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Old growth forest
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Old growth forest (also termed primary forest, ancient forest, virgin forest, primeval forest, frontier forest or in Britain, ancient woodland) is a type of forest that has attained great age and so exhibits unique biological features.
Old growth forests typically contain large live trees, large dead trees (sometimes called "snags"), and large logs, as well as many other common characteristics representative of forests in general.
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Encyclopedia
Old growth forest (also termed primary forest, ancient forest, virgin forest, primeval forest, frontier forest or in Britain, ancient woodland) is a type of forest that has attained great age and so exhibits unique biological features.
Old growth forests typically contain large live trees, large dead trees (sometimes called "snags"), and large logs, as well as many other common characteristics representative of forests in general. Until the stand is hit by stand replacing disturbance only individual tree mortality takes place. This process creates gaps in the main canopy layer. Hence, the light can penetrate the main canopy and create favorable photosynthetic conditions for the understory. That is why the understory in old-growth forest is more developed than in mature stands. Old growth forests are unique usually having multiple horizontal layers of vegetation representing a variety of tree species and age-classes as well as pit and mound soil shape with well established fungal nets. Many old growth forest stands are threatened by habitat destruction through excessive logging. The resulting destruction reduces biodiversity, affecting not only the old growth forest, per se, but also indigenous species that rely upon old growth forest habitat.
Forest regenerated after severe disruptions, such as clear-cut or fire is often called second-growth or regeneration until enough time passes that the effects of the disturbance are no longer evident. Depending on the forest, this may take anywhere from a century to several millennia. Hardwood forests of the eastern United States can develop old-growth characteristics in one or two generations of trees, or 150-500 years.
Old growth forests are often home to rare species, threatened species and endangered species of plants and animals, making them ecologically significant. One example of a rare species reliant upon old growth forest is the Northern Spotted Owl. Levels of biodiversity, the variation of life forms within unique old growth forest ecosystems, may be higher or lower in old growth forests compared to that in second-growth forests, depending on specific circumstances, environmental variables and geographic variables (where the forest is located). Logging in old growth forests is a contentious issue in many parts of the world.
Definitions
- Stand replacing disturbance hits the forest and kills most of the living trees.
- Stand initiation: population of new trees becomes established.
- Stem exclusion: trees grow higher and enlarge their canopy thus competing for the light with neighbors. Light competition mortality kills slow growing trees and reduces forest density. This allows surviving trees to increase in size. Eventually the canopies of neighboring trees touch each other and drastically lowers amount of light that reaches lower layers. Due to that the understory dies and only very shade tolerant species survive.
- Understory reinitiation: trees die from low level mortality, such as windthrow and deceases. Individual canopy gaps start to appear and more light can reach forest floor. Hence, shade tolerant species can establish in the understory.
- Old-growth: Main canopy trees become older and more of them die. That creates even more gaps. Since the gaps appear in different timing, the understory trees establish in different timing from one another. Furthermore, the amount of light that reaches each understory tree depends on its position relative to the gap. Thus, each understory tree grows in different speed. The difference in establishment timing and in growth speed create population of understory trees that are variable in size. Eventually, some understory trees grow to become as tall as the main canopy trees. Hence, the gap created by the old dead tree is closed by younger one that eventually will also die and will be replaced by another tree. This perpetuation process is typical for old-growth stage. This however does not mean that the forest will be old-growth forever. Generally there are three possible futures for old-growth stage forest: a)The forest will be hit by a new stand replacing disturbance and most of the trees will die. b)The tree community will eventually create non-favorable conditions for new trees to regenerate. In this case the old trees will die and smaller plants will create woodland. c)The regenerating understory trees are different species than the main canopy trees. In this case the forest will switch back to Stem Exclusion stage, but with different tree species. The forest in old-growth stage can be stable for centuries and even a thousand years, but it all depends on its tree composition and climate of the area. For example, frequent natural fires does not allow boreal forests to be as old as coastal forests of north western America.
