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Bernuda

The Bermuda islands were once covered in dense forest of endemic tree species, with mangrove forests lining the coasts and inland saltwater ponds. The islands are distinguished as having the northernmost mangrove forests in the Atlantic, which is made possible by the warm Gulf Stream current. Bermuda’s isolation led to the evolution of many endemic species, including the endangered Bermuda petrel (Pterodroma cahow), the Bermuda skink (Eumeces longirostris), and many endemic invertebrates. Restricted to this small archipelago, all endemic species are especially vulnerable to introduced predators and alien pests, and unfortunately the islands have seen the extinction of many species since the time of human settlement. Due to intense human activity, only very small areas of natural habitat remain on Bermuda today. Though the islands have a well-managed and well-funded system of protected areas, this is one of the world’s most densely populated regions. Additionally, Bermuda is subject to intense pressure from a heavy tourist industry.

  • Scientific Code
    (NA0301)
  • Ecoregion Category
    Nearctic
  • Size
    50 square miles
  • Status
    Critical/Endangered
  • Habitats

Description 
 Location and General Description
The Bermuda ecoregion is a crescent-shaped chain of some 150 coral limestone islands and islets, formed along the submerged rim of a long-extinct volcano. It is situated in the western Atlantic Ocean a little over 900 kilometers from the North American coast (Procter and Fleming 1999). Most of the land area is composed of 7 main islands that encompass 53 km2. This land area is surrounded by about 750 km2 of shallow reef platform (Sterrer 1998a), the most northerly in the Atlantic (UNEP 2000). The climate is subtropical, with mean air temperatures ranging from 19 to 30°C (Sterrer 1998a). The average humidity is 77 percent (Sterrer 1998a), and the annual precipitation (146 cm) is distributed relatively evenly throughout the year (Sterrer 1995).

The ecoregion is situated on a more than 75 meter thick coralline limestone cap, covering a volcanic pedestal that rises to just below sea level (Sterrer 1998a). Roughly 110 MYA, volcanic action along the mid-Atlantic ridge created a 2000 m high seamount, which was topped off by a second eruption some 33 MYA (Sterrer 1998a). Over time, changes in sea level led to the deposition on this seamount of alternating layers of soil (paleosols) and wind-blown calcareous sand (Sterrer 1995). These dunes solidified during the Pleistocene into a cover of soil and highly porous limestone (Sterrer 1998a).

Bermuda's topography is moderately hilly and low, with the highest elevation reaching only 79 meters. The shoreline is composed of bays and inlets, with coral sand beaches lining the shores, primarily in the south. The ecoregion has no rivers or surface streams, and the limestone supports a shallow freshwater lens in only 20 percent of the land area, resulting in fewer than 20 brackish and freshwater ponds (Sterrer 1998a). This includes a total of 17 peat marshes (Rueger and von Wallmenich 1996).

The ecoregion originally contained two predominant vegetative features: a once densely forested plateau and mangrove forests. The woodlands were characterized by three endemic trees, each of which is listed as threatened by the IUCN (Hilton-Taylor 2000): Bermuda cedar (Juniperus bermudiana), Bermuda palmetto (Sabal bermudana), and Bermuda olivewood (Elaeodendron laneanum). Also present are the threatened yellow-wood (Zanthoxylem flavum) and southern hackberry (Celtis laevigata). Wax myrtle (Myrica cerifera) dominates the understory of peat marshes, along with St. Andrew’s cross (Ascyrum hypericoides), Bermuda sedge (Carex bermudiana), saw grass (Cladium jamaicensis), and ferns (Rueger and von Wallmenich 1996). Bermuda maidenhair fern (Adiantum bellum) is found in cave damps.

Warmed by the Gulf Stream, the ecoregion’s mangrove forests are the most northerly in the Atlantic (Thomas 1993). These forests are isolated, small in size, and relatively low in tree diversity, with only three species present: red mangrove (Rhizophora mangle), black mangrove (Avicennia germinans), and buttonwood (Conocarpus erectus) (Thomas 1993). An unusual feature of these mangroves is that roughly one-third are situated around inland saltwater ponds, which are mostly tidal and connected to the sea by submarine fissures (Thomas 1993). These inland forests are typically monospecific, with either red or black mangrove present (Thomas 1993). The remaining two-thirds of mangroves are located in coastal bays, where they display typical mangrove zonation (Thomas 1993). The most frequent coastal bay mangrove associations are with red algae, green algae, and three flowering plants: Asparagus sprengeri, Borrichia frutescens, and Sesuvium portulacastrum. The different pond mangroves tend to display unique assemblages of species (Thomas 1993).

