The Permian Triassic Extinction Event

Slides:



Advertisements
Similar presentations
Greenhouse effect. Our climate system (atmosphere, lithosphere, hydrosphere and living things) trap and store energy and distribute it around the world.
Advertisements

Crisis at the end of the Permian: global change and the greatest mass extinction in the history of life Pedro J Marenco Bryn Mawr College Department of.
Extinctions and how to change diversity 1. Sepkoski’s Curves and others. 2. How to change diversity 3. Models of diversity increase 4. Perturbations to.
Lecture 29: Mass Extinctions. X X X X X X X X Phanerozoic Mass Extinctions biodiversity Mississippian Pennsylvanian Ma Jurassic Cambrian.
Mass Extinction By Joe Baraona. What is Mass Extinction? “The extinction of a large number of species within a relatively short period of geological time,
Jacksury Puerta. Extinction is the process by which a species become extinct, no longer existing and living in the world. Extinction is a normal part.
Check web page: Updated study questions & HW #1!.
The Sixth Extinction.  A mass Extinction is:  - When at least half of all species (including animals and plants) die within a relatively short time.
Part 3 Climate Change Basics and Past Climates. The Greenhouse Effect.
A history including how life evolved, how the geosphere changed and major extinction events.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 2 Historical Geology Reference: Chapters 6, 8; Appendix.
Triggers for the Late Ordovician Ice Age: Volcanic Aerosols vs. CO 2 Konrad Cunningham UG Eric Santiago HSS Linda Sohl PI Mark Chandler PI.
INTRODUCTION CAUSES CONSEQUENCES SOLUTIONS Golbal warming refers to the increase in the average temperature of the Earth. The increase resulting from.
Speciation The process by which one species splits into two or more species.

Objective: Learn the Causes and Effects of Mass Extinctions 1. What does “extinction” mean? 2. What is the rate of extinct species in the planet? 3. What.
Today  Hand in any work needed.  Get out a small piece of paper, PUT YOUR NAME ON IT.  When bell rings the quiz will start and you will have 1 minute.
PALEOZOIC ERA (542 Mya Mya) Andrea Villalba, Fabiola Ferrabone, Alfredo de Obaldia, Nicole Cortez.
Global Climate Change: The Evidence Presentation by: Rosa Jaime.
Thurs, Nov 17 th CW: Geologic Time HW: Study for quiz Why are there no fossils in layer F?
21.3 Climate Change. Natural Processes That Change Climate Volcanic eruptions The presence of volcanic ash, dust, & aerosols in the air increases the.
Greenhouse Effect Mechanisms Affecting the Greenhouse Evidence for Climate Change.
 Abiotic: nonliving parts  Biotic: living parts When these factors are altered in some way the ecosystem is affected.
Carbon cycle and Human activity. Carbon cycle Carbon cycles though the atmosphere, living things, soils, and the ocean.Carbon cycles though the atmosphere,
Fundamentals Atmosphere Climate Variation Greenhouse Effect Climate Drivers Carbon Cycle Energy Balance System Inertia Geologic time Causes of Climate.
Trissic period Ethan guest. Environment 251 mya to 199 mya. The start of the Triassic period (and the Mesozoic era) was a desolate time in Earth's history.
Global Warming. What is Global Warming? Global warming is an increase in both land and sea temperatures. Global warming is caused by an increase of CO2.
Elizabeth L. A. Deschner Monique P. V. Viens The Triassic Period.
Earth Timeline. When did these events occur? 1. Find a length of register tape and label it “Earth’s Timeline” 2. Write 4.56 billion years ago on one.
History of the Earth RYAN SULLIVAN 10TH GRADE GEOLOGY Start Lesson.
Evolution. Adaptive Radiation The speciation and adaptation of an array of species Species show different morphological and physiological traits.
Earth History.
Climate Change and Human Impact. Many natural processes cause climate change Volcanic eruptions – volcanic ash and dust in the atmosphere reflect solar.
Earliest life forms were influenced by: The forming atmosphere and oceans Volcanic activity Mountain building Influence of Catastrophes on Earth’s History.
Global Warming Vs Climate Change
P337\Section 4 Geologic Time Scale. 1a How long ago did the Earth form? 4.6 billion years ago.
17-3 Evolution of Multicellular Life How multicellular life evolved from its earliest forms to its present day diversity.
Climate Change Overview: Key Concepts. Climate vs. Weather What is weather? – Conditions of the atmosphere over a short period of time (e.g. day- to-day).
Precambrian Times Occurred from 4.6 BYA to 542 MYA The period of Earth history known as the “Precambrian Times” is broken up into three eons, which are.
For this topic, read the supplemental notes below then read p and answer the questions below:
Mass extinction and Ecological turnovers at the Permian-Triassic boundary (PTB): causes and effects. Barash M.S. (P.P. Shirshov Institute of Oceanology,
Precambrian Times Occurred from 4.6 BYA to 542 MYA The period of Earth history known as the “Precambrian Times” is broken up into three eons, which are.
The Five Worst Extinctions in Earth's History. Ordovician-Silurian extinction about 439 million years ago, caused by a drop in sea levels as glaciers.
Greenhouse Gases: Effects of Warming Emerson Middle School.
Do you think Global Warming is happening?
Human Impacts on Climate
Mass Extinctions in Geologic History
The Earth’s History extinct (def.) – no longer existing on earth
Evil twin of Climate Change
The geologic time scale
Modelling Ancient Earth Climates Manchester Geologist Association
DO NOW Pick up notes and Review #6 Turn in Review #5.
East middle School Climate Change
Chapter 15.
Composition and evolution of the atmosphere
Mass Extinctions.
Time, Life, Soil, Rocks, Ice
The Carbon Cycle.
History of our Earth Geologic Time Scale.
The Permo-Triassic Mass Extinction
History of Life on Earth
The Geologic Time Scale
Mass Extinctions.
Learning Intention: 8.ESS2.1
Air Pollution and Global Warming
The Human Factor.
Greenhouse Gases: Changing the Climate
CLIMATE.
Global annual average temperature (as measured over both land and oceans) has increased by >1.5°F (0.8°C) since 1880 (through 2012). Global annual average.
Presentation transcript:

The Permian Triassic Extinction Event The role of Global Warming in the PTEE Evelin Collado and Matthew Moline

Introduction 251 million years ago Up to 92% of species became extinct. What role did Global Warming play in this crisis?

PTEE Mechanisms CO2 Increase Ocean Circulation Storm Activity Anoxia Volcanism Hypercapnia Methane Release Bolide Impact

Comparison Early Permian Late Permian Early Triassic Modern Era Atmospheric CO2 350 ppm 3550 ppm 11,360 ppm 385 ppm Annual CO2 increase 0.0 ppm .016 ppm .039 ppm 2.0 ppm Average Temperature 15°C 25°C 30°C 14.54°C Avg. Temp. Increase 0°C 5.0 x 10-5°C 2.5 x 10-5°C 2.0 x 10-2°C Early Permian and Modern Era are similar Late Permian: Siberian Traps erupt Early Triassic: Additional Kill Mechanisms

Conclusion Global Warming was a critical component of the most profound extinction event of the last 600 million years. HOWEVER Atmospheric CO2 is currently increasing 100x faster than during the PTEE Temperature is currently increasing 660x faster than during the PTEE