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Anne Ojala Timo Vesala, Jussi Huotari, Elina Peltomaa, Jukka Pumpanen, Pertti Hari Üllar Rannik, Tanja Suni, Sampo Smolander, Andrey Sogachev and Samuli Launiainen Department of Ecological and Environmental Sciences & Department of Physical Sciences 13 December 2007 HERC Carbon gas fluxes from a boreal lake
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Rationale of the study Boreal lakes can act as conduits of terrestrially fixed carbon Importance of catchment area -studies in Amazonas by Richey et al. (2002) -Hanson et al. (2004): 14% of NEE of the surrounding watershed can be mineralized and vented to the atmosphere via the lake Allochthonous vs. autochthonous carbon -DOC -Carbon source for heterotrophs -Microbial food webs Kyoto protocol
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Study site: Lake Valkea-Kotinen Pristine boreal lake Surface area 0.041 km 2 -Max depth 6.5 m, mean depth 2.5 m high content of DOC pH < 6 -inorganic carbon mostly in the form of CO 2 Headwater lake -Catchment area 0.30 km2 -Mainly old-growth forest A true reference lake !
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Characteristics of the lake: stratification Temperature (ºC) Short or incomplete spring turn over meromixis Steep summer stratification Complete autumn turn over Oxygen (g m -3 ) Anoxic hypolimnion (below 2.5 – 3 m) CH 4 production Autumn turn over 2003 2004
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Carbon gas measurements Continuous CO 2 flux measurements since summer 2002 Eddy Covariance (EC) Chamber measurements Measurements based on water column CO 2 concentrations Throughout the growing seasons Striking improvement in temporal resolution
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Results: Allochthonous carbon Precipitation 30% higher in 2004 than in 2003 peak in July DOC (mg C l -1 ) in surface water Clearly higher after July in 2004 Slow recovery -Carry over to the next growing season
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Results: CO 2 in the water column CO 2 concentration (mmol m -3 ) Stratification in summer Autumn turn over Higher in 2004 2003 2004
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Comparison of different methods Month µmol m -2 s -1 *C&C = estimate based on CO 2 concentration difference between the surface water and atmosphere
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Results: CO 2 fluxes based on EC measurements Seasonal pattern in CO 2 exchange -fluxes higher during the fall turn-over than during the spring turn-over -lowest fluxes in summer
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Results: Process parameters Community Respiration (R) and Primary Production (P) CO 2 production to consumption ratio (R to P) higher in 2004 than in 2003 Carry-over effect in 2005? R:P vs CO 2 flux
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CO 2 probes
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Surface water CO 2 concentration: seasonal dynamics
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Determination of CO 2 exchange in water g = CO 2 exchange rate C = CO 2 concentration F a = CO 2 flux from lake to the atmosphere F u = CO 2 flux from deep to surface
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Photosynthesis-irradiance response curves 6-10 September, 200611-15 September, 2006
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P-I Response Curve and Photosynthesis Estimate (submitted to Limnology and Oceanography: Methods) Fall photosynthetic rate: 0.35 g(CO 2 )m -2 day - 1 Daily respiration: 1.00 g(CO 2 )m -2 day - 1 NEE -0.65 g(CO 2 )m - 2 day -1 Lake appeared as a small source of CO 2
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Size-fractionated PP at surface Small microplankton (20-50 µm) dominated in spring (37-73 %) and autumn (79-96 %) Peridinium Large microplankton (> 50 µm) dominated (46-72 %) from the end of June till the end of September Gonyostomum
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Size-fractionated PP at 1,5 meter Picoplankton (0.2-2 µm) dominated (57-62 %) production in autumn zerozero
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Long-term changes in photosynthetic biomass Total biomass; decreasing trend (k = -1,4 x 10 -2 g m -3 a -1 ) Gonyostomum semen; decreasing trend (k = -2,4 x 10 -2 g m -3 a -1 )
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CO 2 fluxes from a larger lake: Lake Pääjärvi and an extreme weather event Summer time precipitation doubled >> a clear peak in CO 2 flux - Not due to in-lake biological processes, but imported from the catchment area FC = chamber measurement ΔCO2 = concentration gradient method
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Remarks Truly interdisciplinary research Techniques already in use in environmental physics and terrestrial ecology introduced to aquatic ecology True integration of studies on soil ecology and limnology Spin-off projects So far created the world’s longest EC data series on CO 2 exchange over a lake Extensive data sets on lake ecosystem ecology New insights on functioning of lake ecosystems on landscape level Not only DOC, but also CO 2
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