OREGON STATE UNIVERSITY

hatfield marine science center

Public meeting set Thursday on Marine Studies Building at Hatfield Center

NEWPORT, Ore. – Oregon State University will host an informational public meeting this Thursday, June 15, to update local residents on plans for a new Marine Studies Building at OSU’s Hatfield Marine Science Center in Newport.

The meeting will run from 5 to 6:30 p.m. in Hatfield’s Visitor Center. A 45-minute presentation and question-and-answer session will be followed by a reception and displays. The Hatfield Center is located at 2030 S.E. Marine Science Drive in Newport, just southeast of the Highway 101 bridge.

The presentation will also be streamed live over Adobe Connect at http://oregonstate.adobeconnect.com/hmsc-fw407/

Oregon State University has launched a Marine Studies Initiative – a new research and teaching model to help sustain healthy oceans and ensure wellness, environmental health and economic prosperity for coastal communities.

“A component of the Marine Studies Initiative includes the construction of a research and teaching facility – the Marine Studies Building on the HMSC campus – and student housing at another location in Newport,” said Steve Clark, vice president for university relations and marketing.

“This public meeting in Newport is an opportunity to hear how the university will ensure that the design, engineering and construction of the Marine Studies Building and student housing meet or exceed the earthquake and tsunami performance and safety commitments that OSU President Ed Ray has made.”

Presentations will be made by­­­­­­­­­­­­­­­­­­­­­­­­­­­ Bob Cowen, director of OSU’s Hatfield Marine Science Center, and Tom Robbins, project manager and architect with Yost Grube Hall Architecture.

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Steve Clark, 541-737-3808, steve.clark@oregonstate.edu; Bob Cowen, 541-867-0211, Robert.Cowen@oregonstate.edu

Acidified ocean water widespread along North American West Coast

CORVALLIS, Ore. – A three-year survey of the California Current System along the West Coast of the United States found persistent, highly acidified water throughout this ecologically critical nearshore habitat, with “hotspots” of pH measurements as low as any oceanic surface waters in the world.

The researchers say that conditions will continue to worsen because the atmospheric carbon dioxide primarily to blame for this increase in acidification has been rising substantially in recent years.

One piece of good news came out of the study, which was published this week in Nature Scientific Reports. There are “refuges” of more moderate pH environments that could become havens for some marine organisms to escape more highly acidified waters, and which could be used as a resource for ecosystem management.

“The threat of ocean acidification is global and though it sometimes seems far away, it is happening here right now on the West Coast of the United States and those waters are already hitting our beaches,” said Francis Chan, a marine ecologist at Oregon State University and lead author on the study.

“The West Coast is very vulnerable. Ten years ago, we were focusing on the tropics with their coral reefs as the place most likely affected by ocean acidification. But the California Current System is getting hit with acidification earlier and more drastically than other locations around the world.”

A team of researchers developed a network of sensors to measure ocean acidification over a three-year period along more than 600 miles of the West Coast. The team observed near-shore pH levels that fell well below the global mean pH of 8.1 for the surface ocean, and reached as low as 7.4 at the most acidified sites, which is among the lowest recorded values ever observed in surface waters.

The lower the pH level, the higher the acidity. Previous studies have documented a global decrease of 0.11 pH units in surface ocean waters since the beginning of the Industrial Revolution. Like the Richter scale, the pH scale in logarithmic, so that a 0.11 pH unit decrease represents an increase in acidity of approximately 30 percent.

Highly acidified ocean water is potentially dangerous because many organisms are very sensitive to changes in pH. Chan said negative impacts already are occurring in the California Current System, where planktonic pteropods – or small swimming snails – were documented with severe shell dissolution.

“This is about more than the loss of small snails,” said Richard Feely, senior scientist with the National Oceanic and Atmospheric Administration’s Pacific Marine Environmental Laboratory. “These pteropods are an important food source for herring, salmon and black cod, among other fish. They also may be the proverbial ‘canary in the coal mine’ signifying potential risk for other species, including Dungeness crabs, oysters, mussels, and many organisms that live in tidepools or other near-shore habitats.”

Previous studies at OSU have chronicled the impact of acidified water on the Northwest oyster industry.

Chan said the team’s observations, which included a broad-scale ocean acidification survey via ship by NOAA, did not vary significantly over the three years – even with different conditions, including a moderate El Niño event.

