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Holopterygius nudus Jessen (P 7789), latest Givetian–earliest Frasnian, Bergisch-Gladbach, Germany. ( a ) Photograph of P 7789a; ( b ) composite drawing based on P7789a-c; and ( c ) reconstruction. Bones outlined in grey in ( c ) were reconstructed based on Allenypterus . Scale bar represents 10 mm. Abbreviations: ano, anocleithrum; bp, basal plate of the second dorsal fin; chy, ceratohyal; cla, calvicle; cle, cleithrum; cop, principal coronoid; ex, extracleithrum; has, haemal arch and spine; gs, indeterminate components of the gill skeleton; nas, neural arch and spine; op, opercle; ot, otolith; pal, palate; pap, parapophyses; pmx, premaxilla; psph, parasphenoid; rd, radials of the dorsal lobe of the caudal fin; rv, radials of the ventral lobe of the caudal fin; sr, skull roof; sym, symplectic; vs, ventral keel scales. 

Holopterygius nudus Jessen (P 7789), latest Givetian–earliest Frasnian, Bergisch-Gladbach, Germany. ( a ) Photograph of P 7789a; ( b ) composite drawing based on P7789a-c; and ( c ) reconstruction. Bones outlined in grey in ( c ) were reconstructed based on Allenypterus . Scale bar represents 10 mm. Abbreviations: ano, anocleithrum; bp, basal plate of the second dorsal fin; chy, ceratohyal; cla, calvicle; cle, cleithrum; cop, principal coronoid; ex, extracleithrum; has, haemal arch and spine; gs, indeterminate components of the gill skeleton; nas, neural arch and spine; op, opercle; ot, otolith; pal, palate; pap, parapophyses; pmx, premaxilla; psph, parasphenoid; rd, radials of the dorsal lobe of the caudal fin; rv, radials of the ventral lobe of the caudal fin; sr, skull roof; sym, symplectic; vs, ventral keel scales. 

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Previously considered an actinopterygian or an osteichthyan incertae sedis, the Devonian (Givetian-Frasnian) Holopterygius nudus is reinterpreted as a coelacanth. This genus is among the oldest coelacanths known from articulated remains, but its eel-like morphology marks a considerable departure from the conventional coelacanth body plan. A cladist...

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Context 1
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 2
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 3
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 4
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 5
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 6
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 7
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 8
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 9
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 10
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 11
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 12
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 13
... a long tooth-bearing fragment on the opposite side of the skull probably represents a portion of the dentary from the other mandible. The deep dorsal process of the jaw is composed of an expanded posterior coronoid ( figure 1 b , cop), which is a coelacanth synapomorphy (Forey 1998). Small teeth anterior to the principal coronoid may be the remains of additional members of the series. The posterior ramus of the jaw corresponds to the retroarticular process of other coelacanths, and is overlain by a stocky cylindrical bone that is identified as the symplectic (figure 1 b , sym), a major component of the coelacanth tandem jaw joint. The ceratohyals (figure 1 b , chy) are flared distally and proximally. Narrow endoskeletal rods represent remains of the gill skeleton (figure 1 b , gs). The cleithrum and clavicles (figure 1 b , cle, cla) are well-preserved and exhibit the slender proportions characteristic of coelacanths crownward of Miguashaia (Cloutier 1996; Forey 1998). Holopterygius also possesses an extracleithrum (figure 1 b , ex), an additional dermal ossification that is a coelacanth synapomorphy (Forey 1998). Although Jessen (1973) noted the similarities between the pectoral girdles of Holopterygius and coelacanths, he did not consider this resemblance sufficient to justify placement within the group. Fragments of the anocleithrum (figure 1 b , ano) are located dorsal to the tip of the cleithrum, and suggest this bone was of the simple unbranched morphology primitive for actinistians. The distinctive postcranium of Holopterygius is leaf- shaped, with a greatly elongated caudal region. Despite the unusual body shape of this genus, the components of its postcranial skeleton conform to the general coelacanth pattern. There are approximately 80 postcranial segments, just over 20 of which are abdominal. Vertebral centra are unossified, but small ossifications located below the abdominal neural arches may represent parapophyses (figure 