Characteristics
The Swedish scientist Carlous Linnaeus (1707-1778) coined
the term Mammalia (Latin, mamma, “breast”) in
1758 to group vertebrate animals that nourish their young
with milk secreted by the mother’s mammary glands.
Visit just about any modern terrestrial environment and you
will find mammals dominant the role of large fauna. If one
uses fossils to track life through the epochs of the Cenozoic
era it becomes clear that this class has played host to an
evolving cast of characters adapting to changing landscapes
and ecosystems. In fact, different mammalian species living
during different times have constituted such an integral
part of ancient ecosystems that the entire 65 million year
history of the Cenozoic era is often referred to as the “age
of mammals”. What are the characteristics and origins
of mammals? Today there are over 5,000 identified living species of mammals,
which represents roughly less then 10% of all vertebrates and
0.4% of all animals. So, measured by the number of species
mammalian diversity is not great; however, mammals exhibit
great diversity in form, which has allowed adaptation to a
wide variety of niches exemplified by organisms as diverse
as humans, whales and bats. What are some of the characteristics
that unite this diverse and successful group?
- Most
mammals, like birds, are homeothermic endotherms.
Homeothermic organisms
use behavioral and physiological strategies
to maintain a constant body temperature regardless
of the environmental temperature. Endothermic organisms
use high metabolic rates
to generate internal body heat. In contrast, many
reptiles are poikilothermic ectotherms. Poikilothermic
organisms have
internal body temperatures that vary with the ambient
environmental temperature. Ectothermic organisms
rely on environmental sources
of heat to control body temperature. Among other
advantages a constant body temperature allows mammals
to be active in
a wide variety of environmental temperatures. This
advantage comes at a cost; mammals must eat up to
10 times as much as
an ectothermic organism to fuel this high metabolism.
- Mammal
skin is watertight and possesses follicles that produce keratinous
hair or fur. Mammal skin may also possess
a variety of glands for sweating, scent production and oil
to maintain fur. A subcutaneous layer of fat is found beneath
the skin. Hair, fat, and sweat glands are important adaptations
for homeothermy.
- Mammals
have a four-chambered heart with a single artery leaving
the heart (aortic arch) that curves to the left.
The four-chambered heart is part of a two-circuit circulatory
system that keeps oxygenated blood separate from deoxygenated
blood. The erythrocytes (red blood cells) of mammals are enucleated
(do not contain nuclei). This system improves the efficiency
of delivering oxygen to cells, an important adaptation for
endothermy.
- Mammal
kidneys possess the loop of Henle, which creates concentrated
urine,
enabling mammals to get rid of nitrogenous
waste with little loss of water. A high metabolic rate generates
a greater amount of metabolic waste; the loope of Henle allows
mammals to rid themselves of this waste.
- Mammals
possess a muscular diaphragm separating the thoracic and
abdominal cavity that helps to ventilate the lungs.
The lung tissue has a high surface area to increase oxygen
absorption.
- Mammals
have an enlarged outer folding of the brain called the neocortex.
Enhanced senses of vision, hearing, and
smell along with a more active lifestyle require a more sophisticated
brain.
The
characteristics above are not usually preserved in
the fossil record, although some, such as brain structure
and presence of a diaphragm can be inferred using skeletal
clues. Paleontologists must look to skeletal structures
shared by mammals when studying mammalian evolution,
we will mention just a few:
- The
lower jaw of mammals is composed of a single bone the dentary,
which articulates with the squamosal bone of the
skull. The lower jaw of primitive amniotes and reptiles is
composed of multiple bones.
- Mammal
teeth are highly differentiated (heterodont dentition) into
incisors,
canines, premolars, and molars. Mammal
molars exhibit a tricuspid pattern and posses multiple roots.
Primitive amniotes and reptiles possess homodont dentition,
having single tooth morphology (all the teeth have pretty much
the same form).
- Mammals
exhibit diphyodont dentition. This means they have two successive
sets of teeth, deciduous (milk teeth) and
permanent (adult teeth). The first generation teeth (milk teeth)
include incisors, canines, and premolars. Incisors, canines,
and premolars are replaced to form the second generation (adult
teeth). A single set of permanent molar teeth is also added
to the adult teeth. Primitive amniotes and reptiles continually
replace their teeth during their lifetime (polyphydont).
