Abstract

doi: http://dx.doi.org/10.15447/sfews.2014v12iss4art3 California’s Feather River Hatchery (FRH) propagates two runs of Chinook salmon (Oncorhynchus tshawytscha): spring run and fall run. Loss of spawning habitat and historical hatchery practices have led to introgression of these runs. Recent efforts to reform hatchery operations at the FRH are focused on reducing introgression and increasing the proportion of natural-origin spawners in the broodstock. Implementing these reforms, however, requires a means of distinguishing FRH fish from natural-origin fish, and FRH spring-run fish from FRH fall-run fish. Coded-wire tagging and parentage-based genetic tagging can be used for this purpose, but are labor-intensive and expensive. Otolith thermal marking (OTM) is a 100% marking technique widely used in the Pacific Northwest, Alaska, and Russia that can be effective and relatively inexpensive. We initiated an OTM program at the FRH in 2005 to determine its viability as a 100% marking tool for a hatchery with an annual production goal of 10 million smolts. Our analysis of otoliths collected from returning adults at the FRH demonstrated that OTM could be successfully applied to identify the origin (FRH or natural) and, for FRH fish, the run type (spring run or fall run). Otoliths collected between 2009 and 2011 show run-type mixing between 12% to 20% in both spring-run and fall-run FRH broodstock. Additionally, results suggest natural-spawner contribution to hatchery broodstock is very low (<1% to 10%). OTM may provide another way to reduce the rate of introgression between FRH spring-run and fall-run Chinook salmon, and increasing the proportion of natural origin spawners in hatchery broodstock, both of which should improve the long-term viability of FRH spring-run and fall-run Chinook salmon.

Highlights

  • The Feather River drainage is located in the Central Valley of California and supports both spring-run and fall-run Chinook salmon (Oncorhynchus tshawytscha) populations

  • Our success in correctly identifying run type of hatchery individuals varied from 48% to 100% for spring-run and 78% to 100% for fall-run (Table 2)

  • We found the accuracy and ease of reading thermal marks to be related to the quality of the thermal marks

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Summary

Introduction

The Feather River drainage is located in the Central Valley of California and supports both spring-run and fall-run Chinook salmon (Oncorhynchus tshawytscha) populations. Fall-run salmon migrate from the ocean in fall and historically spawned in the lower foothill reaches. SAN FRANCISCO ESTUARY & WATERSHED SCIENCE from the ocean in the spring and early summer and historically spawned in the uppermost reaches in cold mountain tributaries (Yoshiyama et al 2001). Life history strategies of spring run and fall run have historically created both temporal and spatial reproductive isolation. All natural-origin river spawning of spring run and fall run is concentrated in the first 12 river kilometers (rkm) below the Oroville Dam. Spring-run still migrate in spring and early summer but hold over in cold deep pools of the lower Feather River during the hot summer months, a by-product of Oroville Dam operations. Because the spawning times of spring-run and fallrun salmon overlap, both spatial and temporal reproductive isolation have been lost

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