Common cultural definitions and common denominators regarding what comprises old growth forest, and of the variables that define, constitute and embody old-growth forests include:
- The forest habitat possesses relatively mature, old trees;
- The old growth trees have long continuity on the same site;
- The forest itself has not been subjected to significant inhabitation by mankind that has altered the appearance of the landscape and its ecosystems, has not been subjected to logging, and has inherently progressed per natural tendencies.
"Ancient woodland" is a term used in the United Kingdom to refer specifically to woodland dating back to 1600 or before (in England and Wales) or 1750 (in Scotland). Before this, planting of new woodland was uncommon, so a wood present at these dates was likely to have developed naturally. By this definition Ancient Woodland may have been affected by human management, and may have no very ancient trees: the important characteristic is long continuity of woodland on the land.
In the United States, the term "old growth" is often (but not always) used to characterize a forest that has experienced little direct disruption or disturbance by humans during contemporary historical epochs, although sometimes determining the long-term history of human land management can be difficult. Additionally, because landscapes are naturally dynamic and continue to change as time progresses, it is difficult to ascertain hypothetical old growth forest characteristics that may have come into fruition had humans not destroyed such a great deal of old growth forests.
The role of natural disturbances in defining old growth is more ambiguous. For example some definitions exclude recently burned forests, even where fire has been part of the natural forest dynamics for millennia. In other cases such natural disturbance is incorporated in the old-growth concept. However, it is sometimes difficult to distinguish the ecological effects of natural disruption from human-caused disruption. Furthermore, many forests that have never experienced direct manipulation by humans have been subjected to indirect effects in the form of invasive species, removal of native species (including megafauna),climate change, and regional modifications of ecological disturbance regimes (e.g., fire suppression).
Characteristics
Many botanists specifically define old growth in terms of meeting several criteria, under which system forests with sufficient age and minimal disturbance are considered old growth. Typical characteristics of old-growth forest include presence of older trees, minimal signs of human disturbance, mixed-age stands, presence of canopy openings due to tree falls, pit-and-mound topography, fallen timber in various stages of decay, standing snags (dead trees), multi-layered canopies, intact soils, a healthy fungal ecosystem, and presence of indicator species.
Mixed age
Forest in old-growth stage has a mix of tree ages, due to distinct regeneration pattern for this stage. New trees regenerate in different time from each other, because each one of them has different spatial location relative to main canopy and hence each one receive different amount of light. This regeneration pattern is different from regeneration of trees after major disturbance when trees regenerate on the site in relatively similar time. In younger forests trees have similar ages, because they all started to grow in the same time after the old forest stand was killed.
Canopy openings
Forest canopy gaps are essential in creating and maintaining mixed-age stands. Also, some herbaceous plants only become established in canopy openings but persist beneath an understory. Openings are a result of tree death due to small impact disturbances such as wind, low-intensity fires and tree deceases.
Topography
The characteristic topography of much old growth forest consists of pits and mounds. Mounds are caused by decaying fallen trees, and pits (tree throws) by the roots pulled out of the ground when trees fall due to natural causes, including being pushed over by animals. Pits expose humus-poor, mineral-rich soil and often collect moisture and fallen leaves soon form a thick organic layer and so able to nurture certain types of organisms, while mounds provide a place free of leaf inundation and saturation, where other types of organisms thrive.
Standing snags
Standing snags provide food sources and habitat for many types of organisms. In particular, many species of dead-wood predators such as woodpeckers must have standing snags available for feeding. In North America the spotted owl is well-known for needing standing snags for nesting habitat.
Decaying ground layer
Fallen timber contributes carbon-rich organic matter directly to the soil, thus providing a substrate for mosses, fungi and for seedlings, and in creating microhabitats by creating relief on the forest floor. In some ecosystems, such as the temperate rain forest of the North American Pacific coast, fallen timber may become nurse logs, providing a substrate for seedling trees.
