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CARBON BALANCE OF A BOREAL BOG DURING A YEAR WITH AN EXCEPTIONALLY DRY SUMMER
Author(s) -
Alm Jukka,
Schulman Leif,
Walden Jari,
Nykänen Hannu,
Martikainen Pertti J.,
Silvola Jouko
Publication year - 1999
Publication title -
ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.144
H-Index - 294
eISSN - 1939-9170
pISSN - 0012-9658
DOI - 10.1890/0012-9658(1999)080[0161:cboabb]2.0.co;2
Subject(s) - ombrotrophic , bog , sphagnum , peat , environmental science , lawn , eddy covariance , mire , ecosystem respiration , moss , growing season , ecology , atmospheric sciences , ecosystem , biology , geology
Northern peatlands are important terrestrial carbon stores, and they show large spatial and temporal variation in the atmospheric exchange of CO 2 and CH 4 . Thus, annual carbon balance must be studied in detail in order to predict the climatic responses of these ecosystems. Closed‐chamber methods were used to study CO 2 and CH 4 in hollow, Sphagnum angustifolium lawn, S. fuscum lawn, and hummock microsites within an ombrotrophic S. fuscum bog. Micrometeorological tower measurements were used as a reference for the CH 4 efflux from the bog. Low precipitation during May–August in 1994 (84 mm below the long‐term average for the same period) and a warm July–August period caused the water table to drop by more than 15 cm below the peat surface in the hollows and to 48 cm below the surface in high hummocks. Increased annual total respiration exceeded gross production and resulted in a net C loss of 4–157 g/m 2 in the different microsites. Drought probably caused irreversible desiccation in some lawns of S. angustifolium and S. balticum and in S. fuscum in the hummocks, while S. balticum growing in hollows retained its moisture and even increased its photosynthetic capacity during the July–August period. Seasonal (12 May–4 October) CH 4 emissions ranged from 2 g CH 4 ‐C/m 2 in drier S. fuscum hummocks and lawns to 7 and 14 g/m 2 in wetter S. angustifolium–S. balticum lawns and hollows, respectively. Aerodynamic gradient measurements at the tower showed slightly higher CH 4 flux rates than the average estimates for the whole bog obtained by closed‐chamber methods. Winter C efflux comprised 30 g CO 2 ‐C/m 2 and 1 g CH 4 ‐C/m 2 out of a total loss of 90 g C/m 2 on average in the bog, and there was an estimated annual loss of 7 g C/m 2 by leaching. This study shows how delicately the boreal bog’s C balance in different microsites depends on climatic variations, especially the distribution of precipitation. It also confirms that severe C losses can occur in boreal bogs during extended summer droughts, even in years with annual temperatures close to the long‐term average and with precipitation clearly greater than the long‐term average.