B31C-0024:
Mangrove forests: a potent nexus of coastal biogeochemical cycling
Wednesday, 17 December 2014
Jordan G Barr, Everglades National Park, Homestead, FL, United States, Jose D Fuentes, Pennsylvania State University Main Campus, University Park, PA, United States, Barclay Shoemaker, US Geological Survey, Davie, FL, United States, Thomas L O'Halloran, Sweet Briar College, Sweet Briar, VA, United States, Guanghui Lin Sr., Center for Earth System Science, Tsinghua University, Beijing, China and Victor Charles Engel, USGS, Baltimore, MD, United States
Abstract:
Mangrove forests cover just 0.1% of the Earth’s terrestrial surface, yet they provide a disproportionate source (~10 % globally) of terrestrially derived, refractory dissolved organic carbon to the oceans. Mangrove forests are biogeochemical reactors that convert biomass into dissolved organic and inorganic carbon at unusually high rates, and many studies recognize the value of mangrove ecosystems for the substantial amounts of soil carbon storage they produce. However, questions remain as to how mangrove forest ecosystem services should be valuated and quantified. Therefore, this study addresses several objectives. First, we demonstrate that seasonal and annual net ecosystem carbon exchange in three selected mangrove forests, derived from long-term eddy covariance measurements, represent key quantities in defining the magnitude of biogeochemical cycling and together with other information on carbon cycle parameters serves as a proxy to estimate ecosystem services. Second, we model ecosystem productivity across the mangrove forests of Everglades National Park and southern China by relating net ecosystem exchange values to remote sensing data. Finally, we develop a carbon budget for the mangrove forests in the Everglades National Park for the purposes of demonstrating that these forests and adjacent estuaries are sites of intense biogeochemical cycling. One conclusion from this study is that much of the carbon entering from the atmosphere as net ecosystem exchange (~1000 g C m-2 yr-1) is not retained in the net ecosystem carbon balance. Instead, a substantial fraction of the carbon entering the system as net ecosystem exchange is ultimately exported to the oceans or outgassed as reaction products within the adjacent estuary.