Holarctic
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The Holarctic ecozone refers to the habitats found throughout the northern continents of the world as a whole. This region is divided into the Palearctic, consisting of Northern Africa and all of Eurasia, with the exception of Southeast Asia and the Indian subcontinent, and the Nearctic, consisting of North America south to northern Mexico. These are further subdivided into a variety of ecoregions. Many ecosystems, and the animal and plant communities that depend on them, are found across multiple continents in large portions of this ecozone. The continuity of these ecosystems results from the shared glacial history of this ecozone. The Floristic Boreal Kingdom corresponds to the Holarctic ecozone.
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[edit] Major Ecosystems
Within the Holarctic ecozone, there are a variety of ecosystems. The type of ecosystem found in an area depends on the latitude and local geography. In the far north, a band of arctic tundra circles the shore of the Arctic Ocean. The ground beneath this land is permafrost, frozen year-round. In these difficult growing conditions, few plants can survive. South of the tundra, the boreal forest stretches across North America and Eurasia. This land is characterized by coniferous trees. South of here, the ecosystems become more diverse. Some areas are covered in temperate grassland, while others are covered in temperate forest, dominated by deciduous trees. The southern extent of the Holarctic typically reaches into the desert, which is dominated by plants and animals adapted to the dry conditions (Schultz 2007).
[edit] Species with a holarctic distribution
A variety of animal species are distributed across continents, throughout much of the Holarctic ecozone. Some of these included the brown bear, grey wolf, red fox, wolverine, moose, caribou, and common raven.
The brown bear (Ursus arctos) is found in mountainous and semi-open areas distributed throughout the Holarctic. It once occupied much larger areas, but has been driven out by human development and the resulting habitat fragmentation. Today it is only found in remaining wilderness areas (Wikipedia).
The grey wolf (Canis lupus) is found in a wide variety of habitats from tundra to desert, with different populations adapted for each. Its historical distribution encompasses the vast majority of the Holarctic Ecozone, though human activities such as development and active extermination have extirpated the species from much of this range (Wikipedia).
The red fox (Vulpes vulpes) is a highly adaptable predator. It has the widest distribution of any terrestrial carnivore, and is adapted to a wide range of habitats, including areas of intense human development. Like the wolf, it is distributed throughout the majority of the Holarctic, but it has avoided extirpation (Wikipedia).
The wolverine (Gulo gulo) is a large member of the weasel family found primarily in the arctic and in boreal forests, ranging south in mountainous regions. It is distributed in such areas throughout Eurasia and North America (Wikipedia).
The moose (Alces alces) is the largest member of the deer family. It is found throughout most of the boreal forest from Scandinavia through Eurasia and into eastern North America. In some areas it ranges south into the deciduous forest (Wikipedia).
The caribou, or reindeer (Rangifer tarandus) is found in boreal forest and tundra in the northern parts of the Holarctic. In Eurasia it has been domesticated. It is divided into several subspecies, which are adapted to different habitats and geographic areas (Wikipedia).
The common raven (Corvus corax) is the most widespread of the corvids, and one of the largest. It is found in a variety of habitats, but primarily wooded northern areas. It has been known to adapt well to areas of human activity. Their distribution also makes up most of the Holarctic Ecozone.
[edit] Origin
The continuity of the northern parts of the holarctic results from their shared glacial history. During the Pleistocene, these areas were subjected to repeated glaciations. Icecaps expanded, scouring the land of life and reshaping its topography. During glacial periods, species survived in refugia, small areas that maintained a suitable climate due to local geography. These areas are believed to have been primarily in southern regions, but some genetic and paleontological evidence points to additional refugia in the sheltered areas of the north (Stewart and Lister 2001).
Wherever these areas were found, they became a source populations during interglacial periods. When the glaciers receded, plants and animals spread rapidly into the newly opened areas. Different taxa responded differently to these rapidly changing conditions. Tree species spread outward from refugia during interglacial periods, but in varied patterns, with different trees dominating in different periods (Taberlet and Chedadi 2002). Insects, on the other hand, shifted their ranges with the climate, maintaining consistency in species for the most part throughout the period (Coope 1994). Their high degree of mobility allowed them to move as the glaciers advanced or retreated, maintaining a constant habitat despite the climatic oscillations. Despite their apparent lack of mobility, plants managed to colonize new areas rapidly as well. Studies of fossil pollen indicate that trees recolonized these lands at an exponential rate (Bennet 1986). Mammals recolonized at varying rates. Brown bears, for instance, moved quickly from refugia with the receding glaciers, becoming one of the first large mammals to recolonize the land (Sommer and Benecke 2005). The last glacial period ended about 10,000 years ago, resulting in the present distribution of ecoregions.
