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Regarding the morphological differences between ceolacanth of the devonian and species today:
https://onlinelibrary.wiley.com/doi/abs/10.1111/j.1525-142X.2007.00169.x
A new fossil from the Middle–Late Devonian of Wyoming preserves the first and only example of a primitive coelacanth pectoral fin endoskeleton. The strongly asymmetrical skeleton of this fin corroborates the hypothesis that this is the primitive sarcopterygian pattern, and that this pattern persisted in the closest fish‐like relatives of land vertebrates. The new material reveals the specializations of paired fins in the modern coelacanth, as well as in living lungfishes. Consequently, the context in which these might be used to investigate evolutionary and developmental relationships between vertebrate fins and limbs is changed. Our data suggest that primitive actinopterygians, rather than living sarcopterygian fishes and their derived appendages, are the most informative comparators for developmental studies seeking to understand the origin of tetrapod limbs.
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1560029/
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 cladistic analysis places Holopterygius as the sister taxon of the Carboniferous (Serpukhovian) genus Allenypterus. Despite the specialized morphology of these genera, they occupy a surprisingly basal position in coelacanth phylogeny; only Diplocercides and Miguashaia are further removed from the crown. A morphometric analysis reveals that coelacanths were anatomically disparate early in their history. Conflicts between this result and those of previous studies challenge the adequacy of systematic character sets for describing historical patterns of morphological variety. Coelacanths have long had an iconic place in the study of vertebrate evolution for their apparent anatomical conservatism over geological time, but Holopterygius provides clear evidence for rapid morphological evolution early in the history of this clade.
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) deposits (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 categories: 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 2a).
The postcranial morphologies of Allenypterus and Holopterygius—and presumably their ecologies—differ radically from those of ‘typical’ coelacanths, but this is not reflected in previous measures of disparity.
More remarkable than the degree of morphological separation between Holopterygius, Miguashaia and other early coelacanths is the short interval over which this variety was generated. With a probable origin of actinistians during the Early Devonian or Late Silurian, each of these distinctive morphologies was established by the close of the Middle Devonian. In contrast, post-Carboniferous forms show no evidence of the radical morphological shifts that characterize the initial phases of the coelacanth radiation, despite higher levels of taxonomic diversity (Forey 1998) and a longer interval over which to develop anatomical novelties. The most extreme departure during this later interval is the Jurassic Libys, which, although deep-bodied, conforms to the stereotypical coelacanth body plan. Such rapid accumulation of morphological variety early in clade histories is a recurrent theme in studies of disparity in the fossil record (Foote 1997), but the causes underlying this pattern remain uncertain (Foote 1996). What is clear, however, is that Holopterygius and its disparate contemporaries provide evidence for early anatomical experimentation in coelacanths that is strongly at odds with the textbook portrayal of the clade as morphologically invariant over geological time.
-------------------------------------
https://www.tandfonline.com/doi/abs/10.1080/02724634.2012.657317
An unusual fork-tailed coelacanth from the Lower Triassic Sulphur Mountain Formation of British Columbia, Canada, marks the first considerable departure in actinistian body form since the Mississippian Period. Rebellatrix divaricerca, gen. et sp. nov., is unique among coelacanths in its possession of a bifurcated caudal fin, reduced segmentation of fin rays, and fusion of caudal fin elements. Parsimony analysis of a character-taxon matrix of 109 characters and 29 taxa recovered R. divaricerca as sister taxon to Latimerioidei. The family Rebellatricidae is erected to include only R. divaricerca. This novel body shape of the new coelacanth raises questions about the idea that coelacanths were morphologically static following the Mississippian. Rebellatrix divaricerca also emphasizes the morphological diversity of coelacanths during the Early Triassic, a time when species diversity of coelacanths was also highest. The slender, fork-tailed body form suggests fast swimming and an active lifestyle, unique among known fossil and extant coelacanths.
https://onlinelibrary.wiley.com/doi/abs/10.1002/bies.201200145
Here, we have examined the available molecular and morphological data and show that: (i) low intra‐specific molecular diversity does not imply low mutation rate, (ii) studies not showing low substitution rates in coelacanth are often neglected, (iii) the morphological stability of coelacanths is not supported by paleontological evidence.
---------------------------------------------------------------
Ok, so above are 4 research papers, that actually discuss morphological differences between ceolacanths of the devonian, the carboniferous, extant species and more.
