What happens when wave-generated air bubbles burst at the ocean surface? Radiocarbon (14C) measurements suggest that they grab hold of some of the oldest organic molecules in the sea and throw them into the air. Read all about it in our team’s latest paper, published online this week in Science Advances :
Beaupré, S. R., D. J. Kieber, W. C. Keene, M. S. Long, J. R. Maben, X. Lu, Y. Zhu, A. A. Frossard, J. D. Kinsey, P. Duplessis, R. Y. W. Chang, and J. Bisgrove (2019), Oceanic efflux of ancient marine dissolved organic carbon in primary marine aerosol, Science Advances, 5(10), doi:10.1126/sciadv.aax6535.
Abstract: Breaking waves produce bubble plumes that burst at the sea surface, injecting primary marine aerosol (PMA) highly enriched with marine organic carbon (OC) into the atmosphere. It is widely assumed that this OC is modern, produced by present-day biological activity, even though nearly all marine OC is thousands of years old, produced by biological activity long ago. We used natural abundance radiocarbon (14C) measurements to show that 19 to 40% of the OC associated with freshly produced PMA was refractory dissolved OC (RDOC). Globally, this process removes 2 to 20 Tg of RDOC from the oceans annually, comparable to other RDOC losses. This process represents a major removal pathway for old OC from the sea, with important implications for oceanic and atmospheric biogeochemistry, the global carbon cycle, and climate.