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Dictionary:
old growth (ōld'grōth') adj. |
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| WordNet: old growth |
The noun has one meaning:
Meaning #1:
forest or woodland having a mature or overly mature ecosystem more or less uninfluenced by human activity
Synonym: virgin forest
| Wikipedia: 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 forest which contains trees which have attained great age (and associated structural features) and so exhibits unique ecological features[1].
Old-growth forest typically contains large and old live trees, large dead trees (sometimes called "snags"), and large logs. Individual tree mortality creates gaps in the main canopy layer, allowing light to penetrate the main canopy and create favorable photosynthetic conditions for the understory (which is why old-growth understory is more developed than in immature stands).
Forest that is regenerated after severe disruptions, such as clear-cutting 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.
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 itself, but also indigenous species that rely upon old-growth forest habitat.[2][3]
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 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.
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The definitions of old-growth forest fall into three major categories: ecological, social, and economic definitions.[4]
Most definitions use forest characteristics to define old-growth forest. Usually the characteristics include presence of old trees, dead standing snags, a multilayered canopy dominated by large overstory trees, and accumulations of large dead woody material.[5][6]
From stand dynamics perspective, old-growth forest is a forest in a stage that follows Understory Reinitiation stage.[7] A review of the stages helps to understand the concept:
It is important to note that while the stand switches from one tree community to another, it is not necessarily that the stand will go through old-growth stage in between. Some tree species have relatively open canopy. That allows more shade-tolerant tree species to establish below even before Understory Reinitiation stage. The shade-tolerant trees will eventually out-compete the main canopy trees in stem-exclusion stage. Therefore, the dominant tree species will change, but the forest will still be in Stem-Exclusion stage.
Stand age can also be used to categorize forest as old-growth.[8] For each geographical area, there is an average time since disturbance when the forest will reach old-growth stage. This method is useful, because it allows quick and objective determination of forest stage. However, this definition does not provide explanation about forest function. It just gives a useful number to measure. Due to that fact, some forests may be excluded from being categorized as old-growth even if they have old-growth attributes just because they are too young. Also, older forests can lack some old-growth attributes and be categorized as old-growth just because they are so old. The idea of using age is also problematic, because human activities can influence the forest in varied ways. For example, after logging of 30% of the trees, we can wait less time for old-growth to come back than after removal of 80% of the trees.
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:
"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 North America, 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).
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.
A forest in old-growth stage has a mix of tree ages, due to a distinct regeneration pattern for this stage. New trees regenerate at different times from each other, because each one of them has different spatial location relative to the main canopy and hence each one receives a different amount of light. This regeneration pattern is different from the regeneration of trees after a 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 at the same time, after the old forest stand was killed.
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 diseases.
Old-growth forests are unique, usually having multiple horizontal layers of vegetation representing a variety of tree species, age classes, and sizes, as well as "pit and mound" soil shape with well-established fungal nets.[9] Because old-growth forest is structurally diverse it provides higher-diversity habitat than forests in other stages. Thus, sometimes higher biological diversity can be sustained in old-growth forest, or at least a biodiversity that is different from other forest stages.
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, forming a thick organic layer that is able to nurture certain types of organisms. Mounds provide a place free of leaf inundation and saturation, where other types of organisms thrive.
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.
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.
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[clarification needed] layers (which are part of the soil profile). Fungal ecosystems are essential for efficient in-situ recycling of nutrients back into the entire ecosystem.
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.
In 2006 Greenpeace identified that the world's remaining Intact forest landscapes are distributed among the continents as follows:[14]
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.[17] 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,[18] 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.[19]
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