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6l<br />

However the use of such winter dens has never been documented in any of the<br />

prevjous studies of Par Pond alljgstors (Murphy 1977, 1981t Brisbin et a1. 1982;<br />

Brandl 1989, 1991). Detailed descrjptions of the behavior of altigators dufing cold<br />

winter weather in this reservoir system by Brisbin et al, (1982) rather have shown<br />

adult alligators to submerge in either shallo!,r water in the reservojr's coves or<br />

along steeply-sloping bottom contours near deeper parts of the lake, where they<br />

Iikely exhjbit the "icing behaviorl described by Hagan et aI. (1983) during periods<br />

of particularly lo\^r temperatures.<br />

On 28 January, 1992 however, an adult alligator was observed inside an<br />

extensjve wjnter den that was located at what, before the drawdown, had been<br />

the waterrs edge of a small cove along the eastern shore of par pondrs Main Lake<br />

(Figure 6). Since only the head and forequafters of this alligator coutd be seen<br />

extending from one of the distant branching tunnels of the den (Figure ?), its<br />

length could only be estimated as being approximately 1.5-2.5m. This alligator<br />

was presumed to be a femaie that was known to inhabit and nest in this particular<br />

cove. Further support for the identification of the denned aUigator as being this<br />

female was provided during subsequent exploration of the den on l0 February,<br />

1992 at wbich time a group of at ieast four small juveniles was discovered in a<br />

side chamber of the den, approximately 1.0 1.5m from where the adult alligator<br />

(which $/as not seen at this time) had b€en previously located (Fig1lle 7). Tbe <strong>size</strong><br />

of the juveniles suggested that they probably had halched in the falt of 1990 at a<br />

time when the entrance and much of the entrvwav of this den had almost<br />

certajnly been undefwater.<br />

The presence of water in winter dens has been thought to provide alligators<br />

with important thermal buffering during periods of cold temperature (Spotila et<br />

al. 1972; Hagan et aI. 1983). The possibiiity that the drawdown of par pond might<br />

result in cold temperature stress to the juveniles and/or the adult atligator in thjs<br />

now dry winter nursery den was therelore examjned by monitoring it with three<br />

temperature probes! (1) 1.0m inside the den entrance, (2) 5.0m further inside the<br />

den near the point where the juveniles had been located, and (3) 3.0m outside the<br />

den entrance at an elevation of l.om above the dry lake bed (Fig1rre?). These<br />

three probes fecorded temperalures (10.01oC) every 30 min from -18 F'ebruary<br />

through 22 April 1992, During this period, temperatures outside the den showed<br />

much higher variability (CV =63.a%) than did temperatures inside the den<br />

entrance (CV=29.0%), whjch in turn were significantly more vaaiable than<br />

temperatutes further inside the den near the brood chamber (CV=10.6%; F=5.3?;<br />

df-2736, 2830; p1 0.0r), Even on days when outside air temperatures felt<br />

below -5'C and varied throughout the day by nearly 25oC, inside den<br />

temperatures varied by less than 2.0"C and were at times more than 15oC warmer<br />

than the outside air temperatures (eg. 13-14 March 1992; Figure ?). The dates for<br />

which den temperature profiles are provided in Figlre ? were among the coldest<br />

recorded during the period that the probes were in place at the den. Even so,<br />

temperatures within the den r^rhere both the adult and juveniles were seen<br />

remained well above the accepted lower limit of body temperature for this<br />

species (5'Ci Bfisbin et al. 1982). Ahhough the den temperatures were<br />

considerably below the speciesrpreferred body temperature of 32-35oC (Colbert<br />

et al. 1946), the ability of a den such as described in this study to function as a<br />

blackbody cavity would indicate that alligators withjn it, regardless of th€ir body<br />

<strong>size</strong>s, should all be well within the limits of their "c.limate space'r (99!Eq Spotila et<br />

al. 1972), and that access to water under such conditions should not be necessary<br />

for thermoregulatory purposes. At some point during the winter, however, access

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