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Megalodon: Largest Ever Shark's Diet Surprises Geoscientists

Megalodon: Largest Ever Shark's Diet Surprises Geoscientists

Newsweek26-05-2025
Based on facts, either observed and verified firsthand by the reporter, or reported and verified from knowledgeable sources.
Newsweek AI is in beta. Translations may contain inaccuracies—please refer to the original content.
A new study has uncovered surprising insights into the feeding habits of the largest predatory fish to ever roam the Earth's oceans, challenging long-standing assumptions about the prehistoric predator.
For centuries, scientists believed that Otodus megalodon hunted exclusively at the top off the food chain, but a new study led by Jeremy McCormack from the Department of Geosciences at Goethe University Frankfurt found that its diet was far more flexible than previously thought.
Longer than a truck with a trailer (reaching up to almost 79 feet long) and weighting almost twice as much, Megalodon, ruled the oceans between 20–3 million years ago, frequently on the hunt for prey to satisfy its astonishing 100,000 kilocalories-per-day nutritional demand.
Its massive jaws were filled with triangular teeth, each the size of a hand, and its deadly bite had the force of an industrial hydraulic press, leaving no hope for any creature crossing its path.
It was thanks to its fossilized teeth that McCormack, in collaboration with other scientists from Germany, France, Austria and the US, were able to discover the apex predator's unusual dietary habits.
A stock image shows a 3D illustration of the Otodus Megalodon, the largest predatory fish that has ever existed.
A stock image shows a 3D illustration of the Otodus Megalodon, the largest predatory fish that has ever existed.
getty images
By analyzing the levels of zinc in the fossils, the study found that while Megalodon did surely feast on whales and dolphins whenever it had a chance, the shark adjusted its diet based on availability of the prey.
Zinc occurs in atomic variants (isotopes) of different weights, and is ingested with food. Less of the heavier isotope zinc-66 than the lighter isotope zinc-64 is stored in muscles and organs. Predatory fish absorb significantly less zinc-66 and those at the top of the food chain absorb even less.
"Since we don't know how the ratio of the two zinc isotopes at the bottom of the food pyramid was at that time, we compared the teeth of various prehistoric and extant shark species with each other and with other animal species. This enabled us to gain an impression of predator–prey relationships 18 million years ago," explained McCormack in a statement.
Sea bream—a fish which fed on mussels, snails and crustaceans—formed the lowest level of the food chain, followed by smaller shark species such as requiem sharks and the ancestors of today's cetaceans, dolphins and whales.
Larger sharks such as sand tiger sharks were further up the food pyramid, and at the top were giant sharks like Araloselachus cuspidatus and the Otodus shark genus, which includes Megalodon.
Results of the study showed that the levels of zinc found in the Megalodon couldn't be sharply differentiated from the lower levels of the pyramid, suggesting that the largest shark that ever lived was flexible enough to feed on both marine mammals and large fish from the top of the food pyramid as well as lower levels.
Jeremy McCormack at the mass spectrometer, which is used to determine the zinc isotope ratio. This ratio provides information about the diet of Otodus megalodon. Photo: Uwe Dettmar for Goethe University
Jeremy McCormack at the mass spectrometer, which is used to determine the zinc isotope ratio. This ratio provides information about the diet of Otodus megalodon. Photo: Uwe Dettmar for Goethe University
Uwe Dettmar, Goethe University
"Our study tends rather to draw a picture of megalodon as an ecologically versatile generalist," McCormack added.
The shark's diet also greatly varied depending on its location and regional availability of prey. The teeth used for the study mostly came from 18-million-year-old fossil deposits in the German cities of Sigmaringen and Passau—and sharks in these locations showed different food habits.
The creatures from Passau fed more on prey from lower levels of the food pyramid, probably due to lack of bigger fish in the area.
McCormack said that the new method of determining tooth zinc isotope ratios has once proven to be a valuable instrument for paleoecological reconstructions.
Kenshu Shimada, paleobiologist at DePaul University in Chicago, USA, and coauthor of the study added: "It gives us important insights into how the marine communities have changed over geologic time, but more importantly the fact that even 'supercarnivores' are not immune to extinction."
Do you have a tip on a science story that Newsweek should be covering? Do you have a question about Megalodon? Let us know via science@newsweek.com.
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Ancient Burial Discovery Might Redefine Our Past
Ancient Burial Discovery Might Redefine Our Past

