<?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_973164</Entry_ID>
<Entry_Title>Accumulation rates of biogenic components of ODP Hole 121-758A</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Wu, Xinying; Hu, Yue; Nan, Jingbo; Yao, Weiqi</Dataset_Creator>
<Dataset_Title>Accumulation rates of biogenic components of ODP Hole 121-758A</Dataset_Title>
<Dataset_Release_Date>2024-11-11</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.973164</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Xinying</First_Name>
<Last_Name>Wu</Last_Name>
<Email>12332224@mail.sustech.edu.cn</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>Sample code/label</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>DEPTH, sediment/rock</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Age</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Accumulation rate, mass</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Barite</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Accumulation rate, barite</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Opal, biogenic silica</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Accumulation rate, biogenic silica</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Calcium carbonate</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Accumulation rate, calcium carbonate mass</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Barium</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Aluminium</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Barium excess</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Productivity of carbon</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>121-758A</Keyword>
<Keyword>Biogenic bloom</Keyword>
<Keyword>Drilling/drill rig</Keyword>
<Keyword>Late Miocene</Keyword>
<Keyword>Leg121</Keyword>
<Keyword>Marine barite</Keyword>
<Keyword>productivity proxies</Keyword>
<Keyword>Upwelling</Keyword>
<Sensor_Name>
<Long_Name>DSDP/ODP/IODP sample designation</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Age model, Gradstein et al. (2020) GTS2020</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Calculated</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Sequential leaching method according to Eagle et al. (2003) and Paytan et al. (1993)</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Opal extraction according to Mortlock et al. (1989) and Lyle et al. (2019)</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Inductively Coupled Plasma - Optical Emission Spectrometry (ICP-OES)</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Inductively Coupled Plasma Mass Spectrometer (ICP-MS), Varian, Varian 820 ES</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>According to Dymond et al. (1992)</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>Joides Resolution</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>1988-06-15</Start_Date>
<Stop_Date>1988-06-24</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>5.3842</Southernmost_Latitude>
<Northernmost_Latitude>5.3842</Northernmost_Latitude>
<Westernmost_Longitude>90.3612</Westernmost_Longitude>
<Easternmost_Longitude>90.3612</Easternmost_Longitude>
<Minimum_Depth>63.38 m (DEPTH, sediment/rock)</Minimum_Depth>
<Maximum_Depth>124.04 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>312 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Summary>The multi-proxies (BAR, bio-SiO2 MAR, and CaCO3 MAR) of productivity in Ocean Drilling Program (ODP) Leg 121 Site 758 Hole A (5°23.05'N, 90°21.67'E) during the late Miocene. Based on the biostratigraphic zones, we convert sediment depths to absolute ages on the Geologic Time Scale 2020 timescale (Gradstein et al., 2020; doi:10.1016/C2020-1-02369-3). We extract barite from marine sediments using the modified sequential leaching method (Eagle et al., 2003; doi:10.1029/2002PA000793; Paytan et al., 1993, doi:10.1038/366445a0) and examine the size and morphology of barite crystals by a scanning electron microscopy coupled with energy dispersive X-ray spectroscopy (SEM-EDX). We use the modified method after Mortlock et al. (1989, doi:10.1016/0198-0149(89)90092-7) and Lyle et al. (2019, doi:10.5194/cp-15-1715-2019) to extract biogenic opal from marine sediments. For the carbonate extraction, we digest sediments with 1.5 ml hydrofluoric acid and 0.5 ml concentrated nitric acid in a 50-ml Teflon tube at 180°C for 12 hours. After digestion, we evaporate all the acids on a 150°C electric heating plate. The sample reacts with 1 ml concentrated nitric acid and 1 ml Milli-Q water at 150°C for 12 hours. The supernatants are diluted to 40 g and are further prepared for Inductively Coupled Plasma Optical Emission Spectrometry analysis. We calculate mass accumulation rate (MAR) as a function of linear sedimentation rate (cm/ka) and dry bulk density (g/cm³). Sedimentation rates are obtained from the known reference points from the chronostratigraphic framework. The ODP reports obtain dry bulk density data (Peirce &amp; Weissel, 1989; doi:10.2973/odp.proc.ir.121.115.1989). The accumulation rates of biogenic components (i.e., BAR, CaCO3 MAR, and bio-SiO2 MAR) are calculated as the product of MAR and the weight percent of biogenic components (wt%) in sediments. In the meantime, we analyze Baexcess to estimate export productivity (Pnew) following the algorithm equation after Dymond et al., 1992; doi:10.1029/92PA00181. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.973164"!</Summary>
<Related_URL>
<URL>http://www.mindat.org/min-4723.html</URL>
<Description>Barite</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/C2020-1-02369-3</URL>
<Description>Age model, Gradstein et al. (2020) GTS2020</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1029/92PA01080</URL>
<Description>According to Dymond et al. (1992)</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.2973/odp.proc.ir.121.1989</URL>
<Description>Leg121</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/resolutn.html</URL>
<Description>Joides Resolution</Description>
</Related_URL>
<Parent_DIF>PANGAEA_973162</Parent_DIF>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2024-11-11</DIF_Creation_Date>
<Last_DIF_Revision_Date>2025-11-08</Last_DIF_Revision_Date>
</DIF>
