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JMS 70 1 031-041 Eyh003 FINAL PHYLOGENY AND HISTORICAL BIOGEOGRAPHY OF LIMPETS OF THE ORDER PATELLOGASTROPODA BASED ON MITOCHONDRIAL DNA SEQUENCES TOMOYUKI NAKANO AND TOMOWO OZAWA Department of Earth and Planetary Sciences, Nagoya University, Nagoya 464-8602,Japan (Received 29 March 2003; accepted 6June 2003) ABSTRACT Using new and previously published sequences of two mitochondrial genes (fragments of 12S and 16S ribosomal RNA; total 700 sites), we constructed a molecular phylogeny for 86 extant species, covering a major part of the order Patellogastropoda. There were 35 lottiid, one acmaeid, five nacellid and two patellid species from the western and northern Pacific; and 34 patellid, six nacellid and three lottiid species from the Atlantic, southern Africa, Antarctica and Australia. Emarginula foveolata fujitai (Fissurellidae) was used as the outgroup. In the resulting phylogenetic trees, the species fall into two major clades with high bootstrap support, designated here as (A) a clade of southern Tethyan origin consisting of superfamily Patelloidea and (B) a clade of tropical Tethyan origin consisting of the Acmaeoidea. Clades A and B were further divided into three and six subclades, respectively, which correspond with geographical distributions of species in the following genus or genera: (AÍ) north­ eastern Atlantic (Patella ); (A2) southern Africa and Australasia ( Scutellastra , Cymbula-and Helcion)', (A3) Antarctic, western Pacific, Australasia ( Nacella and Cellana); (BÍ) western to northwestern Pacific (.Patelloida); (B2) northern Pacific and northeastern Atlantic ( Lottia); (B3) northern Pacific (Lottia and Yayoiacmea); (B4) northwestern Pacific ( Nipponacmea); (B5) northern Pacific (Acmaea-’ânà Niveotectura) and (B6) northeastern Atlantic ( Tectura). Approximate divergence times were estimated using geo­ logical events and the fossil record to determine a reference date. Divergence of the two major clades likely occurred as far back as the early Cretaceous. The phylogeny also suggests that nine principal geographic clades were formed during the late Mesozoic to early Cenozoic in association with the disruption of Pangea, which gave rise to new oceans and seaways. INTRODUCTION limpet shells and that they could be used for generic and familial classification. Thus, the diagnostic characters of shell micro­ The limpets of the order Patellogastropoda are of particular structure provide reliable palaeontological evidence for esti­ evolutionary interest, because they are recognized as a basal mating divergence times of clades (Lindberg & Hickman, 1986; branch of the extant Gastropoda, as revealed by cladistic analy­ Lindberg, 1988; Kase, 1994; Rase & Shigeta, 1996). sis of morphological characters (Haszprunar, 1988; Ponder & The first attempt to incorporate all available data from anato­ Lindberg, 1997). They are abundant and familiar inhabitants of my and shell ultrastructure in a cladistic analysis of patellids was intertidal rocky shores throughout the world oceans from tropi­ that of Ridgway (1994) ; however, this work was largely limited to cal to polar regions, and they play an important role in littoral northern Atlantic species. Later, Ridgway, Reid, Taylor, Branch & marine ecosystems (Branch, 1985a, b). Hodgson (1998) constructed a cladogram of species of Patellidae Historically, taxonomical studies of limpets have used exter­ based on all available sets of informative morphological charac­ nal shell morphology, but the high degree of variability of these ters. In their analysis, geographical distributions were superim­ characters has led to taxonomic confusion. It has been recog­ posed on the cladogram to infer historical biogeography. The nized that the radula is a useful character for species-level resulting phylogenetic tree revealed the existence of several distinctions (Pilsbry, 1891; Thiele, 1929). Other characters that monophyletic clades which were treated taxonomically as gen­ have been successfully used to differentiate species are col­ era: Helcion, Cymbula, Scutellastra and Patella in the superfamily oration of the foot and palliai tentacles (Evans, 1947; Bowman, Patellidae. This analysis also suggested that ancestral forms of the 1981), coloration of the egg (Habe, 1944), sperm ultrastracture Patellidae had been widely distributed in southern African (Healy, 1988; Hodgson & Bernard, 1988; Hodgson, Ridgway, waters, and probably in the Tethyan Sea as well. Morphological Branch & Hawkins, 1996), and karyotype of the chromosomes analysis, however, has so far been unable to resolve the phylogeny (Nakamura, 1987; Cervella, Ramella, Robotti & Sella, 1988). of the Patellidae satisfactorily; some unsolved problems, such as Despite numerous studies on the taxonomy of limpets, evolu­ the divergence time