Show simple item record

dc.contributor.authorThomas, OIiver Robert Bion
dc.date.accessioned2019-03-12T04:05:42Z
dc.date.available2019-03-12T04:05:42Z
dc.date.issued2018en_US
dc.identifier.urihttp://hdl.handle.net/11343/221421
dc.description© 2019 Dr Oliver Robert Bion Thomas
dc.description.abstractAll vertebrates have small bioinorganic “earstones” in their inner ear labyrinth that are essential for hearing and balance. While otoliths play a vital anatomical role in fish, their true value to science is as biochronometers, largely due to their unique pattern of growth. Otoliths first form in embryo and continue to grow throughout the life of an individual, with a double-banded increment composed of a calcium carbonate-rich region and a protein-rich region being deposited daily. In addition to this, they are considered to be metabolically inert, and do not undergo remodelling or resorption. Consequently, otoliths are employed in a variety of ways in fish ecology. Firstly, an individual fish’s age and growth rate can be estimated through counting increments and measuring their widths. Secondly, analysis of increment trace element:calcium ratios, such as by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), can allow for the reconstruction of environmental histories, aiding in the determination of natal origin, movement, habitat use, diet and the impacts of climate change. The utility of specific trace elements as indicators of environmental change, however, is unclear as there is considerable uncertainty as to whether a given trace element is interacting with the mineral or protein components of an increment. This uncertainty is a consequence of otolith research having been largely focussed upon either microstructure or inorganic chemistry, with very few studies on the protein-rich regions of the otolith. As a result, very little is understood about the biochemical mechanisms of biomineralization or trace element incorporation. This is important, as the mechanisms that govern otolith formation and growth underpin the assumptions made in traditional increment analyses. In this thesis, I initially undertook a systematic review of all the literature pertaining to otolith biochemistry, revealing the significant gaps that exist in otolith biochemistry as a discipline. Importantly, I determined that fewer than a score of otolith proteins had been identified – a stark contrast to the hundreds or thousands of proteins that have been identified in comparable biomineral systems such as enamel or bone. Working on black bream (Acanthopagrus butcheri), an extensively studied species endemic to southern Australia, I used size exclusion chromatography coupled with ICP-MS to determine the trace element:protein interactions in endolymph, the inner ear fluid that otoliths are submerged in, and the source of all of its constituents. In this study, I assayed 22 elements, and determined that 12 were solely present in a protein-bound form, 6 were present as free ions, and 4 were present in both forms. This allowed me to make recommendations as to their utility in environmental reconstructions. In my next study, I created a unique, multi-disciplinary workflow that combined transcriptomics with proteomics. In this study, I sequenced the transcriptome of the black bream inner ear and used this to identify proteins from the separated organic phase of otoliths and endolymph from wild caught adult black bream. This resulted in the discovery of hundreds of previously unknown proteins, providing new insights into the likely biochemical mechanisms involved in otolith formation and growth. In my final study, I tested the utility of trace element ratios in environmental reconstructions. Specifically, I compared the ability of different cluster analysis approaches to resolve spatial and temporal differences in the likely spawning and larval nursery habitats of juvenile black bream in the Gippsland Lakes, Australia. The results from my thesis have allowed me to make recommendations as to the utility of trace elements in environmental reconstructions and have revealed exciting new avenues of research that fuse ecology and biochemistry.en_US
dc.rightsTerms and Conditions: Copyright in works deposited in Minerva Access is retained by the copyright owner. The work may not be altered without permission from the copyright owner. Readers may only download, print and save electronic copies of whole works for their own personal non-commercial use. Any use that exceeds these limits requires permission from the copyright owner. Attribution is essential when quoting or paraphrasing from these works.
dc.subjectotolithen_US
dc.subjectproteomicsen_US
dc.subjectmetallomicsen_US
dc.subjectendolymphen_US
dc.subjectinner earen_US
dc.subjectbiomineralizationen_US
dc.subjectcluster analysisen_US
dc.subjectAcanthopagrus butcherien_US
dc.subjectblack breamen_US
dc.subjectGippsland Lakesen_US
dc.subjectlaser ablation-inductively coupled plasma-mass spectrometryen_US
dc.titleBiochemical mechanisms of biomineralization and elemental incorporation in otoliths: implications for fish and fisheries researchen_US
dc.typePhD thesisen_US
melbourne.affiliation.departmentSchool of BioSciences
melbourne.affiliation.facultyScience
melbourne.thesis.supervisornameSwearer, Stephen
melbourne.contributor.authorThomas, OIiver Robert Bion
melbourne.accessrights This item is embargoed and will be available on 2021-03-12. This item is currently available to University of Melbourne staff and students only, login required.


Files in this item

FilesSizeFormatView

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record