Another factor contributing to the continuity of Holarctic ecosystems is the movement between continents allowed by the Bering land bridge, which was exposed by the lowing of sea level due to the expansion of the ice caps. The communities found in the Palearctic and the Nearctic are different, but have many species in common. This is the result of several faunal interchanges that took place across the Bering land bridge. However, these migrations were mostly limited to large, cold-tolerant species (Rodriguez et al 2006). Today it is mainly these species which are found throughout the ecozone.
[edit] Threats
As the Holarctic is an enormous area, it is subject to environmental problems of international scale. The primary threats throughout the region result from global warming and habitat fragmentation. The former is of particular concern in the north, as these ecosystems are adapted to cold. The latter is more of a concern in the south, where development is prevalent.
Global warming is a threat to all the Earth's ecosystems, but it is a more immediate threat to those found in cold climates. The communities of species found at these latitudes are adapted to the cold, so any significant warming can upset the balance. For instance, insects struggle to survive the cold winters typical of the boreal forest. Many do not make it, especially in harsh winters. However, recently the winters have grown milder, which has had a drastic effect on the forest. Winter mortality of some insect species drastically decreased, allowing the population to build on itself in subsequent years. In some areas the effects have been severe. Spruce beetle outbreaks have wiped out up to ninety percent of the Kenai Peninsula's spruce trees; this is blamed primarily on a series of unusually warm years since 1987 (Logan et al 2003).
In this case a native species has caused massive disturbance of habitat as a result of climate change. Warming temperatures may also allow pest species to enlarge their range, moving into habitats that were previously unsuitable. Studies of potential areas for outbreaks of bark beetles indicate that as the climate shifts, these beetles will expand to the north and to higher elevations than they have previously affected (Williams & Liebhold 2002). With warmer temperatures, insect infestation will become a greater problem throughout the northern parts of the Holarctic.
Another potential effect of global warming to norther ecosystems is the melting of permafrost. This can have significant effects on the plant communities that are adapted to the frozen soil, and may also have implications for further climate change. As permafrost melts, any trees growing above it may die, and the land shifts from forest to peatland. In the far north, shrubs may later take over what was formerly tundra. The precise effect depends on whether the water that was locked up is able to drain off. In either case, the habitat will undergo a shift. Melting permafrost may also accelerate climate change in the future. Within the permafrost, vast quantities of carbon are locked up. If this soil melts, the carbon may be released into the air as either carbon dioxide or methane. Both of these are greenhouse gases (Stokstad 2004).
Habitat fragmentation threatens a wide variety of habitats throughout the world, and the Holoarctic is no exception. Fragmentation has a variety of negative effects on populations. As populations become cut off, their genetic diversity suffers and they become susceptible to sudden disasters and extinction. While the northern parts of the Holarctic represent some of the largest areas of wilderness left on Earth, the southern parts are in some places extensively developed. This ecozone contains most of the worlds developed countries, including the United States and the nations of Western Europe. Temperate forests were the primary ecosystem in many of the most developed areas today. These lands are now used for intensive agriculture or have become urbanized. As lands have been developed for agricultural uses and human occupation, natural habitat has for the most part become limited to areas considered unsuitable for human use, such as slopes or rocky areas (Schultz 2007). This pattern of development limits the ability of animals, especially large ones, to migrate from place to place.
Large carnivores are particularly affected by habitat fragmentation. These mammals, such as brown bears and wolves, require large areas of land with relatively intact habitat to survive as individuals. Much larger areas are required to maintain a sustainable population. They may also serve as keystone species, regulating the populations of the species they prey on. Thus, their conservation has direct implications for a wide range of species, and is difficult to accomplish politically due to the large size of the areas they need (Paquet 1996). With increasing development, these species in particular are at risk, which could have effects that carry down throughout the ecosystem.
[edit] Conservation Actions
The threats to the Holarctic ecozone are not going unrecognized. Many efforts are being made to mitigate these threats, with the hope of preserving the biodiversity of the region. International agreements to combat global warming may help to lessen the effects of climate change on this region. Efforts are also underway to fight habitat fragmentation, both on local and regional scales.
