2018
DOI: 10.1038/s41598-018-26147-4
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Peatland vegetation composition and phenology drive the seasonal trajectory of maximum gross primary production

Abstract: Gross primary production (GPP) is a key driver of the peatland carbon cycle. Although many studies have explored the apparent GPP under natural light conditions, knowledge of the maximum GPP at light-saturation (GPPmax) and its spatio-temporal variation is limited. This information, however, is crucial since GPPmax essentially constrains the upper boundary for apparent GPP. Using chamber measurements combined with an external light source across experimental plots where vegetation composition was altered throu… Show more

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Cited by 52 publications
(50 citation statements)
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“…Our results support the importance of plant phenology as a regulator of seasonal GEP dynamics in peatlands (Järveoja et al, ; Linkosalmi et al, ; Peichl et al, , ). While the previous studies provided site‐specific insights, here we demonstrate that the observed relations hold across a range of different peatlands in various climate regions.…”
Section: Discussionsupporting
confidence: 90%
“…Our results support the importance of plant phenology as a regulator of seasonal GEP dynamics in peatlands (Järveoja et al, ; Linkosalmi et al, ; Peichl et al, , ). While the previous studies provided site‐specific insights, here we demonstrate that the observed relations hold across a range of different peatlands in various climate regions.…”
Section: Discussionsupporting
confidence: 90%
“…The importance of peatland vegetation species composition and plant‐specific phenology on GPP has been highlighted in a number of studies (e.g., Korrensalo et al, , Peichl et al, ). Here we find that the growing season started two weeks earlier at the evergreen plant‐dominated bog versus the deciduous plant‐dominated fen (where the growing season start was evaluated as the date daily GPP exceeded 10% of maximum daily GPP; Wu et al, ).…”
Section: Discussionmentioning
confidence: 99%
“…As major soil C stock (Yu et al, 2011), peatlands are expected to contribute to the majority of warming-induced soil C loss over the next century (Crowther et al, 2016). Plant photosynthesis strongly affects C balance of peatlands (Frolking et al, 1998), which in turn influence regional and global climates (Booth et al, 2012;Peichl et al, 2018). More particularly, photosynthesis of peatforming mosses (Sphagnum spp.)…”
mentioning
confidence: 99%