Master of Science
Dr. Tamara Frank
Dr. Rosanna Milligan
Dr. Tracey Sutton
The Charlie Gibbs Fracture Zone (CGFZ) consists of two nearly parallel fracture transform faults that intersect the Mid-Atlantic Ridge (MAR) axis. This area has high primary productivity and biomass levels due to the topography and water. A predominant hydrographic feature of the MAR is the Sub-Polar Front (SPF) which runs along the southern edge of the CGFZ and is known as a biogeographical boundary for multiple species. As part of The Census of Marine Life project Patterns and Processes of the Ecosystem of the northern Mid-Atlantic (MAR-ECO), this study analyzed the abundance and distribution patterns of the CGFZ crustacean community (primarily Decapoda) surveyed during the 2009 Henry B. Bigelow voyage. This study determined that geographic location, in relation to the CGFZ, contributes to pelagic crustacean distribution, but the surrounding water masses are the primary drivers of abundance and diversity variations. Pelagic crustaceans had a larger abundance in the cold waters to the northwest of the CGFZ, presumably due to increased nutrients and food supply and higher diversity in the warmer southeastern waters, possibly due to dominating mesoscale eddies. Benthic crustaceans, however, had a higher abundance and increased diversity in the northwest, possibly due to the MAR acting as a biogeographic barrier separating the two geographic regions and reducing connectivity. Additionally, this study did not find the SPF to be an asymmetric species-specific biogeographic barrier for decapod crustaceans along the CGFZ.
Kathryn Medina. 2022. Crustacean assemblage structure over the Charlie-Gibbs Fracture Zone of the Mid-Atlantic Ridge collected during the 2009 Henry B. Bigelow expedition. Master's thesis. Nova Southeastern University. Retrieved from NSUWorks, . (112)