Low-oxygen impacts on West Coast groundfish, research shows

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http://www.sciencedaily.com/releases/2015/03/150311160529.htm

Low-oxygen impacts on West Coast groundfish, research shows
Date: March 11, 2015
Source: NOAA Fisheries West Coast Region
Summary: Low-oxygen waters projected to expand with climate change create winners and losers among deep-dwelling groundfish, new research shows. Some species are adapted to handle low-oxygen conditions such as those increasingly documented off the West Coast, while the same conditions drive other species away.

Researchers developed a sturdy, protective housing for oxygen sensors attached to trawl nets to protect them from damage. Survey vessels now carry such sensors on all of their tows to document associations between species and dissolved oxygen levels.

Credit: NOAA Fisheries/Northwest Fisheries Science Center
[Click to enlarge image] http://images.sciencedaily.com/2015/03/150311160529-large.jpg
When low-oxygen "dead zones" began appearing off the Oregon Coast in the early 2000's, photos of the ocean floor revealed bottom-dwelling crabs that could not escape the suffocating conditions and died by the thousands.

Ecological succession
But the question everyone asked was, "What about the fish?" recalls Oregon State University oceanographer Jack Barth. "We didn't really know the impacts on fish. We couldn't see them."

Scientists from NOAA Fisheries' Northwest Fisheries Science Center and Oregon State have begun to answer that question with a new paper published in the journal Fisheries Oceanography. The paper finds that low-oxygen waters projected to expand with climate change create winners and losers among fish, with some adapted to handle low-oxygen conditions that drive other species away.

Generally the number of fish species declines with oxygen levels as sensitive species leave the area, said Aimee Keller, a fisheries biologist at the Northwest Fisheries Science Center and lead author of the new paper. But a few species such as Dover sole and greenstriped rockfish appear largely unaffected.

"One of our main questions was, 'Are there fewer species present in an area when the oxygen drops?' and yes, we definitely see that," Keller said. "As it goes lower and lower you see more and more correlation between species and oxygen levels."

Deep waters off the West Coast have long been known to be naturally low in oxygen. But the new findings show that the spread of lower oxygen conditions, which have been documented closer to shore and off Washington and California, could redistribute fish in ways that affect fishing fleets as well as the marine food chain.

The lower the oxygen levels, for example, the more effort fishing boats will have to invest to find enough fish.

"We may see fish sensitive to oxygen levels may be pushed into habitat that's less desirable and they may grow more slowly in those areas," Keller said.

Researchers examined the effect of low-oxygen waters with the help of West Coast trawl surveys conducted every year by the Northwest Fisheries Science Center to assess the status of groundfish stocks. They developed a sturdy, protective housing for oxygen sensors that could be attached to the trawl nets to determine what species the nets swept up in areas of different oxygen concentrations.

The study combined the expertise of fisheries scientists such as Keller who assess fish stocks with oceanographers such as Barth who track ocean conditions to look at the relationship between the two.

"Initially, we would tell them where the low oxygen was, and they would trawl within areas ranging from low to high oxygen," Barth explained. Later, oxygen sensors were deployed on all tows during the groundfish survey. "They would look at the catch and the species richness. We tried to get it down to the individual species level, where we could tell which fish correlated with which oxygen levels."
Low-oxygen waters appear off the West Coast in two ways, Barth said. The first is the eastward movement of deep, oxygen-poor water that laps up against the West Coast. The second occurs when wind-driven upwelling brings nutrients to the surface, fueling blooms of phytoplankton that eventually die and sink to the bottom. Their decay then consumes the oxygen, leaving what scientists call hypoxic conditions where oxygen levels are low enough to adversely affect marine organisms.

The scientists examined the effects of varying oxygen levels on four representative species: spotted ratfish, petrale sole, greenstriped rockfish and Dover sole.

Spotted ratfish and petrale sole were the most sensitive to changes in oxygen levels, with their presence declining sharply as the amount of oxygen dissolved in the water declines. But greenstriped rockfish and Dover sole were largely unaffected by dissolved oxygen levels.

Dover sole is adapted to low-oxygen waters, with gill surface areas two to three times larger than other fish of similar size that allow it to absorb more oxygen from the same amount of water. Dover sole also are among a few fish species that can reduce their oxygen consumption to very low concentrations, probably an adaptation to low-oxygen conditions.