“The highly acidified water was remarkably persistent over the three years,” Chan said. “Hotspots stayed as hotspots, and refuges stayed as refuges. This highly acidified water is not in the middle of the Pacific Ocean; it is right off our shore. Fortunately, there are swaths of water that are more moderate in acidity and those should be our focus for developing adaptation strategies.”

The researchers say there needs to be a focus on lowering stressors to the environment, such as maintaining healthy kelp beds and sea grasses, which many believe can partially mitigate the effects of increasing acidity.

Further, the moderately acidified refuge areas can be strategically used and managed, Chan pointed out.

“We probably have a hundred or more areas along the West Coast that are protected in one way or another, and we need to examine them more closely,” he said. “If we know how many of them are in highly acidified areas and how many are in refuge sites, we can use that information to better manage the risks that ocean acidification poses.”

Managing for resilience is a key, the researchers conclude.

“Even though we are seeing compromised chemistry in our ocean waters, we still have a comparably vibrant ecosystem,” Chan said. “Our first goal should be to not make things worse. No new stresses. Then we need to safeguard and promote resilience. How do we do that? One way is to manage for diversity, from ensuring multiple-age populations to maintaining deep gene pools.

“The greater the diversity, the better chance of improving the adaptability of our marine species.”

Chan, a faculty member in the College of Science at Oregon State University, was a member of the West Coast Ocean Acidification and Hypoxia Panel appointed by the governments of California, Oregon, Washington and British Columbia.

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Francis Chan, 541-737-9131, chanft@science.oregonstate.edu

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ocean acidification 2

Acidification is threatening tidepool organisms

ocean sensors 2

A sensor at the Oregon coast.

OSU to hold public forum May 24 in Corvallis on new building at Hatfield Marine Science Center

CORVALLIS, Ore. – A community forum regarding Oregon State University’s engineering and construction plans for a marine studies building on the Hatfield Marine Science Center campus in Newport will be held Wednesday, May 24, in Corvallis.

The meeting will be held from 5:30 to 7 p.m. on OSU’s Corvallis campus in LaSells Stewart Center’s Agricultural Sciences Room. The meeting also will be live streamed at: ­­­­­http://bit.ly/2rjRmC5

Oregon State University has launched a Marine Studies Initiative, a new research and teaching model to help sustain healthy oceans and ensure wellness, environmental health and economic prosperity for coastal communities.

“A component of the Marine Studies Initiative includes the construction of a research and teaching facility – the Marine Studies Building on the HMSC campus – and student housing at another location in Newport,” said Steve Clark, vice president for university relations and marketing.

“The workshop is an opportunity to hear how the university will ensure that the design, engineering and construction of the Marine Studies Building and student housing meet or exceed the earthquake and tsunami performance and safety commitments that OSU President Ed Ray has made.”

The workshop will include an update on the work of a project oversight committee, as well as updates by the project’s architect and the chair of an independent, third-party technical peer review panel, Clark said.

The meeting also will include an opportunity for attendees to ask questions.

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Steve Clark, 541-737-3808, steve.clark@oregonstate.edu

New video shows how blue whales employ strategy before feeding

NEWPORT, Ore. – Blue whales didn’t become the largest animals ever to live on Earth by being dainty eaters and new video captured by scientists at Oregon State University shows just how they pick and choose their meals.

There is a reason for their discretion, researchers say. The whales are so massive – sometimes growing to the length of three school buses – that they must carefully balance the energy gained through their food intake with the energetic costs of feeding.

“Modeling studies of blue whales ‘lunge-feeding’ theorize that they will not put energy into feeding on low-reward prey patches,” said Leigh Torres, a principal investigator with the Marine Mammal Institute at Oregon State, who led the expedition studying the blue whales. “Our footage shows this theory in action. We can see the whale making choices, which is really extraordinary because aerial observations of blue whales feeding on krill are rare.”

“The whale bypasses certain krill patches – presumably because the nutritional payoff isn’t sufficient – and targets other krill patches that are more lucrative. We think this is because blue whales are so big, and stopping to lunge-feed and then speeding up again is so energy-intensive, that they try to maximize their effort.”

The video, captured in the Southern Ocean off New Zealand, shows a blue whale cruising toward a large mass of krill – roughly the size of the whale itself. The animal then turns on its side, orients toward the beginning of the krill swarm, and proceeds along its axis through the entire patch, devouring nearly the entire krill mass.

