Crustaceans that live in the deepest part of the ocean carry radioactive carbon in their bodies, a legacy of nuclear tests performed during the Cold War.
Researchers recently found elevated levels of radiocarbon in amphipods — shell-less, shrimp-like creatures — from deep trenches in the western Pacific Ocean, up to 7 miles (11 kilometers) below the surface.
In those dark and high-pressure depths, deep-sea amphipods scavenge decaying organic matter that drifts down from above. By eating the remains of animals that were exposed to radioactive fallout from Cold War nuclear tests, the amphipods’ bodies have also become infused with radiocarbon — the isotope carbon-14, or “bomb carbon” — the first evidence of elevated radiocarbon at the sea bottom, scientists wrote in a new study. [In Photos: The Wonders of the Deep Sea]
Some carbon-14 occurs naturally in the atmosphere and in living organisms. But by the mid-1960s, atmospheric radiocarbon levels were roughly twice what they were before nuclear testing began, and those levels didn’t start to drop until testing ceased, the researchers reported.
Soon after the first nuclear explosions, elevated quantities of carbon-14 were already appearing in ocean animals near the sea surface. For the new study, researchers went deeper, examining amphipods collected from three locations on the sea bottom in the tropical western Pacific: the Mariana, Mussau and New Britain Trenches.
Organic matter in the amphipods’ guts held carbon-14, but the carbon-14 levels in the amphipods’ bodies were much higher. Over time, a diet rich in carbon-14 likely flooded the amphipods’ tissues with bomb carbon, the scientists concluded.
They also found that deep-sea amphipods were bigger and longer-lived than their cousins closer to the surface. Amphipods in the ocean trenches lived to be more than 10 years old, and measured nearly 4 inches (10 centimeters) long. By comparison, surface amphipods live to be less than 2 years old and grow to be only 0.8 inches (2 cm) in length.
The deep-sea amphipods’ low metabolic rate and longevity provide fertile ground for carbon-14 to accumulate in their bodies over time, according to the study.
Ocean circulation alone would take centuries to carry bomb carbon to the deep sea. But thanks to the ocean food chain, bomb carbon arrived at the seafloor far sooner than expected, lead study author Ning Wang, a geochemist at the Chinese Academy of Sciences in Guangzhou, said in a statement.
The study underscores how humans’ impact on ocean ecosystems near the surface can circulate through miles of water, affecting creatures in its deepest depths.
“There’s a very strong interaction between the surface and the bottom, in terms of biologic systems,” study co-author Weidong Sun, a geochemist at the Chinese Academy of Sciences in Qingdao, said in the statement.
“Human activities can affect the biosystems even down to 11,000 meters [36,000 feet], so we need to be careful about our future behaviors,” Sun said.
Indeed, recent studies have also shown evidence of plastic in the guts of marine animals inhabiting deep-sea trenches.
The findings were published online April 8 in the journal Geophysical Research Letters.