World_of_Animals_Issue_46_2017
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The wildlife <strong>of</strong> a cave<br />
The cave ecosystem<br />
How do animals survive in the constant<br />
darkness <strong>of</strong> a cave environment?<br />
The deepest part <strong>of</strong> a cave is known as the dark zone,<br />
and this is where troglobites live. As light cannot reach<br />
this region, plant life cannot grow, and so the animal<br />
inhabitants have had to find other sources <strong>of</strong> sustenance.<br />
One way they get access to food is through weather,<br />
as rain washes leaves, twigs and other plant matter into<br />
the cave. Alternatively, non-permanent cave dwellers –<br />
trogloxenes and troglophiles – can bring the food in for<br />
them, or <strong>of</strong> course, become the food themselves. Bats<br />
are an important part <strong>of</strong> many cave food chains, as their<br />
guano is full <strong>of</strong> organic matter. As their droppings pile<br />
up, bacteria and fungi break it down into basic nutrients<br />
for others to feed on. These microscopic organisms<br />
also become food for larger creatures, and so the chain<br />
progresses until you reach the larger mammals at the top.<br />
These delicate cave ecosystems can be found<br />
throughout the world, but they differ slightly depending<br />
on the size, location and conditions <strong>of</strong> each cave. For<br />
example, glacier caves, which have been carved out <strong>of</strong><br />
solid ice, create an environment that only a select few<br />
creatures can live in, while certain solution caves are<br />
home to a rich and diverse selection <strong>of</strong> wildlife.<br />
The olm is well-adapted to cave life<br />
but is currently under threat from the<br />
pollution <strong>of</strong> its underwater habitat<br />
Cave types The many varieties <strong>of</strong> caves that can be found around the world<br />
Solution Lava Sea Glacier<br />
Groundwater containing<br />
natural acid seeps through<br />
the earth to dissolve the<br />
soluble rocks – such as<br />
limestone, chalk and<br />
dolomite – beneath.<br />
As lava flows downhill,<br />
its surface cools and<br />
solidifies, but hot lava<br />
will continue to flow<br />
underneath, leaving a<br />
hollow cave behind.<br />
Also known as littoral<br />
caves, these are formed<br />
when waves slowly<br />
erode zones <strong>of</strong><br />
weakness in sea cliffs,<br />
carving out caves.<br />
Water running through<br />
or underneath a<br />
glacier gradually<br />
melts the ice around<br />
it. Eventually, a cave is<br />
formed as a result.<br />
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