Abstract
In the forests of the Luxembourg cuesta landscape, nutrient cycling is affected by parent material, but in a different way than usually assumed. We challenge the ‘conventional wisdom’ that net N-mineralization is higher in calcareous than in acidic soils, due to higher biological activity and gross N-mineralization. In four separate laboratory incubation experiments, net N-mineralization was higher in acidic than in calcareous soil. Experiments with different tree species showed that soil type was even more important than litter quality. In acidic forests, high net N-mineralization may be due to dense organic layers, but also to differences in soil communities, which are dominated by fungi at low pH versus bacteria at high pH. Fungi have lower N-demand than bacteria, and may thus mitigate low activity and gross N-release. Model studies suggested that microbial immobilization was below 20% in acidic soil, and above 80% in calcareous soil, in both organic layer and mineral topsoil. Differences between fungi and bacteria were supported by selective inhibition. Microbial immobilization significantly decreased with the bactericide streptomycin, while respiration increased with the fungicide cycloheximide. This further supports that bacteria and fungi, and with them calcareous and acidic soils, show different strategies for N-nutrition. For P-nutrition, differences between calcareous and acidic soils are also important, as net P-mineralization mainly occurred in the organic layer, due to chemical sorption in the mineral soil. As a result, in the Luxembourg cuesta landscape, availability of both N and P may be higher in acidic than calcareous forests.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Aerts MAPA, Chapin FS (2000) The mineral nutrition of wild plants revisited: a re-evaluation of process and patterns. Adv Ecol Res 30:1–67
Aubert M, Hedde M, Decaens T, Bureau F, Margerie P, Alard D (2003) Effects of tree canopy composition on earthworms and other macro-invertebrates in beech forests of Upper Normandy (France). Pedobiologia 47:904–912
Bååth E, Anderson TH (2003) Comparison of soil fungal/bacterial ratios in a pH gradient using physiological and PLFA-based techniques. Soil Biol Biochem 35:955–963
Bayley SE, Thormann MN, Szumigalski AR (2005) Nitrogen mineralization and decomposition in western boreal bog and fen peat. Ecoscience 12:455–465
Berendse F, Bobbink R, Rouwenhorst G (1989) A comparative study on nutrient cycling in wet heathland ecosystems. II. Litter decomposition and nutrient mineralization. Oecologia 78:338–348
Berg B (2000) Litter decomposition and organic matter turnover in northern forest soils. For Ecol Manage 133:13–22
Berg B, Ekbohm G (1983) Nitrogen immobilisation in decomposing needle litter at variable carbon:nitrogen ratios. Ecology 64:63–67
Blagodatskaya EV, Anderson TH (1998) Interactive effects of pH and substrate quality on the fungal-to-bacterial ratio and qCO2 of microbial communities in forest soils. Soil Biol Biochem 30:1269–1274
Booth MS, Stark JM, Rastetter E (2005) Controls of nitrogen cycling in terrestrial ecosystems: a synthetic analysis of literature data. Ecol Monogr 75:139–157
Brooks PC, Landman A, Pruden G, Jenkinson DS (1985) Chloroform fumigation and the release of soil nitrogen: a rapid direct extraction method to measure microbial biomass nitrogen in soil. Soil Biol Biochem 17:837–842
Campbell JL, Gower ST (2000) Detritus production and soil N transformations in old-growth eastern hemlock and sugar maple stands. Ecosystems 3:185–192
Cleveland CC, Liptzin D (2007) C:N:P stoichiometry in soil: is there a “Redfield ratio” for the microbial biomass? Biogeochemistry 85:235–252
Cody RP, Smith JK (1987) Applied statistics and the SAS programming language. Elsevier Science Publishers Co. Int., Amsterdam, p 280
Coleman DC, Crossley DA jr (1996) Fundamentals of soil ecology. Academic Press Inc, San Diego
Davy AJ, Taylor K (1974) Seasonal patterns of nitrogen availability in contrasting soils in the chiltern hills. J Ecol 62:793–807
de Vries FT, van Groenigen JW, Hoffland E, Bloem J (2011) Nitrogen losses from two grassland soils with different fungal biomass. Soil Biol Biochem 43:997–1005
Ellenberg H (1977) Stickstoff als Standortsfaktor, insbesondere für mitteleuropäische Pflanzengesellschaften. Oecologia Plant. 12:1–22
Ferraris le Comte de (1777) Reissued in 1965–1970. Carte de Cabinet des Pays-Bas Autrichiens. Bibiliotheque Royale de Belgique, Bruxelles
Fisk MC, Fahey TJ (2001) Microbial biomass and nitrogen cycling responses to fertilization and litter removal in young northern hardwood forests. Biogeochemistry 53:201–223
