GEOL 104 Dinosaurs: A Natural History
Fall Semester 2011
Anatomy & Taxonomy
Our Bodies, Our Selves: Introduction to Vertebrate Osetology

Labeled skeletons of Camarasaurus and Tyrannosaurus; image Courtesy of Sauropod Vertebra Picture of the Week
Homologous structures: the same anatomical structure, regardless of function.
Analogous structures: represent different units of anatomy serving the same function.
Comparative anatomy seeks to describe the structure of the bodies of organisms in terms
of their homologous structures.
Functions of the skeleton:
- Support
- Protection of organs: such as the facial bones protect the sensory capsules, the braincase protects the brain, the ribs protect the
heart and lungs, etc.
- Mechanical Structures:
- Bones contact one another at joints. These joints may be immobile (like many joints in the skull) or permit motion (such as between
vertebrae, in the jaws, or in the limbs)
- Bones are connected to other bones by ligaments; bones are connected to muscles by tendons
- Muscles pull by becoming shorter; they cannot PUSH (instead, a separate set of mucles has to act in order to move the joint back to the
original position)
Anatomical Directions
- Anterior (towards the tip of the snout)/Posterior (towards the tip of the
tail)
- Dorsal (up and out through the spine)/Ventral (down and out through
the belly)
- Medial (towards the middle)/Lateral (towards the sides)
- Proximal (towards the trunk)/Distal (away from the trunk)
- Proximal and distal are normally used only for the limbs, and occasionally for the
tail
- (NOTE: some use "cranial/caudal"
instead of "anterior/posterior" (and "rostral/caudal" within the head itself))
Anatomical views: when a specimen is illustrated, the anatomical view represents that
surface of the specimen that is shown.
Anatomical landmarks: particular homologous structures on the skeleton (openings,
joints, etc.) used for identifying the position of bones or other features of the anatomy.
The skeleton of a dinosaur (or other vertebrate) is divided into a couple of different
sections:
- The skull, composed of:
- The cranium (braincase, face, and upper jaw)
- The mandible (lower jaw)
- The postcranium (everything posterior to the cranium), composed of:
- The axial skeleton (spine, ribs, and related features of the neck, trunk, and tail)
- The appendicular skeleton (forelimb, hindlimb, and their girdles)
(Incidentally, anatomical terms are for the most part based on Latin words. Bones or landmarks
with Latin rather than English plurals are noted below)
Important Bones and Landmarks of the Skull
NOTE: Almost all bones and landmarks of the skull are paired, with one on the right
side and one on the left. Although the skulls of vertebrates are composed of many bones,
these bones are joined by sutures: depending on the type of suture, the joint can
be mobile or immobile.
- Orbit: eyesocket
- Naris (pl. nares): nostril socket
- Antorbital fenestra: a large opening in the facial bones of dinosaurs and their relatives,
anterior to the orbit and posterior to the naris (fenestra, pl. fenestrae:
an large opening in the skeleton, from the Latin word for "window")
- Teeth. In dinosaurs and most other land-dwelling vertebrates, the teeth are found
in three main bones: two on each side of the upper jaw, and on on each side of the lower jaw
- Made of the same material (hydroxylapatite) as bone, but of hard dentine and even harder (more crystalline) enamel
- Dinosaur teeth (like mammals) grow out of "sockets"
- Like most vertebrates (but NOT mammals), they got new teeth from each socket throughout their life
- Socketed teeth consist of:
- A root (formed of dentine) with fits into the socket
- An enamel-covered crown that sticks out of the gumline
- In most dinosaurs, there is no tooth-to-tooth contact (occlusion): instead, the teeth swipe past each other
- The edges of many dinosaur teeth have either serrations (small lumps good for slicing meat) or larger denticles (large projections better for chopping up plants)
- Premaxilla (pl. premaxillae): anterior of the tooth-bearing bones of
the cranium
- Maxilla (pl. maxillae): posterior of the two tooth-bearing bones of
the cranium
- Lacrimal: bone separating the antorbital fenestra and orbit, contains the tear
duct
- Postorbital: bone posterior to the orbit
- Jugal: the "cheek bone", ventral to the orbit
- Temporal fenestrae: openings in the back part of the skull for attachment and
expansion of the jaw muscles. In dinosaurs and their relatives, there are two temporal
fenestrae on each half of the skull (left and right):
- Infratemporal fenestra: also called the lateral temporal fenstra, opening
on the side of the skull
- Supratemporal fenestra: opening on the top of the skull
- Nasal: bone along the top of the snout dorsal to the naris and maxilla
- Braincase: a collection of bones which surrounds the brain cavity
- Foramen magnum: Latin for "great opening", the hole in the back of the braincase
where the spinal cord emerges from the brainstem
- Occipital condyle: a condyle (rounded knob joint) composed of several different
bones just ventral to the foramen magnum; the connection between the cranium and the backbone
- Dentary: the tooth-bearing bone of the mandible; in mammals the whole of the mandible
is composed of just the dentary, but in dinosaurs and most other vertebrates there are various
postdentary bones
- Mandibular fenestra: in dinosaur and their relatives, an opening on the lateral
surface of the mandible surrounded by the dentary and the postdentary bones
Teeth are composed of materials (softer dentine and harder enamel) similar
to bone. Teeth have a root which fits into the socket of the jaws and a crown
covered with enamel which chops, crushes, pulps, tears, slices, and/or grinds food.
Most types of dinosaur teeth do not show occlusion (when one surfae meets another).
In all types of toothed dinosaur, the teeth are renewed throughout life.
Bones and Landmarks of the Axial Skeleton
Most of the axial skeleton is composed of the vertebral column, itself composed of
individual vertebrae (singular, vertebra). Each vertebra contains the following
sections:
Centrum (pl. centra): the large spool-shaped body
Neural arch: an arch of bone on dorsal surface of the centrum
Neural canal: the hole through which the spinal chord passes. (Popular conception
to the contrary, the spinal cord does not pass through the centra
Transverse processes: bony extensions off the lateral sides of the neural arch,
for attachment of muscles, tendons, ribs, etc.
Neural spine: bony extension off the dorsal surface of the neural arch
Various other prongs and crests off the neural arch and centrum, not dealt with in this class

