Now on ScienceBlogs: Q: How do you sex a Smilodon? (A: Very carefully)

Seed Media Group

Deep Sea News

All the news on the Earth's largest environment

screenshot_02.jpg

Profile

scubacraig.jpg Craig is temporarily a post-doctoral fellow at the Monterey Bay Aquarium Research Institute who is looking for a permanent position. He spends most of his time balancing his overwhelming geekdom with normalcy so he can function in the real world. Luckily his wife likes his geekiness.



peter_chinchorro.jpg Peter Etnoyer is a Graduate Research Associate at the Harte Research Institute for Gulf of Mexico Studies, Texas A&M University-Corpus Christi. He studies deep corals and ocean fronts, and he loves to be on the water.



kevvygumby%20copy.jpg Kevin Zelnio is a Graduate Student Researcher at Penn State studying the ecology of hydrothermal vent and methane seep communities. He raises awareness of the plight of the spineless through folk music.

Google All DSN Posts


Awards & Affiliations


ecodaredevil.jpg
Nature Blog Network
Oceana
support_plos_100x157.jpg
Add to Technorati Favorites
thinkingblogger2ql6.jpg 2162223913_dc43c05edc_o.png

Search

Recent Posts

Recent Comments

Archives

Blogroll

Other Information

My book is coming out. Include a link and thumbnail.

Other random info. A link.

Deep Sea News has moved! Make sure to update your bookmarks and feed readers.

« From The Desk of Zelnio: Lucernaria janetae | Main | Friday Deep-Sea Picture (4/27/07) »

PETM, Volcanoes, and #18 in 25 Things You Should Know

Category: 25 Things You Should Know About the Deep SeaNew Research
Posted on: April 26, 2007 11:41 AM, by CR McClain

petm.jpg

Approximately 55 million years ago it was very bad to be a deep-sea animal. First the ocean temperature was rising. At the surface, temperatures rose anywhere from 5-10 degrees and in the deep around 5 degrees. The chemistry of the water also changed significantly. Oxygen became depleted. The ocean became more acidic. Global currents were altered such that deep-water upwelled in the Northern Hemisphere instead of the Southern for ~100,000 years.


This event is used to mark the end of the Paleocene and the start of the Eocene and thus the event is called the Paleocene-Eocene Thermal Maximum. A old instructor of mine use to refer to it as the P.E. S*&^ Storm. I digress but you get the point.

rip.jpg

The warmer, hypoxic, acidic ocean was essentially an inhospitable place leading to a mass extinction event. 30-40% of calcareous benthic forams went extinct. Many other groups like gastropods are also hypothesized to went extinct. In general, the PETM was considered a resetting of the deep-sea fauna especially for those organisms possessing calcareous shells which don't fair well under increased acidity. However, some groups such as isopods are predicted to have made it through the PETM. Oh yeah, mammals died off too.

Another way to grasp the PETM event is by looking at C-13:C-12.  It appears that a few metabolic enzymes, but not all, in organisms prefer C-12 to C-13.  The reason appears to be that C-12 is slightly more energetic and thus more likely to react.  Thus organisms are differentially made up of Carbon-12 as opposed to Carbon-13.  If more phytoplankton growth then theC-12 decreases.  Less C-12 indicates less photosynthesis and production.  Thus shells below made up of of calcium carbonate formed in high C-12 waters would also high C-12 and low C-13:C-12.  A sample of marine sediments from the PETM event with the tons of foram shells would give an indication of the the phytoplankton production at this point.  Samples from the PETM have very high levels of C-12.  But are far greater than that would be expected just from a stop of all photosynthetic activity.  Even if you burned every living thing on the planet, returning on the 12C, it would only be 1/3 that of the  PETM13C:12C ratio. 

What caused the PETM and the sudden rise in C-12? Greenhouse gases other than carbon dioxide. It has been argued that methane, a far more effective greenhouse gas, was released into the atmosphere causing the PETM. It is proposed that the methane source was ice in deep seafloor sediments one of the only massive pools of light carbon (C-12), the methane burp hypothesis.  In once scenario, erosion or seismic activity along the continental margin may have allowed methane to escape from gas reservoirs.  In an other, a gradual surface change in temperature lead to a snowball effct by leading to a thermal dissociation of methane hydrate. However, a very recent study in Science indicates that the PETM may be linked to a massive volcanic eruptions that pushed Greenland and northwest Europe apart to create the North Atlantic Ocean.

"That prehistoric volcanic activity released more than 2000 gigatonnes (billion metric tons) of carbon into the oceans and atmosphere in the form of methane and carbon dioxide - two potent greenhouse gases," said Michael Storey of Roskilde University in Denmark, the study's lead author. "The carbon probably came from the heating of earlier deposits of decayed organic matter - similar to deposits in the Atlantic and North Sea we tap today for oil and gas."
You can have some confidence in the dating of the ash layer as...
That dating method, performed in labs at the three universities, renders precise ages in geological time frames, based on known decay rates of potassium to argon trapped in the volcanic material.
Foram image from http://www.palmod.uni-bremen.de/FB5/geochron/Robert/RPSpeb.html

TrackBacks

TrackBack URL for this entry: http://scienceblogs.com/mt/pings/39158

Comments

1

can you elaborate/clarify how the 12C:13C ratio helps understand the PETM extinctions?

Another way to grasp the PETM extinction event is by looking at 13C:12C. Organisms are differentially made up of Carbon-12 as opposed to Carbon-13. Increases in biological activity requiring more 12C thus inrease the 13C:12C ratio. If you burned every living thing on the planet, returning on the 12C, it would only be 1/3 that of the PETM13C:12C ratio.

Posted by: Jim Lemire | April 26, 2007 8:58 PM

2

NP, Revamped the post above

Posted by: CR McClain | April 27, 2007 9:44 AM

Post a Comment

(Email is required for authentication purposes only. On some blogs, comments are moderated for spam, so your comment may not appear immediately.)





ScienceBlogs

Search ScienceBlogs:

Go to:

Advertisement
Follow ScienceBlogs on Twitter
Visit the Collective Imagination blog
Advertisement

© 2006-2009 Seed Media Group LLC. ScienceBlogs is a registered trademark of Seed Media Group. All rights reserved.

Sites by Seed Media Group: Seed Media Group | ScienceBlogs | SEEDMAGAZINE.COM