Biodiversity Features
As many as 320 bird species have been observed in the ecoregion (Wingate 1973). But Bermuda’s position as an isolated oceanic island has contributed in large part to an overall low diversity of species in most taxa, low endemism, and absence of native mammals, amphibians, or large predators (Wingate 1959). Low floral diversity in particular is attributed to isolation and lack of anthropogenic influence prior to the 1600s (Rueger and von Wallmenich 1996). The ecoregion’s biological composition is also a product of prehistoric sea level fluctuations of up to 150 meters, which alternately favored marine and terrestrial species and led to the demise of land snails, many endemic birds, and a tortoise (Sterrer 1998b). Other factors limiting biodiversity include the ecoregion’s low elevation, small size, geologic composition and age, as well as regional ocean currents and past and present climate and weather patterns (Sterrer 1998a).

Bermuda is home to 165 native vascular plants, and 15 of these are endemic (Procter and Fleming 1999). Endemic trees include: Bermuda cedar (Juniperus bermudiana), Bermuda palmetto (Sabal bermudana), and Bermuda olivewood (Elaeodendron laneanum). Other vascular plant endemics are: Bermuda spike rush (Eloecharis bermudiana), Bermuda sedge (Carex bermudiana), wild pepper (Peperomia septentrionalis), wild Bermuda bean (Phaseolus lignosus), St. Andrew’s cross (Ascyrum hypericoides), Bermuda snowberry (Chiococca bermudiana), Darrell’s fleabane (Erigeron darrellianus), and Bermudiana (Sisyrinchium bermudiana) (Procter and Fleming 1999). There are also 4 endemic ferns: Governor Laffan’s fern (Diplazium laffanianum), Bermuda maidenhair fern (Adiantum bellum), Bermuda shield fern (Goniopteris bermudiana), and Bermuda cave fern (Ctenitis sloanei) (Procter and Fleming 1999). The two endemic mosses are Campylopus bermudiana and Trichostomum bermudanum (Sterrer 1998a). Also present are 40 endemic fungi and ten endemic lichens (Sterrer 1998a).

Bermuda contains no native mammal or amphibian residents, although four species of visiting bats have been recorded. Two of the ecoregion’s bird taxa are endemic, representing a low endemism rate of less than one percent. These are the cahow, or Bermuda petrel (Pterodroma cahow), and the locally-termed "chick-of-the-village" (Vireo griseus bermudianus), a subspecies of the white-eyed vireo that has shorter wings, a larger head, and stout legs (BBP 1997). The only native terrestrial reptile is the endemic Bermuda skink (Eumeces longirostris), a rock lizard that is also unique in being the sole non-avian, native land vertebrate. There are at least 41 endemic insects, including 11 species of Lepidoptera, 17 Diptera, seven dragonflies, and three damselflies (Sterrer 1998a). There is also one potentially endemic spider, 11 endemic terrestrial mollusks, and one (now-extinct) endemic nemertean, Pantinonemertes agricola (Sterrer 1998a).

The ecoregion has witnessed the recent extinction of many endemic species, including the Bermuda spike rush (Eloecharis bermudiana) (Procter and Fleming 1999) and the only endemic nemertean, Pantinonemertes agricola (Sterrer 1998a). An estimated 16 insect species have disappeared in the last century, including the flightless grasshopper, Paroxya bermudensis and seven Diptera (Sterrer 1998a). The near-eradication of Bermuda cedar in the 1940s led to extinction of two associated endemic insects, the cicada Tibicen bermudiana, and the geometrical moth Semiothisa ochrifascia (Sterrer 1998a). Other losses include the apparent extinction of at least two endemic land snails, Poecilozonites spp., probably due to the introduction of carnivorous snails (Sterrer 1998b). Among birds, at least ten presumed endemics are known from Pleistocene fossils including the crane Baeopteryx latipes, the duck Anas paschyscelus, four species of rail, a woodpecker, a hawk, a heavy-billed passerine, and a small owl (Sterrer 1998a). Most of these birds are thought to have gone extinct due to sea level changes before human settlement, although the passerine and owl are were present at the time of the first settlers (Sterrer 1998a). Finally, scientists are also preparing a description of a recently excavated fossil land tortoise (Sterrer 1998a).

