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dc.contributorUniversity of Texas at Austin. Marine Science Institute
dc.contributorTexas Water Development Board
dc.creatorMontagna, Paul A.
dc.date.accessioned2017-05-16T21:53:14Z
dc.date.available2017-05-16T21:53:14Z
dc.date.issued1997
dc.identifierdoi:10.15781/T2BV7B16X
dc.identifier.urihttp://hdl.handle.net/2152/46914
dc.description"The primary goal of the current research program is to define quantitative relationships between marine resource populations and freshwater inflows to the State's bays and estuaries. However, we know that there is year-to-year variability in the population densities and successional events of estuarine communities. This year-to-year variability is apparently driven by long-term, and global-scale climatic events that affect the rates of freshwater inflow. Therefore, this report documents long-term changes in populations and communities that are influenced by freshwater inflow. The best indicator of productivity is the change in biomass of the community. A secondary goal of the current research program is to quantify the loss of nitrogen in Texas estuaries. Nitrogen is the key element that limits productivity. A simple budget would account for nitrogen entering the bay via freshwater inflow, how it is captured and transformed into biomass, and finally how it is lost from the ecosystem. One aspect of nitrogen loss is very poorly understood: How much nitrogen is buried and lost from the system? We report here nitrogen content changes with respect to sediment depth. Presumably nitrogen is labile in the upper, biologically active, layers of sediment, and refractory at depth. Therefore, it is important to determine the sediment depth at which nitrogen content is at a low and constant value. This study is a continuation of freshwater inflow studies that began in 1984. The goals have evolved over the years to reflect the synthesis of new information and the management needs of the Texas Water Development Board (TWDB). The original studies (1984-1986) were designed to determine the effect of inflow on Lavaca Bay. One station used during that study is still being sampled. San Antonio Bay was studied in 1987, and the Nueces Estuary (Nueces and Corpus Christi Bays) were studied in 1988. Long-term studies of the Lavaca-Colorado and Guadalupe Estuaries began in 1990. Although, there is ten years worth of data in some cases, we have not sampled over two entire wet-dry cycles. We have sampled over one and one-half cycles. We are currently beginning to enter a dry cycle. The completion of this research will take about two more years and should end when we enter the next wet cycle, which will be heralded by the next El Nino event.en_US
dc.descriptionFrom University of Texas at Austin Marine Science Institute ... to Texas Water Development Board
dc.descriptionInteragency cooperative contract, TWDB contract no. 97-483-199
dc.descriptionDecember 1997
dc.language.isoengen_US
dc.relation.ispartofMSI Technical Reportsen_US
dc.relation.ispartofseriesTechnical report (University of Texas at Austin. Marine Science Institute); no. TR/97-02
dc.subject.lcshEstuaries--Freshwater inflow--Texas--Gulf Coast
dc.subject.lcshMarine invertebrate populations--Texas--Gulf Coast
dc.subject.lcshSeawater--Nitrogen content--Texas--Gulf Coast
dc.subject.lcshBenthos--Ecology--Texas--Gulf Coast
dc.subject.lcshEstuarine ecology--Texas--Gulf Coast
dc.subject.lcshMarine productivity--Texas--Gulf Coast
dc.titleEffect of freshwater inflow on macrobenthos productivity and nitrogen losses in Texas estuaries : final reporten_US
dc.title.alternativeFinal report : effect of freshwater inflow on macrobenthos productivity and nitrogen losses in Texas estuariesen_US
dc.typeTechnical reporten_US
dc.description.departmentMarine Scienceen_US
dc.rights.restrictionOpenen_US


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