<?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_995768</Entry_ID>
<Entry_Title>Beryllium isotope and planktonic foraminifera d18O for sediment core MD05-2970</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Nemoto, Karin; Horiike, Satoshi; Miyairi, Yosuke; Aze, Takahiro; Yokoyama, Yusuke</Dataset_Creator>
<Dataset_Title>Beryllium isotope and planktonic foraminifera d18O for sediment core MD05-2970</Dataset_Title>
<Dataset_Release_Date>2026-07-08</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.995768</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Yusuke</First_Name>
<Last_Name>Yokoyama</Last_Name>
<Email>yokoyama@aori.u-tokyo.ac.jp</Email>
</Personnel>
<Personnel>
<Role>Investigator</Role>
<First_Name>Karin</First_Name>
<Last_Name>Nemoto</Last_Name>
<Email>nemoto@aori.u-tokyo.ac.jp</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>Event label</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>LATITUDE</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>LONGITUDE</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>DEPTH, sediment/rock</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>AGE</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Beryllium-9</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Beryllium-9, error</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Beryllium-10</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Beryllium-10, error</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Beryllium-10/Beryllium-9</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Beryllium-10/Beryllium-9 ratio, error</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Globigerinoides ruber, δ18O</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>beryllium isotope</Keyword>
<Keyword>Calypso Corer II</Keyword>
<Keyword>Indonesian Throughflow</Keyword>
<Keyword>MD052970</Keyword>
<Keyword>MD05-2970</Keyword>
<Keyword>MD148</Keyword>
<Sensor_Name>
<Long_Name>High-resolution inductively coupled plasma mass spectrometer (HR-ICP-MS), Thermo Scientific, ELEMENT XR</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Accelerator mass spectrometry (AMS)</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>Marion Dufresne (1995)</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>2005-07-07</Start_Date>
<Stop_Date>2005-07-07</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>-9.25</Southernmost_Latitude>
<Northernmost_Latitude>-9.25</Northernmost_Latitude>
<Westernmost_Longitude>130.5999999999992</Westernmost_Longitude>
<Easternmost_Longitude>130.5999999999992</Easternmost_Longitude>
<Minimum_Depth>0.0 m (DEPTH, sediment/rock)</Minimum_Depth>
<Maximum_Depth>28.9 m (DEPTH, sediment/rock)</Maximum_Depth>
</Spatial_Coverage>
<Access_Constraints>access rights needed</Access_Constraints>
<Use_Constraints>CC-BY-4.0: Creative Commons Attribution 4.0 International (License comes into effect after moratorium ends)</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>659 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Reference>Khan, Hidayatullah; Govil, Pawan; Panchang, Rajani; Kumar, Pankaj; Agrawal, Shailesh (2022): Surface hydrographic variations in the western Arabian Sea through the last 172 kyr. Geo-Marine Letters, 42(2), 10, https://doi.org/10.1007/s00367-022-00733-y</Reference>
<Reference>Kim, Ji-Eun; Khim, Boo-Keun; Ikehara, Minoru; Lee, Jongmin (2018): Orbital-scale denitrification changes in the Eastern Arabian Sea during the last 800 kyrs. Scientific Reports, 8(1), https://doi.org/10.1038/s41598-018-25415-7</Reference>
<Reference>Korte, Monika; Constable, Catherine; Donadini, Fabio; Holme, Richard (2011): Reconstructing the Holocene geomagnetic field. Earth and Planetary Science Letters, 312(3-4), 497-505, https://doi.org/10.1016/j.epsl.2011.10.031</Reference>
<Reference>Lathika, Nambiyathodi; Rahaman, Waliur; Tarique, Mohd; Gandhi, Naveen; Kumar, Avinash; Thamban, Meloth (2021): Deep water circulation in the Arabian Sea during the last glacial cycle: Implications for paleo-redox condition, carbon sink and atmospheric CO2 variability. Quaternary Science Reviews, 257, 106853, https://doi.org/10.1016/j.quascirev.2021.106853</Reference>
