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9 Spatio-Temporal Distribution of Mediterranean Cold-Water Corals

  • Agostina VertinoEmail author
  • Marco Taviani
  • Cesare Corselli
Chapter
Part of the Coral Reefs of the World book series (CORW, volume 9)

Abstract

Cold-water corals have inhabited the Mediterranean basin since at least the Miocene, undergoing important modifications through time. Most information regarding pre-Pleistocene occurrences of extant cold-water coral species still relies on ancient literature records in need to be updated according to modern taxonomic and chronostratigraphic concepts. In this chapter, Neogene and Quaternary coral records are discussed. Many occurrences have been revised from the taxonomic point of view through the analysis of historical museum collections, newly collected specimens and original species descriptions and illustrations. In particular, this study summarises the current state of knowledge on Mediterranean frame-building cold-water corals and associated solitary species from the Miocene onwards. Several growth and demise phases, as well as changes in composition of dominant species have been observed so far. A shift from Dendrophyllia- to “Atlantic-like” Lophelia-dominated paleocommunities occurred at the Pliocene – Pleistocene boundary. “Golden ages” for the species Lophelia pertusa, and large bioconstructions formed by this coral, are thus far known in the Early Pleistocene (Calabrian stage), at the boundary Bølling- Allerød – Younger Dryas and in the Early Holocene (at least in the western basin). A large knowledge gap currently exists between the end of the Calabrian stage and the last 50 kyr BP. Several Atlantic deep-sea species (including frame-building and “psychrosperic” cold-water corals), common in the Early Pleistocene, disappeared in the Mediterranean after the Late Pleistocene, but how and when this event occurred is not known yet. Further studies need to be carried out to understand if there is any correlation between this deep-sea basin-scale extinction and the decline of Lophelia-dominated bioconstructions observed in the late Younger-Dryas and after the Early Holocene. In order to fill knowledge gaps on the fossil record of Mediterranean cold-water corals and to fully exploit the valuable potential of these organisms as palaeoenvironmental archives, the setup of a comprehensive open access database, including quality-controlled data on both modern and fossil species, is highly recommended. This would also provide a useful tool for managing, valorising and preserving the unique, yet undervalued paleontological heritage of the Mediterranean regions.

Keywords

Cold-water coral Mediterranean Neogene Quaternary Deep-sea Bioconstruction 

Notes

Acknowledgements

This chapter is dedicated to the memory of our friend and colleague, Jean-Pierre Henriet, a unique scientist and a special person, whose pioneer studies on CWC mounds have inspired many young academics and promoted important advances in this research field. His endless enthusiasm has been the motor of the COCARDE-ERN (European Research Network) programme, funded by the European Science Foundation, from which the study presented herein greatly benefited. This research is also part of EU F.P. VII Projects COCONET, (contract no. 287844), and EVER-EST (contract no. 674907), DG Environment programme IDEM (grant agreement No 11.0661 /2017/750680/SUB/EN V.C2), and the Flag Project Ritmare (Ricerca Italiana per il Mare) project, and is Ismar-Bologna scientific contribution n. 1938. We are very grateful to Fabio Marchese for providing the georeferenced map of the Mediterranean used as background in Fig. 9.3. We warmly thank Lydia Beuck, Francesca Bosellini, Italo Di Geronimo, André Freiwald, Juergen Titschack, Alessandro Vescogni and Helmut Zibrowius for constructive discussions on the evolution of modern and ancient Mediterranean deep-sea coral environments. We are moreover grateful to Antonietta Rosso, Italo Di Geronimo, Francesca Bosellini, Enzo Burgio, Daniele Ormezzano, Paolo Serventi for help in accessing the fossil scleractinian historical collections in the following Italian repositories: Museum of Paleontology, University of Catania, Museum of Paleobiology and Botanical Garden, University of Modena and Reggio Emilia, “G. Gemmellaro” Museum of Palaeontology and Geology, University of Palermo, Museum of Natural History, Torino University. Marco Sami, Vincenzo Bugnano and Massimo Rocca kindly made available to us a number of Neogene scleractinians. Paolo Montagna and Tim Collart are warmly thanked for useful suggestions regarding the treatment of 14C coral datings. Last but not least, special thanks go to the editors (Covadonga Orejas and Carlos Jiménez) and the reviewers (Antonietta Rosso and Jarek Stolarski) who provided constructive criticism that helped us to improve the manuscript.

Supplementary material

394268_1_En_9_MOESM1_ESM.docx (72 kb)
Appendix 9.1_May2019_Vertino (DOCX 73 kb)
394268_1_En_9_MOESM2_ESM.docx (64 kb)
Ch 9_Appendices 2-3_FullChapter_FINAL_Appendices_27012018_AV (DOCX 65 kb)

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Copyright information

© Springer International Publishing AG, part of Springer Nature 2019

Authors and Affiliations

  • Agostina Vertino
    • 1
    • 2
    Email author
  • Marco Taviani
    • 3
    • 4
    • 5
  • Cesare Corselli
    • 1
  1. 1.CONISMA Local Research Unit (LRU) of Milano-Bicocca, Department of Earth and Environmental SciencesMilano-Bicocca UniversityMilanItaly
  2. 2.Department of Geology, Renard Centre of Marine GeologyGhent UniversityGhentBelgium
  3. 3.Institute of Marine Sciences (ISMAR-CNR)BolognaItaly
  4. 4.Biology DepartmentWoods Hole Oceanographic InstitutionWoods HoleUSA
  5. 5.Stazione Zoologica Anton DohrnNaplesItaly

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