Dissolved rare earth elements (REEs) and neodymium isotopes (ϵNd) have been jointly used to evaluate water mass mixing and lithogenic inputs in the ocean. As the largest marginal sea of the West Pacif
Radium isotopes (radium-228 and radium-226), water isotopes (oxygen-18 and deuterium), and salinity were measured on the slope of the East Siberian Sea in coordination with the 2018 Nansen and Amundse
²³⁰Th-normalized fluxes of ²³²Th, Baₓₛ and Fe from ODP 1240 (0.02°N, 86.46°W; 2.9 km) in the eastern equatorial Pacific Ocean. Supplement to: Jacobel, Allison W; Anderson,...
Biogeochemical maps of coastal regions can be used to identify important influences and inputs that define nearshore environments and biota. Biogeochemical tracers can also track animal movement and t
