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Park Profile – Guatemala Tikal National Park

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Park Profile – Guatemala Tikal National Park Park Profile – Guatemala Tikal National Park Date of most recent on-site evaluation: September 2002 Date of publication: November 2002 Location: Department of Petén in the Maya Biosphere Reserve Year created: 1955 Area: 57,582 ha Ecoregion: Tehuantepec humid forest Habitat: Wetlands, cloud forest and lowland forest Summary Description Tikal National Park is located in northern Guatemala, between the municipalities of Flores and San José, Petén. Created in 1955, it is Guatemala’s best-known park and most popular tourist destination. It features a set of striking archaeological sites and a complex habitat of wetlands, lowland and highland forests, which have been well conserved. The park is one of few protected areas in Guatemala to have received the full support of authorities for its conservation. In 1979, Tikal was declared a UNESCO World Heritage Site. Biodiversity Regionally endemic species found in the park include: the crocodile (Crocodylus moreletii), Central American river turtle (Dermatemys mawii), the howler monkey (Alouatta pigra), spider monkey (Ateles geoffroyi) and ocellated turkey (Agriocharis ocellata). Felines include the jaguar (Panthera onca), puma (Puma concolor) and ocelot (Leopardus wiedii). Several of the species in the area are on IUCN’s red list (2001). Guatemala’s National Council of Protected Areas (CONAP 2001a) also considers that C. moreletii, A. pigra, A. geoffroyi, P. onca, P. concolor and L. wiedii are in serious danger of extinction. Threats ParksWatch classifies Tikal National Park as vulnerable, meaning that continuous efforts must be made to ensure the long-term success of biodiversity protection. The main threats to the park are forest fires, illegal extraction of forestry products, and poaching. Additionally, due to an imbalance between the number of personnel in charge of the archeological and tourist areas and the number of personnel available to patrol the natural areas, there are not enough park guards to adequately address the threats. The lack of job stability of those in charge of administration has also hampered the park’s management. 1 www.parkswatch.org A photo of showing the start of excavation Current view of Tikal National Park. work in the park, compared with a recent photo. Description Physical Description Tikal National Park lies in northern Guatemala, located between the municipalities of Flores and San José, Petén. It is located within the Maya Biosphere Reserve (MBR), and is one of the core zones of the reserve. The park stretches across 57,582 ha. It is bordered on the southwest by the San Miguel la Palotada Protected Biosphere (El Zotz). There is a strip between the biosphere and the park, which the National Council of Protected Areas (CONAP) has declared in a category for special use, with the same management goals as the core zones (CONAP, 2001b). To the east it is bordered by Yaxhá, Nakum, Naranjo National Monuments and to the northwest by a biological corridor that leads towards El Mirador-Río Azul National Park. The multi-use zone of the Maya Biosphere Reserve borders it to the north, while its southern edge is protected by a buffer zone. Map showing the location of Tikal National Park within Maya Biosphere Reserve 2 www.parkswatch.org The park features striking ruins, mainly from the classic Maya period. Tikal and Calakmul were the greatest and most heavily populated cities of the Maya civilization during the Classic Period (Schele & Freidel, 1999). The civilization was at its peak from 700-850 AD, when it covered an area of 120 km2 and wielded influence over an area of 2,500 km2 (Valdés et al., 1997). Tikal gradually became more important from the Late Pre-classic Period onwards (250 BC – 250 AD). Its decline was apparently due to internal fighting which led to the downfall of the civilization’s leading cities (Fahsen, 2002, per. com.). In 1979 UNESCO declared Tikal National Park a Mankind Heritage Site for its exceptional cultural and biological characteristics (UNESCO, 1979). View of the archaeological site of the North This carving is a portrait of one of the most Acropolis seen from the II Temple. important rulers of the Classic Period, called Stormy Sky. This is one of the best-preserved carvings found at Tikal, and is a work of art stored in the park’s Pottery Museum. The landscape of the national park is generally rolling. To the northwest, there is a range of hills that extends into the Zotz Biosphere and the MBR Multiple Use Zone. From southeast to northwest the area is crossed by mid-altitude highlands with a flatter topography. From southwest to northeast, the area is covered by lowland forest that stretches as far as the park boundaries and is split only in the highest reaches of the central area of Tikal. The highest points, in the northeastern section, reach a height of 400 meters, while the lowest areas are 200 meters high (CEMEC/CONAP, 2001), and lie in the lowland areas of the northeast and southwest. The surface layer of organic matter is shallow, with an underlying layer of clay- like soil that lies on top of limestone. According to data provided by Tikal’s meteorological station, the climate in the area is mainly warm and humid, although there is no clearly defined dry season. Average annual temperatures is 23.9° C, ranging from 20-30.7° C. Relative air humidity rates 81%, with a maximum of 100% and a minimum of 36%. Average annual rainfall is 1,323 mm. February - May are generally considered the dry months. There may be up to an 11°C temperature difference between the warmest and coldest months. 