Sea Grant: A Science Partnership Serving America’s Coasts - NOAA (.gov)

Credit: Jeffry Madrigal. Baby manta rays escape predators by avoiding them until they grow large enough for a face-off, a new study has found. Tracking data shows that young giant manta rays in Central America strictly stick to comparatively safe coastal areas for the first few years of their life. When they’re large enough that natural enemies are a lesser concern, they leave these sanctuaries and embark on journeys spanning hundreds of kilometers. This shift in space use allows mantas to grow in safety before facing another type of danger in the open oceans: industrial fisheries and vessel strikes in unprotected waters. The authors say underwater corridors are needed to protect adult mantas on their treks. Giant manta rays can grow up to nine meters long with a disc size of seven meters across and weigh up to 2,000kg. This size leaves them with very few natural enemies once they reach adulthood at around eight to ten years old. But giant manta ray babies, called pups, cannot rely on their size to protect them from predators that live in the open ocean, including several species of shark and orcas.

One of the manta rays tracked in the study. Credit: Jeffry Madrigal Giant manta rays can grow up to nine meters (30 feet) long with a disk size of seven meters (23 feet) across and weigh up to 2,000 kg (4,400 pounds). This size leaves them with very few natural enemies once they reach adulthood at around eight to 10 years old. But giant manta ray babies, called pups, cannot rely on their size to protect them from predators that live in the open ocean, including several species of shark and orcas.

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Simulations suggest Earth’s ancient magma ocean could not create the unusually light hydrogen signatures found in some volcanic rocks. The modeled mantle retained nearly uniform hydrogen isotope ratios, despite differences among minerals and crystallization conditions. The findings strengthen the case for hydrogen escaping Earth’s core, although the transfer mechanism remains unresolved. Some volcanic rocks carry hydrogen signatures that may trace back to Earth’s metallic core. Lavas from Baffin Island in the Canadian Arctic and Iceland contain unusually little deuterium, hydrogen’s heavier stable isotope. Explaining that imbalance could reveal whether the core has supplied material to the mantle over billions of years. Work led by Wenzhong Wang at the University of Science and Technology of China tests a competing explanation. Published in Science Advances, the study examines whether crystallization of Earth’s ancient magma ocean could have created those distinctive signatures. Its simulations indicate that this process produced far too little separation between hydrogen isotopes.