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Historical geology or palaeogeology is a discipline that uses the principles and methods of geology to reconstruct the geological history of Earth. [1] Historical geology examines the vastness of geologic time, measured in billions of years, and investigates changes in the Earth , gradual and sudden, over this deep time .
Relative dating by biostratigraphy is the preferred method in paleontology and is, in some respects, more accurate. [1] The Law of Superposition, which states that older layers will be deeper in a site than more recent layers, was the summary outcome of 'relative dating' as observed in geology from the 17th century to the early 20th century.
Basic Palaeontology is a basic textbook on the study of paleontology written by the palaeontologists Michael J. Benton and David A.T. Harper, and published by Prentice Hall in 1997. It was described in a 1998 review by palaeontologist Mark Purnell as being uniquely inclusive in its coverage of the subject, going into detail about the history of ...
The simplest definition of "paleontology" is "the study of ancient life". [7] 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".
Jean Léopold Nicolas Frédéric, baron Cuvier (23 August 1769 – 13 May 1832), known as Georges Cuvier (/ ˈ k j uː v i eɪ /; [1] French: [ʒɔʁʒ(ə) kyvje]), was a French naturalist and zoologist, sometimes referred to as the "founding father of paleontology". [2]
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.
In archaeology and paleontology a faunal assemblage is a group of animal fossils found together in a given stratum. [1] In a non-deformed deposition, fossils are organized by stratum following the laws of uniformitarianism [2] and superposition, [3] which state that the natural phenomena observable today (such as death, decay, or post-mortem transport) also apply to the paleontological record ...
Paleontology – Study of life before the Holocene epoch; Petroleum geology – Study of the origin, occurrence, movement, accumulation, and exploration of hydrocarbon fuels; Petrology – Branch of geology that studies the formation, composition, distribution and structure of rocks