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Recent research outlines the severe consequences that bottom trawling has on loose sediment on the ocean floor.

Bottom trawling is a widespread industrial fishing practice that involves dragging heavy nets, large metal doors, and chains over the seafloor to catch fish. Although previous studies have documented the direct impacts of bottom trawling on corals, sponges, fishes, and other animals, an understanding of the global impact of this practice on the seabed remained unclear until now. The first calculation of how much of the seabed is resuspended (or stirred up) by bottom-trawling shows that the sediment mass is approximately the same as the amount of all sediment being deposited on the world’s continental shelves by rivers each year (almost 22 gigatons). 

Understanding regional and global magnitudes of resuspended sediment is essential for analyzing the environmental consequences of trawling for continental shelf habitats and their associated seafloor and open-ocean ecosystems. The scientists compared natural causes of resuspension (waves and currents) with bottom trawling-induced resuspension and found new ways to look at and into the seabed to document the effects of bottom trawling. 

Conceptual drawing of bottom trawling from a fishing boat, showing a net and metal plate being dragged behind a boat.
Conceptual drawing of bottom trawling from a fishing boat, showing a net and metal plate being dragged along the seafloor behind a boat on the surface.

Bottom trawling can produce vastly different effects on different types of seabed sediment (such as sand, silt, or mud), each with different ecological consequences. Trawling destroys the natural seafloor habitat by essentially rototilling the seabed. All of the bottom-dwelling plants and animals are affected, if not outright destroyed, by tearing up root systems or animal burrows. Resuspending bottom sediment changes the entire chemistry of the water, including nutrient levels. Resuspended sediment can lower light levels in the water and reduce photosynthesis in ocean-dwelling plants, the foundation of the food web. The resuspended sediment is carried away by currents and often lost from the local ecosystem. It may be deposited elsewhere along the continental shelf, or in many cases, permanently lost from the shelf to deeper waters. Changing parts of the seafloor from soft mud to bare rock can eliminate those creatures that live in the sediment. Species diversity and habitat complexity are directly affected when trawling changes the physical environment of sand, mud, or rock. 


Photo shows the back of the (R/V) Meteor, floating on the ocean.
Picture of the back of the (R/V) Meteor as it floats on the ocean, photo by Ferdinand Oberle.
Side-on photograph of the research vessel (R/V) Meteor taken from a distance.
Side view of the oceanographic research vessel (R/V) Meteor floating on the ocean, taken from a distance.


“This study raises serious concerns about the future stability of continental shelves—the very source of the vast majority of the fish we consume,” said geological oceanographer and lead author Ferdinand Oberle, now a visiting scientist at the USGS and previously with the Woods Hole Oceanographic Institution. He was at MARUM, the Center for Marine Environmental Sciences, University of Bremen (Germany), when the study was done. “A farmer would never plow his land again and again during a rainstorm, watching all his topsoil be washed away, but that is exactly what we are doing on continental shelves on a global scale.”  

As part of the study, scientists developed a new, universal approach to calculate bottom-trawling-induced sediment resuspension that gives marine management a new and important tool to assess the impact from bottom trawling. Previous studies characterized the seabed as either “trawled” or “untrawled,” but with these novel methodologies it was possible to show systematically a range of bottom-trawling-induced changes to the seabed and classify them in accordance with how often the seabed was disturbed by bottom trawlers. 


Image shows an overhead view of a piece of scientific equipment being lowered into the water.
Scientific equipment mounted on a tripod being deployed from the R/V Meteor.
Picture shows a bottom trawling boat on the ocean, taken from the deck of the (R/V) Meteor.
One of the many passing bottom trawlers on the northwest Iberian shelf as seen from the R/V Meteor.


“The global calculations were a big surprise, and we calculated them at least 10 times to make sure we were not making a mistake. I am still in awe of these results and their environmental implications,” said USGS oceanographer Curt Storlazzi, a coauthor of the paper who helped develop the computational models for the study.  

These new understandings about the effects of bottom trawling come out of scientific cruises on the research vessel (R/V) Meteor from Germany to the offshore area northwest of the Iberian Peninsula with a team of international scientists. During the cruises, scientists conducted sidescan-sonar surveys and collected bottom current data. Laser sediment-particle samplers and a remotely operated submersible vessel were used as well. After the cruises, scientists conducted laboratory work involving lead-isotope dating and sediment grain-size analysis and developed a sediment-mobilization model, all of which contributed to the conclusions of the study.  

Two new research papers from this study were published in Elsevier’s Journal of Marine Systems and are available online. The full citations are: 

  • Oberle, F.K.J., Storlazzi, C.D., and Hanebuth, T.J.J., What a drag—Quantifying the global impact of chronic bottom trawling on continental shelf sediment: Journal of Marine Systems, published online 30 December 2015,

  • Oberle, F.K.J., Swarzenski, P.W., Reddy, C.M., Nelson, R.K., Baasch, B., and Hanebuth, T.J.J., Deciphering the lithological consequences of bottom trawling to sedimentary habitats on the shelf: Journal of Marine Systems, published online 31 December 2015,

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