<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>8(1)</volume><submitter>Noonan SHC</submitter><pubmed_abstract>Ocean acidification from increasing atmospheric CO&lt;sub>2&lt;/sub> is progressively affecting seawater chemistry, but predicting ongoing and near-future consequences for marine ecosystems is challenging without empirical field data. Here we quantify tropical coral reef benthic communities at 37 stations with varying exposure to submarine volcanic CO&lt;sub>2&lt;/sub> seeping, and determine the aragonite saturation state (Ω&lt;sub>Ar&lt;/sub>) where significant changes occur in situ. With declining Ω&lt;sub>Ar&lt;/sub>, reef communities displayed progressive retractions of most reef-building taxa and a proliferation in the biomass and cover of non-calcareous brown and red algae, without clear tipping points. The percent cover of all complex habitat-forming corals, crustose coralline algae (CCA) and articulate co</pubmed_abstract><journal>Communications biology</journal><pagination>1518</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12644485</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Progressive changes in coral reef communities with increasing ocean acidification.</pubmed_title><pmcid>PMC12644485</pmcid><pubmed_authors>Fisher R</pubmed_authors><pubmed_authors>Fabricius KE</pubmed_authors><pubmed_authors>Birrell C</pubmed_authors><pubmed_authors>Noonan SHC</pubmed_authors></additional><is_claimable>false</is_claimable><name>Progressive changes in coral reef communities with increasing ocean acidification.</name><description>Ocean acidification from increasing atmospheric CO&lt;sub>2&lt;/sub> is progressively affecting seawater chemistry, but predicting ongoing and near-future consequences for marine ecosystems is challenging without empirical field data. Here we quantify tropical coral reef benthic communities at 37 stations with varying exposure to submarine volcanic CO&lt;sub>2&lt;/sub> seeping, and determine the aragonite saturation state (Ω&lt;sub>Ar&lt;/sub>) where significant changes occur in situ. With declining Ω&lt;sub>Ar&lt;/sub>, reef communities displayed progressive retractions of most reef-building taxa and a proliferation in the biomass and cover of non-calcareous brown and red algae, without clear tipping points. The percent cover of all complex habitat-forming corals, crustose coralline algae (CCA) and articulate co</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Nov</publication><modification>2026-06-05T19:16:52.529Z</modification><creation>2026-05-20T03:14:33.575Z</creation></dates><accession>S-EPMC12644485</accession><cross_references><pubmed>41286363</pubmed><doi>10.1038/s42003-025-08889-w</doi></cross_references></HashMap>