Abstract
Background and aims
Northern peatlands are large repositories of carbon. Peatland vascular plant community composition has been functionally associated to a set of biogeochemical processes such as carbon cycling. Yet, we do not fully understand to what extent vascular plant functional types (PFTs) affect the quality of dissolved organic matter, and if there is any feedback on soil microbial activity.
Methods
Using a longer–term plant removal experiment in a boreo–nemoral peatland in Southern Sweden, we relate the dominance of different vascular plant functional types (i.e. ericoids and graminoids) to the chemistry of the dissolved organic matter (DOM) and microbial enzymatic activities (fluorescein diacetate hydrolysis, FDA).
Results
Our results show that PFTs modifies the composition of DOM moieties, with a decrease of low molecular weight organic compounds after vascular plant removal. The decrease of enzymatic activity by up to 68 % in the plant removal plots suggests a reduction in DOM mineralization in the absence of vascular plants.
Conclusions
Our results show that plant–derived low molecular organic compounds enhance peatland microbial activity, and suggest that an increase of vascular plant cover in response to climate change can potentially destabilize the OM in peatlands, leading to increased carbon losses.
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References
Albrecht R, Ziarelli F, Alarcón Gutiérrez E, et al. (2008) 13C solid-state NMR assessment of decomposition pattern during co-composting of sewage sludge and green wastes. Eur J Soil Sci 59:445–452
Albrecht R, Verrecchia E, Pfeifer HR (2015) The use of solid-phase fluorescence spectroscopy in the characterisation of organic matter transformations. Talanta 134:453–459
Biasi C, Rusalimova O, Meyer H, et al. (2005) Temperature-dependent shift from labile to recalcitrant carbon sources of Arctic heterotrophs. Rapid Commun Mass Spectrom 19:1401–1408
Biester H, Knorr KH, Schellekens J, et al. (2014) Comparison of different methods to determine the degree of peat decomposition in peat bogs. Biogeosciences 11:2691–2707
Bird JA, Herman DJ, Firestone MK (2011) Rhizosphere priming of soil organic matter by bacterial groups in a grassland soil. Soil Biol Biochem 43:718–725
Blagodatskaya Е, Kuzyakov Y (2008) Mechanisms of real and apparent priming effects and their dependence on soil microbial biomass and community structure: critical review. Biol Fertil Soils 45:115–131
Bloor JMG, Bardgett RD (2012) Stability of above-ground and below-ground processes to extreme drought in model grassland ecosystems: interactions with plant species diversity and soil nitrogen availability. Perspect Plant Ecol, Evol Systemetics 14:193–204
Bragazza L, Parisod J, Buttler A, Bardgett RD (2013) Biogeochemical plant-soil microbe feedback in response to climate warming in peatlands. Nat Clim Chang 3:273–277
Bragazza L, Bardgett RD, Mitchell EAD, Buttler A (2015) Linking soil microbial communities to vascular plant abundance along a climate gradient. New Phytol 205:1175–1182
Breeuwer A, Robroek BJM, Limpens J, et al. (2009) Decreased summer water table depth affects peatland vegetation. Basic Appl Ecol 10:330–339
Breeuwer A, Heijmans MMPD, Robroek BJM, Berendse F (2010) Field simulation of global change: transplanting northern bog mesocosms southward. Ecosystems 13:712–726
Bret-Harte MS, García EA, Sacré VM, et al. (2004) Plant and soil responses to neighbour removal and fertilization in Alaskan tussock tundra. J Ecol 92:635–647
Bro R, Kiers HAL (2003) A new efficient method for determining the number of components in PARAFAC models. J Chemom 17:274–286
Broder T, Blodau C, Biester H, Knorr KH (2012) Peat decomposition records in three pristine ombrotrophic bogs in southern Patagonia. Biogeosciences 9:1479–1491
Bubier JL, Moore TR, Bledzki LA (2007) Effects of nutrient addition on vegetation and carbon cycling in an ombrotrophic bog. Glob Chang Biol 13:1168–1186
Buttler A, Robroek BJM, Laggoun-Défarge F, et al. (2015) Experimental warming interacts with soil moisture to discriminate plant responses in an ombrotrophic peatland. J Veg Sci 26:964–974
Chanton JP, Glaser PH, Chasar LS, et al. (2008) Radiocarbon evidence for the importance of surface vegetation on fermentation and methanogenesis in contrasting types of boreal peatlands. Glob Biogeochem Cycles 22:GB4022
