In "Increased carbon transport in the Hudson River: unexpected consequence of nitrogen deposition?" published in the April issue of Frontiers in Ecology and the Environment, Findlay explores what may be driving this phenomenon.
Most large rivers contain dissolved organic carbon (DOC) in fair quantities, but recent tests have shown a doubling of the amount of DOC accumulating in the Hudson River over the past fifteen years. Soggy peatlands, wetlands, or increased agriculture could all lead to increases in the carbon levels. Some areas have shown increased DOC after nitrogen fertilization of forests. Yet activity along the Hudson River, including agricultural use, has declined over the years.
According to the paper, "temperature, water yield, and land cover have not changed in ways that would make these viable causes for the altered DOC."
Findlay proposes two possible suspects: either the composition of materials flowing into the Hudson has changed or the bacteria that normally process carbon are not metabolizing some of the carbon material entering the river. The second possibility, that the metabolism of the bacteria in the river has changed, would result in higher levels of DOC flowing downstream to the freshwater tidal flats.
According to Findlay, if the bacteria are bypassing the material flowing into the river, then downstream waters would receive larger amounts of DOC. This process would add to oxygen demand, increasing the river's susceptibility to eutrophication-driven problems of hypoxia, such as regularly occurs in the Gulf of Mexico.