The Cretaceous-Paleogene (K-Pg) period, formerly known as the Cretaceous-Tertiary (K-T) period, is a geological time period that spans from approximately 145 million years ago to 66 million years ago. It is known for being the time when the dinosaurs went extinct, marking the end of the Mesozoic Era and the beginning of the Cenozoic Era.
Key Events and Characteristics
Dinosaurs Extinction: The most notable event of the K-Pg period is the mass extinction of the dinosaurs and many other species. This event is believed to have been caused by a combination of factors, including a massive asteroid impact and volcanic activity.
Geological Changes: The K-Pg boundary is marked by significant geological changes, including the formation of the Chicxulub crater in modern-day Mexico, which is believed to be the result of the asteroid impact.
Flowering Plants: The K-Pg period saw the diversification and spread of flowering plants, leading to the development of diverse ecosystems and the evolution of new plant and animalspecies.
Marine Life: Many marinespecies, including ammonites and marine reptiles, also went extinct during this period, while others diversified and evolved to fill the ecologicalniches left vacant by the extinction event.
Study Guide
If you're studying the Cretaceous-Paleogene period, here are some key points to focus on:
What are the major events that occurred during the K-Pg period?
How did the extinction of the dinosaurs impact the Earth'secosystems?
What geological evidence supports the theory of an asteroid impact at the K-Pg boundary?
Be sure to review the geological, paleontological, and ecological evidence related to the K-Pg period, as well as the theories and hypotheses proposed to explain the mass extinction event that occurred during this time.
The student demonstrates an understanding of geochemical cycles by describing that most smaller rocks come from the breaking and weathering of larger rocks as part of the rock cycle.
The student demonstrates an understanding of geochemical cycles by recognizing the physical properties of water as they relate to the rock cycle.