De Deyn GB, Cornelissen JHC, Bardgett RD (2008) Plant functional traits and soil carbon sequestration in contrasting biomes. Ecol Lett 11:516–531
Dise NB (2009) Peatland response to global change. Science 326:810–811
Dorrepaal E, Toet S, RSP VL, et al. (2009) Carbon respiration from subsurface peat accelerated by climate warming in the subarctic. Nature 460:616–619
Elmendorf SC, Henry GHR, Hollister RD, et al. (2012) Global assessment of experimental climate warming on tundra vegetation: heterogeneity over space and time. Ecol Lett 15:164–175
Fenner N, Freeman C (2011) Drought-induced carbon loss in peatlands. Nat Geosci 4:895–900
Fornara DA, Tilman D (2008) Plant functional composition influences rates of soil carbon and nitrogen accumulation. J Ecol 96:314–322
Freeman C, Ostle N, Kang H (2001) An enzymic “latch” on a global carbon store. Nature 409:149
Green, Stott, Diack (2006) Assay for fluorescein diacetate hydrolytic activity: optimization for soil samples. Soil Biol Biochem 38:693–701
Greenup AL, Bradford MA, McNamara NP, et al. (2000) The role of Eriophorum vaginatum in CH4 flux from an ombrotrophic peatland. Plant Soil 227:265–272
Gunnarsson U, Malmer N, Rydin H (2002) Dynamics or constancy in Sphagnum dominated mire ecosystems? A 40-year study. Ecography 25:685–704
He X, Xi B, Wei Z, et al. (2011) Spectroscopic characterization of water extractable organic matter during composting of municipal solid waste. Chemosphere 82:541–548
Hodgkins SB, Tfaily MM, McCalley CK, et al. (2014) Changes in peat chemistry associated with permafrost thaw increase greenhouse gas production. PNAS 111:5819–5824
Ingham ER, Klein DA (1982) Relationship between fluorescein diacetate-stained hyphae and oxygen utilization, glucose utilization, and biomass of submerged fungal batch cultures. Appl Environ Microbiol 44:363–370
Isbell F, Calcagno V, Hector A, et al. (2011) High plant diversity is needed to maintain ecosystem services. Nature 477:199–202
Jassey VEJ, Chiapusio G, Gilbert D, et al. (2011a) Experimental climate effect on seasonal variability of polyphenol/phenoloxidase interplay along a narrow fen-bog ecological gradient in Sphagnum fallax. Glob Chang Biol 17:2945–2957
Jassey VEJ, Chiapusio G, Mitchell EAD, et al. (2011b) Fine-scale horizontal and vertical micro-distribution patterns of testate amoebae along a narrow fen/bog gradient. Microb Ecol 61:374–385
Kalbitz K (2003) Changes in properties of soil-derived dissolved organic matter induced by biodegradation. Soil Biol Biochem 35:1129–1142
Kothawala DN, Wachenfeldt von E, Koehler B, Tranvik LJ (2012) Selective loss and preservation of lake water dissolved organic matter fluorescence during long-term dark incubations. Sci Total Environ 433:238–246
Kuiper JJ, Mooij WM, Bragazza L, Robroek BJM (2014) Plant functional types define magnitude of drought response in peatland CO2 exchange. Ecology 95:123–131
Limpens J, Berendse F, Klees H (2003) N deposition affects N availability in interstitial water, growth of sphagnum and invasion of vascular plants in bog vegetation. New Phytol 157:339–347
Luciani X, Redon R, Mounier S (2013) How to correct inner filter effects altering 3D fluorescence spectra by using a mirrored cell. Chemom Intell Lab Syst 126:91–99
Malmer N, Johansson T, Olsrud M, et al. (2005) Vegetation, climatic changes and net carbon sequestration in a north-Scandinavian subarctic mire over 30 years. Glob Chang Biol 1:1895–1909
Murphy KR, Stedmon CA, Graeber D, Bro R (2013) Fluorescence spectroscopy and multi-way techniques. PARAFAC. Anal Methods 5:6557–6511
Neff JC, Hooper DU (2002) Vegetation and climate controls on potential CO2, DOC and DON production in northern latitude soils. Glob Chang Biol 8:872–884
Niemeyer J, Chen Y, Bollag JM (1992) Characterization of humic acids, composts, and peat by diffuse reflectance Fourier-transform infrared spectroscopy. Soil Sci Soc Am J 56:135–140
Pengerud A, Cécillon L, Johnsen LK, et al. (2013) Permafrost distribution drives soil organic matter stability in a subarctic palsa peatland. Ecosystems 16:934–947
Phillips RP, Finzi AC, Bernhardt ES (2011) Enhanced root exudation induces microbial feedbacks to N cycling in a pine forest under long-term CO2 fumigation. Ecol Lett 14:187–194
R Core Team (2015) R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. ISBN 3-900051-07-0, URL http://www.R-project.org/.