In another vignette, the same whale approaches a smaller mass of krill, which lies more perpendicular to its approach, and blasts through it without feeding.

“We had theorized that blue whales make choices like this and the video makes it clear that they do use such a strategy,” explained Torres, who works out of Oregon State’s Hatfield Marine Science Center in Newport, Oregon. “It certainly appears that the whale determined that amount of krill to be gained, and the effort it would take to consume the meal wasn’t worth the effort of slowing down.

“It would be like me driving a car and braking every 100 yards, then accelerating again. Whales need to be choosy about when to apply the brakes to feed on a patch of krill.”

The researchers analyzed the whale’s lunge-feeding and found that it approached the krill patch at about 6.7 miles per hour. The act of opening its enormous mouth to feed slowed the whale down to 1.1 mph – and getting that big body back up to cruising speed again requires a lot of energy.

The rare footage was possible through the use of small drones. The OSU team is trained to fly them over whales and was able to view blue whales from a unique perspective.

“It’s hard to get good footage from a ship,” Torres said, “and planes or helicopters can be invasive because of their noise. The drone allows us to get new angles on the whales without bothering them.”

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Leigh Torres, 541-867-0895, leigh.torres@oregonstate.edu

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Photo at left: Blue whale feeding on a krill patch.

 

Launching Drone
Launching of the drone.

Oregon State part of new NSF research program in the Arctic

CORVALLIS, Ore. – Oregon State University and five other universities this week received an award to initiate a new Long-Term Ecological Research (LTER) project in the Arctic that will explore how relationships between the land and water affect coastal ecosystems along the northern Alaskan coast.

The project has been funded by a five-year, $5.6 million grant from the National Science Foundation and will join 25 existing and two recently awarded coastal LTER sites that form a network of terrestrial and aquatic biomes worldwide.

Two of the new coastal sites, the Northern Gulf of Alaska and the Northeastern U.S. Shelf, are in very productive regions for fisheries. The third site, The Beaufort Sea Lagoons, is the first marine ecosystem LTER in the Arctic Ocean. The project, “Beaufort Sea Lagoons: An Arctic Coastal Ecosystem in Transition,” is supported by NSF’s Office of Polar Programs.

 “It is a very rich, very important ecosystem and we don’t have a good understanding of how it works,” said Yvette Spitz, one of two OSU oceanographers who are principal investigators with the project. “There are chemicals, nutrients and other organic materials that are transported from the land to the ocean, passing through lagoons along the way.”

“One of the goals of the project is to understand how the transport of these materials is affected by changing precipitation, sea ice and melting permafrost – and what effect that has on biological productivity. These changes are presently occurring and are the most rapid in the Arctic”

Scientists at the University of Texas at Austin are leading the project, in collaboration with researchers at Oregon State, University of Alaska Fairbanks, University of Texas El Paso, University of Massachusetts at Amherst and University of Toronto Mississauga.

Also participating will be young scientists from the native Iñupiat communities of Utqiagvik (formerly Barrow) and Kaktovik, and the U.S. Fish and Wildlife Service, which manages the Arctic National Wildlife Refuge.

“An important aspect of this LTER is the collaboration between scientists and the Iñupiat residents of the Beaufort Sea coast, which will greatly deepen our comprehensive understanding of these ecosystems,” said William Ambrose, director of the Arctic Observing Network in the NSF Office of Polar Programs.

The research will be based in Kaktovik, Utqiagvik, and Prudhoe Bay, Alaska. It will focus on a series of large, shallow (5-7 meters deep) lagoons that play a role in the transition of materials from land to sea.

Byron Crump, the other OSU oceanographer who is a principal investigator on the project, will focus on the smallest but most abundant organisms in the ecosystem – phytoplankton, bacteria, and other microbes.

“The old school of thinking was that bacteria were important in warmer ecosystems but not so much in colder regions like the Arctic,” Crump said. “We’re finding that isn’t true at all. Bacteria and other tiny organisms play critical roles in maintaining the food web that supports everything from krill to whales as well as important fisheries.”

Crump will look at the growth rates and genomic diversity of microbes, while Spitz will develop computer models that will evaluate how microbes, plankton and other small organisms influence the ecosystem and how they will be affected in the future under different scenarios of warming, increased precipitation and changes in groundwater.

Spitz and Crump are faculty members in OSU’s College of Earth, Ocean, and Atmospheric Sciences.

