GEOL 331 Invertebrate Paleontology

Fall Semester 2004
Vertebrate Paleontology

Synapomorphies of Craniata:

In terms of metabolic rate and aerobic capacity, only cephalopod mollusks and some arthropods are comparable to craniates.

Living jawless craniates include Myxinoidea (aka Hyperotreti, aka hagfish) and Petromyzontida (aka Hyperoartei, aka lampreys). Together were once called Cyclostomata or Agnatha, but are almost certainly paraphyletic.

Myxinoidea seem to be basal to all other craniates, living or fossil. Myxinoids have tentacles, and (at least the living ones) have large ventrolateral slime glands, esophago-cutaneous duct on the left side, and elongate body shape. Primitive condition is several pairs of small gill openings. Primitive features relative to vertebrates:

Only fossil record of hagfish is from Mazon Creek, but some possible Chenjiang forms, including Haikouella (actual specimens here) and Myllokunmingia may represent other types of basal non-vertebrate craniates.

Vertebrata, characterized by:

Only living jawless vertebrates are petromyzontids. They are characterized by a large sucker surrounding the mouth, strengthened by annular cartilage and by pine-shaped processes on gill arches. Also, they unique among extant vertebrates in having a median dorsal "nostril" (the nasohypophysial opening), but some other fossil vertebrates also display the same structure. All fossil lampreys are Mazon Creek forms.

Another possible basal vertebrate is Haikouichtys (Chengjiang Fm.).

A problematic group of basal craniates, probably basal vertebrates: Euconodonta

Presence of a phosphatic hard parts suggests that they are closer to the "ostracoderms" and gnathostomes than are petromyzontids; however, some dispute claim that conodont elements are true bone, dentine, and enamel

"Ostracoderms": paraphyletic grade of armored jawless vertebrates. "Ostracoderms" share with gnathostomes:

An Upper Cambrian form (Anatolepis) is known from bony plates, but the morphology of the whole animal is not known.

Many clades of "ostracoderms" (see here, and websites linked therein, for an extensive overview). "Ostracoderm"-grade vertebrates common in Ordovician through Late Devonian strata.

Some major groups and trends of "ostracoderms"

However, as long as jawless, gills had to serve "double duty": as organs of feeding and of respiration.

One unusual "ostracoderm" group, the Thelodonti (?Late Ordovician-Late Devonian), had scales with hollow pulp cavity, which resemble the dermal scales of sharks and the teeth of gnathostomes. Some of these scales even wrap into the mouth of thelodonts. Proto-teeth? Perhaps, but general anatomy doesn't suggest that they were particularly close to the origin of gnathostomes.

Origin of the head
What do all of these taxa have in common that the outgroup (Cephalochordata) lacks? Heads! What phenomena are implicated in the sudden appearance of this complex structure?

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