What Lives at the Bottom of Challenger Deep?

The Challenger Deep, located within the Mariana Trench in the western Pacific Ocean, represents the deepest known point in Earth’s oceans. Plunging to an estimated 10,935 meters (35,876 feet) below sea level, this extreme environment has captivated scientists and explorers. They seek to understand what life can endure its conditions. The existence of organisms in such an inhospitable place challenges our understanding of life’s limits.

Conditions of the Challenger Deep

The Challenger Deep is characterized by environmental extremes that pose significant challenges for life. The hydrostatic pressure at its bottom is immense, exceeding 1,000 times the atmospheric pressure at sea level, reaching approximately 1,086 bars or 15,750 pounds per square inch (psi). This pressure is equivalent to an elephant standing on your thumb.

Temperatures in this deep-sea environment are near freezing, typically 1 to 4 degrees Celsius (34 to 39 degrees Fahrenheit). The complete absence of sunlight means the Challenger Deep exists in perpetual darkness, eliminating photosynthesis as a basis for the food web. Food and nutrient availability are scarce, as organic matter from the surface slowly drifts down. These combined factors make the discovery of life within it noteworthy.

Creatures of the Abyss

Despite the harsh conditions, various organisms inhabit the Challenger Deep. Single-celled organisms such as xenophyophores (giant amoebas) have been discovered. Other inhabitants include invertebrates like amphipods (small crustaceans), marine worms (polychaete and scale worms), shrimp, and sea cucumbers.

While fish are generally found at shallower hadal depths, the Mariana snailfish (Pseudoliparis swirei) is a notable exception, thriving at depths up to 8,000 meters (26,200 feet) in the Mariana Trench. This pale, scaleless, tadpole-like fish can reach nearly 29 centimeters. These deep-sea creatures often display translucent, gelatinous bodies, reflecting their adaptations to their environment.

Unique Survival Strategies

The organisms of the Challenger Deep have evolved adaptations to survive the extreme pressure. Many deep-sea creatures lack gas-filled organs like swim bladders, relying instead on specialized fatty tissues or flexible, less calcified skeletal structures. Their cell membranes have higher concentrations of unsaturated fatty acids, allowing them to remain fluid and functional under high pressure. Proteins contain modifications and produce piezolytes, such as trimethylamine N-oxide (TMAO), which stabilize proteins and prevent them from denaturing under intense pressure.

Adaptations to the cold include slow metabolic rates, which allow these organisms to conserve energy in a food-scarce environment. Some deep-sea invertebrates can survive for months without food.

In the absence of sunlight, these creatures rely on alternative energy sources. Chemosynthesis, where microorganisms use chemical energy from vents and seeps to produce food, forms the base of some deep-sea food webs. Many organisms feed on detritus, or “marine snow,” which is organic matter drifting down from the upper ocean layers. Bioluminescence is used by some creatures for communication or hunting in the darkness.

Unveiling the Deep

Exploring the Challenger Deep requires specialized technology due to its extreme conditions. The history of deep-sea exploration includes significant milestones, such as the 1960 descent by Jacques Piccard and Don Walsh in the Bathyscaphe Trieste. They reached a depth of approximately 10,916 meters, spending about 20 minutes on the seafloor.

In 2012, James Cameron made a solo dive in the Deepsea Challenger, which was equipped with scientific instruments and 3D cameras. Modern exploration utilizes uncrewed vehicles, including remotely operated vehicles (ROVs) and autonomous underwater vehicles (AUVs), which can withstand the crushing pressures. Specialized landers are deployed to collect samples and data. Pressure-resistant cameras, built with robust materials, capture images and video of the deep-sea environment. Continued research, supported by these advancements, remains important for understanding this ecosystem.