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Principles of terrestrial ecosystem ecology.pdf

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182 8. Terrestrial Plant Nutrient Use<br />

Roots grow preferentially in resource hot<br />

spots. Root growth in the soil is not random.<br />

Roots that encounter microsites <strong>of</strong> high nutrient<br />

availability branch pr<strong>of</strong>usely (Hodge et al.<br />

1999), allowing plants to exploit preferentially<br />

zones <strong>of</strong> high nutrient availability. This explains<br />

why root length is greatest in surface soils (Fig.<br />

7.3), where nutrient inputs and mineralization<br />

are greatest, even though roots tend to be<br />

geotropic (i.e., grow vertically downward).<br />

This exploitation <strong>of</strong> nutrient hot spots ensures<br />

that plants maximize the nutrient return for a<br />

given investment in roots and reduces the<br />

fine-scale heterogeneity in soil nutrient concentrations.<br />

At a finer scale, root hairs, the<br />

elongate epidermal cells <strong>of</strong> the root that extend<br />

out into the soil, increase in length (e.g., from<br />

0.1 to 0.8mm) in response to a reduction in the<br />

supply <strong>of</strong> nitrate or phosphate (Bates and<br />

Lynch 1996). Both <strong>of</strong> these responses increase<br />

the length and surface area <strong>of</strong> roots available<br />

for nutrient uptake. Exploitation <strong>of</strong> hot spots<br />

does not always occur, however (Robinson<br />

1994), and may be more pronounced in fastgrowing<br />

than in slow-growing species (Huante<br />

et al. 1998).<br />

Root length is a better predictor <strong>of</strong> nutrient<br />

uptake than is root biomass. Root length correlates<br />

closely with nutrient acquisition in<br />

short-term studies <strong>of</strong> nutrient uptake by plants<br />

from soils. Roots with a high specific root length<br />

(SRL; i.e., root length per unit mass) maximize<br />

their surface area per unit root mass and therefore<br />

the volume <strong>of</strong> soil that can be explored<br />

by a given investment in root biomass. We<br />

know much less about the morphology and<br />

physiology <strong>of</strong> roots in soil than <strong>of</strong> leaves. The<br />

limited available data suggest, however, that<br />

herbaceous plants (especially grasses) <strong>of</strong>ten<br />

have a greater SRL than woody plants and that<br />

there is a wide range in SRL among roots in any<br />

<strong>ecosystem</strong>. Much <strong>of</strong> the variation in SRL<br />

reflects the multiple functions <strong>of</strong> belowground<br />

organs. Roots can have a high SRL either<br />

because they have a small diameter or because<br />

they have a low tissue density (mass per unit<br />

volume). Some belowground stems and coarse<br />

roots have large diameters to store carbohydrates<br />

and nutrients or to transport water and<br />

nutrients and play a minor role in nutrient<br />

uptake. There may also be a trade<strong>of</strong>f between<br />

SRL and longevity among fine roots, with highdensity<br />

roots being less prone to desiccation<br />

and herbivory than low-density roots. Both the<br />

leaves and roots <strong>of</strong> slowly growing species <strong>of</strong>ten<br />

have high tissue density, low rates <strong>of</strong> resource<br />

acquisition (carbon and nutrients, respectively)<br />

but greater longevity than do leaves and roots<br />

<strong>of</strong> more rapidly growing species (Craine et al.<br />

2001).<br />

Mycorrhizae<br />

Mycorrhizae increase the volume <strong>of</strong> soil<br />

exploited by plants. Mycorrhizae are symbiotic<br />

relationships between plant roots and fungal<br />

hyphae, in which the plant acquires nutrients<br />

from the fungus in return for carbohydrates<br />

that constitute the major carbon source for the<br />

fungus. About 80% <strong>of</strong> angiosperm plants, all<br />

gymnosperms, and some ferns are mycorrhizal<br />

(Wilcox 1991). These mycorrhizal relationships<br />

are important across a broad range <strong>of</strong> environmental<br />

and nutritional conditions, including<br />

fertilized crops (Allen 1991, Smith and Read<br />

1997). With respect to nutrient uptake, mycorrhizal<br />

hyphae basically serve as an extension <strong>of</strong><br />

the root system into the bulk soil, <strong>of</strong>ten providing<br />

1 to 15m <strong>of</strong> hyphal length per centimeter<br />

<strong>of</strong> root—that is, an increase in absorbing<br />

length <strong>of</strong> two to three orders <strong>of</strong> magnitude.<br />

Because the nutrient transport through hyphae<br />

occurs more rapidly than by diffusion along a<br />

tortuous path through soil water films, mycorrhizae<br />

reduce the diffusion limitation <strong>of</strong> uptake<br />

by plants. The small diameter <strong>of</strong> mycorrhizal<br />

hyphae (less than 0.01mm) compared to roots<br />

(generally 0.1 to 1mm) enables plants to exploit<br />

more soil with a given biomass investment in<br />

mycorrhizal hyphae than for the same biomass<br />

invested in roots. Plants typically invest 4 to<br />

20% <strong>of</strong> their gross primary production (GPP)<br />

in supporting mycorrhizal hyphae (Lambers et<br />

al. 1996). Most <strong>of</strong> this carbon supports mycorrhizal<br />

respiration rather than fungal biomass,<br />

so a given carbon investment in mycorrhizal<br />

biomass can represent a large carbon cost to<br />

the plant. Mycorrhizae are most important in<br />

supplementing the nutrients that diffuse<br />

slowly through soils, particularly phosphate and

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