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Ancient Alteration of Seawater Chemistry Linked With Past Climate Change

By Guest PostJuly 22, 2012Environmentadina paytan, alteration, antarctic ice sheet, candace major, cenozoic era, climate and evolution, climate change, collision, dissolution, eocene epoch, eurasia, greenhouse periods, gypsum, gypsum belt, gypsum deposit, hydrated calcium sulfate, icehouse climate, India, iodp, iran, joides resolution, marine, million years, mineral, national science foundation, ocean drillship, oman, Pakistan, phosphorus cycling, plate tectonics, santa cruz, seawater chemistry, sulfate aerosols, sulfate concentration, sulfur composition, ulrich wortmann, university of california, university of toronto, zagros mountains

Dissolution or creation of huge gypsum deposits changed sulfate content of the oceans

Scientists have discovered a potential cause of Earth’s “icehouse climate” cooling trend of the past 45 million years. It has everything to do with the chemistry of the world’s oceans.

“Seawater chemistry is characterized by long phases of stability, which are interrupted by short intervals of rapid change,” says geoscientist Ulrich Wortmann of the University of Toronto, lead author of a paper reporting the results and published this week in the journal Science.

“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.” (more…)

Sea Cucumbers: Dissolving Coral Reefs?

Washington, D.C. — Coral reefs are extremely diverse ecosystems that support enormous biodiversity. But they are at risk. Carbon dioxide emissions are acidifying the ocean, threatening reefs and other marine organisms. New research led by Carnegie’s Kenneth Schneider analyzed the role of sea cucumbers in portions of the Great Barrier Reef and determined that their dietary process of dissolving calcium carbonate (CaCO3) from the surrounding reef accounts for about half of at the total nighttime dissolution for the reef. The work is published December 23 by the Journal of Geophysical Research.

Reefs are formed through the biological deposition of calcium carbonate (CaCO3). Many of the marine organisms living on and around a reef contribute to either its destruction or construction. Therefore it is crucial that the amount of calcium carbonate remain in balance. When this delicate balance is disrupted, the reef ceases to grow and its foundations can be weakened. (more…)

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Ancient Alteration of Seawater Chemistry Linked With Past Climate Change

Sea Cucumbers: Dissolving Coral Reefs?