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Basso et al.: Lithothamnion crispatum Hauck 145
bridge Stereoscan 360 at 15 or 20 kV at the Milano facilities Harvey et al. 2003: 654–658, fig 7, A–C; Woelkerling et al.
and in a SEM Leica Stereoscan 430i in the Trieste CSPA, 2005: 460).
centre for Coordinamento e Sviluppo di Progetti e Appa-
recchiature. Modern Mediterranean collections were pre- Mesophyllum superpositum (Foslie) Adey (1970: 26) (see also
served in 4% commercial formalin in seawater. For light Woelkerling 1993: 218).
microscopy (LM), pieces of thallus were decalcified with
Tellyesniczkyi’s solution (Bressan 1970) for 12–48 h, MATERIAL EXAMINED: Western Mediterranean: Elba Is-
washed in distilled water, dehydrated through a graded land, 45 m (D. Basso, R/V Minerva site min90abe120-121,
ethanol series and embedded in methacrylate resin (Tech- 1 December 1990, GR/MMmes1, GR/MMmes2); Pontian
novit 7100, Heraeus Kulzer, Wehrheim, Germany). Prep- Islands, 73–78 m (D. Basso, R/V Minerva site min89edg02,
aration of serial sections follows Basso & Rodondi (2006). 7 July 1989, 020692b4), misidentified in Basso (1995, pl. 5,
Permanent slides for LM were examined and photographed fig. 5) as Lithothamnion philippii Foslie; Egads, Marettimo
with a Leica DMRB photomicroscope. Island, 40 m (D. Basso, 25 August 1993, 4894b4-b5)
misidentified in Basso (1996) as Mesophyllum agariciformis
Anatomical terminology follows Adey & Adey (1973) Pallas; CMF1; CMF3; DMF2A; DMF3B; DMF8;
and Woelkerling (1988), and growth form terminology FMU2B; FMU1A. Eastern Mediterranean: Rovinj, north-
follows Woelkerling et al. (1993). Conceptacle measure- ern Adriatic Sea, lectotype of L. crispatum Foslie (collector
ments follow the system of Adey & Adey (1973) and were and date unknown); Moscenicka Draga (Rijeka Bay),
made directly from the SEM or under LM using a infralittoral zone, middle Adriatic Sea (S. Kaleb, September
calibrated eyepiece micrometer. Cell measurements follow 2004, TSB 1147 LTT CRS 1c); Assos, Pelitko¨ y, Foc¸a,
Basso et al. (2004). Karaburun, Sıg˘acık, O¨ zdere-Kalemlik, Dilek Peninsula,
Aegean coasts of Turkey, 2–5 m depth. Indian Ocean:
OBSERVATIONS Araher, Socotra Island, Yemen, rhodolith in a carpet reef at
18 m depth (A. Caragnano, 13 March 2010, SO9b/DB614);
Lithothamnion crispatum Hauck (1878: 289) Corner Inlet, Victoria (southeastern Australia) 4.5–7 m
depth, lectotype of Lithothamnion indicum Foslie (J.
Figs 1–30; Table 1 Gabriel, 1897) designated by Woelkerling (1993: 125),
TRH: B7-2084, Woelkerling et al. 2005: 280.
LECTOTYPE: L, 943.7-75 (Rijksherbarium, Leiden, Nether-
lands), box 9395 #1 (Woelkerling & Verheij 1995). HABITAT AND PHENOLOGY: Mediterranean and Atlantic
plants unattached, forming rhodoliths, on infralittoral and
ETYMOLOGY: Crispatum means curly or wrinkled, as the upper circalittoral biodetritic soft substrates at 2–78 m
habit of the Mediterranean plant described and illustrated depth (Basso 1995, Keats et al. 2000; Bressan & Babbini
by Hauck (1878, pl. 3, figs 1–4) 2003, Kurt et al. 2009, da No´ brega Farias et al. 2010).
Tetrasporangial plants collected in August and December;
ILLUSTRATIONS OF TYPE MATERIAL: Cabioch & Mendoza gametangial plants collected in August. Australian plants
1998: 218, figs 28–29. epilithic or unattached as rhodoliths, down to depths of
20 m (Wilks & Woelkerling 1995, as L. indicum; Harvey et
HOMOTYPIC SYNONYM: Lithophyllum crispatum (Hauck) al. 2003, as L. superpositum). South African plants collected
Hauck (1885: 270); on hard substrates, attached (Keats et al. 2000).
HETEROTYPIC SYNONYMS: GEOGRAPHIC DISTRIBUTION: Lithothamnion crispatum is a
cosmopolitan species. It has been recorded from Madeira,
Archaeolithothamnion crispatum (Hauck) Foslie (1898: 3) Mauritania and South Africa (as L. superpositum, Keats et
al. 2000), and westward to the Atlantic coast of South
Lithothamnion brasiliense f. heteromorpha Foslie (1900: 4) (see America along the Brazilian coast (as L. superpositum, da
also Woelkerling et al. 2005: 455; da No´ brega Farias et al. No´ brega Farias et al. 2010). The species has been identified
2010: 211–214) from the eastern and western Mediterranean (Babbini &
Bressan 1997; Bressan & Babbini 2003 and present work).
Lithothamnion fruticulosum f. confinis Foslie (1904b: 4) (see also In the Indian Ocean, it is recorded from the Amirante
Woelkerling 1993: 58) Islands, Djibuti, Indonesia, Maldives and Seychelles (as L.
indicum, Silva et al. 1996), and eastward to Victoria,
Lithothamnion heteromorphum (Foslie) Foslie (1908: 10) (see Australia (as L. indicum, Wilks & Woelkerling 1995;
also Adey 1970: 20; da No´ brega Farias et al. 2010: 210–216; Woelkerling 1996) and the Pacific coast of Australia (Coffs
Woelkerling et al. 2005: 455) Harbour, as L. superpositum, Harvey et al. 2003).
Lithothamnion indicum Foslie (1907: 7) as Lithothamnion HABIT AND VEGETATIVE STRUCTURE: The lectotype is a
indicum f. typica (see also Printz 1929: 42, pl. 13, figs 24, rhodolith with fruticose to foliose growth form. The
29, as Lithothamnion indicum f. typica; Adey & Lebednik protuberances are cylindrical to lamellate, up to 15 mm
1967: 58; Woelkerling 1993: 125; Wilks & Woelkerling 1995: long and up to 3 mm wide at their flared, distal end
558, fig 7; Harvey et al. 2003: 658–659, figs D–F; (Hauck 1878, pl. 3, figs 1, 2; Hauck 1885, pl. 2, fig. 3;
Woelkerling et al. 2005: 279–280). Cabioch & Mendoza 1998, fig. 28). The lectotype thallus
fragments are pseudoparenchymatous, monomerous and
Lithothamnion philippii Foslie f. crispata (Hauck) Foslie (1904a:
13) (see also Cabioch & Mendoza 1998: 215, figs 30, 31);
Lithothamnion superpositum Foslie (1900: 8, figs 3–7) (see also
Printz 1929: pl. 12, fig. 10; Adey & Lebednik 1967: 82;
Woelkerling 1993: 218; Keats et al. 2000: 381, figs 31, 32;