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  2. Paleozoology - Wikipedia

    en.wikipedia.org/wiki/Paleozoology

    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.

  3. Paleobiology - Wikipedia

    en.wikipedia.org/wiki/Paleobiology

    Paleozoology uses the methods and principles of paleobiology to understand fauna, both vertebrates and invertebrates. See also vertebrate and invertebrate paleontology, as well as paleoanthropology. Micropaleontology applies paleobiologic principles and methods to archaea, bacteria, protists and microscopic pollen/spores.

  4. Paleontology - Wikipedia

    en.wikipedia.org/wiki/Paleontology

    The simplest definition of "paleontology" is "the study of ancient life". [5] The field seeks information about several aspects of past organisms: "their identity and origin, their environment and evolution, and what they can tell us about the Earth's organic and inorganic past".

  5. Category:Paleozoology - Wikipedia

    en.wikipedia.org/wiki/Category:Paleozoology

    Paleozoology — a subfield of paleontology and zoology for the study of prehistoric animals in paleobiology; Subcategories. This category has the following 4 ...

  6. Portal:Paleontology/Introduction - Wikipedia

    en.wikipedia.org/wiki/Portal:Paleontology/...

    The major subdivisions of paleontology include paleozoology (animals), paleobotany (plants) and micropaleontology (microfossils). Paleozoologists may specialise in invertebrate paleontology , which deals with animals without backbones or in vertebrate paleontology , dealing with fossils of animals with backbones, including fossil hominids ...

  7. Paleozoic - Wikipedia

    en.wikipedia.org/wiki/Paleozoic

    The Paleozoic (/ ˌ p æ l i. ə ˈ z oʊ. ɪ k,-i. oʊ-, ˌ p eɪ-/ PAL-ee-ə-ZOH-ik, -⁠ee-oh-, PAY-; [1] or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon. . Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Er

  8. History of invertebrate paleozoology - Wikipedia

    en.wikipedia.org/wiki/History_of_invertebrate...

    By far, invertebrate paleozoology is the easiest type of fossil collecting. Unlike the difficult-to-analyze and hard-to-interpret fossils of paleobotany (plants) and micropaleontology (microbes), and unlike the rarely found and poorly preserved skeletons of vertebrate paleontology , invertebrate fossils are usually both common and simple to ...

  9. Invertebrate paleontology - Wikipedia

    en.wikipedia.org/wiki/Invertebrate_paleontology

    Invertebrate paleontology (also spelled invertebrate palaeontology) is sometimes described as invertebrate paleozoology or invertebrate paleobiology. Whether it is considered to be a subfield of paleontology , paleozoology , or paleobiology , this discipline is the scientific study of prehistoric invertebrates by analyzing invertebrate fossils ...