Lesson 9: Stratigraphy and Geologic Time Flashcards
The tendency for rock layers to be chronologically stacked is called the ___ ___ ___.
Principle of Superposition.
What is stratigraphy?
Stratigraphy is the science of using the arrangement and composition of rock layers to interpret geological history.
What is a formation?
A large uninterrupted sequence of rock that is made of multiple layers that all share similar properties (such as mineral composition and average sediment grain size) and that all formed under similar conditions is termed a formation.
The Principle of Superposition allows a stratigrapher to infer the relative age of rock layers (that is, how old one layer is relative to another), but it does not determine the absolute age (that is, how old in years the layers are). To age rocks in absolute terms, a technique called radiometric dating is used. Describe radiometric dating.
When a new rock forms, it has a ratio of isotopes and decay products that matches that of the environment. As the rock ages, the isotopes decay and the ratio of isotopes to decay products decreases. Using a special machine called a mass spectrometer, it is possible to measure the isotope ratio of a rock, and this ratio can tell you how long ago the rock formed.
What is the geological timescale?
The geologic time scale is a standardized series of chronological divisions that parses the Earth’s history into discrete named units. The largest units in the time scale are Eons, followed by Eras, Periods, and Epochs.
Describe THE HADEAN EON – 4.6 TO 4 BILLION YEARS AGO.
- The surface of the earth partially molten and with volcanic activity widespread.
- At roughly 4.5 billion years ago, the young earth collided with a smaller planetoid. Eventually formed the moon.
- By the end of the Hadean, the earth had cooled and large oceans covered much of its surface. Complex organic molecules are thought to have formed in these early oceans and possibly the earliest true life forms.
- The oldest rocks on earth have been dated at only about 4.4 billion years old, though rocks discovered on the moon are older.
Describe THE ARCHEAN EON – 4 TO 2.5 BILLION YEARS AGO.
- The oldest known fossils come from the Archean Eon. These fossils are of simple single-celled organisms.
- More advanced forms later evolved in the Archean, including cyanobacteria. The cyanobacteria were photosynthetic and eventually produced large amounts of oxygen gas, which became concentrated in the earth’s atmosphere. Some cyanobacteria formed structures called stromatolites, which are some of the best records of early life.
Describe THE PROTEROZOIC EON – 2.5 BILLION TO 541 MILLION YEARS AGO.
- At approximately 1.7 billion years ago, the first multicellular organisms evolved. Because single-celled and early multicellular life had no bones or other hard parts and was usually microscopic, the fossil record of this early life is poor.
- Within the Proterozoic, the time span from 630 to 542 million years ago is known as the Ediacaran Period. During the Ediacaran, large forms of life with some harder parts evolved, including the first animal life.
Describe THE PHANEROZOIC EON – 541 TO 0 MILLION YEARS AGO.
- The Phanerozoic Eon is subdivided into three eras, which are themselves subdivided into numerous periods.
- It is during the Phanerozoic that animal life rapidly evolved into a multitude of diverse forms, including dinosaurs.
Describe The Paleozoic Era – 541 to 252 million years ago.
-At the start of the Paleozoic, animal life was restricted to primitive invertebrates living in the oceans, but, by its close, great forests covered the land and teamed with reptiles, amphibians, and insects.
Describe The Cambrian Period – 541 to 485 million years ago.
- The beginning of the Cambrian marks such a dramatic diversification of aquatic animal life that it is often referred to as The Cambrian Explosion.
- Sponges, molluscs, worms, and many kinds of arthropods (including trilobites) evolved.
- A close early relative of the vertebrates, called Pikaia, didn’t have vertebrae, but had several other features found in vertebrates.
Refer to pg 4-5 of study guide for examples and pics of creatures from Cambrian explosion.
Refer to pg 4-5 of study guide for examples and pics of creatures from Cambrian explosion.
Describe The Ordovician Period – 485 to 443 million years ago.
- Global sea levels were high.
- Life in the oceans continued to diversify, with fish increasingly becoming the dominant large aquatic animals.
Describe The Silurian Period – 443 to 419 million years ago.
- Until this point, fish had not yet evolved jaws. With the evolution of jaws came the evolution of large predatory fish.
- Primitive plant life began to flourish on land.
Describe The Devonian Period – 419 to 359 million years ago.
- The first forests appeared on land.
- Huge jawed fishes, like Dunkleosteus, evolved in the seas, and the first true sharks appeared.
- Lobe-finned ‘fishapods’, like Tiktaalik, ventured onto land, and give rise to the tetrapods.