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Researchers find oldest rocks on Earth
Researchers find oldest rocks on Earth

... The oldest zircon dates are 4.36 billion years. Before this study, the oldest dated rocks were from a body of rock known as the Acasta Gneiss in the Northwest Territories, which are 4.03 billion years old. The Earth is 4.6 billion years old, and remnants of its early crust are extremely rare—most of ...
Slide 1
Slide 1

... of mud or sand that gradually turn into stone. Over time, the organism remains themselves may turn to stone, becoming preserved within the rock layer in which they came to rest. By measuring radioactivity in the rock in which a fossil is embedded, paleontologists (scientists who study the fossil rec ...
Reviewing Biology: The Living Environment
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... In studying undisturbed sedimentary rock, scientists assume that each layer is older than all the layers, or strata, above it. Thus, fossils in the lower strata are older than fossils in the overlying strata. Fossils in the upper strata of a sedimentary rock sample are generally more complex than fo ...
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... His idea was rejected when he was alive because he could not explain HOW it worked even though he provided evidence that the continents were moving. Pangea: This was a supercontinent around 300 million years ago. Wegener named this continent Pangea. Pangea began to break apart and the pieces moved t ...
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... species based on similarities and dierences in genetic or physical traits or both. A phylogenetic tree is composed of branch points, or nodes, and branches. The internal nodes represent ancestors and are points in evolution when, based on scientic evidence, an ancestor is thought to have diverged ...
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... 1. 200 million years ago, all the continents were one called Pangaea. Evidence is continents fitting together, fossils of same organism on two different continents, similar mountain ranges on diff. continents. 2. Seismic waves tell us that the inside of the Earth is made up of layers. 3. Continental ...
Week 11 – SEDIMENTARY ROCKS
Week 11 – SEDIMENTARY ROCKS

... iii. Organic debris: Broken up shells or decaying plant matter b. Sediment is produced by the UPLIFT, WEATHERING & EROSION of other rocks (yellow arrows in diagram above). c. The type and size of the sediment controls the texture of the rock. ...
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Paleontology



Paleontology or palaeontology (/ˌpeɪlɪɒnˈtɒlədʒi/, /ˌpeɪlɪənˈtɒlədʒi/ or /ˌpælɪɒnˈtɒlədʒi/, /ˌpælɪənˈtɒlədʒi/) is the scientific study of life existent prior to, and sometimes including, the start of the Holocene Epoch roughly 11,700 years before present. It includes the study of fossils to determine organisms' evolution and interactions with each other and their environments (their paleoecology). Paleontological observations have been documented as far back as the 5th century BC. The science became established in the 18th century as a result of Georges Cuvier's work on comparative anatomy, and developed rapidly in the 19th century. The term itself originates from Greek παλαιός, palaios, i.e. ""old, ancient"", ὄν, on (gen. ontos), i.e. ""being, creature"" and λόγος, logos, i.e. ""speech, thought, study"".Paleontology lies on the border between biology and geology, but differs from archaeology in that it excludes the study of morphologically modern humans. It now uses techniques drawn from a wide range of sciences, including biochemistry, mathematics and engineering. Use of all these techniques has enabled paleontologists to discover much of the evolutionary history of life, almost all the way back to when Earth became capable of supporting life, about 3,800 million years ago. As knowledge has increased, paleontology has developed specialised sub-divisions, some of which focus on different types of fossil organisms while others study ecology and environmental history, such as ancient climates.Body fossils and trace fossils are the principal types of evidence about ancient life, and geochemical evidence has helped to decipher the evolution of life before there were organisms large enough to leave body fossils. Estimating the dates of these remains is essential but difficult: sometimes adjacent rock layers allow radiometric dating, which provides absolute dates that are accurate to within 0.5%, but more often paleontologists have to rely on relative dating by solving the ""jigsaw puzzles"" of biostratigraphy. Classifying ancient organisms is also difficult, as many do not fit well into the Linnean taxonomy that is commonly used for classifying living organisms, and paleontologists more often use cladistics to draw up evolutionary ""family trees"". The final quarter of the 20th century saw the development of molecular phylogenetics, which investigates how closely organisms are related by measuring how similar the DNA is in their genomes. Molecular phylogenetics has also been used to estimate the dates when species diverged, but there is controversy about the reliability of the molecular clock on which such estimates depend.
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