<?xml version="1.0" encoding="UTF-8"?><!--*** Generated from internal PANGAEA metadata schema by dif.xslt ***--><DIF xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.4.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/">
<Entry_ID>PANGAEA_997239</Entry_ID>
<Entry_Title>Revised depth offsets alignment between ODP Site 145-882A and Site 145-882B</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Lyle, Mitchell W; Olivarez Lyle, Annette</Dataset_Creator>
<Dataset_Title>Revised depth offsets alignment between ODP Site 145-882A and Site 145-882B</Dataset_Title>
<Dataset_Release_Date>2026-09-23</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.997239</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Mitchell W</First_Name>
<Last_Name>Lyle</Last_Name>
<Email>mlyle@coas.oregonstate.edu</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>Event label</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Latitude of event</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Longitude of event</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Date/Time of event</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Core</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Cumulative Offset</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>145-882A</Keyword>
<Keyword>145-882B</Keyword>
<Keyword>Drilling/drill rig</Keyword>
<Keyword>Drilling composite sediment section</Keyword>
<Keyword>Leg145</Keyword>
<Keyword>Ocean Drilling</Keyword>
<Sensor_Name>
<Long_Name>Calculated</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>Joides Resolution</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>1992-07-08</Start_Date>
<Stop_Date>1992-08-08</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>50.3633</Southernmost_Latitude>
<Northernmost_Latitude>50.3633</Northernmost_Latitude>
<Westernmost_Longitude>167.5996</Westernmost_Longitude>
<Easternmost_Longitude>167.6</Easternmost_Longitude>
</Spatial_Coverage>
<Access_Constraints>unrestricted</Access_Constraints>
<Use_Constraints>CC-BY-4.0: Creative Commons Attribution 4.0 International</Use_Constraints>
<Data_Set_Language>English</Data_Set_Language>
<Data_Center>
<Data_Center_Name>
<Short_Name>PANGAEA</Short_Name>
<Long_Name>Data Publisher for Earth &amp; Environmental Science</Long_Name>
</Data_Center_Name>
<Data_Center_URL>https://www.pangaea.de/</Data_Center_URL>
<Personnel>
<Role>Data Center Contact</Role>
<First_Name>Michael</First_Name>
<Last_Name>Diepenbroek</Last_Name>
<Email>info@pangaea.de</Email>
<Contact_Address>
<Address>Leobener Str.</Address>
<City>Bremen</City>
<Province_or_State>Bremen</Province_or_State>
<Postal_Code>28359</Postal_Code>
<Country>Germany</Country>
</Contact_Address>
</Personnel>
</Data_Center>
<Distribution>
<Distribution_Media>online</Distribution_Media>
<Distribution_Size>142 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Reference>Lyle, Mitchell W; Olivarez Lyle, Annette (preprint): 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. Climate of the Past, https://doi.org/10.5194/egusphere-2026-3515</Reference>
<Summary>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. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.997239"!</Summary>
<Related_URL>
<URL>http://ceoas.oregonstate.edu/profile/lyle/</URL>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.5194/egusphere-2026-3515</URL>
<Description>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</Description>
</Related_URL>
<Related_URL>
<URL>https://www-odp.tamu.edu:443/resolutn.html</URL>
<Description>Joides Resolution</Description>
</Related_URL>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2026-09-23</DIF_Creation_Date>
<Last_DIF_Revision_Date>2026-09-23</Last_DIF_Revision_Date>
</DIF>
