EGU2020-11698
https://doi.org/10.5194/egusphere-egu2020-11698
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Time averaging and stratigraphic unmixing: reconstructing ecological decline in molluscan production (Holocene, Brijuni, NE Adriatic)

Adam Tomašových1, Martin Zuschin2, Ivo Gallmetzer2, and Alexandra Haselmair2
Adam Tomašových et al.
  • 1Earth Science Institute, Slovak Academy of Sciences, Bratislava, Slovakia (adam.tomasovych@savba.sk)
  • 2University of Vienna, Department of Palaeontology, Althanstrasse 14, 1090 Vienna

The northeastern Adriatic seafloor is formed by warm-temperate bioclastic carbonates with coralline algae, bryozoans and mollusks. These sediments represent a mixture of past and present-day production owing to low sedimentation rates and bioturbation. Although low sedimentation rates do not allow resolution of ecological history at centennial or even millennial scales on the basis of raw stratigraphic data, age unmixing based on radiocarbon-calibrated amino acid racemization shows that one of the major molluscan sediment producers – the infaunal suspension-feeder Timoclea ovata  – markedly peaked in production ~5,000 years during the maximum flooding and earliest highstand phase and significantly diminished in abundance during the late highstand phase at Brijuni, with a large proportion of dead shells now present in surface sediments representing shells that are several centuries old. This species still occurs in living assemblages but our analyses indicate that its former production was by several orders of magnitude higher. In contrast, stratigraphic trends in absolute and proportional abundance of this species in ~1.5 m-thick sediment cores show a gradual or a very mild upcore decline, indicating that raw stratigraphic data do not efficiently detect millennial-scale ecological dynamic. The temporal decline in production of Timoclea ovata is associated with an increase in water depth and an increase in sediment-accumulation rate, and led to a transition from molluscan oyster-scallop shell bed to late highstand bryomol sediments.

How to cite: Tomašových, A., Zuschin, M., Gallmetzer, I., and Haselmair, A.: Time averaging and stratigraphic unmixing: reconstructing ecological decline in molluscan production (Holocene, Brijuni, NE Adriatic), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11698, https://doi.org/10.5194/egusphere-egu2020-11698, 2020

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