Caecilians are odd critters. While they are amphibians they don't much resemble others in that group being worm-like (no limbs) and possessing teeth and live a life burrowing through soil using tentacles around their eyes to sense things. We don't know a whole lot about them including how they evolved or how they are related to other amphibians.
We may now finally be getting some answers thanks to the first unmistakable caecilian fossil dating back to the Triassic being discovered on what is called "Thunder Ridge" in Arizona's Petrified Forest National Park.
Previously, only 10 fossil caecilian occurrences have been discovered by scientists, and they only date back to roughly 183 mya to the Early Jurassic whereas DNA analysis estimates that they likely originated sometime back during the Carboniferous or Permian (approximately 370 million to 270 mya). That makes for at least a 87 million year gap from which no fossils had been found. The new discovery extends their fossil record back by some 35 million years thereby narrowing that gap substantially.
The material discovered included a number of postcranial fragments and several jaws. It was the jaws, some of which were barely a quarter of an inch (6.3mm) long, with their distinctive double row of teeth, that allowed the researchers to identify the remains as having come from an early caecilian. The remains from at least 70 individuals have been uncovered since the initial discovery in 2019.
The group named the creature Funcusvermis gilmorei. The genus name translates to "funky worm" and was inspired by a song by the Ohio Players called "Funky Worm," which was apparently a favorite excavation tune of the researchers.
Analysis reveals that Funcusvermis demonstrates a strong link between caecilians and other lissamphibians (frogs and salamanders) in that it shares a number of skeletal features with early members of this subclass, as well as extinct dissorophoid temnospondyls such as Gerobatrachus. which lived during the Early Permian.
As co-author Ben Kligman of the Department of Resource Management and Science, Petrified Forest National Park, Petrified Forest and Department of Geosciences, Virginia Tech, observed, "Unlike living caecilians, Funcusvermis lacks many adaptations associated with burrowing underground, indicating a slower acquisition of features associated with an underground lifestyle in the early stages of caecilian evolution."
The team also said that the discovery supports the consensus hypothesis regarding lissamphibian evolution, with Lissamphibia as a monophyletic group with a single common ancestor among the dissorophoids.
The paper, Triassic stem caecilian supports dissorophoid origin of living amphibians can be read in its entirety by clicking the hyperlink, although the abstract is made available below
5ce7dc2b-7cf4-42c8-a6a5-73c7c66ed43c.jpg
a–c, Composite reconstruction of craniomandibular elements in lateral (a), medial (b) and dorsal (c) views. d,e, Holotype right
pseudodentary (PEFO 43891) in medial and ventral views. f, Paratype right pseudodentary (PEFO 46284) in medial view.
g–i, Referred left maxillopalatine (PEFO 46481) in medial (g), ventral (h) and dorsal (i) views. j,k, Referred left pseudoangular
(PEFO 46480) in medial and lateral views. l–o, Paratype right pseudodentary (PEFO 45800) in medial (l; expanded view in m)
and dorsal (n; expanded view in o) views. abcnV, alveolar branch cranial nerve V; adtr, adsymphyseal tooth row; af, adductor fossa;
att, attachment tissue; bp, basal pore; cnV, cranial nerve V insertions; cp, coronoid process; dpaf, dorsal pseudoangular facet;
dpdf, dorsal pseudodentary facet; dtr, dentary tooth row; dz, dividing zone; ebcnV, external branch cranial nerve V; fr, facial ramus;
hp, hamate process; imf, intramandibular foramen; jas, jaw articulation surface; lcm, lateral choanal margin; lecnV, lateral exit
cranial nerve V; mtr, maxillary tooth row; om, orbital margin; pap, posterior pseudoangular process; pc, pulp cavity; pd, pedicel;
pgp, preglenoid process; ptr, palatal tooth row; rtl, replacement tooth locus; sf, symphyseal foramen; sp, symphyseal prongs;
vpaf, ventral pseudoangular facet; vpdf, ventral pseudodentary facet. Arrows indicate anterior direction.
