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. 2013 Jun 11;110(24):9824-9.
doi: 10.1073/pnas.1307701110. Epub 2013 May 23.

Present and future global distributions of the marine Cyanobacteria Prochlorococcus and Synechococcus

Pedro Flombaum  1 , José L Gallegos, Rodolfo A Gordillo, José Rincón, Lina L Zabala, Nianzhi Jiao, David M Karl, William K W Li, Michael W Lomas, Daniele Veneziano, Carolina S Vera, Jasper A Vrugt, Adam C Martiny
Affiliations

Present and future global distributions of the marine Cyanobacteria Prochlorococcus and Synechococcus

Pedro Flombaum et al. Proc Natl Acad Sci U S A. .

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 × 10(27) and 7.0 ± 0.3 × 10(26) 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.

Keywords: climate change; marine biogeochemistry; microbial biogeography.

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Conflict of interest statement

The authors declare no conflict of interest.

Figures

Fig. 1.
Fig. 1.
Observations of Prochlorococcus and Synechococcus cell abundance. (A) Geographic distribution of samples used in this study. (B) Prochlorococcus and Synechococcus as a function of temperature, PAR, nitrate, and phosphate concentration. Symbol color represents the number of overlapping observations.
Fig. 2.
Fig. 2.
Present global distribution of Prochlorococcus and Synechococcus abundance. (A) Prochlorococcus and (B) Synechococcus mean annual abundances at the sea surface.
Fig. 3.
Fig. 3.
Projected change in global abundance and distribution of Prochlorococcus and Synechococcus for 2100. Percent change in mean annual abundance between present and future climate (end of 20th and 21st century) at the sea surface for (A) Prochlorococcus and (B) Synechococcus. Colored areas represent the change in abundance in regions with >104 cells mL−1 at present climate. Purple lines represent the distribution limit of 104 cells mL−1 under future climate. Mean annual abundance estimated for present and future climate for a north–south transect at the Atlantic Ocean (330° meridian) for (C) Prochlorococcus and (D) Synechococcus. Lines represent the annual mean for the multimodel ensemble (thick) and each of the four models (thin).
Fig. 4.
Fig. 4.
Prochlorococcus and Synechococcus observations and quantitative niche model for temperature and PAR. Cell abundance as a function of (A and C) temperature at constant PAR (10−1 ± 0.05 E m−2 d−1) and (B and D) PAR at constant temperature (20 ± 0.05 °C). Symbol color represents the number of overlapping observations, and the lines show the model output.
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