Barnacles that hitch rides on the backs of humpback and gray whales not only record details about the whales’ yearly travels, they also retain this information after they become fossilized, helping scientists reconstruct the migrations of whale populations millions of years in the past, according to a new University of California, Berkeley, study.

Oxygen isotope ratios in barnacle shells change with ocean condition and allow scientists to chart the migration of the host whale, for example to warmer breeding grounds or colder feeding grounds. Now, marine paleobiologists led by UC Berkeley doctoral student Larry Taylor have discovered that barnacles retain this information even after they fall off the whale, sink to the ocean bottom, and become fossils.”

As a result, the travels of fossilized barnacles can serve as a proxy for the peregrinations of whales in the distant past, like GPS trackers from the Pleistocene.

“One of the more exciting things about the paper, in my mind, is that we find evidence for migration in all of these ancient populations, from three different sites and time periods, but also from both humpback and gray whale lineages, indicating that these animals, which lived hundreds of thousands of years ago, were all undertaking migrations similar in extent to those of modern-day whales,” Taylor said.

One surprise finding is that the coast of Panama has been a meeting ground for different subpopulations of humpback whales for at least 270,000 years and still is today. Whales visit Panama from as far away as Antarctica and the Gulf of Alaska.

This information about ancient migration will help scientists understand how migration patterns may have affected the evolution of whales over the past 3 to 5 million years, how these patterns changed with changing climate and help predict how today’s whales will adapt to the rapid climate change happening today.

“We want to understand how malleable migratory behavior has been through time, how rapidly whales have adapted to previous climate changes, and see if this can give us some clues as to how they might respond to the current changes in Earth’s climate,” he said. “How will whales cope with that, how will the food base shift, how will the whales themselves respond?”

Taylor and his colleagues, senior author Seth Finnegan, a UC Berkeley associate professor of integrative biology, Aaron O’Dea of the Smithsonian Tropical Research Institute in Panama and Timothy Bralower of Pennsylvania State University in University Park, will publish their findings this week in the journal Proceedings of the National Academy of Sciences.

Riding the whales

Barnacles are crustaceans, like crabs, lobsters and shrimp, that remain stuck in one place their whole lives, encased in a protective hard shell and sticking out their legs to snatch passing food. Most glue themselves to rocks, boats or pilings, but whale barnacles attach to a whale’s skin by boring down into it. Some whales have been estimated to carry up to 1,000 pounds of barnacles, which are visible when they breech. Clusters of barnacles are used to identify individual whales.

“This gives the barnacle several advantages: a safe surface to live on, a free ride to some of the richest waters in the world and a chance to meet up with other (barnacles) when the whales get together to mate,” O’Dea said.

Taylor’s technique works because different species of whale barnacle hitch rides on different species of whale, so paleontologists can know, when they find a fossilized barnacle, which species it rode with. Normally, the barnacles stay with a whale between one and three years, until they fall or are brushed off, often at whale breeding grounds. At least 24 fossil assemblages of whale barnacles have been found around the world, Taylor said.

The new discovery means that the fossilized barnacles recovered at these sites can tell about ancient migrations of humpbacks, gray whales and perhaps other baleen whales (toothed whales, such as sperm whales, do not host many barnacles), potentially turning up previously unsuspected feeding and breeding areas.

The technique is based on measuring the oxygen isotopes in the calcium carbonate, or calcite, shell of the barnacle. The ratio of oxygen-18 to oxygen-16 goes up as the temperature drops. Since barnacles lengthen their shells by a few millimeters a month as they try to stay attached to whales in the face of the mammals’ shedding skin, the composition of the new shell reflects the ocean temperature and general isotopic composition where it formed.

Taylor built on previous work showing that barnacles attached to living gray whales record a chemical signature of their migrations. He confirmed that the isotopic composition of the humpback whale barnacle (Coronula diadema) also tracks its environment today during the whales’ yearly migration, showing monthly changes. He then demonstrated that fossilized barnacles from Panama and from the California coast could be analyzed similarly, and that they showed isotopic changes similar to that of today’s whales.”

This technique will be particularly valuable for studying prehistoric humpback populations, Taylor said, because the humpback was and is more cosmopolitan than the California gray whale, cruising widely through the Pacific and Atlantic oceans. Scientists theorize that whale migration began as food sources became more scattered as the climate changed 5 million years ago. Modern Pacific whales migrate tens of thousands of miles annually, visiting several known feeding areas and returning to warm waters off Central and South America or Hawaii to breed.

“We plan to push this approach further back in time and across different whale populations,” Finnegan said. “We hope that by analyzing other aspects of the geochemistry of the barnacles shells we might ultimately be able to figure out what areas different ancient whale populations were migrating to.”

This study was supported by the National Science Foundation (EAR 1325683), the National System of Investigators (SENACYT) in Panama, the Paleontological Society, the Geological Society of America, Sigma Xi and the University of California Museum of Paleontology.

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