in Tasmania's
Hellyer Gorge Forests account for 75% of the
gross primary productivity of the Earth's
biosphere, and contain 80% of the Earth's plant biomass. Global forest biomass in 2025 is estimated at 709 gigatonnes, which is an average of 171 tonnes per ha. The forest carbon stock, including all carbon pools, is estimated at 714 gigatonnes, or 172 tonnes per ha. 46% of the forest carbon stock is in soil, 44% is in living (above ground and below ground) biomass and 10% is in litter and deadwood. Forests have intricate three-dimensional structures that increase in complexity with lower levels of disturbance and greater variety of tree species. The biodiversity of forests varies considerably according to factors such as forest type, geography, climate, and soils – in addition to human use. Most forest habitats in temperate regions support relatively few animal and plant species, and species that tend to have large geographical distributions, while the montane forests of Africa, South America, Southeast Asia, and lowland forests of Australia, coastal Brazil, the Caribbean islands, Central America, and insular Southeast Asia have many species with small geographical distributions.
Layers , featuring various
Adansonia (baobab) species,
Alluaudia procera (Madagascar ocotillo) and other vegetation The main layers of all forest types are the
forest floor, the understory, and the canopy. The emergent layer, above the canopy, exists in tropical rainforests. Each layer has a different set of plants and animals, depending upon the availability of sunlight, moisture, and food. • The
Forest floor is covered in dead plant material such as fallen leaves and decomposing logs, which
detritivores break down into new soil. The layer of decaying leaves that covers the soil is necessary for many insects to overwinter and for amphibians, birds, and other animals to shelter and forage for food.
Leaf litter also keeps the soil moist, stops erosion, and protects roots against extreme heat and cold. The
fungal mycelium that helps form the
mycorrhizal network transmits nutrients from decaying material to trees and other plants. The
forest floor supports a variety of plants, ferns, grasses, and tree seedlings, as well as animals such as
ants,
amphibians,
spiders, and
millipedes. •
Understory is made up of bushes, shrubs, and young trees that are adapted to living in the shade of the canopy. •
Canopy is formed by the mass of intertwined branches, twigs, and leaves of mature trees. The crowns of the dominant trees receive most of the sunlight. This is the most productive part of the trees, where maximum food is produced. The canopy forms a shady, protective "umbrella" over the rest of the forest. •
Emergent layer exists in a tropical rain forest and is composed of a few scattered trees that tower over the canopy. In botany and countries like Germany and Poland, a different classification of forest vegetation is often used: tree, shrub, herb, and moss layers (see
stratification (vegetation)).
Types Forests are classified differently and to different degrees of specificity. One such classification is in terms of the
biomes in which they exist, combined with leaf longevity of the dominant species (whether they are
evergreen or
deciduous). Another distinction is whether the forests are composed predominantly of broadleaf trees,
coniferous (needle-leaved) trees, or mixed. •
Boreal forests occupy the
subarctic zone and are generally evergreen and coniferous. •
Temperate zones support both broadleaf deciduous forests (e.g.,
temperate deciduous forest) and evergreen coniferous forests (e.g.,
temperate coniferous forests and
temperate rainforests). Warm temperate zones support broadleaf evergreen forests, including
laurel forests. • Tropical and
subtropical forests include
tropical and subtropical moist forests,
tropical and subtropical dry forests, and
tropical and subtropical coniferous forests. • Forests are classified according to physiognomy based on their overall physical structure or
developmental stage (e.g.
old growth vs.
second growth). • Forests can also be classified more specifically based on the climate and the dominant tree species present, resulting in numerous different forest types (e.g.,
Ponderosa pine/
Douglas fir forest). The number of trees in the world, according to a 2015 estimate, is 3 trillion, of which 1.4 trillion are in the tropics or sub-tropics, 0.6 trillion in the temperate zones, and 0.7 trillion in the coniferous boreal forests. The 2015 estimate is about eight times higher than previous estimates, and is based on tree densities
measured on over 400,000 plots. It remains subject to a wide margin of error, not least because the samples are mainly from Europe and North America. Forests can also be classified according to the amount of human alteration.
Old-growth forest contains mainly natural patterns of biodiversity in established
seral patterns, and they contain mainly species native to the region and habitat. In contrast,
secondary forest is forest regrowing following timber harvest and may contain species originally from other regions or habitats. Different global forest classification systems have been proposed, but none has gained universal acceptance.
UNEP-
WCMC's forest category classification system is a simplification of other, more complex systems (e.g.
UNESCO's forest and woodland 'subformations'). This system divides the world's forests into 26 major types, which reflect climatic zones as well as the principal types of trees. These 26 major types can be reclassified into 6 broader categories: temperate needleleaf, temperate broadleaf and mixed, tropical moist, tropical dry, sparse trees and parkland, and forest plantations.
Tropical dry Tropical dry forests are characteristic of areas in the tropics affected by seasonal drought. The seasonality of rainfall is usually reflected in the deciduousness of the forest canopy, with most trees being leafless for several months of the year. Under some conditions, such as less fertile soils or less predictable drought regimes, the proportion of evergreen species increases and the forests are characterised as "
sclerophyllous".
Thorn forest, a dense forest of low stature with a high frequency of thorny or spiny species, is found where drought is prolonged, and especially where grazing animals are plentiful. On very poor soils, and especially where fire or herbivory are recurrent phenomena,
savannas develop.
Sparse trees and savanna Sparse trees and
savanna are forests with sparse tree-
canopy cover. They occur principally in areas of transition from forested to non-forested landscapes. The two major zones in which these
ecosystems occur are in the
boreal region and in the seasonally dry tropics. At high latitudes, north of the main zone of boreal forestland, growing conditions are not adequate to maintain a continuously closed
forest cover, so tree cover is both sparse and discontinuous. This vegetation is variously called open
taiga, open
lichen woodland, and
forest-tundra. A savanna is a mixed
woodland–
grassland ecosystem characterized by the trees being sufficiently widely spaced so that the canopy does not close. The open canopy allows sufficient light to reach the ground to support an unbroken
herbaceous layer that consists primarily of grasses. Savannas maintain an open canopy despite a high tree density.
Plantations Forest plantations are generally intended for the production of timber and
pulpwood. Commonly mono-specific, planted with even spacing between the trees, and intensively managed, these forests are generally important as habitat for native
biodiversity. Some are managed in ways that enhance their biodiversity protection functions and can provide ecosystem services such as nutrient capital maintenance,
watershed and soil structure protection and carbon storage. == Area ==