Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- Miscellaneous Frontmatter
- 1 Introduction
- Part I Connecting Ecosystem and Geoscience Processes
- Part II Transport Processes and Conservation Budgets in Biogeoscience
- Part III Coupling Hillslope Geomorphology, Soils, Hydrology, and Ecosystems
- 5 Landscape Evolution Models and Ecohydrologic Processes
- 6 Soil Mantled Hillslopes: Intersections of Geomorphology, Soil Science, and Ecology
- 7 Interactions between Precipitation and Vegetation Canopies
- 8 Constraints on Nutrient Dynamics in Terrestrial Vegetation
- 9 Evapotranspiration
- Part IV Coupling Fluvial and Aeolian Geomorphology, Hydrology/Hydraulics, and Ecosystems
- Index
- References
8 - Constraints on Nutrient Dynamics in Terrestrial Vegetation
from Part III - Coupling Hillslope Geomorphology, Soils, Hydrology, and Ecosystems
Published online by Cambridge University Press: 27 October 2016
Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- Miscellaneous Frontmatter
- 1 Introduction
- Part I Connecting Ecosystem and Geoscience Processes
- Part II Transport Processes and Conservation Budgets in Biogeoscience
- Part III Coupling Hillslope Geomorphology, Soils, Hydrology, and Ecosystems
- 5 Landscape Evolution Models and Ecohydrologic Processes
- 6 Soil Mantled Hillslopes: Intersections of Geomorphology, Soil Science, and Ecology
- 7 Interactions between Precipitation and Vegetation Canopies
- 8 Constraints on Nutrient Dynamics in Terrestrial Vegetation
- 9 Evapotranspiration
- Part IV Coupling Fluvial and Aeolian Geomorphology, Hydrology/Hydraulics, and Ecosystems
- Index
- References
Summary
Introduction
Every limit is a beginning as well as an ending.
George Eliot, Middlemarch.Nutrients, along with carbon, water and solar radiation, are required by virtually all plants to produce new biomass and, eventually, new offspring. Terrestrial plant growth is almost always limited strongly by the availability of one or more nutrients. On some soils growth is restricted by the excessive availability of potentially toxic elements. Plant biomass production and turnover have a major influence on nutrient cycling processes because many are microbial, fueled by plant-derived carbon (Bardgett, 2005; Mulder et al., 2013). This interdependence between nutrient availability and growth is manifested at large spatial and over long temporal scales as variations in ecosystem productivity, vegetation composition and soil development (Anderson-Teixeira et al., 2008; Fernández-Martínez et al., 2014; Hayes et al., 2014), but it originates at the scale of a soil pore, root cell or fungal hypha. It is at this scale that nutrients enter vegetation, but also at which nutrient capture is limited by important physical, chemical and biological factors. These small-scale constraints are the focus of this chapter.
The aim of this chapter is to explain how these constraints operate, how plants have evolved ways to subvert them, and to examine some of their consequences at the larger spatial and longer temporal scales at which ecological and biogeochemical processes are often studied. To achieve this aim, I use information that originated in mechanistic studies of nutrient dynamics in agriculture (Tinker and Nye, 2000; Gregory, 2006), but which is now recognized as a fundamental aspect of both plant ecology and terrestrial biogeochemistry (Fitter and Hay, 2002; Chapin et al., 2011; Schlesinger and Bernhardt, 2013).
Nutrients in Vegetation
Fundamentals
Macronutrients (N, P, K, S, Ca, Mg and Si) are those present in plant tissues in the largest quantities; micronutrients (Na, Cl, Mn, Fe, Cu, Zn, Mo, B and, in some species, Ni and Co) are required in much smaller abundances. Both macro- and micronutrients are essential for plant metabolism; some (Na, Si, Co and Ni) are essential only for certain species or in particular circumstances.
- Type
- Chapter
- Information
- A Biogeoscience Approach to Ecosystems , pp. 254 - 291Publisher: Cambridge University PressPrint publication year: 2016
References
and (2013).