1 b , pap). There are no ossified ribs. Neural arches and spines (figure 1 b , nas) and haemal arches and spines (figure 1 b , has) are co-ossified. The dorsal and ventral lobes of the diphycercal caudal fin are each supported by a single row of endoskeletal radials (figure 1 b , rd, rv). There is a one-to-one ratio between radials and neural or haemal spines and a greater than one-to-one relationship between fin rays and radials. Jessen (1973) reconstructed Holopterygius with multiple radials per body segment, but this seems to have been informed by reference to conditions in tarrasiid actinopterygians (Lund & Melton 1982; Taverne 1996). Direct comparison with Tarrasius problematicus (Natural History Museum, London, P.1167, P.18064, P.18065, P.18061) confirms the difference in spine to radial ratios. It is not possible to determine whether the fin rays were segmented in Holopterygius as in most coelacanths, or unsegmented as in Allenypterus (Lund & Lund 1985). The dorsal and ventral lobes of the caudal fin are strongly asymmetrical, with the dorsal lobe extending much further anteriorly, as in Allenypterus (Lund & Lund 1985; Forey 1998). No components of the first dorsal, pectoral, anal or pelvic fins are preserved. An irregularly shaped ossification located dorsal to the neural spines immediately anterior to the first radial of the caudal fin probably represents the basal plate of the second dorsal fin (figure 1 b , bp). No squamation is preserved on the flanks of Holopterygius , but a series of keel scales run along the ventral margin of the body from just behind the skull to approximately the midpoint of the abdominal region (figure 1 b , vs). It is possible that the absence of scales covering the body of Holopterygius is size-related, as scales are often not preserved in small fossil coelacanths (Lund & Lund 1985). There is no indication of the ossified swim bladder characteristic of derived coelacanths. Widely cited studies place coelacanths as the most basal extant sarcopterygian radiation (Cloutier & Ahlberg 1996; Forey 1998), but little is known about their early history. While the first crown-group sarcopterygians are known from Lower Devonian (Lochkovian; 411–416 Ma) depos- its (Cloutier & Ahlberg 1996), the oldest unequivocal coelacanths are of Givetian age (385–392 Ma; Forey 1998; Long 1999; Forey et al . 2000). Previously described Devonian coelacanths fall into two morphological cat- egories: primitive forms ( Gavinia , Miguashaia ) with postcrania resembling those of other plesiomorphic sarcopterygians, and more crownward taxa ( Chagrinia , Diplocercides ) whose postcranial anatomy is similar to that of stratigraphically younger and phylogenetically more derived coelacanths, including the Recent Latimeria . Holopterygius marks a considerable anatomical departure from other Devonian forms, and a cladistic analysis places it as the sister taxon of Allenypterus , another early coelacanth with unusual postcranial morphology (analysis and results are described in figure 2 a ). Two unequivocal synapomorphies link these genera: a series of ventral keel scales and an asymmetrical caudal fin in which the dorsal lobe extends far beyond the anterior extremity of the ventral lobe. Both of these fishes have unstable taxonomic histories resulting from their unconventional body profiles; like Holopterygius , Allenypterus was identified as an actinopterygian (Melton 1969) before being recognized as a coelacanth (Lund & Lund 1984). Although Holopterygius and Allenypterus are unusual among coelacanths in having greatly elongated caudal regions, they are easily distinguished. While the deep body of Allenypterus is strongly arched dorsally and compara- tively straight ventrally, the postcranium of Holopterygius is shallower with more symmetrical dorsal and ventral margins. Small specimens of Allenypterus have a less exaggerated dorsal hump than larger individuals (Lund & Lund 1985; Field Museum, Chicago, PF10942, PF 10943a,b), but they retain greatly elongated neural spines above the abdominal region, unlike the short structures in Holopterygius . Both genera share asymmetrical lobes of the caudal fin, but the ventral lobe is more extensive in Holopterygius than in Allenypterus , where it is reduced to a minor series of shortened fin rays near the tip of the tail. Additional dissimilarities are present in the skulls. The premaxillae and mandibles of Allenypterus are edentulous (Lund & Lund 1985; Forey 1998) but bear well- developed teeth in Holopterygius . Additionally, lower jaw proportions of Holopterygius are unlike those of Allenypterus , but are similar to those of other early coelacanths (Lund & Lund 1985; Forey et al . 2000), suggesting that it had a more conventional skull shape than Allenypterus , in which the cranial region is drastically ...
