Ice Melting Can Change DMSP Production and Photosynthetic Activity of the Haptophyte Phaeocystis antarctica1

© 2020 Phycological Society of America.

Bibliographische Detailangaben
Veröffentlicht in:Journal of phycology. - 1966. - 56(2020), 3 vom: 06. Juni, Seite 761-774
1. Verfasser: Kameyama, Sohiko (VerfasserIn)
Weitere Verfasser: Otomaru, Maki, McMinn, Andrew, Suzuki, Koji
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2020
Zugriff auf das übergeordnete Werk:Journal of phycology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Phaeocystis antarctica Southern Ocean dimethylsulfoniopropionate photosynthetic capacity sea ice melting Sulfonium Compounds dimethylpropiothetin C884XA7QGG
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520 |a Phaeocystis antarctica is an important primary producer in the Southern Ocean and plays roles in sulfur cycles through intracellular production of dimethylsulfoniopropionate (DMSP), a principal precursor of dimethyl sulfide (DMS). Haptophytes, including P. antarctica, are known to produce more DMSP than other phytoplankton groups such as diatoms and green algae, suggesting their important contribution to DMS concentrations in the Southern Ocean. We assessed how sea ice formation and melting affect photosynthesis and DMSP accumulation in P. antarctica both in seawater and in sea ice. Incubations were undertaken in an ice tank, which simulated sea ice formation and melting dynamics. The maximum quantum yield of photochemistry (Fv /Fm ) in photosystem II, as estimated from pulse-amplitude-modulated (PAM) fluorometry, was generally higher under low-light conditions than high-light conditions. Values of Fv /Fm , the relative maximum electron rate (rETRmax ), and photosynthetic efficiency (α) were lower in sea ice than in seawater, implying reduced photosynthetic function inside the sea ice. The reduction in photosynthetic function was probably due to the hypersaline environment in the brine channels. Total DMSP (DMSPt) concentration normalized by chlorophyll-a concentration was significantly higher in the sea ice than in the other environments, suggesting high accumulation of DMSP, probably due to its osmotic properties. Fv /Fm , specific growth rate, and DMSPt concentrations decreased with decreasing salinity with the lowest values found at a salinity of 22, that is, the lowest salinity tested. These results suggest that sea ice melting is responsible for a reduction in growth rate and DMSP production of P. antarctica 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Phaeocystis antarctica 
650 4 |a Southern Ocean 
650 4 |a dimethylsulfoniopropionate 
650 4 |a photosynthetic capacity 
650 4 |a sea ice melting 
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650 7 |a dimethylpropiothetin  |2 NLM 
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700 1 |a Otomaru, Maki  |e verfasserin  |4 aut 
700 1 |a McMinn, Andrew  |e verfasserin  |4 aut 
700 1 |a Suzuki, Koji  |e verfasserin  |4 aut 
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