Abstract

Abstract. Benthic foraminifera from Bottsand coastal lagoon, western Baltic Sea, have been studied since the mid-1960s. They were monitored annually in late autumn since 2003 at the terminal ditch of the lagoon. There were 12 different species recognised, of which three have not been recorded during earlier investigations. Dominant species showed strong interannual fluctuations and a steady increase in population densities over the last decade. Elphidium incertum, a stenohaline species of the Baltic deep water fauna, colonised the Bottsand lagoon in 2016, most likely during a period of salinities >19 units and water temperatures of 18 ∘C on average in early autumn. The high salinities probably triggered their germination from a propagule bank in the ditch bottom sediment. The new E. incertum population showed densities higher by an order of magnitude than those of the indigenous species. The latter did not decline, revealing that E. incertum used another food source or occupied a different microhabitat. Elphidium incertum survived transient periods of lower salinities in late autumn 2017, though with reduced abundances, and became a regular faunal constituent at the Bottsand lagoon.

Highlights

  • Benthic foraminifera are reliable indicators for environmental conditions at the sea floor and general ecosystem status

  • The aim of the project is to create a complement to the Boknis Eck time series (Bange et al, 2011) because the Bottsand lagoon and the adjacent salt marsh are influenced by both surface water dynamics of the Baltic Sea and predominant seasonal weather conditions

  • The trend of increasing species richness continued in the early 2000s as described above, in particular with the recurrent recruitment of two more Elphidium species, Elphidium incertum, and the repopulation of the terminal ditch by Ammotium salsum

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Summary

Introduction

Benthic foraminifera are reliable indicators for environmental conditions at the sea floor and general ecosystem status. Storm surges, turbidites, or drifting sea ice were invoked as the mechanisms of species dispersal beyond these ecological boundaries (Murray et al, 1982; Dieckmann et al, 1987; Lin et al, 2005; Bolliet et al, 2014), whereas only a very few foraminiferal species have been displaced by human activities (McGann et al, 2000; Asteman and Schönfeld, 2016) This static concept of foraminiferal distribution has been challenged by the discovery of foraminiferal propagules (Alve and Goldstein, 2002), i.e. unilocular sexually or asexually produced juveniles, which are on the move and have not yet commenced with growth and chamber formation (Alve and Goldstein, 2003)

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