Journal of Wildlife Diseases, 39(4), 2003, pp. 914–917
q Wildlife Disease Association 2003
Bilateral Uric Acid Nephrolithiasis and Ureteral Hypertrophy in a
Free-ranging River Otter (Lontra canadensis)
Robert A. Grove,1,4 Rob Bildfell,2 Charles J. Henny,1 and Donald R. Buhler3 1 USGS-Forest and Range
Ecosystem Science Center, 3200 SW Jefferson Way, Corvallis, Oregon 97331, USA; 2 OSU Veterinary Diagnostic Laboratory, College of Veterinary Medicine, Oregon State University, P.O. Box 429, Corvallis, Oregon
97339-0429, USA; 3 Department of Environmental and Molecular Toxicology, Oregon State University, ALS 1007,
Corvallis, Oregon 97331, USA; 4 Corresponding author (email:robertpgrove@usgs.gov)
ABSTRACT:
We report the first case of uric acid
nephrolithiasis in a free-ranging river otter
(Lontra canadensis). A 7 yr old male river otter
collected from the Skagit River of western
Washington (USA) had bilateral nephrolithiasis
and severely enlarged ureters (one of 305 examined [0.33%]). The uroliths were 97% uric
acid and 3% protein. Microscopic changes in
the kidney were confined to expansion of renal
calyces, minor loss of medullary tissue, and
multifocal atrophy of the cortical tubules. No
inflammation was observed in either kidney or
the ureters. The ureters were enlarged due to
marked hypertrophy of smooth muscle plus dilation of the lumen. Fusion of the major calyces
into a single ureteral lumen was several cm distal to that of two adult male otters used as histopathologic control specimens. This case report is part of a large contaminant study of river
otters collected from Oregon and Washington.
It is important to understand diseases and lesions of the otter as part of our overall evaluation of this population.
Key words: Lontra canadensis, river otter,
ureter hypertrophy, uric acid nephrolithiasis,
urolithiasis.
Uroliths (urinary calculi) are concretions
that can form at any level of the urinary
tract and are usually composed of inorganic salts, organic acids, or other compound
such as cystine, xanthine, or silica. The
most common uroliths in mammals are
composed of calcium as an oxalate or
phosphate, magnesium as ammonium or
hydrogen phosphate, purines, and cystine
(Cotran et al., 1994; Osborne et al., 1995).
Uric acid uroliths make up less than 1% of
total uroliths analyzed in dogs and cats
(Osborne et al., 1995), and from 4–40% of
uroliths in humans (Shekarriz and Stoller,
2002). Urolithiasis has been reported in a
few species of the family Mustelidae
(Chaddock, 1947; Sompolinsky, 1950; Keymer et al., 1981; Thomlinson et al., 1982).
In particular, some otters such as the Asian
small-clawed otter (Aonyx cinerea) have a
high incidence of calcium oxalate mono
and dihydrate urolithiasis (Keymer et al.,
1981; Karesh, 1983; Nelson, 1983; Calle
and Robinson, 1985; Petrini, 1999) in captivity. Urolithiasis has not previously been
reported in river otters (Lontra canadensis). Little is known about normal renal
function of river otters or adaptations in
renal physiology necessary for their largely
aquatic life (Hoover and Tyler, 1986). The
anatomy of the river otter kidney is described in detail in Baitchman et al.
(2000). In short, the kidney of otters is
reniculated (Hoover and Tyler, 1986;
Baitchman et al., 2000). This renal architecture is absent in other mustelids but
present in sea otters (Enhydra lutris), pinnipeds, cetaceans, and a few other mammals (Baitchman et al., 2000). The significance of reniculated kidneys in otters but
not in other mustelids is unknown.
An adult male river otter (RAG-245)
was trapped as part of a larger study at the
mouth of the Sauk River on the Skagit River, near Rockport, Washington (USA,
48828954.440N, 121836915.180W) in January 1997. The otter was frozen at 220 C
until necropsy was performed in July 1997
at the Veterinary Diagnostic Laboratory,
College of Veterinary Medicine, Oregon
State University (Corvallis, Oregon, USA).
The otter’s age was estimated to be 7 yr
by microscopic analysis of cementum annuli from an upper canine tooth (Matson’s
Laboratory LLC, Milltown, Montana,
USA) as described by Fancy (1980) and
Matson (1981). During necropsy, body
condition was evaluated and morphometric information recorded. Major organs
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FIGURE 2. Left kidney of adult male river otter
RAG-245, showing several stones (arrows) within the
minor calyces.
FIGURE 1. Cross sections of a ureter from the affected adult male river otter RAG-245 (top row A)
and a ureter from a control adult male (bottom row
B). Specimens on the left side of each row were collected 3 cm proximal to bladder. Specimens on the
right side of each row were collected 3 cm distal to
renal hilus.
were weighed and measured and abnormalities noted. Sections of abnormal tissues were preserved in 10% buffered formalin and histologic slides were prepared
and stained with hematoxylin and eosin.
The otter had bilaterally enlarged ureters (Fig. 1). We used urogenital tracts of
similar age adult male otters as controls for
gross and microscopic comparisons. A normal ureter is approximately 4.5 mm in diameter (Fig. 1), while the diameter of the
ureters of the affected otter were 8 mm.
The proximal ⅔ of each abnormal ureter
was composed of three distinct lumina
measuring approximately 1 mm in diameter. These lumina gradually converged,
with the distal ⅓ of the ureter having a
single lumen 3 mm in diameter. This point
of union was several cm distal to that of
the two luminal passages seen in the control otter. The muscular walls of the abnormal ureters at this point were approximately 2.5 mm thick.
