Sound of the Deep

Two of the lander systems recorded sound and related parameters such as temperature while they descended, then sat on the bottom for a few hours before returning to the surface. These returned with the deepest sound recordings ever collected. Michael Buckingham from Scripps and David Barclay from the Woods Hole Oceanographic Institution, both experts in ambient ocean noise, led this work. Overall, the team was interested in sound at the bottom of the trench because they want to understand how animals use acoustics in this unique environment.

Many marine animals such as mantis shrimp, reef fish, and dolphins use sound for hunting food, communicating, and other purposes. The team suspects that trench animals might be especially dependent on sound because mates and food in that realm are sparse. A trench is relatively enclosed by steep sides, and in deep waters the high pressure and low temperature cause sound to travel faster. This makes for an environment particularly conducive to the travel and containment of sound, meaning animals might be able to use it to find what they need from far away.

Microbial Role Call

The researchers configured a second group of lander systems with equipment for collecting microbial samples, and for observing—and in some cases capturing—larger animals. Some of the basic tools included lights, video cameras, and baited traps to collect species like crustaceans known as amphipods, that have proven to be one of the most common residents of hadal (below 6,000 meters) waters during past research.

One goal was to coordinate lander deployments in hopes of using video and possibly even trapped samples to identify the animals responsible for sounds that the Deep Sound landers record. So little work has been done in the hadal zone, that there is really no telling yet what they will see, hear, or collect.

Bartlett and his colleagues analyzed animal samples from the traps and sediment cores to determine what bacteria are present in their bodies. They also used various strategies to collect other bacteria for work on understanding how these organisms are able to survive the mind boggling pressures found at these great depth. At the deepest point, the pressure is about 11,250 kilograms per square meter (16,000 pounds per square inch), or roughly equivalent to balancing three SUVs on your big toe.

One method was to attach small, pressurized samplers developed at Old Dominion University in Virginia that had never been used before at such great depths. These instruments collect water samples and maintain the high pressure and low temperature conditions at the bottom. Samples will be kept under the same conditions onFalkor and ultimately returned to Bartlett’s lab for experiments with the live bacteria.

For instance, Bartlett and his colleagues looked at what effect lowering and raising pressure has on the microbes present, including analyses of the genes that are active, and the compounds the bacteria produce. By experimenting at different pressures Bartlett hopes to better understand how the microbes survive the high pressures. He and his colleagues have already discovered certain compounds that appear to be critical to bacterial survival under very high pressures and further work could identify others.

Intriguing Fixation

In related work, the team outfited certain water sampling bottles with packets of fixative whose release was triggered once a sample bottle closes. This chemical effectively freezes molecular activity, so genetic material—specifically RNA—can later be analyzed. This will help in understanding the genetic makeup of bacteria in the water samples, offering clues as to which genes are important for withstanding pressure. Analyses can also reveal bacteria that are alive and active, which is a key question as numerous bacterial species not capable of surviving the pressure end up on the trench bottom after falling there dead or inactive.

Food Puzzle

The team searched for genes tied to the consumption of hydrogen as an energy source. This relates to a fundamental question about trench bacterial life—whether the diverse species found there depend more on food that rains down from above in the form of decaying biological material, or food that is produced at the seafloor.

An important process called serpentinization may be at play. This involves water seeping down or otherwise coming in contact with mantle rock from beneath the seafloor to produce serpentine, or asbestos. The process gives off heat, hydrogen, and minerals that can support bacterial life.

Genes for hydrogen consumption could suggest dependence on serpentinization. Scientists found some evidence of exposed rocks produced by the phenomenon and bacterial use of the byproducts of serpentinization during the James Cameron DEEPSEA CHALLENGER expedition, for which Bartlett was the chief scientist. During the December cruise the team attempted to return a lander to the vicinity of that work to further their studies.

Lander Advancement

Another group goal was to test additional technologies aimed at advancing lander science. For instance, they used a type of structural foam developed for James Cameron’s expedition that provides buoyancy and structural rigidity while avoiding the need for glass spheres commonly used for buoyancy in the deep sea. These spheres have a number of drawbacks including the potential for damaging implosions and a relatively short lifespan.

The team deployed their landers as many times as possible, and left one lander on the bottom at the end of the cruise for retrieval during a future expedition. This will enable a long-term study of how microbes in this deep zone colonize wood and other materials placed strategically on the lander.