In situ high-frequency observations of mycorrhizas. New Phytologist, 200, 222–8.CrossRefGoogle Scholar
, and (2008). Amplified temperature dependence in ecosystems developing on the lava flows of Mauna Loa, Hawai'i. Proceedings of the National Academy of Sciences (USA), 105, 228–33.CrossRefGoogle Scholar
(1975). A quantitative analysis of the factors affecting plant nutrient uptake from some soils. Journal of Soil Science, 26, 195–206.CrossRefGoogle Scholar
(2005). The Biology of Soil: A Community and Ecosystem Approach. Oxford: Oxford University Press.CrossRef
(1989). Root growth, macro-nutrient uptake dynamics and soil fertility requirements of a high-yielding winter oilseed rape crop. Plant and Soil, 119, 59–70.CrossRefGoogle Scholar
(1996). Total carbon and nitrogen in the soils of the world. European Journal of Soil Science, 47, 151–63.CrossRefGoogle Scholar
(2002). Ecological Climatology: Concepts and Applications. Cambridge: Cambridge University Press.
, , , and (2012a). Function of nutrients: micronutrients. In Marschner's Mineral Nutrition of Higher Plants, ed. . London: Elsevier, pp. 191–248.
, , et al. (2012b). Beneficial elements. In Marschner's Mineral Nutrition of Higher Plants, ed. . London: Elsevier, pp. 249–69.
, , et al. (2012). Using ground-penetrating radar to detect tree roots and estimate biomass. In Measuring Roots, ed. . Berlin: Springer-Verlag, pp. 213–45.CrossRef
, and (2014). Allometric constraints on, and trade-offs in, belowground carbon allocation and their control of soil respiration across global forest ecosystems. Global Change Biology, 20, 1674–84.CrossRefGoogle Scholar
(1977). Internal cycling of 15nitrogen in shortgrass prairie. Ecology, 58, 1322–33.CrossRefGoogle Scholar
and (2012). Nitrogen fixation. In Marschner's Mineral Nutrition of Higher Plants, ed. . London: Elsevier, pp. 389–408.CrossRef
and (2002). Root exudates as mediators of mineral acquisition in low-nutrient environments. Plant and Soil, 245, 35–47.CrossRefGoogle Scholar
(1969). The relation of growth to the chief ionic constituents of the plant. In Ecological Aspects of the Mineral Nutrition of Plants, ed. . Oxford: Blackwell Scientific Publications, pp. 201–13.
, , et al. (2015). Challenges and opportunities for quantifying roots and rhizosphere interactions through imaging and image analysis. Plant, Cell and Environment, 38, 1213–32.CrossRefGoogle Scholar
, and (1969). The supply of nutrient ions by diffusion to plant roots in soil. I. Absorption of potassium by cylindrical roots of onion and leek. Plant and Soil, 30, 252–70.CrossRefGoogle Scholar
and (1997). The ecology of root lifespan. Advances in Ecological Research, 27, 1–60.CrossRefGoogle Scholar
and (2012). Land plants: new theoretical directions and empirical prospects. In Metabolic Ecology: A Scaling Approach, ed. , and . Chichester: John Wiley and Sons Ltd., pp. 164–87.CrossRef
and (2002). Global allocation rules for patterns of biomass partitioning in seed plants. Science, 295, 1517–20.CrossRefGoogle Scholar
, , et al. (2014). Nutrient availability as the key regulator of global forest carbon balance. Nature Climate Change, 4, 471–6.CrossRefGoogle Scholar
and (1986). The photosynthesis-nitrogen relationship in wild plants. In On the Economy of Plant Form and Function, ed. . Cambridge: Cambridge University Press, pp. 25–55.
and (2002). Environmental Physiology of Plants,. San Diego: Academic Press.
and (2001). The Biological Chemistry of the Elements: The Inorganic Chemistry of Life,. Oxford: Oxford University Press.
