IOWA STATE (US) — Radiocarbon data from clam shells are telling the story of the Atlantic Ocean’s past.
Off the coast of Maine, clams can live up to 240 years, year after year adding another band to their shells, just like a tree adds another growth ring. In the colder waters of the North Atlantic near Iceland, the clams can live up to 500 years, recording even more information in what scientists call annual shell increments.
It turns out those shell increments are a lot like sensors at the bottom of the ocean—they record long records of information about the ocean, including growing conditions, temperatures, and circulation patterns.
A paper published by Nature Communications this summer reports how lead author Alan Wanamaker, an assistant professor of geological and atmospheric sciences at Iowa State University, and an international team of researchers used radiocarbon data from shells to determine when clams collected north of Iceland were living in “young” or “old” water.
Young water had been at the surface more recently and probably came from the Atlantic. Old water had been removed from the surface much longer and probably came from the Arctic Ocean.
The paper reports warmer, younger water from the Gulf Stream during the warmer Medieval Climate Anomaly from about AD 950 to 1250. The paper also reports that shell data showed older, colder water during Europe’s Little Ice Age from about AD 1550 to 1850.
The researchers’ interpretation of the data says the Gulf Stream carrying warm water from the subtropical Atlantic was strong in the medieval era, weakened during the Little Ice Age and strengthened again after AD 1940. Those fluctuations amplified the relative warmth and coolness of the times.
Wanamaker says a better understanding of the ocean’s past can help researchers understand today’s climate trends and changes.
“Is the natural variability only that, or is it influenced by burning fossil fuels?” he adds. “Maybe we can understand what will happen in the next 100 years if we understand oceans over the past 1,000 years.”
And so Wanamaker works with students to carefully collect, process, and study clam shells. In his lab, the shells are cleaned, sorted, measured, cut, polished, drilled, and otherwise prepared for careful microscopic imaging, geochemical testing, and radiocarbon analysis.
The research is painstaking—the shell increments are measured in millionths of a meter and microscopes are required at the most important steps.
The tools are sophisticated—two mass spectrometers measure shell fragments for different isotopes of carbon and oxygen. (Isotopes are elements with varying numbers of neutrons. Heavier isotopes of oxygen in the shell material generally correspond to colder ocean temperatures.)
“Isotopes are just wonderful tracers in nature,” Wanamaker notes.
“In the broadest sense, we’re trying to add to our understanding of oceans over the last several thousand years,” he adds. “We have a terrestrial record—we can get an excellent chronology from tree rings and there is a climate signal there. But that’s missing 70 percent of the planet.”
Source: Iowa State University