3 Cambrian to Cretaceous Flashcards

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1
Q

Marine Radiation of Fishes - Paleozoic

A

Cambrian saw the origin of Chordates

450-420MYA - jawed fish radiation ‘Gnathostomata’

Fish are split into 2 main groups - chrondricthyes = cartilaginous fish / osteichthyes = bony fish (sub groups - actinopterygii = lobe finned fish / sarcopterygii = lung fish)

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2
Q

Enabling feature for jawed fish radiation - genome duplication

A

Early chordates had 2 genome duplication events

4 Hox gene clusters

Enables morphological complexities (jaws, limbs) —> Devonian

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3
Q

Jawless fish to jawed fish timeline

A

100 MYA of stasis as ‘jawless fish’

Genome duplication enables complexity

Radiation of jawed fish and later tetrapods

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4
Q

The Greening of the Land - Paleozoic

A

Land plant life cycle evolved from algal plants

In algae most of their life is spent in the diploid cell

Large change is the diploid phase

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5
Q

Bryophytes - the early land plants (liverworts and mosses)

A

Long haploid phase, short diploid

No vascular tissue

Don’t requre soil

Evidence by fossilised sporangia

Mosses also evolves stomata (gas and water regulation)

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6
Q

Land plants accompanies by terrestrial fungi

A

Evolution of desiccation-resistant fungal hypha from aquatic form

Hypothesised fungi enabled plant life on land through symbiosis

Fungal plant interactions essential for many bryophytes

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7
Q

Plant death —> organic bearing terrestrial soil

A

Creates soil = breakdown of plant matter (fungal, microbial action) / soil enables the growth of larger plants

Bryophytes don’t need soil but do create soil

Paleo soil in the Devonian

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8
Q

Vascular Plants (Devonian)

A

Phloem / xylem transport system

Bifurcating (branching) growth / increased size through lignification

Leaves and fronds —> above ground photosynthetic surfaces / evolved on multiple occasions

Vascular plants result in richer soil - PO4 / NO3 are fuel for plant growth (but may have poisoned oceans via eutrophication)

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9
Q

Devonian Mass Extinction

A

75% in 3 million years (many taxa disappear)

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10
Q

Land plant evolution accompanies by terrestrial arthropods

A

First insects - flightless / derived from Crustacea (in silurian)

Devonian - winged formed (+ millipedes / aranaea spiders)

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11
Q

The Carboniferous - Paleozoic (age of coal)

A

Carboniferous rocks —> appearance of organic rich deposits

Coal beds have abundant plant and other fossils - large woody plants appear, alongside large ferns / derived from lowland marsh and wetland

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12
Q

Paleozoic - Why did the increased deposition of organic carbon occur

A

Tall woody plants had become dominant —> wood Is rigid and plants can grow tall due to lignin = complex carbohydrate, decomposes much more slowly which results in more organic carbon buried and coal strata

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13
Q

Palaeozoic - Impacts of high oxygen levels

A

Biological consequences —> insect giganticism (aerobic respiration is more efficient —> more growth)

O2 limits body size where diffusion supports gas exchange —> O2 content of water increases with latitude and decreases in saltwater —> larger fish found in cooler oceans

Fire - 10-20% of coal beds are charcoal based (common) wildfires

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14
Q

Paleozoic- Carboniferous also saw radiation of tetrapods

A

Warm, wet climate, green terrestrial biome enables movement out of water

Amphibian lifestyle - still linked to laying eggs in water

Closest ancestors - lobe finned fish

Giganticism also seen in amphibian - dominated predators of the Carboniferous

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15
Q

The Permian

A

Rise of reptiles and the Permian mass extinction

End of the Carboniferous / eaely Permian saw a period of drying —> one large land pass (Pangea)

This drying makes a poor environemnt for amphibians —> selection for water retention

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16
Q

Adaptations of reptiles for life away from water (4)

A
  1. Amniotic egg
  2. Keratinous scales
  3. Alteration in excretion
  4. Internal fertilisation
17
Q

Adaptations of reptiles for life away from water - amniotic egg

A

zygote in fluid filled cavity / chorion and shell - able to gas exchange but retains water

18
Q

Adaptations of reptiles for life away from water - keratinous scales

A

water impermeable skin

19
Q

Adaptations of reptiles for life away from water - alteration in excretion

A

uric acid / utilise arid landscape areas

20
Q

Adaptations of reptiles for life away from water - internal fertilisation

A

Reproduction on land necessitates transition to internal fertilisation

21
Q

Permian also saw the rise of metamorphosing insects

A
  1. Hemimetabolous development
  2. Holometabolous development
22
Q

The Permian mass extinction

A

End of the Permian saw largest mass extinction event in fossil record ‘The Great dying’

23
Q

Causes of the Permian Mass Extinction

A
  1. Occurred at the same time as very high volcanic activity in Siberia
  2. Massive SO2, CO2 release
  3. Ocean acidification
  4. Reduced primary productivity
  5. Death of consumers
24
Q

Does mass extinction hit evenly

A

No - in general large things die out more than small things and non-motile things die out more than motile things

25
Q

The Mesozoic

A

Age of dinosaurs origins of birds, mammals (and flowers)

252-66 MYA

26
Q

Why cant DNA be used to reconstruct biology of dinosaurs

A

The DNA is decomposed

27
Q

Scientists study the new remains to determin relationshios to other known species and genera

A

Comparisons are made between these and living animals —> reconstruct skeleton and lifestyle

Aspects such as size, movement, weight and shape can also be determined

Can also look at trackways of footprints and use principles of anatomy and biomechanics -> movement and running speed

28
Q

Thermal biology

A

SA/V ratio - retained heat - can’t tell behaviour (eg. Basking or metabolism) - try to use species today to infer what their behaviour was likely to be

Current idea is that dinosaurs were both endothermic and edothermic

29
Q

What does brain size indicate

A

Indicates cognitive complexity - birds and mammals have complex cognitive capacity

30
Q

Origin of mammals

A

220 MYA

Derived from synapsids (non-dinosaur reptiles, no living examples) / mammals remained a minor taxa during the age of the dinosaurs

31
Q

Origin of birds

A

160 MYA

Evolved from theropod dinosaurs during the Jurassic (165-150MYA)

Classic small, lightweight, feathered and winged body plan —> evolved over tens of millions of years of evolution rather than one burst of innovation

Many non-avian dinosaurs had feathers

32
Q

Origin of Angiosperm (flowering plants)

A

130 MYA

First fossils 130MYA —> fast growing compared to gymnosperms (conifers)

Initially wind pollinated / insect pollination (110 MYA)

33
Q

Origin of Plant and insect diversification

A

Massive plant diversification 100-70MYA —> resulted in 250k species today

Loss of gymnosperms in the tropics

Diversification in beetles

34
Q

Plants and their herbivores escape and radiate process

A

Plant group —> novel defences —> escaped herbivores colonise new niches —> radiates —> herbivore that establishes onto that group (creates large number of new niches that then radiate again and REPEAT)