Skeleton of Giraffatitan, with sections of the vertebral column labeled; image Courtesy of Sauropod Vertebra Picture of the Week
The vertebral column is divided into four sections in dinosaurs and their relatives:
- Cervical: the neck
- Dorsal: the back
- Sacral: the hips
- (Sometimes the sacral vertebrae are fused into a single unit, called a sacrum)
- Caudal: the tail


Labeled portions of the skeleton of Camarasaurus; image Courtesy of Sauropod Vertebra Picture of the Week
Attached to the cervical and dorsal vertebrae are ribs (one on each side). Sacral
ribs also exist, but are often fused to the pelvic girdle (see below). Instead of ribs,
caudal vertebrae have chevrons, single bones which protect the nerves and blood
vessels that run underneath the caudal centra.
Ventral to the guts of dinosaurs and many other land vertebrates are gastralia
(singular gastralium), or "belly ribs". In dinosaurs they are one or two pieces
per side.
Some dinosaurs have dermal ossifications or scutes: bones in the skin of
the animal used for armor.
Bones and Landmarks of the Appendicular Skeleton
The appendicular skeleton is comprised of the limbs and their girdles (bones
that attach the limbs to the axial skeleton.
The Pectoral Girdle
The forelimb is attached to the dorsal part of the axial skeleton by the pectoral
girdle. The pectoral girdle is composed of the following bones:
Scapula (pl. scapulae): the shoulder blade
Coracoid: a bone on the ventral side of the shoulder blade. The shoulder joint
of dinosaurs faces mostly posteriorly
Clavicle: collar bone. Paired and separate in most dinosaurs, but in meat-eating
dinosaurs the clavicles are fused along the midline to form a single bone, the furcula
(pl. furculae), or "wishbone".
Sternum (pl. sterna): the brestbone. In some dinosaurs it is composed
of seperate sternal plates; in other it is fused. It is on the ventral surface of
the chest

Left lateral view of the left pectoral girdle and forelimb of Camarasaurus; image Courtesy of Sauropod Vertebra Picture of the Week

Right lateral view of right pectoral girdle and forelimb of Centrosaurus; image courtesy of The Open Dinosaur Project
The Forelimb
Humerus (pl. humeri: upper arm bone. Meets with the scapula & coracoid
at the shoulder, and the radius and ulna at the elbow
Ulna (pl. ulnae): (generally) larger and more posterior of the forearm bones.
The "funny bone" (techincally the olecranon process) is the backwards-pointing projection of
the ulna.
Radius (pl. radii): smaller and more anterior of the forearm bones.
Manus (pl. manus): the hand. Composed of:
- Carpals: various small bones of the wrist. The wrist as a whole is called
the carpus (pl. carpi)
- Metacarpals: the long bones of the palm of the hand. These are numbered I-V, with
I being the medialmost (the one to which the thumb is attached) and V being the lateralmost
(the one to which the pinky is attached). All the metacarpals as a unit are called the
metacarpus (pl. metacarpi)
- Digits: fingers. Digits are numbered I-V as above, with I being the thumb, and
V being the pinky. Digits are composed of individual finger bones or phalanges
(singular phalanx). The distalmost, claw- or hoof-bearing phalanx is called the
ungual

