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&amp;lt;p&amp;gt;The following table is a statistical summary of results:&amp;lt;br /&amp;gt;
&amp;lt;a href=&amp;quot;http://dmoserv3.whoi.edu/data_docs/Coral_climate_effects/Table1.pdf&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;Table1, Wang et al., 2016&amp;lt;/a&amp;gt; (pdf)&amp;lt;/p&amp;gt; Methods and Sampling: The “age” for these corals were determined by either counting growth rings on X-ray images of the coral skeleton or matching with other parameters (Sr/Ca or oxygen isotopes) in the same coral skeleton.

At each site, the core-averaged skeletal d15N was first calculated by averaging all available d15N data in each coral core. Then the site-averaged skeletal d15N was calculated by averaging the core-averaged skeletal d15N of all coral cores from the same site.

Samples from Bermuda were collected from a single brain coral (of the species Diploria labyrinthiformis) at Hog Reef, Bermuda (32.45811, -64.83445) in July of 2014 at a depth of 3m.

For more details, see Wang et al., 2016.</gco:CharacterString>
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from Deployment: CoralClimateProj_Kiritimati &lt;p&gt;Sampling took place in 1998.&lt;/p&gt;


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