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Review, 1st Paleozoic Vertebrate lecture
• At one point in their lives, all chordates have:– Notochord– Dorsal hollow nerve cord– Gill/phyrangeal slits– Tail
• First vertebrates were marine fish without jaws– Ostracoderms
• Devonian = Age of Fish
Evolution in the Devonian
• Evolution of jaws was a big deal– Extended ecological web/opened new
ecological niches
• Ray Finned Fish and Lobe Finned fish– Lobe fins -> lungfish, crossopterigians (both
have protolungs)– Crossopterygians -> amphibians
• First creatures on land were Arthropods (early Devonian)
• Although amphibians were the first vertebrates to live on land, they were not the first land-living organisms
• Land plants, which probably evolved from green algae, first evolved during the Ordovician
• Furthermore, insects, millipedes, spiders, and snails invaded the land before amphibians
Amphibians—Vertebrates Invade the
Land
• The oldest amphibian fossils Ichthyostega– found in the Devonian of eastern Greenland– streamlined bodies, long tails, and fins– four legs, a strong backbone, a rib cage, and
pelvic and pectoral girdle
Precursor organism (Acanthostega)Was adapted to movement in Wet boggy environments
Oldest Amphibians
• Like other groups that moved into previously unoccupied niches – amphibians underwent rapid adaptive radiation – became abundant during the Carboniferous and Early Permian
• Little resemblance to modern amphibians
• Much more diverse
Rapid Adaptive Radiation
• Reconstruction of a Carboniferous coal swamp
Carboniferous Coal Swamp
Large labyrinthodont amphibian Eryops
The serpentlike Dolichosoma
• In passing from water to land, plants and animals had to solve the same basic problem
– the method of reproduction was the major barrier to expansion into the various terrestrial environments
– required evolution of the seed in plants and the amniote egg in animals
Transition from Water to Land
• Amphibians limited in colonizing the land – had to return to water to lay their gelatinous eggs
• Evolution of the amniote egg freed reptiles from this constraint
Evolution of the Reptiles —
the Land is Conquered
http://www.geoclassics.com/mesosour.htm
• In an amniote egg – the embryo is
surrounded by a liquid sac, the amnion cavity
– provided with a food source (yolk sac) and waste sac
• Its evolution freed reptiles to inhabit all parts of the land
Amniote Egg
• In this way the emerging reptile is – in essence a miniature adult– bypassing the need for a larval stage in the water
• The evolution of the amniote egg allowed vertebrates – to colonize all parts of the land – no longer had to return to the water as part of their
reproductive cycle
Able to Colonize All Parts of the Land
• Reconstruction and skeleton of Hylonomus lyelli from the Pennsylvanian Period
One of the Oldest Known Reptiles
– Hylonomus lyelli was about 30 cm long
• Evolutionary relationship among the Paleozoic reptiles
Paleozoic Reptile Evolution
• Most pelycosaurs have a characteristic sail on their back• Sail explanations: display, thermoregulation• Odd: not closely related; neither had ‘sailed’ predecessor• Adaptive escalation?
Pelycosaurs (Finback Reptiles)
The carnivore Dimetrodon
The herbivore Edaphosaurus
• The pelycosaurs became extinct during the Permian – and were succeeded by the therapsids – that evolved from the carnivorous pelycosaur lineage – and rapidly diversified into
• herbivorous • and carnivorous lineages
Therapsids—Mammal-like Reptiles
• A Late Permian scene in southern Africa showing various therapsids
Therapsids
Dicynodon
Moschops
– Many paleontologists think therapsids were endothermic– and may have had a covering of fur
• Therapsids were small- to medium-sized animals – displaying the beginnings of many mammalian features
• Many paleontologists think therapsids were endothermic
• or warm-blooded – enabling them to maintain a constant internal body
temperature– allowing them to expand into a variety of habitats
Therapsid Characteristics
How are we related to them anyway?
• Relationships among Amniota are tracked via ‘fenestrae’, or openings in the head.
• Fenestrae:– Make the head
lighter– Anchor points for
muscles
Fenestrae in the descendents of proterothyrids
• Fish– First appeared in the Cambrian (jawless fish – first vertebrate)– Diversified in Devonian (Age of Fish)
• Amphibians– First appeared in the Devonian– Evolved from lobe-finned fish
• Reptiles– First appeared in Pennsylvanian– Did not need to return to water to reproduce
Summary
Plant Evolution
• Evolution of photosynthesis: Archaean cyanobacteria
• Genetic evidence suggests that plants evolved from green algae
• No Cambrian explosion for plants– Many steps needed to move plants
onto the land
Buoyancy and humidity
• How to keep your guts wet in a dry world?– Cutin: exterior plant waxes protect from dessication
• How to stay upright when you’re not buoyant in air?– Cellulose and lignin: rigid polymers that make cells
strong
• How to grow bigger than a few centimeters in a dry world?– Develop the ability to move fluids from soils to
leaves
• Earliest plants did not produce seeds
• The sedimentary rocks in which these plant fossils are found – indicate that they lived in low, wet, marshy, freshwater
environments
Earliest Land Plant
• The earliest known fertile land plant was Cooksonia– seen in this fossil from
the Upper Silurian of South Wales
Vascular plants
– Vascular system:• network of tubes which distribute nutrients and
remove wastes• Not clear if Cooksonia was truly vascular• First definitive vascular plant: ferns
• Major events in the evolution of land plants– The Devonian Period was a time of rapid evolution for the land
plants
Plant Evolution
– the appearance of leaves
– and emergence of seeds
Early Devonian Plants• Reconstruction of an Early Devonian landscape
Dawsonites
Protolepidodendron
Bucheria
– showing some of the earliest land plants
• Early Devonian – relatively small – low-growing
– bog-dwelling types of plants
• Late Devonian – tree-size plants up to 10 m
tall
Early and Late Devonian Plants
Chaleuria cirrosa
• The evolution of the seed during the Late Devonian – liberated land plants from their dependence on moist
conditions – and allowed them to spread over all parts of the land
• In the seed method of reproduction– the spores are not released to the environment
– but are retained on the spore-bearing plant
– where they grow into the male and female forms
Evolution of Seeds
• In the case of the gymnosperms • or flowerless seed plants
– male cone produces pollen – egg is contained in the female cone– After fertilization
• seed develops into a mature, cone-bearing plant
• Seed plants • like reptiles
– were no longer restricted to wet areas – but were free to migrate into previously unoccupied dry
environments
Gymnosperms
• Rocks of the Pennsylvanian Period are the major source of the world's coal
• The geologic and geographic conditions of the Pennsylvanian – ideal for the growth of seedless vascular plants – these coal swamps had a very diverse flora
Late Carboniferous and Permian Floras
• Reconstruction of a Pennsylvanian coal swamp with its characteristic vegetation
Pennsylvanian Coal Swamp
• An important non-swamp dweller was Glossopteris, the famous plant so abundant in Gondwana (a seed fern)– Great resource for paleobiogeographers
Glossopteris
http://www.lowcountrygeologic.com/plants/gloss1.htm