84b34f0f-cca8-4460-a7c2-5da18427d665.jpg
Squares denote important apomorphies (including non-mandibular features); apomorphies are optimized computationally unless followed
by an asterisk, which denotes an apomorphy suggested by our results but lacking sufficient sampling to optimize computationally. Topology
is derived from parsimony results (Extended Data Fig. 5); Yaksha peretti, Salamandra and Rana approximate conditions are found in taxa sampled
in the analysis. Illustrations represent right mandibles in medial (bottom) and dorsal (top) views for Doleserpeton annectens9, Eocaecilia micropodia12
(Illustration adapted from ref. 12, with the permission of Museum of Comparative Zoology, Harvard University), Epicrionops petersi12,
Funcusvermis gilmorei, Rana, Salamandra and Y. peretti28, excepting Greererpeton burkemorani35 (dorsal only) and Cacops aspidephorus37
(medial only). All scale bars are 2 mm except for G. burkemorani (2 cm) and C. aspidephorus (2 cm). Brackets on the branches
indicate stem groups, whereas circles indicate node groups. Crosses indicate extinct taxa.
We may now finally be getting some answers thanks to the first unmistakable caecilian fossil dating back to the Triassic being discovered on what is called "Thunder Ridge" in Arizona's Petrified Forest National Park.
Previously, only 10 fossil caecilian occurrences have been discovered by scientists, and they only date back to roughly 183 mya to the Early Jurassic whereas DNA analysis estimates that they likely originated sometime back during the Carboniferous or Permian (approximately 370 million to 270 mya). That makes for at least a 87 million year gap from which no fossils had been found. The new discovery extends their fossil record back by some 35 million years thereby narrowing that gap substantially.
The material discovered included a number of postcranial fragments and several jaws. It was the jaws, some of which were barely a quarter of an inch (6.3mm) long, with their distinctive double row of teeth, that allowed the researchers to identify the remains as having come from an early caecilian. The remains from at least 70 individuals have been uncovered since the initial discovery in 2019.
The group named the creature Funcusvermis gilmorei. The genus name translates to "funky worm" and was inspired by a song by the Ohio Players called "Funky Worm," which was apparently a favorite excavation tune of the researchers.
Analysis reveals that Funcusvermis demonstrates a strong link between caecilians and other lissamphibians (frogs and salamanders) in that it shares a number of skeletal features with early members of this subclass, as well as extinct dissorophoid temnospondyls such as Gerobatrachus. which lived during the Early Permian.
As co-author Ben Kligman of the Department of Resource Management and Science, Petrified Forest National Park, Petrified Forest and Department of Geosciences, Virginia Tech, observed, "Unlike living caecilians, Funcusvermis lacks many adaptations associated with burrowing underground, indicating a slower acquisition of features associated with an underground lifestyle in the early stages of caecilian evolution."
The team also said that the discovery supports the consensus hypothesis regarding lissamphibian evolution, with Lissamphibia as a monophyletic group with a single common ancestor among the dissorophoids.
The paper, Triassic stem caecilian supports dissorophoid origin of living amphibians can be read in its entirety by clicking the hyperlink, although the abstract is made available below
Abstract
Living amphibians (Lissamphibia) include frogs and salamanders (Batrachia) and the limbless worm-like caecilians (Gymnophiona). The estimated Palaeozoic era gymnophionan–batrachian molecular divergence1 suggests a major gap in the record of crown lissamphibians prior to their earliest fossil occurrences in the Triassic period2,3,4,5,6. Recent studies find a monophyletic Batrachia within dissorophoid temnospondyls7,8,9,10, but the absence of pre-Jurassic period caecilian fossils11,12 has made their relationships to batrachians and affinities to Palaeozoic tetrapods controversial1,8,13,14. Here we report the geologically oldest stem caecilian—a crown lissamphibian from the Late Triassic epoch of Arizona, USA—extending the caecilian record by around 35 million years. These fossils illuminate the tempo and mode of early caecilian morphological and functional evolution, demonstrating a delayed acquisition of musculoskeletal features associated with fossoriality in living caecilians, including the dual jaw closure mechanism15,16, reduced orbits17 and the tentacular organ18. The provenance of these fossils suggests a Pangaean equatorial origin for caecilians, implying that living caecilian biogeography reflects conserved aspects of caecilian function and physiology19, in combination with vicariance patterns driven by plate tectonics20. These fossils reveal a combination of features that is unique to caecilians alongside features that are shared with batrachian and dissorophoid temnospondyls, providing new and compelling evidence supporting a single origin of living amphibians within dissorophoid temnospondyls.
