Things are as they are because they were as they were.
Summary of Life from Paleozoic to Cenozoic
Arthropods
Eurypterids and Trilobites (become extinct)Brachiopods
Insects, etc.
Abundant, decline at end of PaleozoicEchinoderms
Commonly stemmed (blastoids, crinoids), now mostly extinctMollusca
AmmonitesOther groups, not placed in phyla
Gastropods and Bivalves not especially important
GraptolitesPermian extinctions (80% of species)
Conodonts
Archaeocyathids (formed reefs)
Fusilinids (formed reefs)
All of the above are now extinct
CoralsTriassic extinctions
Bryozoans
Brachiopods
Crinoids
Trilobites
ConodontsThe survivors diversify in the Jurassic and Cretaceous:
More coral groups
Clams, particularly oyster-typesCretaceous extinctions
Inoceramus (index fossil for the Jurassic)Ammonites
Gryphaea
Rudistids
Belemnites
AmmonitesNew on the scene in Cretaceous
Belemnites
Major microrganism groups
Large reptiles of nearly every type, in air, water or on land
Flowers (Angiosperms)
Diatoms
Useful links:
Earth Science Picture of the Day
Return to Historical Geology syllabus