Present and future global distributions of the marine Cyanobacteria Prochlorococcus and Synechococcus
- Departments of aEarth System Science,
- hCivil Engineering, and
- iEcology and Evolutionary Biology, University of California, Irvine, CA 92697;
- bCentro de Investigaciones del Mar y la Atmósfera, Departamento de Ciencias de la Atmósfera y los Océanos, and Instituto Franco Argentino sobre Estudios del Clima y sus Impactos, Consejo Nacional de Investigaciones Científica y Tecnológicas and Universidad de Buenos Aires, 1428 Buenos Aires, Argentina;
- cInstitute of Microbes and Ecosphere, State Key Lab for Marine Environmental Sciences, Xiamen University, Xiamen 361005, People’s Republic of China;
- dCenter for Microbial Oceanography: Research and Education (C-MORE), University of Hawaii, Honolulu, HI 96822;
- eFisheries and Oceans Canada, Bedford Institute of Oceanography, Dartmouth, NS, Canada B2Y 4A2;
- fBigelow Laboratory for Ocean Sciences, East Boothbay, ME 04544; and
- gDepartment of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139
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Contributed by David M. Karl, April 25, 2013 (sent for review January 22, 2013)

Abstract
The Cyanobacteria Prochlorococcus and Synechococcus account for a substantial fraction of marine primary production. Here, we present quantitative niche models for these lineages that assess present and future global abundances and distributions. These niche models are the result of neural network, nonparametric, and parametric analyses, and they rely on >35,000 discrete observations from all major ocean regions. The models assess cell abundance based on temperature and photosynthetically active radiation, but the individual responses to these environmental variables differ for each lineage. The models estimate global biogeographic patterns and seasonal variability of cell abundance, with maxima in the warm oligotrophic gyres of the Indian and the western Pacific Oceans and minima at higher latitudes. The annual mean global abundances of Prochlorococcus and Synechococcus are 2.9 ± 0.1 × 1027 and 7.0 ± 0.3 × 1026 cells, respectively. Using projections of sea surface temperature as a result of increased concentration of greenhouse gases at the end of the 21st century, our niche models projected increases in cell numbers of 29% and 14% for Prochlorococcus and Synechococcus, respectively. The changes are geographically uneven but include an increase in area. Thus, our global niche models suggest that oceanic microbial communities will experience complex changes as a result of projected future climate conditions. Because of the high abundances and contributions to primary production of Prochlorococcus and Synechococcus, these changes may have large impacts on ocean ecosystems and biogeochemical cycles.
Footnotes
- ↵1To whom correspondence may be addressed. E-mail: dkarl{at}hawaii.edu or amartiny{at}uci.edu.
Author contributions: P.F., J.A.V., and A.C.M. designed research; P.F., D.V., J.A.V., and A.C.M. performed research; N.J., D.M.K., W.K.W.L., M.W.L., D.V., and C.S.V. contributed new reagents/analytic tools; P.F., J.L.G., R.A.G., J.R., L.L.Z., D.V., and A.C.M. analyzed data; and P.F., N.J., D.M.K., W.K.W.L., M.W.L., D.V., J.A.V., and A.C.M. wrote the paper.
The authors declare no conflict of interest.
This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1307701110/-/DCSupplemental.
Freely available online through the PNAS open access option.