Forest Ecology. Dan Binkley

FIGURE 2.1 The vegetation in the Front Range of the Rocky Mountains in northern Colorado, USA grades from primarily grass/shrub domination at low, dry elevations, through open pine‐dominated woodlands, to aspens mixed with a variety of conifers, to forests of spruce and fir and then to tundra (alpine) at the highest elevations

      (Source: based on a diagram from Laurie Huckaby).

      The patterns depend on direct effects of environmental factors on tree physiology, and also environmental influences on fires, insects, and other forest‐shaping agents.

Climate Influences Where Forest Occur, and How They Grow

The distributions of forests can be mapped across the world, showing regions where major forest types occupy most of the landscapes (Figure 2.2). Forests essentially occur everywhere there is enough water for trees to cope with evaporative demands driven by temperature and atmospheric humidity. The two exceptions to this generalization would be areas that are too cold, and areas that have enough water but high frequency of fires leads to greater success of grasses and fire‐tolerant shrubs.

The productivity of the world's vegetation has been mapped by satellites, where the wavelengths of light reflected from vegetation across time periods are combined with simulation models to estimate growth rates. Such global estimates may come close to pegging the actual global averages and totals, but the accuracy for any single region or landscape would need to be verified for confidence (as with any map).

FIGURE 2.2 The distributions of major types of forests can be mapped across the world (upper), along with typical rates of aboveground net primary production of forests and other vegetation types (middle; for more information on production, see Chapter 7;

      Source: maps based on Pan et al. 2013).

      The spatial patterns can also be examined in a functional way, where aboveground net primary production is plotted relative to annual temperatures, and the balance between precipitation and the energy available to evaporate water (wetter conditions occur above the 0 point on the Y‐axis;

      Source: Based on Running et al. 2004.

The same information can be examined in relation to environmental factors rather than spatial locations (Figure 2.2). It's not surprising that the most productive forests (and other vegetation types) tend to occur in warmer locations where precipitation is close to (or higher than) the water that could be evaporated by available energy. Is it possible to be too warm for high growth rates, even where plenty of water is available? This is not clear from Figure 2.2, but the hottest tropical forests do appear to have lower growth rates than somewhat cooler forests (see Figure 2.18).

Warmer Forests Have More Species of Trees

Patterns in forests across environmental gradients can also be examined in terms of structure and species composition. Trees tend to be taller under favorable environmental conditions of moderate‐to‐warm temperatures and high rainfall (Figure 2.3). Part of the geographic pattern in tree heights relates to the physics of supplying leaves high above the ground with sufficient water to meet the evaporative demand of the atmosphere; dry air requires more water than the tallest trees could transport (see Chapter 4). The number of species found in forests is low at higher elevations, and high at lower elevations and in warmer areas.

FIGURE 2.3 The tallest trees in the world occur in cool, wet locations, and most tall trees are limited to relatively wet areas. More severe growing conditions limit average tree heights

      (Source: upper map, from Pan et al. 2013/Annual reviews,Inc.).

      The diversity of tree species in a tropical forest in Costa Rica dropped by about half with a 1000 m increase in elevation (lower left,

      Source: Data from Veintimilla et al. 2019, photo by Cristian Montes).

      Across eastern China, the number of tree species that co‐occur in 600 m² (=0.06 ha) plots increases rapidly with temperature, but levels off (and might even decline) on the hottest sites.

      Source: Based on Wang et al. 2009.

Chemical and Biological Reactions Go Faster with Increasing Temperature

Extreme temperatures tend to stop biological processes. Little biological activity occurs below the freezing point of water, and at very high temperatures organs fail and organisms die. Between these extremes, most biological processes respond strongly to temperature, often changing by a factor of two or more for a 10 °C change in temperature (Figure 2.4). Chemical reactions may follow a simple trend, but the response of biological processes derives from a suite of interacting factors. Some biological reactions such as respiration (the oxidation of carbon compounds to release energy and CO₂) may show an exponential temperature trend, as the effect of temperature on breakdown of carbon compounds is similar to simple chemical reactions.

      The temperature effect on more complex biochemical reaction rates includes any effects on the breakdown and regeneration rates of enzymes and other proteins. Biological reactions also change as temperatures affect the supplies of reactants. Higher temperatures lead to greater evaporative stresses, which reduce the supply rate of carbon dioxide flowing into leaves. The products of reactions can suppress rates of further reaction if they accumulate in cells, which can be a problem at high temperatures. Rates of photosynthesis do not increase with a simple exponential trend like rates of respiration (Figure 2.3). The temperature effect on rates of photosynthesis might have a humped shape, reflecting the balance between carbon gains and losses in leaves, as photosynthesis declines in response to rising photorespiration (the diversion of energy to producing water rather than sugar).

      The temperature of an object, such as a tree leaf, represents the thermal energy contained within the object. Thermal energy is the kinetic energy of molecules; the molecules of nitrogen in a volume of air move at velocities of about 450 to 500 m per second. A molecule of nitrogen might move about 100 nm before colliding with another air molecule, which translates into billions of collisions for each molecule each second. Molecules move faster as temperatures rise, leading to