Chapter 12 Geologic Time - PC\|MAC

Chapter 12 Geologic Time - PC\|MAC

CHAPTER 12 GEOLOGIC TIME SECTION 12.1 DISCOVERING EARTHS HISTORY Uniformitarianism the idea that physical, chemical, and biological laws that operate today also operated in the

past; the present is the key to the past. James Huttons work was the basis for the science of geology. He was a Scottish physician and farmer in the 1700s. He is known as the father of geology. STENOS THE LAW OF SUPERPOSITION Relative Dating simply tells you which rock layers formed first,

second, third, etc. It does not give you an exact age. Law of Superposition in an undisturbed sequence of sedimentary rock, each layer is older than the one above it and younger than the one below it. (Oldest are on the bottom and the youngest on top.) GEOLOGIC PRINCIPLES Stenos Principle of Original Horizontality sediment is

deposited in flat, horizontal layers. Principle of Cross-Cutting Relationships a fault or intrusion must by younger than the geologic formation through which it cuts. UNCONFORMITIES A BREAK IN THE ROCK RECORD

Angular Unconformity layers of sedimentary rock form over older layers that are tilted and folded. UNCONFORMITIES A BREAK IN THE ROCK RECORD Disconformity two sedimentary rock layers are separated by

an erosional surface. UNCONFORMITIES A BREAK IN THE ROCK RECORD Nonconformity an erosional surface separates older metamorphic or igneous rocks from younger sedimentary rocks.

CORRELATION Correlation the process of matching rocks layers at different locations that formed at the same time and by the same processes. Scientists correlate rock layers at different locations to piece together a more complete interpretation of the rock

record. Scientists must sometimes rely on fossils to complete the correlation. CORRELATION SECTION 12.2 FOSSILS: EVIDENCE OF PAST

LIFE Extinct all members of a species have died on Earth. Fossil the preserved remains or traces of an organism. There are many different types of fossils which include petrified fossils, molds and casts, compressions, impressions, unaltered remains, and trace fossils.

TYPES OF FOSSILS Petrified Fossils organic remains are replaced by minerals over a long period of time. Molds when a shell or hard part of an organism gets buried in sediment and decays leaving an empty cavity behind in the rock which details the outside of the structure. Casts when the empty cavity of a mold fills with mud or minerals and

hardens. TYPES OF FOSSILS Compression Fossils 2D organic remains. Thin film of carbon left behind by an organism. Impression Fossils 2D fossils that do not contain organic matter. They show fine details of the external structure of the organism.

Unaltered remains when parts or whole organisms are frozen, trapped in tar seeps, or trapped in amber (tree sap). Trace fossils footprints, burrows, coprolites (fossilized dinosaur dung), and gastroliths (polished stomach stones of dinosaurs). COMPRESSION FOSSILS

IMPRESSION FOSSILS UNALTERED REMAINS TRACE FOSSILS THE FOSSIL RECORD

All the fossils found, arranged by their relative ages, make up the fossil record. Two conditions that favor preservation of a fossil rapid burial and hard parts. Fossil succession fossil organisms tend to found in the same general order at different locations on Earth. Index fossils fossil that was geographically widespread and abundant

in the fossil record, but existed for only a limited span of time. Fossils can help build detailed pictures of past environments. FOSSILS AND EVOLUTION Fossils provide evidence of evolution. Evolution change in organisms over time. Darwins Natural Selection traits that improve an individuals chance

of survival and reproduction will be passed on more frequently to future generations than traits that do not. (survival of the fittest) Adaptations beneficial traits SECTION 12.3 DATING WITH RADIOACTIVITY Radioactivity unstable atomic nuclei spontaneously break apart, or

decay, releasing energy. Radioactive isotopes elements with more neutrons than normal. They will decay from their parent isotopes into daughter products until stability is reached. Uranium 238 decays over millions of years until it eventually turns into Lead 206. Half Life the amount of time necessary for one half of the nuclei in a sample of radioactive isotope to decay to its stable isotope.

RADIOMETRIC DATING Method of calculating the absolute age, or exact age, of rocks and minerals that contain certain radioactive isotopes. Scientists measure the ratio between the radioactive parent isotope and the daughter products in a sample to be dated. The older the sample, the more daughter product it contains.

Radiometric Dating of rocks and minerals now have the age of the Earth to be at least 4.6 billion years old. DATING WITH CARBON-14 Carbon-14 is used to date organic materials in a method called radiocarbon dating. When an organism dies, the amount of carbon-14 gradually decreases

as the carbon-14 decays. By comparing the ratio of carbon-14 to carbon-12 in a sample, radiocarbon dates can be determined. SECTION 12.4: THE GEOLOGIC TIME SCALE Geologic time scale a record that includes both geologic events and major developments in the evolution of life. Eons represent the longest intervals of geologic time. Eons are divided

into eras. Each era is subdivided into periods. Finally, periods are divided into still smaller units called epochs. We live in the Phanerozoic Eon, Cenozoic Era, Quaternary Period, and Holocene Epoch. THE GEOLOGIC TIME SCALE Eons - there are 4 total. 88 percent of geologic time is made up of

the 1st three eons ( Hadean, Archean, Proterozoic), which are all included in Precambrian time. The Phanerozoic is the current eon. Precambrian time the Earth formed, the atmosphere and oceans developed, and early life evolved. Eras there are 3 eras within the Phanerozoic eon (Paleozoic, Mesozoic, and Cenozoic)

THE GEOLOGIC TIME SCALE Periods characterized by geologic events, environmental conditions, and life forms. Epochs a smaller unit of a period. The Cenozoic Era is divided into periods and epochs due to the abundant fossil record of the recent past.

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