How my research benefits society
Understanding the mechanisms that influence the temporal and spatial magnitude of how material is transported from the sea surface to the seafloor, is of global importance for a variety of reasons. Organisms play a key role in the transformation of carbon, in the form of carbon dioxide or CO2, into biomass via photosynthesis. As the material sinks through the ocean, it carries the organic carbon trapped as biomass to depth, where it is removed from atmospheric exchange on the order of 1000s of years. This process, known as the biological pump, is a major mechanism by which atmospheric carbon dioxide (CO2), a potent greenhouse gas, is removed from the atmosphere. Without the biological pump, it is estimated that atmospheric CO2 concentrations would be about 40% higher than what it currently is today. In addition to carbon, sinking particles also carry a number of important elements to the deep ocean. These particles become part of the community of organisms that make up the base of up the marine food chain (called the benthic foodweb) or they are buried in sediments. These particles can play an important role in the contamination of seafood with heavy metals, such as Mercury, and algal blooms with harmful toxins, such as the neurotoxin domoic acid.
In 2006, I received AGU’s Ocean Sciences Early Career Award in recognition of significant contributions to and promise in the ocean sciences. I was named USC’s Distinguished Professor of the Year in 2013, and I was awarded the 2014 Sulzman Award for Excellence in Education and Mentoring from the Biogeosciences Section of AGU.