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Kiel and Taviani—Miocene methane-seep bivalves from Italy


Taviani, M., Aharon, P., and Vai, G.B., 1992, Discovery of vesicomyid-faunas in the Marnoso Arenacea Formation (Miocene of Romagna Apennines, Italy): IUGS-SOG Miocene Columbia Project, Portonovo (Ancona, Italy), 11–14 November 1992, Abstracts, unpg.


Taviani, M., Angeletti, L., and Ceregato, A., 2011, Chemosynthetic bivalves of the family Solemyidae (Bivalvia, Protobranchia) in the Neogene of the Mediterranean Basin: Journal of Paleontology, v. 85, p. 1067–1076.


Taylor, J.D., Glover, E.A., and Williams, S.T., 2014, Diversification of chemosymbiotic bivalves: origins and relationships of deeper water Lucinidae: Biological Journal of the Linnean Society, v. 11, p. 401–420.


Taylor, J.D., Glover, E.A., Smith, L., Dyal, P., and Williams, S.T., 2011, Molecular phylogeny and classification of the chemosymbiotic bivalve family Lucinidae (Mollusca: Bivalvia): Zoological Journal of the Linnean Society, v. 163, p. 15–49.


Terzi, C., 1993, The “Calcari a Lucina” (Lucina limestone) of the Tuscan-Romagna Apennines as indicators of Miocene cold seep activity (northern Apennines, Italy): Giornale di Geologia, v. 55, p. 71–81.


Terzi, C., Aharon, P., Ricci Lucchi, F., and Vai, G.B., 1994, Petrography and stable isotope aspects of cold-vent activity imprinted on Miocene- age “calcari a Lucina” from Tuscan and Romagna Apennines, Italy: Geo-Marine Letters, v. 14, p. 177–184.


Thubaut, J., Puillandre, N., Faure, B.M., Cruaud, C., and Samadi, S., 2013, The contrasted evolutionary fates of deep-sea chemosynthetic mussels (Bivalvia, Bathymodiolinae): Ecology and Evolution, v. 3, p. 4748–4766.


Vai, G.B., Taviani,M., Conti, S., and Aharon, P., 1997, Cold-E-Vent. Hydrocarbon Seepage and Chemosynthesis in Tethyan Relic Basins: Products, Processes and Causes, in An International Field Workshop to be held in Bologna and nearby Apennines. June 23–26/1997, Abstracts with Program: Bologna, p. 30.


Valdés, F., Sellanes, J., and D’Elía, G., 2013, Phylogenetic position of vesico- myid clams from a methane seep off central Chile (~36°S) with a molecular timescale for the diversification of the Vesicomyidae: Zoological Studies, v. 51, p. 1154–1164.


von Cosel, R., 2002, A new species of bathymodioline mussel (Mollusca, Bivalvia, Mytilidae) from Mauritania (West Africa), with comments of the genus Bathymodiolus Kenk &Wilson, 1985: Zoosystema, v. 24, p. 259–271.


von Cosel, R., and Janssen, R., 2008, Bathymodioline mussels of the Bathymodiolus (s. l.) childressi clade from methane seeps near Edison Seamount, New Ireland, Papua New Guinea (Bivalvia: Mytilidae): Archiv für Molluskenkunde, v. 137, p. 195–224.


von Cosel, R., and Olu, K., 1998, Gigantism in Mytilidae.Anew Bathymodiolus from cold seep areas on the Barbados accretionary Prism: Comptes Rendus de l’Académie des Sciences, Paris, v. 321, p. 655–663.


von Cosel, R., Métivier, B., and Hashimoto, J., 1994, Three new species of Bathymodiolus (Bivalvia: Mytilidae) from hydrothermal vents in the Lau Basin and the North Fiji Basin, western Pacific, and the Snake Pit area, Mid-Atlantic Ridge: The Veliger, v. 37, p. 374–392.


Woodring, W.P., 1925, Miocene Mollusca from Bowden Jamaica, pelecypods and scaphopods: Carnegie Institution of Washington publications, v. 336, p. 1–564.


Zuschin, M., Mandic, O., Harzhauser, M., and Pervesler, P., 2001, Fossil evidence for chemoautotrophic bacterial symbiosis in the thyasirid bivalve Thyasira michelottii from the Middle Miocene (Badenium) of Austria: Historical Biology, v. 15, p. 223–234.


