Esmeraldas-Pacific Colombia mangroves (NT1409) | |
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Ecology | |
Realm | Neotropical |
Biome | Mangroves |
Geography | |
Area | 6,500 km2 (2,500 sq mi) |
Countries | Colombia, Ecuador |
Coordinates | 4°12′32″N77°30′32″W / 4.209°N 77.509°W |
Geology | Chocó, Tumaco Basins |
The Esmeraldas-Pacific Colombia mangroves (NT1409) is an ecoregion of mangrove forests along the Pacific coast of Colombia and Ecuador. It is threatened by human population growth, leading to over-exploitation for wood and clearance for farming and aquaculture.
Mangroves are found along the coast of Colombia and Ecuador from the Gulf of Tribugá in the north to Mompiche Bay in the south. Between these bays there are extensive stands of mangroves in the mouths of the San Juan, Naya, Guapi, Mira and Esmeraldas rivers. The mangroves cover 6,500 square kilometres (2,500 sq mi). The largest block is the almost continuous strip from the Mataje River to Chanzará bay near Guapi. [1] In 1996 it was estimated that 2,927 square kilometres (1,130 sq mi) of mangroves were growing in the four Colombian Pacific coast departments. [2] The mangroves border the Chocó–Darién moist forests ecoregion along most of the Pacific coast of Colombia. In the extreme south they border the Western Ecuador moist forests. [3]
The ecoregion may be divided into two large zones to the north and south of Cabo Corrientes. [1] [lower-alpha 1] In the northern section the continental shelf is narrow, with the land rising steeply from the shore to around 1,500 metres (4,900 ft) above sea level. Many small rivers supply clear water to the ecoregion year round. There are strong low-intensity upwellings along the coast. [1]
The southern section fringes a flat sedimentary coastal plain with a broad continental shelf. There are no coastal upwellings. Rocks are mostly lutite, sandstone and conglomerates, with some limestone. [1] The mangroves along the low, alluvial coast that stretches over 400 miles (640 km) from Cabo Corrientes into Esmeraldas Province are the largest mangrove area in northwest South America, forming the tidal fringe of the coastal plain 8 to 50 kilometres (5.0 to 31.1 mi) wide. [5] There are large river deltas at the mouths of the Mataje, Mira, Patía, Sanquianga and Guapi rivers, and smaller deltas at the mouths of about 25 smaller rivers. There provide more fresh water than in the north, and often carry much more sediment. [1] The mangrove forest strips run parallel to the coast in the southern section and may extend inland for as much as 20 kilometres (12 mi) due to the 4 metres (13 ft) tides. [6]
The mangroves adjoin wet tropical forest with temperatures over 24 °C (75 °F) and very high rainfall. The climate is influenced by the Intertropical Convergence Zone. Annual rainfall in the northern section is from 4,000 to 8,000 millimetres (160 to 310 in), while the southern section receives 1,000 to 4,000 millimetres (39 to 157 in). [1]
The mangrove forests may release 8 to 15 tons of organic material per hectare each year, providing food to many other organisms. The forests play a crucial role as nurseries and food sources for fish, and also protect the coastline from erosion. The ecoregion is in the neotropical realm, in the mangroves biome. [1] The Panama Bight Mangroves, a Global ecoregion, contains the Gulf of Panama mangroves, Esmeraldas-Pacific Colombia mangroves, Manabí mangroves and Gulf of Guayaquil-Tumbes mangroves. [7]
Depending on the local topography and climate, mangrove formations include bar, inverse estuary, coastal, dwarf, border and small island. [2] Compared to the Caribbean, the Pacific mangroves of Colombia have lower salinity due to the high rainfall and tidal action, and their zoning may be more dependent on stability of the substrate. The abundant nutrient-rich fresh water results in exuberant growth, with heights over 40 metres (130 ft), and high production of organic detritus. Bromeliads and orchids grow on the trunks of the mangroves, and their branches hold water and falling material. [6]
Mangrove species include mangle caballero ( Rhizophora harrisonii ), red mangrove ( Rhizophora mangle ), Rhizophora racemosa , Samoan mangrove ( Rhizophora samoensis ), nato mangrove ( Mora oleifera ), black mangrove ( Avicennia germinans ), Avicennia tonduzzii , buttonwood ( Conocarpus erectus ), white mangrove ( Laguncularia racemosa ) and tea mangrove ( Pelliciera rhizophorae ). [1] The Conocarpus erectus mangroves are rare, found as isolated individuals. [2]