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Yvette Spitz, 541-737-3227, yspitz@coas.oregonstate.edu;

Byron Crump, 541-737-4369, bcrump@coas.oregonstate.edu

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Photo of Beaufort lagoons (left): https://flic.kr/p/Sp3DZ5

 

 

 

Coastal erosion

Coastal erosion is one of the processes researchers will study.

Anomalous ocean conditions in 2015 may bode poorly for juvenile Chinook salmon survival

NEWPORT, Ore. – Fisheries managers have been predicting a slightly below-average run of spring Chinook salmon on the Columbia River this year but a newly published suggests that it may be worse.

According to researchers from Oregon State University and the National Oceanic and Atmospheric Administration, ocean conditions were historically bad in the spring of 2015, when migrating yearling fish that will comprise the bulk of this spring’s adult Chinook salmon run first went out to sea. In fact, Pacific Decadal Oscillation values – which reflect warm and cold sea surface temperatures – suggest it was one of the warmest nearshore oceans encountered by migrating Chinook salmon dating back to at least 1900.

The lack of food for the salmon in 2015 may have resulted in significant mortality that will show in this year’s run of Columbia River springers. One way or another, it will provide new information on fish survival and whether juvenile salmon prey data can help resource managers predict future returns.

Results of the research, which was funded by the Bonneville Power Administration and NOAA, have just been published in the journal Marine Ecology Progress Series.

About 80 percent of a typical spring Chinook run on the Columbia River come from fish that went out to sea as yearlings two years earlier, according to lead author Elizabeth Daly, a senior faculty research assistant with the Cooperative Institute for Marine Resource Studies, jointly operated by OSU and NOAA out of the Hatfield Marine Science Center in Newport.

“When juvenile salmon first enter the ocean, it is a critical time for them,” Daly said. “They are adjusting to a salt-water environment, they have to eat to survive, and they have to avoid becoming prey themselves. When we sampled juvenile salmon in May and June of 2015, the fish were much smaller and thinner than usual, and many of them had empty stomachs. There just wasn’t anything for them to eat.”

Two key statistics stand out from 2015, the researchers noted. The California Current system off the West Coast was more than 2.5 degrees Celsius (or 4.5 degrees Fahrenheit) warmer than normal, and the juvenile Chinook were smaller and skinnier than during a cold-water year, weighing an average of 17.6 percent less.

When the oceanic waters off Oregon and Washington are cold, young salmon primarily feed on readily available fish prey such as Pacific sand lance and smelts, which triggers their growth spurt. When waters are warmer, there is less food available, and they primarily eat juvenile anchovies and rockfish, which are less-desirable prey than cold-water species.

Daly said 2015 began on a somewhat positive note. Although cold-water larval fish species were absent, the researchers found abundant amounts of other larval fish in January, February and March, the fourth highest biomass in the last 18 years. Thus even in the absence of preferred cold-water species, there was food in the California Current system – at least for a while.

However, by the time the juvenile Chinook salmon migrated to the ocean later that spring, these larval anchovies and rockfish had all but disappeared – making even backup food sources for the salmon scarce.

The researchers theorize that these larval fish died off because they themselves had little to eat. Long-time NOAA biologist Bill Peterson told Daly and her colleagues that the Pacific Ocean off the Northwest coast in early 2015 was devoid of cold-water, lipid-rich copepods, a key element in the food chain. In 2015, it was so warm offshore that virtually no lipid-rich copepods were to be found.

“We think the larval anchovies and rockfish had nothing to eat, so they died off,” Daly said. “So when the salmon entered the ocean later that spring of 2015, the cupboard was bare.”

“During warm years, there is typically less upwelling that brings cold, nutrient-rich water to the surface,” said Richard Brodeur, a biologist with the NOAA Northwest Fisheries Science Center and co-author on the study. “Salmon populations may be able to handle one year of warm temperatures and sparse food. But two or three years in a row could be disastrous.”

“The young salmon may have to travel farther north to find food, and they become highly susceptible to becoming prey themselves because of their weakened condition.”

Preliminary results from 2016 by study co-author Toby Auth suggest that ichthyoplankton biomass was again high in late winter, but it was dominated once more by anchovies and sardines, which normally spawn off Oregon in summer. Juvenile salmon sampled in the spring were small and somewhat thinner than normal, Daly said.

