4.2 Article

The effect of temperature and salinity on DMSP production in Gephyrocapsa oceanica (Isochrysidales, Coccolithophyceae)

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PHYCOLOGIA
卷 62, 期 2, 页码 152-163

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TAYLOR & FRANCIS LTD
DOI: 10.1080/00318884.2023.2170636

关键词

CLAW hypothesis; DMS; Global warming

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A subtropical clone of Gephyrocapsa oceanica was tested for its response to temperature and salinity. It was found that DMSP content in the cells increased with salinity and decreased with temperature. Furthermore, net DMSP production rate depended on cell size and growth rate, with the highest production rate observed below the optimum growth temperature. These findings suggest a complex relationship between temperature and DMSP production.
A subtropical clone of Gephyrocapsa oceanica was grown over the temperature and salinity range 10-30 degrees C and 20 parts per thousand-45 parts per thousand respectively. Cellular DMSP increased with increasing salinity, compatible with the hypothesis that DMSP is a compatible osmolyte. Cellular DMSP content was highest at colder temperatures and decreased as temperature increased. Net DMSP production rate also depended on cell size and growth rate was greatest about 2 degrees C below the optimum growth temperature of 20 degrees C for this clone. This resulted in a unimodal response of net DMSP production to increasing temperature: net DMSP production increased with increasing temperature when the cells were growing at temperatures below optimum for growth. At and above optimum growth temperature, further warming decreased net DMSP production. For the effect of temperature alone, in the subtropical oceans, where G. oceanica is growing at or above its optimum, further warming due to climate change will result in decreased net DMSP production and so a probable decrease in the flux of DMS to the atmosphere and sulphate aerosol production. Inasmuch as these aerosols modulate cloud albedo and longevity then these too will both decrease, resulting in a positive feedback response for temperature. The reverse effect may occur in higher latitude oceans where growth temperature is below optimum. The exact response in both regions is complicated because warming will also enhance water column stratification and may reduce mixed layer depths, affecting both nutrient and light regimes, as well as possible species succession effects. Further work is required to investigate these other indirect temperature effects.

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