Serengeti National Park

The Serengeti National Park is a large national park in northern Tanzania that stretches over 14,763 km2 (5,700 sq mi).[1] It is located entirely in eastern Mara Region and north east portion of Simiyu Region and contains over 1,500,000 hectares (3,700,000 acres) of virgin savanna. The park was established in 1940.

Serengeti National Park
Swahili: Hifadhi ya Serengeti
Landscape in Serengeti National Park
LocationTanzania
Coordinates2°20′S 34°34′E
Area14,763 km2 (5,700 sq mi)
Established1951
Visitors350,000 per year
Governing bodyTanzania National Parks Authority
TypeNatural
Criteriavii, x
Designated1981 (5th session)
Reference no.156
RegionAfrica

The Serengeti is well known for the largest annual animal migration in the world of over 1.5 million blue wildebeest and 250,000 zebra along with smaller herds of Thomas' Gazelle and eland.[2] The national park is also home to the largest lion population in Africa. It is under threat from deforestation, population growth and ranching.

Etymology

The name "Serengeti" is an approximation of the word siringet used by the Maasai people for the area, which means "the place where the land runs on forever".[3][4]

History

In 1930, an area of 2,286 square kilometres (883 sq mi) was designated as a game reserve in southern and eastern Serengeti.[5] In the 1930s, the government of Tanganyika established a system of national parks compliant with the Convention Relative to the Preservation of Fauna and Flora in their Natural State. The area became a national park in 1940. It was granted strict protection in 1948 when the Serengeti National Park Board of Trustees was formed to administer the national park. The government restricted the movements of the resident Maasai people, and the park boundaries were finalized in 1951.[6] In 1959, an area of 8,300 km2 (3,200 sq mi) was split off in the eastern part of the national park and re-established as Ngorongoro Conservation Area intended to accommodate the traditional land use interests of the Maasai people in a multiple land use area.[7] In 1981, the Serengeti National Park covered 12,950 km2 (5,000 sq mi), which was less than half of the Serengeti.[8]

The Serengeti gained fame after Bernhard Grzimek and his son Michael produced a book and documentary titled Serengeti Shall Not Die in 1959.[9]

Wildlife

Serengeti National Park forms a Lion Conservation Unit since 2005 together with Maasai Mara National Reserve.[10] More than 3,000 lions live in this ecosystem.[11] The population density of the African leopard is estimated at 5.41 individuals per 100 km2 (39 sq mi) in the dry season.[12]

African bush elephant herds recovered from a population low in the 1980s caused by poaching, and numbered over 5,000 individuals by 2014.[13] The African buffalo population declined between 1976 and 1996 due to poaching, but increased to 28,524 individuals by 2008.[14] The black rhinoceros population was reduced to about 10 individuals in the 1980s due to poaching, and less than 70 individuals survive in the park today.[15] Rhinos mostly browse on grasses, woody Indigofera, Acacia and Crotalaria forbs and shrubs.[16]

Other mammal carnivores include the Cheetah,[17] about 3,500 spotted hyena, Black-backed jackal, African golden wolf, honey badger, striped hyena, caracal, serval, banded mongoose, and two species of otters. The African wild dog was reintroduced to the area in 2012 after disappearing in 1991.[18] Other mammals include hippopotamus, common warthog, aardvark, aardwolf, African wildcat, African civet, common genet, zorilla, african striped weasel, bat-eared fox, ground pangolin, crested porcupine, three species of hyraxes and cape hare.[19] Primates such as yellow and olive baboons, patas monkeys, and vervet monkey, mantled guereza are also seen in the gallery forests of the Grumeti River.[19]

Reptiles include Nile crocodile, leopard tortoise, serrated hinged terrapin, rainbow agama, Nile monitor,Jackson's chameleon , African python, black mamba, black-necked spitting cobra, and puff adder.

