Connectivity of the bay scallop (Argopecten irradians) in Buzzards Bay, Massachusetts, USA

Authored by Chang Liu, Geoffrey W Cowles, James H Churchill, Kevin D E Stokesbury

Date Published: 2015

DOI: 10.1111/fog.12114

Sponsors: United States National Science Foundation (NSF)

Platforms: FISCM

Model Documentation: Other Narrative Mathematical description

Model Code URLs: Model code not found

Abstract

The harvest of bay scallops (Argopecten irradians) from Buzzards Bay, Massachusetts, U.S.A. undergoes large interannual fluctuations, varying by more than an order of magnitude in successive years. To investigate the extent to which these fluctuations may be due to yearly variations in the transport of scallop larvae from spawning areas to suitable juvenile habitat (settlement zones), a high-resolution hydrodynamic model was used to drive an individual-based model of scallop larval transport. Model results revealed that scallop spawning in Buzzards Bay occurs during a time when nearshore bay currents were principally directed up-bay in response to a persistent southwesterly sea breeze. This nearshore flow results in the substantial transport of larvae from lower-bay spawning areas to settlement zones further up-bay. Averaged over the entire bay, the spawning-to-settlement zone connectivity exhibits little interannual variation. However, connectivities between individual spawning and settlement zones vary by up to an order of magnitude. The model results identified spawning areas that have the greatest probability of transporting larvae to juvenile habitat. Because managers may aim to increase scallop populations either locally or broadly, the high-connectivity spawning areas were divided into: (i) high larval retention and relatively little larval transport to adjoining settlement areas, (ii) both significant larval retention and transport to more distant settlement areas, and (iii) little larval retention but significant transport to distant settlement areas.

Tags

Model Recruitment Variability Transport Larvae New-york Coastal ocean Finite-volume Retention Lamarck