HONR219d
Lecture 11
3-6-2008

The origin of jaws and Gnathostome diversity

Gnathostomata: The jawed vertebrates. Quantum leap forward.

Jaw anatomy: Up until now, when we have spoken of a "skull" we have meant only a plating of dermal bone around the head, or, in the case of Galeaspids and Osteostraci, that plus in endochondrally ossified neurocranium or braincase. With the appearance of the gnathostome jaws and branchial skeleton, the skull becomes a complex composite structure. The following illustrations show its components using the fossil bony fish Eusthenopteron as an example.

Origin of jaws: Many gnathostome synapomorphies are continuations of longstanding vertebrate trends toward increased skeletal ossification, brain enlargement, and improvement of swimming. Big exceptions are changes to the pharynx, especially jaws. We have:
Oddly, fossil intermediaries between jawed and jawless vertebrates just don't seem to exist in the fossil record. What's up?

Four general hypotheses for this radical transformation:

Gnathostome diversity: Three major groups of unknown relationships: Placodermi, Chondrichthyes, Osteichthyes.

Placodermi: Silurian to Devonian armored gnathostomes experienced a rapid worldwide diversification and sudden decline.


Coccosteus from Wikipedia (sorry)

Placoderms were very diverse and occupied a wide range of ecological roles. Their specializations included: Fossil record: Fragmentary records of placoderms appear in the Middle Silurian. this is followed by a rapid diversification. During the Devonian, placoderms were the dominant vertebrate group. Both marine and fresh water forms are recorded with a worldwide distribution except for puzzling absence in South American sediments. Placoderm diversity was greatly reduced by an extinction event in the Late Devonian. They were completely extinguished by the mass extinction event at the end of the Devonian. Thus, entire radiation took up only about 50 million years, but while it lasted, it was spectacular.

What placoderms lacked:


From University of Southern Maine - Biology

The myomeres of living gnathostomes differ from those of lampreys and hagfish in that there myomeres are divided into upper and lower halves by a horizontal septum of connective tissue. Lampreys' are not. Recent work on placoderm fossils with soft tissue preservation show that the placoderms, like lampreys, lacked the horizontal septum. This feature, therefore, is a synapomorphy of the two remaining gnathostome groups: Chondrichthyes and Osteichthyes.

Chondrichthyes - Cartilaginous fish (Silurian - Rec.)


Ctenacanthus from Julius T. Csotonyi web site

Basic definitions:

Fossil Material: Sharks are arguably the oldest known gnathostomes, but their fossil record is poor because their bodies lack preservable hard parts that stay articulated when they die. Two notable exceptions:

Ecological specializations: Before discussing phylogeny, consider what body types reveal about an animal's mode of life. These are informal designations and do not refer to groups necessarily related by common ancestry.

Phylogeny:

From Discovery Education Ancient Sharks

Basal chondrichthyans: The earliest unambiguous chondrichthyan remains are from the Early Silurian, but consist of isolates scales. Some controversy over where on the tree the basal members of chondrichthyes belong, however we get a good idea of what a primitive chondrichthyan looked like from Cladoselache: (Devonian) Earliest known chondrichthyan from numerous well preserved skeletons. Roughly half meter adult length. Superficially shark like, but hardly a proper modern shark.
Anatomically suited as fast pursuit predator with tall tail, narrow trunk, and finlets to reduce drag of tail base. Stomach contents can include fish swallowed tail first, conodont animals, and invertebrates. One odd feature is the reduction of the pelvic fins and absence of anal fins.

  • Chimaeras and kin:
    In addition, many holocephalians develop dermal skull plates made not of bone, but of dentine. Generally speaking, holocephalians are slow moving and specialize on crushing hard-shelled organisms.

  • Their less specialized fossil relatives likeSymmorida (Late Devonian - Pennsylvanian) Synapomorphy is very long axis of pectoral fin. Interesting feature is their tendency to develop sexually dimorphic display structures on their heads and anterior dorsal fins. Possible uses include:
    Note: Although Symmorids are superficially shark-like they are evidently closer relatives of Holocephali. Synapomorphy is that their lateral lines are protected by an armor of tiny calcified rings.

    Elasmobranchii: (Devonian - Recent) Proper sharks. Synapomorphy is a specialization of the branchial arches (don't ask). Earliest known elasmobranch is Antarctilamna from the Middle Devonian.

    Note: each dorsal fin has a fin spine. Although these are prominent in sharks, they are probably plesiomorphich for chondrichthyes as a whole. Cladoselache has them, as do many non-chondrichthyan gnathostomes.

  • Like placoderms, elasmobranchs have occupied many ecological niches and embrace great diversity. Some interesting cases include:

    Diversity through time:

    From Biology of Sharks and Rays

    Early history:

    Chondrichthyans appear in fossil record as isolated denticles or teeth definitely by Middle Silurian, maybe Late Ordovician! Full body fossils don't appear until Middle Devonian. when primitive chondrichthyans like Cladoselache (neither shark nor chimaera) and early elasmobranchs appear.

    From Biology of Sharks and Rays

    Late Paleozoic:

    During the early Late Paleozoic, chondrichthyan diversity climbed significantly. The Mississippian was a "first golden age" for chondrichthyans. Both holocephali and elasmobranchs became very common in both fresh and salt water. Possibly, terminal Devonian extinction of placoderms provided opportunity. By the end of this interval, almost all of the major chondrichthyan groups are accounted for, save one.

    From Biology of Sharks and Rays

    Mesozoic:

    Chimaeras and sharks persist at lower diversity. In oceans, more primitive sharks like Hybodus (left) become rare as sharks more closely related to modern forms are dominant. The common ancestor of all living proper sharks lived in the Late Triassic or Early Jurassic (same time as rise of dinosaurs on land). They become the most common chondrichthyans during the Cretaceous and early Cenozoic. Rays appear in Late Jurassic.

    From Biology of Sharks and Rays

    Cenozoic:

    A "second golden age" in chondrichthyan diversity occurred during the Neogene.