4.6 Article

A Key Marine Diazotroph in a Changing Ocean: The Interacting Effects of Temperature, CO2 and Light on the Growth of Trichodesmium erythraeum IMS101

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PLOS ONE
卷 12, 期 1, 页码 -

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PUBLIC LIBRARY SCIENCE
DOI: 10.1371/journal.pone.0168796

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资金

  1. UK Natural Environment Research Council (NERC) PhD studentship at the University of Essex [NE/J500379/1 DTB]
  2. Natural Environment Research Council [NE/F002971/1] Funding Source: researchfish
  3. NERC [NE/F002971/1] Funding Source: UKRI

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Trichodesmium is a globally important marine diazotroph that accounts for approximately 60 - 80% of marine biological N-2 fixation and as such plays a key role in marine N and C cycles. We undertook a comprehensive assessment of how the growth rate of Trichodesmium erythraeum IMS101 was directly affected by the combined interactions of temperature, pCO(2) and light intensity. Our key findings were: low pCO(2) affected the lower temperature tolerance limit (T-min) but had no effect on the optimum temperature (T-opt) at which growth was maximal or the maximum temperature tolerance limit (T-max); low pCO(2) had a greater effect on the thermal niche width than low-light; the effect of pCO(2) on growth rate was more pronounced at suboptimal temperatures than at supraoptimal temperatures; temperature and light had a stronger effect on the photosynthetic efficiency (F-v/F-m) than did CO2; and at T-opt, the maximum growth rate increased with increasing CO2, but the initial slope of the growth-irradiance curve was not affected by CO2. In the context of environmental change, our results suggest that the (i) nutrient replete growth rate of Trichodesmium IMS101 would have been severely limited by low pCO(2) at the last glacial maximum (LGM), (ii) future increases in pCO(2) will increase growth rates in areas where temperature ranges between T-min to T-opt, but will have negligible effect at temperatures between T-opt and T-max, (iii) areal increase of warm surface waters (> 18 degrees C) has allowed the geographic range to increase significantly from the LGM to present and that the range will continue to expand to higher latitudes with continued warming, but (iv) continued global warming may exclude Trichodesmium spp. from some tropical regions by 2100 where temperature exceeds T-opt.

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