“For the first time, we found that the salmon were eating juvenile sardines in 2016 – a new prey for them,” she noted. “Sardines were spawning off the central Oregon coast for one of the first times because of the warm water. We don’t know the long-term impact this will have on salmon. Hopefully, it can become a new food source for them if waters remain warm.”

As this year’s run of spring Chinook salmon unfolds on the Columbia River, Daly and her colleagues will be watching to see if the numbers of adult fish returning align with predictions of a poor return based on 2015 ocean conditions, prey availability, and juvenile fish size.

It could provide valuable information to resource managers in the future.

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Elizabeth Daly, 541-270-1370, elizabeth.daly@oregonstate.edu;

Ric Brodeur, 541-867-0335, Richard.Brodeur@noaa.gov

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OSU to expand sediment core collection to one of largest in the world

CORVALLIS, Ore. – One of the nation’s most important repositories of oceanic sediment cores, located at Oregon State University, will more than double in size later this year when the university assumes stewardship of a collection of sediment cores taken from the Southern Ocean around Antarctica.

OSU has received a pair of grants from the National Science Foundation to assume the curatorial stewardship of the Antarctic and Southern Ocean National Collection of Rock and Sediment Cores, housed at Florida State University since the mid-1960s. Oregon State will house the expanded collection in a sophisticated new facility located just off-campus.

NSF manages the U.S. Antarctic Program, whose logistical support and awards to researchers allowed many of the cores to be obtained.

The OSU Marine and Geology Repository will be available to scientists around the world to study the sediment cores, which provide evidence of the Earth’s climate over the past millions of years, oceanic conditions, the history of the magnetic field, plate tectonics, seismic and volcanic events, ice ages and interglacial periods, and even the origin of life.

“These cores are time capsules, allowing scientists today to compare the conditions on the Earth we live in with the way it was eons ago,” said Thom Wilch, Earth Sciences program manager at NSF. “This collection of cores and samples is an incredible resources that has yielded many important scientific findings about the past. Preservation and curation by OSU ensures that the cores are available for future research by the national and international scientific communities.”

Oregon State has operated a sediment core lab since the 1970s, but its origins were rather modest, according to Joseph Stoner, a geologist in the College of Earth, Ocean, and Atmospheric Sciences and co-director of the OSU Marine and Geology Repository. Lacking a storage facility, the first cores were kept in a cooler at a Chinese restaurant in Corvallis.

From those humble beginnings, the repository has grown into a treasure trove for scientists, storing thousands of cores – mostly from the Pacific Ocean, with a few from the Arctic, Bering Sea, and many terrestrial lakes. The collection also includes dry terrestrial cores and dredged rocks from submarine volcanoes and the ocean floor.

“The expanded collection will include some 35 kilometers, or about 22 miles, of sediment cores, more than doubling the size of our current repository at Oregon State,” Stoner said. “OSU already shares on average 5,000 subsamples of the cores with scientists each year – a number that will more than double with the expansion.”

When completed over the next two years, the expanded repository will give Oregon State the premier collection of sediment cores from the Pacific and Southern oceans. It is difficult to put a dollar value on the cores, OSU researchers say, though their worth can be calculated in a different way.

“If we had to replace the cores in our current OSU repository, it would cost roughly a half billion dollars just in ship time to go collect them,” Stoner said. “That doesn’t include the cost of the people involved. To replace the Antarctic collection would easily cost more than $1 billion, since the Southern Ocean is so remote, travel is difficult, and you can only work two or three months out of the year.”

The real worth, though, is the cores’ scientific value, noted Anthony Koppers, co-director of the OSU repository and also a faculty member in the College of Earth, Ocean, and Atmospheric Sciences. The OSU collection includes cores that have sediments as old as 50 million years, and from as deep as a kilometer below the Earth’s surface.

The new Antarctic collection has the most complete set of cores from the Southern Ocean in the world and those cores provide an important look into the Earth’s climate history over the last few million years. The Southern Ocean collection also includes numerous cores gathered under the NSF-funded international Antarctic DRILLing Project (ANDRILL) program and provides clues to the history of the Antarctic Ice Sheet over the past 17 million years.

“This will bring a lot of researchers from around the world to Oregon State,” Koppers said. “The Antarctic research community is very active, very enthusiastic, and very diverse. With our new facility, we will have the capacity to work with researchers in numerous disciplines studying a variety of scientific questions.”

