Individual phytoplankton cells were collected on the GEOTRACES North Atlantic Transect cruises were analyzed for elemental content using SXRF (Synchrotron radiation X-Ray Fluorescence). Carbon was calculated from biovolume using the relationships of Menden-Deuer & Lessard (2000). Trace metal concentrations are reported.
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SXRF maps
SXRF spectra
Related references:
Menden-Deuer, S. and E. J. Lessard (2000). Carbon to volume relationships for dinoflagellates, diatoms, and other protist plankton. Limnology and Oceanography 45(3): 569-579.
* Twining, B. S., S. Rauschenberg, P. L. Morton, and S. Vogt. 2015. Metal contents of phytoplankton and labile particulate material in the North Atlantic Ocean. Progress in Oceanography 137: 261-283.)
Twining, B. (2015) Cellular elemental content of individual phytoplankton cells collected during US GEOTRACES North Atlantic Transect cruises in the Subtropical western and eastern North Atlantic Ocean during Oct and Nov, 2010 and Nov. 2011.. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2015-02-17) Version Date 2015-02-17 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.641155 [access date]
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