<?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_997243</Entry_ID>
<Entry_Title>Original revised depths and age data from Haug et al. (1995) compared with newer discrete CaCO3 data of ODP Site 145-882</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Lyle, Mitchell W; Olivarez Lyle, Annette</Dataset_Creator>
<Dataset_Title>Original revised depths and age data from Haug et al. (1995) compared with newer discrete CaCO3 data of ODP Site 145-882</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.997243</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>Sample code/label</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>DEPTH, sediment/rock</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Depth, composite revised</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Reference/source</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>AGE</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Calcium carbonate</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Sedimentation rate</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>145-882A</Keyword>
<Keyword>145-882B</Keyword>
<Keyword>Calcium Carbonate content</Keyword>
<Keyword>Drilling/drill rig</Keyword>
<Keyword>Leg145</Keyword>
<Keyword>Ocean Drilling</Keyword>
<Sensor_Name>
<Long_Name>DSDP/ODP/IODP sample designation</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>IODP Depth Scale Terminology</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>From the original publication</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Age, revised</Long_Name>
</Sensor_Name>
<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>
<Minimum_Depth>0.3 m (DEPTH, sediment/rock)</Minimum_Depth>
<Maximum_Depth>274.82 m (DEPTH, sediment/rock)</Maximum_Depth>
</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>7086 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>
<Reference>Lyle, Mitchell W; Olivarez Lyle, Annette (2026): Discrete CaCO3 and organic carbon (POC) measurements of ODP Site 145-882 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.997244</Reference>
<Reference>Haug, Gerald H; Maslin, Mark A; Sarnthein, Michael; Stax, Rainer; Tiedemann, Ralf (1995): Evolution of Northwest Pacific Sedimentation Patterns since 6 Ma (Site 882). In: Rea, DK, Basov, LA, Scholl, DW, Allan, JF (eds.), Proceedings of the Ocean Drilling Program, 145 Scientific Results, Proceedings of the Ocean Drilling Program, 145, Ocean Drilling Program, https://doi.org/10.2973/odp.proc.sr.145.115.1995</Reference>
<Summary>The depths and ages of the discrete CaCO3 data from Haug et al. (1995) were revised and are listed in this table. Haug et al. (1995) analyzed discrete samples every 30 cm to a depth of 315 m CCSF. We checked the data by comparing it to the discrete CaCO3 data we collected and found that they matched the newer data. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.997243"!</Summary>
<Related_URL>
<URL>http://ceoas.oregonstate.edu/profile/lyle/</URL>
</Related_URL>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/Kyr</URL>
<Description>AGE</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.2973/odp.proc.sr.145.115.1995</URL>
<Description>Evolution of Northwest Pacific Sedimentation Patterns since 6 Ma (Site 882)</Description>
</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://doi.pangaea.de/10.1594/PANGAEA.997244</URL>
<Description>Discrete CaCO3 and organic carbon (POC) measurements of ODP Site 145-882</Description>
</Related_URL>
<Related_URL>
<URL>https://hdl.handle.net/10013/epic.27914.d001</URL>
<Description>DSDP/ODP/IODP sample designation</Description>
</Related_URL>
<Related_URL>
<URL>https://hdl.handle.net/10013/epic.50267.d001</URL>
<Description>IODP Depth Scale Terminology</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>2026-10-22</Last_DIF_Revision_Date>
</DIF>