Context 14
... probably precedes its first appearance (Harland et al . 1990). Therefore, the age of the fish beds is probably latest Givetian–earliest Frasnian ( ca 385 Ma; all dates in this article are from Gradstein et al . 2004). The skull roof of Holopterygius (figure 1 b , sr) is preserved primarily as an impression of its visceral surface, but intact areas are perforated by large, irregular pores for the supraorbital sensory canal. The premaxilla (figure 1 b , pmx) is squat and bears four large, irregularly shaped teeth. The dorsal surface of the splint-like parasphenoid (figure 1 b , psph) is exposed, and is marked by a well- developed hypophysial fossa. Much of the palate is visible (figure 1 b , pal), and it has the triangular shape characteristic of coelacanths (Forey 1998). The quadrate is preserved as a thickened region at the posteroventral corner of the palate, while a series of teeth along its ventral margin represent the remains of the ectopterygoid. A large, subspherical structure in the otic region is interpreted as an otolith (figure 1 b , ot; cf. Clack 1996). No dermal bones of the cheek can be identified. The opercle (figure 1 b , op) is a large rectangular bone with a long vertical axis, and resembles that of Allenypterus (Lund & Lund 1985; Forey 1998). The lower jaw of Holopterygius bears a long anterior ramus, a well-developed dorsal process at mid length, and another ramus posteriorly. The anterior arm of the lower jaw resembles the slender dentary of many early coelacanths (Lund & Lund 1985; Forey et al . 2000). Although the dentary of the intact jaw is preserved only as ...
Context 15
... probably precedes its first appearance (Harland et al . 1990). Therefore, the age of the fish beds is probably latest Givetian–earliest Frasnian ( ca 385 Ma; all dates in this article are from Gradstein et al . 2004). The skull roof of Holopterygius (figure 1 b , sr) is preserved primarily as an impression of its visceral surface, but intact areas are perforated by large, irregular pores for the supraorbital sensory canal. The premaxilla (figure 1 b , pmx) is squat and bears four large, irregularly shaped teeth. The dorsal surface of the splint-like parasphenoid (figure 1 b , psph) is exposed, and is marked by a well- developed hypophysial fossa. Much of the palate is visible (figure 1 b , pal), and it has the triangular shape characteristic of coelacanths (Forey 1998). The quadrate is preserved as a thickened region at the posteroventral corner of the palate, while a series of teeth along its ventral margin represent the remains of the ectopterygoid. A large, subspherical structure in the otic region is interpreted as an otolith (figure 1 b , ot; cf. Clack 1996). No dermal bones of the cheek can be identified. The opercle (figure 1 b , op) is a large rectangular bone with a long vertical axis, and resembles that of Allenypterus (Lund & Lund 1985; Forey 1998). The lower jaw of Holopterygius bears a long anterior ramus, a well-developed dorsal process at mid length, and another ramus posteriorly. The anterior arm of the lower jaw resembles the slender dentary of many early coelacanths (Lund & Lund 1985; Forey et al . 2000). Although the dentary of the intact jaw is preserved only as ...
