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Satellite-detected chlorophyll fluorescence reveals physiology and photosynthetic pigments of global ocean phytoplankton

Michael Behrenfeld, Department of Botany and Plant Pathology,, Oregon State University, mjb@science.oregonstate.edu (Presenting)
Toby Westberry, Department of Botany and Plant Pathology,, Oregon State University, westbert@science.oregonstate.edu
Emmanuel Boss, School of Marine Sciences,, University of Maine, emmanuel.boss@maine.e
Robert O'Malley, Department of Botany and Plant Pathology,, Oregon State University, omalleyr@science.oregonstate.edu
Jerry Wiggert, Department of Marine Sciences, University of Southern Mississippi, jerry.wiggert@usm.edu
David Siegel, Institute for Computational Earth System Sciences, Department of Geography, University of California, Santa Barbara, davey@icess.ucsb.edu
Bryan Franz, NASA Goddard Space Flight Center, bryan.a.franz@nasa.gov
Chuck McClain, NASA Goddard Space Flight Center, charles.r.mcclain@nasa.gov
Gene Feldman, NASA Goddard Space Flight Center, gene.c.feldman@nasa.gov
Giorgio Dall'Olmo, Department of Botany and Plant Pathology,, Oregon State University, giorgiod@science.oregonstate.edu
Allen Milligan, Department of Botany and Plant Pathology,, Oregon State University, allen.milligan@science.oregonstate.edu
Scott Doney, Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, sdoney@whoi.edu
Ivan Lima, Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, ivan@whoi.edu
Natalie Mahowald, Cornell University, nmm63@cornell.edu

We conducted a global investigation of surface ocean phytoplankton using satellite chlorophyll fluorescence measurements. Comparison of fluorescence data with independent chlorophyll estimates from empirical and bio-optical algorithms indicates improved performance of the bio-optical approaches in the expansive, clearest-water regions of the open ocean, while the traditional empirical approach retains greater fidelity at higher chlorophyll concentrations. Calculation of fluorescence quantum yields provides additional insights into phytoplankton physiology. The dominant physiological signal is a relatively-constrained global expression of protective mechanisms against high-light damage. Removing this primary factor reveals a secondary signature of iron-stress, with high fluorescence quantum yields associated with low iron environments.


NASA Carbon Cycle & Ecosystems Active Awards Represented by this Poster:

  • Award: NNX08AF72G
     

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