Oregon State will spend the next several months preparing the new facility, which will be unlike almost every other repository in the world. It will have a refrigerated industrial storage space of 18,000 square feet, the researchers note, providing plenty of room for the collection to grow over the next five decades.

The size of the facility likely will lead to other collections moving to Oregon State, Koppers predicted.

“Most core repositories are starving for space,” he said. “We anticipate hearing from them as word about the transfer and our new facility gets out.”

The new repository facility will occupy much of the former Nypro Building in Corvallis. In addition to the enormous refrigerated storage area, which has 28-foot-high ceilings for both cold and dry storage, it will include:

  • Up to 11 laboratory areas, including facilities for core splitters, imagery, microscopy, rock analysis, sediment analysis CT scanning and other scanning techniques;
  • Freezer storage for frozen ice cores from Greenland and Antarctica;
  • A laboratory where researchers can work on eight different cores at once while using digital imaging and data from the individual cores displayed on large-screen computer monitors;
  • A seminar room for 35 people, where cores can be brought in for classes and presentations;
  • Office space for resident scientists, staff, and visiting scientists.

Florida State University made the decision in 2015 not to compete for renewal as its Earth, Ocean, and Atmospheric Science program was moving in a different academic direction. Koppers and Stoner submitted a bid for Oregon State to acquire the collection and were awarded two grants from NSF to transfer the Antarctic collection and to provide stewardship for it.

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Joseph Stoner, 541-737-9002, jstoner@coas.oregonstate.edu;

Anthony Koppers, 541-737-5425, akoppers@coas.oregonstate.edu

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(Photo available at: https://flic.kr/p/QRcnho)

Scientists: Warming temperatures could trigger starvation, extinctions in deep oceans by 2100

CORVALLIS, Ore. – Researchers from 20 of the world’s leading oceanographic research centers today warned that the world’s largest habitat – the deep ocean floor – may face starvation and sweeping ecological change by the year 2100.

Warming ocean temperatures, increased acidification and the spread of low-oxygen zones will drastically alter the biodiversity of the deep ocean floor from 200 to 6,000 meters below the surface. The impact of these ecosystems to society is just becoming appreciated, yet these environments and their role in the functioning of the planet may be altered by these sweeping impacts. 

Results of the study, which was supported by the Foundation Total and other organizations, were published this week in the journal Elementa.

“Biodiversity in many of these areas is defined by the meager amount of food reaching the seafloor and over the next 80-plus years – in certain parts of the world – that amount of food will be cut in half,” said Andrew Thurber, an Oregon State University marine ecologist and co-author on the study. “We likely will see a shift in dominance to smaller organisms. Some species will thrive, some will migrate to other areas, and many will die. 

“Parts of the world will likely have more jellyfish and squid, for example, and fewer fish and cold water corals.”

The study used the projections from 31 earth system models developed for the Intergovernmental Panel on Climate Change to predict how the temperature, amount of oxygen, acidity (pH) and food supply to the deep-sea floor will change by the year 2100. The authors found these models predict that deep ocean temperatures in the “abyssal” seafloor (3,000 to 6,000 meters deep) will increase as much as 0.5 to 1.0 degrees (Celsius) in the North Atlantic, Southern and Arctic oceans by 2100 compared to what they are now. 

Temperatures in the “bathyal” depths (200 to 3,000 meters deep) will increase even more – parts of this deep-sea floor are predicted to see an increase of nearly 4 degrees (C) in the Pacific, Atlantic and Arctic oceans.

“While four degrees doesn’t seem like much on land, that is a massive temperature change in these environments,” Thurber said. “It is the equivalent of having summer for the first time in thousands to millions of years.” 

The over-arching lack of food will be exacerbated by warming temperatures, Thurber pointed out.

“The increase in temperature will increase the metabolism of organisms that live at the ocean floor, meaning they will require more food at a time when less is available.” 

Most of the deep sea already experiences a severe lack of food, but it is about to become a famine, according to Andrew Sweetman, a researcher at Heriot-Watt University in Edinburgh and lead author on the study.

“Abyssal ocean environments, which are over 3,000 meters deep, are some of the most food-deprived regions on the planet,” Sweetman said. “These habitats currently rely on less carbon per meter-squared each year than is present in a single sugar cube. Large areas of the abyss will have this tiny amount of food halved and for a habitat that covers half the Earth, the impacts of this will be enormous.” 