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Ancient Burial Discovery Might Redefine Our Past

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You Could Receive COVID Vaccines via Dental Floss in Future
You Could Receive COVID Vaccines via Dental Floss in Future

Newsweek

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You Could Receive COVID Vaccines via Dental Floss in Future

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Floss-based vaccination targets the gingival sulcus for mucosal and systemic immunization. Nature Biomedical Engineering.

Beneath America, a Large Buried Heat Blob Is Moving
Beneath America, a Large Buried Heat Blob Is Moving

Newsweek

time16 hours ago

  • Newsweek

Beneath America, a Large Buried Heat Blob Is Moving

Based on facts, either observed and verified firsthand by the reporter, or reported and verified from knowledgeable sources. Newsweek AI is in beta. Translations may contain inaccuracies—please refer to the original content. There's something large moving deep beneath New England. This is the conclusion of a new paper by researchers from the University of Southampton, England, who have been studying a mysterious patch of unusually hot rock below the Appalachian Mountains. This region—known as the Northern Appalachian Anomaly (NAA)—is some 200 miles wide and lies around 125 miles beneath the surface. According to the researchers, the anomaly is part of a slow-moving underground "mantle wave" triggered by tectonic events that happened more than 90 million years ago. 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As the continents split, stress fractured deep layers of rock, triggering convective instabilities—blobs of rock slowly dripping downward under gravity. Gernon explained: "As the continent stretches and begins to split, space opens up beneath the rift. That space is rapidly filled by an inflow of soft, flowing asthenosphere." (The asthenosphere is a semi-molten part of the Earth's upper mantle, beneath the tectonic crust.) "This sudden movement disturbs the edge of the continent's root, triggering a chain reaction. Much like falling dominoes, blobs of the root begin to drip downward one after another. "These 'drips' migrate inland over time, away from the rift. We think this same process might explain unusual seismic patterns beneath the Appalachians. The timing lines up perfectly. These "drips" move slowly—about 20 kilometers every million years—which matches perfectly with the NAA's current location and age. Not a Lone Hot Spot The NAA may be just one part of a larger chain. Further south, another underground heat anomaly—the Central Appalachian Anomaly (CAA)—may represent an earlier drip in this chain. That one likely dates back around 135 million years, consistent with the early stages of the Labrador Sea rift. Together, these anomalies form a "mantle wave": a hidden, progressive disturbance deep inside the Earth, slowly traveling westward like a chain reaction. This idea, pioneered by Gernon's team, is gaining traction in explaining elevated plateaus, seismic activity, and even past volcanism in areas once considered geologically "dead." Origin of the Northern Appalachian Anomaly. Origin of the Northern Appalachian Anomaly. University of Southampton What It Means for the Surface While the Northern Appalachian Anomaly lies deep underground, its presence could help explain some of the long-term uplift seen in parts of the Appalachian Mountains. However, the region's dry climate and low erosion rates suggest that not much visible change has occurred in recent geological time. Earlier convective instabilities—like those possibly linked to the Central Appalachian Anomaly—may have had a greater impact, contributing to the reshaping of the landscape millions of years ago. The pattern of these features suggests that such deep mantle processes may have occurred repeatedly, moving step by step inland over tens of millions of years. Because there's limited seismic data in northern areas like Newfoundland and the Gulf of St. Lawrence, it's still unclear whether more of these ancient "drips" exist along the same path. But their potential connection hints at a larger, hidden system of mantle activity beneath the eastern edge of North America. Do you have a tip on a science story that Newsweek should be covering? Do you have a question about the mantle? Let us know via science@ Reference Gernon et al. (2025). A viable Labrador Sea rifting origin of the Northern Appalachian and related seismic anomalies. Geology.

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