The research is continuing, with trawl survey vessels carrying oxygen sensors on all of their tows since 2009, Keller said. Further data should provide insight into the response of additional fish species to low oxygen conditions, Keller said.

Story Source: The above story is based on materials provided by NOAA Fisheries West Coast Region. Note: Materials may be edited for content and length.

Journal Reference: Aimee A. Keller, Lorenzo Ciannelli, W. Waldo Wakefield, Victor Simon, John A. Barth, Stephen D. Pierce. Occurrence of demersal fishes in relation to near-bottom oxygen levels within the California Current large marine ecosystem. Fisheries Oceanography, 2015; 24 (2): 162 DOI: 10.1111/fog.12100 http://dx.doi.org/10.1111/fog.12100
 
http://www.iflscience.com/environment/ocean-dead-zones-are-spreading-and-spells-disaster-fish

Ocean 'Dead Zones' Are Spreading – And That Spells Disaster For Fish

April 9, 2015 | by Lee Bryant


Photo credit: Fish can suffocate too. Bruce Evans, CC BY-NC-SA

Falling ocean oxygen levels due to rising temperatures and influence from human activities such as agrochemical use is an increasingly widespread problem. Considering that the sea floors have taken more than 1,000 years to recover from past eras of low oxygen, according to a recent University of California study, this is a serious problem.

Ocean regions with low oxygen levels have a huge impact on aquatic organisms and can even destroy entire ecosystems. Areas of extremely low oxygen, known as oxygen minimum zones or “dead zones”, are estimated to constitute 10% and rising of the world’s ocean.

This expansion has been attributed to a warming climate, which increases water temperature, changes ocean circulation, and decreases the solubility of oxygen in sea water. At the same time fertiliser and pesticide run-off from farming and other human activities leads to rising levels of nutrients such as nitrogen and phosphorous reaching the sea.

Together, these two processes speed up the release of chemicals from ocean sediments and promote algal blooms. Subsequent algal death and decay result in increased consumption of oxygen in the water. The result is that other aquatic species such as invertebrates on the seafloor and fish suffocate for lack of oxygen.

Due to circulation and runoff effects, dead zones are especially severe around large cities on the western continental coasts such as the coast of Peru, and within enclosed or semi-enclosed regions like the Baltic Sea or Gulf of Mexico.
Oxygen levels at 300m, with extremely low oxygen oceanic ‘dead zones’ marked in red. World Ocean Atlas/Max Planck Institute for Marine Microbiology, Author provided

Looking to the past

What effects will these changes have? We don’t yet know how great the effects of human-caused climate change will be, nor how much can be done to try and mitigate the effects on the environment. Even if oceanic oxygen levels rise again, will the world’s ocean ecosystems be able to recover?

The University of California study, published in the Proceedings of the National Academy of Sciences, studies fossils of over 5,400 sea animals including seed shrimps, molluscs, and brittle stars in order to try and answer this question. By examining seafloor sediments the researchers assessed how global warming affected sealife during the transition from the last ice age to the more-recent interglacial period, between 17,000-3,000 years ago.

What the study found was that within only 130 years the oceans underwent devastating changes that led to complete collapse of invertebrates on the seafloor. More worryingly, the fossil records show that ecosystem recovery took at least 1,000 years.

So the current growth of dead zones could leave drastic and long-lasting changes to marine life biodiversity. Climate change caused by human activity has already caused significant environmental damage over a relatively short time – the vast increase in pollution, ocean acidification, overfishing and deforestation in just the last 50-100 years, for example. However long it takes us to reverse the effects of global warming, if indeed we can, it will likely take ocean ecosystems many orders of magnitude longer to recover.

Headed for collapse?

Though microscopic organisms residing in the ocean and on the seafloor might seem to have little relevance to us, even small changes in ocean ecosystems can have enormous effects on the entire ocean food chain, from the smallest bacteria to the largest fish. Any impact on the creatures higher up in the food chain will have a massive impact on the human communities that rely on them economically and as a food source.

Algal blooms - the green sludge - are on the rise. Lee Bryant, Author provided

Studies have shown that populations of mid-water fish such as Pacific hake decreased by up to 60% during periods of low oxygen off the coast of Southern California.