The impacts on the deep ocean are unlikely to remain there, the researchers say. Warming ocean temperatures are expected to increase stratification in some areas yet increase upwelling in others. This can change the amount of nutrients and oxygen in the water that is brought back to the surface from the deep sea. This low-oxygen water can affect coastal communities, including commercial fishing industries, which harvest groundfish from the deep sea globally and especially in areas like the Pacific Coast of North America, Thurber said.

“A decade ago, we even saw low-oxygen water come shallow enough to kill vast numbers of Dungeness crabs,” Thurber pointed out. “The die-off was massive.” 

Areas most likely to be affected by the decline in food are the North and South Pacific, North and South Atlantic, and North and South Indian oceans.

“The North Atlantic in particular will be affected by warmer temperatures, acidification, a lack of food and lower oxygen,” Thurber said. “Water in the region is soaking up the carbon from the atmosphere and then sending it on its path around the globe, so it likely will be the first to feel the brunt of the changes.” 

Thurber, who is a faculty member in Oregon State’s College of Earth, Ocean, and Atmospheric Sciences and the OSU College of Science, has previously published on the “services” or benefits provided by the deep ocean environments. The deep sea is important to many of the processes affecting the Earth’s climate, including acting as a “sink” for greenhouse gases and helping to offset growing amounts of carbon dioxide emitted into the atmosphere.

These habitats are not only threatened by warm temperatures and increasing carbon dioxide; they increasingly are being used by fishing and explored by mining industries for extraction of mineral resources. 

“If we look back in Earth’s history, we can see that small changes to the deep ocean caused massive shifts in biodiversity,” Thurber said. “These shifts were driven by those same impacts that our model predict are coming in the near future. We think of the deep ocean as incredibly stable and too vast to impact, but it doesn’t take much of a deviation to create a radically altered environment.

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Andrew Thurber, 541-737-4500, athurber@coas.oregonstate.edu; Andrew Sweetman, +44 (0) 131 451 3993, a.sweetman@hw.ac.uk

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Sea pig (Image Courtesy of Ocean Networks Canada)

SeaPig

Methane seep (Image by Andrew Thurber, OSU)

CRSeep

Marine ecologist offers suggestions for achieving a strong, lasting ‘blue economy’

BOSTON – Incentive-based solutions offer significant hope for addressing the myriad environmental challenges facing the world’s oceans – that’s the central message a leading marine ecologist delivered today in during a presentation at the annual meeting of the American Association for the Advancement of Science. 

Jane Lubchenco, a distinguished professor in the Oregon State University College of Science, shared lessons from around the world about ways “to use the ocean without using it up” as nations look to the ocean for new economic opportunities, food security or poverty alleviation.

Elizabeth Cerny-Chipman, a former postdoctoral scholar under Lubchenco who’s now a Knauss Fellow at the National Oceanic and Atmospheric Administration, co-authored the presentation, titled “Getting Incentives Right for Sustained Blue Growth: Science and Opportunities.”

In her presentation, Lubchenco pointed out that achieving the long-term potential of blue growth will require aligning short- and long-term economic incentives to achieve a diverse mix of benefits. Blue growth refers to long-term strategies for supporting sustainable growth in the marine and maritime sectors as a whole.

“If we harness human ingenuity and recognize that a healthy ocean is essential for long-term prosperity, we can tackle the enormous threats facing the ocean,” Lubchenco says, “and we can make a transition from vicious cycles to virtuous cycles.”

Lubchenco and her collaborators note that the world’s oceans are the main source of protein production for 3 billion people; are directly or indirectly responsible for the employment of more than 200 million people; and contribute $270 billion to the planet’s gross domestic product.

“The right incentives can drive behavior that aligns with both desired environmental outcomes and desirable social outcomes,” Lubchenco says.

The first step in building increased support for truly sustainable blue growth, she says, is highlighting its potential. That means working with decision-makers to promote win-win solutions with clear short-term environmental and economic benefits. Governments, industry and communities all have important roles to play, Lubchenco notes.

“Another key step is transforming the social norms that drive the behavior of the different actors, particularly in industry,” Lubchenco says. “Finally, it will be critical to take a cross-sector approach.

“Some nations, like the Seychelles, Belize and South Africa, are doing integrated, smart planning to deconflict use by different sectors while also growing their economies in ways that value the health of the ocean, which is essential to jobs and food security. They are figuring out how to be smarter about ocean uses, not just to use the ocean more intensively.”

