Mediterranean Corals Through Time: From Miocene to Present

  • Agostina Vertino
  • Jarosław Stolarski
  • Francesca R. Bosellini
  • Marco Taviani
Chapter

Abstract

Stony corals, especially scleractinians, are a recurrent component of the benthic fauna of the Mediterranean basin and its Mesozoic-to-Cenozoic precursors. Both morphological and geochemical features of coral skeletons place these organisms among the most important natural paleoarchives of the Mediterranean geological history. The present day low diversity of the Mediterranean scleractinian fauna (25 genera and only 33 species) strikingly contrasts with its high diversity in the Early-Middle Miocene (over 80 genera and hundreds of species). The decline in coral richness has occurred since the late Middle Miocene onwards. This impoverishment trend was not linear, but abrupt in shallow-water environments during and immediately after the Late Miocene and more gradual since the Pliocene onwards. At the end of the Miocene, the Mediterranean coral fauna underwent a drastic modification that led to the disappearance of almost all zooxanthellate corals and the well-established shallow-water coral-reef province. However, the generic diversity of azooxanthellate and deep-water corals did not undergo significant modifications, that were instead much stronger at the end of the Pliocene and of the Pleistocene. Indeed, before the Calabrian stage, all remnant Indo-Pacific-like azooxanthellate genera disappeared and a clear NE Atlantic affinity was established, whereas at the Pleistocene – Holocene boundary, there was a clear reduction in psychrospheric deep-water taxa. The causes that led to the impoverishment of the Mediterranean coral fauna diversity are complex and not all fully understood. However, there is a clear link between the coral diversity decrease, the gradual northward shift outside the tropical belt of the Mediterranean region, and the major climate modifications on a global scale during the last 20 million years.

Keywords

Corals Scleractinia Mediterranean Neogene Pleistocene Recent Climate 

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Copyright information

© Springer Science+Business Media Dordrecht 2014

Authors and Affiliations

  • Agostina Vertino
    • 1
  • Jarosław Stolarski
    • 2
  • Francesca R. Bosellini
    • 3
  • Marco Taviani
    • 4
    • 5
  1. 1.Department of Earth and Environmental SciencesUniversity of Milano-BicoccaMilanItaly
  2. 2.Institute of PaleobiologyPolish Academy of SciencesWarsawPoland
  3. 3.Department of Chemical and Geological SciencesUniversity of Modena and Reggio EmiliaModenaItaly
  4. 4.Institute of Marine SciencesNational Research Council (ISMAR-CNR), BolognaBolognaItaly
  5. 5.Biology DepartmentWoods Hole Oceanographic InstitutionWoods HoleUSA

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