Articles | Volume 15, issue 3
https://doi.org/10.5194/esd-15-671-2024
https://doi.org/10.5194/esd-15-671-2024
Review
 | 
03 Jun 2024
Review |  | 03 Jun 2024

Are physiological and ecosystem-level tipping points caused by ocean acidification? A critical evaluation

Christopher E. Cornwall, Steeve Comeau, and Ben P. Harvey

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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 esd-2023-24', Anonymous Referee #1, 06 Oct 2023
    • AC1: 'Reply on RC1', Christopher Cornwall, 14 Dec 2023
    • AC3: 'New figure', Christopher Cornwall, 17 Dec 2023
  • RC2: 'Comment on esd-2023-24', Anonymous Referee #2, 01 Nov 2023
    • AC2: 'Reply on RC2', Christopher Cornwall, 14 Dec 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (18 Dec 2023) by Steven Lade
AR by Christopher Cornwall on behalf of the Authors (18 Dec 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (22 Jan 2024) by Steven Lade
RR by Ashley Deevesh Hemraj (05 Feb 2024)
ED: Publish subject to minor revisions (review by editor) (29 Feb 2024) by Steven Lade
AR by Christopher Cornwall on behalf of the Authors (11 Mar 2024)  Author's response   Author's tracked changes 
EF by Sarah Buchmann (15 Mar 2024)  Manuscript 
ED: Publish as is (21 Mar 2024) by Steven Lade
AR by Christopher Cornwall on behalf of the Authors (31 Mar 2024)  Manuscript 
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Short summary
Ocean acidification will cause profound shifts in many marine ecosystems by impairing the ability of calcareous taxa to grow and by influencing the photophysiology of many others. Physiological tipping points will likely be reached in the next 20 years. Small changes in organism physiology result in larger ecological tipping points being crossed. Ecosystems will shift from having higher abundances of calcifying taxa and towards increased abundances of non-calcareous species under elevated CO2.
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