Prior to her presentation, Lubchenco gave a related press briefing on how to create the right incentives for sustainable uses of the ocean.

In November 2016, Lubchenco, Cerny-Chipman, OSU graduate student Jessica Reimer and Simon Levin, the distinguished university professor in ecology and evolutionary biology at Princeton University, co-authored a paper on a related topic for the Proceedings of the National Academy of Sciences.

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By Steve Lundeberg, 541-737-4039

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Catch share

"Catch share" fisheries program

2015-16 weather event took toll on California beaches; not so much for Oregon, Washington

CORVALLIS, Ore. – The 2015-16 El Niño was one of the strongest climate events in recent history with extraordinary winter wave energy, a new study shows, though its impact on beaches was greater in California than in Oregon and Washington.

The reason, researchers say, is that the Pacific Northwest had experienced comparatively mild wave conditions in the years prior to the onset of the El Niño, while California was experiencing a severe drought and “sediment starvation.”

Results of the study are being published this week in Nature Communications.

“Rivers still supply the primary source of sand to California beaches, despite long-term reductions due to extensive dam construction,” said Patrick Barnard, a geologist with the U.S. Geological Survey and lead author on the study. “But as California was in the midst of a major drought, the resulting lower river flows equated to even less sand being carried to the coast to help sustain beaches.

“Therefore, many of the beaches in California were in a depleted state prior to the El Niño winters, and thereby were subjected to extreme and unprecedented landward erosion due to the highly energetic winter storm season of 2015-16.”

The West Coast, on average, experienced a “shoreline retreat” – or degree of beach erosion – that was 76 percent above normal and 27 percent higher than any other winter on record, eclipsing the El Niño events of 2009-10 and 1997-98. Coastal erosion was greatest in California, where 11 of the 18 beaches surveyed experienced historical levels of erosion.

Peter Ruggiero, an Oregon State University coastal hazards expert and co-author on the study, said Oregon and Washington were not affected to the same extent.

“You would have thought that there would be massive damage associated with erosion in Oregon and Washington with the strength of this El Niño,” said Ruggiero, a professor in OSU’s College of Earth, Ocean, and Atmospheric Sciences. “But the previous three years had mild winters and therefore the sand buildup was much higher than in California. It helped the Northwest offset the potential erosion from the El Niño.”

Oregon and Washington also have broader beaches than in California, Ruggiero pointed out, which also eases the erosion of sand dunes and impacts to development.

The 2015-16 El Niño, in some ways, was stronger than the 1982-83 event, which caused an estimated $11.5 billion in damages, the researchers say in the study. Only a portion of the damage was directly related to coastal erosion, with damage to houses and roads, they note. Most of the impact was from related storms, flooding and other damage that occurred inland.

The Nature Communications study is important, the authors say, because it is one of the first attempts to document the oceanographic “forcing” directly related to beach impacts created by El Niño. The study documents the amount of power created by winter storm waves, using height and “period” – or the length of time between waves. It is the level of forcing, along with relative beach health, that dictates the amount of erosion that occurs and the associated impacts from that erosion.

“During an El Niño, the nearshore experiences higher water levels because of the storms and the fact that the water is warmer and expands,” Ruggiero said. “In Oregon, the water was about 15-17 centimeters (roughly 6-7 inches) higher than average, which led to higher storm tides.”

Although Northwest beaches were buffered from catastrophic damage, Ruggiero said, they did experience significant retreat. And it may take a while for the beaches to rebuild.

“We’re not completely recovered yet, and it may take years for some beaches to build back up,” he said. “After the 1997-98 El Niño, it took some beaches a decade to recover.”

Ruggiero, his students and colleagues have been monitoring Northwest beaches since 1997, and in 2015, they received a National Science Foundation rapid response grant to study the impact of El Niño on beaches. Ruggiero also receives support from the Northwest Association of Networked Ocean Observing Systems (NANOOS) and the U.S. Army Corps of Engineers for additional monitoring.

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Peter Ruggiero, 541-737-1239, pruggier@coas.oregonstate.edu; Patrick Barnard, 831-460-7556, pbarnard@usgs.gov

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South Beach, Oregon
Oregon's South Beach

 

(Left: Crescent Beach in Callifornia. Photos by Nick Cohn, Oregon State University. https://flic.kr/p/RwDLsb)