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  Langebaan
General information

 

Land uses
Ecology
Topography and geology
Hydrology and geohydrology
Climate
Threats
References
Useful links
Map

General information      Top

This wetland became part of the Ramsar Convention on the 25th of April 1988.  The Langebaan Lagoon (approximately 6 000ha) is situated on the west coast of South Africa, within the West Coast National Park (approximately 27 000ha) about 100 km northwest of Cape Town (33°06'S, 18°01' E), adjoining the coastal village of Langebaan.

The Langebaan Lagoon comprises:

  • The intertidal sandflats.

  • Marshlands and Geelbek annex (5 7000 ha).

  • Precincts of the lagoon (46 ha).

  • The inshore islands: Jutten (43 ha), Marcus (17 ha) and Scaapen (19 ha).

  • A section of Sixteen-mile beach bordering on the farm Stofbergfontein (100 ha).

Classification of these wetlands includes:

  • Shallow marine waters.

  • Marine beds.

  • Rocky shores.

  • Sand/shingle shores (including dune systems).

  • Tidal mudflats (including intertidal flats and saltflats).

  • Salt marshes.

  • Coastal brackish/saline lagoons.

  • Saline/brackish lakes/marshes: seasonal/ intermittent.

  • Freshwater marshes/pools: seasonal/intermittent.

The Langebaan Lagoon is a large (approximately 16 km long and 2-3 km wide), shallow (between 2 and 6 m deep) and tidal lagoon. It has salinities of between 34 - 35% and can thus be described as entirely marine.  During the summer, thousands of waders (Charadrii) congregate on the extensive intertidal sandflats and saltmarshes. The four inshore islands are important breeding sites for many "endemic" seabirds.

Land uses        Top

The entire inter- and subtidal lagoon and approximately 70 percent of the land on its immediate perimeter is controlled by National Parks Board and private contractual parks. The rest is owned by the South African Defence Force, Langebaan Municipality , private land owner and companies.

The West Coast National Park , which was established in 1985, administers the lagoon and most of the land along its perimeter according to a draft management plan.  

Natural:  

The lagoon is divided into three different utilization zones namely:

  • The wilderness zone includes the southern end of the lagoon and the inshore islands, which are the key refuge sites of the waders and breeding seabird populations respectively. Access to these areas is limited to a few scientists and participants of educational excursions organised by National Parks Board and it is restricted to certain sites.

  • The limited recreation zone includes the middle reaches of the lagoon, where activities such as sailing and canoeing are permitted.

  • The mouth region is a multi-purpose recreation zone for power boats, yachts, water-skiers and fishermen. However, no collecting or removal of perlemoen and crayfish is allowed in the lagoon. This legislation and protection of the waterfowl are effectively maintained by the National Parks Board.
Agricultural:    

Farming activities inland do not significantly influence the lagoon system.

The aquaculture farm, Atlans Farms grows the alien mussel Mytilys galloprovincialis and oysters Crassotrea sp. from floating rafts anchored in Saldanha Bay .  
Further inland several farms produce a variety of items, such as potatoes, wheat, sheep, cattle and pig.  
Industrial: 

The larger Saldanha town (15 km from Langebaan) has a large commercial fishing harbour and tow fish processing factories.

The nearby Saldanha-Sishen terminal is used for loading iron ore and unloading crude oil.  
Casts of the alga Gracilaria verrucosa are collected from the beaches just north of the lagoon for commercial gain.
Urban:  
The Langebaan Lagoon is adjacent to the village Langebaan and closer to the lagoon’s entrance to the sea, is the larger town of Saldanha
Recreational:  
The Langebaan Lagoon - Saldanha Bay area is a popular holiday mecca, and restaurants and accommodation are available at the West Coast National Park , Langebaan village and Club Mykonos. The National Parks Board has "Educational" boating, canoeing and hiking excursions for their visitors, while the general public can sail, boat, water-ski and fish in the multi-purpose recreational zone of the lagoon. No new, major developments are apparently planned for the immediate future.
Ecology     Top

In 1995, the main habitat and vegetation types of the lagoon were:

  • A shallow marine aquatic system - having a soft substratum, which is unvegetated, except for large beds of the alga Gracilaria verrucosa near the mouth of the lagoon, and the Zostera capensis near the southern end of the lagoon.

