the study of fossil animals
The branch of zoology dealing with fossils, and the creatures that were transformed into them
the Paleozoic time or strata
Origin: [Paleo- + Zoology.]
Palaeozoology, also spelled as Paleozoology, is the branch of paleontology, paleobiology, or zoology dealing with the recovery and identification of multicellular animal remains from geological contexts, and the use of these fossils in the reconstruction of prehistoric environments and ancient ecosystems. Definitive, macroscopic remains of these metazoans are found in the fossil record from the Ediacaran period of the Neoproterozoic era onwards, although they do not become common until the Late Devonian period in the latter half of the Paleozoic era. Perhaps the best known macrofossils group is the dinosaurs. Other popularly known animal-derived macrofossils include trilobites, crustaceans, echinoderms, brachiopods, mollusks, bony fishes, sharks, Vertebrate teeth, and shells of numerous invertebrate groups. This is because hard organic parts, such as bones, teeth, and shells resist decay, and are the most commonly preserved and found animal fossils. Exclusively soft-bodied animals—such as jellyfish, flatworms, nematodes, and insects—are consequently rarely fossilized, as these groups do not produce hard organic parts.
The numerical value of paleozoology in Chaldean Numerology is: 5
The numerical value of paleozoology in Pythagorean Numerology is: 2
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"paleozoology." Definitions.net. STANDS4 LLC, 2017. Web. 19 Nov. 2017. <http://www.definitions.net/definition/paleozoology>.