英文摘要: | Diatoms are responsible for ~40% of marine primary productivity1, fuelling the oceanic carbon cycle and contributing to natural carbon sequestration in the deep ocean2. Diatoms rely on energetically expensive carbon concentrating mechanisms (CCMs) to fix carbon efficiently at modern levels of CO2 (refs 3, 4, 5). How diatoms may respond over the short and long term to rising atmospheric CO2 remains an open question. Here we use nitrate-limited chemostats to show that the model diatom Thalassiosira pseudonana rapidly responds to increasing CO2 by differentially expressing gene clusters that regulate transcription and chromosome folding, and subsequently reduces transcription of photosynthesis and respiration gene clusters under steady-state elevated CO2. These results suggest that exposure to elevated CO2 first causes a shift in regulation, and then a metabolic rearrangement. Genes in one CO2-responsive cluster included CCM and photorespiration genes that share a putative cAMP-responsive cis-regulatory sequence, implying these genes are co-regulated in response to CO2, with cAMP as an intermediate messenger. We verified cAMP-induced downregulation of CCM gene δ-CA3 in nutrient-replete diatom cultures by inhibiting the hydrolysis of cAMP. These results indicate an important role for cAMP in downregulating CCM and photorespiration genes under elevated CO2 and provide insights into mechanisms of diatom acclimation in response to climate change.
Burning fossil fuels and land-use change have accelerated CO2 emissions to the atmosphere by a factor ~100 above natural levels6. About a third of anthropogenic emissions have been absorbed by the oceans7, 8, increasing dissolved CO2 and reducing pH (ref. 9). Despite these changes, CO2 concentrations in surface waters remain below half-saturation for most forms of ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco)3, the central enzyme used to fix carbon. Consequently, marine phytoplankton, including diatoms, rely on carbon concentrating mechanisms (CCMs) to ensure adequate delivery of CO2 to the Rubisco active site, minimizing the competitive fixation of oxygen3, 4, 5. The required bicarbonate transporters and carbonic anhydrases of these CCMs concentrate CO2 against a gradient, which is energetically costly10. Downregulation of CCMs as part of acclimation to elevated CO2 should result in energy savings to the diatom cell and metabolic rearrangement. Here we use nitrate-limited chemostats to simulate in situ nutrient limitation11 while precisely controlling cell biomass and CO2 (ref. 12), allowing us to identify potential signalling pathways triggered either by an abrupt transition to increased CO2, as might occur during coastal upwelling13, or at steady-state exposure to elevated CO2, including 800 μatm predicted for 2100 (ref. 14; Fig. 1a, b).
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