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middle paloezoic

Quiz yourself by thinking what should be in each of the black spaces below before clicking on it to display the answer.
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Question
Answer
Taconic land eroded flat   Silurian  
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transgression   Phase 1  
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abundant salt deposits developed ~500 m thick   Phase 1  
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shallow epicontinental seas   Phase 1  
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eastern US and Europe   Acadian orogeny  
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in Europe the equivalent event   Caledonian orogeny  
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collision first in the north - then migrated south   Phase 2  
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regression   Phase 2  
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Late Devonian - expressed in Nevada rocks   orogenic activity  
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western US (small scale event)   Antler orogeny  
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2. off shore sediments and island arcs thrust on land   Antler orogeny  
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D. Climate relatively warm through the Silurian to the later Devonian   Antler orogeny  
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high latitude cooler temperatures during the   Devonian  
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global climate deteriorated toward the Earth   carboniferous  
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glaciation started   Famennian- latest devonian  
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necessary before animals can live on land   Silurian Life land plants  
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rigid stalk or stem as a support system   Silurian plants  
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vascular systems to distribute nutrients   Silurian plants  
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leaves to increase surface area   Silurian plants  
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reproduction using spores   Silurian plants  
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require warm climates   major reef complexes  
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corals   major reef complexes  
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stromatoporoids and tabulates   major reef complexes  
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dominant predator, to 2 meters in size   eurypterid  
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major diversity of brachiopods   Silurian life  
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nautiloids and crinoids abundant   Silurian life  
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fauna flourishing   Ordovician  
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trilobites recovery limited   Late Ordovician extinction  
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major fish adaptive radiation   vertebrates  
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(bony skin fish) in fresh water deposits   ostracoderms  
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no jaws   ostracoderms  
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armored   ostracoderms  
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acanthodians (fish) marine and fresh water   acanthodians  
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fins and spines   acanthodians  
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scales and jaws   acanthodians  
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generally mud-grubbers   acanthodians  
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a root system to collect nutrients   Early Devonian plants  
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reproduction using spores   Early Devonian plants  
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restricted to damp habitats   Early Devonian plants  
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branching root systems   Middle Devonian  
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first forests   Middle Devonian  
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plants widely spread over land   Middle Devonian  
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most primitive gymnosperms   Middle Devonian  
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first seeds   Middle Devonian  
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liberated plants from moist habitats   Middle Devonian  
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pollen for reproduction   Middle Devonian  
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trees occupied land for the first time   Late Devonian  
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spore plant; first tree (30 m)   Archaeopteris  
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due to broad leaves to capture sunlight   Archaeopteris  
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swimming predators   ammonites  
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(Lower Devonian)   Emsian Stage  
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spiny brachiopods   Emsian Stage  
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conodont high point   Emsian Stage  
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animals move on land   Early Devonian  
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scorpions   Early Devonian  
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flightless insects   Early Devonian  
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main guide fossil for GSSPs   conodonts  
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Age of the Fishes   Devonian  
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sharks   cartilagenous  
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rays   cartilagenous  
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most successful fish   bony  
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lobe finned fish   bony  
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direct line to land vertebrates   lobe finned fish  
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endo-skeleton - most important   lobe finned fish  
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muscular   lobe finned fish  
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most fresh water   lobe finned fish  
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coelacanths invaded oceans   lobe finned fish  
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only remaining relative alive   coelacanths  
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includes lungfishes   lobe finned fish  
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dominant in later Phanerozoic   ray finned fish  
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Late Devonian - land vertebrates   Amphibians  
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reason: competition in water was fierce   Amphibians  
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lobe finned fish out of water; had a lung   Amphibians  
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converted into a walking limb   fin  
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found in Greenland rocks; ~60 cm long   ichthyostega  
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limited by need of water for reproduction   ichthyostega  
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classed by backbone structure   ichthyostega  
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- due to necessary support against gravity   ichthyostega  
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- one of five greatest in Earth history - maybe   Late Devonian Mass Extinction  
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occurred at the Frasnian-Famennian stage boundary   Late Devonian Mass Extinction  
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cause unknown - perhaps due to Greenhouse cooling   Late Devonian Mass Extinction  
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- resulting from CO2 reduction in the atmosphere by forests   Late Devonian Mass Extinction  
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further extinctions due to glaciation   D-C boundary  
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Land plants abundant; Trees in the Devonian   Plants  
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intense competition from predators   Invertebrates  
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trending toward mobile forms   Invertebrates  
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Fish advanced; Amphibians on land   Vertebrates  
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