Spatially varying peatland initiation, Holocene development, carbon accumulation patterns and radiative forcing within a subarctic fen

• Published in: Quaternary Science Reviews
• Main Authors: Piilo, Sanna, Korhola, Atte, Heiskanen, Lauri, Tuovinen, Juha-Pekka, Aurela, Mika, Juutinen, Sari, Marttila, Hannu, Saari, Markus, Tuittila, Eeva-Stiina, Turunen, Jukka, Väliranta, Minna
• Other Authors: Helsinki Institute of Sustainability Science (HELSUS), Environmental Change Research Unit (ECRU), Ecosystems and Environment Research Programme, Environmental Sciences, Department of Forest Sciences
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier Scientific Publ. Co 2022
• Subjects: 1171 Geosciences; Aapa mire; Carbon dynamics; Lateral expansion; Autogenic succession; Paleoecology; Vegetation dynamics; Climate variation; High latitudes; CLIMATE-CHANGE; TEMPERATURE VARIABILITY; BOREAL PEATLAND; SHORT-TERM; NORTHERN; DYNAMICS; FINLAND; MIRES; DIOXIDE; Northern Finland; Subarctic
• Online Access: http://hdl.handle.net/10138/349660

High latitude peatlands act as globally important carbon (C) sinks and are in constant interaction with the atmosphere. Their C storage formed during the Holocene. In the course of time, the aggregate effect of the C fluxes on radiative forcing (RF) typically changes from warming to cooling, but the timing of this shift varies among different peatlands. Here we investigated Holocene peatland development, including vegetation history, vertical peat growth and the lateral expansion of a patterned subarctic fen in northern Finland by means of multiple sampling points. We modelled the Holocene RF by combining knowledge on past vegetation communities based on plant macrofossil stratigraphies and present in situ C flux measurements. The peatland initiated at ca. 9500 calibrated years Before Present (cal yr BP), and its lateral expansion was greatest between ca. 9000 and 7000 cal yr BP. After the early expansion, vertical peat growth proceeded very differently in different parts of the peatland, regulated by internal and external factors. The pronounced surface microtopography, with high strings and wet (larks, started to form only after ca. 1000 cal yr BP. C accumulation within the peatland recorded a high degree of spatial variability throughout its history, including the recent past. We applied two flux scenarios with different interpretation of the initial peatland development phases to estimate the RF induced by C fluxes of the fen. After ca. 4000 cal yr BP, at the latest, the peatland RF has been negative (cooling), mainly driven by C uptake and biomass production, while methane emissions had a lesser role in the total RF. Interestingly, these scenarios suggest that the greatest cooling effect took place around ca. 1000 cal yr BP, after which the surface microtopography established. The study demonstrated that despite the high spatial heterogeneity and idiosyncratic behaviour of the peatland, the RF of the studied fen followed the general development pattern of more southern peatlands. Holocene climate variations ...