The Serengeti (//) ecosystem is a geographical region in Africa. It is located in north Tanzania and extends to south-western Kenya between latitudes 1 and 3 degrees south latitude and 34 and 36 degrees east longitude. It spans approximately 30,000 km2 (12,000 sq mi). The Kenyan part of the Serengeti is known as Maasai Mara.
The Serengeti hosts the largest terrestrial mammal migration in the world, which helps secure it as one of the Seven Natural Wonders of Africa and one of the ten natural travel wonders of the world. The Serengeti is also renowned for its large lion population and is one of the best places to observe prides in their natural environment. The region contains the Serengeti National Park in Tanzania and several game reserves.
Approximately 70 larger mammal and 500 bird species are found there. This high diversity is a function of diverse habitats, including riverine forests, swamps, kopjes, grasslands, and woodlands. Blue wildebeests, gazelles, zebras, and buffalos are some of the commonly found large mammals in the region.
Much of the Serengeti was known to outsiders as Maasailand. The Maasai are known as fierce warriors and live alongside most wild animals with an aversion to eating game and birds, subsisting exclusively on their cattle. Historically, their strength and reputation kept the newly arrived Europeans from exploiting the animals and resources of most of their land. A rinderpest epidemic and drought during the 1890s greatly reduced the numbers of both Maasai and animal populations. The Tanzanian government later in the 20th century re-settled the Maasai around the Ngorongoro Crater. Poaching and the absence of fires, which had been the result of human activity, set the stage for the development of dense woodlands and thickets over the next 30–50 years. Tsetse fly populations now prevented any significant human settlement in the area.
By the mid-1970s, wildebeest and the Cape buffalo populations had recovered and were increasingly cropping the grass, reducing the amount of fuel available for fires. The reduced intensity of fires has allowed Acacia to once again become established.
Each year around the same time, the circular great wildebeest migration begins in the Ngorongoro Conservation Area of the southern Serengeti in Tanzania. This migration is a natural phenomenon determined by the availability of grazing. This phase lasts from approximately January to March, when the calving season begins – a time when there is plenty of rain-ripened grass available for the 260,000 zebra that precede 1.7 million wildebeest and the following hundreds of thousands of other plains game, including around 470,000 gazelles.
During February, the wildebeest spend their time on the short grass plains of the southeastern part of the ecosystem, grazing and giving birth to approximately 500,000 calves within a 2 to 3-week period. Few calves are born ahead of time and of these, hardly any survive. The main reason is that very young calves are more noticeable to predators when mixed with older calves from the previous year. As the rains end in May, the animals start moving northwest into the areas around the Grumeti River, where they typically remain until late June. The crossings of the Grumeti and Mara rivers beginning in July are a popular safari attraction because crocodiles are lying in wait. The herds arrive in Kenya in late July / August, where they stay for the remainder of the dry season, except that the Thomson's and Grant's Gazelles move only east/west. In early November, with the start of the short rains the migration starts moving south again, to the short grass plains of the southeast, usually arriving in December in plenty of time for calving in February.
About 250,000 wildebeest die during the journey from Tanzania to the Maasai Mara National Reserve in southwestern Kenya, a total of 800 kilometres (500 mi). Death is usually from thirst, hunger, exhaustion, or predation.
The Serengeti has some of East Africa's finest game areas. The governments of Tanzania and Kenya maintain a number of protected areas, including national parks, conservation areas, and game reserves, that give legal protection to over 80 percent of the Serengeti.
The southeastern area lies in the rain shadow of the Ngorongoro Conservation Area's highlands and is composed of shortgrass treeless plains with abundant small dicots. Soils are high in nutrients, overlying a shallow calcareous hardpan. A gradient of soil depth northwestward across the plains results in changes in the herbaceous community and taller grass. About 70 kilometres (43 mi) west, Acacia woodlands appear suddenly and stretch west to Lake Victoria and north to the Loita Plains, north of the Maasai Mara National Reserve. The sixteen Acacia species vary over this range, their distribution determined by edaphic conditions and soil depth. Near Lake Victoria, flood plains have developed from ancient lakebeds.
