<?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_796267</Entry_ID>
<Entry_Title>(Table 1) Organic carbon, nitrogen and sulphur concentrations and δ¹³C of TOC from ODP Hole 167-1017E sediments</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Ishiwatari, Ryoshi; Matsumoto, Kohei; Seki, Osamu; Yamamoto, Shuichi</Dataset_Creator>
<Dataset_Title>(Table 1) Organic carbon, nitrogen and sulphur concentrations and δ¹³C of TOC from ODP Hole 167-1017E sediments</Dataset_Title>
<Dataset_Release_Date>2000</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Other_Citation_Details>Supplement to: Ishiwatari, Ryoshi; Matsumoto, Kohei; Seki, Osamu; Yamamoto, Shuichi (2000): Variations in organic carbon isotopic composition in sediments at Site 1017 during the last 25 k.y. In: Lyle, M; Koizumi, I; Richter, C; Moore, TC Jr (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 167, 1-4, https://doi.org/10.2973/odp.proc.sr.167.210.2000</Other_Citation_Details>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.796267</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Ryoshi</First_Name>
<Last_Name>Ishiwatari</Last_Name>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>Sample code/label</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Number</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>DEPTH, sediment/rock</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Carbon, organic, total</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Nitrogen, total</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Sulfur, total</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Carbon/Nitrogen ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>δ13C, organic carbon</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>167-1017E</Keyword>
<Keyword>Drilling/drill rig</Keyword>
<Keyword>Leg167</Keyword>
<Sensor_Name>
<Long_Name>DSDP/ODP/IODP sample designation</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Element analyser, Fisons NA 1500 NCS</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Mass spectrometer Finnigan Delta-S</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>Joides Resolution</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>1996-05-28</Start_Date>
<Stop_Date>1996-05-28</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>34.535</Southernmost_Latitude>
<Northernmost_Latitude>34.535</Northernmost_Latitude>
<Westernmost_Longitude>-121.107</Westernmost_Longitude>
<Easternmost_Longitude>-121.107</Easternmost_Longitude>
<Minimum_Depth>0.014 m (DEPTH, sediment/rock)</Minimum_Depth>
<Maximum_Depth>5.637 m (DEPTH, sediment/rock)</Maximum_Depth>
</Spatial_Coverage>
<Project>
<Short_Name>ODP</Short_Name>
<Long_Name>Ocean Drilling Program</Long_Name>
</Project>
<Access_Constraints>unrestricted</Access_Constraints>
<Use_Constraints>CC-BY-3.0: Creative Commons Attribution 3.0 Unported</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>1377 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Summary>A high-resolution analysis of Hole 1017E revealed that total organic carbon (TOC) concentrations (24.8 ± 2.9 mg/g) and d13C of TOC (-21.3 ± 0.2 per mil) in Holocene sections are higher than those in glacial sediments (14.2 ± 4.8 mg/g and -22.1 per mil ± 0.1 per mil, respectively). The 306- to 280-cm section has high total sulfur concentrations, which may correspond to anoxia Event 1 (1 of the warm interstadials of GISP2) in the Santa Barbara Basin. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.796267"!</Summary>
<Related_URL>
<URL>https://doi.org/10.2973/odp.proc.sr.167.210.2000</URL>
<Description>Variations in organic carbon isotopic composition in sediments at Site 1017 during the last 25 k.y.</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://www-odp.tamu.edu:443/</URL>
<Description>ODP</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/>
<Last_DIF_Revision_Date>2026-07-11</Last_DIF_Revision_Date>
</DIF>
