Taking the metabolic pulse of the world’s coral reefs

Ocean Acidification Alkalinity Biogeochemistry Biogeochemical Cycle
DOI: 10.1371/journal.pone.0190872 Publication Date: 2018-01-09T19:13:49Z
ABSTRACT
Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of anthropogenic perturbations including ocean warming and acidification, increased sedimentation, eutrophication, overfishing, which could shift reefs to condition net calcium carbonate (CaCO3) dissolution erosion. Herein, we determine the calcification potential relative balance organic carbon metabolism (net community production; NCP) inorganic calcification; NCC) within 23 locations across globe. In light these results, consider suitability using two metrics developed total alkalinity (TA) dissolved (DIC) measurements collected on different spatiotemporal scales monitor biogeochemistry under change. All in this study were calcifying for majority observations as inferred depletion offshore, although occasional occurred at most locations. However, with lower (i.e., TA depletion) towards sooner than higher potential. The percent influence fluxes changes NCP compared sum ranged 32% 88% reflected inherent biogeochemical differences between reefs. Reefs largest percentage experienced variability seawater pH given change DIC, is directly related ability elevate or suppress local open ocean. This work highlights value measuring chemistry when evaluating their susceptibility ongoing global environmental offers baseline guide future conservation efforts aimed preserving valuable ecosystems.
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