- Mammals
have a secondary palate over the roof of the mouth that separates
the nasal and food passages. The secondary
palate allows mammals to breathe while they swallow. Primitive
amniotes and reptiles must hold their breath when swallowing.
- Mammals
have a single external nasal opening.
- The
mammal cranium is enlarged and connected to the vertebrae
column
by a double occipital condyle. The cranium
and the mandible of mammals are fused.
- Mammals have three inner ear bones, the malleus, incus, and
stapes, which transmit sound from the eardrum to the oval
window. The malleus and incus are remnants of the articular
and quadrate bones in the lower jaw of primitive amniotes.
Mammals also tend to have fleshy ears that funnel sound
into the head.
- Mammal
vertebrae are differentiated into cervical, thoracic, and
lumbar regions.
Most mammals have 7 cervical
vertebrae. Mammals have no ribs on their lumbar or cervical
vertebrae.
- Mammals
share important characteristics exhibited by the shoulder
and pelvic girdles that reflect a more erect
gait with limbs tucked underneath the body. The head of the
thighbone (femur) is positioned to one side to accommodate
this gait. The vertebral column is articulated for an up and
down flexion instead of side to side.
- Mammals
grow rapidly after birth and slow to a terminal, adult growth
stage (most other animals grow continuously throughout
their lives). Growth patterns are recorded within the bones.
Mammal Origins
In the Early Carboniferous amniotes split into two lineages
the synapsids (class Synapsida) and the reptiles (class Sauropsida).
Traditionally, synapsids have been referred to as mammal-like
reptiles. Synapsids did not evolve from reptiles, but both
groups share a common ancestry with basal amniotes. Since synapsids
did not evolve from reptiles, the non-taxonomic term protomammals
is preferred over mammal-like reptiles (Prothero, 2004, p.
394).
Synapsids
are traditionally divided into two successive groups, the
pelycosaurs (order
Pelycosauria Greek, “bowl lizard”)
that span from the Mid-Carboniferous to the Late Permian and
the therapsids (order Therapsida) that span from the Mid Permian
to the Mid Jurassic. Many skeletal features common to mammals
evolved among the therapsids. One therapsid evolutionary line,
known as the cynodonts (suborder Cynodontia), would give rise
to mammals sometime during the Triassic.
The synapsid fossil record is rich with transitional forms
illustrating evolutionary trends in skeletal structure, which
lead to and define mammals. The synapsid article on our website
explores some of these skeletal transitions (jaw and ear)
revealed by the fossil record. Triassic carnivorous cynodonts
over time acquired an increasing number of mammalian skeletal
features. Determining when these organisms became mammals is
difficult because they
exhibit a mosaic of mammalian and primitive amniote characteristics.
So, paleontologists must establish a decision based upon evidence
and logic.
There
is a debate regarding how to define the mammalian clade.
Some paleontologists say that logically, we should define
mammals as all of the descendants of the last common ancestor
of
monotremes
(egg
laying mammals) and therians (marsupials and placentals)
(Benton, 2005, p. 289). Under this definition what traditionalists
would call basal or ancient mammals are referred to as
mammaliformes or mammaliaformes (closest relatives of mammals).
Although the definition is logical pinpointing which, if
any fossil fits this criterion is problematic.
The
traditional paleontological view suggests the dentary-squamosal
jaw
joint is the key
mammalian
character
that defines the
node for the clade mammalia, although others use the
presence of an incus and malleus in the middle ear to define
a mammal (Prothero, 2004, p. 399). The node at which morganucontids
branched off the mammalian line marks the base of the mammal
clade if one uses the dentary-squamosal jaw criterion.
This practical definition is supported by evidence that
is easily fossilized; teeth and jaws are the most
common mammalian fossil. However, basal mammals that
meet this criterion possess skeletal structures that consist
of a
mosaic of
mammalian
and primitive
amniote characteristics. We
adopt the traditional view in our museum, using the presence
of the dentary/squamosal jaw joint to
recognize
the first fossil mammals. The dentary/squamosal jaw joint
first appears in shrew-like organisms such as Sinoconodon and Morganucodon.
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