Ocean Resources


King Kelp

Scott Lindell

To help fuel our future energy needs, researchers are sizing up thousands of blades of sugar kelp—a promising source of biofuels—to breed strains that grow larger, heartier, and more abundantly.

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FAQs

What is deep-sea mining? Deep-sea mining is the proposed extraction of metallic and non-metallic mineral resources from the ocean floor…

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Marine Protected Areas

What are Marine Protected Areas? Marine protected area (MPA) refers to any part of the ocean that receives some level…

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Seafloor Mining

Hot, buoyant, mineral-laden fluids rise from deep within ocean crust and mix with cold seawater. That triggers the precipitation of…

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On (and Below) the Waterfront

On (and Below) the Waterfront

The expansion of the New York metropolitan area’s harbor over the decades has led to big but hidden changes in tidal flows that have environmental impacts.

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WHOI Among First Funding Recipients of The Audacious Project

WHOI Among First Funding Recipients of The Audacious Project

What if we explored the ocean’s vast twilight zone, teeming with undiscovered life? Today, the Woods Hole Oceanographic Institution (WHOI) was awarded $35 million – ”the largest philanthropic gift in the Institution’s history – ”to do just that. The award comes from The Audacious Project, a bold new philanthropic collaboration housed at TED to fund critical ideas that have potential to create massive, global change.

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Fueling the Future

Fueling the Future

WHOI was awarded $5.7 million from ARPA-E’s Macroalgae Research Inspiring Novel Energy Resources (MARINER) Program for two projects that develop tools and technology to advance the mass production of seaweed for biofuels and bio-based chemicals.

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Fresh Water Below the Seafloor?

Fresh Water Below the Seafloor?

Using a new method to distinguish fresh water from oil or salt water, scientists are exploring beneath the continental shelf off New England to look for large pockets of trapped fresh water. This water may be continually filling from groundwater flowing from land or, alternatively, may have been left behind by ice ages glaciers.

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