Dataset: The 13C/12C stable carbon isotopic ratio of the dissolved inorganic carbon from samples collected on the GEOTRACES EPZT cruise (R/V Thomas G. Thompson TN303) in the Eastern Tropical South Pacific from October to December 2013

Final no updates expectedDOI: 10.26008/1912/bco-dmo.676537.1Version 1 (2017-01-26)Dataset Type:Cruise Results

Principal Investigator: Paul Quay (University of Washington)

BCO-DMO Data Manager: Shannon Rauch (Woods Hole Oceanographic Institution)


Program: U.S. GEOTRACES (U.S. GEOTRACES)

Project: U.S. GEOTRACES East Pacific Zonal Transect (GP16) (U.S. GEOTRACES EPZT)

Project: US GEOTRACES Pacific: Measuring the d13C-DIC distribution and quantifying the impact of organic matter export on d13C, nutrients and trace metals (EPZT d13C-DIC)


Abstract

The 13C/12C stable carbon isotopic ratio of the dissolved inorganic carbon from samples collected on the GEOTRACES EPZT cruise (R/V Thomas G. Thompson TN303) in the Eastern Tropical South Pacific from October to December 2013.

The 13C/12C stable carbon isotopic ratio of the dissolved inorganic carbon from samples collected on the R/V Thomas G. Thompson cruise TN303 in the Eastern Tropical South Pacific (GEOTRACES EPZT).


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Methods

Quay, P., & Stutsman, J. (2003). Surface layer carbon budget for the subtropical N. Pacific: constraints at station ALOHA. Deep Sea Research Part I: Oceanographic Research Papers, 50(9), 1045–1061. doi:10.1016/s0967-0637(03)00116-x