In the far northwest, Acacia woodlands are replaced by broadleaved Terminalia-Combretum woodlands, caused by a change in geology. This area has the highest rainfall in the system and forms a refuge for the migrating ungulates at the end of the dry season.
Altitudes in the Serengeti range from 920 to 1,850 metres (3,020 to 6,070 ft) with mean temperatures varying from 15 to 25 °C (59 to 77 °F). Although the climate is usually warm and dry, rainfall occurs in two rainy seasons: March to May, and a shorter season in October and November. Rainfall amounts vary from a low of 508 millimetres (20 in) in the lee of the Ngorongoro highlands to a high of 1,200 millimetres (47 in) on the shores of Lake Victoria. The highlands, which are considerably cooler than the plains and are covered by montane forest, mark the eastern border of the basin in which the Serengeti lies.
The Serengeti plain is punctuated by granite and gneiss outcroppings known as kopjes. These outcroppings are the result of volcanic activity. Kopjes provide a microhabitat for non-plains wildlife. One kopje likely to be seen by visitors to the Serengeti is the Simba Kopje (Lion Kopje). The Serengeti was used as inspiration for the animated Disney feature film The Lion King and subsequent theatrical production.
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- Seven Natural Wonders of Africa
- Partridge, Frank (20 May 2006). "The fast show". The Independent (London). Retrieved 2007-03-14.
- Nolting, Mark (2012). Africa's Top Wildlife Countries. Global Travel Publishers Inc. p. 356. ISBN 978-0939895151.
- http://www.ath.aegean.gr/srcosmos/showpub.aspx?aa=8868[dead link]
- Briggs, Phillip (2006), Northern Tanzania: The Bradt Safari Guide with Kilimanjaro and Zanzibar, Bradt Travel Guides, p. 198, ISBN 978-1-84162-146-3
- "Maa (Maasai) Dictionary". Darkwing.uoregon.edu. Retrieved 2010-10-23.
- Morell, Virginia (1997), "Return of the Forest", Science 278 (5346): 2059, doi:10.1126/science.278.5346.2059
- Sinclair, Anthony Ronald Entrican; Arcese, Peter, eds. (1995). Serengeti II: Dynamics, Management, and Conservation of an Ecosystem. University of Chicago Press. pp. 73–76. ISBN 978-0-226-76032-2. Retrieved 2010-10-23.
- Anouk Zijlma. "The Great Annual Wildlife Migration – The Great Migration of Wildebeest and Zebra". About.com. Retrieved 3 June 2014.
- "How to Get There, Ngorongoro Crater". Ngorongoro Crater Tanzania. 2013. Retrieved 3 June 2014.
- "Ngorongoro Conservation Area". United Nations Educational, Scientific and Cultural Organization – World Heritage Centre. Retrieved 3 June 2014.
- Croze, Harvey; Mari, Carlo; Estes, Richard D. (2000). Serengeti's Great Migration. Abbeville Press. ISBN 978-0-789-20669-5.
- Pavitt, Nigel (2001), Africa's Great Rift Valley, Harry N. Abrams, p. 122, ISBN 978-0-8109-0602-0
- Sinclair, A. R. E.; Mduma, Simon A. R.; Fryxell, John M. (2008), Serengeti III: Human Impacts on Ecosystem Dynamics, Chicago: University of Chicago Press, p. 11, ISBN 978-0-226-76033-9
- Sinclair, A. R. E.; Mduma, S. A.; Hopcraft, J. G.; Fryxell, J. M.; Hilborn, R.; Thirgood, S. (2007), "Long-Term Ecosystem Dynamics in the Serengeti: Lessons for Conservation" (PDF), Conservation Biology 21 (3): 580–590, doi:10.1111/j.1523-1739.2007.00699.x
- "The Serengeti National Park". Glcom.com. Retrieved 2010-10-23.