Context 16
... probably precedes its first appearance (Harland et al . 1990). Therefore, the age of the fish beds is probably latest Givetian–earliest Frasnian ( ca 385 Ma; all dates in this article are from Gradstein et al . 2004). The skull roof of Holopterygius (figure 1 b , sr) is preserved primarily as an impression of its visceral surface, but intact areas are perforated by large, irregular pores for the supraorbital sensory canal. The premaxilla (figure 1 b , pmx) is squat and bears four large, irregularly shaped teeth. The dorsal surface of the splint-like parasphenoid (figure 1 b , psph) is exposed, and is marked by a well- developed hypophysial fossa. Much of the palate is visible (figure 1 b , pal), and it has the triangular shape characteristic of coelacanths (Forey 1998). The quadrate is preserved as a thickened region at the posteroventral corner of the palate, while a series of teeth along its ventral margin represent the remains of the ectopterygoid. A large, subspherical structure in the otic region is interpreted as an otolith (figure 1 b , ot; cf. Clack 1996). No dermal bones of the cheek can be identified. The opercle (figure 1 b , op) is a large rectangular bone with a long vertical axis, and resembles that of Allenypterus (Lund & Lund 1985; Forey 1998). The lower jaw of Holopterygius bears a long anterior ramus, a well-developed dorsal process at mid length, and another ramus posteriorly. The anterior arm of the lower jaw resembles the slender dentary of many early coelacanths (Lund & Lund 1985; Forey et al . 2000). Although the dentary of the intact jaw is preserved only as ...
Context 17
... probably precedes its first appearance (Harland et al . 1990). Therefore, the age of the fish beds is probably latest Givetian–earliest Frasnian ( ca 385 Ma; all dates in this article are from Gradstein et al . 2004). The skull roof of Holopterygius (figure 1 b , sr) is preserved primarily as an impression of its visceral surface, but intact areas are perforated by large, irregular pores for the supraorbital sensory canal. The premaxilla (figure 1 b , pmx) is squat and bears four large, irregularly shaped teeth. The dorsal surface of the splint-like parasphenoid (figure 1 b , psph) is exposed, and is marked by a well- developed hypophysial fossa. Much of the palate is visible (figure 1 b , pal), and it has the triangular shape characteristic of coelacanths (Forey 1998). The quadrate is preserved as a thickened region at the posteroventral corner of the palate, while a series of teeth along its ventral margin represent the remains of the ectopterygoid. A large, subspherical structure in the otic region is interpreted as an otolith (figure 1 b , ot; cf. Clack 1996). No dermal bones of the cheek can be identified. The opercle (figure 1 b , op) is a large rectangular bone with a long vertical axis, and resembles that of Allenypterus (Lund & Lund 1985; Forey 1998). The lower jaw of Holopterygius bears a long anterior ramus, a well-developed dorsal process at mid length, and another ramus posteriorly. The anterior arm of the lower jaw resembles the slender dentary of many early coelacanths (Lund & Lund 1985; Forey et al . 2000). Although the dentary of the intact jaw is preserved only as ...
Context 18
... probably precedes its first appearance (Harland et al . 1990). Therefore, the age of the fish beds is probably latest Givetian–earliest Frasnian ( ca 385 Ma; all dates in this article are from Gradstein et al . 2004). The skull roof of Holopterygius (figure 1 b , sr) is preserved primarily as an impression of its visceral surface, but intact areas are perforated by large, irregular pores for the supraorbital sensory canal. The premaxilla (figure 1 b , pmx) is squat and bears four large, irregularly shaped teeth. The dorsal surface of the splint-like parasphenoid (figure 1 b , psph) is exposed, and is marked by a well- developed hypophysial fossa. Much of the palate is visible (figure 1 b , pal), and it has the triangular shape characteristic of coelacanths (Forey 1998). The quadrate is preserved as a thickened region at the posteroventral corner of the palate, while a series of teeth along its ventral margin represent the remains of the ectopterygoid. A large, subspherical structure in the otic region is interpreted as an otolith (figure 1 b , ot; cf. Clack 1996). No dermal bones of the cheek can be identified. The opercle (figure 1 b , op) is a large rectangular bone with a long vertical axis, and resembles that of Allenypterus (Lund & Lund 1985; Forey 1998). The lower jaw of Holopterygius bears a long anterior ramus, a well-developed dorsal process at mid length, and another ramus posteriorly. The anterior arm of the lower jaw resembles the slender dentary of many early coelacanths (Lund & Lund 1985; Forey et al . 2000). Although the dentary of the intact jaw is preserved only as ...
