Abstract

The Mediterranean Sea shows a trend of increasing temperature and decreasing productivity from the western to the eastern basin. In this work we investigate whether this trend is reflected in the cephalopod assemblages found throughout the Mediterranean. Data obtained with bottom trawl surveys carried out during the last 22 years by EU Mediterranean countries were used. In addition to analysing spatial differences in cephalopod assemblages, we also analysed putative temporal changes during the last two decades. For this purpose, the basin was spatially divided into bioregions, the trawling grounds were subdivided into depth strata, and the dataset was split into two time series of 11 years each. All analyses were done using PRIMER software. The species richness did not vary with the longitudinal gradient, though in most bioregions it showed a mild decrease with depth before plummeting in the deepest waters. Cluster analysis revealed four different bathymetric assemblages in all bioregions. Despite the contrasting conditions between basins and the claims of biodiversity loss, our study revealed that spatial and temporal differences during the last two decades were restricted to changes in the relative abundance of species from a common pool of species inhabiting the whole Mediterranean.

Highlights

  • The distribution of living species and communities is determined by a combination of large-scale biogeographic history, migration patterns and environmental conditions (Wiens and Donoghue 2004)

  • Summary: The Mediterranean Sea shows a trend of increasing temperature and decreasing productivity from the western to the eastern basin

  • In this work we investigate whether this trend is reflected in the cephalopod assemblages found throughout the Mediterranean

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Summary

Introduction

The distribution of living species and communities is determined by a combination of large-scale biogeographic history, migration patterns and environmental conditions (Wiens and Donoghue 2004). Between six and five million years ago, the connection between the Atlantic and the Mediterranean Sea through the Strait of Gibraltar was closed, giving rise to the Messinian Salinity Crisis (Manzi et al 2013, Vasiliev et al 2017). This salinity crisis involved the complete disappearance of former deep benthic fauna, which means that the present deep Mediterranean organisms have originated from Atlantic migrations since 5.5 million years ago (Lugli et al 2015)

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