Abstract
The Mississippi River is the largest river in the United States and discharges substantial amounts of nutrients, organic carbon, and sediments onto the Texas-Louisiana continental shelf in the northern Gulf of Mexico. As a basic part of an initiative to describe processes at the sediment-water interface in the northern Gulf of Mexico shelf ecosystem we measured sediment grain size and per cent total organic carbon. This paper reports sediment grain size characteristics and per cent carbon, and makes preliminary associations between these variables and carbon utilization by the benthos (calculated from sediment oxygen consumption rates) and macrofauna biomass.Comments
This work is licensed under a Creative Commons Attribution 4.0 International License.
Copyright (c) 1993 Revista de Biología Tropical
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