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Your Bearded Dragon - It's Habitat and Water

 

Water is a hotly-debated issue among some Dragon keepers, with opinions ranging from "daily baths, with spraying" to "no water is needed".

 

In this article, Rick Catt, a Bearded Dragon breeder from Australia, looks at their natural habitat to explain his views on water provision.

 

Many thanks to Rick for allowing me to use this article. Hopefully it will provide some insight to Dragon keepers who have never visited their natural range.

 

 

Introducing Australia

"Put simply, the arid and semi-arid lands are those remote and sparsely populated areas of inland Australia, defined by the presence of desert vegetation and land forms as well as by low rainfall. They are bound by median annual rainfalls of about 250 mm in the south but up to 800 mm in the north and about 500 mm in the east.

Together with sub-tropical regions and the mountain high plains, they form the rangelands, where rainfall is too low or unpredictable or where terrain is too inhospitable for sustainable cropping or timber harvesting. The rangelands amount to 70% of Australia's land surface, and by far the largest part is arid or semi arid. The vegetation of the arid lands has a strong influence on land use and productivity. The saltbush, mulga and grassy plains provide pasture for sheep and cattle as well as habitat for unique mammals and birds. In the dry infertile interior, the spinifex-covered sand plains and stony deserts are too tough for livestock. Instead they are home to a multiplicity of termite species and the world's richest lizard fauna.

It is an uncompromising environment at times but never monotonous. The climate of arid Australia is more variable than in arid lands anywhere else in the world, with highly erratic rainfall, extremes of long dry periods and flooding deluges. As well, soils are characteristically very infertile over vast areas compared to other deserts of comparable aridity.
The range of flora and fauna occupying the various ecosystems also contrasts with that from other arid regions of the world. Major differences include the lack of many succulents, the small number of large mammals and the high numbers and diversity of lizards as well as social insects such as ants and termites. These factors combined determine the arid zone's uniqueness………."


© Copyright CSIRO Australia 2000 - 2006
The full content of this may be viewed at http://www.cazr.csiro.au/aridlands.htm together with additional information regarding this area of our country.
 

 

 

 

Their Wild Habitat

To better understand your dragon some knowledge of their territory including climatic conditions is needed.





The first picture indicates the approximate territory inhabited by Pogona vitticeps; North-South some 1500 km, East-West about 1000 km.

 

The next is a physical representation from which it can be seen that the area of habitation is generally low lying, and on the eastern side, cut off from the coast by a mountain range which severely limits all rainfall.






 


From this rainfall analysis it can then be seen that the majority of their territory receives less than 100 mm of rain in the 6 month period covering the height of their activity and the following temperature analysis again shows mean max temps in excess of 33C over the same period.
 



 


The picture emerging already indicates that the land is dry and hot during the majority of the time that they are active.

 

 


However these are only averages so a look at specifics can make things even clearer. I'll use data from Alice Springs as everyone knows where it is and it is situated well within the dragons preferred range. The data I refer to can be found on the
Australian Bureau of Meteorology website.

In October the mean minimum temperature is only 15.8C - probably not much warmer (if at all) than your overnight house temps but more to the point the rainfall of 6.8 mm total with a rate of evaporation of 364.8 mm.

Dragons are starting to get around at this point, mating and laying.

By December you can expect that babies are hatching. The mean lowest temperature is 21.3C and mean highest 35.2C. Again look at the water, total rainfall 21mm with a total evaporation rate of 396mm.

February when everything is peaking, temperatures are little changed and total rainfall is still low at 6.4mm with total evaporation at 424mm.

A quick bit of maths shows that total rainfall in these three months is 34.2 mm BUT evaporation has been at the rate of a massive 1184.8 mm. Given that only 34.2 mm fell this means that another 1150.6 mm of standing water would have evaporated in those three months. This leads on to the next section...


 



Puddles? What Puddles...?


Open water that is not flowing or well shaded at the bottom of gorges doesn’t stand much chance in these conditions, which is why dragons (among many other creatures) have developed the ability to survive perfectly happily without the need to drink (or bathe) and are able extract their fluid needs from their food. Their kidneys act like a recirculatory system removing as much as possible and then excreting urates (a semi-solid). The cloaca then has another go and hauls out as much additional fluid as it can leaving the final deposit as a near-solid excretion.

Now the pretty pictures to illustrate this; as I don’t have any personal ones from around Alice Springs I’m using an area stretching from around Uluru, south to Coober Pedy and east to White Cliffs instead. All three places are available to view using Google Earth.




This proves that water does exist but you’ll note that it is concealed in a steep sided gorge of which there are not a lot as seen by the flatness of the land in the following shots.


In the following photos you can get an idea of exactly how sparse the vegetation is and how flat the land, leaving very little in the way of shaded areas for water to remain.
 





 

The first photo is of gum trees near Uluru and the second is of the land approaching Mt Connor which is around 88 km from Uluru. Notice also the ground itself - a hard baked surface with a scattering of small rocks and over everything a fine layer of red dust.
 

For anyone who’s interested it’s just as flat on the road near Coober Pedy around 500 km south of Uluru.

 



 

To get some perspective on these two shots, the blob on the road is my brother-in-law - and no I didn’t leave him out there!

 



Maps carry warnings on them, such as:-

“The majority of water features shown on this map do not contain permanent water.”


And;


“Travellers should familiarise themselves with prevailing conditions before departure and take care to ensure their vehicle is roadworthy and that they carry adequate supplies of petrol, water and food.”


 


Having broken down on the Stuart Highway 60 km past Coober Pedy I can tell you that there are two questions that get asked by everyone who stops (and over here that is everyone who goes past);

1. Do you need help?
2. Have you got enough to drink ?

You can’t just stroll down the road a bit and find a small stream or similar; they just aren’t there.




In conclusion you can hopefully see that the land is harsh, day time temperatures are high but night time temperatures are low.

 

Water is practically non-existent thus your dragon does not need or want swimming and drinking lessons as he lives happily without a constant water supply (in most areas – no water supply).

 

To replicate this you will need a high temperature basking spot of 35C+ (remembering that dragons thermoregulate by moving from sunlight to shade) and a cool side of around 25C during daylight plus bright white lighting to simulate the sun. For night, no light and temps dropping to 16~20C. For furnishing, a basking rock, a hiding area, climbing frame and mixed sand and stone as a base. Only one other item and that is a small bowl of water. Although your dragon will almost certainly never drink, if the occasion arises that he feels dehydrated, water should be available to him.

 

For those who would like to check these facts (or do some further research) all the climate related information may be obtained from Climate Data Online.


© Rick Catt 2008-2010

 

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