Scientists Use Ocean Drilling Data to Connect Seawater Chemistry with Climate Change and Evolution

2016-06-29T09:24:39+00:00 July 23, 2012|
A technician works with core samples at the Gulf Coast Repository (GCR) at Texas A&M University in College Station, Texas, USA. The GCR is one of three core repositories worldwide that stores core samples from scientific ocean drilling, including those acquired during the current Integrated Ocean Drilling Program (IODP). The repositories also accommodate sample requests from scientists across the globe. (Credit: Integrated Ocean Drilling Program/United States Implementing Organization [IODP-USIO])

(Click to enlarge) A technician works with core samples at the Gulf Coast Repository (GCR) at Texas A&M University in College Station, Texas, USA. The GCR is one of three core repositories worldwide that stores core samples from scientific ocean drilling, including those acquired during the current Integrated Ocean Drilling Program (IODP). The repositories also accommodate sample requests from scientists across the globe. (Credit: Integrated Ocean Drilling Program/United States Implementing Organization [IODP-USIO])

Humans get much of the blame for modern climate change, with little attention paid to the contribution of other natural forces. But a new study in the July 20 issue of the journal Science sheds some light on one potential cause of the cooling trend of the past 45 million years. And it has everything to do with the chemistry of the world’s oceans.

Ulrich Wortmann of the University of Toronto and Adina Paytan of the University of California, Santa Cruz are co-authors of a new study that points to the collision between India and Eurasia approximately 50 million years ago as a trigger of one interval of rapid change. This collision enhanced dissolution of the most extensive belt of water-soluble gypsum on Earth, stretching from modern-day Oman to Pakistan, and well into Western India – remnants of which are exposed in the Zagros Mountains in Iran.

“Seawater chemistry is characterized by long phases of stability, which are interrupted by short intervals of rapid change,” says Wortmann. “We’ve established a new framework that helps us better interpret evolutionary trends and climate change over long periods of time. The study focuses on the past 130 million years, but similar interactions have likely occurred through the past 500 million years.”

The scientific drillship JOIDES Resolution sits at a dock in Yokohama, Japan, in September 2009. As one of the main facilities of the Integrated Ocean Drilling Program (IODP), the JOIDES Resolution travels the world's oceans with international teams of geoscientists in order to sample and measure geological features deep below the seafloor. (Credit: Integrated Ocean Drilling Program/United States Implementing Organization [IODP-USIO])

(Click to enlarge) The scientific drillship JOIDES Resolution sits at a dock in Yokohama, Japan, in September 2009. As one of the main facilities of the Integrated Ocean Drilling Program (IODP), the JOIDES Resolution travels the world’s oceans with international teams of geoscientists in order to sample and measure geological features deep below the seafloor. (Credit: Integrated Ocean Drilling Program/United States Implementing Organization [IODP-USIO])

The study, which relies heavily on samples collected by the scientific drillship JOIDES Resolution, suggests that the dissolution or creation of such massive gyspum deposits will change the sulfate content of the ocean, and that this will affect the amount of sulfate aerosols in the atmosphere – and thus climate.

“We propose that times of high sulfate concentrations in ocean water correlate with global cooling, just as times of low concentration correspond with greenhouse periods. When India and Eurasia collided, it caused dissolution of ancient salt deposits, which resulted in drastic changes in seawater chemistry,” says Paytan. “This may have led to the demise of the Eocene epoch – the warmest period of the modern-day Cenozoic era – and the transition from a greenhouse to icehouse climate, culminating in the beginning of the rapid expansion of the Antarctic ice sheet.”

The researchers combined data of past seawater sulfur composition, assembled by Paytan in 2004, with Wortmann’s recent discovery of the strong link between marine sulfate concentrations and carbon and phosphorus cycling. They were able to explain the seawater sulfate isotope record as a result of massive changes to the accumulation and weathering of gyspum – the mineral form of hydrated calcium sulfate.

This Landsat 7 image shows the Zagros Mountains of Iran, which host remnants of what was once the largest belt of water-soluble gypsum on Earth. A recent study in the journal Science suggests that the collision of India and Eurasia some 50 million years ago enhanced the dissolution of salts in this deposit, resulting in a large-scale alteration of seawater chemistry and global climate. (Credit: United States Geological Survey [USGS] Earth Resources Observation and Science [EROS] Center)

(Click to enlarge) This Landsat 7 image shows the Zagros Mountains of Iran, which host remnants of what was once the largest belt of water-soluble gypsum on Earth. A recent study in the journal Science suggests that the collision of India and Eurasia some 50 million years ago enhanced the dissolution of salts in this deposit, resulting in a large-scale alteration of seawater chemistry and global climate. (Credit: United States Geological Survey [USGS] Earth Resources Observation and Science [EROS] Center)

“While it has been known for a long time that gyspum deposits can be formed and destroyed rapidly, the effect of these processes on seawater chemistry has been overlooked,” says Wortmann. “The idea represents a paradigm shift in our understanding of how ocean chemistry changes over time and how these changes are linked to climate.”

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This announcement is adapted from a press release issued by the University of Toronto. The paper, titled “Rapid Variability of Seawater Chemistry over the Past 130 Million Years,” appears in the July 20, 2012 issue of the journal Science.

About IODP

The Integrated Ocean Drilling Program (IODP) is an international research program dedicated to advancing scientific understanding of the Earth through drilling, coring, and monitoring the subseafloor. The JOIDES Resolution is a scientific research vessel managed by the U.S. Implementing Organization of IODP (USIO). Together, Texas A&M University, Lamont-Doherty Earth Observatory of Columbia University, and the Consortium for Ocean Leadership comprise the USIO.  IODP is supported by two lead agencies: the U.S. National Science Foundation (NSF) and Japan’s Ministry of Education, Culture, Sports, Science, and Technology. Additional program support comes from the European Consortium for Ocean Research Drilling (ECORD), the Australia-New Zealand IODP Consortium (ANZIC), India’s Ministry of Earth Sciences, the People’s Republic of China (Ministry of Science and Technology), and the Korea Institute of Geoscience and Mineral Resources. For more information, visit www.iodp.org.

To the left of this image, taken from the Space Shuttle Atlantis, are the Zagros Mountains of Iran – which host remnants of what was once the largest belt of water-soluble gypsum on Earth. A recent study in the journal Science suggests that the collision of India and Eurasia some 50 million years ago enhanced the dissolution of salts in this deposit, resulting in a large-scale alteration of seawater chemistry and global climate. (Credit: Image Science & Analysis Laboratory, NASA Johnson Space Center)

(Click to enlarge) To the left of this image, taken from the Space Shuttle Atlantis, are the Zagros Mountains of Iran – which host remnants of what was once the largest belt of water-soluble gypsum on Earth. A recent study in the journal Science suggests that the collision of India and Eurasia some 50 million years ago enhanced the dissolution of salts in this deposit, resulting in a large-scale alteration of seawater chemistry and global climate. (Credit: Image Science & Analysis Laboratory, NASA Johnson Space Center)

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Media Contacts:

Ulrich G. Wortmann
Department of Geology
University of Toronto
uli.wortmann@utoronto.ca
416-978-7084 (office)
647-780-2037 (cell)

Sean Bettam
Communications, Faculty of Arts & Science
University of Toronto
s.bettam@utoronto.ca

416-946-7950

Adina Paytan
Institute of Marine Sciences
University of California Santa Cruz
apaytan@ucsc.edu

650-274-6084

Matthew Wright
Consortium for Ocean Leadership
Washington, D.C. USA
mwright@oceanleadership.org

+1-202-448-1254