New paper finds algae have to manufacture their own CO2 due to a paucity in the atmosphere
A paper published today in Nature finds that marine algae, which evolved and thrived with atmospheric CO2 levels 15 times higher than the present, required a novel adaptation to adjust to the relatively low CO2 levels during the Cenozoic era, when CO2 levels were still more than twice current levels. According to the paper, this novel adaptation was to manufacture their own CO2 at the reaction site for photosynthesis, required due to a paucity of CO2 in the atmosphere. Algae evolved more than 500 million years ago, when CO2 levels were ~15-17 times higher than the present; current CO2 levels are near the lowest levels of the past 500 million years.
Algae evolved more than 500 million years ago, when CO2 levels were ~15-17 times higher than the present.
Late Miocene threshold response of marine algae to carbon dioxide limitation
Clara T. Bolton
& Heather M. Stoll
Nature 500, 558–562 (29 August 2013) doi:10.1038/nature12448
21 January 2013
12 July 2013
28 August 2013
Coccolithophores are marine algae that use carbon for calcification and photosynthesis. The long-term adaptation of these and other marine algae to decreasing carbon dioxide levels during the Cenozoic era1 has resulted in modern algae capable of actively enhancing carbon dioxide at the site of photosynthesis. This enhancement occurs through the transport of dissolved bicarbonate (HCO3−) and with the help of enzymes whose expression can be modulated by variable aqueous carbon dioxide concentration, [CO2], in laboratory cultures2, 3. Coccolithophores preserve the geological history of this adaptation because the stable carbon and oxygen isotopic compositions of their calcite plates (coccoliths), which are preserved in the fossil record, are sensitive to active carbon uptake and transport by the cell. Here we use a model of cellular carbon fluxes and show that at low [CO2] the increased demand for HCO3− at the site of photosynthesis results in a diminished allocation of HCO3− to calcification, which is most pronounced in larger cells. This results in a large divergence between the carbon isotopic compositions of small versus large coccoliths only at low [CO2]. Our evaluation of the oxygen and carbon isotope record of size-separated fossil coccoliths reveals that this isotopic divergence first arose during the late Miocene to the earliest Pliocene epoch (about 7–5 million years ago). We interpret this to be a threshold response of the cells’ carbon acquisition strategies to decreasing [CO2]. The documented coccolithophore response is synchronous with a global shift in terrestrial vegetation distribution between 8 and 5 Myr ago, which has been interpreted by some studies as a floral response to decreasing partial pressures of carbon dioxide ( ) in the atmosphere4, 5, 6. We infer a global decrease in carbon dioxide levels for this time interval that has not yet been identified in the sparse proxy record7 but is synchronous with global cooling and progressive glaciations8, 9.
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