Anterior view of right manus of Centrosaurus; image courtesy of The Open Dinosaur Project
The Pelvic Girdle

Left lateral view of the left pelvic girdle and hindlimb of Camarasaurus; image Courtesy of Sauropod Vertebra Picture of the Week
The hindlimb is attached to the sacral part of the axial skeleton by the pelvic
girdle (aka the pelvis (pl. pelves) or "hips"). The pelvic girdle is
composed of three bones on each side:
Ilium (pl. ilia): the dorsalmost of the bones, which connects directly
to the sacral vertebrae
Pubis (pl. pubes>: the lower pelvic bone that always attaches to
the ilium anterior to the ischium (see below), although the shaft of the pubis in some
dinosaurs points backwards
Ischium (pl. ischia): the lower pelvic bone that always attaches posterior
to the pubis, and points posteriorly as well
Acetabulum (pl. acetabula): the hip socket, where the femur (see below)
fits into the pelvis. In most vertebrates there is a sheet of solid bone formed by
the pelvic bones on the medial surface of the acetabulum, but dinosaurs are specialized
in having a perforate (opened) acetabulum (i.e., only a sheet of cartilage rather
than bone on the medial surface).

Right lateral view of right pelvic girdle and hindlimb of Centrosaurus; image courtesy of The Open Dinosaur Project
The Hindlimb
Note that the structure of the hindlimb is very similar to that of the forelimb.
Femur (pl. femora: thigh bone. Fits into the acetabulum by the
femoral head, and meets the tibia and fibula (below) at the knee. Often the
single largest bone in the body (except for small running dinosaurs, in which the tibia
is generally larger).
Tibia (pl. tibiae): the main shin bone. Generally thicker than, and medial
to, the fibula
Fibula (pl. fibulae): smaller and lateral of the shin bones. Note that,
popular misconception to the contrary, there is NO such bone as a
"fibia"!
Pes (pl. pedes): the foot. Composed of:
- Tarsals: various small bones of the ankle. The wrist as a whole is called
the tarsus (pl. tarsi. Two tarsals of importance in dinosaurs are the two
proximal tarsals, the astragalus (pl. astragali) and calcaneum (pl.
calcanea), which fit onto the distal ends of the tibia and fibula
Incidentally, dinosaurs and their closest relatives lack a heel (which is formed in
other land vertebrates by a backwards projection of the calcaneum)
- Metatarsals: the long bones of the body of the foot. These are numbered I-V, with
I being the medialmost (the one to which the big toe is attached) and V being the lateralmost
(the one to which the little toe is attached). All the metacarpals as a unit are called the
metatarsus (pl. metatarsi). Unlike humans and bears, but like cats and dogs
and horses (and birds...), dinosaurs held their metatarsi upright, so that their ankles
did not normally touch the ground
- Digits: toes. Digits are numbered I-V as above, with I being the big toe, and
V being the little toe. Digits are composed of individual finger bones or phalanges
(singular phalanx). The distalmost, claw- or hoof-bearing phalanx is called the
ungual