Most of the mangrove forest is a transition zone in which Mora oleifera and Euterpe species dominate. Mora oleifera is endemic to the Pacific Coast from Parrita in Costa Rica to Esmeraldas in Ecuador. Further inland there are freshwater marshes with plants such as golden leather fern ( Acrostichum aureum ), Virola species), Campnosperma panamensis , milk tree ( Brosimum utile ) and palms such as Mauritiella pacifica , sheath palm ( Manicaria saccata ) and Euterpe cuatrecasa . [1]
Common plants include Amphitecna Gentry , black calabash ( Amphitecna latifolia ), Crenea patentinervis , açaí palm (Euterpe oleracea), coast cottonwood ( Hibiscus tiliaceus ), Lonchocarpus monilis , Mora oleifera, Pavonia rhizophorae , Phryganocydia phellosperma , mangle marica ( Tabebuia palustris ), Tuberostylis axillaris and Tuberostylis rhizophorae . Sandy areas have field sandbur ( Cenchrus pauciflorus ), Homolepis aturensis , and climbers such as beach bean ( Canavalia rosea ), bayhops ( Ipomoea pes-caprae ), fiddle-leaf morning glory ( Ipomea stolonifera ), Pectis arenaria and St. Augustine grass (Stenotaphrum secundatum). [6] Bromeliaceae and Orchidaceae epiphytes that invade the canopy include Vrissia grandioliflora , Guzmania musaica and Heliconia bihai . [8]
Core samples have shown that in the south of the Gulf of Tribugá dominant populations of Rhizophora mangroves have been relatively stable for the last 4,500 years. In recent years abundant Acrostichum aureum have appeared, probably introduced by humans. In one area of the northern gulf there have been populations of Pelliciera rhizophorae for about 2,600 years, but in another area the mangroves are from recent colonization. [9]
The mangroves host invertebrates, shellfish, fish, reptiles, birds and mammals. The mangrove cockle ( Anadara tuberculosa ) is important for artisanal fisheries in the south-central region. Reptiles include iguanas and snakes. Mammals include oncilla (Leopardus tigrinus), coypu (Myocastor coypus), deer, lowland paca (Cuniculus paca) and white-lipped peccary (Tayassu pecari). [1] The mangroves are refuges for locally or regionally threatened species including bare-throated tiger heron (Tigrisoma mexicanum), American yellow warbler (Setophaga petechia), crab-eating raccoon (Procyon cancrivorus), American crocodile (Crocodylus acutus) and spectacled caiman (Caiman crocodilus). [10]
Common bivalves include Anomia fidenas , Gould's shipworm ( Bankia gouldi ), pleasure oyster ( Crassostrea corteziensis ), thin purse-oyster ( Isognomon janus ), striate piddock ( Martesia striata ) and brown falsejingle ( Pododesmus foliatus ). Common gastropods include mangrove periwinkle ( Littoraria scabra ), Littorina fasciata , Littorina varia , Littorina zebra , great pond snail ( Lymnaea stagnalis ), Melampus carolianus , Nassarius wilsoni , ornate nerite ( Nerita scabricosta ), Thais kiosquiformis and Theodoxus luteofasciatus . Common crustaceans include grapsid crab ( Armases angustum ), Callodes gibbosus , Eurypanopeus transversus , Eurytium tristani , Glyptograpsus impressus , Latreutes antiborealis , Macrocoeloma villosum , Notolopas lamellatus , Panopeus chilensis , Panopeus purpureus , Pinnotheres angelicus , Cangrejo de pantano ( Sesarma aequatoriale ), Sholometopus occidentalis and Sholometopus rhizophorae . The mangrove tree crab ( Aratus pisonii ) is very common. [10]
The World Wide Fund for Nature gives the ecoregion the status "Critical/Endangered". Mangroves are traditionally used for fuel, construction material, fishing equipment and as a source of tannin. They are threatened by expansion of towns, aquaculture, unsustainable extraction of wood, overfishing and clearance for farms or coconut plantations. Domestic and industrial pollution is a growing problem. The ecoregion is protected in Colombia by the Sanquianga National Natural Park and the Utría National Natural Park. Civil Society Natural Reserves are also starting to protect parts of northern Colombia. [1]
The Gulf of Guayaquil–Tumbes mangroves (NT1413) are an ecoregion located in the Gulf of Guayaquil in South America, in northern Peru and southern Ecuador. It has an area of 3,300 km2.
