<?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_983364</Entry_ID>
<Entry_Title>Stable isotope (δ13C and δ18O) and element/Calcium ratios of Plio/Pleistocene planktic foraminifers (G. bulloides, N. pachyderma sin., G. inflata) of core SO264_53-2 (Minnetonka Seamount)</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Nürnberg, Dirk; Gehre, Nadine; Fessler, Sebastian</Dataset_Creator>
<Dataset_Title>Stable isotope (δ13C and δ18O) and element/Calcium ratios of Plio/Pleistocene planktic foraminifers (G. bulloides, N. pachyderma sin., G. inflata) of core SO264_53-2 (Minnetonka Seamount)</Dataset_Title>
<Dataset_Release_Date>2025-11-03</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.983364</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Dirk</First_Name>
<Last_Name>Nürnberg</Last_Name>
<Email>dnuernberg@geomar.de</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>DEPTH, sediment/rock</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>AGE</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Neogloboquadrina pachyderma sinistral, δ13C</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Neogloboquadrina pachyderma sinistral, δ18O</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Neogloboquadrina pachyderma, Magnesium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Neogloboquadrina pachyderma sinistral, Strontium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Neogloboquadrina pachyderma, Aluminium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Neogloboquadrina pachyderma, Iron/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Neogloboquadrina pachyderma, Manganese/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerina bulloides, δ13C</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerina bulloides, δ18O</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerina bulloides, Magnesium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerina bulloides, Strontium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerina bulloides, Aluminium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerina bulloides, Iron/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerina bulloides, Manganese/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globorotalia inflata, δ13C</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globorotalia inflata, δ18O</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globorotalia inflata, Magnesium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globorotalia inflata, Strontium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globorotalia inflata, Aluminium/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globorotalia inflata, Iron/Calcium ratio</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globorotalia inflata, Manganese/Calcium ratio</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>Foraminiferal geochemistry</Keyword>
<Keyword>Foraminiferal stable isotopes</Keyword>
<Keyword>Gravity corer</Keyword>
<Keyword>North Pacific</Keyword>
<Keyword>Paleoceanography</Keyword>
<Keyword>Plio-Pleistocene.</Keyword>
<Keyword>SO264</Keyword>
<Keyword>SO264_53-2</Keyword>
<Sensor_Name>
<Long_Name>Oxygen isotope stratigraphy; Hidden Markov Model (HMM)</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>ICP-OES, VARIAN 720-ES</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>Sonne_2</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>2018-08-05</Start_Date>
<Stop_Date>2018-08-05</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>47.6489</Southernmost_Latitude>
<Northernmost_Latitude>47.6489</Northernmost_Latitude>
<Westernmost_Longitude>169.34028</Westernmost_Longitude>
<Easternmost_Longitude>169.34028</Easternmost_Longitude>
<Minimum_Depth>0.005 m (DEPTH, sediment/rock)</Minimum_Depth>
<Maximum_Depth>8.605 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>3356 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Reference>Jacobi, Lara; Nürnberg, Dirk; Chao, Weng-si; Lembke-Jene, Lester; Tiedemann, Ralf (2023): ENSO vs glacial-interglacial-induced changes in the Kuroshio-Oyashio transition zone during the Pleistocene. Frontiers in Marine Science, 10, 1074431, https://doi.org/10.3389/fmars.2023.1074431</Reference>
