Democratic Underground Latest Greatest Lobby Journals Search Options Help Login
Google

Coral Proxy Data Shows Ocean Thermocline (Cool/Warm Water Boundary) Rising Since 1970s

Printer-friendly format Printer-friendly format
Printer-friendly format Email this thread to a friend
Printer-friendly format Bookmark this thread
This topic is archived.
Home » Discuss » Topic Forums » Environment/Energy Donate to DU
 
hatrack Donating Member (1000+ posts) Send PM | Profile | Ignore Thu Oct-14-10 12:40 PM
Original message
Coral Proxy Data Shows Ocean Thermocline (Cool/Warm Water Boundary) Rising Since 1970s
EDIT

Specifically, the researchers were interested in how the boundary layer between the warmer, shallow water and the colder deeper water -- the thermocline -- has changed. But directly measuring that over time and across a broad area is impossible. Instead, they used the soft corals as a substitute, a proxy, for determining how the thermocline rose and fell over time. Working with samples taken from corals at five meters (16.4 feet), 85 meters (279 feet) and 105 meters (345 feet), they analyzed the chemical structure of the coral skeleton that had built up over time.

Slices cut through the base “trunk” of the coral revealed concentric circles resembling tree rings which showed the growth of the “trunk” over time. By analyzing material from the rings from the outer surface inward to the center, they assembled a growth record covering the last century or so.

They were looking for the ratio between two isotopes of nitrogen in the material as a clue to how the thermocline rose or fell over time. Warmer waters above the thermocline contained lower levels of nutrients resulting in organic matter with a high ratio of nitrogen-15 to nitrogen-14 isotopes. Waters below the thermocline held higher levels of nutrients resulting in organic matter with a low ratio of nitrogen-15 to nitrogen-14 isotopes. As the polyps in the coral consumed the organic matter over the years, the nitrogen isotopes were chemically recorded in the coral. By comparing the nitrogen-15 to nitrogen-14 ratios in samples from the three depths, they could draw a picture of how the thermocline moved.

“Over several decades, specifically since the mid- to late-1970s, the records show that the mean depth of the thermocline has been getting shallower,” Williams said. The researchers did a similar analysis of the ratio of two carbon isotopes in the coral samples as well. “I think it’s fair to say that the carbon isotope record supports this interpretation,” Grottoli said. “It’s another piece of evidence backing our conclusions.”

EDIT

http://www.redorbit.com/news/science/1930637/coral_records_show_ocean_thermocline_rise_with_global_warming/index.html?source=r_science
Printer Friendly | Permalink |  | Top

Home » Discuss » Topic Forums » Environment/Energy Donate to DU

Powered by DCForum+ Version 1.1 Copyright 1997-2002 DCScripts.com
Software has been extensively modified by the DU administrators


Important Notices: By participating on this discussion board, visitors agree to abide by the rules outlined on our Rules page. Messages posted on the Democratic Underground Discussion Forums are the opinions of the individuals who post them, and do not necessarily represent the opinions of Democratic Underground, LLC.

Home  |  Discussion Forums  |  Journals |  Store  |  Donate

About DU  |  Contact Us  |  Privacy Policy

Got a message for Democratic Underground? Click here to send us a message.

© 2001 - 2011 Democratic Underground, LLC