More than 500 bird species can be seen such as Masai ostrich, secretarybird, kori bustards, helmeted guineafowls, Grey-breasted spurfowl, blacksmith lapwing, african collared dove, red-billed buffalo weaver, southern ground hornbill, crowned cranes, sacred ibis, cattle egrets, black herons, knob-billed ducks, saddle-billed storks, white stork, goliath herons, marabou storks, yellow-billed stork, spotted thick-knees, lesser flamingo, shoebills, abdim's stork, hamerkops, hadada ibis, african fish eagles, pink-backed pelicans, tanzanian red-billed hornbill, martial eagles, egyptian geese, lovebirds, spur-winged geese, oxpeckers, and many species of vultures.[20][21]

Great migration

The great migration is the world's longest overland migration. The complete migration route is around 800 km (500 mi). South of this migration route covers the Ngorongoro Conservation Area where around half a million Wildebeest are born between January and March. By March, at the beginning of the dry season, roughly 1.5 million and 250,000 zebras start to migrate heading north towards Maasai Mara in Kenya. Common eland, plains zebra, and Thomson's gazelle join the wildebeest. In April and May, the migrating herds pass through the Western Corridor. To get to the Maasai Mara, the herds have to cross the Grumeti and Mara Rivers where around 3,000 crocodiles lie in wait. For every wildebeest captured by the crocodiles, 50 drown. When the dry season ends in late October, the migrating herds start to head back south. Around 250,000 wildebeests and 30,000 plains zebras die annually from drowning, predation, exhaustion, thirst, or disease.[22]

Geology

Carbonatite lava at Ol Doinyo Lengai volcano

The basement complex consists of Archaen Nyanzian System greenstones (2.81–2.63 Ga in age), Archaean granite-gneiss plutons (2.72–2.56 Ga in age), which were uplifted 180 Ma ago) forming koppies and elongated hills, the Neoproterozoic Mozambique Belt consisting of quartzite and granite, and the Neoproterozoic Ikorongo Group, consisting of sandstone, shale and siltstone that form linear ridges. The southeast portion of the park contains Neogene-aged volcanic rock and Oldoinyo Lengai Holocene-aged volcanic ash. The Grumeti, Mara, Mbalageti, and Orangi rivers flow westward to Lake Victoria, while the Oldupai River flows eastward into the Olbalbal Swamps.[23]

On the eastern portion of the park lies the Serengeti volcanic grasslands which is a Tropical Grassland Ecozone. The grasslands grow on deposits of volcanic ash from the Kerimasi Volcano, which erupted 150,000 years ago, and also from the Ol Doinyo Lengai volcanic eruptions, which created layers of calcareous tuff and calcitic hard-pan soil (vertisols) from rapid weathering of the natrocarbonatite lava produced by the volcanoes.[24][25][26]

Geography

Serengeti Plains
Wildebeest in the Western Corridor

The park covers 14,750 km2 (5,700 sq mi)[27] of grassland plains, savanna, riverine forest, and woodlands. The park lies in northwestern Tanzania, bordered to the north by the Kenyan border, where it is continuous with the Maasai Mara National Reserve. To the southeast of the park is the Ngorongoro Conservation Area, to the southwest lies Maswa Game Reserve, to the west are the Ikorongo and Grumeti Game Reserves, and to the northeast and east lies the Loliondo Game Control Area.

The landscape of the Serengeti Plain is extremely varied, ranging from savannah to hilly woodlands to open grasslands. The region's geographic diversity is due to the extreme weather conditions that plague the area, particularly the potent combination of heat and wind. The diverse habitats in the region may have originated from a series of volcanoes, whose activity shaped the basic geographic features of the plain by adding mountains and craters to the landscape.

The Mara River, which flows through Maasai Mara National Reserve from the Kenyan highlands to Lake Victoria, is the only permanently-flowing river in the Serengeti ecosystem.[28]

The park is divided into three regions:

  • Serengeti plains: The best-known feature of the Serengeti is the almost treeless grassland in the south. It has kopjes, granite formations that serve as observation posts for predators. The Volcanic Grasslands is a edaphic plant community that grows on soils derived from volcanic ash from nearby volcanos.
  • Western corridor: The main geographic feature is the pair of rivers, Grumeti and Mbalageti. There are big groups of riverine forest and some small mountain ranges. The great migration passes through the corridor from May to July. It stretches to Lake Victoria. The area is flatter than the northern parts of the park and more densely covered with plants than the southern plains.
  • Northern Serengeti: the landscape is dominated by open woodlands, predominantly Commiphora and hills, ranging from Seronera in the south to the Mara River on the Kenyan border. It is remote and relatively inaccessible.