<Reference>Nürnberg, Dirk (2018): RV SONNE Fahrtbericht / Cruise Report SO264 - SONNE-EMPEROR: The Plio/Pleistocene to Holocene development of the pelagic North Pacific from surface to depth - assessing its role for the global carbon budget and Earth ́s climate, Suva (Fiji) - Yokohama (Japan), 30.6. - 24.8.2018. GEOMAR Report (N. Ser.), 46, 284 pp, https://doi.org/10.3289/GEOMAR_REP_NS_46_2018</Reference>
<Reference>Wang, Wanzhang; von Dobeneck, Tilo; Frederichs, Thomas; Zhang, Yang; Lembke-Jene, Lester; Tiedemann, Ralf; WInklhofer, Michael; Nürnberg, Dirk (2021): Dating North Pacific Abyssal Sediments by Geomagnetic Paleointensity: Implications of Magnetization Carriers, Plio-Pleistocene Climate Change, and Benthic Redox Conditions. Frontiers in Earth Science, 9, 683177, https://doi.org/10.3389/feart.2021.683177</Reference>
<Summary>Sediment cores from the volcanic Emperor Seamount Chain obtained during RV SONNE cruise SO264 (SONNE-EMPEROR) in August 2018 allow us to reconstruct lateral changes in the subarctic and subtropical gyres in the pelagic North Pacific over the last ~0.5 million years. This dataset comprises planktic stable carbon (δ13C) and oxygen isotope (δ18O) data, as well as foraminiferal element/Calcium ratios from gravity core SO264_53-2, which was recovered from Minnetonka Seamount (47°38.931 N 169°20.417 E) from 2325 m water depth. Measurements were performed on the planktic foraminiferal species Globigerina bulloides and Neogloboquadrina pachyderma sinistral, and Globorotalia inflata. Sampling and analytical studies were carried out from 0.005–8.605 m core depth at ~2 cm spatial resolution. The isotope analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV carbonate preparation device. Trace metal analyses were performed on a VARIAN 720-ES Axial ICP-OES. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.983364"!</Summary>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/Kyr</URL>
<Description>AGE</Description>
</Related_URL>
<Related_URL>
<URL>http://www.marinespecies.org/aphia.php?p=taxdetails&amp;id=113434</URL>
<Description>Globigerina bulloides, δ13C</Description>
</Related_URL>
<Related_URL>
<URL>http://www.marinespecies.org/aphia.php?p=taxdetails&amp;id=113434</URL>
<Description>Globigerina bulloides, δ18O</Description>
</Related_URL>
<Related_URL>
<URL>http://www.marinespecies.org/aphia.php?p=taxdetails&amp;id=113449</URL>
<Description>Globorotalia inflata, Magnesium/Calcium ratio</Description>
</Related_URL>
<Related_URL>
<URL>http://www.marinespecies.org/aphia.php?p=taxdetails&amp;id=113449</URL>
<Description>Globorotalia inflata, Strontium/Calcium ratio</Description>
</Related_URL>
<Related_URL>
<URL>http://www.marinespecies.org/aphia.php?p=taxdetails&amp;id=113449</URL>
<Description>Globorotalia inflata, δ13C</Description>
</Related_URL>
<Related_URL>
<URL>http://www.marinespecies.org/aphia.php?p=taxdetails&amp;id=113449</URL>
<Description>Globorotalia inflata, δ18O</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.3289/GEOMAR_REP_NS_46_2018</URL>
<Description>RV SONNE Fahrtbericht / Cruise Report SO264 - SONNE-EMPEROR: The Plio/Pleistocene to Holocene development of the pelagic North Pacific from surface to depth - assessing its role for the global carbon budget and Earth ́s climate, Suva (Fiji) - Yokohama (Japan), 30.6. - 24.8.2018</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.3389/feart.2021.683177</URL>
<Description>Dating North Pacific Abyssal Sediments by Geomagnetic Paleointensity: Implications of Magnetization Carriers, Plio-Pleistocene Climate Change, and Benthic Redox Conditions</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.3389/fmars.2023.1074431</URL>
<Description>ENSO vs glacial-interglacial-induced changes in the Kuroshio-Oyashio transition zone during the Pleistocene</Description>
</Related_URL>
<Related_URL>
<URL>https://uol.de/icbm/forschungsplattformen-schiffe/sonne</URL>
<Description>Sonne_2</Description>
</Related_URL>
<Related_URL>
<URL>https://www.geomar.de/dnuernberg/</URL>
</Related_URL>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2025-11-03</DIF_Creation_Date>
<Last_DIF_Revision_Date>2026-04-29</Last_DIF_Revision_Date>
</DIF>
