LXVIII.—<i>The Cirripede</i> Chelonibia <i>in the Miocene of Gironde, France, and Vienna, Austria</i>

Withers, Thomas H.

doi:10.1080/00222932908673099

Cited by 6 publications

(10 citation statements)

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“…Anderson, 1994: 297; Bacon, 1976: 34; Barnard, 1924: 93; Borradaile, 1903: 443; Broch, 1924a: 16; Bugoni et al, 2001: 7; Caine, 1986: 19; Daniel, 1955: 32; Darwin, 1854: 394; Dawydoff, 1952: 129; Dobbs & Landry, 2004: 674; Farrapeira, 2010: 212; Frick & Ross, 2002: 10; Frick et al, 1998: 213; 2003a: 9; 2003b: 19; 2011: 638; Fuller et al, 2010: 1743; Gittings et al, 1986: 3; González et al, 2012: 132; Gramentz, 1988: 33; Gray, 1825: 105; Gruvel, 1905a: 266; Hayashi, 2012: 109; Hincks, 1840: 333; Hiro, 1936a: 61; 1937a: 69; Holthius, 1952: 77; Innocenti, 2006: 6; Jones, 2003: 483; 2004: 122; 2010: 208; Jones et al, 1990: 11; 2000: 260; Kobayashi, 2000: 91; Kolosváry, 1943: 99; Korschelt, 1933: 13; Limpus et al, 1983a: 192; Loop et al, 1995: 246; Matsuura & Nakamura, 1993: 1803; Monroe, 1981: 237; Monroe & Limpus, 1979: 199; Mörch, 1852: 67; Nilsson-Cantell, 1938: 14; Pfaller et al, 2006: 3; 2008: 1096; Pilsbry, 1916: 267; Rawson et al, 2003: 2699; Ritchie, 1924: 166; Ross, 1963b: 223; Ross & Frick, 2011: 61; Schärer, 2003: 88; Spengler, 1790: 185; Stubbings, 1967: 297; Utinomi, 1969: 92; Wells, 1966: 84; Weltner, 1897: 254; 1910: 528; Wirtz et al, 2006: 209; Withers, 1928a: 391; 1929: 567; Young, 1991: 191; 1998: 271; Zullo, 1963: 13; 1982: 2; Zullo & Bleakney, 1966: 164.…”

Section: Checklistunclassified

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A checklist of turtle and whale barnacles (Cirripedia: Thoracica: Coronuloidea)

Hayashi

2012

J. Mar. Biol. Ass.

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Section: Checklistunclassified

“…Harzhauser et al, 2011: 477; Ross, 1963b: 223; Ross & Frick, 2011: 61; Rothpletz & Simonelli, 1890: 724; Withers, 1928a: 390; 1929: 567; Zullo, 1982: 2.…”

Section: Checklistunclassified

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A checklist of turtle and whale barnacles (Cirripedia: Thoracica: Coronuloidea)

Hayashi

2012

J. Mar. Biol. Ass.

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“…The Mediterranean fossil record of coronuloid barnacles is marked by a predominance of whale barnacles that are represented by at least five species in three genera (Cetopirus Ranzani, 1817, Coronula Lamarck, 1802 and Tubicinella Lamarck, 1802) from various Upper Pliocene to Holocene deposits in Italy, Cyprus and Spain (e.g., Aradas 1854;Seguenza 1873;Simonelli 1893;De Alessandri 1895, 1906De Gregorio 1895;Menesini 1968;Cipolla 1978;Bossio et al 1993;Bianucci et al 2006;Dominici et al 2011;Álvarez-Fernández et al 2014;Collareta 2016;Collareta et al 2016bCollareta et al , 2018aCollareta et al , 2018bBosselaers et al 2017). In the same broad region, fossil turtle barnacles are known to start occurring from the Miocene (Seguenza 1876;De Alessandri 1895, 1906Withers 1929;Bianucci 1996;Harzhauser et al 2011;Collareta et al 2016a) but, up to now, they merely comprise a few Neogene occurrences of the chelonibiid genera Chelonibia Leach, 1817 and †Protochelonibia Harzhauser & Newman 2011in Harzhauser et al, 2011. Therefore, MSNC 4562 represents the first occurrence of a fossil platylepadid in the Mediterranean Basin.…”

