<?xml version="1.0" encoding="utf-8"?>
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					   <title>&quot;Why does the Northwest Pacific Ocean (Kamchatka Margin) have a different carbonate time series than the rest of the Pacific? Regional carbonate production is greater than deep Pacific dissolution at the start of interglacials&quot; - Interactive discussion</title>
					   <link href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-3515/" />
					   <id>https://egusphere.copernicus.org/preprints/2026/egusphere-2026-3515/</id>
					   <updated>2026-08-26T07:51:59+02:00</updated>
					   <author><name>Copernicus Publications</name></author></feed>