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Cambrian Explosion What is meant by “Explosion”:
Adaptive radiation of animals
Morphological diversification
Development of hard-part skeletons
Global expansion of the fauna in the ocean
Burgess Shale (cambrian rock)
A representative Cambrian rock deposit in British Columbia, Canada.
What is significant about Burgess Shale?
Rock that is evidence for the cambrian explosion
Many specimens preserve soft-body parts
Break up of Pannotia:
Six major continents (incl. Laurentia & Gondwana)
Expansion of well-circulated shallow seas
Warmer climate & oceanic crust than today
Crust was warmer than today because it rotated faster
Higher sea level
Abundant oceanic invertebrates & first vertebrates:
Archaeocyathid (Cambrian)/ Bryozoan (Ordovician) reefs
Brachiopods
Mollusks (e.g., nautiloids)
Arthropods (e.g., trilobites)
Jawless fishes
What happened at the end of early Paleozoic (Cambrian-ordovician) and what did it lead to?
Major glaciation -> Mass extinction
what are Archaeocyathid (Cambrian)/ Bryozoan (Ordovician)?
reefs
What are Brachiopods?
are marine invertebrates with two shells hinged at the back. They are filter feeders and have a rich fossil record dating back over 500 million years.
what are Mollusks (e.g., nautiloids)?
are soft-bodied invertebrates with a muscular foot, visceral mass, and a mantle that often secretes a calcium carbonate shell.
What are Arthropods (e.g., trilobites)?
are invertebrate animals with exoskeletons, segmented bodies, and jointed appendages. Trilobites are an extinct group of marine arthropods.
Extensive shallow season continued in what phase
mid-paleozoic
What are Tabulate & rugose corals
reef builders
First jawed fishes happened when
Silurian [Ordovician]
what was the devonian known for
“Age of Fishes”
What animals existed during the age of fishes
Placoderms, early ‘sharks’ & bony fishes
What emerged during the mid-paleozoic
First land plants during silurian but possibly ordovician
What did the first land plants cause
Thickened ozone layer
What did the thickened ozone layer cause
First land animals (e.g., arthropods)
When did the first tetrapod occur
late devonian
When was there a mass extinction in mid-paleozoic
Devonian cause(s) still in debate
Evolution of land plants in mid-paleozoic
Bryophytes (non-vascular plants; mosses)
Tracheophytes (vascular plants: plants with stems (+ roots + leaves) = ‘most plants’)
Rhyniophytes (first tracheophytes without roots or leaves)
Evolution of land vertebrates in mid-paleozoic
Tiktaalik (= ‘transitional form’ between fishes and tetrapods during the late Devonian)
Appendicular bones (basic limb architecture of tetrapods have already evolved)
Pectoral girdle still attached to skill (this is still a fish characteristics)
Tetrapods (amphibians & reptiles diversified during the ‘late’ Paleozoic)
Bryophytes
non-vascular plants; mosses
Tracheophytes
vascular plants: plants with stems (+ roots + leaves) = ‘most plants’
Rhyniophytes
first tracheophytes without roots or leaves
Tiktaalik
‘transitional form’ between fishes and tetrapods during the late Devonian
Appendicular bones
basic limb architecture of tetrapods have already evolved
Pectoral girdle still attached to skull
this is still a fish characteristics
Tetrapods
amphibians & reptiles diversified during the ‘late’ Paleozoic
‘Late’ Paleozoic
Carboniferous-Permian
What happened during the late paleozoic
Gathering of continents (Carboniferous)
Formation of Pangaea & Panthalassa Ocean (Permian)
late paleozoic climate
Carboniferous:
Major glaciation (Gondwana)
Warm & humid (other regions)
Permian:
Widespread arid condition
Carboniferous climate
Major glaciation (Gondwana)
Warm & humid (other regions)
Permian climate
Widespread arid condition
Marine life in Late paleozoic
Brachiopods
Mollusks (e.g., nautiloids)
Arthropods (e.g., trilobites)
Echinoderms (e.g., crinoids)
Jawed fishes
land life late paleozoic
Coal swamps & forest (e.g., ferns, lycopods, & seed-bearing trees)
Insects
Amphibians gave rise to ‘amniotes’ that lay shelled eggs (e.g., ancestral reptiles & ‘mammal-like’ reptiles)
Mass extinction in paleozoic
The greatest mass extinction in the Earth’s history
Over 90% of life disappeared
Cause(s) still in debate but likely intense volcanism & poor oceanic circulation
When did Archaeocyathid happen
Cambrian
when did bryozoan occur
Ordovician
what are Brachiopods
are marine invertebrates with two shells that are hinged at the back. They are filter feeders and have a unique feeding structure called a lophophore.
