Skip Navigation

ICES Journal of Marine Science: Journal du Conseil 2006 63(5):811-821; doi:10.1016/j.icesjms.2006.02.003
This Article
Right arrow Full Text Freely available
Right arrow FREE Full Text (PDF) Freely available
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to My Personal Archive
Right arrow Download to citation manager
Right arrowRequest Permissions
Google Scholar
Right arrow Articles by Harris, B. P.
Right arrow Articles by Stokesbury, K. D.E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Harris, B. P.
Right arrow Articles by Stokesbury, K. D.E.
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

© 2006 International Council for the Exploration of the Sea

Shell growth of sea scallops (Placopecten magellanicus) in the southern and northern Great South Channel, USA

Bradley P. Harris* and Kevin D.E. Stokesbury

School for Marine Science and Technology, University of Massachusetts Dartmouth 706 South Rodney French Boulevard, New Bedford, MA 02744, USA

*Correspondence to B. P. Harris: tel: +1 508 910 6359; fax: +1 508 999 8197. e-mail: bharris{at}umassd.edu.

Shell growth of sea scallops in two commercially productive regions of the Great South Channel (GSC) (41°4'N 69°16'W) was studied using tag–recapture experiments. Commercial fishers captured and returned 9.7% of the 11 704 sea scallops tagged in the southern GSC study area, and 7.9% of the 18 274 sea scallops tagged in the northern GSC study area. Scallop density and shell height distribution were sampled with underwater video in the two study areas. In the southern GSC tagged scallops grew faster, reached larger asymptotic size, and had higher growth performance ({Phi}') than in the northern GSC study area. Mean sea scallop density in the southern GSC was 0.117 scallops m–2 (s.e. = 0.01), and 2.601 scallops m–2 (s.e. = 0.28) in the northern GSC. Environmental factors, fishing pressure, and sea scallop density all influence shell growth on a fine geographic scale (1–100 km2) and should be considered in area-specific management strategies, such as that currently used in the USA sea scallop fishery.

Keywords: area-specific management, growth performance index, Placopecten magellanicus, sea scallop shell growth

Received 10 June 2005; accepted 6 February 2006.


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?


This article has been cited by other articles:


Home page
ICES J. Mar. Sci.Home page
D. R. Hart and A. S. Chute
Estimating von Bertalanffy growth parameters from growth increment data using a linear mixed-effects model, with an application to the sea scallop Placopecten magellanicus
ICES J. Mar. Sci., December 1, 2009; 66(10): 2165 - 2175.
[Abstract] [Full Text] [PDF]



Disclaimer: Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.