Highly endangered endemics include the Bermuda petrel (Pterodroma cahow), whose nesting sites are currently restricted to a few outlying islets, and the Bermuda skink (Eumeces longirostris). Rare endemic plants include Bermuda olivewood (Elaeodendron laneanum), wild Bermuda bean (Phaseolus lignosus), and Bermuda sedge (Carex bermudiana), which is confined to Paget Marsh and 5 upland sites. The endemic fern Diplazium laffanianum is extinct in the wild, but a few individuals still survive in the Bermuda Botanical Gardens (Procter and Fleming 1999).

Current Status
Currently, some ten percent of the ecoregion’s land area is covered by forest or woodland (Procter and Fleming 1999). Within this, only very small and fragmented areas of natural habitat survive. An estimated 95 percent of the surviving population of native Bermuda cedar (Juniperus bermudiana) was destroyed between 1946 and 1951 (Rueger and von Wallmenich 1996), following the accidental introduction of two coccoid scale insects (Sterrer 1998a). Only an estimated one percent of the original cedar forest survived the blight (BBP 1997). Subsequent reforestation using a scale-resistant strain has returned the cedar to roughly ten percent of its former abundance (Procter and Fleming 1999), though these efforts have been hampered by the introduction of fast-growing casuarinas and other exotics into much of the cedar habitat (Sterrer 1995). Of the 116 hectares of inland peat marshes present in the ecoregion in 1900, only some 48 hectares remain (UNEP 2000), including the 19.6 hectare Devonshire Marsh, Pembroke Marsh, and Paget Marsh (Rueger and von Wallmenich 1996). Only small, scattered areas of mangroves remain, totaling 16.7 hectares in 1980 (Procter and Fleming 1999). The largest mangrove forests are found at Hungry Bay Mangrove Swamp and Mangrove Lake (Thomas 1993).

Bermuda holds the distinction of having passed the first conservation laws in the New World, protecting the cahow (Pterodroma cahow) and other birds as early as 1616 (Sterrer 1998a) and limiting the uses of native cedar as early as 1622 (Rueger and von Wallmenich 1996). A comprehensive and well-managed protected areas system currently exists, comprising 12 nature reserves that cover some 48 hectares, as well as 63 parks (Procter and Fleming 1999). The 25-acre Paget Marsh Nature Reserve is the best surviving example of native cedar, palmetto, and mangrove forests. The largest wildlife sanctuary is Spittal Pond, covering some 60 acres and home to at least 25 species of waterfowl. Other important protected areas include Devonshire and Pembroke Marshes, Warwick Pond, and the upland hills of Castle Harbour and Walsingham (Procter and Fleming 1999).

One important conservation success story has been the recovery of the endemic Bermuda petrel. Early visitors to Bermuda had been terrified by the cahow’s screeching cries, but they soon found the bird easy to catch and good to eat (Raine 1994). Birds that were overlooked by humans were quickly consumed by introduced pigs (Wingate 1959), and as a result the cahow was thought to be extinct as early as the mid-1600s (Procter and Fleming 1999). But in 1951, 18 breeding pairs were rediscovered off the island’s East End, and subsequent recovery efforts have raised that number to 55 by 1998 (Procter and Fleming 1999). The birds are currently protected in off-limits offshore sanctuaries (BBP 1997).

Bermuda (the UK) is party to a number of relevant international environmental treaties, including: the World Heritage Convention, the Ramsar Convention, CITES, and the Bonn Convention on Migratory Species.

Types and Severity of Threats
In 1514, Spanish chronicler Oviedo y Valdes commented on the abundance of fish and bird life in Bermuda, and in 1593 shipwrecked English sailors joyfully discovered "an unbroken forest of cedar" from which to build their new vessel (Raine 1994). But four centuries of settlement have all but eliminated Bermuda’s native flora and fauna. Predominant threats to the ecoregion include conversion of habitat for agriculture and development, introductions of exotic plant species, and sea level rise.