(1965). Movement of nitrogen in soil. In Soil Nitrogen, ed. and . Madison, WI: American Society of Agronomy, pp. 550–72.
and (2014). Scaling of physical constraints at the root-soil interface to macroscopic patterns of nutrient retention in ecosystems. American Naturalist, 183, 418–30.Google Scholar
, and (2014). It's time to make some changes: modulation of root system architecture by nutrient signals. Journal of Experimental Botany, 65, 769–78.CrossRefGoogle Scholar
and (2000). Global patterns of root turnover for terrestrial ecosystems. New Phytologist, 147, 13–31.CrossRefGoogle Scholar
(2006). Plant Roots: Growth, Activity and Interaction with Soils. Oxford: Blackwell Publishing.CrossRef
, , et al. (1997). Integrated screening validates primary axes of specialisation in plants. Oikos, 79, 259–81.CrossRefGoogle Scholar
, , and (1982). Plant-induced changes in the rhizosphere of rape (Brassica napus var. Emerald) seedlings. I. pH change and the increase in P concentration in the soil solution. New Phytologist, 91, 19–29.CrossRefGoogle Scholar
(1977). Population Biology of Plants. London: Academic Press.
, , et al. (2012). Functions of macronutrients. In Marschner's Mineral Nutrition of Higher Plants, ed. . London: Elsevier, pp. 135–89.CrossRef
, , and (2014). Foliar nutrient concentrations and resorption efficiency in plants of contrasting nutrient-acquisition strategies along a 2-million-year dune chronosequence. Journal of Ecology, 102, 396–410.CrossRefGoogle Scholar
and (1985). Soil structure and potassium supply. II. The effect of ped size and root density on the supply to plants of exchangeable and non-exchangeable potassium from a chalky boulder clay soil. Journal of Soil Science, 36, 61–9.CrossRefGoogle Scholar
(2004). The plastic plant: root responses to heterogeneous supplies of nutrients. New Phytologist, 162, 9–24.CrossRefGoogle Scholar
and (2015). Arbuscular mycorrhiza and nitrogen: implications for individual plants through to ecosystems. Plant and Soil, 386, 1–19.CrossRefGoogle Scholar
, , and (2005). Phylogenetic variation in the silicon composition of plants. Annals of Botany, 96, 1027–46.CrossRefGoogle Scholar
, , , and (1990). Simulation of nutrient uptake by a growing root system considering increasing root density and inter-root competition. Plant and Soil, 124,149–55.CrossRefGoogle Scholar
(2012). Precipitation, soils, NPP, and biodiversity: resurrection of Albrecht's curve. Ecological Monographs, 82, 277–96.CrossRefGoogle Scholar
and (2009). The global distribution of net primary production: resolving the paradox. Ecological Monographs, 79, 343–77.CrossRefGoogle Scholar
, , et al. (1996). A global analysis of root distributions for terrestrial biomes. Oecologia, 108, 389–411.CrossRefGoogle Scholar
and (2001). The distribution of soil nutrients with depth: global patterns and the imprint of plants. Biogeochemistry, 53, 51–77.CrossRefGoogle Scholar
, and (2004). Plant and mycorrhizal regulation of rhizodeposition. New Phytologist, 163, 459–80.CrossRefGoogle Scholar
, , , and (2005). Dissolved organic nitrogen uptake by plants—an important N uptake pathway?
Soil Biology and Biochemistry, 37, 413–23.Google Scholar
(2012). Stoichiometry. In Metabolic Ecology: A Scaling Approach, ed. , and . Chichester: John Wiley and Sons Ltd, pp. 34–47.CrossRef
, , and (2014). Sodium fertilization increases termites and enhances decomposition in an Amazonian forest. Ecology, 95, 795–800.CrossRefGoogle Scholar
, and (1969). Ion uptake from soils by plant roots, subject to the Epstein-Hagen relation. Australian Journal of Soil Research
6, 159–67.Google Scholar
, , et al. (2012). Reciprocal rewards stabilize cooperation in the mycorrhizal symbiosis. Science, 333, 880–2.CrossRefGoogle Scholar
, , et al. (2013). Hyperspectral remote sensing of foliar nitrogen content. Proceedings of the National Academy of Sciences (USA), 110, E185–92.CrossRefGoogle Scholar
(1960). Wurzelatlas Mitteleuropäischer Ackerunkräuter und Kulturpflanzen. Frankfurt am Main: DLG-Verlag.
