Test Flashcards
(421 cards)
Chordata
(A) Deuterostomata “Deuterostomia”
(blastopore forms into anus)
(B) paired gill slits
(C) dorsal hollow nerve chord
(D)Chordata (notochord well developed,
post-anal tail)
(E) mesodermal somites, lateral-plate
mesoderm
(I) Ambulacraria (trimeric adult coelom) Yunnanozoon
(Chenjiang
fauna) Middle
Cambrian
•Found in the earliest
Cambrian (530mya)
Cephalochordates
: living fossils
Pikaia: The burgessshale
The ordivician
stabilized.
Oxygen concentrations were about 14%
or about 2/3 of what they are today.
• How would this have impacted on life?
Carbon dioxide levels were over 10X
what they are today.
• Eventually the CO2 in the atmosphere began to
drop Early Ordovician was very warm with mean global
temperatures of around 16˚C.
• Two major climatic events occurred in the
transition between the Early and Middle
Ordovician and once again in the transition
between the Middle and Late Ordovician.
• In each case the mean temperature dropped by as much
as 6-8˚C.
• Glaciation event at the end of the Ordovician.
Life in the sediment
– More burrowers à pump O2-rich
water into sediment
– Indicated by increased bioturbation
through time
Conodont
Conodont
Anatomy
•Resembled modern day hagfish
and lampreys.
•Tooth-like structures suggest
predatory role.
• No evidence of true jaw
Geology of
the
Ordovician
Geology of
the
Ordovician
• Major Orogeny (Appalachian
Mountains)
• Rodinia continued to break-
up resulting in three discrete
land masses: Laurentia (N.
America), Siberia (Asia), &
Gondwana (Africa, India
Antarctica, S. America, &
Australia).
Jawless
Fish
Vertebrata, neural crest brain, paired olfactory capsules,
1+ set semicircular canals.
B)Extrinsic eye muscles, 2+
semicircular canals, braincase,
neuromasts.
C) Calcified dermal skeleton.
D)Cerebellum, dermal skeleton
of trunk.
E)Pteraspidomorphi- tubercles
oak-leaf shaped.
F) Large unpaired dorsal and
ventral dermal plates on head.
G) Paired fins
Ostracoderms
Ostracoderms
Armoured agnathans from the past
(possess dermal bone) Dermal bone- intramembraneous, formed in dermis. Dentine with pulp cavity. Osteostraci
- Ordovician to Devonian, 200+ species
• Well
-developed pectoral fins*
• Ventral gills • Ecologically diverse
- All
• aquatic and marine • \environments
Osteostraci
&
Lam
p
r
e
y
s
ÑOlfactory organs similar to modern lampreys ÑOrbits close together on top of head; pineal
ʻeye
ʼ
ÑEndolymphatic ducts connect inner ear to external
environment; sand entered inner ear chambers
Osteostraci &
Gnathostomes
Osteostraci &
Gnathostomes
Characters shared with jawed
vertebrates(gnathostomes):
• Paired fins (homologous?)
• Cellular bone
• Sclerotic ring in eyes
• Hypocercal caudal fin
Defining Homology
•
Defining Homology
• Homology: trait that is shared and derived.
• Analogy: trait that is not shared (i.e., evolved due to
convergence). For example, the wings of a bat and
a bird were not present in the common ancestor of
either group, therefore, the presence of wings in
these taxa is not informative.
Cladistic/Phylogenetic
Terminology
Apomorphy: Derived Trait
• Synapomorphy: Shared and derived (i.e., unique to closely
related taxa) trait
• Plesiomorphy: Primitive Trait
• Symplesiomorphy: Shared but primitive (ancestral) trait
• Autapomorphy: Uniquely derived (i.e., present on only
one taxon) trait
• Homoplasy: Superficially similar (i.e., analogous) trait
that is not shared
• Sister-group: Sharing a common ancestry (i.e., common
descent)
• Out-Group: Distantly related ancestor (i.e., does not
form part of the group
Ordovician glaciation and mass
extinction
Toward end of Ordovician,
Gondwanaland (now the
southern continents) neared
south pole
– Glaciers expand → sea-level fall
– Mass extinction (2 pulses)
Image: Stanley (2009)
Ordovician glaciation and mass
extinction
Pulse 1: Warm-
adapted taxa
Pulse 2: Cold-
adapted taxa
Silurian
the end Ordovician glaciation the climate of the Silurian warmed.
• Three distinct episodes occur (Primo & Secundo episodes)
• Primo events lead to higher CO2 concentrations reducing the temperature gradient between
the equator and higher latitudes. Climate is more tropical.
• Secundo events lead to lower CO2 concentrations, which raises the temperature gradient
between the equator and the higher latitudes. Climate is drier.
• Geological processes isolated some large bodies of water turning them in
enormous Salt Lakes.
• Windsor salt in the Windsor area of southern Ontario is an example of the massive
salt deposits in the form of dolomite.
• Combination of changing temperature gradients based on the episodes in
question results in oceanic stratifciation Interesting relationship between sea-level
change and temperature
Impact on the evolution of vertebrates
and notably the evolution of jaws
Anaspids
Anaspids
Inclined row of gill openings
Anal fin present;
Sometimes ventral paired fins
Hypocercal tail Possible placement of an aspids as the sister-group to modern lampreys, as the sister-taxon to all ostracoderms, all ostracoderms with the exclusion of pteraspidomorphs, or as the sister-taxon to Gnathostomata (shown in blue).