Calculi were present in all minor calyces
of the kidneys (Fig. 2). Calculi were removed, rinsed in distilled water, and air
dried. A total of 4.9 g (3.2% of kidney
weight) of calculi were removed from the
two kidneys. Mean calculus diameter was
6.02 mm (n530, SD50.75 mm), with diameters ranging from 4.52 to 7.76 mm. A
sample of the calculi was sent to Louis C.
Herring and Company, Analytical and
Consulting Chemists (Orlando, Florida,
USA), for integrated crystallographic analysis. The calculi were analyzed as described by Lloyd and Oldroyd (1983). Uric
acid stones are classified based on crystalline composition, of which the anhydrous
form is the most stable. The calculi were
found to be composed of compact masses
of monoclinic crystals of anhydrous uric
acid, indicating homogeneous nucleation.
Protein matrices were demonstrated. The
calculi were composed of 97% uric acid
and 3% protein.
Histologic examination of the abnormal
kidneys revealed expansion of the renal calyces with concurrent loss of medullary tissue. Two of the four calyces observed contained lamellated masses of basophilic,
non-refractile, and finely filamentous material consistent with urates. Medullary tubules contained unidentified green-brown
crystalline debris. Multifocal atrophy of
cortical tubules was found with concomitant increase in the proportion of interstitial collagen in these areas. Ureteral
changes were characterized by hyperplasia
of the urothelial layer and a remarkable
hypertrophy of the smooth muscle component. No cellular infiltrates suggestive of
an inflammatory component were found in
the ureters or kidneys.
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JOURNAL OF WILDLIFE DISEASES, VOL. 39, NO. 4, OCTOBER 2003
Uric acid (2,6,8-trioxypurine) is the end
product of purine metabolism which is derived by both endogenous and exogenous
routes via a series of enzymatic reactions
involving xanthine oxidase (Shekarriz and
Stoller, 2002). Endogenous uric acid production results from de novo purine synthesis and tissue catabolism under normal
circumstances. However, the exogenous
pool varies widely with diet, with diets rich
in animal protein (such as the river otter’s
diet) contributing significantly to the uric
acid pool. Hoover and Tyler (1986) reported river otter mean fasting uric acid
serum levels of 2.01 (60.66) mg/dl; BenDavid et al. (2001) reported similar findings. The primary mode of uric acid clearance is through urinary excretion, accounting for about two-thirds of its elimination.
Almost all serum uric acid is in the ionized
form (monosodium urate) with ;5% of
the urate bound with serum protein at
physiologic pH. Uric acid is completely filtered at the renal glomerulus. Two factors
contribute to uric acid solubility: uric acid
concentration and solution pH (Shekarriz
and Stoller, 2002). Uric acid is a weak acid
with two dissociation constants (pKa’s at
pH of 5.5 and 10.3) of which the second
pKa is of no physiologic significance. Supersaturation of urine with uric acid occurs when urine pH is less than 5.5, causing uric acid precipitation and subsequent
urolithiasis in a few cases. Hoover and Tyler (1986) reported mean river otter urine
pH at 6.22 with a pH range of 5.029.0.
Therefore, the factors that usually contribute to uric acid calculi formation are acidic
urine, hyperuricosuria, and dehydration
with low urinary volume or stasis.
Bilateral ureteral hypertrophy is often a
consequence of obstruction at the level of
the urinary bladder or urethra, but no lesions were detected in these portions of
the urinary tract. Decreased ureteral function can lead to intra-renal urine stasis,
which may promote nephrolith formation.
It is postulated that the abnormal ureters
in this otter may have been an important
predisposing factor to the development of
nephrolithiasis. Comparison with more otters is required to determine if the unusual
fusion of major calyces seen in this case
represented a congenital anomaly.
Approximately 50% of human uric acid
nephrolithiasis cases are idiopathic. However, certain predisposing factors specific
to this condition have been identified.
These include defects in protein metabolism, as is seen in Dalmations or in dogs
with portosystemic shunts (Osborne et al.,
1995). Otters are carnivorous and thus
must metabolize large amounts of purine
compounds, yet little is known about uric
acid metabolism and clearance in this species. Reference serum biochemical values
for uric acid suggest river otters produce
uric acid in quantities similar to other
mammalian species (Swenson, 1993; Kaneko et al., 1997). There was no opportunity for antemortem assessment of protein metabolism in RAG-245 but the animal was in excellent body condition with
normal muscle mass.
Urease-splitting bacteria within the affected portion of the urinary tract may also
promote uric acid urolith formation (Maxie, 1993). Bacterial cultures were not attempted, but the lack of any inflammation
in the renal or ureteral tissue makes such
an infection unlikely.
We are currently evaluating the river otter as a potential sentinel species for monitoring persistent environmental contaminants (e.g., polychlorinated biphenyls, dioxins, furans) because of its position as a
top predator in most aquatic food chains.
It is important to document and understand diseases and lesions associated with
this species which might affect interpretations of findings concerning contaminant
exposure and accumulation. Also, the large
number of river otters examined during
our study provided a unique opportunity
to discover some of the rarer lesions not
normally found in studies of smaller
groups of animals.
We gratefully acknowledge V. R. Bentley for his assistance during necropsies,
and K. Fisher for her assistance in the
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preparation of histology slides. This study
was funded through both the U.S. Geological Survey and U.S. Fish and Wildlife Service.
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Received for publication 10 March 2003.