<Reference>Lee, T; Rand, Devin S; Lisiecki, Lorraine E; Gebbie, Geoffrey; Lawrence, Charles E (2023): Bayesian age models and stacks: combining age inferences from radiocarbon and benthic δ 18 O stratigraphic alignment. Climate of the Past, 19(10), 1993-2012, https://doi.org/10.5194/cp-19-1993-2023</Reference>
<Reference>Lu, Wanyi; Wang, Yi; Oppo, Delia W; Nielsen, Sune G; Costa, Kassandra M (2022): Comparing paleo-oxygenation proxies (benthic foraminiferal surface porosity, I/Ca, authigenic uranium) on modern sediments and the glacial Arabian Sea. Geochimica et Cosmochimica Acta, 331, 69-85, https://doi.org/10.1016/j.gca.2022.06.001</Reference>
<Reference>Matsuzaki, Hiroyuki; Nakano, Chuichiro; Tsuchiya, Yoko Sunohara; Kato, Kazuhiro; Maejima, Yuji; Miyairi, Yosuke; Wakasa, Sachi; Aze, Takahiro (2007): Multi-nuclide AMS performances at MALT. Nuclear Instruments &amp; Methods in Physics Research Section B-Beam Interactions with Materials and Atoms, 259(1), 36-40, https://doi.org/10.1016/j.nimb.2007.01.145</Reference>
<Reference>Nemoto, Karin; Yokoyama, Yusuke; Horiike, Satoshi; Obrochta, Stephen P; Miyairi, Yosuke (2024): Meridional migrations of the Intertropical Convergence Zone during the last deglaciation in the Timor Sea detected by extensive radiocarbon dating. Radiocarbon, 66(6), 1958-1967, https://doi.org/10.1017/RDC.2024.13</Reference>
<Reference>Nishiizumi, Kunihiko; Imamura, Mineo; Caffee, Marc W; Southon, John R; Finkel, Robert C; McAninch, Jeffrey (2007): Absolute calibration of 10Be AMS standards. Nuclear Instruments &amp; Methods in Physics Research Section B-Beam Interactions with Materials and Atoms, 258(2), 403-413, https://doi.org/10.1016/j.nimb.2007.01.297</Reference>
<Reference>Qian, Fang; Wang, Yi; Costa, Kassandra M; Nielsen, Sune G (2025): Ocean Oxygenation Changes in the Arabian Sea Oxygen Minimum Zone During the Penultimate Glacial Cycle. Paleoceanography and Paleoclimatology, 40(6), e2024PA005059, https://doi.org/10.1029/2024PA005059</Reference>
<Reference>Saher, Margot; Rostek, Frauke; Jung, S J A; Bard, Edouard; Schneider, Ralph R; Greaves, Mervyn; Ganssen, Gerald M; Elderfield, Henry; Kroon, Dick (2009): Western Arabian Sea SST during the penultimate interglacial: A comparison of UK'37 and Mg/Ca paleothermometry. Paleoceanography, 24(2), PA2212, https://doi.org/10.1029/2007PA001557</Reference>
<Reference>Sproson, Adam; Aze, Takahiro; Behrens, Bethany; Yokoyama, Yusuke (2021): Initial measurement of beryllium-9 using high-resolution inductively coupled plasma mass spectrometry allows for more precise applications of the beryllium isotope system within the Earth Sciences. Rapid Communications in Mass Spectrometry, 35(8), e9059, https://doi.org/10.1002/rcm.9059</Reference>
<Reference>von Blanckenburg, Friedhelm; Bouchez, Julien; Ibarra, Daniel E; Maher, Kate (2015): Stable runoff and weathering fluxes into the oceans over Quaternary climate cycles. Nature Geoscience, 8(7), 538-542, https://doi.org/10.1038/ngeo2452</Reference>
<Summary>Reactive phase Be isotopes, 10Be and 9Be, and major elament measurements were performed on 53 samples from core MD05-2970. d18O of Globigerinoides ruber are measured from the same core for 288 samples, respectively. We constrained a new age model using planktonic foraminifera (G. ruber) δ18O data along with the existing radiocarbon ages (Nemoto et al., 2024) in BIGMACS (Lee et al., 2023). The use of planktonic rather than benthic foraminifera δ18O is consistent with previous studies in the Indian Ocean (Khan et al., 2022; Kim et al., 2018; Lathika et al., 2021; Lu et al., 2022; Qian et al., 2025; Saher et al., 2009). A Thermo ELEMENT XR™ single collector sector field high resolution inductively coupled plasma mass spectrometry (HR-ICP-MS) installed at the Atmosphere and Occean Research Institute was used to obtain [9Be] (Sproson, Aze et al., 2021). 