The role of plant phenology as a regulator for gross ecosystem productivity (GEP) in peatlands is empirically not well constrained. This is because proxies to track vegetation development with daily coverage at the ecosystem scale have only recently become available and the lack of such data has hampered the disentangling of biotic and abiotic effects. This study aimed at unraveling the mechanisms that regulate the seasonal variation in GEP across a network of eight European peatlands. Therefore, we described phenology with canopy greenness derived from digital repeat photography and disentangled the effects of radiation, temperature and phenology on GEP with commonality analysis and structural equation modeling. The resulting relational network could not only delineate direct effects but also accounted for possible effect combinations such as interdependencies (mediation) and interactions (moderation). We found that peatland GEP was controlled by the same mechanisms across all sites: phenology constituted a key predictor for the seasonal variation in GEP and further acted as a distinct mediator for temperature and radiation effects on GEP. In particular, the effect of air temperature on GEP was fully mediated through phenology, implying that direct temperature effects representing the thermoregulation of photosynthesis were negligible. The tight coupling between temperature, phenology and GEP applied especially to high latitude and high altitude peatlands and during phenological transition phases. Our study highlights the importance of phenological effects when evaluating the future response of peatland GEP to climate change. Climate change will affect peatland GEP especially through changing temperature patterns during plant phenologically sensitive phases in high latitude and high altitude regions.
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Sci Total Environ
January 2025
Department of Hydrology, Meteorology and Water Management, Institute of Environmental Engineering, Warsaw University of Life Sciences-SGGW, ul Nowoursynowska 166, 02-787 Warsaw, Poland.
With their net carbon accumulation determined by the balance between gross ecosystem productivity (GEP) and carbon losses (from processes such as oxidation and decomposition), peatlands can function as either carbon sinks or carbon sources. Healthy, pristine peatlands are vital carbon sinks, while degraded peatlands can release significant amounts of carbon (C) into the atmosphere. This study investigates the use of peat vertical displacement (VD), detectable via remote sensing, as a proxy for net carbon accumulation in northern boreal and temperate peatlands.
View Article and Find Full Text PDFNew Phytol
February 2023
Laboratoire Ecologie Fonctionnelle et Environnement (LEFE), Université Paul Sabatier, CNRS, F-31000, Toulouse, France.
Plants produce a wide diversity of metabolites. Yet, our understanding of how shifts in plant metabolites as a response to climate change feedback on ecosystem processes remains scarce. Here, we test to what extent climate warming shifts the seasonality of metabolites produced by Sphagnum mosses, and what are the consequences of these shifts for peatland C uptake.
View Article and Find Full Text PDFGlob Chang Biol
February 2020
Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå, Sweden.
The role of plant phenology as a regulator for gross ecosystem productivity (GEP) in peatlands is empirically not well constrained. This is because proxies to track vegetation development with daily coverage at the ecosystem scale have only recently become available and the lack of such data has hampered the disentangling of biotic and abiotic effects. This study aimed at unraveling the mechanisms that regulate the seasonal variation in GEP across a network of eight European peatlands.
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