  • Unvegetated intertidal sandflats - consisting of unconsolidated sand.

  • Rocky islands - having little soil cover and sparse vegetation in summer.

  • Intertidal saltmarshes - with Chenolea - Salicornia dwarf succulent scrubland.

  • "Supratidal" Marshes - with Juncus krausii sedgeland.

  • Most of the plant communities bordering the lagoon are shrublands (dwarf restioid or evergreen) belonging to the West Coast Strandveld, a vegetation type which is seriously threatened by agricultural activities and urban development.

Algae:  
 Over 71 species of marine algae (13 Chlorophyta, 10 Phaeophyta and 48 Rhodophyta) have been recorded in the Saldanha Bay-Langebaan Lagoon area. The more common species are Ulva spp., Ecklonia maxima, Laminaria pallida, Aeodes orbitosa, Gigartina radula, Gracilaria verrucosa and Porphyra capensis (Ref. 3).
Vegetation:  
Aquatic vegetation:  
Extensive marshlands occur along the south-eastern edges of the lagoon. The dominant species (Arthrocnemum pillanssi var. pillanssi, Salicornia capensis and Disphyma crassifolium, Juncus krausii, Scirpus nodosus, Nidorella foetida, Senecio Haliminfolius, Typha capensis and Phragmites australis) are generally common in marshlands throughout the region
Terrestrial Vegetation: 
Most of the other plant communities bordering the lagoon belong to the West Coast Strandveld and the park conserves about 12 percent of this "threatened" vegetation type (Ref. 1 and 2). The dominant plants include Atriplex semibaccata, Drosanthemum floribundum, Zygophyllum morgsana, Z. cordifoloum, Z. flexuosum, Rushia geminiflora, Mesembryanthemum crystallinum, Rhus glauca, R. longispina, Ehrharta erecta, E. calycina, Senecio floribunda, Rushia geminiflora, Euphorbia mauretanica, Salvia lanceolata, Willdenowia striata, Ericocephalus africanus, Putterlickia pyracantha and Euclea racemosa.
The iris Moraea loubseri is probably extinct from its natural habitat, while possibly threatened species are: Vanizijlia rostella, Hessea chaplinii, H. mathewsii, Felicia elongata, Pauridia longituba, Ferraria langebaanensis, Geissorhiza lewisae, Gladiolus gracilis var latifolius, Ixia purpureorosea, Romulea elliptica, R. saldanhensis, Watsonia hysterantha, Hyacinthus paucifolius, Lachenalia viridiflora, Oxalis subsessilis, O. burtoniae, Muraltia harveyana, Leucospermum tomentosum and Agathosma thymifolia (Ref.1).  
Invertebrates:

The invertebrate fauna of the intertidal mudflats are an important food source for waders. The snail Assiminea globulus, which comprises about 62,5 percent of the invertebrate biomass in the surface layers of the intertidal mudflats (Ref. 4), is the major prey item of the dominant curlew sandpiper (Ref. 5). The deeper burrowing mud prawn Upogebia africana is important to the kelp gull (Larus dominicanus), grey plover (Pluvialis squatarola), whimbrel (Numenius phaeopus) and common tern (Sterna hirundo) (Ref. 6), while the sand prawn (Callianassa kraussi) is the bait organism most frequently used by anglers in the lagoon    (Ref. 7).

Fish:  
Fish populations in the lagoon are generally low, Gobies (Gobiidae) and clinids (Clinidae), pipefish (Syngnathidae) and Cape silverside (Antherina Breviceps) are common in the weed beds, while shoals of the southern mullet (Liza richardsoni) and maasbanker (Trachurus trachurus) often frequent the deeper, sandier area of the lagoon (Ref. 8). Other important fish species in the lagoon are the West Coast streenbras (Lithognathus aureti), white stumpnose (Rhadosargus globiceps), steentjie (Spondyliosoma emarginatum), hottentot (Pachymetopon blochi) and sand shark (Rhinobatos annulatus).
Reptiles and Amphibians
Birds: 

Langebaan Lagoon supports approximately 37 000 birds in summer, of which about 34500 are waders (93% of these are Palaearctic migrants) with Curlew sandpiper (Calidris ferruginea) (59,2%), Grey plover (Pluvialis squatarola) (10,5%), Sanderling (Calidris alba) (8,3%), Knot (Calidris canutus) (8,1%) and Turnstone (Arenaria interpres) (5,7%) being the most abundant (Underhill 1987). In winter the numbers decline to about 10500 birds, which include approximately 3900 waders and 4515 flamingos (Phoenicipterus ruber and P. minor) (Ref. 9).

