The Southern Ocean played a critical role in the rapid atmospheric carbon dioxide increase during the last deglaciation that took place 20,000 to 10,000 years ago, according to a new report by Boston College geochemist Xingchen (Tony) Wang and an international team in the online edition of Science Advances.
In this new study, Wang and his coauthors analyzed deep-sea coral fossils from 20,000 to 10,000 years ago, when atmospheric carbon dioxide was on the rise.
By examining the chemical signatures of nitrogen and carbon in the coral fossils, the researchers revealed that ocean carbon sequestration decreased as phytoplankton failed to devour macronutrients supplied by upwelling currents in the Southern Ocean and trap carbon dioxide in the deep ocean.
As atmospheric carbon dioxide levels rise because of human activities—dominated by fossil fuel consumption—the findings raise questions about the ocean’s ability to absorb the anthropogenic carbon dioxide and the environmental consequences, including global warming, rising sea levels, and more frequent wildfires, according to Wang.
For all the carbon dioxide emitted by human activities since the industrial revolution, roughly 50 percent stayed in the atmosphere, with about a quarter absorbed by the ocean and approximately 25 percent sequestered by the ecosystem on land. To better predict the fate of anthropogenic carbon dioxide in the future, Wang and his collaborators have looked at the past variations in atmospheric carbon dioxide before any significant human activities, from 20,000 to 10,000 years ago when the Earth was moving out of the last ice age.
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“A clearer understanding of carbon dioxide variations in the past provides important insights into the fate of anthropogenic carbon dioxide in the future,” said Wang, an assistant professor in the Department of Earth and Environmental Sciences.
By studying air bubbles trapped in ancient ice from Antarctic, scientists learned that the atmospheric carbon dioxide concentration during the ice ages was about 30 percent lower than the preindustrial level. This lower carbon dioxide level encouraged the growth of large ice sheets in North America and cooled the ice-age Earth. However, there has been strong debates about why the carbon dioxide concentration was lower during the ice ages. In a previous study led by Wang, he found strong evidence suggesting that the Southern Ocean was largely responsible for the lower concentrations of carbon dioxide during the ice ages.
Phytoplankton growth in the ocean, supported by macronutrients nitrogen and phosphorus, assimilates carbon dioxide from the atmosphere and transforms them into organic carbon. When these organisms die, their biomass sinks into the deep ocean and decomposes back to carbon dioxide. This process, called the “biological pump”, transfers carbon dioxide from the atmosphere and surface ocean into the dark, deep ocean. In most parts of the modern ocean, phytoplankton consume all the nutrients supplied to the sunlit ocean and the “biological pump” reaches its maximum efficiency. However, in the Southern Ocean, phytoplankton growth is limited by the supply of the key nutrient iron, as well as sunlight. As a result, large amounts of nitrogen and phosphorus remain in this ocean region, representing a wasted opportunity for atmospheric carbon dioxide sequestration.
By analyzing the isotopic composition of nitrogen in deep-sea coral fossils, Wang found that the biological pump in the Southern Ocean was more efficient during the last ice age, sequestering more carbon dioxide from the atmosphere and thus reducing the concentration of atmospheric carbon dioxide.
Nitrogen has two stable isotopes, Nitrogen-14 and Nitrogen-15, with Nitrogen-15 representing approximately 0.4 percent of the total nitrogen atoms in nature. The small variations in the ratios of Nitrogen-15 to Nitrogen-14 in natural samples contain useful information about the cycling of the nitrogen in the ocean. For example, when phytoplankton assimilates nitrogen to build their biomass, they prefer Nitrogen-14 to Nitrogen-15, leaving behind nitrogen that is enriched in Nitrogen-15.
Wang has previously developed a highly sensitive and precise method to measure the ratios of the nitrogen isotopes in coral’s skeleton with a mass spectrometer. This capability has allowed him to measure the isotopic composition of nitrogen in deep-sea coral fossils from the Southern Ocean.
“Deep-sea corals are a wonderful archive for studying the ocean’s history. You can find them in a lot of places in the deep ocean. And their ages can be known very precisely using radiometric dating methods,” said Nanjing University’s Tao Li, first author of the new study, titled “Rapid shifts in circulation and biogeochemistry of the Southern Ocean during deglacial carbon cycle events.”
In this new study, Wang and his coauthors focused on well-dated deep-sea coral fossils from 20,000 to 10,000 years ago, when the atmospheric carbon dioxide was increasing from the ice age level to the preindustrial level. The precise ages of the deep-sea coral fossils made it possible to directly compare the changes in the Southern Ocean with the carbon dioxide record from the ice cores in Antarctic.
“If you look closely at the carbon dioxide record during the deglaciation, you will see that there are a few sudden jumps,” said Wang. “Each of these jumps is a 10-15 parts-per-million carbon dioxide increase over 100 to 200 years. That’s pretty fast but we didn’t quite understand why these jumps happened.”
The new data from deep-sea coral fossils, including nitrogen isotopes and radiocarbon, suggest that the Southern Ocean was also the primary cause of these rapid carbon dioxide jumps 20,000-10,000 years ago. When these rapid carbon dioxide changes happened, the biological pump in the Southern Ocean was less efficient and the ventilation of the Southern Ocean was faster, the study found.
“However, it should be noted that the current anthropogenic carbon dioxide increase is at least 10 times faster than these natural rapid carbon dioxide jumps during the last deglaciation. We are changing our planet at an unprecedented rate,” said Wang.
Wang said he plans to continue his research on past atmospheric carbon dioxide variations using deep-sea corals.
“It’s very exciting to collect deep-sea corals using remotely operated vehicles,” said Wang. “We plan to go the Brazil margin for the next phase of our research.”
More information: Tao L et al. Rapid shifts in circulation and biogeochemistry of the Southern Ocean during deglacial carbon cycle events. Science Advances (2020). DOI: 10.1126/sciadv.abb3807
Image: Researchers examined deep-sea coral fossils – species Desmophyllum dianthus – to study carbon sequestration in the Southern Ocean 20,000 to 10,000 years ago. The chemical signatures of nitrogen and carbon in the coral fossils revealed that ocean carbon sequestration decreased as phytoplankton failed to devour macronutrients supplied by upwelling currents in the Southern Ocean and trap carbon dioxide in the deep ocean.
Credit: Tony Wang, Boston College