Robroek BJM, Schouten MGC, Limpens J, et al. (2009) Interactive effects of water table and precipitation on net CO2 assimilation of three co-occurring Sphagnum mosses differing in distribution above the water table. Glob Chang Biol 15:680–691
Robroek BJM, Wubs E, Marti M, et al. (2014) Microclimatological consequences for plant and microbial composition in sphagnum-dominated peatlands. Boreal Environ Res 19:195–208
Robroek BJM, Jassey VEJ, Kox MAR, et al. (2015) Peatland vascular plant functional types affect methane dynamics by altering microbial community structure. J Ecol 103:925–934
Smith BC (1998) Infrared spectral interpretation: a systematic approach. CRC Press LLC, Boca Raton
Tfaily MM, Hamdan R, Corbett JE, et al. (2013) Investigating dissolved organic matter decomposition in northern peatlands using complimentary analytical techniques. Geochim Cosmochim Acta 112:116–129
Tfaily MM, Corbett JE, Wilson R, et al. (2015) Utilization of PARAFAC-modeled excitation-emission matrix (EEM) fluorescence spectroscopy to identify biogeochemical processing of dissolved organic matter in a northern peatland. Photochem Photobiol 91:684–695
Walker TN, Ward SE, Ostle NJ, Bardgett RD (2015) Contrasting growth responses of dominant peatland plants to warming and vegetation composition. Oecologia 178:141–151
Ward SE, Bardgett RD, McNamara NP, Ostle NJ (2009) Plant functional group identity influences short-term peatland ecosystem carbon flux: evidence from a plant removal experiment. Funct Ecol 23:454–462
Ward SE, Ostle NJ, Oakley S, et al. (2013) Warming effects on greenhouse gas fluxes in peatlands are modulated by vegetation composition. Ecol Lett 16:1285–1293
Ward SE, Orwin KH, Ostle NJ, et al. (2015) Vegetation exerts a greater control on litter decomposition than climate warming in peatlands. Ecology 96:113–123
Wiedermann MM, Gunnarsson U, Nilsson MB, et al. (2008) Can small-scale experiments predict ecosystem responses? An example from peatlands. Oikos 118:449–456
Yu ZC (2012) Northern peatland carbon stocks and dynamics: a review. Biogeosciences 9:4071–4085
Acknowledgments
We are indebted to Länsstyrelsen i Jönköpings län and the staff of the Store Mosse National Park, particularly Arne Andersson, Peter Mattiasson and Martha Wageus, for granting access to the peatland (permission 521-895-2011) and make use of the infrastructure of the park. Roy van Grunsven and two anonymous reviewers provided valuable comments on the scientific content. This work has been financed partially by the Swiss National Science Foundation (SPHAGNOL project; grant number 315280-14807).
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Robroek, B.J.M., Albrecht, R.J.H., Hamard, S. et al. Peatland vascular plant functional types affect dissolved organic matter chemistry. Plant Soil 407, 135–143 (2016). https://doi.org/10.1007/s11104-015-2710-3
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DOI: https://doi.org/10.1007/s11104-015-2710-3