Abstract

Restoration of native oyster (Crassostrea virginica) populations in Chesapeake Bay shows great promise after three decades of failed attempts. Population models used to inform oyster restoration had integrated reef habitat quality, demonstrating that reef height determines oyster population persistence and resilience. Larval recruitment drives population dynamics of marine species, yet its impact with reef height and sediment deposition upon reef restoration is unknown. To assess the influence of reef height, sediment deposition and larval supply, we adapted a single-stage population model to incorporate stage structure using a system of four differential equations modeling change in juvenile density (J), and changes in volume of adults (A), oyster shell reef (R), and sediment (S) on an oyster reef. The JARS model was parameterized with empirical data from field experiments. Larval supply included larvae from the natal population and from outside populations. The stage-structured model possessed multiple non-negative equilibria (i.e., alternative stable states). Different initial conditions (e.g., oyster shell reef height) resulted in different final states. The main novel findings were that the critical reef height for population persistence and resilience was jointly dependent on sediment input and larval supply. A critical minimum larval supply was necessary for a reef to persist, even when initial sediment deposition was zero. As larval supply increased, the initial reef height needed for reef persistence was lowered, and oyster reef resilience was enhanced. A restoration oyster reef with higher larval influx could recover from more severe disturbances than a reef with lower larval influx. To prevent local extinction and assure a positive population state, higher levels of larval supply were required at greater sediment concentrations to overcome the negative effects of sediment accumulation on the reef. In addition, reef persistence was negatively related to sediment deposited on a reef prior to larval settlement and recruitment, implying that restoration reefs should be constructed immediately before settlement and recruitment to minimize sediment accumulation on a reef before settlement. These findings are valuable in oyster reef restoration because they can guide reef construction relative to larval supply and sediment deposition on a reef to yield effective and cost-efficient restoration strategies.

Highlights

  • Native oyster species are dominant ecosystem engineers, which provide a diverse suite of ecosystem services, including water filtration, food and habitat for various species, shoreline stabilization, coastal defense, and enhanced fisheries production (Cerco and Noel, 2007; Coen et al, 2007; Grabowski and Peterson, 2007; Grabowski et al, 2012)

  • A stage-structured model composed of juvenile density J, and volumes of adults A, dead oyster shell reef R, and sediment S on an oyster reef (JARS model) was parameterized with empirical data from field experiments

  • This enabled us to determine the collective influence of larval supply P and sediment deposition C on oyster reef resilience, and the critical initial dead-shell reef height R0 for reef persistence

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Summary

INTRODUCTION

Native oyster species are dominant ecosystem engineers, which provide a diverse suite of ecosystem services, including water filtration, food and habitat for various species, shoreline stabilization, coastal defense, and enhanced fisheries production (Cerco and Noel, 2007; Coen et al, 2007; Grabowski and Peterson, 2007; Grabowski et al, 2012) These species were once abundant worldwide, such as the eastern oyster Crassostrea virginica of the western Atlantic and Gulf of Mexico coasts (Winslow, 1881; Baylor, 1895). We conduct numerical and bifurcation analyses of the model for initial reef height under differing levels of larval supply and sediment concentration to produce a comprehensive evaluation of population dynamics relevant for oyster restoration

STAGE-STRUCTURED DEMOGRAPHIC MODEL
Juvenile Oyster Density
References φ
Switching Functions
Live Adult Oyster Volume
Dead Oyster Shell Volume
Sediment Accumulation
PARAMETER ESTIMATES
Maturation Rate
Conversion of Juvenile Density to Oyster Volume
Larval Recruitment Function
Carrying Capacity
Dead Oyster Shell Degradation Rate
Consistency of Single-Stage and Stage-Structured Models
Bifurcation Analysis
Bifurcation Structure as a Function of P
Bifurcation Structure as a Function of C and P
Threshold Reef Height
DISCUSSION
DATA AVAILABILITY STATEMENT
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