Living amphibians (Lissamphibia) include frogs and salamanders (Batrachia) and the limbless worm-like caecilians (Gymnophiona). The estimated Palaeozoic era gymnophionan–batrachian molecular divergence1 suggests a major gap in the record of crown lissamphibians prior to their earliest fossil occurrences in the Triassic period2,3,4,5,6. Recent studies find a monophyletic Batrachia within dissorophoid temnospondyls7,8,9,10, but the absence of pre-Jurassic period caecilian fossils11,12 has made their relationships to batrachians and affinities to Palaeozoic tetrapods controversial1,8,13,14. Here we report the geologically oldest stem caecilian—a crown lissamphibian from the Late Triassic epoch of Arizona, USA—extending the caecilian record by around 35 million years. These fossils illuminate the tempo and mode of early caecilian morphological and functional evolution, demonstrating a delayed acquisition of musculoskeletal features associated with fossoriality in living caecilians, including the dual jaw closure mechanism15,16, reduced orbits17 and the tentacular organ18. The provenance of these fossils suggests a Pangaean equatorial origin for caecilians, implying that living caecilian biogeography reflects conserved aspects of caecilian function and physiology19, in combination with vicariance patterns driven by plate tectonics20. These fossils reveal a combination of features that is unique to caecilians alongside features that are shared with batrachian and dissorophoid temnospondyls, providing new and compelling evidence supporting a single origin of living amphibians within dissorophoid temnospondyls.
5ce7dc2b-7cf4-42c8-a6a5-73c7c66ed43c.jpg
a–c, Composite reconstruction of craniomandibular elements in lateral (a), medial (b) and dorsal (c) views. d,e, Holotype right
pseudodentary (PEFO 43891) in medial and ventral views. f, Paratype right pseudodentary (PEFO 46284) in medial view.
g–i, Referred left maxillopalatine (PEFO 46481) in medial (g), ventral (h) and dorsal (i) views. j,k, Referred left pseudoangular
(PEFO 46480) in medial and lateral views. l–o, Paratype right pseudodentary (PEFO 45800) in medial (l; expanded view in m)
and dorsal (n; expanded view in o) views. abcnV, alveolar branch cranial nerve V; adtr, adsymphyseal tooth row; af, adductor fossa;
att, attachment tissue; bp, basal pore; cnV, cranial nerve V insertions; cp, coronoid process; dpaf, dorsal pseudoangular facet;
dpdf, dorsal pseudodentary facet; dtr, dentary tooth row; dz, dividing zone; ebcnV, external branch cranial nerve V; fr, facial ramus;
hp, hamate process; imf, intramandibular foramen; jas, jaw articulation surface; lcm, lateral choanal margin; lecnV, lateral exit
cranial nerve V; mtr, maxillary tooth row; om, orbital margin; pap, posterior pseudoangular process; pc, pulp cavity; pd, pedicel;
pgp, preglenoid process; ptr, palatal tooth row; rtl, replacement tooth locus; sf, symphyseal foramen; sp, symphyseal prongs;
vpaf, ventral pseudoangular facet; vpdf, ventral pseudodentary facet. Arrows indicate anterior direction.
84b34f0f-cca8-4460-a7c2-5da18427d665.jpg
Squares denote important apomorphies (including non-mandibular features); apomorphies are optimized computationally unless followed
by an asterisk, which denotes an apomorphy suggested by our results but lacking sufficient sampling to optimize computationally. Topology
is derived from parsimony results (Extended Data Fig. 5); Yaksha peretti, Salamandra and Rana approximate conditions are found in taxa sampled
in the analysis. Illustrations represent right mandibles in medial (bottom) and dorsal (top) views for Doleserpeton annectens9, Eocaecilia micropodia12
(Illustration adapted from ref. 12, with the permission of Museum of Comparative Zoology, Harvard University), Epicrionops petersi12,
Funcusvermis gilmorei, Rana, Salamandra and Y. peretti28, excepting Greererpeton burkemorani35 (dorsal only) and Cacops aspidephorus37
(medial only). All scale bars are 2 mm except for G. burkemorani (2 cm) and C. aspidephorus (2 cm). Brackets on the branches
indicate stem groups, whereas circles indicate node groups. Crosses indicate extinct taxa.
Comment