, and (2014). Environmental filtering explains variation in plant diversity along resource gradients. Science, 345, 1602–5.Google Scholar
, and (2008). Plant Physiological Ecology,. New York: Springer Science+Business Media.
, , and (2008). Plant nutrient-acquisition strategies change with soil age. Trends in Ecology and Evolution, 23, 95–103.Google Scholar
, , et al. (2011). Phosphorus nutrition of Proteaceae in severely phosphorus-impoverished soils: are there lessons to be learned for future crops?
Plant Physiology, 156, 1058–66.Google Scholar
, , et al. (2007). Ecological feedbacks following deforestation create the potential for a catastrophic ecosystem shift in tropical dry forest. Proceedings of the National Academy of Sciences (USA), 104, 20696–701.CrossRefGoogle Scholar
and (2008). Nitrogen limitation of net primary productivity in terrestrial ecosystems is globally distributed. Ecology, 89, 371–9.CrossRefGoogle Scholar
and (1983). The effects of fertilizers and drought on the concentrations of potassium in the dry matter and tissue water of field-grown spring barley. Journal of Agricultural Science, 101, 741–8.CrossRefGoogle Scholar
and (1984). A hypothesis relating critical potassium concentrations form growth to the distribution and functions of this ion in the plant cell. New Phytologist, 91, 1–13.CrossRefGoogle Scholar
, and (1991). Phosphorus depletion and pH decrease at the root-soil and hyphae-soil interfaces of VA mycorrhizal white clover fertilized with ammonium. New Phytologist, 119, 397–404.CrossRefGoogle Scholar
, , et al. (2012). RooTrak: automated recovery of three-dimensional plant root architecture in soil from x-ray microcomputed tomography images using visual tracking. Plant Physiology, 158, 561–9.Google Scholar
(1999). Roots in soil: unearthing the complexities of roots and their rhizospheres. Annual Review of Plant Physiology and Plant Molecular Biology, 50, 695–718.CrossRefGoogle Scholar
and (1995). Phosphorus and carbon budgets: mycorrhizal contribution in Hyacinthoides non-scripta (L.) Chouard ex Rothm. under natural conditions. New Phytologist, 129, 619–27.CrossRefGoogle Scholar
, , and (2014). Convergence of terrestrial plant production across global climate gradients. Nature, 512, 39–43.CrossRefGoogle Scholar
and (2010). Nitrogen storage and remobilization by trees: ecophysiological relevance in a changing world. Tree Physiology, 30, 1083–95.CrossRefGoogle Scholar
, , et al. (2013). Connecting the green and brown worlds: allometric and stoichiometric predictability of above- and below-ground networks. Advances in Ecological Research, 49, 69–175.CrossRefGoogle Scholar
and (2012). Rhizosphere chemistry in relation to plant nutrition. In Marschner's Mineral Nutrition of Higher Plants, ed. . London: Elsevier, pp. 347–68.CrossRef
(1988). Mycorrhizal links between plants: their functioning and ecological significance. Advances in Ecological Research, 18, 243–70.CrossRefGoogle Scholar
, and (1989). The functioning of roots in grassland communities. Aspects of Applied Biology, 22, 263–9.Google Scholar
, and (1998). Polyphenols as regulators of plant-litter-soil interactions in northern California's pygmy forest: a positive feedback?
