Articles | Volume 25, issue 7
https://doi.org/10.5194/acp-25-4107-2025
https://doi.org/10.5194/acp-25-4107-2025
Research article
 | 
10 Apr 2025
Research article |  | 10 Apr 2025

Marine organic aerosol at Mace Head: effects from phytoplankton and source region variability

Emmanuel Chevassus, Kirsten N. Fossum, Darius Ceburnis, Lu Lei, Chunshui Lin, Wei Xu, Colin O'Dowd, and Jurgita Ovadnevaite

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-2890', Anonymous Referee #1, 22 Nov 2024
    • AC1: 'Reply on RC1', Emmanuel Chevassus, 24 Jan 2025
  • RC2: 'Comment on egusphere-2024-2890', Anonymous Referee #2, 04 Dec 2024
    • AC2: 'Reply on RC2', Emmanuel Chevassus, 24 Jan 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Emmanuel Chevassus on behalf of the Authors (24 Jan 2025)  Author's response   Author's tracked changes 
EF by Polina Shvedko (27 Jan 2025)  Manuscript 
ED: Publish as is (27 Jan 2025) by Eliza Harris
AR by Emmanuel Chevassus on behalf of the Authors (04 Feb 2025)
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Short summary
This study presents the first source apportionment of organic aerosol at Mace Head via high-resolution mass spectrometry. Introducing transfer entropy as a novel method reveals that aged organic aerosol originates from both open-ocean ozonolysis and local peat-burning oxidation. Methanesulfonic acid and organic sea spray both mirror phytoplankton activity, with the former closely tied to coccolithophore blooms and the latter linked to diatoms, chlorophytes, and cyanobacteria.
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