<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Wall M</submitter><funding>Austrian Science Fund FWF</funding><pagination>30688</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC4967918</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>6</volume><pubmed_abstract>The resilience of tropical corals to ocean acidification depends on their ability to regulate the pH within their calcifying fluid (pHcf). Recent work suggests pHcf homeostasis under short-term exposure to pCO2 conditions predicted for 2100, but it is still unclear if pHcf homeostasis can be maintained throughout a corals lifetime. At CO2 seeps in Papua New Guinea, massive Porites corals have grown along a natural seawater pH gradient for decades. This natural gradient, ranging from pH 8.1-7.4, provides an ideal platform to determine corals' pHcf (using boron isotopes). Porites maintained a similar pHcf (~8.24) at both a control (pH 8.1) and seep-influenced site (pH 7.9). Internal pHcf was slightly reduced (8.12) at seawater pH 7.6, and decreased to 7.94 at a site with a seawater pH of 7.4</pubmed_abstract><journal>Scientific reports</journal><pubmed_title>Internal pH regulation facilitates in situ long-term acclimation of massive corals to end-of-century carbon dioxide conditions.</pubmed_title><pmcid>PMC4967918</pmcid><funding_grant_id>J 3667</funding_grant_id><pubmed_authors>Fabricius KE</pubmed_authors><pubmed_authors>Wall M</pubmed_authors><pubmed_authors>Schmidt GM</pubmed_authors><pubmed_authors>de Beer D</pubmed_authors><pubmed_authors>Hofmann LC</pubmed_authors><pubmed_authors>Fietzke J</pubmed_authors><pubmed_authors>Fink A</pubmed_authors></additional><is_claimable>false</is_claimable><name>Internal pH regulation facilitates in situ long-term acclimation of massive corals to end-of-century carbon dioxide conditions.</name><description>The resilience of tropical corals to ocean acidification depends on their ability to regulate the pH within their calcifying fluid (pHcf). Recent work suggests pHcf homeostasis under short-term exposure to pCO2 conditions predicted for 2100, but it is still unclear if pHcf homeostasis can be maintained throughout a corals lifetime. At CO2 seeps in Papua New Guinea, massive Porites corals have grown along a natural seawater pH gradient for decades. This natural gradient, ranging from pH 8.1-7.4, provides an ideal platform to determine corals' pHcf (using boron isotopes). Porites maintained a similar pHcf (~8.24) at both a control (pH 8.1) and seep-influenced site (pH 7.9). Internal pHcf was slightly reduced (8.12) at seawater pH 7.6, and decreased to 7.94 at a site with a seawater pH of 7.4</description><dates><release>2016-01-01T00:00:00Z</release><publication>2016 Aug</publication><modification>2026-05-05T15:42:01.372Z</modification><creation>2019-03-27T02:19:34Z</creation></dates><accession>S-EPMC4967918</accession><cross_references><pubmed>27477963</pubmed><doi>10.1038/srep30688</doi></cross_references></HashMap>