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Petition to List Lynn Canal Pacific Herring under the Endangered ...

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1984). The corresponding stray rates of 6-34% indicate <strong>the</strong>re is more than<br />

sufficient gene flow between neighboring spawning areas <strong>to</strong> compromise <strong>the</strong><br />

ability of allozyme markers <strong>to</strong> discriminate between putative s<strong>to</strong>cks (Smith and<br />

Jamieson 1986; Bembo et al. 1996; Waples 1998). Waples (1998) warned,<br />

“because <strong>the</strong> amount of migration necessary <strong>to</strong> obscure most genetic evidence of<br />

s<strong>to</strong>ck structure (only a handful of individuals per generation) is generally<br />

inconsequential as a force for rebuilding depleted populations on a time scale of<br />

interest <strong>to</strong> humans, <strong>the</strong>re is no guarantee that genetic methods alone will provide<br />

sufficient precision for key management decisions involving marine species”.<br />

(Otis and Heintz 2003).<br />

4. Distinct Spawning Time and Location<br />

The <strong>Lynn</strong> <strong>Canal</strong> <strong>Herring</strong> are separated from o<strong>the</strong>r populations of herring in<br />

Sou<strong>the</strong>ast Alaska by a distinct spawning time. Skud (1959) first described different<br />

spawning times as follows:<br />

Each year <strong>the</strong> initial spawning in Sou<strong>the</strong>astern Alaska occurs in <strong>the</strong> vicinity of<br />

Craig during late March. Kah Shakes, Sitka, and Auke Bay spawnings follow and<br />

are usually completed in early May. Spawning times in Behm <strong>Canal</strong>, E<strong>to</strong>lin<br />

Island, and Frederick Sound are variable and have been reported in late April,<br />

May, and early June. Some areas do not conform <strong>to</strong> <strong>the</strong> nor<strong>the</strong>rly and westerly<br />

progression in spawning time described by Rounsefell (1930).<br />

(Skud 1959: 16).<br />

5. Distinct Wintering and Summer Feeding Location and<br />

Migration<br />

The wintering grounds and summer feeding grounds for <strong>Lynn</strong> <strong>Canal</strong> <strong>Herring</strong> are<br />

entirely within <strong>the</strong> confines of <strong>Lynn</strong> <strong>Canal</strong> and adjacent waters. Whereas o<strong>the</strong>r <strong>Pacific</strong><br />

<strong>Herring</strong> populations in Sou<strong>the</strong>ast Alaska venture fur<strong>the</strong>r out in<strong>to</strong> <strong>the</strong> open ocean for<br />

summer feeding (i.e. Sitka population) <strong>Lynn</strong> <strong>Canal</strong> <strong>Herring</strong> remain in <strong>Lynn</strong> <strong>Canal</strong> and do<br />

not <strong>under</strong>go a large migration (Carlson 1980). In addition, <strong>the</strong> wintering grounds for<br />

<strong>Lynn</strong> <strong>Canal</strong> <strong>Herring</strong> near Auke Bay also isolate <strong>the</strong>m from o<strong>the</strong>r herring populations in<br />

Sou<strong>the</strong>ast Alaska (Carlson 1980).<br />

Based on Carlson (1980) NMFS has described <strong>the</strong> <strong>Lynn</strong> <strong>Canal</strong> <strong>Herring</strong> as a<br />

“discrete population” of <strong>the</strong> <strong>Pacific</strong> herring since at least 1980.<br />

The <strong>Lynn</strong> <strong>Canal</strong>/Auke Bay herring s<strong>to</strong>ck is a discrete population distinguishable<br />

by <strong>the</strong>ir concentration for overwintering in Auke Bay and Fritz Cove (Carlson<br />

1980). The location of this wintering area probably accounts, in part, for <strong>the</strong><br />

geographic proximity of <strong>the</strong> observed major spawning grounds.<br />

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