Green RN, Trowbridge RL, Klinka K (1993) Towards a taxonomic classification of humus forms. Supplement to Forest Science, vol 39
Güsewell S (2004) N: P ratios in terrestrial plants: variation and functional significance. New Phytol 164:243–266
Hart SC, Nason GE, Myrold DD, Perry DA (1994) Dynamics of gross nitrogen transformations in an old-growth forest: the carbon connection. Ecology 75:880–891
Hassink J (1994) Effects of soil texture and grassland management on soil organic C and N and rates of C and N mineralization. Soil Biol Biochem 26:1221–1231
Henderson-Sellers B, Henderson-Sellers A (1993) Factorial techniques for testing environmental model sensitivity. In: Beck MB, McAleer MJ, Jakeman AJ (eds) Modelling change in environmental systems. Wiley, Chichester, England
Högberg MN, Myrold DD, Giesler R, Högberg P (2006) Contrasting patterns of soil N-cycling in model ecosystems of Fennoscandian boreal forests. Oecologia 147:96–107
Högberg MN, Högberg P, Myrold DD (2007) Is microbial community composition in boreal forest soils determined by pH, C-to-N ratio, the three, or all three? Oecologia 150:590–601
ICMSF (2000) Microorganisms in Foods I, their significance and methods of enumeration, 2nd edn. University of Toronto Press, Toronto
IUSS (2015) World Reference Base for Soil Resources 2014, update 2015. International soil classification system for naming soils and creating legends for soil maps. World Soil Resources Reports No. 106. FAO, Rome
Jonard M, Fuerst A, Verstraeten A, Thimonier A, Timmermann V, Potocic N, Waldner P, Benham S, Hansen K, Merila P, Ponette Q, de la Cruz AC, Roskams P, Nicolas M, Croise L, Ingerslev M, Matteucci G, Decinti B, Bascietto M, Rautio P (2014) Tree mineral nutrition is deteriorating in Europe. Glob Change Biol 21:418–430
Koerselman W, Meuleman AFM (1996) The vegetation N:P ratio: a new tool to detect the nature of nutrient limitation. J Appl Ecol 33:1441–1450
Kooijman AM, Besse M (2002) On the higher availability of N and P in lime-poor than in lime-rich coastal dunes in the Netherlands. J Ecol 90:94–403
Kooijman AM, Hedenäs L (2009) Changes in nutrient availability from calcareous to acid wetland habitats with closely related brown moss species: increase instead of decrease in N and P. Plant Soil 324:267–278
Kooijman AM, Martinez-Hernandez GB (2009) Effects of litter quality and parent material on organic matter characteristics and N-dynamics in Luxembourg beech and hornbeam forests. For Ecol Manag 257:1732–1739
Kooijman AM, Smit A (2009) Paradoxical differences in N-dynamics between Luxembourg soils: litter quality or parent material? Eur J Forest Res 128:555–565
Kooijman AM, Kooijman-Schouten MM, Martinez-Hernandez GB (2008) Alternative strategies to sustain N-fertility in acid and calcaric beech forests: low microbial N-demand versus high biological activity. Basic Appl Ecol 9:410–421
Kooijman AM, van Mourik J, Schilder MLM (2009) The relationship between N mineralization or microbial biomass N with micromorphological properties in beech forest soils with different texture and pH. Biol Fertil Soils 45:449–459
Kooijman AM, Cammeraat E (2010) Biological control of beech and hornbeam affects species richness via changes in the organic layer, pH and soil moisture characteristics. Funct Ecol 24:469–477
Kooijman AM, Bloem J, van Dalen BR, Kalbitz K (2016) Differences in activity and N demand between bacteria and fungi in a longer-term incubation experiment with selective inhibition. Appl Soil Ecol 99:26–39
Kuehn KA, Churchill PF, Suberkropp K (1998) Osmoregulatory responses of fungi inhabiting standing litter of the freshwater emergent macrophyte Juncus effusus. Appl Environ Microbiol 64:607–612
Lang F, Bauhus J, Frossard E, George E, Kaiser K, Kaupenjohann M, Krueger J, Matzner E, Polle A, Prietzel J, Rennenberg H, Wellbrock N (2016) Phosphorus in forest ecosystems: new insights from an ecosystem nutrition perspective. J Plant Nutr Soil Sci 179:129–135
Laskowski R, Niklinska M, Maryanski M (1995) The dynamics of chemical elements in forest litter. Ecology 76:1393–1406
Lindsay WL, Moreno EC (1966) Phosphate phase equilibria in soils. Proceedings of the SSSA 24:177–182
Marhan S, Scheu S (2005) Effects of sand and litter availability on organic matter decomposition in soil and in casts of Lumbricus terrestris L. Geoderma 128:155–166
Measures JC (1975) Role of amino acids in osmoregulation of non-halophilic bacteria. Nature 257:398–400
Mettrop IS, Cusell C, Kooijman AM, Lamers LPM (2014) Nutrient and carbon dynamics in peat from rich fens and Sphagnum-fens during different gradations of drought. Soil Biol Biochem 68:317–328
Moore JC, McCann K, de Ruiter PC (2005) Modelling trophic pathways, nutrient cycling, and dynamic stability in soils. Pedobiologia 49:499–510
