NOAA/WDS Paleoclimatology - Seasonal Galapagos coral D14C, d18O and d13C values from 1602-1835 AD

We report measurements of near monthly D14C and d18O during selected decades from an east equatorial Pacific coral that grew during the past four centuries. We find that El Niño events occurred regularly during the late 1700s. During the early 1800s, El Niño events occurred less often, and La Niña conditions prevailed, which were accompanied by unprecedented, low cool season D14C values and high cool season d18O values. These results indicate that shallow overturning water (e.g., Central Mode Water) from the North Pacific was likely an important source of water to the Galapagos area during the early 1800s.