The Maranhão mangroves is a mangrove ecoregion of northern Brazil. It supports half of the shorebird population of the country. The combination of flat land, heavy rainfall and high tides causes the mangroves to extend up to 40 kilometres (25 mi) inland, where they are interspersed with other rainforest species.
The Guianan mangroves (NT1411) is a coastal ecoregion of southeastern Venezuela, Guyana, Suriname, French Guiana and Brazil. The mangroves provide an important habitat for migrating birds that winter in the area. Large areas are intact, although they are threatened by destruction of the trees for timber and to make way for agriculture, and from upstream agricultural and industrial pollution.
The Amapá mangroves (NT1402) is an ecoregion along the Atlantic coast of the state of Amapá in Brazil. The low coastal plain has been formed from recent sedimentation, including sediments deposited by the rivers and sediments carried northward from the mouth of the Amazon River by strong currents and deposited by the tides. The extensive mangroves grow on the newly formed coastal mudflats and along the edges of estuaries. They merge into freshwater várzea flooded forests further inland. The ecoregion is generally well-preserved, although excessive extraction of natural resources including timber and shrimps is a concern.
The Pará mangroves (NT1427) is an ecoregion along the Atlantic coast of the state of Pará in Brazil. They constitute the western extension of the Maranhão mangroves ecoregion. The mangroves are relatively intact, although they are under some pressure from agriculture and logging.
The South American Pacific mangroves, or Panama Bight mangroves, is an ecoregion along the Pacific coast of Panama, Colombia, Ecuador and Peru.
The Gulf of Panama mangroves (NT1414) is an ecoregion along the Pacific coast of Panama and Colombia. The mangroves experience seasonal flooding with high levels of sediment, and occasional extreme storms or very low rainfall due to El Niño effects. They are important as a breeding or nursery area for marine species. Areas of the mangroves have been recognized as Important Bird Areas and Ramsar wetlands. The ecoregion has been severely degraded by clearance of mangroves for agriculture, pasturage and shrimp farming, by urban pressure around Panama City, and by pollution related to the Panama Canal.
The Manabí mangroves (NT1418) is an ecoregion along the Pacific coast of Ecuador. The mangroves serve important functions in the marine and terrestrial ecology. They have been severely degraded and fragmented, particularly in the northern region. Construction of shrimp farms caused much damage in the past, but is now banned. Sedimentation caused by overgrazing in higher lands is an issue, as are human activities such as port and highway construction, urbanization, waste disposal and so on.
The Gulf of Tribugá is a gulf on the Pacific coast of Colombia. It contains exuberant mangroves. The bay is a spawning ground for humpback whales. Tourist attractions include diving and watching whales and turtles. There are plans to build a major deep-water port at the village of Tribugá in the main river estuary.
