This mangrove ecoregion found along the Pacific coast of Costa Rica is unique as it marks the transition from dry to moist forest along this coast. Vegetation zones can be divided into external and internal areas, and vegetation is characterized by the geneses Rhizopora and Avicennia. The ecoregion serves as an important nesting site for a number of bird species as well as providing habitat for such fauna species as mantled howler monkey, spectacled caiman, and the largest bat species in the New World, the false vampire bat. The main threat to this region is the conversion of habitat for agricultural development.
Location and General Description
This ecoregion runs along the Pacific coast of Central America beginning just south of the Golfo de Fonseca in Nicaragua then continuing south to the Gulf of Nicoya in Costa Rica. This southern dry pacific coast ecoregion encompasses the Gulfo de Nicoya that marks the transition zone from dry to moist on the pacific coast. The mangroves in this ecoregion is structurally less developed than that further south as a result of its orientation within the dry tropical climate zone. Also there is lower annual rainfall, than further south of the transition line, ranging from 1,300 millimeters (mm) in Nicaragua to 2,000 mm in Costa Rica, but mostly falling during the short wet season resulting in a longer dry season from December to April. Annual temperature fluctuates between 25°C and 27°C with lean high or low depending on northern or southern areas of the ecoregion.
Because of high evapotranspiration rates and severity of the dry seasons, there is high salinity and a water deficit most of the year. Two kinds of zones can be distinguished in this ecoregion external and internal. The external areas are directly exposed to estuarine waters. The internal areas are isolated from the estuaries' waters mostly however, seasonally the tides inundate these areas. There is a strong salinity gradient between the mouth and the inland areas where salt pans may form. Evapotranspiration, marine water, and a supply of freshwater from rainfall, river discharge, and surface runoff regulate these salinity variations in the soil. In areas of seasonal climate fluctuation, salinity concentrations increase towards the internal side of the forest. With greater distance from the tidal channels, and diminishing intensity of tidal inundation's, salt accumulates in the soil as freshwater evaporates, leaving salt pans in the driest areas. The dry internal zone receives freshwater input during the dry season through runoff, which may come from small wetlands that function as reserves. Throughout the ecoregion fine sediment dominates most sites soil types but sandy areas are also found.
Vegetation in this ecoregion is mainly represented by mangrove ecosystems including species, which grow in association with mangroves and some aquatic plants. Dominant mangrove species such as Rhizopora mangle, R. harrisonii, R. racemosa, Avicennia germinans, A. bicolor, A. tonduzii, Laguncularia racemosa, Pelliciera rhizophorae, and Conocarpus erecta in less flooded areas. The dryness of the region is associated with a clear zonation pattern among the mangrove species Rhizopora species are found at the seaward edge, and Avicennia along the inland fringe.
Vegetation that grows in moist areas in association with mangrove species include ferns Acrostichum aureum, Tabebuia palustris while Canavalia maritima, Ipomoea pescaprae, Caesalpinia bonduc, Prosopis juliflora, Sesuvium portulacastrum, Plutapapron vermiculare, Jouvea straminea, Fimbristylis spadicea, Capparis odoratissima, Randia, sp. and Tamarindus indica grow in dry zones.
Forests in the dry internal zone are composed of Avicennia subspecies bicolor, which are nesting areas for the yellow-naped parrot (Amazona auropalliata). A faunal inventory at the Juan Venado Natural Reserve counted 95 species of birds, 24 reptiles, 23 mammals, 14 fishes and 6 amphibian species. This ecoregion is said to be extremely important for nesting, staging, and wintering birds. Birds most specific to mangroves include the Panama flycatcher (Myiarchus panamensis), whimbrel (Numenius phaeopus), yellow-crowned night-heron (Nyctanassa violacea), black-crowned night-heron (Nycticorax nycticorax), scaly-breasted hummingbird (Phaeochroa cuvierii), black-bellied plover (Pluvialis squatarola), prothonotary warbler (Protonotaria citrea), northern waterthrush (Seiurus noveboracensis), northern scrub-flycatcher (Sublegatus arenarum), mangrove swallow (Tachycineta albilinea), and greater yellowlegs (Tringa melanoleuca) just to name a few.
Mammals, although not as numerous as birds, also utilize the resources available in this mangrove ecoregion including the paca (Agouti paca), mantled howler monkey (Allouatta palliata), white-faced capuchin (Cebus capucinus), pygmy anteater (Cyclopes didactylus), nine banded armadillo (Dasypus novemcinctus), Central American otter (Lutra annectens), white-tailed deer (Odocoileus virginianus), northern raccoon (Procyoon lotor), crab-eating raccoon (P. cancrivorus), which can be found both on the ground and in the canopy consuming crabs and mollusks and the Mexican anteater (Tamandua mexicana). The great false vampire bat (Vampyrum spectrum) is also found in this ecoregion and is considered the largest bat in the new world.
Reptiles such as the Basilisk lizard (Basiliscus basiliscus), snakes (Boa constrictor) American crocodile (Crocodilus acutus), spectacled caiman (Caiman crocodilus), Ctenosaur (Ctenosaura similis), iguana (Iguana iguana), and a few species of sea turtle such as the Pacific Ridley sea turtle (Lepidochelys olivacea).