of the clades, remain. tionary relationships among them are poorly known. This is largely Molecular techniques can provide important information due to the scant fossil record, reflecting that the high-energy con­ about phylogenetic relationships and divergence times of evolu­ dition of their habitat on intertidal rocky shores is unfavorable for tionary lineages and clades. A molecular phylogenetic study of preservation of shells. Even if a fossil shell is preserved, it is often Patellidae using m itochondorial 12S and 16S ribosomal RNA difficult to make generic and even familial assignments based genes was done recently by Koufopanou, Reid, Ridgway & on the shell structure. However, MacClintock (1967) showed that Thomas (1999). This study clarified, in some detail, the phylo­ shell microstructures were often sufficiently well preserved in fossil genetic relationships and divergence times of geographical clades among the Patellidae in the Atlantic and southern Africa. Correspondence: T. Ozawa; e-mail : [email protected] Their area of origin, however, rem ained unclear in the analysis. J. Moll. Stud, (2004) 70: 31-41 © The Malacological Society of London 2004 T. NAKANO & T. OZAWA Furthermore, there were some incongruities between the results Table 1. List of species newly sequenced in this study. of the cladistic analysis (Ridgway et al, 1998) and the m olecular analysis (Koufopanou et al, 1999). Species Localities Extant limpets show the highest diversity in southern Africa, Acm aea mitra Rathke, 1833 Boiler Bay, W ashington, USA Australia-New Zealand, the Japanese Islands and the west coast of North America (Powell, 1973; Lindberg, 1988), where kelp Cellana grata (Gould, 1859) 1. Kaino, Mie, Japan forests are well developed in the strong upwelling of nutrient- 2. Cape d’Aguilar, Hong Kong rich deep sea waters. As mentioned above, a great deal of effort Cellana nigrolineata (R eeve,1839) Kaino, Mie, Japan has been made on the phylogeny of the Patellidae derived Cellana orientalis (Pilsbry, 1891 ) Okinawa, Japan from the Atlantic, southern Africa and Australia. However, little Cellana testudinaria (Linnaeus, 1758) 1. Shinzato fishing port, Okinawa, progress has been made on the phylogenies of the Lottiidae and Japan the Acmaeidae in the Pacific Ocean. In a comprehensive review 2. Vietnam of patellogastropods, Lindberg (1988) applied cladistic analysis Cellana toreuma(Ree\/e. 1854) 1. Oga, Akita, Japan to all available character sets, and presented the relationships of the Lottiidae and Acmaeidae from the eastern Pacific and 2. Cape d’Aguilar, Hong Kong the western Atlantic seacoasts of North America; however, no Lottia atrata (Carpenter, 1857) Campus Point, California, USA detailed consideration of the Patellidae was made. The purpose Lottia cassis (Eschscholtz, 1833) Akkeshi, Hokkaido, Japan of the present study is to clarify the molecular phylogenetic rela­ Lottia digitalis (Rathke, 1833) Cattle Point, W ashington, USA tionships of the patellogastropods of the world oceans with par­ Lottia dorsuosa (Gould, 1859) Morozaki, Aichi, Japan ticular reference to the Lottiidae in the Pacific and the Atlantic, Lottia emydia (Dali, 1914) Aininkappu, Hokkaido, Japan using combined mitochondrial 12S and 16S sequence data from Lottia fenestrata (Reeve, 1855) Strawberry Hill, Washington, USA the present study and from previous authors (Koufopanou et al., Lottia gigantea Sowerby, 1834 Royal Palms, Los Angeles, USA 1999). A scenario of the phylogenetic evolution and historical biogeography of the patellogastropods is presented by integrat­ Lottia kogam ogai Sasaki & Okutani, 1994 Hiraiso, Ibaraki, Japan ing molecular, morphological, paleontological and geological Lottia langfordi (Habe. 1994) Goshikinohama, Kochi, Japan data. Lottia lim atula (Carpenter, 1864) Coal Oil Point, California, USA Lottia lindbergi Sasaki & Okutani, 1994 Akkeshi, Hokkaido, Japan MATERIAL AND METHODS Lottia luchuana (Pilsbry, 1901) 1. Ogimi, Okinawa, Japan 2. Cape d’Aguilar, Hong Kong Collection of samples andD N A extraction- Lottia pelta (Rathke, 1833) Cattle Point, W ashington, USA Lottia persona (Rathke, 1833) Cattle Point, W ashington, USA Table 1 lists the species and collection localities of specimens analysed by the present authors. Generic assignments were made Lottia scabra (Gould, 1846) Royal Palms, Los Angeles, USA following Lindberg (1986) and Sasaki (1998a, 1999a) with minorLottia scutum (Rathke, 1833) Cattle Point, W ashington, USA amendments. The new samples include most of the species of Lottiasp. cf. borealis (Lindberg, 1982) Akkeshi, Hokkaido, Japan Lottiidae, two species of Patellidae and five species of Nacellidae Lottia tenuisculpta Sasaki & Okutani, 1994 Kaino, Mie, Japan from the Japanese Islands; two lottiid and three nacellid species
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