Context 19
... probably precedes its first appearance (Harland et al . 1990). Therefore, the age of the fish beds is probably latest Givetian–earliest Frasnian ( ca 385 Ma; all dates in this article are from Gradstein et al . 2004). The skull roof of Holopterygius (figure 1 b , sr) is preserved primarily as an impression of its visceral surface, but intact areas are perforated by large, irregular pores for the supraorbital sensory canal. The premaxilla (figure 1 b , pmx) is squat and bears four large, irregularly shaped teeth. The dorsal surface of the splint-like parasphenoid (figure 1 b , psph) is exposed, and is marked by a well- developed hypophysial fossa. Much of the palate is visible (figure 1 b , pal), and it has the triangular shape characteristic of coelacanths (Forey 1998). The quadrate is preserved as a thickened region at the posteroventral corner of the palate, while a series of teeth along its ventral margin represent the remains of the ectopterygoid. A large, subspherical structure in the otic region is interpreted as an otolith (figure 1 b , ot; cf. Clack 1996). No dermal bones of the cheek can be identified. The opercle (figure 1 b , op) is a large rectangular bone with a long vertical axis, and resembles that of Allenypterus (Lund & Lund 1985; Forey 1998). The lower jaw of Holopterygius bears a long anterior ramus, a well-developed dorsal process at mid length, and another ramus posteriorly. The anterior arm of the lower jaw resembles the slender dentary of many early coelacanths (Lund & Lund 1985; Forey et al . 2000). Although the dentary of the intact jaw is preserved only as ...

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... The fin rays also reveal several evolutionary trends within coelacanth history. Early coelacanths have a more than one-to-one relationship between fin rays and radials in the caudal fin (e.g., Miguashaia, Serenichthys, Diplocercides, Holopterygius, Allenypterus, Lochmocercus) [8,9,13,62,63] and some show distal bifurcation of the lepidotrichia (e.g., Miguashaia, Gavinia, Diplocercides) [13,14,61]. All Mesozoic coelacanths display the derived condition of unbranched fin rays with a one-to-one relationship between the radials and lepidotrichia (the previously described condition of Rieppelia [7] may be incorrect as pairs of hemirays may have been identified as separated lepidotrichia). ...
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Although the split of coelacanths from other sarcopterygians is ancient, around 420 million years ago, the taxic diversity and the morphological disparity of the clade have remained relatively low, with a few exceptions. This supposedly slow evolutionary pace has earned the extant coelacanth Latimeria the nickname “living fossil”. This status generated much interest in both extinct and extant coelacanths leading to the production of numerous anatomical studies. However, detailed descriptions of extinct taxa are made difficult due to the quality of the fossil material which generally prevents fine comparisons with the extant Latimeria. Here we describe a new genus and species of coelacanth, Graulia branchiodonta gen. et sp. nov. from the Middle Triassic of Eastern France, based on microtomographical imaging using synchrotron radiation. Through exquisite 3D preservation of the specimens, we reconstructed the skeletal anatomy of this new species at an unprecedented level of detail for an extinct coelacanth, and barely achieved for the extant Latimeria. In particular, we identified a well-developed trilobed ossified lung whose function is still uncertain. The skeletal anatomy of G. branchiodonta displays the general Bauplan of Mesozoic coelacanths and a phylogenetic analysis resolved it as a basal Mawsoniidae, shedding light on the early diversification of one of the two major lineages of Mesozoic coelacanths. However, despite its exquisite preservation, G. branchiodonta carries a weak phylogenetic signal, highlighting that the sudden radiation of coelacanths in the Early and Middle Triassic makes it currently difficult to detect synapomorphies and resolve phylogenetic interrelationships among coelacanths in the aftermath of the great Permo-Triassic biodiversity crisis.
... One primary critique is the lack of an explanation for the coupling of low rates of lineage diversification and phenotypic change in clades thought to exhibit stasis. Indeed, our analyses confirm that classic living fossil lineages, such as coelacanths and rhynchocephalians, have rates of molecular evolution similar to most other vertebrate clades (Chalopin et al. 2014;Gemmell et al. 2020) (Fig. 3a, Fig. S2), matching their higher ancient phenotypic disparity (Friedman and Coates 2006;Herrera-Flores et al. 2017) and contrasting with previous estimates of genomic evolutionary rates in these clades based on fewer sampled species and loci. ...
