Cretaceous–Paleogene boundary

KT boundary 054

Cretaceous–Paleogene boundary (K–Pg boundary), formerly known as the Cretaceous–Tertiary (K–T) boundary, is a geological signature, usually a thin band, marking the end of the Cretaceous period, approximately 66 million years ago. This boundary is significant for the mass extinction event that occurred during this time, leading to the demise of a large number of species, including all non-avian dinosaurs, marking the end of the Mesozoic Era and the beginning of the Cenozoic Era.

Overview

The K–Pg boundary is characterized by a distinct layer of sediment worldwide, which contains high levels of the rare earth element iridium. This anomaly is often associated with the impact of a large asteroid or comet, which is believed to have struck the Earth in the area of what is now the Yucatán Peninsula, at the Chicxulub crater. The energy released by this impact would have triggered global climate change, including a "nuclear winter" effect that significantly reduced sunlight reaching the Earth's surface, leading to a dramatic drop in temperature and photosynthesis.

Evidence

Evidence for the K–Pg boundary event includes the presence of tektites and shocked quartz in the boundary layer, indicative of an impact event, as well as the global iridium anomaly. Additionally, fossil records show a sudden mass extinction of many species coinciding with this boundary. The discovery of the Chicxulub crater, with its size and age matching predictions for the K–Pg impact event, has provided strong support for the impact hypothesis.

Consequences

The immediate consequences of the K–Pg boundary event were catastrophic for life on Earth. It is estimated that about 75% of all species, including most dinosaurs, went extinct. However, this event also paved the way for the rise of mammals and eventually the dominance of humans. The aftermath of the extinction saw the rapid evolution and diversification of surviving species, including the emergence of the first mammals that would go on to dominate the planet in the Cenozoic Era.

Research and Discovery

Research into the K–Pg boundary has involved multiple disciplines, including geology, paleontology, and astrobiology. The integration of evidence from different fields has been crucial in piecing together the events surrounding the boundary. The study of the K–Pg boundary continues to evolve, with new technologies and methodologies shedding light on the complexities of this pivotal moment in Earth's history.

Impact on Science and Culture

The K–Pg boundary event has had a profound impact on science, particularly in the fields of geology, paleontology, and evolutionary biology. It has also captured the public imagination, illustrating the vulnerability of life on Earth to catastrophic events and the dynamic nature of the planet's history.

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