2016 |
| Předmět: |
010506 paleontology
Archeology Global and Planetary Change geography Peat geography.geographical_feature_category 010504 meteorology & atmospheric sciences Ecology Paleontology Macrofossil Wetland Carbon sequestration 01 natural sciences Habitat Mire Poor fen Environmental science Ecosystem 0105 earth and related environmental sciences Earth-Surface Processes |
| Zdroj: | The Holocene. 27:651-664 |
| ISSN: | 1477-0911 0959-6836 |
| Popis: | Wetlands are very vulnerable ecosystems and sensitive to changes in the ground water table. For the last few thousand years, hydrological balance has also been influenced by human activity. To improve their cropping features, drainage activity and fertilizing were applied. The drainage process led to an abrupt change of environment, the replacement of plant communities and the entire ecosystem. The problem of carbon sequestration is very important nowadays. A higher accumulation rate is related to higher carbon accumulation, but the intensity of carbon sequestration depends on the type of mire, habitat, and climatic zone. The main aim of this article was an examination of the changes in poor-fen ecosystem during the last 200 years in relation to natural and anthropogenic factors, using paleoecological methods (pollen and macrofossils). The second aim was a detailed investigation of the sedimentary record to aid our understanding of carbon sequestration in the poor fen of temperate zone. This case study shows that fens in temperate zones, in comparison with boreal ones, show higher carbon accumulation rates which have been especially intensive over the last few decades. To reconstruct vegetation changes, detailed palynological and macrofossil analyses were done. A 200-year history of the mire revealed that it was influenced by human activity to much degree. However, despite the nearby settlement and building of the drainage ditch, the precious species and plant communities still occur. |
| Databáze: | OpenAIRE |
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