Section: Discussionmentioning

confidence: 99%

The oldest platylepadid turtle barnacle (Cirripedia, Coronuloidea): a new species of Platylepas from the Lower Pleistocene of Italy

Collareta

Reitano

Rosso

et al. 2019

EJT

677

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Coronuloid barnacles are epibionts of several marine vertebrates (including cetaceans and sea turtles) as well as invertebrates, and are assigned to two families of turtle barnacles (Chelonibiidae Pilsbry, 1916 and Platylepadidae Newman & Ross, 1976) and one family of whale barnacles (Coronulidae Leach, 1817). Chelonibiids and coronulids have a scanty, albeit significant fossil record extending back to the Eocene and Pliocene, respectively; in turn, the fossil record of platylepadids is limited to a single record from the Upper Pleistocene. Here we report on an isolated carinolateral compartment of Platylepas Gray, 1825, the type genus of the family, from Lower Pleistocene (Gelasian) epibathyal deposits exposed at Milazzo (Sicily, Italy). This specimen is here designated holotype of a new species, †Platylepas mediterranea sp. nov. We argue that, like most extant members of Platylepas, †P. mediterranea sp. nov. lived partially embedded in the skin of a sea turtle. This record of an extinct platylepadid – the first from the Mediterranean region and the second worldwide – pushes back the fossil record of Platylepadidae to the lowermost Quaternary, thus possibly supporting an even earlier (e.g., Neogene) timing for the origin of this family and adding a new chapter to the evolutionary history of one of the most diverse and successful lineages of epizoic crustaceans.

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“…aChelonibia patula dentata Henry, 1943: 370, here regarded as not unambiguously distinguishable from the patula morph above, Rec. †Chelonibia solida Withers, 1929: 568, stat. nov., herein, L.…”

Section: Emended Diagnosis (Modified After Ross and Frick 2011)mentioning

confidence: 99%

A new chelonibiid from the Miocene of Zanzibar (Eastern Africa) sheds light on the evolution of shell architecture in turtle and whale barnacles (Cirripedia: Coronuloidea)

et al. 2021

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The fossil history of turtle and whale barnacles (Coronuloidea: Chelonibiidae, Platylepadidae, Coronulidae and †Emersoniidae) is fragmentary and has only been investigated in part. Morphological inferences and molecular phylogenetic analyses on extant specimens suggest that the roots of whale barnacles (Coronulidae) are to be found among the chelonibiid turtle barnacles, but the hard‐part modifications that enabled early coronuloids to attach to the cetacean skin are still largely to be perceived. Here, we reappraise a fossil chelonibiid specimen from the Miocene of insular Tanzania that was previously referred to the living species Chelonibia caretta. This largely forgotten specimen is here described as the holotype of the new species †Chelonibia zanzibarensis. While similar to C. caretta, †C. zanzibarensis exhibits obvious external longitudinal parietal canals occurring in‐between external longitudinal parietal septa that abut outwards to form T‐shaped flanges, a character so far regarded as proper of the seemingly more derived Coronulidae and Platylepadidae. Along with these features, the presence of a substrate imprint on the shell exterior indicates that †C. zanzibarensis grasped its host's integument in much the same way as coronulids and platylepadids, albeit without the development of macroscopic parietal buttresses and bolsters. Thin section analyses of the inner parietal architecture of some extant and extinct coronuloids conclusively demonstrate that vestiges of comparable external parietal microstructures are present in some living members of Chelonibiidae. This observation strengthens the unity of Coronuloidea while significantly contributing to our understanding of the evolution of the coronuloid shell structure in adapting to a diverse spectrum of hosts.

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LXVIII.—The Cirripede Chelonibia in the Miocene of Gironde, France, and Vienna, Austria

Cited by 6 publications

References 0 publications

A checklist of turtle and whale barnacles (Cirripedia: Thoracica: Coronuloidea)

A checklist of turtle and whale barnacles (Cirripedia: Thoracica: Coronuloidea)

The oldest platylepadid turtle barnacle (Cirripedia, Coronuloidea): a new species of Platylepas from the Lower Pleistocene of Italy

A new chelonibiid from the Miocene of Zanzibar (Eastern Africa) sheds light on the evolution of shell architecture in turtle and whale barnacles (Cirripedia: Coronuloidea)

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