Human habitation is forbidden in the park except for the Tanzania National Parks Authority staff, researchers and staff of the various lodges, campsites, and hotels. The main settlement is Seronera with its primary airstrip.

Administration and protection

Siam weed, a introduced invasive species

The park is listed by the United Nations Educational, Scientific and Cultural Organization as a World Heritage Site. It is designated as a Category II protected area under the system developed by the International Union for Conservation of Nature, which means that it should be managed to protect the ecosystem or ecological processes.[29]

The administrative body for all parks in Tanzania is the Tanzania National Parks Authority. Myles Turner was one of the park's first game wardens and is credited with bringing its rampant poaching under control.[30]

Threats

Deforestation in the Mau Forest region has changed the hydrology of the Mara River.[31] There are invasive species of plants such as Siam weed, Prickly pear, Feverfew and Mexican sunflower.[32] A study in 1996 estimated that the human population of the western side of the park is growing by four percent yearly.[21] Livestock use is also growing which increased the amount of land turned over to farming and ranching. A study by the World Conservation Monitoring Centre in 2001 estimated that roughly 200,000 animals are killed by poaching every year.[21]

References

  1. "Black rhino dies aged 43 in Tanzania's Serengeti National Park-Xinhua". english.news.cn. Retrieved 17 April 2022.
  2. Sinclair, Anthony Ronald Entrican (1995). Serengeti II: Dynamics, Management, and Conservation of an Ecosystem. University of Chicago Press. p. 15.
  3. Poole, R. M. (2012). "Heartbreak on the Serengeti (continued)". National Geographic Magazine. Archived from the original on 29 June 2012. Retrieved 26 September 2019.
  4. "Serengeti National Park – Kalama Safaris". Retrieved 3 August 2021.
  5. "Serengeti National Park travel information - Tanzania". serengeti.com. Retrieved 3 August 2021.
  6. Neumann, R.P. (1995). "Ways of seeing Africa: colonial recasting of African society and landscape in Serengeti National Park". Ecumene. 2 (2): 149–169. doi:10.1177/147447409500200203. S2CID 145421779.
  7. Wanitzek, U. & Sippel, H. (1998). "Land rights in conservation areas in Tanzania". GeoJournal. 46 (2): 113–128. doi:10.1023/A:1006953325298. S2CID 150734077.
  8. Makacha, S.; Msingwa, M.J. & Frame, G.W. (1982). "Threats to the Serengeti herds". Oryx. 16 (5): 437–444. doi:10.1017/S0030605300018111.
  9. Boes, T. (2013). "Political animals: Serengeti Shall Not Die and the cultural heritage of mankind". German Studies Review. 36 (1): 41–59. JSTOR 43555291.
  10. IUCN Cat Specialist Group (2006). Conservation Strategy for the Lion Panthera leo in Eastern and Southern Africa. Pretoria, South Africa: IUCN.
  11. Mésochina, P.; Mbangwa, O.; Chardonnet, P.; Mosha, R.; Mtui, B.; Drouet, N. & Kissui, B. (2010). Conservation status of the lion (Panthera leo Linnaeus, 1758) in Tanzania (Report). Paris: SCI Foundation, MNRT-WD, TAWISA & IGF Foundation.
  12. Allen, M.L.; Wang, S.; Olson, L.O.; Li, Q. & Krofel, M. (2020). "Counting cats for conservation: seasonal estimates of leopard density and drivers of distribution in the Serengeti". Biodiversity and Conservation. 29 (13): 3591–3608. doi:10.1007/s10531-020-02039-w. S2CID 221167378.
