Spawning run estimates and phenology for an extremely small population of Atlantic Sturgeon in the Marshyhope Creek–Nanticoke River system, Chesapeake Bay

Author:

Coleman Nicholas1ORCID,Fox Dewayne2,Horne Ashlee3,Hostetter Nathan J.4,Madsen John5,O'Brien Michael1ORCID,Park Ian6,Stence Chuck3ORCID,Secor David1ORCID

Affiliation:

1. Chesapeake Biological Laboratory Center for Environmental Science, University of Maryland Solomons Maryland USA

2. College of Agriculture and Related Sciences Delaware State University Dover Delaware USA

3. Maryland Department of Natural Resources Annapolis Maryland USA

4. U.S. Geological Survey, North Carolina Cooperative Fish and Wildlife Research Unit, Department of Applied Ecology North Carolina State University Raleigh North Carolina USA

5. Department of Geological Sciences University of Delaware Newark Delaware USA

6. Delaware Division of Fish and Wildlife Dover Delaware USA

Abstract

AbstractObjectiveOnce thought to be extirpated from the Chesapeake Bay, fall spawning runs of Atlantic Sturgeon Acipenser oxyrinchus have been rediscovered in the Marshyhope Creek (MC)–Nanticoke River (NR) system of Maryland, United States. High recapture rates in past telemetry surveys suggested a small population in the two connected tributaries. This study aims to generate estimates of abundance and understand within system connectivity for spawning runs in 2020 and 2021.MethodsData from mobile side‐scan sonar surveys and detections of acoustically tagged adults on stationary telemetry receivers were analyzed in an integrated model to estimate spawning season abundance and examine run timing and system connectivity for this population. An array of acoustic receivers was deployed throughout the MC–NR system to monitor the movement of tagged fish during the spawning run period from mid‐August to late October. Side‐scan sonar surveys were conducted weekly in September in an area of high spawner aggregation to generate count data on spawning run abundance.ResultIn 2020 and 2021, 32 (95% credible interval [CRI] = 23–47) and 70 (95% CRI = 49–105) Atlantic Sturgeon, respectively, used the MC–NR system. The lower estimate for 2020 coincided with an earlier end to the spawning run related to cooler September temperatures in that year.ConclusionIn both years, high spawning run connectivity between MC and the upper NR was observed. Overall, run estimates supported previous hypotheses that the MC–NR system supports a very small population and that both MC and the upper NR serve as important areas for spawning activity.

Funder

National Oceanic and Atmospheric Administration

Publisher

Wiley

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