**The title, authors, and abstract for this completion
report are provided below. For a copy of
the completion report, please contact the GLFC via e-mail or via telephone at 734-662-3209**
MORPHOLOGICAL
DIVERSITY OF LAKE TROUT: DIFFERENTIATION
BETWEEN
DEEP AND SHALLOW FORMS
Andrew Muir1, Charles C. Krueger1,
Randy L. Eshenroder1, Mara S. Zimmerman2
1 2100
Commonwealth Blvd. Suite 100, Ann Arbor, Michigan 48105
2 Washington
Department of Fish and Wildlife, 600 Capitol Way N, Olympia,
WA 98501
December 2011
ABSTRACT:
Rehabilitation of deepwater lake trout in
the Laurentian Great Lakes requires a scientific basis for understanding
deepwater forms and how they differ from those found in shallow water. Efforts
in this regard were fueled by recent discoveries of multiple lake trout forms
in Great Bear Lake (Alfonso 2004, Blackie et al. 2003) as well as from our own
field work in Great Slave Lake. We requested funding to broaden the geographic
range of lakes included in our analysis of lake trout phenotypic diversity to
better define the diversity and differentiation expected in rehabilitated
deepwater communities. Our research objectives were as follows: (1) determine
the prevalence of humper- , siscowet-, and lean-like morphologies in deepwater
communities at a broad geographic scale; (2) determine whether buoyancy is
associated with deepwater morphologies of lake trout at a broad geographic
scale; and (3) compare the depths of capture and gut contents of forms within
and among these five lakes. We found evidence of similar patterns of diversity
in Great Slave Lake, Lake Mistassini, and Great Bear Lake with shallow and
deepwater morphs occurring, but the patterns were not parallel as we predicted.
In Great Slave Lake, shallow-water (<50m), large lake trout were light in
color, low buoyancy, streamlined, and possessed short pectoral fins. In deep
water (>50m), small lake trout were dark in color, high buoyancy, deep
bodied, and had long pectoral fins. In Lake Mistassini, a shallow-water form
(< 50-m depth) was identified by streamlined shape, dark body coloration,
and high buoyancy. A second deep-water form (> 50-m depth) was identified by
a deep anterior-body profile, light body coloration, and low buoyancy. Low
buoyancy tissue was characteristic of the deep-water morphotype in Great Slave
Lake but not Great Bear Lake or Lake Mistassini. Ontogenetic changes in
habitat, depth, and buoyancy supported the conclusion that “humper” and
“siscowet” deep-water forms are ecologically unique from each other and from
sympatric shallow-water forms. Humper-like trout fed in marginal, deep-water
habitats and grew slowly; siscowet-like trout transitioned at ~ 40 cm length to
feed on deep-water pelagic prey and grew fat. Invertebrate eaters and
piscivores, shallow-water morphotypes unique to Great Bear Lake, may be
maintained by ready shallow-water access to both fish and invertebrate
resources in this cold lake.