Soil
Intact soils harbor many life-forms and usually have well-defined soil profiles. Different organisms may need different soil profiles to adapt to the forest, while many trees need well-structured soils free of disturbance. Some herbaceous plants in northern hardwood forests need thick duff layers (which are part of the soil profile). Fungal ecosystems are essential for efficient in-situ recycling of nutrients back into the entire ecosystem.
Importance
- Old growth forests often contain rich communities of plants and animals that settle there thanks to the long period of forest stability. These varied and sometimes rare species may depend on the unique environmental conditions created by these forests.
- Old growth forest serves as a reservoir for species which cannot thrive or easily regenerate in younger forest, and so can be used as a baseline for research.
- Plant species that are native to old growth forests may someday prove to be invaluable towards curing various human ailments, as has been realized in numerous plants in tropical rainforests.
- Old growth forests also store large amounts of carbon above and below the ground (either as humus, or in wet soils as peat). They collectively represent a very significant store of carbon. Destruction of these forests releases this carbon as greenhouse gases, and may increase the risk of global climate change.
Logging
The large trees in old growth forests are often economically valuable, so these forests have been subjected to aggressive logging around the world. This has led to much controversy between logging companies and environmental groups. An example of this was that over Spotted Owls in the 1980s and 1990s.
In Australia, the regional forest agreement (RFA) attempted to prevent the clearfelling of defined "Old Growth Forests". This led to struggles over what constitutes "Old Growth". For example in Western Australia, the timber industry tried to limit the area of Old Growth in the karri forests of the Southern Forests Region; this led to the creation of the Western Australian Forests Alliance, the splitting of the Liberal Government of Western Australia and the election of the Gallop Labor Government. Old Growth Forests in this region have now been placed inside National Parks. A small proportion of Old Growth Forest also exists in South-West Australia, and is protected by a Federal laws from logging, which hasn't occurred there for more than twenty years.
Locations of remaining intact forests
In 2006 Greenpeace identified that the world's remaining intact old growth forest area was distributed among the continents as follows:
- 35% in Latin America. The Amazon rainforest is mainly located in Brazil, which clears a larger area of forest annually than any other country in the world.
- 28% in North America. North America harvests 10,000 square kilometres of ancient forests every year. Many of the fragmented forests of southern Canada and the US lack adequate animal travel corridors and functioning ecosystems for large mammals.
- 19% in Northern Asia. Northern Asia is home to the largest boreal forest in the world. The Siberian tiger once roamed across huge areas of Northern Asia but today can only be found in a small area of intact forest near the Sea of Japan. Only about 400 remain in the wild and 800 in zoos.
- 8% in Africa. Africa has lost most of its intact forest landscapes in the last 30 years. The timber industry is responsible for destroying huge areas of intact forest landscapes and continues to be the single largest threat to these areas.
- 7% in South Asia Pacific. The Paradise Forests of Asia Pacific are being destroyed faster than any other forest on Earth. Much of the large intact forest landscapes have already been cut down, 72% in Indonesia and 60% in Papua New Guinea.
- Less than 3% in Europe. In Europe, more than 150 square kilometres of intact forest landscapes are cleared every year and the last areas of the region’s intact forest landscapes in European Russia are shrinking rapidly.
Effect on climate change
Old growth forests store large amounts of carbon, which is stored in wood, soil humus and peat. When forests are cut, the trees' wood, soil humus and peat all decay, releasing the carbon as carbon dioxide or methane. Logging practices often include burning of the logged area, releasing further CO2.
While old growth forests are often perceived to be in equilibrium — releasing as much carbon dioxide as they capture; or even in a state of decay, studies of soils in undisturbed tropical rain forests, Siberian woods and in German national parks have found that soils contain enormous amounts of carbon derived from fallen leaves, twigs and buried roots that can bind to soil particles and remain for 1,000 years or more. Replacing old growth forests with plantations is counter-productive from a carbon-storage view, as the new forest may take centuries to recapture the carbon lost. Further, the loss of biodiversity in a plantation monoculture lessens the performance of ecosystems regarding biomass production, nutrient retention and carbon dioxide absorption.
See also
External links
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