1 / 12

Aaron Cevallos Advisor: Andreas Andersson , Ph.D. Summer 2010

The Effects of Ocean Acidification on Coral A Comparison between the Alkalinity Anomaly and Buoyant Weight Methods of Measurement. Aaron Cevallos Advisor: Andreas Andersson , Ph.D. Summer 2010. What is ocean acidification? What is causing it?.

aiden
Download Presentation

Aaron Cevallos Advisor: Andreas Andersson , Ph.D. Summer 2010

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 Effects of Ocean Acidification on CoralA Comparison between the Alkalinity Anomaly and Buoyant Weight Methods of Measurement Aaron Cevallos Advisor: Andreas Andersson, Ph.D. Summer 2010

  2. What is ocean acidification? What is causing it? • The ocean absorbs approximately 1/3rd of the CO2 emitted to the atmosphere from the burning of fossil fuels. • As CO2 dissolves in seawater, the pH of the water decreases. Since the beginning of the industrial revolution, ocean pH has dropped globally by approximately 0.1 pH units. • By the end of this century, we may expect to see changes in pH that are the greatest in 21 million years. • http://ioc3.unesco.org/oanet/FAQacidity.html

  3. Evidence of ocean acidification at BATS N. Bates

  4. Bermuda coral reef: the canary in a coal mine? Buddemeier et al. 2004, based on Veron 1995 [CO32-] across coral reef platform -Marginal reef -Lower [CO32-] -Healthy reef -No major industries or pollution -Natural gradient in [CO32-] Alex Venn Mid-platform Inshore Outer rim

  5. What can we expect in the future ? Changes in atmospheric CO2 under the "business as usual" scenario to the year 2100 and associated changes in ocean pH and carbon chemistry. Adapted from Wolf-gladrow et al., 1999 • The IPCC expects: • a drop in ocean pH of about 0.4 pH units by the end of this century • a 60% decrease in the concentration of calcium carbonate http://ioc3.unesco.org/oanet/FAQacidity.html

  6. Why is ocean acidification a problem? • Seawater acid-base balance important in regulating biological and chemical processes, e.g.: • Function of enzyme and proteins • Chemical reaction rates • Availability of nutrients and trace metals • CO32- is an essential building block for marine calcifiers depositing skeletons or shells made of CaCO3† • Less building material equals slower growth, weaker structures (similar to osteoporosis in humans) and increased vulnerability to environmental stress in general †Ca2+ is the other building block, but there are plenty of calcium in seawater

  7. Ca2+ CO32- CaCO3 The Alkalinity Anomaly Method • The alkalinity anomaly method relies on the principle that when a calcifying organism produces a mole of calcium carbonate, total alkalinity is decreased by two moles. • I will be able to know the exact degree to which synthesis or dissolution is taking place using this method.

  8. Average Daytime vs. Nighttime Calcification Rates

  9. The Buoyant Weighing Method Calcification (or dissolution) of a coral sample is inferred from changes in the sample’s mass. The weight can be determined in water using the formula: Wa= Ww / [1-(pw/ps)] http://www.aagaines.com/man/graphics/scale.jpg

  10. AA Predicted Weight Change vs. BW Actual Weight Change

  11. Thank You!

More Related