Jordan River
ID
438
Author(s)
Brian Coad, Jennifer Hales
Countries
Egypt
Israel
Jordan
Lebanon
Occupied by Israel
Syria
West Bank
Major Habitat Type
Xeric freshwaters and endorheic (closed) basins
Drainages flowing into
Dead Sea
Main rivers to other water bodies
The main river is the Jordan, which originates in the Anti-Lebanon Mountains in Syria. It connects the Sea of Galilee (Lake Kinneret or Tiberias) to the Dead Sea, but is actually little more than a stream. Wadis – valleys with intermittent watercourses – that flow into the Jordan include Wadi Mujib, Wadi Mousa, Wadi Hassa, and Wadi Zarqa.
Description
Boundaries
The ecoregion encompasses the drainage basin of the Jordan River. It is bounded by the Coastal Levant ecoregion [436] to the west, Arabian Interior ecoregion [440] to the east, and Sinai ecoregion [435] to the south.
Topography
This ecoregion lies along the Jordan Valley, a narrow rift valley with mountains to the east and west reaching over 2500 m. It forms part of the Great Rift Valley, which extends from southern Turkey down through East Africa.
The Jordan River flows into the Dead Sea, which lies at the lowest point on earth’s surface (402 m below sea level).
Freshwater habitats
The flow of the Jordan River has been greatly reduced, and its salinity increased due to the diversion of water resources for agricultural uses. Lake Hula has been completely drained. Lake Kinneret is a fresh, warm monomictic lake with a high mineral content. The Dead Sea, which is landlocked and fed by the Jordan River and run-off from side wadis, is hypersaline and fishless. Springs, however, harbor fishes; some are saline oasis springs.
Terrestrial habitats
Much of the ecoregion is a semi-desert environment with large irrigated agricultural tracts. It is subdivided into three separate biomes: Mediterranean forests, woodlands, and scrub; temperate greasslands, savannas, and shrublands; and xeric shrublands and desert. Higher elevations support oak and pine forests. Olive, eucalyptus, and cedar are common in the highlands and valley. Shrubs occur throughout the ecoregion.
Description of endemic fishes
Nearly a third of the species in the ecoregion are endemic and fall into the Cyprinidae (Acanthobrama hulensis, Acanthobrama lissneri, Garra ghorensis, Pseudophoxinus drusensis), Balitoridae (Nemacheilus insignis, Nun galilaeus), and Cichlidae (Astatotilapia flaviijosephi, Tristramella sacra) families. The only endemic genus is Nun in Balitoridae. Mirogrex species are more generally placed in the wider ranging genus Acanthobrama. Acanthobrama hulensis from the former Lake Hula is extinct (IUCN 2009).
Other noteworthy fishes
The North African catfish (Clarias gariepinus) is found here and in the Levant, but is not in the Tigris-Euphrates drainage basin.
Ecological phenomena
Mass appearances of dinoflagellates occur in Lake Kinneret. Exotics are affecting the ecology of the remaining marshes in the Hula Nature Reserve.
Justification for delineation
This ecoregion is distinguished by its endemics, Tethyan relicts, and the varied (for Southwest Asia) cichlid fauna of African origin. The Hula Nature Reserve is a Ramsar site.
Level of taxonomic exploration
Good
References
- Krupp, F. and Schneider, W. (1989). "The fishes of the Jordan River Drainage Basin and Azraq Oasis" Fauna of Saudi Arabia 10 pp. 347-416.
- Por, F. D.;Dimentman, C. (1989). "The Legacy of Tethys: an aquatic biogeography of the Levant" 63 Dordrecht: Kluwer Academic Publishers.
- Scott, D. A. (1995) A Directory of Wetlands in the Middle East IUCN and International Waterfowl and Wetlands Research Bureau : Gland, Switzerland and Slimbridge, U.K
- Serruya, C.;Pollingher, U. (1983). "Lakes of the warm belt" Cambridge: Cambridge University Press.
- Hijmans, R. J., S. Cameron and Parra., J. (2004) \WorldClim, Version 1.4 (release 3). A square kilometer resolution database of global terrestrial surface climate\ "<"[http://www.worldclim.org]">" (16 July 2009)
- IUCN (2009) \IUCN Red List of Threatened Species. Version 2009.1\ "<"http://www.iucnredlist.org">" (08 July 2009)