January 10, 2008 The new study in the Jan. 11 issue of the journal Science titled, "Isotopic Evidence for Glaciation During the Cretaceous Supergreenhouse," examines geochemical and sea level data retrieved from marine microfossils deposited on the ocean floor 91 million years ago during the Cretaceous Thermal Maximum. This extreme warming event in Earth's history raised tropical ocean temperatures to 35-37 C (95-98.6 F), about 10 C (50 F) warmer than today, thus creating an intense greenhouse climate. These independent methods provided Andre Bornemann, lead author of the study, with strong evidence to conclude that an ice sheet about 50-60 percent the size of the modern Antarctic ice cap existed for about 200,000 years. Bornemann conducted this study as a postdoctoral researcher at Scripps Oceanography and continues this research at Universitat Leipzig in Germany. Researchers are still unclear as to where such a large mass of ice could have existed in the Cretaceous or how ice growth could have started. The authors suggest that climate cycles may have favored ice growth during a few times in the Cretaceous when natural climate variations produced unusually cool summers. Likewise, high mountains under the modern Antarctic ice cap could have been potential sites for growth of large ice masses during the Cretaceous. Ice sheets were much less common during the Cretaceous Thermal Maximum than during more recent "icehouse" climates. Paradoxically, past greenhouse climates may have aided ice growth by increasing the amount of moisture in the atmosphere and creating more winter snowfall at high elevations and high latitudes, according to the paper's authors. The results from the study are consistent with other studies from Russia and New Jersey that show sea level fell by about 25-40 meters (82-131 feet) at the same time that the ice sheets were growing during the Cretaceous period. Sea level is known to fall as water is removed from the oceans to build continental ice sheets; conversely, sea level rises as ice melts and returns to the sea. The presence or absence of sea ice has major environmental implications, specifically in terms of sea level rise and global circulation patterns. As humans continue to add large amounts of carbon dioxide and other greenhouse gases that accelerate the heating of the atmosphere and oceans, research on Earth's past climate conditions is critical to predict what will happen as Earth's climate continues to warm.## Contact: Annie Reisewitz University of California - San Diego 858-534-3624 scrippsnews@ucsd.edu This text derived from: http://ucsdnews.ucsd.edu/newsrel/science/01-08WarmingClimateGlacialIce.asp Recommend this Article to a Friend Back to: News |
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