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<md:lastName>Lyle</md:lastName>
<md:firstName>Mitchell W</md:firstName>
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<md:lastName>Olivarez Lyle</md:lastName>
<md:firstName>Annette</md:firstName>
<md:eMail>malyle@verizon.net</md:eMail>
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<md:year>2026</md:year>
<md:title>Revised depth offsets alignment between ODP Site 145-882A and Site 145-882B</md:title>
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<md:dateTime>2026-09-23T05:11:37</md:dateTime>
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<md:abstract>After finding an error in the composite section for ODP Site 145-882, we reconstructed a new composite (continuous sediment section) using Hole 145-882A and Hole 145-882B. Equivalent sediment features in cores from each hole are aligned by changing the depth of cores from each hole by an offset added to the original CSF depth. This dataset displays the offsets in meters for each core to align them with each other.</md:abstract>
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<md:title>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</md:title>
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<md:source id="ref141534.journal17491" type="journal">Climate of the Past</md:source>
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<md:number>OCE-9811272</md:number>
<md:title>Collaborative Research: Millennial-Scale Carbonate Deposition Events Along the California Margin and their links to Paleoceanography and Paleoclimate</md:title>
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<md:comment>42 cores; 398.3 m cored; 0 m drilled; 103.2 % recovery</md:comment>
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<md:comment>29 cores; 270.4 m cored; 0 m drilled; 103.9 % recovery</md:comment>
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<md:lastName>Lyle</md:lastName>
<md:firstName>Mitchell W</md:firstName>
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<md:lastName>Lyle</md:lastName>
<md:firstName>Mitchell W</md:firstName>
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<md:orcid>0000-0002-0861-0511</md:orcid>
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<md:comment>Top of core offset</md:comment>
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