10Be/9Be was measured using a National Electrostatic Corporation (NEC) accelerator mass spectrometer (AMS), of 5 MV terminal voltage, at the University of Tokyo (UTokyo), Micro Analysis Laboratory, Tandem accelerator (Matsuzaki et al., 2007). Absolute values were obtained using the KNB5-2 standard (10Be/9Be = 8.558 × 10−12; (Nishiizumi et al., 2007). Decay correction is performed on 10Be concentration using a 10Be half-life of 1.387 Ma. The 10Be/9Be ratios were corrected for 10Be paleo-production using the paleomagnetic reference records of the geomagnetic dipole moment (Korte et al., 2011) following von Blanckenburg et al. (2015). ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.995768"!</Summary>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/ISO_6709</URL>
<Description>LATITUDE</Description>
</Related_URL>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/ISO_6709</URL>
<Description>LONGITUDE</Description>
</Related_URL>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/Kyr</URL>
<Description>AGE</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1002/rcm.9059</URL>
<Description>Initial measurement of beryllium-9 using high-resolution inductively coupled plasma mass spectrometry allows for more precise applications of the beryllium isotope system within the Earth Sciences</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1007/s00367-022-00733-y</URL>
<Description>Surface hydrographic variations in the western Arabian Sea through the last 172 kyr</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/j.epsl.2011.10.031</URL>
<Description>Reconstructing the Holocene geomagnetic field</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/j.gca.2022.06.001</URL>
<Description>Comparing paleo-oxygenation proxies (benthic foraminiferal surface porosity, I/Ca, authigenic uranium) on modern sediments and the glacial Arabian Sea</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/j.nimb.2007.01.145</URL>
<Description>Multi-nuclide AMS performances at MALT</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/j.nimb.2007.01.297</URL>
<Description>Absolute calibration of 10Be AMS standards</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/j.quascirev.2021.106853</URL>
<Description>Deep water circulation in the Arabian Sea during the last glacial cycle: Implications for paleo-redox condition, carbon sink and atmospheric CO2 variability</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1017/RDC.2024.13</URL>
<Description>Meridional migrations of the Intertropical Convergence Zone during the last deglaciation in the Timor Sea detected by extensive radiocarbon dating</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1029/2007PA001557</URL>
<Description>Western Arabian Sea SST during the penultimate interglacial: A comparison of UK'37 and Mg/Ca paleothermometry</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1029/2024PA005059</URL>
<Description>Ocean Oxygenation Changes in the Arabian Sea Oxygen Minimum Zone During the Penultimate Glacial Cycle</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1038/ngeo2452</URL>
<Description>Stable runoff and weathering fluxes into the oceans over Quaternary climate cycles</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1038/s41598-018-25415-7</URL>
<Description>Orbital-scale denitrification changes in the Eastern Arabian Sea during the last 800 kyrs</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.5194/cp-19-1993-2023</URL>
<Description>Bayesian age models and stacks: combining age inferences from radiocarbon and benthic δ 18 O stratigraphic alignment</Description>
</Related_URL>
<Related_URL>
<URL>https://en.wikipedia.org/wiki/Marion_Dufresne_(1994)</URL>
<Description>Marion Dufresne (1995)</Description>
</Related_URL>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2026-07-08</DIF_Creation_Date>
<Last_DIF_Revision_Date>2026-08-06</Last_DIF_Revision_Date>
</DIF>
