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Biogeosciences An interactive open-access journal of the European Geosciences Union
Biogeosciences, 13, 3461-3474, 2016
https://doi.org/10.5194/bg-13-3461-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
15 Jun 2016
Long-term macrobioerosion in the Mediterranean Sea assessed by micro-computed tomography
Claudia Färber1, Jürgen Titschack1,2, Christine Hanna Lydia Schönberg3,4, Karsten Ehrig5, Karin Boos2, Daniel Baum6, Bernhard Illerhaus5, Ulla Asgaard7, Richard Granville Bromley7, André Freiwald1, and Max Wisshak1 1Senckenberg am Meer, Abteilung Meeresforschung, Südstrand 40, 26382 Wilhelmshaven, Germany
2MARUM, Center for Marine Environmental Sciences, University of Bremen, Leobener Straße, 28359 Bremen, Germany
3Oceans Institute, University of Western Australia, Crawley, WA 6009, Australia
4Western Australian Museum, Welshpool, WA 6106, Australia
5Bundesanstalt für Materialforschung und -prüfung (BAM), Unter den Eichen 87, 12205 Berlin, Germany
6ZIB, Zuse Institute Berlin, Takustraße 7, 14195 Berlin, Germany
7Department of Geography and Geology, University of Copenhagen, 1350 Copenhagen K, Denmark
Abstract. Biological erosion is a key process for the recycling of carbonate and the formation of calcareous sediments in the oceans. Experimental studies showed that bioerosion is subject to distinct temporal variability, but previous long-term studies were restricted to tropical waters. Here, we present results from a 14-year bioerosion experiment that was carried out along the rocky limestone coast of the island of Rhodes, Greece, in the Eastern Mediterranean Sea, in order to monitor the pace at which bioerosion affects carbonate substrate and the sequence of colonisation by bioeroding organisms. Internal macrobioerosion was visualised and quantified by micro-computed tomography and computer-algorithm-based segmentation procedures. Analysis of internal macrobioerosion traces revealed a dominance of bioeroding sponges producing eight types of characteristic Entobia cavity networks, which were matched to five different clionaid sponges by spicule identification in extracted tissue. The morphology of the entobians strongly varied depending on the species of the producing sponge, its ontogenetic stage, available space, and competition by other bioeroders. An early community developed during the first 5 years of exposure with initially very low macrobioerosion rates and was followed by an intermediate stage when sponges formed large and more diverse entobians and bioerosion rates increased. After 14 years, 30 % of the block volumes were occupied by boring sponges, yielding maximum bioerosion rates of 900 g m−2 yr−1. A high spatial variability in macrobioerosion prohibited clear conclusions about the onset of macrobioerosion equilibrium conditions. This highlights the necessity of even longer experimental exposures and higher replication at various factor levels in order to better understand and quantify temporal patterns of macrobioerosion in marine carbonate environments.

Citation: Färber, C., Titschack, J., Schönberg, C. H. L., Ehrig, K., Boos, K., Baum, D., Illerhaus, B., Asgaard, U., Bromley, R. G., Freiwald, A., and Wisshak, M.: Long-term macrobioerosion in the Mediterranean Sea assessed by micro-computed tomography, Biogeosciences, 13, 3461-3474, https://doi.org/10.5194/bg-13-3461-2016, 2016.
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In this study we present results from the first long-term bioerosion experiment (1–14 years of exposure) outside the tropical realm. A novel micro-CT approach was used to visualise and to quantify the development of macrobioerosion traces. After 14 years, 30 % of the original substrate volume was excavated chiefly by sponges. High spatio-temporal variability prohibited clear conclusions about the onset of macrobioerosion equilibrium conditions, calling for further long-term experiments.
In this study we present results from the first long-term bioerosion experiment (1–14 years of...
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