Search results
Results from the WOW.Com Content Network
Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the fossil record. Though the fossil record is incomplete, numerous studies have demonstrated that there is enough information available to give a good ...
The trackway Protichnites from the Cambrian, Blackberry Hill, central Wisconsin. A trace fossil, also known as an ichnofossil (/ ˈ ɪ k n oʊ f ɒ s ɪ l /; from Greek: ἴχνος ikhnos "trace, track"), is a fossil record of biological activity by lifeforms but not the preserved remains of the organism itself. [1]
The prehistoric bones of the spinosaurid were found in a geological layer of rock known as the Vectis Formation in Compton Chine, it is the first identifiable theropod from the Vectis Formation. The study was led by Christopher Barker, a PhD doctoral student in vertebrate paleontology at the University of Southampton .
Paleontology (/ ˌ p eɪ l i ɒ n ˈ t ɒ l ə dʒ i, ˌ p æ l i-,-ən-/ PAY-lee-on-TOL-ə-jee, PAL-ee-, -ən-), also spelled palaeontology [a] or palæontology, is the scientific study of life that existed prior to the start of the Holocene epoch (roughly 11,700 years before present).
The history of paleontology traces the history of the effort to understand the history of life on Earth by studying the fossil record left behind by living organisms. Since it is concerned with understanding living organisms of the past, paleontology can be considered to be a field of biology, but its historical development has been closely tied to geology and the effort to understand the ...
A skeleton in a bioarchaeology lab. Paleodemography studies demographic characteristics of past populations. [5] Bioarchaeologists use paleodemography to create life tables, a type of cohort analysis, to understand zdemographic characteristics (such as risk of death or sex ratio) of a given age cohort within a population.
The iconic Altar Stone at the center of Stonehenge in southern England was likely moved over hundreds of miles nearly 5,000 years ago, according to new research.
Plant roots normally remove calcium from soil while lowering its pH, by exchanging H + ions for Ca 2+, Mg 2+, K +, and other cations. [11] This contributes to the ability of roots to bore through rock, but it works against precipitation of calcite around roots. Several explanations have been offered for how rhizoliths are nonetheless able to form.