Biogeochemistry, 42,189–220.Google Scholar
(1994). The effect of root shrinkage on soil water inflow. Philosophical Transactions of the Royal Society of London, B345, 395–402.CrossRefGoogle Scholar
, , et al. (2008). Canopy nitrogen, carbon assimilation, and albedo in temperate and boreal forests: functional relations and potential climate feedbacks. Proceedings of the National Academy of Sciences (USA), 105, 19336–41.Google Scholar
, , et al. (2008). Plants can use protein as a nitrogen source without assistance from other organisms. Proceedings of the National Academy of Sciences (USA), 105, 4524–9.CrossRefGoogle Scholar
(2007). Explaining variation in fine root life span. Progress in Botany, 68, 282–398.CrossRefGoogle Scholar
, , , and (2012a). Pot size matters: a meta-analysis of the effects of rooting volume on plant growth. Functional Plant Biology, 39, 839–50.Google Scholar
, , et al. (2012b). Biomass allocation to leaves, stems and roots: meta-analyses of interspecific variation and environmental control. New Phytologist, 193, 30–50.Google Scholar
and (2005). Effects of temperature on nutrient uptake. In Nutrient Acquisition by Plants: An Ecological Perspective, ed. . Heidelberg: Springer-Verlag, pp. 277–310.CrossRef
, , et al. (2003). Plant roots release phospholipid surfactants that modify the physical and chemical properties of soil. New Phytologist, 157, 315–26.CrossRefGoogle Scholar
and (2003). Mycorrhizas and nutrient cycling in ecosystems—a journey towards relevance?
New Phytologist, 157, 475–92.Google Scholar
(1995). Growth responses of some fungi to spatially heterogeneous nutrients. FEMS Microbiology Ecology, 26, 269–80.CrossRefGoogle Scholar
(1994a). Resource capture by single roots. In Resource Capture by Crops, ed. , and . Nottingham: Nottingham University Press, pp. 53–76.
(1994b). The responses of plants to non-uniform supplies of nutrients. New Phytologist, 127, 635–74.Google Scholar
(1996). Variation, co-ordination and compensation in root systems in relation to soil variability. Plant and Soil, 187, 57–66.CrossRefGoogle Scholar
(2001). Root proliferation, nitrate inflow and their carbon costs during nitrogen capture by competing plants in patchy soil. Plant and Soil, 232, 41–50.CrossRefGoogle Scholar
(2004). Scaling the depths: below-ground allocation in plants, forests and biomes. Functional Ecology, 18, 290–5.Google Scholar
and (1999). The magnitude and control of carbon transfer between plants linked by a common mycorrhizal network. Journal of Experimental Botany, 50, 9–13.Google Scholar
and (1987). Root hairs and plant growth at low nitrogen availabilities. New Phytologist, 107, 681–93.CrossRefGoogle Scholar
, , and (1989). Root-induced nitrogen mineralisation: a theoretical analysis. Plant and Soil, 117, 185–93.CrossRefGoogle Scholar
, , and (1999). Plant root proliferation in nitrogen-rich patches confers competitive advantage. Proceedings of the Royal Society of London, B266, 431–5.CrossRefGoogle Scholar
, and (1991). What limits nitrate uptake from soil?
Plant, Cell and Environment, 14, 77–85.Google Scholar
, , et al. (2012). Carbon trading for phosphorus gain: the balance between rhizosphere carboxylates and arbuscular mycorrhizal symbiosis in plant phosphorus acquisition. Plant, Cell and Environment, 35, 2170–80.Google Scholar
and (1973). Phosphate flow into mycorrhizal roots. Pesticide Science, 4, 385–95.CrossRefGoogle Scholar
and (2013). Biogeochemistry,. Waltham, MA: Elsevier.
, , et al. (2004). Developmental physiology of cluster-root carboxylate synthesis and exudation in harsh hakea. Expression of phosphoenolpyruvate carboxylase and the alternative oxidase. Plant Physiology, 135, 549–60.CrossRefGoogle Scholar
and (2004). Mycorrhizal networks: a review of their extent, function, and importance. Canadian Journal of Botany, 82, 1140–65.Google Scholar
, and (2002). Carbon and nutrient fluxes within and between mycorrhizal plants. In Mycorrhizal Ecology, ed. and . Heidelberg: Springer-Verlag, pp. 33–74.
and (2008). Mycorrhizal Symbioses,. London: Academic Press.
