Hydrobiologia

, Volume 687, Issue 1, pp 163–177

Role of deep sponge grounds in the Mediterranean Sea: a case study in southern Italy

Authors

    • Dip. Scienze della Vita e dell’AmbienteUniversità Politecnica delle Marche
  • Marco Bertolino
    • Dip. Scienze della Vita e dell’AmbienteUniversità Politecnica delle Marche
  • Giorgio Bavestrello
    • Dip. Scienze della Vita e dell’AmbienteUniversità Politecnica delle Marche
  • Simonepietro Canese
    • ISPRA
  • Michela Giusti
    • ISPRA
  • Michela Angiolillo
    • ISPRA
  • Maurizio Pansini
    • Dip. per lo Studio del Territorio e delle sue RisorseUniversità degli Studi di Genova
  • Marco Taviani
    • ISMAR-CNR
SPONGE RESEARCH DEVELOPMENTS

DOI: 10.1007/s10750-011-0964-1

Cite this article as:
Bo, M., Bertolino, M., Bavestrello, G. et al. Hydrobiologia (2012) 687: 163. doi:10.1007/s10750-011-0964-1

Abstract

The Mediterranean spongofauna is relatively well-known for habitats shallower than 100 m, but, differently from oceanic basins, information upon diversity and functional role of sponge grounds inhabiting deep environments is much more fragmentary. Aims of this article are to characterize through ROV image analysis the population structure of the sponge assemblages found in two deep habitats of the Mediterranean Sea and to test their structuring role, mainly focusing on the demosponges Pachastrella monilifera Schmidt, 1868 and Poecillastra compressa (Bowerbank, 1866). In both study sites, the two target sponge species constitute a mixed assemblage. In the Amendolara Bank (Ionian Sea), where P. compressa is the most abundant species, sponges extend on a peculiar tabular bedrock between 120 and 180 m depth with an average total abundance of 7.3 ± 1.1 specimens m−2 (approximately 230 gWW m−2 of biomass). In contrast, the deeper assemblage of Bari Canyon (average total abundance 10.0 ± 0.7 specimens m−2, approximately 315 gWW m−2 of biomass), located in the southwestern Adriatic Sea between 380 and 500 m depth, is dominated by P. monilifera mixed with living colonies of the scleractinian Madrepora oculata Linnaeus, 1758, the latter showing a total biomass comparable to that of sponges (386 gWW m−2). Due to their erect growth habit, these sponges contribute to create complex three-dimensional habitats in otherwise homogenous environments exposed to high sedimentation rates and attract numerous species of mobile invertebrates (mainly echinoderms) and fish. Sponges themselves may represent a secondary substrate for a specialized associated fauna, such zoanthids. As demonstrated in oceanic environments sponge beds support also in the Mediterranean Sea locally rich biodiversity levels. Sponges emerge also as important elements of benthic–pelagic coupling in these deep habitats. In fact, while exploiting the suspended organic matter, about 20% of the Bari sponge assemblage is also severely affected by cidarid sea urchin grazing, responsible to cause visible damages to the sponge tissues (an average of 12.1 ± 1.8 gWW of individual biomass removed by grazing). Hence, in deep-sea ecosystems, not only the coral habitats, but also the grounds of massive sponges represent important biodiversity reservoirs and contribute to the trophic recycling of organic matter.

Keywords

Deep benthosPoriferaMediterranean SeaBiodiversityPelagic–benthic coupling

Copyright information

© Springer Science+Business Media B.V. 2011