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dc.rights.licenseCC-BY-NC-ND
dc.contributor.advisorReichart, Gert-Jan
dc.contributor.authorKingma, Enzo
dc.date.accessioned2022-05-03T00:00:32Z
dc.date.available2022-05-03T00:00:32Z
dc.date.issued2022
dc.identifier.urihttps://studenttheses.uu.nl/handle/20.500.12932/41536
dc.description.abstractExcavating sponges are the most common and destructive macro-eroders present in carbonate dominated habitats, such as coral- and oyster reefs. These sponges penetrate in carbonate skeletons and shells, forming a complex network of tunnels and chambers. In temperate climates, their presence can pose a threat to services provided by oyster reefs due to weakening and damaging the oyster shells, which in the long term leads to loss of the reef structure. Sponge bioerosion proceeds by a combination of chemical dissolution and mechanical chip removal. However, the exact chemical conditions during sponge bioerosion are largely unknown. Here, we provided insights into the bioeroding mechanism of Cliona celata present in oyster shells collected from the Grevelingenmeer and the Oosterschelde, The Netherlands. By growing C. celata on pieces of Iceland spar (a pure transparent form of crystalline calcium carbonate) the conditions of dissolution at the sponge-CaCO3 interface were investigated. Using a pH fluorescent probe followed by fluorescence microscopy, we were able to show that the intracellular pH at this interface is lower compared to ambient seawater. This suggests active proton pumping and release of low proton bundles, to be responsible for creating an acidic microenvironment and hence promoting dissolution of CaCO3. Using a model based on the linear Heat-Diffusion equation, we estimated a local proton flux of 3.02 x 10-8 mol dm-2 s-1 towards the edge of the sponge tissue where etching takes place. Additionally, using scanning electron microscopy we showed that bioerosion by C. celata occurs in successive phases; from dissolution of lattice deficiencies, to etching marks that over time form well-developed pitted holes/tunnels and chips. This study adds to the understanding of the mechanisms that drive sponge bioerosion and provides more insight on how environmental conditions can affect calcium carbonate dissolution by excavating sponges as well as making predictions about future rates of sponge activity.
dc.description.sponsorshipUtrecht University
dc.language.isoEN
dc.subjectExcavating sponges are common macro-eroders present in carbonate dominated habitats. These sponges penetrate in carbonate skeletons and shells, which in temperate climates can pose a threat to services provided by oyster reefs. Sponge bioerosion proceeds by a combination of chemical dissolution and mechanical chip removal. In this thesis more insight is provided about the bioeroding mechanism of Cliona celata present in oyster shells collected from the Grevelingenmeer and the Oosterschelde.
dc.titleThe role of the excavating sponge Cliona celata in oyster shells
dc.type.contentMaster Thesis
dc.rights.accessrightsOpen Access
dc.subject.keywordsBioerosion; Excavating sponges; Cliona celata; Fluorescence microscopy; Grevelingenmeer
dc.subject.courseuuMarine Sciences
dc.thesis.id3602


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