So now that we have cleared up the nonsense about ceolacanth being morphologically the same in the devonian versus those of today, can we go back on subject regarding the predictions involved in determining the locality of tiktaalik? @inquiring mind and @Justatruthseeker
https://onlinelibrary.wiley.com/doi/abs/10.1111/j.1525-142X.2007.00169.x
A new fossil from the Middle–Late Devonian of Wyoming preserves the first and only example of a primitive coelacanth pectoral fin endoskeleton. The strongly asymmetrical skeleton of this fin corroborates the hypothesis that this is the primitive sarcopterygian pattern, and that this pattern persisted in the closest fish‐like relatives of land vertebrates. The new material reveals the specializations of paired fins in the modern coelacanth, as well as in living lungfishes. Consequently, the context in which these might be used to investigate evolutionary and developmental relationships between vertebrate fins and limbs is changed. Our data suggest that primitive actinopterygians, rather than living sarcopterygian fishes and their derived appendages, are the most informative comparators for developmental studies seeking to understand the origin of tetrapod limbs.
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1560029/
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 cladistic analysis places Holopterygius as the sister taxon of the Carboniferous (Serpukhovian) genus Allenypterus. Despite the specialized morphology of these genera, they occupy a surprisingly basal position in coelacanth phylogeny; only Diplocercides and Miguashaia are further removed from the crown. A morphometric analysis reveals that coelacanths were anatomically disparate early in their history. Conflicts between this result and those of previous studies challenge the adequacy of systematic character sets for describing historical patterns of morphological variety. Coelacanths have long had an iconic place in the study of vertebrate evolution for their apparent anatomical conservatism over geological time, but Holopterygius provides clear evidence for rapid morphological evolution early in the history of this clade.
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) deposits (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 categories: 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 2a).
The postcranial morphologies of Allenypterus and Holopterygius—and presumably their ecologies—differ radically from those of ‘typical’ coelacanths, but this is not reflected in previous measures of disparity.
More remarkable than the degree of morphological separation between Holopterygius, Miguashaia and other early coelacanths is the short interval over which this variety was generated. With a probable origin of actinistians during the Early Devonian or Late Silurian, each of these distinctive morphologies was established by the close of the Middle Devonian. In contrast, post-Carboniferous forms show no evidence of the radical morphological shifts that characterize the initial phases of the coelacanth radiation, despite higher levels of taxonomic diversity (Forey 1998) and a longer interval over which to develop anatomical novelties. The most extreme departure during this later interval is the Jurassic Libys, which, although deep-bodied, conforms to the stereotypical coelacanth body plan. Such rapid accumulation of morphological variety early in clade histories is a recurrent theme in studies of disparity in the fossil record (Foote 1997), but the causes underlying this pattern remain uncertain (Foote 1996). What is clear, however, is that Holopterygius and its disparate contemporaries provide evidence for early anatomical experimentation in coelacanths that is strongly at odds with the textbook portrayal of the clade as morphologically invariant over geological time.
-------------------------------------
https://www.tandfonline.com/doi/abs/10.1080/02724634.2012.657317
An unusual fork-tailed coelacanth from the Lower Triassic Sulphur Mountain Formation of British Columbia, Canada, marks the first considerable departure in actinistian body form since the Mississippian Period. Rebellatrix divaricerca, gen. et sp. nov., is unique among coelacanths in its possession of a bifurcated caudal fin, reduced segmentation of fin rays, and fusion of caudal fin elements. Parsimony analysis of a character-taxon matrix of 109 characters and 29 taxa recovered R. divaricerca as sister taxon to Latimerioidei. The family Rebellatricidae is erected to include only R. divaricerca. This novel body shape of the new coelacanth raises questions about the idea that coelacanths were morphologically static following the Mississippian. Rebellatrix divaricerca also emphasizes the morphological diversity of coelacanths during the Early Triassic, a time when species diversity of coelacanths was also highest. The slender, fork-tailed body form suggests fast swimming and an active lifestyle, unique among known fossil and extant coelacanths.
https://onlinelibrary.wiley.com/doi/abs/10.1002/bies.201200145
Here, we have examined the available molecular and morphological data and show that: (i) low intra‐specific molecular diversity does not imply low mutation rate, (ii) studies not showing low substitution rates in coelacanth are often neglected, (iii) the morphological stability of coelacanths is not supported by paleontological evidence.
---------------------------------------------------------------
Ok, so above are 4 research papers, that actually discuss morphological differences between ceolacanths of the devonian, the carboniferous, extant species and more.
So now that we have cleared up the nonsense about ceolacanth being morphologically the same in the devonian versus those of today, can we go back on subject regarding the predictions involved in determining the locality of tiktaalik? @inquiring mind and @Justatruthseeker
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