Searching for an ecological baseline

Long-term ecology of a post-extraction restored bog in Northern Estonia

Datos Bibliográficos

ID14980686
AutoresDominika Łuców (0000-0001-9966-7478), Martin Küttim (0000-0002-8879-2422), Michał Słowiński (0000-0002-3011-2682), Piotr Kołaczek (0000-0003-2552-8269), Monika Karpińska-Kołaczek, Liisa Küttim (0000-0003-0238-3714), Meryt Salme, Mariusz Lamentowicz (0000-0003-0429-1530)
Año2022
Volumen607
Páginas65-78
Fecha de publicación2022-01-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaQuaternary International (JOURNAL)
Identificadores de la revistaISSN: 1040-6182 • E-ISSN: 1873-4553
EditorialElsevier BV (PUBLISHER)
DOI10.1016/j.quaint.2021.08.017
OpenAlexW3198753779
IdiomaEN
Citas recibidas2
Referencias citadas84

The exploitation of peatlands in Estonia, which began in the 17th century, has degraded them to a great extent. Consequently, cutover and drained peatlands have become the sources of CO2. Global warming has led to a need for policies focusing on the protection and restoration of drained and degraded peatlands. Hence, to compare the effect/progress of restoration with the past pristine ecosystem baseline before the peatland was destroyed by cutting, we examined a peat core from North Estonia using chronology based on 14C by analyzing several proxies in high resolution including testate amoebae, plant macrofossils, pollen, non-pollen palynomorphs, and diatoms. The results revealed a striking ecological contrast between the pristine (ca. 2 kyrs) and restored state (currently) of the peatland. The pristine state was characterized by a domination of Sphagnum fuscum/rubellum and Archerella flavum, suggesting that extraction area of Hara peatland was a wet and stable ombrotrophic bog. As a result of peat exploitation, deposits comprising the last ca. 2 kyrs were cut. In turn an important feature of the restored section of the peat core was the domination of a green algae (Chlorophyta) and Eriophorum vaginatum as well as testate amoebae species Arcella discoides, which is considered an indicator of hydrological instability. The main difference between the predisturbed and restored parts of the peat core section was that a minor cover of peat-forming Sphagnum and mixotrophic testate amoebae was present in the top inundated part. We state that a healthy raised bog—the target of restoration—should consist abundant mixotrophic testate amoebae such as Archerella flavum and Hyalosphenia papilio which are good indicators of a well-functioning Sphagnum bog ecosystem even if the Sphagnum species differ from the reconstructed ecological baseline conditions. Our study highlights the extensive damage caused to the peat-forming ombrotrophic peatland by extraction and how difficult, challenging, and time-consuming is the process of ecological restoration

Biology · Bog · Macrofossil · Ombrotrophic · Peat · Pollen · Sphagnum · Testate amoebae · Coastal wetland ecosystem dynamics · Geology and Paleoclimatology Research · Peatlands and Wetlands Ecology · Ecology