Niemeyer T, Ries C, Härdtle W (2010) Die Waldgesellschaften Luxemburgs. Vegetation, Standort, Vorkommen und Gefährdung. Ferrantia 57, Musée national d’histoire naturelle, Luxembourg, 122 pp
Parton WP, Silver WL, Burke IC, Grassens L, Harmon ME, Currie WS, King JY, Adair EC, Brandt LA, Hart SC, Fasth B (2007) Global-scale similarities in nitrogen release patterns during long-term decomposition. Science 315:361–364
Phoenix GK, Booth RE, Leake JR, Read DJ, Grime JP, Lee JA (2003) Effects of enhanced nitrogen deposition and phosphorus limitation on nitrogen budgets of semi-natural grasslands. Glob Change Biol 9:1309–1321
Ponge JF (2003) Humus forms in terrestrial ecosystems: a framework to biodiversity. Soil Biol Biochem 35:935–945
Pop V (1997) Earthworm-vegetation-soil relationships in the Romanian Carpathians. Soil Biol Biochem 29:223–229
Pulleman MM, Six J, van Breemen N, Jongmans AG (2005) Soil organic matter distribution and microaggregate characteristics as affected by agricultural management and earthworm activity. Eur J Soil Sci 56:453–467
Reich PB, Grigal DF, Aber JD, Gower ST (1997) Nitrogen mineralization and productivity in 50 hardwood and conifer stands on diverse soils. Ecology 78:335–347
Rousk J, Bååth E, Brookes PC, Lauber CL, Lozupone C, Caporaso JG, Knight R, Fierer N (2010) Soil bacterial and fungal communities across a pH gradient in an arable soil. Int Soc Microb Ecol J 4:1340–1351
Ruess RW, Seagle SW (1994) Landscape patterns in soil microbial processes in the Serengeti National Park, Tanzania. Ecology 75:892–904
Scheu S (1997) Effects of litter (beech and stinging nettle) and earthworms (Octolasion lacteum) on carbon and nutrient cycling in beech forests on a basalt-limestone gradient: a laboratory experiment. Biol Fertil Soils 24:384–393
Schimel DS (1988) Calculation of microbial growth efficiency from 15N immobilization. Biogeochemistry 6:239–243
Schimel JP, Bennett J (2004) Nitrogen mineralization: challenges of a changing paradigm. Ecology 85:591–602
Shen J, Yuan L, Zhang J, Li H, Bai Z, Chen X, Zhang W, Zhang Z (2011) Phosphorus dynamics: from soil to plant. Plant Physiol 156:997–1005
Swift MJ, Heal OW, Anderson JM (1979) Decomposition in terrestrial ecosystems. University of California Press, Berkeley
Talkner J, Jansen M, Beese FO (2009) Soil phosphorus status and turnover in central-European beech forest ecosystems with differing tree species diversity. Eur J Soil Sci 60:338–346
Tietema A (1992) Abiotic factors regulating nitrogen transformations in the organic layer of acid forest soils: moisture and pH. Plant Soil 147:69–78
Tietema A, Wessel WW (1992) Gross nitrogen transformations in the organic layer of acid forest ecosystems subjected to increased atmospheric nitrogen input. Soil Biol Biochem 24:943–950
Turner BL, Condron LM (2013) Pedogenesis, nutrient dynamics, and ecosystem development: the legacy of T.W. Walker and J.K. Syers. Plant Soil 367:1–10
Veer MAC (1997) Nitrogen availability in relation to vegetation changes resulting from grass-encroachment in Dutch dry dunes. J Coast Conserv 3:41–48
Verhoeven JTA, Kooijman AM, van Wirdum G (1988) Mineralization of N and P along a trophic gradient in a freshwater mire. Biogeochemistry 6:31–43
Verhoeven JTA, Maltby E, Schmitz MB (1990) Nitrogen and phosphorus mineralization in fens and bogs. J Ecol 78:713–726
Walker TW, Syers JK (1976) The fate of phosphorus during pedogenesis. Geoderma 15:1–19
Westerman RL (1990) Soil testing and plant analysis, 3rd edn. Soil Science Society America, Madison, Wisconsin
Zöttle H (1960) Dynamik der Stickstoffmineralisation im Waldbodenmaterial III. pH-wert und Mineralstickstoff-Nachlieferung. Plant Soil 13:207–223
Acknowledgements
The authors would like to thank Bas van Dalen, Greet Kooijman-Schouten, Benito Martinez-Hernandez, Jan van Mourik and Madeleine Schilder for their contribution to fieldwork and data collection, and Leo Hoitinga, Leen de Lange, Piet Wartenbergh and Joke Westerveld for their support in the laboratory.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2018 Springer International Publishing AG
About this chapter
Cite this chapter
Kooijman, A.M., Kalbitz, K., Smit, A. (2018). Alternative Strategies for Nutrient Cycling in Acidic and Calcareous Forests in the Luxembourg Cuesta Landscape. In: Kooijman, A., Cammeraat, L., Seijmonsbergen, A. (eds) The Luxembourg Gutland Landscape. Springer, Cham. https://doi.org/10.1007/978-3-319-65543-7_7
Download citation
DOI: https://doi.org/10.1007/978-3-319-65543-7_7
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-65541-3
Online ISBN: 978-3-319-65543-7
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)