Principles of terrestrial ecosystem ecology.pdf
Principles of terrestrial ecosystem ecology.pdf
Principles of terrestrial ecosystem ecology.pdf
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
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