  • The inshore islands support large breeding colonies of "piscivorous" (fish eating) seabird which:

  • Langebaan Lagoon supports approximately 37 000 birds in summer, of which about 34500 are waders (93% of these are Palaearctic migrants) with Curlew sandpiper (Calidris ferruginea) (59,2%), Grey plover (Pluvialis squatarola) (10,5%), Sanderling (Calidris alba) (8,3%), Knot (Calidris canutus) (8,1%) and Turnstone (Arenaria interpres) (5,7%) being the most abundant (Underhill 1987). In winter the numbers decline to about 10500 birds, which include approximately 3900 waders and 4515 flamingos (Phoenicipterus ruber and P. minor) (Ref. 9).

  • The inshore islands support large breeding colonies of "piscivorous" (fish eating) seabird which:

Furthermore some 400 (or 12 percent of the world's population of) African black oystercatcher (Haematopus moguini) are found in the Langebaan area (Ref. 12 and 13).  
The most recent results are available from the Avian Demography Unit (ADU) at University of Cape Town , from a survey in March 1995. A total of 29 026 birds of 57 species were counted. The most numerous species was curlew sandpiper (± 14 000), followed by turnstone, grey plover and greater flamingo.  
The Sea Fisheries Research Institute counted pairs of seabirds breeding at the islands in the West Coast National Park in 1994.  The results showed that the Cape cormorant were the most abundant (10029 pair) in their habitat at Jutten Island, followed by the Kelp gull (5168 pairs) at Scaapen Island (Ref. 8).  
Mammals: 

Compared with the more tropical regions of southern Africa, the South West Cape has a depauperate mammal fauna. Nevertheless the area surrounding Langebaan Lagoon has rodents (19 species), insectivores (11 species), carnivores (13 species) and antelope (10 species), and although the "populations" are small, the following Red Data Book Species have been recorded (Ref. 14) as vulnerable Aardvark (Orycteropus afer), Honey badger (Mellivora capensis) and African wild cat (Felis lybica).  Rare red data species were the Bontebok (Damaliscus dorcas dorcas) and Grant's golden mole (Eremitalpa granti).

Topography and geology      Top
Topography and geography: 
 The average depth of the Langebaan Lagoon, which is 2 - 6 m, does not vary with seasons.  
Geology: 
  The three major substrata are limestone, granite and sand - all of natural origin
Soils:  
Fine, unconsolidated quartzitic sand, poor in nutrients, underlies most of the lagoon
  
Hydrology and geohydrology      Top

The lagoon, which is perennial and entirely marine, has a strong tidal exchange with no marked seasonal variation in flow.

The lagoon is an open marine system and the effect of freshwater flooding is small.  
No major rivers discharge into the lagoon, but fresh-water does drain from the surrounding catchment area and collects in the Juncus krausii marshes along the southern end of the lagoon. These marshlands and eelgrass beds in the lagoon act as sediment traps, and freshwater flooding after rain does not significantly affect the system. Water quality and "nutrient" transport in the lagoon is maintained by a strong tidal exchange of seawater. Current speeds in the middle section of the lagoon are about 20 cm per second, and approximately 12 percent of the volume of the lagoon-bay system is exchanged during a spring tide (Ref. 15). Erosion along the banks of the lagoon is minimal, but unconsolidated sand dunes nearby have been "stabilized" through intensive planting of indigenous vegetation.
Climate      Top
Precipitation:  

  The mean annual precipitation is 250 mm, falling mainly in winter

Temperature:  
The ranges in the mean monthly minimum and maximum temperatures are ±8,7 - 17,1 ºC and 14,6 - 21,0 ºC respectively
Threats      Top

The Saldanha-Sishen terminal has the potential of "causing" a major oil spill, as well as long-term, windblown, ore dust pollution, and thereby the food source of the waders. Likewise, commercial fishing activities in the seabird colonies and recreational activities in the area could become a major disturbance factor.

