Earth's Crazy Climate :: Astrobiology Magazine - earth science - evolution distribution Origin of life universe - life beyond :: Astrobiology is study of earth science evolution distribution Origin of life in universe terrestrial
Skip to page main content
NASA Logo - Astrobiology Magazine - earth science - evolution distribution Origin of life universe - life beyond: Astrobiology is study of earth science evolution distribution Origin of life in universe terrestrial + Astrobiology Portal
+ NASA Home
FIND IT @ NASA
NASA HomepageAstrobiology Magazine - earth science - evolution distribution Origin of life universe - life beyond: Astrobiology is study of earth science evolution distribution Origin of life in universe terrestrial
Home Science and Research Datasets and Images Publications Multimedia
News flash!
Astrobio.net is getting a makeover!
Click here to submit your Poll
Great Debates
Collision_Course_for_Earth

Collision Course for Earth
Main Menu
Today's Story
Today's most-read story is:

Dark Moon Cooling
Other Stories
 
Earth's Crazy Climate
Terrestrial Climate History Summary (Sep 27, 2006): Ancient rocks from the bottom of the Pacific Ocean suggest dramatic climate changes during the dinosaur-dominated Mesozoic Era, a time once thought to have been monotonously hot and humid.

Display Options: Send this story to someone Printer-friendly page _FAX _PDF _RTF _XLS _PALM _XML _WML _S2D _ESP _PS _TTS Larger font Smaller font


Earth's Crazy Climate

based on an Indiana University release

Analysis of the shale led scientists to conclude significant temperature variations occurred during the Cretaceous Period.
Credit: Simon Brassell

Ancient rocks from the bottom of the Pacific Ocean suggest dramatic climate changes during the dinosaur-dominated Mesozoic Era, a time once thought to have been monotonously hot and humid.

In this month's Geology, scientists from Indiana University Bloomington and the Royal Netherlands Institute for Sea Research present new evidence that ocean surface temperatures varied as much as 6 degrees Celsius (about 11 degrees Fahrenheit) during the Aptian Epoch of the Cretaceous Period 120 million years ago.

The finding is relevant to the ongoing climate change discussion, IUB geologist Simon Brassell says, because it portrays an ancient Earth whose temperatures shifted erratically due to changes in carbon cycling and did so without human input.

"Combined with data from the Atlantic, it appears clear that climate changes were taking place on a global scale during this time period," said Brassell, who led the study.

A previous study from an Atlantic Ocean site had suggested a changeable climate around the same time period. But it was not known whether the Atlantic data indicated regional climate change unique to the area or something grander.

"We had virtually no data from the middle of the largest ocean at that time period," Brassell said. "The data we collected suggest significant global fluctuations in temperature."

As part of the National Science Foundation's Ocean Drilling Project, the geoscientists voyaged in 2001 to Shatsky Rise, a study site 1,600 kilometers (1,000 miles) east of Japan and 3,100 meters below the ocean surface. Shatsky Rise is known to have formed at the end of the Jurassic Period immediately prior to the beginning of the Cretaceous, the last period of the Mesozoic Era.

The scientists' vessel, the JOIDES Resolution, is specially outfitted with a drill that can be lowered to the sea floor for the collection of rock samples.

IU Bloomington geochemist Simon Brassell (right), Penn State sedimentologist Michael Arthur (middle), and Tohoku Univ. sedimentologist Harumasa Kano (left) inspect an ancient shale aboard the JOIDES Resolution research vessel.
Credit: Ocean Drilling Program

The drill bit was driven 566 meters into Shatsky Rise. Rocks freed by the drill were transported directly to the surface for analysis. The rocks corresponding to early Aptian time were extremely rich in organic material. By analyzing the carbon and nitrogen content of the samples, the geochemists found evidence for changes in carbon cycling and in nitrogen fixation by ocean biological communities associated with changing climate. A special analysis method targeting certain complex carbon-containing molecules provided values for a measurement called TEX86 that revealed mean temperature variations between 30 deg C (86 deg F) and 36 deg C (97 deg F) with two prominent cooling episodes of approximately 4 deg C (7 deg F) in tropical surface temperatures during the early Aptian. By comparison, today's tropical sea surface temperatures typically lie between 29 and 30 deg C.

Brassell says that findings of a changeable climate during the Cretaceous, a time period dominated by dinosaurs and noted for the spread of flowering plants, could influence the current climate change debate.

"One of the key challenges for us is trying to predict climate change," Brassell said. "If there are big, inherent fluctuations in the system, as paleoclimate studies are showing, it could make determining Earth's climatic future even harder than it is. We're learning our climate, throughout time, has been a wild beast."

Related Web Pages

Carbon Balance Killed the Dinos
Did Hades Freeze Over?
Predicting Primordial Weather
Earth Slushie
Titanic Primordial Pull
Snowball Earth Culprit Found?
Discovering Dinos

Note: Terrestrial Climate History
Display Options: Send this story to someone Printer-friendly page _FAX _PDF _RTF _XLS _PALM _XML _WML _S2D _ESP _PS _TTS Larger font Smaller font

Wednesday, September 27, 2006
 
Credits Feedback Related Links Sitemap
FIRST GOV + Privacy, Security, Notices
+ Syndication Help
+ RSS Syndication
+ NASA Ames Astrobiology Portal net
Home Page + Chief Editor & Executive Producer: Helen Matsos
+ Site & Server Maintenance : Turbo Inc.