Abstract

Recruitment of estuarine organisms can vary dramatically from year to year with abiotic and biotic conditions. The San Francisco Estuary (California, USA) supports a dynamic ecosystem that receives freshwater flow from numerous tributaries that drain one of the largest watersheds in western North America. In this study, we examined distribution and habitat use of two forage fish larvae of management interest, Longfin Smelt Spirinchus thaleichthys and Pacific Herring Clupea pallasii, during a low-flow and a high-flow year to better understand how their rearing locations (region and habitat) may affect their annual recruitment variability. During the low-flow year, larval and post-larval Longfin Smelt were distributed landward, where suitable salinity overlapped with spawning habitats. During the high-flow year, larval Longfin Smelt were distributed seaward, with many collected in smaller tributaries and shallow habitats of San Francisco Bay. Local spawning and advection from seaward habitats were speculated to be the primary mechanisms that underlie larval Longfin Smelt distribution during the high-flow year. Larval Pacific Herring were more abundant seaward in both years, but a modest number of larvae were also found landward during the low-flow year. Larval Pacific Herring abundance was lower overall in the high-flow year, suggesting advection out of the area or poor recruitment. Future monitoring and conservation efforts for Longfin Smelt and Pacific Herring should recognize that potential mechanisms underlying their recruitment can vary broadly across the San Francisco Estuary in any given year, which suggests that monitoring and research of these two species expand accordingly with hydrologic conditions that are likely to affect their spawning and larval rearing distributions.

Highlights

  • Nursery habitat within estuarine ecosystems is shaped by the timing and magnitude of SAN FRANCISCO ESTUARY & WATERSHED SCIENCEVOLUME 18, ISSUE 3, ARTICLE 6 freshwater flow, its influence on other dynamic habitat features, and where it intersects with static habitat features (Peterson 2003)

  • In the San Francisco Estuary, research of estuarine biota and their responses to freshwater flow has been focused in the landward region of the estuary where the predominant source of freshwater flow enters the Sacramento-San Joaquin Delta from the Central Valley watershed drainage

  • For Longfin Smelt larvae, a couple of key mechanisms may explain the seaward shift in their distribution during the high-flow year

Read more

Summary

Introduction

Nursery habitat within estuarine ecosystems is shaped by the timing and magnitude of SAN FRANCISCO ESTUARY & WATERSHED SCIENCEVOLUME 18, ISSUE 3, ARTICLE 6 freshwater flow, its influence on other dynamic habitat features (e.g., water temperature, salinity), and where it intersects with static habitat features (Peterson 2003). In the San Francisco Estuary (hereafter “the estuary”), research of estuarine biota and their responses to freshwater flow has been focused in the landward region of the estuary where the predominant source of freshwater flow enters the Sacramento-San Joaquin Delta (hereafter “the Delta”) from the Central Valley watershed drainage. This landward area has a well-defined low-salinity zone that is considered important nursery habitat for many fishes and invertebrates (Stevens and Miller 1983; Jassby et al 1995; Kimmerer et al 2009). These water diversions can affect estuarine biota directly through entrainment mortality (Grimaldo et al 2009; Kimmerer 2008) or indirectly through changes to water quality and habitat availability (Kimmerer 2002a, 2002b; Kimmerer et al 2009)

Objectives
Methods
Results
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call