Abstract

The large-scale deep-sea biodiversity distribution of the benthic fauna was explored in the Mediterranean Sea, which can be seen as a miniature model of the oceans of the world. Within the framework of the BIOFUN project (“Biodiversity and Ecosystem Functioning in Contrasting Southern European Deep-sea Environments: from viruses to megafauna”), we investigated the large spatial scale variability (over >1,000 km) of the bathyal macrofauna communities that inhabit the Mediterranean basin, and their relationships with the environmental variables. The macrofauna abundance, biomass, community structure and functional diversity were analysed and the α-diversity and β-diversity were estimated across six selected slope areas at different longitudes and along three main depths. The macrobenthic standing stock and α-diversity were lower in the deep-sea sediments of the eastern Mediterranean basin, compared to the western and central basins. The macrofaunal standing stock and diversity decreased significantly from the upper bathyal to the lower bathyal slope stations. The major changes in the community composition of the higher taxa and in the trophic (functional) structure occurred at different longitudes, rather than at increasing water depth. For the β-diversity, very high dissimilarities emerged at all levels: (i) between basins; (ii) between slopes within the same basin; and (iii) between stations at different depths; this therefore demonstrates the high macrofaunal diversity of the Mediterranean basins at large spatial scales. Overall, the food sources (i.e., quantity and quality) that characterised the west, central and eastern Mediterranean basins, as well as sediment grain size, appear to influence the macrobenthic standing stock and the biodiversity along the different slope areas.

Highlights

  • Different studies have been conducted worldwide to define latitudinal and longitudinal diversity patterns of marine biodiversity [1,2,3], which have often been coupled to the bathymetric trends of organisms [4,5,6,7]

  • The bottom water temperature and salinity increased significantly moving eastwards, with values that ranged from 13.1uC and 38.5 for the WM basin to 14.7uC and 38.8 in the EM basin

  • The dissolved oxygen content ranged between 3.7 ml l21 and 4.8 ml l21, with the lowest concentration registered in the EM basin at 1200 m in depth, and the highest in the WM basin (WM-1) at 2400 m in depth

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Summary

Introduction

Different studies have been conducted worldwide to define latitudinal and longitudinal diversity patterns of marine biodiversity [1,2,3], which have often been coupled to the bathymetric trends of organisms [4,5,6,7]. For the last three of these benthic components, they reported that the community standing-stock decreases with depth, and interpreted this to be a universal phenomenon This is, controversial, and should be related to the taxon considered each time within each benthic size component [13,14,15]. For the bathymetric trends in the standing stock, the well-known ‘hump-shape’ distribution in species richness with a diversity maximum at midslope depths might not always be the rule [16,17,18]

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