Areas with the highest remaining concentrations of mangroves in this ecoregion, in Costa Rica are Puerto Soley (near NI border; Tamarindo (400 hectares (ha)), Golfo de Nicoya (15,173 ha), and Puntarenas. In Nicaragua: Estero Padre Ramos (4,590 ha), Aserradores-Poneloya (10,700), Las Peñitas to Salinas Grandes (2,420), and Estero Ciego to Puerto Sandino (1,990 ha).
Types and Severity of Threats
In general, the river basins that drain into this ecoregion are of high relief, therefore seasonally intense rainfall and highly erodable soils make them prone to erosion caused the removal of vegetation for agricultural practices, timber, fuelwood, and livestock grazing. The direct result is high sedimentation of nutrients that are naturally brought to the mangrove areas but in much lower concentrations, during the rainy season.
Major threats include the pressure to convert mangroves to agricultural uses even though mangrove soils are too poor for agricultural purposes and have problems of drainage, salinity, and acidity. Converted lands are often then abandoned because of high maintenance costs. In this ecoregion in particular vast areas of mangrove have been destroyed to construct salt ponds, which also requires cutting of mangroves for fuelwood to crystallize the salt. Also, urban encroachment, runoff of pesticide residues, and eutrophication. In the Gulf of Nicoya, between 1964 and 1989, 633 ha of mangroves were lost to shrimp culture and 115 to salt production.
Justification of Ecoregion Delineation
Classification and linework for all mangrove ecoregions in Latin America and the Caribbean follow the results of a mangrove ecoregion workshop and subsequent report.
Additional Information on this Ecoregion
- For a shorter summary of this entry, see the WWF WildWorld profile of this ecoregion.
- To see the species that live in this ecoregion, including images and threat levels, see the WWF Wildfinder description of this ecoregion.
- World Wildlife Fund Homepage
- Chapman, V. J., editor. 1992. Ecosystems of the World; Wet coastal ecosystems. Netherlands, Amsterdam: Elsevier Science Publishers B. V. ISBN: 0444415602
- Ecoregional Workshop: A Conservation Assessment of Mangrove Ecoregions of Latin America and the Caribbean. 1994. Washington D.C., World Wildlife Fund.
- Jimenez, Jorge A. 1999. Ambiente, distribucíon y características estructurales en los manglares del Pacífico de Centro América: contrastes climáticos. Pages 380 in Yáñez-Arancibia, Alejandro and Ana Laura Lara-Domínguez, editors, Ecosistemas de Manglar en América Tropical. Spring, MD USA: Instituto de Ecologia, A.C. Xalapa, México; UICN/ORMA Costa Rica; NOAA/NMFS Silver.
- Olson, David M., Eric Dinerstein, Gilberto Cintrón and Pia Iolster. 1996. A Conservation Assessment of Latin America and the Caribbean: Report from WWF's Conservation Assessment of Mangrove Ecosystems of Latin America and the Caribbean Workshop. WWF, Washington D.C.
- Polanía J. 1993. Mangroves of Costa Rica. In: Lacerda, L. D., editor. Conservation and sustainable utilization of Mangrove Forests in Latin America and Africa Regions. Part 1; Volume 2:
- Polanía J., and V. Mainardi V. 1993. Mangrove Forests of Nicaragua. Lacerda, L. D., editor. Conservation and sustainable utilization of Mangrove Forests in Latin America and Africa Regions. Part 1; Volume 2.
- Ramsar, 1993. A Directory of Wetlands of International Importance, 4th ed. Volume IV: Neotropics and North America. Compiled by Tim Jones. ISBN: 2831700140
- Ramsar, 1999. A Directory of Wetlands of International Importance designated under the Convention on Wetlands of International Importance Especially as Waterfowl Habitat. Ramsar, 1971. Scott Frazier, editor. Compiled by Wetlands International for the Seventh Meeting of the Conference of Contracting Parties to the Ramsar Convention San José, Costa Rica, May 1999 ISBN: 2940073171
- Strattersfield, A.J., M.J. Crosby, A.J.Long, and D.C. Wege, 1998. Endemic bird areas of the World, priorities for biodiversity conservation. Birdlife Conservation Series, No. 7. BirdLife International, Cambridge, UK. ISBN: 1560985747
- Spalding, Mark, Francois Blasco, and Colin Field., editors. 1997. World mangrove atlas. Chapter 7: The Americas: Costa Rica and Panama. Okinawa, Japan: The International Society for Mangrove Ecosystems.
- Tosi Jr., J.A. 1969. Republica de Costa Rica: mapa ecológico. Map 1:750,000. Tropical Science Center,San Jose, Costa Rica.
Disclaimer: This article is taken wholly from, or contains information that was originally published by, the World Wildlife Fund. Topic editors and authors for the Encyclopedia of Earth may have edited its content or added new information. The use of information from the World Wildlife Fund should not be construed as support for or endorsement by that organization for any new information added by EoE personnel, or for any editing of the original content.