what are Mollusks
are soft-bodied invertebrates with shells, like snails, clams, and octopuses. They have a muscular foot and a mantle that secretes the shell.
what are Arthropods
are invertebrate animals with segmented bodies, exoskeletons, and jointed appendages. They include insects, spiders, crustaceans, and millipedes.
What are Echinoderms
are marine animals characterized by radial symmetry, a water vascular system, and spiny skin. Examples include starfish, sea urchins, and sea cucumbers.
When did mass extinctions occur
end of pleistocene
end of cretaceous
end of triassic
end of permian
End of devonian
end of ordovician
What is the Mesozoic Era known as
age of reptiles
What happened during mesozoic era
Breakup of pangaea:
Laurasia (north america, greenland, eurasia)
Gondwana (south am., africa, india, australia, antarctica)
Tethy and Atlantic Oceans
what was the climate like in mesozoic era
Triassic: Dry in low-mid latitude and wet in high latitude
Cretaceous: Equably warm worldwide
What was the plants like in mesozoic era
Seed-bearing trees (conifers: Triassic-Jurassic)
Flowering plants (Cretaceous-Today)
Invertebrates in Mesozoic era
Mollusks (ammonoids, bivalves, & gastropods)
Echinoderms (e.g., sea urchins)
Crustaceans (crabs & lobsters)
Mammals (evolved from mammal-like reptiles) mesozoic
Egg-laying mammals
Multituberculates
Live-bearing mammals (marsupials and placentals)
Reptiles mesozoic
Turtles, lizards and snakes
Ichthyosaurs & plesiosaurs
Mesozoic marine reptiles (thrived during this time)
Archosaurians:
Crurotarsans (incl. crocodiles)
Pterosaurs (= flying reptiles)
Dinosaurs (one lineage gave rise to birds)
Mass extinction mesozoic cause
asteroid impact near Yucatan peninsula
What was the cenozoic era known as
Age of mammals
what was the tectonic activity like in cenozoic
Present-day arrangement of continents & oceans
Expanding Pacific and Atlantic Oceans
India-Eurasia collision & closure of Tethys Ocean
Formation of Indian Ocean
Orogenic belts:
Circum-Pacific Belt (so-called “ring of fire” because of extensive volcanism)
Alpine-Himalayan Belt
Circum-Pacific Belt
“ring of fire”
Climate of cenozoic
History:
Paleogene: tropical
Neogene: Cool
Pleistocene: Series of ice ages and warm periods
Causes (natural):
Plate tectonics and volcanism
Milankovitch theory
Just know its the idea that explains how the ice age occurs
Variation in solar energy
Organism
paleogene climate
tripical
neogene climate
cool
pleistocene climate
series of ice ages and warm periods
causes of climate cenozoic
Plate tectonics and volcanism
Milankovitch theory
Just know its the idea that explains how the ice age occurs
Variation in solar energy
Organism
Cenozoic life:
Flowering plants (incl. grasslands: Oligocene-Today)
Scleractinian corals, mollusks, and echinoids
Birds and placental mammals (incl. humans)
Milankovitch Theory
explains how changes in Earth's orbit and axial tilt influence climate change over long periods of time.
India-Eurasia collision & closure of Tethys Ocean
Formation of Indian Ocean
orogenic belts in cenozoic era
circum-pacific belt
alpine-himalayan belt
Archosaurians
Crurotarsans
Pterosaurs
Dinosaurs
What is significant about dinosaurs mesozoic
one lineage gave rise to birds
pterosaurs
flying reptiles
crurotarsans
are a group of archosaurs that includes crocodiles and their extinct relatives. They have a unique ankle joint structure.
Triassic climate
Dry in low-mid latitude & wet in high latitude
cretaceous climate
Equably warm worldwide
Laurasia
[North America, Greenland, Eurasia]
Gondwana
[South Am., Africa, India, Australia, Antarctica] → tethys and atlantic oceans
Warmer climate & oceanic crust than today caused what
higher sea levels