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Cambrian

541-485 M.a.

Cambrian derives its name from rock outcrops in an area of the United Kingdom which the Romans called Cambria.
Mapamundi

Pannotia has broken up into four continents: Laurentia (approximately America and Greenland), Baltica (approximately Northern Europe), Siberia and Gondwana. The latter is a supercontinent containing South America, Africa, India, Australia, Antarctica and much of Asia and Europe, including the Iberian Peninsula.


In a short period of time, in geological terms, an explosion of life occurs. The main groups of marine invertebrates appear: arthropods, molluscs, brachiopods, annelids and the first jawless vertebrates, among others. Many of them fossilise well because they have shells and have left us characteristic fossils like trilobites or archaeocyathids.


Opabinia a marine arthropod specimen
Opabinia, a marine arthropod specimen.
Cambrian fauna.
Reproduction of Cambrian fauna.

Hadean ~4600-4000 M.a.
Archean 4000-2500 M.a.
Proterozoic 2500-541 M.a.
Cambrian 541-485 M.a.
Ordovician 485-443 M.a.
Silurian 443-419 M.a.
Devonian 419-359 M.a.
Carboniferous 359-299 M.a.
Permian 299-252 M.a.
Triassic 252-201 M.a.
Jurassic 201-145 M.a.
Cretaceous 145-66 M.a.
Paleogene 66-23 M.a.
Neogene 23-2,6 M.a.
Quaternary 2,6 M.a.-act.


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