<?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_937818</Entry_ID>
<Entry_Title>Magnetic susceptibility of the LAR sediment core</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Troch, Matthias; Bertrand, Sebastien; Lange, Carina Beatriz; Cárdenas, Paola; Arz, Helge Wolfgang; Pantoja, Silvio; De Pol-Holz, Ricardo; Kilian, Rolf</Dataset_Creator>
<Dataset_Title>Magnetic susceptibility of the LAR sediment core</Dataset_Title>
<Dataset_Release_Date>2021-11-03</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.937818</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Matthias</First_Name>
<Last_Name>Troch</Last_Name>
<Email>matthias.troch@ugent.be</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>Depth, composite</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Magnetic susceptibility, volume</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>Alkenones</Keyword>
<Keyword>Baker-Martínez fjord system</Keyword>
<Keyword>biogenic silica</Keyword>
<Keyword>Bulk organic geochemistry</Keyword>
<Keyword>Calcium carbonate</Keyword>
<Keyword>Chilean Patagonia</Keyword>
<Keyword>Composite Core</Keyword>
<Keyword>density</Keyword>
<Keyword>Diatoms</Keyword>
<Keyword>Grain Size</Keyword>
<Keyword>Holocene</Keyword>
<Keyword>LAR</Keyword>
<Keyword>LAR_GC_PC</Keyword>
<Keyword>Late Glacial</Keyword>
<Keyword>Magnetic susceptibility</Keyword>
<Keyword>stable carbon isotopes</Keyword>
<Sensor_Name>
<Long_Name>Bartington MS2E point sensor</Long_Name>
</Sensor_Name>
<Temporal_Coverage>
<Start_Date>2008-09-12</Start_Date>
<Stop_Date>2008-09-12</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>-47.905467</Southernmost_Latitude>
<Northernmost_Latitude>-47.905467</Northernmost_Latitude>
<Westernmost_Longitude>-74.334233</Westernmost_Longitude>
<Easternmost_Longitude>-74.334233</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>17862 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Reference>Troch, Matthias; Bertrand, Sebastien; Lange, Carina B; Cárdenas, Paola; Arz, Helge Wolfgang; Pantoja, Silvio; De Pol-Holz, Ricardo; Kilian, Rolf (2022): Glacial isostatic adjustment near the center of the former Patagonian Ice Sheet (48°S) during the last 16.5 kyr. Quaternary Science Reviews, 277, 107346, https://doi.org/10.1016/j.quascirev.2021.107346</Reference>
<Summary>Continuous high-resolution logging of magnetic susceptibility was accomplished using a Bartington MS2E spot sensor integrated into an automatic logging system. Measurements were performed on the split cores in steps of 1 mm with drift correction every 10 mm using readings in air. The gravity and piston cores were correlated using the magnetic susceptibility data, resulting in a composite core length of 9.20 m. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.937818"!</Summary>
<Related_URL>
<URL>https://doi.org/10.1016/j.quascirev.2021.107346</URL>
<Description>Glacial isostatic adjustment near the center of the former Patagonian Ice Sheet (48°S) during the last 16.5 kyr</Description>
</Related_URL>
<Related_URL>
<URL>https://en.wikipedia.org/wiki/Magnetic_susceptibility</URL>
<Description>Magnetic susceptibility, volume</Description>
</Related_URL>
<Parent_DIF>PANGAEA_937823</Parent_DIF>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2021-11-03</DIF_Creation_Date>
<Last_DIF_Revision_Date>2026-04-30</Last_DIF_Revision_Date>
</DIF>
