Summary
Research reveals that the West Arm of Glacier Bay National Park and Preserve, Alaska, is divided into two distinct marine environments: a dynamic upper fjord and a relatively static lower fjord. This differentiation is driven by high glacial sediment flux and meltwater inputs, which dominate the seafloor substrate with mud and create a highly dynamic estuarine ecosystem. The study utilized multibeam sonar, ground-truthed observations, and geological interpretations to map benthic habitats using the CMECS classification scheme. Additionally, sediment accumulation data from differential bathymetry and water-column characteristics from CTD measurements and circulation models were analyzed. These findings not only test the utility of the CMECS classification in glacimarine environments but also establish a baseline for future research on the correlations between seafloor substrate, benthic habitats, and glacial processes.
Citation
Hodson, T. O., Cochrane, G. R., & Powell, R. D. (2013). Marine benthic habitat mapping of the West Arm, Glacier Bay National Park and Preserve, Alaska. Scientific Investigations Map. https://doi.org/10.3133/sim3253