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Evolutionary stasis characterizes lineages that seldom speciate and show little phenotypic change over long stretches of geological time. Although lineages that appear to exhibit evolutionary stasis are often called living fossils, no single mechanism is thought responsible for their slow rates of morphological evolution and low species diversity. Some analyses of molecular evolutionary rates in a handful of living fossil lineages have indicated they exhibit slow rates of genomic change. Here, we investigate mechanisms of evolutionary stasis using a dataset of 1,105 exons for 481 vertebrate species. We demonstrate that two ancient clades of ray-finned fishes classically called living fossils, gars and sturgeons, exhibit the lowest rates of molecular substitution in protein coding genes among all jawed vertebrates. Comparably low rates of evolution are observed at four-fold degenerate sites in gars and sturgeons, implying a mechanism of stasis decoupled from selection that we speculate is linked to a highly effective DNA repair apparatus. We show that two gar species last sharing common ancestry over 100 million years ago naturally produce morphologically intermediate and fertile hybrids. This makes gars the oldest naturally hybridizing divergence among eukaryotes and supports a theoretical prediction that slow rates of nucleotide substitution across the genome slows the accumulation of genetic incompatibilities, enabling hybridization across deeply divergent lineages and perhaps slowing the rate of speciation. Our results help establish molecular stasis as a barrier to speciation and phenotypic innovation and provide a mechanism to explain the low species diversity in living fossil lineages.
... One primary critique is the lack of an explanation for the coupling of low rates of lineage diversification and phenotypic change in clades thought to exhibit stasis. Indeed, our analyses confirm that classic living fossil lineages, such as coelacanths and rhynchocephalians, have rates of molecular evolution similar to most other vertebrate clades (Chalopin et al., 2014;Gemmell et al., 2020) (Figure 3A, Supplementary Figure S2), matching their higher ancient phenotypic disparity (Friedman & Coates, 2006;Herrera-Flores et al., 2017) and contrasting with previous estimates of genomic evolutionary rates in these clades based on fewer sampled species and loci. ...
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... Although their extant and extinct species diversity is extremely low (e.g., Schaeffer, 1952;Casane and Laurenti, 2013;Cavin and Guinot, 2014;Cavin et al., 2021;Toriño et al., 2021), coelacanths show an appreciable degree of morphological and body size evolution across their more than 400-million-year evolutionary history (Friedman, 2007;Toriño et al., 2021). This high degree of phenotypic innovation produced some of the largest freshwater fishes (e.g., Cavin et al., 2021), anguilliform (Friedman and Coates, 2005), hump-backed (Cavin et al., 2017), and fork-tailed (Wendruff and Wilson, 2012) forms, as well as deepwater species like the extant genus Latimeria. ...
... 22:90 Coelacanths (Actinistia) are one of the most famous species-depauperate lineages. This clade diverged from other jawed vertebrates during the Silurian [3,29,30,43] and represents the living sister clade to all other sarcopterygians, or lobe-finned fishes [3,8,55]. Despite their historical notoriety as a species-poor, morphologically conservative lineage, the fossil record of coelacanths has shown that this clade diversified into a wide variety of morphologies in the ancient past [17,29,49]. ...
... This clade diverged from other jawed vertebrates during the Silurian [3,29,30,43] and represents the living sister clade to all other sarcopterygians, or lobe-finned fishes [3,8,55]. Despite their historical notoriety as a species-poor, morphologically conservative lineage, the fossil record of coelacanths has shown that this clade diversified into a wide variety of morphologies in the ancient past [17,29,49]. Fossil coelacanths show bursts of species diversity during the Devonian and Triassic [83] and achieved a high degree of body size variation ranging from diminutive species less than 5 cm long to 6 + m giants representing some of the largest freshwater fishes [18]. ...
