The stable isotopes of nitrogen ( 14 N and 15 N) can offer important insights into present and past changes in the cycling of this key element through organisms, food webs, and environments (

The proposed Anthropocene Global Boundary Stratotype Section and Point (GSSP) candidate site of West Flower Garden Bank (27.8762°N, 93.8147°W) is an open ocean location in the Gulf of Mexico with a submerged coral reef and few direct human impacts. Corals contain highly accurate and precise (<±1 year) internal chronologies, similar to tree rings, and their exoskeletons are formed of aragonite and can be preserved in the rock record. Here we present results from a large Siderastrea siderea coral (core 05WFGB3; 1755–2005 CE) sampled with annual and monthly resolutions that show clear markers of global and regional human impacts. Atmospheric nuclear bomb testing by-products (14C, 239+240Pu) have clear increases in this coral starting in 1957 for 14C and the first increase in 1956 for 239+240Pu (potential bases for the Anthropocene GSSP). Coral δ13C declined especially after 1956 consistent with the Suess Effect resulting from the burning of fossil fuels. Coral skeletal δ15N starts to increase in 1963 corresponding with the increase in agricultural fertilizers. Coral Hg concentrations (1933–1980) loosely track fluctuations in industrial pollution and coral Ba/Ca increases from 1965–1983 when offshore oil operations expand after 1947. Coral temperature proxies contain the 20th-century global warming trend whereas coral growth declines during this interval.

The stable isotopes of nitrogen ( 14 N and 15 N) can offer important insights into present and past changes in the cycling of this key element through organisms, food webs, and environments (

The stable isotopes of nitrogen ( 14 N and 15 N) can offer important insights into present and past changes in the cycling of this key element through organisms, food webs, and environments (

The stable isotopes of nitrogen ( 14 N and 15 N) can offer important insights into present and past changes in the cycling of this key element through organisms, food webs, and environments (