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Study
Site
San
Salvador Island (24o05'N, 74o30'W), located in the southeastern
edge of the Bahamian Archipelago, possesses numerous small
hypersaline lakes. San Salvador is a small island (~ 180 km2),
isolated from other Bahamian Islands (the nearest island is
> 50 km away), and supports a small human population (<
2,500). The earliest recorded observation of the hypersaline
lakes (45 to >160 ) is contained in the diary of
Christopher Columbus, who is thought to have first set foot
in the New World on San Salvador. Dense microbial mats blanket
the shallow sediments in many of these lakes and are the dominant
biotic feature. The lakes are virtually unimpacted by terrigenous,
atmospheric, or anthropogenic nutrient inputs. By far, the
largest perturbations the lakes experience are the freshwater
and sediment inputs attributable to hurricanes and other major
storms.
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rainfall on San Salvador averages only ~ 101 cm and evaporation
exceeds precipitation in most years. With the onset of the dry
season in November, large areas of the mats become and remain
desiccated for much of the year. At the edges of the lakes,
some communities may remain desiccated for several years, depending
on yearly rainfall. Additionally, as lake levels recede and
water within the mats evaporates, exposed mats are subjected
to intense solar radiation (>2300 µE m-2 s-1), high
temperatures (> 35oC), and even greater salinity levels.
In many respects, these systems represent 'life at the edge',
while, at the same time, typifying much of the earth's more
desiccated environments. |
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