... We also sampled an additional five specimens from the Old Granton Quarry in Bergen, New Jersey and examined a skull and partial skeleton of a large coelacanth collected in 1975 from the Solite Quarry site in North Carolina. Measurements made on this dataset using digital calipers were combined with measurement data from [29,70,72,76]. Together, this dataset represents the largest known collection of coelacanth material from a single region and time (Carnian-Norian, e.g., [45]). ...
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... Only the question of evolutionary rate is addressed here, not the question of ancestral status or other "living fossil" characteristics attributed to coelacanths. The low rate of evolution based on a lasting generalist morphological Bauplan has been confirmed by most subsequent authors who have worked on the group (Schaeffer, 1952;Cloutier, 1991;Forey, 1998;Schultze, 2004;Zhu et al., 2012;Cavin and Guinot, 2014), knowing that there are also exceptions to this general Bauplan (e.g., Friedman and Coates, 2006;Wendruff and Wilson, 2012;Cavin et al., 2017). However, part of the community of researchers working on fossil and living coelacanths avoids using this expression. ...
... Rapid trophic divergence in the lungfish lineage. The major lineages of crown sarcopterygians first appear in the Early Devonian fossil records, leading to inferences of rapid evolutionary change in the early history of several groups [66][67][68] , including lungfishes 69 . Our quantitative analyses reinforce this hypothesis. ...
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... Molecular data have also revealed the existence of a putative third coelacanth species in Indonesia (Kadarusman et al., 2020). However, the supposed morphological stasis of coelacanths has been challenged by new fossil discoveries (Casane & Laurenti, 2013) that highlighted important differences in the skull, axial skeleton and internal organs throughout their evolutionary history (Brito et al., 2010;Cavin et al., 2017;Cupello et al., 2017;Forey, 1998;Friedman & Coates, 2006;Lund & Lund, 1984Wendruff & Wilson, 2012). ...
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Coelacanths have traditionally been described as morphologically conservative throughout their long evolutionary history, which spans more than 400 million years. After an initial burst during the Devonian, a morphological stasis was long thought to have prevailed since the Carboniferous, as shown by the extant Latimeria. New fossil discoveries have challenged this view, with punctual and sometimes unusual departures from the general coelacanth Bauplan. The dermal skeleton is considered to represent one, if not the main, example of morphological stasis in coelacanth evolution and as a consequence, has remained poorly surveyed. The lack of palaeo-histological data on the dermoskeleton has resulted in a poor understanding of the early establishment and evolution of the coelacanth squamation. Here we describe the scales of Miguashaia bureaui from the Upper Devonian of Miguasha, Québec (Canada), revealing histological data for a Palaeozoic coelacanth in great detail and adding to our knowledge on the dermal skeleton of sarcopterygians. Miguashaia displays rounded scales ornamented by tubercules and narrow ridges made of dentine and capped with enamel. At least two generations of superimposed odontodes occur, which is reminiscent of the primitive condition of stem osteichthyans like Andreolepis or Lophosteus, and onychodonts like Selenodus. The middle vascular layer is well developed and shows traces of osteonal remodelling. The basal plate consists of a fully mineralised lamellar bone with a repetitive rotation pattern every five layers indicating a twisted plywood-like arrangement of the collagen plies. Comparisons with the extant Latimeria and other extinct taxa show that these features are consistently conserved across coelacanth evolution with only minute changes in certain taxa. The morphological and histological features displayed in the scales of Miguashaia enable us to draw a comprehensive picture of the onset of the coelacanth squamation and to propose and discuss evolutionary scenarios for the coelacanth dermoskeleton. K E Y W O R D S coelacanth, dermoskeleton, histology, odontodes, Palaeozoic, scales
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... Only Forey (1998), Friedman andCoates (2006), Yabumoto (2008) and Zhu et al. (2012) perform complementary analyses bringing differential weights to the characters, using a posterior weighting according to the rescaled consistency index (successive weighting, Farris 1969). Forey (op. ...
... Character 7 corrected according to Friedman & Coates (2006). Character 31 corrected according to Clément (2005) and Forey in Friedman and Coates (2006). It must be noted that Gess & Coates (2015) propose an alternative scoring combining Porolepis and Glyptolepis (only modifying the scoring of character 7). ...
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