For the second time in as many months, the IODP Arctic Coring Expedition (ACEX) is making news with new analysis of ocean-floor sediments. In the Aug. 10 issue of Nature, an article by several of the expedition scientists summarizes their findings: more evidence that the Arctic was extremely warm, unusually wet, and ice-free up to the time the last massive amounts of greenhouse gases were released into the Earth's atmosphere – a period calculated to have occurred 55 million years ago, and known as the Paleocene/Eocene thermal maximum, or PETM.
Researchers have long recognized that a massive release of greenhouse gases, probably carbon dioxide or methane, occurred during the PETM. Surface temperatures also rose in many places by as much as 15 degrees Fahrenheit in the (relative) geological instant of about 100,000 years.
Arctic sediment samples were largely unavailable until 2004, when ACEX scientists recovered the first deep-ocean sediment samples from beneath the ice-laden waters near the North Pole. ACEX, only the second scientific expedition to be conducted by the Integrated Ocean Drilling Program (established 2003), recovered 339 meters of subseafloor sediment samples.
"Building a picture of ancient climatic events is a lot like putting together a jigsaw puzzle, and what ACEX allowed us to do was fill in a blank section of the PETM picture," said Gerald Dickens, a Rice University geochemist and co-author, who conducted the initial, shipboard chemical analyses of all the ACEX core samples.
"The ACEX cores clearly show that the Arctic got very warm and wet during the PETM," Dickens said. "Even tropical marine plants thrived in the balmy conditions."
In today's oceans, certain species of microscopic plants are known to rapidly multiply and create algal blooms. Dickens said that fossils of these plants – known only to originate in the tropics before the PETM – are commonly seen in the ACEX cores. Furthermore, the chemistry of the organic carbon in the ACEX cores may rule out some earlier theories about what caused the PETM. The diminution of these alternate explanations strongly suggests that an enormous amount of carbon entered the atmosphere at the beginning of the PETM, either from volcanic eruptions, or the melting of oceanic gas hydrates – mixtures of methane and ice on the seafloor.
ACEX co-authors include Mark Pagani and Nikolai Pedentchouk of Yale University, Matthew Huber of Purdue University, Appy Sluijs and Henk Brinkhuis of Utrecht University (Netherlands), and Stefan Schouten and Jaap Sinninghe Damsté of the Royal Netherlands Institute for Sea Research.
ACEX was a scientific operation of the Integrated Ocean Drilling Program (IODP), an international marine research program primarily funded by the National Science Foundation, and Japan's Ministry of Education, Culture, Sports, Science and Technology. The Arctic Coring Expedition was led by the European Consortium on Ocean Research Drilling (ECORD), an IODP contributing member that represents 17 nations. ECORD is responsible for managing all IODP mission-specific operations, i.e. scientific expeditions conducted in unusual or demanding environments in which specific platform requirements must be used to meet specific science objectives. In all, 21 countries participate in IODP.
To see earlier news releases about ACEX, go to www.iodp.org/news-releases. The expedition page with background information, photos, a list of scientists who participated in the expedition, logbooks, the expedition's final Proceedings volume, and more, go to www.ecord.org/exp/acex/302.html
Contacts:
Jade Boyd
Rice University
e-mail; jadeboyd@rice.edu
Alan Stevenson
ECORD Science Operator (ESO)
agst@bgs.ag.uk
Nancy Light
nlight@iodp.org
Journal
Nature