Cabo Corrientes is a cape on the Pacific coast of Colombia in the Chocó Department.
The Mesoamerican Gulf-Caribbean mangroves ecoregion covers the series of disconnected mangrove habitats along the eastern coast of Central America. These salt-water wetlands are found in river deltas, lagoons, and low-lying areas facing the Gulf of Mexico and Caribbean Sea, from Tampico, Mexico to central Panama. The mangroves are areas of high biodiversity and endemism. Many of the sites are protected as national parks or nature reserves.
The Bocas del Toro-San Bastimentos Island-San Blas mangroves ecoregion covers the mangrove habitats along the Caribbean Sea coast of Costa Rica and across the northern coast of Panama. An offshore reef and barrier islands of the region help protect the mangroves from destructive waves. The ecoregion has a high number of endangered and threatened species, including the loggerhead sea turtle, green sea turtle, and hawk's bill sea turtle.
The Coastal Venezuelan mangroves ecoregion covers the salt-water mangrove forests along the Caribbean Sea and Atlantic Ocean coast of Venezuela, from Cocinetas Basin to the edge of the Caño Manamo River and the Orinoco Delta in the east. It is one of the largest mangrove ecoregions in South America, with an area of 5,698 km2, and stretching across over 400 km of Venezuelan coastline.
The Gulf of Fonseca mangroves ecoregion covers the brackish mangrove forests around the Gulf of Fonseca on the Pacific Ocean. The Gulf is the meeting point El Salvador, Honduras, and Nicaragua. The Gulf is one of the two primary nesting sites of the critically endangered Hawksbill turtle in the eastern Pacific. In the Honduras portion, there are seven nature reserves that collectively make up a RAMSAR wetland of international importance, providing protection for migratory birds, sea turtle, and fish.
The Magdalena-Santa Marta mangroves ecoregion covers the mangrove forests along the coast of Colombia on the Caribbean Sea, from Gulf of Urabá in the west at the Colombia-Panama border to the Guajira Peninsula in the east. The region is relatively dry, with low precipitation and high evapotranspiration, so the mangroves depend for water and nutrients on the rivers flowing across the estuarine plain from the Sierra Nevada de Santa Marta mountains to the east. Efforts are currently underway to restore mangroves degraded by development and road building from the 1950s to 1980s.
The Mexican South Pacific Coast mangroves ecoregion covers the mangrove sites along the coast of the Pacific Ocean coast of Mexico, across the states of Michoacán, Guerrero, and Oaxaca. These mangrove forests are mostly around lagoons, typically those fed by rivers from the interior in the Sierra Madre del Sur Mountains. The ecoregion is small: collectively, it covers only 1,295 km2.
The Moist Pacific Coast mangroves ecoregion covers a series of disconnected mangrove sites along the Pacific Ocean coast of Costa Rica and Panama. These sites occur mostly on coastal flatlands around lagoons, particularly where rivers from the inland mountains reach the sea, bringing fresh water to the coastal forests. The area is in a transition zone from the drier coastline to the north; rainfall in this ecoregions is over 2,000 mm/year, and reaches over 3,600 mm/year at the southern end.
The Southern Dry Pacific Coast mangroves ecoregion covers a series of mangrove forests along the Pacific Ocean coast of Nicaragua and Costa Rica, from the southern margin of the Gulf of Fonseca to the Gulf of Nicoya near the border with Panama. Because the area is drier than the mangroves further south, evapotranspiration leaves some areas with higher salinity and even salt pans in the internal areas.
The Trinidad mangroves ecoregion covers the separate mangrove forest areas on the coast of the island of Trinidad, in the country of Trinidad and Tobago. The character of the mangroves is affected by the large amount of fresh water flowing out of the Orinoco River and Amazon River to the south, which flow northwest around the island. The mangroves of Trinidad are found on all coasts, and are usually in the estuaries of rivers, but also found in coastal lagoons.