By the end of the 17th century, settlers on Bermuda were already clearing the native land cover to make room for fields, gardens, hedgerows, and houses. They brought new pets and pests and planted ornamental plants, herbs and spices, and crops like tobacco and cotton. The conversion of land to agriculture continued through the 19th century, when Bermuda became a market garden for rapidly growing New York City (Raine 1994). Over the centuries, residents cleared mangrove forests for development and used the bark in tanning and as fuel (Thomas 1993). The native cedar was felled for housing, shipbuilding, furniture, and export, while the thick-trunked palmetto was used for roof thatch, to weave fashionable hats, ropes, and baskets, and even to concoct a potent alcoholic beverage (Rueger and von Wallmenich 1996).

Over the past century, Bermuda’s agricultural importance has declined, but the pressures of development continue to grow. Twenty of Bermuda’s 150 islands are currently inhabited, and the country remains one of the most densely populated in the world (Sterrer 1998a). As the population has expanded over the last 20 years, and the demand for housing grown, undisturbed areas of natural vegetation have diminished rapidly. An estimated 10 percent of the land area is now covered by houses, roads, and other surfaces (Sterrer 1995), and many peat marshes have been converted to landfills (Rueger and von Wallmenich 1996). The pressure on biodiversity is further intensified by the arrival of an estimated half million tourists each year (Sterrer 1998a).

Introductions of exotic species continue to crowd out native wildlife. An estimated 1500 plant species have been brought to the island over the centuries (Sterrer 1998a). Exotic trees like guava and mulberry threaten to replace native plant communities with monocultures, though conservationists employ culling and other techniques to keep these invasions at bay. Meanwhile, the activities of introduced birds like the great kiskadee (Pitangus sulphuratus) (brought in 1957 to control Anolis lizards) (Wingate 1973) continue to aid in invasive plant dispersal.

In the future, sea level rise will pose another serious threat to native vegetation as global temperatures increase, likely contributing to accelerated retreat of the region’s remaining mangrove forests.

Justification of Ecoregion Delineation
Bermuda’s position as an isolated oceanic island has contributed to a flora and fauna quite distinctive from any continental area or from Neotropical islands to the south. The ecoregion’s unique biological composition is also a product of prehistoric sea level fluctuations as well as a lack of anthropogenic influence prior to the 1600s.

References
Bermuda Biodiversity Project (BBP), on website of the Bermuda Aquarium, Museum & Zoo, <www.bamz.org/biodiversity/cahow.htm>, copyright 1997.

Hilton-Taylor, C. (Compiler). 2000. 2000 IUCN Red List of threatened species. IUCN, Gland, Switzerland, and Cambridge, UK.

Procter, D., and L. V. Fleming (eds.). 1999. Biodiversity: the UK Overseas Territories. Peterborough, Joint Nature Conservation Committee.

Raine, D. 1994. Insight pocket guides: Bermuda. Houghton Mifflin. Boston.

Rueger, B. F. and T. N. von Wallmenich. 1996. Human impact on the forests of Bermuda: the decline of endemic cedar and palmetto since 1609, recorded in the Holocene pollen record of Devonshire Marsh. Journal of Paleolimnology 16: 59-66.

Sterrer, W. 1995. Bermuda’s natural history in a nutshell. In Proceedings of the 1st Symposium of "Fauna & Flora of the Atlantic Islands", Funchal—October 1993. Boletim do Museo Municipal do Funchal, Suplemento No. 4.

Sterrer, W. 1998a. How many species are there in Bermuda? Bulletin of Marine Science 62(23): 809-840.

Sterrer, W. 1998b. Changes in Bermuda’s biota. In Proceedings of the 2nd Symposium of ‘Fauna and Flora of the Atlantic Islands’, Las Palmas—Fevereiro 1996, Boletim do Museo Municipal do Funchal, Suplemento No. 5.

Thomas, M. L. H. 1993. Mangrove swamps in Bermuda. Atoll Research Bulletin 386:1-17.

Wingate, D. B. (ed.). 1959. A check list of the birds, mammals, reptiles and amphibians of Bermuda. Bermuda Audubon Society.

Wingate, D. B. 1973. A checklist and guide to the birds of Bermuda.

United Nations Environment Programme (UNEP), "Islands of Bermuda," Earthwatch website, <www.unep.ch/islands/ISD.htm>. Viewed 2000.

Prepared by: Lisa Mastny
Reviewed by: In process

 

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