  13. Mduma, H.; Musyoki, C.; Maliti Kyale, D.; Nindi, S.; Hamza, K.; Ndetei, R.; Machoke, M.; Kimutai, D.; Muteti, D.; Maloba, M.; Bakari, S. & Kohi, E. (2014). Aerial Total Count of Elephants and Buffaloes in the Serengeti-Mara Ecosystem (PDF) (Report). Nairobi, Kenya: WWF-World Wide Fund For Nature. Archived from the original (PDF) on 9 September 2016.
  14. Metzger, K.L.; Sinclair, A.R.E.; Hilborn, R.; Hopcraft, J.G.C. & Mduma, S.A. (2010). "Evaluating the protection of wildlife in parks: the case of African buffalo in Serengeti". Biodiversity and Conservation. 19 (12): 3431–3444. doi:10.1007/s10531-010-9904-z.
  15. "How black rhinos and local communities help each other in Namibia". Mongabay Environmental News. 2015.
  16. Anderson, T.M.; Ngoti, P.M.; Nzunda, M.L.; Griffith, D.M.; Speed, J.D.; Fossøy, F.; Røskaft, E. & Graae, B.J. (2020). "The burning question: does fire affect habitat selection and forage preference of the black rhinoceros Diceros bicornis in East African savannahs?". Oryx. 54 (2): 234–243. doi:10.1017/S0030605318000388.
  17. "Tanzania: Concern As Serengeti Leopards Resort to Cannibalism". allafrica. Retrieved 23 July 2019.
  18. "Why did Serengeti's wild dogs disappear? Study challenges controversial hypothesis". Mongabay Environmental News. 2019. Retrieved 28 May 2021.
  19. Kennedy, A. S.; Kennedy, V. (2014). Animals of the Serengeti, and Ngorongoro Conservation Area. Princeton, New Jersey. ISBN 978-1-4008-5138-6. OCLC 873760148.
  20. "Bird Checklist for Serengeti National Park". www.exoticbirding.com. Retrieved 28 May 2021.
  21. "Eastern Africa: the Greater Serengeti grassland ecosystem in northern Tanzania | Ecoregions | WWF". World Wildlife Fund. Retrieved 7 June 2021.
  22. Medina, N. (2019). Where Is the Serengeti?. WhoHQ. New York: Penguin Random House. ISBN 9781524792565.
  23. Scoon, Roger (2018). Geology of National Parks of Central/ Southern Kenya and Northern Tanzania: Geotourism of the Gregory Rift Valley, Active Volcanism and Regional Plateaus. Springer. pp. 69–79. ISBN 9783319737843.
  24. "Global Volcanism Program | Ol Doinyo Lengai". Smithsonian Institution | Global Volcanism Program. Retrieved 25 May 2021.
  25. "Hawaiian Volcano Observatory". volcanoes.usgs.gov. Retrieved 25 June 2021.
  26. Kindt, R., Lillesø, J.-P. B., van Breugel, P., Bingham, M., Sebsebe Demissew, Dudley, C., Friis, I., Gachathi, F., Kalema, J., Mbago, F., Minani, V., Moshi, H. N., Mulumba, J., Namaganda, M., Ndangalasi, H.J., Ruffo, C.K., Jamnadass, R. and Graudal, L. 2011. Potential natural vegetation of eastern Africa. Volume 5: Description and tree species composition for other potential natural vegetation types. Forest & Landscape Working Paper 65-2011
  27. World Database on Protected Areas (2021). "Serengeti National Park". Protected Planet, United Nations Environment World Conservation Monitoring Centre. Retrieved 24 May 2021.
  28. "Geology of Serengeti National Park - Tanzania". serengeti.com. Retrieved 14 July 2021.
  29. "Category II: National Park". International Union for the Conservation of Nature. 5 February 2016. Retrieved 18 June 2020.
  30. "Serengeti – Myles Turner". Retrieved 22 October 2016.
  31. Conniff, R. (2015). "A New Threat in the Serengeti to the World's Greatest Animal Migration". Take Part. Retrieved 23 May 2021.
  32. "Conservation". Grumeti Fund. Retrieved 26 May 2021.
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