1 / 20

Erica Shook Honors Climate Change Biology- NCSSM Online 20 December 2011

The PETM and Leaf Margin Analysis: How does the PETM and Leaf Margin Analysis Relate to Climate Change we are facing today?. Erica Shook Honors Climate Change Biology- NCSSM Online 20 December 2011. What is the PETM?. PETM stands for Paleocene Eocene Thermal Maximum .

sissy
Download Presentation

Erica Shook Honors Climate Change Biology- NCSSM Online 20 December 2011

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. The PETM andLeaf Margin Analysis:How does the PETM and Leaf Margin Analysis Relate to Climate Change we are facing today? Erica Shook Honors Climate Change Biology- NCSSM Online 20 December 2011

  2. What is the PETM? • PETM stands for Paleocene Eocene Thermal Maximum. • The PETM was a phenomenon in Earth’s history were the temperature jumped to high temperatures for about 10,000 years. This jump reached 6 degrees Celsius in average temperature. • 6 degrees Celsius may not seem like much but remember that annual temperature is a average of global temperature so in some places the jump was more than 6 degrees.

  3. When Was the PETM? • Cenozoic Era is known as age of mammals.

  4. What caused the PETM? • There is controversy over what caused the PETM. • Most theories believe there was a release of a green house gas from some kind of sink. • As of now the leading theories include... • A release of Methane from Methane stores deep below the ocean’s surface. • Volcanic eruption that released Carbon Dioxide. • A comet impact that released Carbon Dioxide. • …. And more! • Some people also argue that just one of these events would not be enough to trigger the PETM and that it would take multiple of these events to cause it. • In the end as of now we do not know what caused the PETM.

  5. Why is the PETM important?

  6. What did the Earth look like during the PETM? • The Earth was virtually ice-free. • Midwest America looked more like what coastal South Carolina does today. • Palm trees grew in Canada. • Alligators even swam in Artic swamps.

  7. Relative Position of Continents during PETM

  8. Leaf Margin Analysis • Leaf margin Analysis is the process of comparing the amount of smoothed edged leaves to the amount of toothed edged leaves in a sample by a percent. • This percent is then put into a linear function that has been created from data collected of actual samples of temperature compared to the percent of smooth to rough edged leaves. • The output of the linear function is the average annual temperature in Celsius of the time and place from which the leaves are from.

  9. How does this method Work? • The reason this method works is because toothed leaves are able to begin photosynthesis earlier than smooth edged leaves in the spring. • However toothed leaves lead to a high amount of water loss which does not provide adequate water to the tree in a hot climate. • So because of this smooth edged leaves are more likely to be able to grow in warm climates

  10. How does Leaf Margin Analysis help us learn about the PETM? • In the Big Horn Basin in Wyoming fossils have been found from the PETM. • Fossils of Plants and animals were buried by eroded mud of the still growing Rocky Mountains and as this mud hardened the plants and animals fossilized. • Today millions of years later scientists have discovered these fossils. • Scientists can sort these plant fossils by smooth and rough edged leaves and use Leaf Margin Analysis to estimate the temperature of the PETM.

  11. Lab Activity Hypothesis: Do you believe that your group estimate or the total class estimate will be a more accurate estimate of the annual temperature of Hickory, NC?

  12. Smooth VS. Rough Edged leaves

  13. Finding Percent We now will find the percent of smooth edged leaves to the total collected. Smooth Edged Leaves Total Number of Leaves So for example if we had 6 out of 10 smooth edged leaves we would plug into the above formula and get… 6/10= .6 However we need a percent answer so we have to multiply our answer by 100…. (6/10) x 100 = 60%

  14. Calculating Temperature Now we can plug in our percent answer in for x in the linear function… F(x)= 30.06x+ 1.141 Or Y=30.06x+1.141 X=Our Percent answer With our example of 60% we would plug .60 in for X … Y=30.06(.60)+1.141 And Get… Y=19.177°C Where Y equals the estimated temperature in Celsius.

  15. Do our results align with the actual annual temperature? • The actual annual temperature in Hickory, NC in 2011 was 57.6 degrees Fahrenheit or 14.223 degrees Celsius. • Why Might our results not align? • Sample Size • Time collected

  16. Leaf Margin Analysis an Imperfect Technique? • The process of Leaf Margin Analysis used by scientists makes the assumption that the percent of smooth to total leaves are relatively the same as million of years ago. • Do we know that Leaf Margin Analysis 100% works… no. • We do have other evidence to support the data concluded from leaf margin analysis from other sources.

  17. How does the PETM relate to Climate Change today?

  18. How is the PETM different from today’s Climate Change?

  19. Works Cited • Hickory Weather, Forecast, Temperature and Precipitation. n.d. 2011 14 September <http://www.clrsearch.com/Hickory_Demographics/NC/Weather-Forecast-Temperature-Precipitation>. • "Prehistoric Climate Change and Why it Matters." n.d.Smithsonian Education. 15 December 2011 <http://www.smithsonianeducation.org/educators/lesson_plans/climate_change/index.html>. • The Energy Collective. n.d. 15 December 2011 <http://theenergycollective.com/davidlevy/55886/arguing-rocks>. • The Paleocene Eocene Thermal Maximum. n.d. 15 December 2011 <wikipedia.org>.

More Related