Effects of terrestrial sediment on the burial behaviour of post-settlement Macomona liliana

aut.embargoNoen_NZ
aut.thirdpc.containsNoen_NZ
aut.thirdpc.permissionNoen_NZ
aut.thirdpc.removedNoen_NZ
dc.contributor.advisorVopel, Kay
dc.contributor.authorHohaia, Aysha Kefira
dc.date.accessioned2013-06-11T23:11:16Z
dc.date.available2013-06-11T23:11:16Z
dc.date.copyright2012
dc.date.created2013
dc.date.issued2012
dc.date.updated2013-06-09T23:59:30Z
dc.description.abstractTerrestrial and marine environments are connected ecosystems that are similarly vulnerable to the effects of anthropogenic stressors. Climate change and other anthropogenically-induced stressors have resulted in an increased rate of supply (mass per time per area) of terrestrial (land-derived) sediment. This sediment is exported from catchments to rivers, and subsequently, to estuarine and marine systems. Episodic events result in the catastrophic deposition of terrestrial sediment, while small-scale spatial deposition of terrestrial sediment is widespread, and frequent. One pressing issue is the effect of thin depositions of terrestrial sediment on one ecosystem function, such as recruitment of benthic fauna. The tellinid bivalve Macomona liliana is an important component of estuarine and coastal benthos throughout New Zealand, representing one of the most common community dominants across marine ecosystems. Significantly, M. liliana is a sensitive ecological indicator of change. Post-settlement juveniles have been demonstrated to actively avoid adverse local conditions, including sediments affected by the deposition of thin terrestrial sediment. This behavioural response may be triggered by deposit-induced changes in the porewater chemistry of the deposit-underlying sediment, but not by contact of the juveniles with the terrestrial sediment. A laboratory flume experiment was conducted to assess the effect of millimetre-thick terrestrial sediment deposits on porewater chemistry, and the burial behaviour of M. liliana post-settlement juveniles. Terrestrial sediment deposits impeded the diffusion of solutes across the visible sediment surface. This impedance, however, had a negligible effect on the sediment porewater chemistry as a result of resident infauna mediating the exchange of solutes between porewater and bottom water. As such, the deposition of millimetre-thick terrestrial sediment did not negatively affect the burial behaviour of post-settlement juveniles. This study has highlighted the need for a greater understanding of the contribution of bioturbation by resident infauna to solute exchange in sediments affected by periodic deposition of terrestrial sediment. Bioturbation appears to be one of the most important variables to consider when investigating the effects of terrestrial deposits on juvenile M. liliana burial behaviour.en_NZ
dc.identifier.urihttps://hdl.handle.net/10292/5464
dc.language.isoenen_NZ
dc.publisherAuckland University of Technology
dc.rights.accessrightsOpenAccess
dc.subjectSediment biogeochemistryen_NZ
dc.subjectRecruitmenten_NZ
dc.subjectTerrestrial depositsen_NZ
dc.subjectMacomona lilianaen_NZ
dc.subjectMicroprofilesen_NZ
dc.subjectBioturbationen_NZ
dc.subjectLaboratory flumeen_NZ
dc.titleEffects of terrestrial sediment on the burial behaviour of post-settlement Macomona lilianaen_NZ
dc.typeThesis
thesis.degree.discipline
thesis.degree.grantorAuckland University of Technology
thesis.degree.levelMasters Theses
thesis.degree.nameMaster of Applied Scienceen_NZ
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