Ecology and distribution of living planktonic foraminifera of the south Texas outer continental shelf

dc.contributor.advisorCasey, Richard E.
dc.creatorBauer, Mary Alvina
dc.date.accessioned2018-12-18T21:18:29Z
dc.date.available2018-12-18T21:18:29Z
dc.date.issued1976
dc.descriptionNo pages 44, 52, 76, 87-92
dc.description.abstractA seasonal study of the ecology and distribution of planktonic foraminifera was undertaken for the south Texas outer continental shelf. Twelve stations were occupied for winter, spring, and summer seasons. A total of 36 vertical plankton tows were obtained using a 76 micron mesh Nansen net. Fifteen live planktonic foraminiferal species were identified. In addition, seventeen live benthonic foraminiferal species were also encountered in the plankton tows. One benthonic species, Bolivina lowmani. was a major constituent of inner shelf samples. This species is believed to undergo a meroplanktonic stage. Total live planktonic foraminiferal densities averaged 7.2, 3.91, and 8.15 individuals/m for winter, spring, and summer, respectively. The largest standing crop occurred contemporaneously with the smallest densitiy of empty planktonic foraminiferal tests. Both densities and diversities were found to increase seaward across the shelf. The approximate ecologie niche of planktonic foraminifera was ascertained from their relationship to large, solitary, centric diatoms. Multivariate numerical techniques of R and Q mode cluster analysis were utilized to discern subtle seasonal assemblages and distributional patterns. Assemblages of planktonic foraminifera and their spatial distributions across the shelf were found to be correlabe to physical oceanography and, thus, to exhibit seasonal variations. Twelve sediment samples from the study area were also examined to compare populations of planktonic foraminifera in the water column with those preserved in the fossil record. A striking discrepancy was noted between tests of planktonic foraminifera in the plankton and those in the sen diments. Sediment forams were at least two to three times larger than individuals of the same species in the plankton. Absence of these small individuals is believed caused by rapid dissolution of the fragile tests from acidic conditions initiated by decomposition of the organism's protoplasm shortly after death (McMillen, 1976). Chi-square test and cluster analysis were also utilized in plankton to sediment comparisons. Results from these statistical methods indicated that the two populations were not the same. Thus, it can be inferred that the bottom sediment samples represent relict shelf sediments.
dc.format.digitalOriginreformatted digital
dc.format.extent181 pp
dc.identifier.callnoThesis Geol. 1976 Bauer
dc.identifier.citationBauer, Mary Alvina. "Ecology and distribution of living planktonic foraminifera of the south Texas outer continental shelf." (1976) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/104183">https://hdl.handle.net/1911/104183</a>.
dc.identifier.digitalRICE1810
dc.identifier.urihttps://hdl.handle.net/1911/104183
dc.language.isoeng
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.
dc.titleEcology and distribution of living planktonic foraminifera of the south Texas outer continental shelf
dc.typeThesis
dc.type.materialText
thesis.degree.departmentEarth Science
thesis.degree.disciplineNatural Sciences
thesis.degree.grantorRice University
thesis.degree.levelMasters
thesis.degree.nameMaster of Arts
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