3 www.parkswatch.org Vegetation According to the classification by Dinerstein et al. (1995), the biosphere lies within the Tehuantepec humid forest ecoregion. According to MBR’s functional landscape map (CONAP, 2001b), habitats found in the protected area include highland and medium foliage forest, lowland forest and year-round wetlands. The forest of Tikal has been described as “an anthropogenic forest” due to the fact it features a large number of useful tree species such as cedar (Cedrela odorata), mahogany (Swietenia macrophylla), chicle tree (Manilkara achras), allspice (Pimenta dioica) and copal (Protium copal), among others (Balas, 2002). The forest is representative of the eastern section of the Maya Biosphere Reserve. The Rapid Ecological Evaluation of MBR (APESA, 1993) determined this to be a forest of medium tree diversity, as it is home to approximately 200 species per hectare, although Schulze & Whitacre (1999) calculate that the number is actually higher. The presence of the highlands means that the variety of vegetation in the area is determined by drainage. Like habitats found elsewhere in the Maya Biosphere Reserve, in areas that are only temporarily flooded one can find formations that are characteristic of dry savannah, with spiny, thick bushes. Highland forest and medium foliage in the highlands This type of forest grows in the highest parts of the protected area, in the upper highland reaches which cross the area, over an altitude of 300 meters. Due to the fact the soil layers are often shallow and the material is porous, rapid drainage occurs. The canopy opens up at a height of 6-20 meters (CONAP, 2001b). The canopy is thin in some parts, as some trees lose their leaves during the dry season. Existing species include breadnut (Brosimum alicastrum) with guaya (Talisia olivaeformis), malerio (Aspidosperma megalocarpon), pucté (Bucida buceras) and manchiche (Lonchocarpus castilloi), among others (Schulze & Whitacre, 1999). Detail of the highland forest in Tikal Highland forest and medium foliage on the plains This type of forest grows in well-drained soil. It is one of the most common habitats in the area (CONAP, 2001b). The forest canopy can reach a height of 40 meters, although it is highly variable. The highland forest plant life is dominated by ramón (Brosimum alicastrum), some sapotaceous and meliaceous species. In the lower part of the forest one can also find species like allspice (Pimenta dioica). 4 www.parkswatch.org Lowland forest This type of forest is common in the southwestern and western stretches of the protected area. It grows in areas with shallow, heavy and sticky topsoil that is flooded during the rainy season, but dries and cracks in the dry season. The trees grow in small or medium-sized hollows. During the rainy season, the soil does not properly drain and a sheet of water covers the area. Variations in the soil drainage can lead to differing water availability and therefore influence the composition of the plant life. In some parts one can find forests with stubby vegetation where dominating species include the logwood (Haematoxylum campechianum), as well as the pucté (Bucida buceras) and the palo gusano (Lonchocarpus guatemalensis). The canopy rarely surpasses 11 meters in height (Lundell 1937). The areas of sunken hollows are covered by marshland. The driest areas are carpeted with xerophtic shrubs, stubby and compact, in characteristic savannah formations, with acacias (Acacia sp.) and thorny plants (Schulze & Whitacre, 1999). Other areas are covered with grasses and palm tree species such as escobo (Chryosophila argentea) and Mexican palmetto (Sabal mexicana). A detail of the palm tree grove. In some places, the corozo (Orbignya cohune) is common, while other areas are covered with xate (Chamaedorea sp.) Biodiversity Researchers working in the Tikal National Park have discovered to date 185 tree species, and there are believed to be more than 200 (Schulze & Whitacre, 1999). The park features the highest density of xate (Chamaedorea sp.) in the entire Maya Biosphere Reserve, with 500 trees per hectare (Balas, 2002, per. com.). Over 352 bird species have been spotted, including 30 birds of prey and 60 migratory species (Balas, 2002). Due to the rarity and number of species of fauna, Tikal is considered an important area in Guatemala (SEGEPLAN/PROSELVA, 2000).
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