Accepted 4 November 2016 Appendix


Details of localities (see Figure 1) of Miocene methane-seep bivalves reported in this paper. Regarding the localities from Piedmont mentioned here in the context of the Sacco collection at MRSN (Albugnano, Bersano, Pera del Gal , Pino Torinese, etc.), the reader must refer to the catalog edited byMerlino (2007). The material illustrated by Moroni (1966) was reported to have been stored in the Museo Geologico Giovanni Capellini, University of Bologna, with the S. Sofia collection (catalog numbers 121–140); however, the collection is not present in this museum and is possibly kept in the University of Palermo, but not traceable at present (G. Ruggieri, personal communication, 1996).


1. Abisso “Mornig”.—Micritic limestone blocks near the entrance of “Mornig” cave, SE of Castelnuovo, not far from Brisighella (Ravenna province), Romagna Apennine, northern


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Italy; coordinates: 44°13'40''N, 11°44'72''E; Tossignano marls, late Miocene (late Tortonian).


2. Ca’ Carnè.—Marly to micritic limestone deposits just S-SE of Ca’ Carnè (“Vena del Gesso Romagnola” Regional Park visit center), near Brisighella (Ravenna province), Romagna Apen- nine, northern Italy; coordinates: 44°13'40''N, 11°44'72''E; Tossignano marls, late Miocene (late Tortonian).


3. Ca’ Cavalmagra.—Limestone (calcarenitic) deposit SSE of Palazzuolo (Firenze province), Tuscan Romagna Appenine, northern Italy; coordinates: 44°05'78''N, 11°33'62''E; Marnoso- arenacea Formation, middle Miocene (upper Langhian).


4. Monticino-Limisano – Castelnuovo junction.—Few scattered limestone blocks near the junction between Castelnuovo street and Calbane street, not far from Brisighella (Ravenna province), Romagna Appenine, northern Italy; coordinates 44°14'03.07''N; 11°44'18.72''E; late Miocene (late Tortonian).


5. Ca’ Fornace.—Erratic limestone blocks in the Sintria Creek downstream of the bridge near Ca’ Fornace, near Brisighella (Ravenna province), Romagna Apennine, northern Italy; coordinates: 44°14'14''N, 11°44'40''E; late Miocene (late Tortonian).


6. Ca’ Pianté.—Scattered marly to micritic limestone blocks SW of Ca’ Pianté, not far from Ca’ Carnè and near Brisighella (Ravenna province), Romagna Appenine, northern Italy; late Miocene (late Tortonian); additional information can be found in Conti and Fontana (1998).


7. Case Rovereti.—Large isolated limestone block just NW of the small village of Raggio, near Santa Sofia (Forlì province), Romagna Appenine, Italy; coordinates: 43°55'38''N, 11°56'43''E; located on San Paolo Marls but not necessarily belonging to such stratigraphic unit, late Miocene (middle Tortonian–early Messinian). This deposit has previously been described in more detail (Moroni, 1966; Taviani, 1994; Terzi et al., 1994; Clari et al., 2004a).


8. Castelvecchio.—Limestone (calcarenitic) deposit just W of small village of Castelvecchio, Piancaldoli, near Firenzuola (Firenze province), Tuscan Romagna Apennine, northern Italy; coordinates: 44°11'53''N, 11°24'18''E; Marnoso-arenacea Formation, middle Miocene (early Serravallian).


9. Deruta.—Small blocks at Fosso Castelleone 2 km SE of Deruta (Perugia province), central Italy; coordinates 42°58'15.47''N; 12°26'35.48''E. Upper Miocene (Serravallian). This area was described by Clari et al. (2004b).


10. Le Colline.—Scattered marly to micritic limestone blocks outcrop NE of Salecchio, near Palazzuolo (Firenze province), Tuscan Romagna Appenine, northern Italy; coordi- nates: 44°06'17''N, 11°34'53''E; Marnoso-arenacea Formation, middle Miocene (early Serravallian); further information on this outcrop is provided by Conti and Fontana (1998).


11.Marmorito.—Limestone deposits near the village of Marmorito in the Monferrato hills, east of Torino in the Piedmont Basin in northern Italy; coordinates: 45°03'24''N, 08°01'11''E; late Miocene


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