Numerous factors have negatively impacted on the ecology of the lagoon. These are: 
  • The building of a breakwater in the late 1970's between the mainland and Marcus island, which enabled predators to invade the penguins, swift, terns and bank cormorants colonies on the island.

  • The collecting of guano on the inshore islands until the mid 1980's.

  • Ongoing military activities at Donkergat, near the mouth of the lagoon.

  • The processing activities at Donkergat, near the mouth of the lagoon.

  • The introduction of rabbits onto the inshore islands, (only Scaapen and Jutten islands have significant numbers left).

  • The spread of the alien wattle (Acacia cyclops) and mussel (Mytilys galloprovincialis) into the wilderness zone.

  • The construction of unapproved dwellings, house boats and a canal at Bokramsloot for the launching of boats at the southern end of the lagoon.

  • The cultivation of wheat at Oudepos.

Despite these activities the ecosystem is still intact and healthy.

References   Top
Ref 1:  BOUCHER, C. and JARMAN, M.L. (1977). The vegetation of the Langebaan area, South Africa . Transaction of the royal Society of South Africa 42 (3 & 4): 241 - 272
Ref 2: JARMAN, M.L. (Ed) 1986. Conservation priorities in lowland regions of the fynbos biome. South African national scientific Programme Report No 87. CSIR, Pretoria : 55 pp
Ref 3: SIMONS, R.H. (1977). The algal flora of Saldanha Bay Transaction of the royal Society of South Africa 42 (3 & 4): 461 - 483
Ref 4: PUTTICK, G.M. 1977. Spatial and temporal variations in intertidal animal distribution at Langebaan Lagoon , South Africa . Transactions of the royal Society of South Africa . 42 (3): 403 - 433
Ref 5:  PUTTICK, G.M. 1980. Energy budgets of Curlew Sandpipers at Langebaan Lagoon , South Africa . Estuarine coastal marine Science. 11: 207 - 215
Ref 6:  Martin J.L. (1991) The Parus caeruleus complex revisited. ARDEA 79 (3) : 429 - 438
Ref 7:    WYNBERG, R.P. & BRANCH G.M. 1991. An assessment of bait-collecting for Callianassa kraussi Stebbing in Langebaan Lagoon , Western Cape , and of associated avian predation. South African Journal of marine Science. 11: 141 - 153.
Ref 8:        http://www.environment.gov.za/Branches/BioConservation/17Ramsar/langebaan/langebaan_ris.htm
Ref 9:  UNDERHILL, L.G. (1987). Waders (Charadrii) and other waterbirds at Langebaan Lagoon , South Africa , 1975 - 1986. Ostrich 58 (4): 145 - 155:
Ref 10:  BERRUTI, A. (1989). Resident seabirds. In. Oceans of Life off Southern Africa . Payne, A.I.L. & Crawford, R.J.M. (Eds). Vlaeberg Publishers, Cape Town : 257 - 273:
Ref 11:  COOPER, J., CRAWFORD, R.J.M., SUTER, W. & WILLIAMS, A.J. (1990). Distribution, population size and conservation of the swift tern Sterna bergii in southern Africa . Ostrich 61: 56 - 65
Ref 12:  HOCKEY, P.A.R. (1983). The distribution, population movement and conservation of the African black Oystercatcher Haematopus moquini. Biological Conservation 25: 233 - 262
Ref 13:  HOCKEY, P.A.R. (1985). Haematopus ostralegus in perspective: a review of the world's oystercatchers. In: Goss-Custard, J.D. (Ed.). Ecology of the eurasian Oystercatcher: from individuals to populations. London : Academic Press
Ref 14:  AVERY, D.M., RAUTENBACH, I.L. & RANDALL, R.M. (1990). An annotated check list of the land mammal fauna of the West Coast National Park . Koedoe 33 (1): 1 - 18
Ref 15:  SHANNON, L.V. & STANDER G.M. (1977). Physical and chemical characteristics of water in Saldanha Bay and Langebaan Lagoon. Transaction of the royal Society of South Africa 42 (3 & 4): 411 - 461
Useful links      Top

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