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A hidden treasure: Ecological implications from benthic foraminiferal propagule banks in coastal environments of Corfu (Ionian Sea)

Subject Area Ecology and Biodiversity of Animals and Ecosystems, Organismic Interactions
Palaeontology
Term from 2016 to 2022
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 323009980
 
Final Report Year 2022

Final Report Abstract

The project “A hidden treasure: Ecological implications from benthic foraminiferal propagule banks in coastal environments of Corfu (Ionian Sea)” covered several aspects of the ecology and diversity of shallow-water foraminifera. A total of 200 benthic species were identified that showed specific distribution patterns along the island: assemblages from the rocky shores of the north and the sandy bays of the south showed the most striking differences. Water depth and vegetation cover contributed highly to the different faunal compositions. Most sediment samples contained specimens of Amphistegina lobifera, which is classified as an invasive alien species. Whenever A. lobifera exceeded 20% of the relative abundances in a sample, it had a significant negative effect on diversity. In particular, small miliolid foraminifera and attached or partially attached epiphytes showed reductions in abundances as they occupy the same microhabitats. However, for the moment this was only observed in a few samples. Nevertheless, with ongoing ocean warming and a continuing proliferation of A. lobifera, further assemblage changes in the shallow-water communities can be expected. Several independent culture experiments on foraminiferal propagules (small juveniles) from lagoon sites in Corfu offered new insights into the structure and composition of local propagule banks as well as assemblage reactions to different environmental variables: The experiments showed that the propagule assemblages varied between seasons (spring and fall) and that sampling time appears to be important for interpretation. Propagule banks from different lagoons were also composed differently, even though environmental conditions were comparable. Contrary to expectations, the use of different substrate types during the experiments had no significant effect on the resulting assemblages. Overall, there seemed to be a more dominant influence from the higher amount of organic material in fine sediments. Cultivation experiments of propagule banks under different pH-values revealed significant differences between higher (7.8) and lower pH conditions (7.2). Higher treatments were dominated by porcelaneous specimens, while lower treatments showed much higher abundances in agglutinated specimens. Propagules grown under lower pH and subsequently under higher pH were again strongly dominated by porcelaneous specimens. Interestingly, mortality was rather low even under low pH conditions and some porcelaneous specimens were able to survive with broken or partially diluted shells. This suggests some recovery potential of shallow-water communities. Cultivation experiments of propagules under different temperatures showed differences between the settings, which corroborates previous studies. Assemblages were able to grow under temperatures of 29–36°C, but in lower numbers and with a lower survival rate than in 22°C. When material from both settings was re-cultivated under lower temperatures (22°C and 26°C), the assemblages still exhibited significant differences according to the first treatment (29–36°C and 22°C). This suggests that shallow-water assemblages are able to sustain episodes of very high temperatures, but could be lastingly influenced by these conditions. High numbers of allochthonous (non-local) foraminifera grew in all experiments. As these species suggest a “hidden” diversity within the propagule banks, sub-samples of long-term cultivation experiments were analyzed with morphological and molecular methods (metabarcoding). Both approaches revealed comparable patterns in the resulting assemblages, mostly influenced by sampling season (spring or fall) and cultivation time (5, 10, or 15 weeks). With the metabarcoding, it was possible for the first time to compare the fine fraction (<63 µm) and the grown fraction (> 63 µm), which revealed significant differences that also sustained over the course of the experiments. This gives insights into the mechanisms behind quick assemblage reactions of foraminifera to environmental changes.

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