Anterior view of right pes of Centrosaurus; image courtesy of The Open Dinosaur Project
Excellent overview of
dinosaur anatomy, and here,
and here as well.
Taxonomy and Species
TAXONOMY
Taxon (pl. taxa): a named group of organisms.
Traditionally, each culture had its own name for the animals, plants, and other organisms in their region. But EACH culture had its own set of names, so the same type of animal might have many different names. During the 1600s and 1700s, methods were proposed for a formal scientific set of names.
Carl von Linne' (Linnaeus) developed a universal set of rules in the Systema Naturae ("System of Nature") in 1758; later workers added and modified the system (primarily with the addition of new "ranks").
Some of the Linnean rules:
- All names are in Latin or Greek, or are modified into Latin form;
- Each name must be unique;
- All names are fit into a nested hierarchy (species into genera, genera into families,
and so forth);
- In traditional Linnean taxonomy, there is a set of official ranks (from smallest to
largest, species, genus, family, order, class, phylum) (later workers added additional
intermediate ranks, such as tribes, subfamilies, superfamilies, subphyla, etc.);
- The primary unit is the species (pl. species):
- Refers to a "specific" kind of organism
- Definition of a "species" varies from biologist to biologist; some definitions
("naturally occurring interbreeding populations") cannot be tested for fossils!
- Each species has a type specimen accessioned in an appropriate institution (museum, zoological or botanical garden, or other such collection);
- Whoever describes the type specimen of a new species has the right to name that new species (following the rules below);
- The next higher unit, the genus (pl. genera) is composed of one or more species
- Refers to a more "generic" category than species
- Definition of a "genus" is problematic as well, since it is composed of one or more "species";
- Each genus has a type species: all other species are assigned to the
genus based on their similarity to the type species;
Linnean taxonomy has its own special set of grammatical rules:
- Genera have one word names (e.g., Panthera, Homo,
Ginkgo, Tyrannosaurus);
- The genus name is always Capitalized and italicized (or
underlined if you don't have access to italics);
- Species have two word names, the first part of which is the same as the
genus name (e.g., Panthera leo, Homo sapiens, Ginkgo biloba,
Tyrannosaurus rex)
- The genus name is ALWAYS capitalized, the second part ("trivial nomen") is
ALWAYS in lower case, and the name is ALWAYS italicized or underlined;
- Species names can be abbreviated by using only the first letter of the genus name,
followed by a period (NEVER by a hyphen): H. sapiens and T. rex are correct;
H. Sapiens or T-Rex are WRONG!! (Subtle hint: do not
use the incorrect form on your homework or tests);
- All taxon names other than species have one word names, which are capitalized;
all taxon names other than genera and species are in roman letters (i.e., they are
never italicized/underlined): Dinosauria, Tyrannosauridae, Animalia; not Dinosauria,
tyrannosauridae, or animalia.
- Taxon names of whatever "rank" have some etymology (derivation) (that's true of all words, really). Sometimes
the name might be descriptive (e.g., "Triceratops horridus", the "roughened three-horned face") or
it might honor a place of discovery (e.g., "Albertosaurus", found in the Canadian Province of Alberta)
or some individual (e.g., "Diplodocus carnegii", after billionaire Andrew Carnegie who's funding
supported the expedition and museum which found this species). But the name can be inaccurate (e.g., "Basilosaurus"--Emperor
Reptile--is a whale, not a reptile!) but if the name was formed obeying the rules of taxonomy, that inaccurate
descriptor is fine.
Because there is disagreement about the features used to define a particular species or
genus, different biologists and paleontologists will sometimes disagree about which
specimens belong in a particular species, and which species belong in a particular genus
(and so forth).
- Taxonomists who consider a particular set of specimens to represent many taxa are
called splitters; those who consider a particular set to represent few taxa are
called lumpers;
- If a taxonomist feels that some specimens of a genus belong to an as-yet unnamed
species, they can split these specimens off as a new species (which a new type specimen);
- On the other hand, if a taxonomist considers that two previously named species are
not distinct enough from each other to truly be distinct species (that is, the taxonomist
regards the two names as synonyms), they may lump them together:
- In these cases, the Rule of Priority is used: whichever of the names was
published first, even if only by days, is the name that must be used;
- The same case applies to genera: if two genera are thought to represent the same
genus, the first named genus name is the one that is used.
For those interested in a website concerning some unusual Linnean species names, click
here.
SPECIES
What is a species? Above we see the rules for these names, but it doesn't tell us about what it is being named.
Linnaeus' "species" were taxa like lions, tigers, black bears, etc. These were assemblages of individuals that share certain attributes:
- Similar appearance
- Similar habits and behaviors
- Similar habitats
Darwin did not regard species as a distinct "kind" of biological entity. Instead, he considered them as essentially
the same thing as goegraphic or stratigraphic variations (see these below), but ones in which extinction has removed the
intermediate forms that otherwise would blend into the closest living relative group.
20th Century biologist Ernst Mayr (and most contemporary biologists) formalized their definition of a species as
a "naturally occurring populations that interbreed and produce viable fertile offspring".
But there are some problems with this. For one: hybrids (crosses between two separate species) do occur naturally, and many of
these are actually fertile! And for paleontologists: we can't test interfertility between populations because they are dead!
So we are stuck looking only at shapes (and in fact, only the shapes of those hard parts that survive fossilization).
The question then becomes: how different do two individuals, or two populations, have to be for us to consider them different species?
This is actually a terribly difficult question even with living organisms!! There are several sources of variation:
- Sexual dimorphism: different sexes are different sizes and shapes and have different structures
- Ontogenetic (growth): babies look different from juveniles look different from subadults look different from adults (can be even more
extreme in animals that undergo metamorphosis, like amphibians and many insects)
- Geographic: populations in different regions might have slightly different sizes, color patterns, proportions, behaviors,
etc. For example, some biologists consider the populations of ourangutans, tigers, African elephants, etc. as distinct species; others simply regard them as regional variants
- Stratigraphic: lineages (ancestor and descendant populations) may shift in some traits or characteristics over time
- Individual: one of the great "discoveries" of Darwin and Wallace, the recognition that no two individuals in a population
are identical! (Before them, many people thought that there existed the perfect "type" of each kind of organism, and all variation is
degeneration from that perfection. Darwin and Wallace showed that the variation is the reality)
In fact, the recognition that species were NOT absolute kinds, but instead have "fuzzy" boundaries that
blend into each other, is one of the main clues to the discovery of evolution.
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Last modified: 9 September 2011