Tooth
formation
histological structure of teeth
is virtually identical to the scaly
denticles present in some later
placoderms Tooth formation and
eruption:
dental lamina- inward
growth of longitudinal
ridge of ectoderm into
underlying dermis.
-initiates aggregation of
neural crest cells from
dermis into tooth buds.
Gnathostomata
(synapomorphies
)
Gnathostomata
(synapomorphies
)
A) Upper (palatoquadrate) and
lower (Meckel’
s cartilage) jaws
- Endoskeletal girdles
- 3rd semicircular canal
B) Teeth erupt from dental
lamina
-Nasal capsule fused to
neurocranium
-Postorbial connection of
palatoquadrate to braincase.
C) Ventral cranial fissure.
Devonian
Mountain building continues with the Caledonian
and Appalachian orogenies contributing to
extensive mountain ranges across north
-western
Europe and the north
-eastern portion of N.
America. • Continental movement continues to this day.
For example, at present, N. America move
closer to each other by about 10 cm every
year.
• Baltica (Europe) and N. America collide, which in
-
turn increase the mountain building phase. • Changes to geography will influence climate
patterns. Can you think
why this happens
? Global temperatures steadily increase – reaching
approximately 30˚C across much of the Earth’s
surface.
• Sea-level rises and evidence shows that it tracked
the increasing temperature trend.
• However, ocean and freshwater systems
experienced reduction in oxygen levels. The latter part of the Devonian witnessed one of
the 5 mass extinctions of the Proterozoic.
• Unlike some of the other mass extinctions, this one
occurred in two stages.
• The Kellwasser event that occurred between
the Middle and early part of the Upper
Devonian
• The Hangeberg event that occurred at the
Devonian/Carboniferous boundary.
Chondrichthyes
Chondrichthyes- calcified cartilage (CaPO,), dorsal fin at pelvic level, metapterygial fin w/5+ radials, pelvic claspers.
Elasmobranchii- hypochordal lobe of caudal fin large
Euselachii- tribasal pectoral fin
Neose ach- calcitied ventcom centra.
Osteichthyes
Actinopterygia (ray-finned) Represented by small fish (30 cm or
less) with heavy rhomboid scales
• Includes relatively large forms > than
50 cm in length.
• Predatory with large fangs – likely to
feed on the smaller actinopterygians
Acanthodians
Acanthodians
(Spiny Sharks)
• Enigmatic taxon.
• Affinities with modern clades unclear.
• Most were small – no more than 50 cm.
• Characterized by prominent spines on most of
their fins.
Psarolepis & Meemannia
shared by Psarolepis
and Sarcoptrygians:
Three large infradentary
foramina
Presence of a parasymphyseal
tooth whorl (long hooked teeth
that point up and forward)
Teeth have multiple enfolding
(grooves) of their surface and are
covered with a type of bony
material known as cosmine. The characteristic spines
so common to
acanthodians and
found in some sharks
have never been
known in bony fish yet
Psarolepis shares this
trait with
acanthodians.
What really is a Bony
Fish?
Traits found in common between Psarolepis & Meemannia and
actinopterygians include:
• An actinopterygian-like skull roof pattern
• The absence of a dermal joint between the parietal and
the postparietal
• The superimposition of enamel–odontode layers of the
scales
• Loss of the squamosal elements of the skull.
• Sensory canal running through preopercular has a ventral
extension leading to the maxilla.
Blue characters represent primitive states for the clade uniting
sarcopterygians and actinopterygians
Sarcopterygi
a and stem
tetrapods
Paraphyletic assemblage Early
Tetrapod
Phylogeny
NODE A: Dorsal fin lost, frontal present.
NODE B: Pre- & postzygapophyses, rudimentary sacrum
present.
Tetrapoda: Carpus, tarsus, ilium attached to vertebral
column by sacral rib. Stapes, pectoral girdle free from skull,
zeugopodial elements articulate w/autopodial elements.
Crown-group tetrapods: 6 or less digits, tail fin lost. From Fin to
Hand!
Hox genes play major
role.
Paralogous gene
expression results in the
transition from fin to
hand.
Developmental timing of
gene expression is
responsible.
Ichthyostega
Autapomorphies:
• The intertemporal bone is lost.
• There is a single, median postparietal instead of paired.
• It has sturdy ribs with uncinate processes
(posterior flanges articulating with the rib
behind it).
• They probably helped to strengthen the axial
skeleton because the vertebrae were not very sturdy •The first true tetrapod.
•Note how it resembles the rhipidistian fish Eusthenopteron snout is longer and it is composed of fewer, larger bones.
There were anterior and posterior articulations between the vertebrae.
The anterior articulation, called the prezygapophysis, faces dorsally, and the posterior
articulation, called the postzygapophysis, faces ventrally. These connect to each other,
and provide additional support for the vertebral column.
There is a sacral vertebra, whose rib articulates with the pelvic girdle.
NOTE: the three pelvic elements (in colour) are shown with the
hindlimb outline superimposed*