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Phylogenetic analysis of rhodolith formation in the Corallinales (Rhodophyta)
Authors:Jazmín J. Hernández-Kantún  Rafael Riosmena-Rodriguez  Jason M. Hall-Spencer  Viviana Peña  Christine A. Maggs  Fabio Rindi
Affiliation:1. Martin Ryan Institute, National University of Ireland, Galway, Irelandjaz1083@gmail.com;3. Departamento de Biología Marina, Universidad de Baja California Sur (UABCS) Apartado postal 19-B, km. 5.5 Carretera al sur, La Paz, B.C.S. 23080, México;4. School of Marine Science and Engineering, Plymouth University, PL4 8AA, UK;5. BIOCOST Research Group, Universidade da Coru?a, Campus de A Zapateira, S/N, 15071, A Coru?a, Spain;6. UMR 7205 ISYEB CNRS, MNHN, UPMC, EPHE, Equipe Exploration, Espèces et Evolution, Institut de Systématique, Evolution, Biodiversité, Muséum National d′Histoire Naturelle, case postale no 39, 57 rue Cuvier, 75231, Paris, France;7. Phycology Research Group, Ghent University, Krijgslaan 281, Building S8, 9000, Ghent, Belgium;8. School of Biological Sciences, The Queen’s University of Belfast, 97 Lisburn Road, Belfast BT9 7BL, Northern Ireland;9. Martin Ryan Institute, National University of Ireland, Galway, Ireland;10. Dipartimento di Scienze della Vita e dell’Ambiente, Università Politecnica delle Marche, Via Brecce Bianche, 60131 Ancona, Italy
Abstract:Although the ecological importance of rhodolith (maerl, free-living coralline algae) beds is well-known, rhodolith-forming species have been neglected in molecular phylogenetic studies. This is the first molecular systematic study aimed at understanding whether the rhodolith habit is a fixed feature in lineages and determining the relationship (phylogenetic vs. environmental) between rhodolith and crustose habits. Phylogenetic relationships of rhodolith-forming species and encrusting coralline algae at generic and species levels were analysed using SSU rDNA and psbA sequences. Extensive sampling in the European North Atlantic, Pacific and Caribbean Mexico of Phymatolithon, Lithothamnion, Lithophyllum and Neogoniolithon taxa forming rhodoliths and crusts was accompanied by examination of type or topotype material. Phylogenetic reconstruction showed that Neogoniolithon contained a monophyletic group of rhodolith-forming species whereas other rhodolith-formers were closely related to encrusting forms in the genera Phymatolithon, Lithothamnion, Mesophyllum, Hydrolithon, Spongites and Sporolithon. DNA analysis showed that the crust-forming Lithophyllum cf. incrustans/dentatum also forms rhodoliths with a stone nucleus that occur on rocky shores. In contrast, species that form beds of non-nucleate rhodoliths (e.g. Neogoniolithon spectabile, N. strictum, Lithophyllum cf. incrustans/dentatum or sp. 1 and Phymatolithon calcareum) rarely form crusts. The rhodolith habit cannot be used to delimit species for taxonomic or identification purposes. Extensive taxonomic revision will be required to deal with problems such as the position of specimens identified as Lithophyllum margaritae in two unrelated lineages.
Keywords:cryptic species  Lithophyllum  maerl  Phymatolithon  psbA  rhodolith  SSU rDNA  synapomorphy
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