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Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
Riverine inputs, groundwater efflux, and terrestrial runoff enrich coastal waters with silica. Diatoms, which require silicic acid (Si(OH)4) for frustule formation and cell growth, are therefore predominantly found in these waters. Less...
State of the art fully three-dimensional ocean models are very computationally expensive and their adjoints are even more resource intensive. However, many features of interest are approximated by the first baroclinic mode over much of...
The purpose of this dissertation is to study the interannual flows along the western and southern Australian coasts and along the northern coast of the Gulf of Mexico. Along the western and southern Australian coasts, sea levels are...
The redox speciation of dissolved iron in open ocean seawater was evaluated during two Pacific Ocean research cruises. Using a sensitive flow injection method based on luminol chemiluminescence, vertical profiles of reduced iron...
The objective of this study was to investigate oxygen consumption rates in permeable Gulf coast sediments and their link to changes in the water and sediment chlorophyll concentrations. The investigation was initiated to improve our...
Denitrification in coastal sediments is a process of significant scientific interest and a major concern in coastal management. Reliable estimates of denitrification in coastal ecosystems are unavailable due in large part to a lack of...
The traditional method for producing taxonomic illustrations requires the preparation of inked copies of pencil originals. These individual figures are then grouped into plates for publication. I describe an alternative, computer-based...
Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
