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It is derived from the Greek palaiós (παλαιός, "old") and zōḗ (ζωή, "life") meaning "ancient life". [6] The Paleozoic was a time of dramatic geological, climatic, and evolutionary change.
Palaeozoology, also spelled as Paleozoology (Greek: παλαιόν, palaeon "old" and ζῷον, zoon "animal"), is the branch of paleontology, paleobiology, or zoology dealing with the recovery and identification of multicellular animal remains from geological (or even archeological) contexts, and the use of these fossils in the reconstruction of prehistoric environments and ancient ecosystems.
Paleozoic rocks include conglomerate, sandstone, siltstone, tuff and limestone. Carbonate nerite deposited in the Triassic, together with bauxite and an ophiolite nappe was thrust to the west. Cretaceous limestones are the top unit, the Zone of Eastern Greece is overthrust onto external zones (which appear as tectonic windows).
The Carboniferous (/ ˌ k ɑːr b ə ˈ n ɪ f ər ə s / KAR-bə-NIF-ər-əs) [6] is a geologic period and system of the Paleozoic era that spans 60 million years from the end of the Devonian Period 358.86 Ma (million years ago) to the beginning of the Permian Period, 298.9 Ma.
Definition; Chronological unit: Eon: ... deriving from the Ancient Greek words ... The Paleozoic is a time in Earth's history when active complex life forms evolved ...
The definition of standardised international units of geological time is the responsibility of the ... Paleozoic (old life ... From Greek φανερός ...
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The name is a combination of the Ancient Greek παλαιός palaiós meaning "old" and the Eocene Epoch (which succeeds the Paleocene), translating to "the old part of the Eocene". The epoch is bracketed by two major events in Earth's history.