| Literature DB >> 26988182 |
Gwenn M M Hennon1, Paul Quay1, Rhonda L Morales1, Lyndsey M Swanson1, E Virginia Armbrust1.
Abstract
Diatoms are responsible for a large proportion of global carbon fixation, with the possibility that they may fix more carbon under future levels of high CO2 . To determine how increased CO2 concentrations impact the physiology of the diatom Thalassiosira pseudonana Hasle et Heimdal, nitrate-limited chemostats were used to acclimate cells to a recent past (333 ± 6 μatm) and two projected future concentrations (476 ± 18 μatm, 816 ± 35 μatm) of CO2 . Samples were harvested under steady-state growth conditions after either an abrupt (15-16 generations) or a longer acclimation process (33-57 generations) to increased CO2 concentrations. The use of un-bubbled chemostat cultures allowed us to calculate the uptake ratio of dissolved inorganic carbon relative to dissolved inorganic nitrogen (DIC:DIN), which was strongly correlated with fCO2 in the shorter acclimations but not in the longer acclimations. Both CO2 treatment and acclimation time significantly affected the DIC:DIN uptake ratio. Chlorophyll a per cell decreased under elevated CO2 and the rates of photosynthesis and respiration decreased significantly under higher levels of CO2 . These results suggest that T. pseudonana shifts carbon and energy fluxes in response to high CO2 and that acclimation time has a strong effect on the physiological response.Entities:
Keywords: Thalassiosira pseudonana; acclimation; carbon dioxide; chemostat; diatom; ocean acidification; oxygen isotopes
Year: 2014 PMID: 26988182 DOI: 10.1111/jpy.12156
Source DB: PubMed Journal: J Phycol ISSN: 0022-3646 Impact factor: 2.923