The most comprehensive effort to combat global warming to date is the Kyoto Protocol. Developed countries who sign this protocol agree to cut their collective greenhouse gas emissions by five percent since 1990 by sometime between 2008 and 2012. The vast majority of these nations are found within the Holarctic. Each country is given a target for emission levels, and they may trade emissions credits in a market-based system that includes developing countries as well. Once this period is ended, a new agreement will be written to further mitigate the effects of climate change. The process of drafting a new agreement has already begun. In late 2007, an international meeting in Bali was held to begin planning for the successor to the Kyoto Protocol. This agreement will aim to build on the successes and failures of Kyoto to produce a more effective method of cutting greenhouse gas emissions (UNFCCC). If these efforts are successful, the biodiversity of the Holarctic and the rest of the world will see fewer effects of climate change.
Fighting habitat fragmentation is a major challenge in conserving the wide-ranging species of the Holarctic. Some efforts are limited to a local scale of protection, while others are regional in scope. Local efforts include creating reserves and establishing safe routes for animals to cross roads and other human-made barriers. Regional efforts to combat habitat fragmentation take a broader scope.
One major such effort in the Holarctic is the Yellowstone to Yukon Conservation Initiative. This organization was started in 1997 to help establish a contiguous network of protection for the northern Rocky Mountains, from mid Wyoming to the border between Alaska and Canada's Yukon. It brings together a wide variety of environmental organizations for a shared purpose. The goal of the Initiative is to create a core of protected areas, connected by corridors and surrounded by buffer zones. This will build on the many existing protected areas in this region, with a focus on integrating existing and future human activities into the conservation plan rather than seeking to exclude them (Yellowstone to Yukon). If these efforts are successful, they will be especially beneficial to wide-ranging species such as grizzly bears. If these species can survive, other members of the communities they live in will survive as well.
[edit] Conclusion
The Holarctic Ecozone represents an enormous area, made up of a variety of habitats. These habitats are diverse, but have some commonalities that stretch across continents. Many plant and animal species are found across continents as well. These similarities result from the shared glacial history of these regions. Habitat fragmentation and global climate change are responsible for many threats to these ecosystems, but actions are being taken to mitigate these threats.
[edit] References
Bennet, K. D.; J. H. Lawton; A. Gibbs; M. H. Williamson; M. W. Holdgate; W. D. Hamilton; G. R. Conway. 1986. The Rate of Spread and Population in Increase of Forest Trees During the Postglacial [and Discussion]. Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences 314:1167:523-531
Rodriguez, J;J. Hortal.;M. Nieto. 2006. An evaluation of the influence of environment and biogeography on community structure: the case of Holarctic mammals. Journal of Biogeography Vol. 33:2:291-303
Williams, D. W.; A. M. Liebhold. 2002. Climate change and the outbreak ranges of two North American bark beetles. Agricultural and Forest Entomology 4:2:87–99.
Taberlet, P.; R. Cheddadi 2002. Quaternary Refugia and Persistence of Biodiversity (in Science's Compass; Perspectives). Science, New Series 297:5589:2009-2010.
Coope, G. R.; A. S. Wilkins. 1994. The Response of Insect Faunas to Glacial-Interglacial Climatic Fluctuations [and Discussion] (in Historical Perspective). Philosophical Transactions: Biological Sciences 344:1307:19-26.
Logan, J. A.; J. Régnière; J. A. Powell. 2003. Assessing the Impacts of Global Warming on Forest Pest Dynamics (in Reviews). Frontiers in Ecology and the Environment 1:3:130-137.
Paquet, P. C.; R. F. Noss; H. B. Quigley; M. G. Hornocker; T. Merrill. 1996. Conservation Biology and Carnivore Conservation in the Rocky Mountains (in Special Section: Large Carnivore Conservation in the Rocky Mountains of the United States and Canada). Conservation Biology 10:4:949-963.
Stewart, J.R.; A.M. Lister. 2001. Cryptic northern refugia and the origins of the modern biota. Trends in Ecology and Evolution 16:11:608-613.
Stokstad, E. 2004. Defrosting the Carbon Freezer of the North. Science 304:5677:1618-1620
Sommer, R. S.; N. Benecke. 2005. The recolonization of Europe by brown bears Ursus arctos Linnaeus, 1758 after the Last Glacial Maximum. Mammal Review 35:2:156-164.
United Nations Framework Convention on Climate Change. Available at: http://unfccc.int/2860.php. Accessed December 2007.
Yellowstone to Yukon Conservation Initiative. Updated 2006. Available at http://www.y2y.net. Accessed December 2007.
Schultz, J. 2007. The Ecozones of the World. Translated by B. Ahnert. Second Edition. Springer, Verlag, Netherlands.