, , and (2011). Roles of arbuscular mycorrhizas in plant phosphorus nutrition: interactions between pathways of phosphorus uptake in arbuscular mycorrhizal roots have important implications for understanding and manipulating plant phosphorus acquisition. Plant Physiology, 156, 1050–7.Google Scholar
, , , and (2003). Rapid turnover of hyphae of mycorrhizal fungi determined by AMS microanalysis of 14C. Science, 300, 1138–40.CrossRefGoogle Scholar
and (2002). Ecological Stoichiometry: The Biology of Elements from Molecules to the Biosphere. Princeton, NJ: Princeton University Press.
, and (2002). Rapid fine root disappearance in a pine woodland: a substantial carbon flux. Canadian Journal of Forest Research, 32, 2225–30.CrossRefGoogle Scholar
, , et al. (2014). Crystal structure of the plant dual-affinity nitrate transporter NRT1.1. Nature, 507, 73–7.Google Scholar
, and (1979). Decomposition in Terrestrial Ecosystems. Oxford: Blackwell Scientific Publications.
, and (2014). Complementary plant nutrient-acquisition strategies promote growth of neighbour species. Functional Ecology, 28, 819–28.CrossRefGoogle Scholar
, , and (1997). A comparative study of leaf nutrient concentrations in a regional herbaceous flora. New Phytologist, 136, 679–89.Google Scholar
(1976). Transport of water to plant roots in soil. Philosophical Transactions of the Royal Society of London, B273, 445–61.CrossRefGoogle Scholar
and (2000). Solute Movement in the Rhizosphere. New York: Oxford University Press.
, , and (2013). Dynamic trajectories of growth and nitrogen capture by competing plants. New Phytologist, 193, 948–58.CrossRefGoogle Scholar
, and (1996). Nutrient inflow and root proliferation during the exploitation of a temporally and spatially discrete source of nitrogen in soil. Plant and Soil, 178, 185–92.CrossRefGoogle Scholar
, , , and (2012a). A global database of carbon and nutrient concentrations of green and senesced leaves. Data set available online [http://daac.ornl.gov] from Oak Ridge National Laboratory Distributed Active Archive Center, Oak Ridge, Tennessee, U.S.A. http://dx.doi.org/10.3334/ORNLDAAC/1106.
, , , and (2012b). Global resorption efficiencies and concentrations of carbon and nutrients in leaves of terrestrial plants. Ecological Monographs, 82, 205–20.Google Scholar
, , et al. (2012). Mycorrhizal networks: common goods of plants shared under unequal terms of trade. Plant Physiology, 159, 789–97.CrossRefGoogle Scholar
, and (2002). Rapid induction of regulatory and transporter genes in response to phosphorus, potassium, and iron deficiencies in tomato roots. Evidence for cross talk and root/rhizosphere-mediated signals. Plant Physiology, 130, 1361–70.CrossRefGoogle Scholar
, , et al. (2007). Evolutionary control of leaf element composition in plants. New Phytologist, 174, 516–23.Google Scholar
, , et al. (2000). Environment-induced modifications to root longevity in Lolium perenne and Trifolium repens
. Annals of Botany, 85, 397–401.CrossRefGoogle Scholar
and (2013). Common mycorrhizal networks amplify size inequality in Andropogon gerardii monocultures. New Phytologist, 198, 203–13.Google Scholar
, and (1999). A general model for the structure and allometry of plant vascular systems. Nature, 400, 664–7.CrossRefGoogle Scholar
(2012). Ion uptake mechanisms of individual cells and roots: short-distance transport. In Marschner's Mineral Nutrition of Higher Plants, ed. , pp. 7–47. London: Elsevier.CrossRef
, , and (2007). Extraordinarily high leaf selenium to sulfur ratios define “Se-accumulator” plants. Annals of Botany, 100, 111–8.CrossRefGoogle Scholar
, , et al. (1996). Effects of inorganic nitrogen application on the dynamics of the soil solution composition in the root zone of maize. Plant and Soil, 180, 1–9.Google Scholar
(1994). A steady-state model of nutrient uptake accounting for newly grown roots. Soil Science Society of America Journal, 58, 1562–71.CrossRefGoogle Scholar
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