Conversely, numbers of Humboldt squid, which are more tolerant of low-oxygen waters, have increased significantly in the same location. Even the fish that can survive in dead zones are not faring well: large numbers of female Atlantic Croaker have been found to be growing testes-like organs instead of ovaries, a sexual deformation which causes infertility.

Feedback loop

Any shifts in ecosystem biodiversity can lead to a vicious feedback loop: dead zone seafloors turn into biodiversity deserts, where little but methane- and hydrogen sulphide-producing bacteria survive. Paired with changes in nutrient cycling which result in the release of nitrogen gas, levels of greenhouse gases being released from the ocean to the atmosphere increase and contribute to further global warming.

To prevent the possibility of a 1,000-year (or longer) recovery period from a dead zone seafloor, we need to be much more aware of how the various environmental aspects are connected. An understanding of how de-oxygenation has affected the ocean in the past and how our actions are affecting the ocean in the present is critical to either preventing a recurrence or at least minimising effects of what we have already done.
 

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http://www.sciencedaily.com/releases/2015/04/150409162451.htm

Dynamic dead zones alter fish catches in Lake Erie

Date: April 9, 2015

Source: United States Geological Survey

Summary: Lake Erie's dead zones are actually quite active, greatly affecting fish distributions, catch rates and the effectiveness of fishing gear, scientists report. "Our study shows that Lake Erie contains a patchwork of low and high-density fish populations," said a researcher. "This understanding of fish distributions can inform policy decisions, such as how many walleye, yellow perch and others can be fished from the lake."

New research shows that Lake Erie's dead zones are actually quite active, greatly affecting fish distributions, catch rates and the effectiveness of fishing gear.

Scientists with the U.S. Geological Survey, the Illinois-Indiana Sea Grant and partners recently found that dead zones caused by hypoxia, the depletion of oxygen in water, are unexpectedly variable in Lake Erie, sometimes disappearing and reemerging elsewhere in the matter of hours. They also found that fish like yellow perch cluster at the edges of these areas. The discovery of erratic dead zones can help commercial fishers and scientists determine where and how to effectively catch and study fish.

The study, conducted near Fairport Harbor, Ohio, during August and September of 2011-2013, was recently published in the Canadian Journal of Fisheries and Aquatic Sciences.

"We were amazed by how quickly hypoxic areas moved during our study," said Richard Kraus, a USGS scientist and the lead author. "These findings can help managers sustain valuable fish populations in Lake Erie, which is one of the world's largest commercial fisheries."

Hypoxia at the bottom of Lake Erie occurs during the summer as a result of biological activity in the colder bottom layer that consumes dissolved oxygen in the water. The warmer surface layer floats on top, preventing oxygen from mixing down to the bottom. The researchers used sensors to measure oxygen levels and lakebed temperatures, and found that dead zones are frequently moving as a result of internal waves in the lake.

Although bottom waters might be a refuge for cool-water fish species, hypoxia can force fish to seek less suitable habitats. Acoustic surveys during the study revealed that when fish shift because of seasonal hypoxia, they cluster at the edges of dead zones rather than avoiding hypoxic areas entirely. Using fishing gear like trawls and nets, the scientists caught fish at the highest rates along dead zone boundaries.

"Our study shows that Lake Erie contains a patchwork of low and high-density fish populations," said Paris Collingsworth, a Great Lakes Ecosystem Specialist with Sea Grant. "This understanding of fish distributions can inform policy decisions, such as how many walleye, yellow perch and others can be fished from the lake."

Story Source: The above story is based on materials provided by United States Geological Survey. Note: Materials may be edited for content and length.

Journal Reference: 1.Richard T. Kraus, Carey T. Knight, Troy M. Farmer, Ann Marie Gorman, Paris D. Collingsworth, Glenn J. Warren, Patrick M. Kocovsky, Joseph D. Conroy, Yves Prairie. Dynamic hypoxic zones in Lake Erie compress fish habitat, altering vulnerability to fishing gears1. Canadian Journal of Fisheries and Aquatic Sciences, 2015; 1 DOI: 10.1139/cjfas-2014-0517 http://dx.doi.org/10.1139/cjfas-2014-0517
 
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