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&amp;lt;p&amp;gt;See related data for 2016-2018 coral growth: https://www.bco-dmo.org/dataset/747484&amp;lt;/p&amp;gt;</gco:CharacterString>
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&lt;p&gt;Global climate change is now the leading cause of coral-reef degradation, but the extent to which mesoscale oceanography overprints climatic forcing is poorly understood. Previous studies in Pacific Panama showed that reef ecosystems collapsed from 4100 to 1600 years ago. The 2500-yr hiatus in reef-building occurred at locations throughout the Pacific, and the primary cause was increased variability of the El Nino-Southern Oscillation. This study will determine the influence of contemporary variability in mesoscale oceanography in the eastern tropical Pacific (ETP) on variability in the condition of local coral populations. Insights from the living populations will be combined with paleoecological and geochemical studies of reef frameworks to infer past conditions that were inimical or beneficial to coral growth and reef accretion. Three primary hypotheses will be tested in Pacific Panama:&lt;br /&gt;
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http://lod.bco-dmo.org/id/dataset-parameter/776372.rdf
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&amp;lt;li&amp;gt;replaced version 1 (2019-09-09) with version 2 (2019-10-24): new&amp;amp;nbsp;FinalMass and ChangeMass values&amp;lt;/li&amp;gt;
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