cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.979373
title: Foraminifera occurrences of IODP Hole 386-M0084F

description: Results of Foraminifera assemblage analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, micropaleontology samples were taken from the end of split cores at 5 m intervals. During the onshore phase approximately 2 cubic centimetres of sediment from each of these samples were analysed for foraminifera. After drying overnight in a ~40°C oven, samples were disaggregated in a solution of deionized water, Calgon, and H2O2 to ensure removal of clay-sized particles. Samples were then wet sieved through a 63 μm mesh sieve and rinsed with deionized water. The coarse fraction was placed on filter paper in an oven at ~40°C until it dried completely. Faunal identifications were made using a Meiji Techno RZ binocular light microscope. Taxonomic composition, abundance, and preservation state were observed in the &gt;63 μm size fraction.For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).Preservation and other abbreviations key: VG = very good, G = good, M = moderate, P = poor, S = brown-orange stained, R = radiolarians, D = diatoms, SS = sponge spicules, Ims = Iron monosulfides.
DOI: 10.1594/pangaea.979370
title: Foraminifera occurrences of IODP Hole 386-M0084C

description: Results of Foraminifera assemblage analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, micropaleontology samples were taken from the end of split cores at 5 m intervals. During the onshore phase approximately 2 cubic centimetres of sediment from each of these samples were analysed for foraminifera. After drying overnight in a ~40°C oven, samples were disaggregated in a solution of deionized water, Calgon, and H2O2 to ensure removal of clay-sized particles. Samples were then wet sieved through a 63 μm mesh sieve and rinsed with deionized water. The coarse fraction was placed on filter paper in an oven at ~40°C until it dried completely. Faunal identifications were made using a Meiji Techno RZ binocular light microscope. Taxonomic composition, abundance, and preservation state were observed in the &gt;63 μm size fraction.For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).Preservation and other abbreviations key: VG = very good, G = good, M = moderate, P = poor, S = brown-orange stained, R = radiolarians, D = diatoms, SS = sponge spicules, Ims = Iron monosulfides.
DOI: 10.1594/pangaea.979390
title: Foraminifera occurrences of IODP Hole 386-M0089C

description: Results of Foraminifera assemblage analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, micropaleontology samples were taken from the end of split cores at 5 m intervals. During the onshore phase approximately 2 cubic centimetres of sediment from each of these samples were analysed for foraminifera. After drying overnight in a ~40°C oven, samples were disaggregated in a solution of deionized water, Calgon, and H2O2 to ensure removal of clay-sized particles. Samples were then wet sieved through a 63 μm mesh sieve and rinsed with deionized water. The coarse fraction was placed on filter paper in an oven at ~40°C until it dried completely. Faunal identifications were made using a Meiji Techno RZ binocular light microscope. Taxonomic composition, abundance, and preservation state were observed in the &gt;63 μm size fraction.For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).Preservation and other abbreviations key: VG = very good, G = good, M = moderate, P = poor, S = brown-orange stained, R = radiolarians, D = diatoms, SS = sponge spicules, Ims = Iron monosulfides.
DOI: 10.1594/pangaea.979412
title: Foraminifera occurrences of IODP Hole 386-M0090C

description: Results of Foraminifera assemblage analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, micropaleontology samples were taken from the end of split cores at 5 m intervals. During the onshore phase approximately 2 cubic centimetres of sediment from each of these samples were analysed for foraminifera. After drying overnight in a ~40°C oven, samples were disaggregated in a solution of deionized water, Calgon, and H2O2 to ensure removal of clay-sized particles. Samples were then wet sieved through a 63 μm mesh sieve and rinsed with deionized water. The coarse fraction was placed on filter paper in an oven at ~40°C until it dried completely. Faunal identifications were made using a Meiji Techno RZ binocular light microscope. Taxonomic composition, abundance, and preservation state were observed in the &gt;63 μm size fraction.For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).Preservation and other abbreviations key: VG = very good, G = good, M = moderate, P = poor, S = brown-orange stained, R = radiolarians, D = diatoms, SS = sponge spicules, Ims = Iron monosulfides.
DOI: 10.1594/pangaea.979362
title: Foraminifera occurrences of IODP Hole 386-M0082C

description: Results of Foraminifera assemblage analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, micropaleontology samples were taken from the end of split cores at 5 m intervals. During the onshore phase approximately 2 cubic centimetres of sediment from each of these samples were analysed for foraminifera. After drying overnight in a ~40°C oven, samples were disaggregated in a solution of deionized water, Calgon, and H2O2 to ensure removal of clay-sized particles. Samples were then wet sieved through a 63 μm mesh sieve and rinsed with deionized water. The coarse fraction was placed on filter paper in an oven at ~40°C until it dried completely. Faunal identifications were made using a Meiji Techno RZ binocular light microscope. Taxonomic composition, abundance, and preservation state were observed in the &gt;63 μm size fraction.For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).Preservation and other abbreviations key: VG = very good, G = good, M = moderate, P = poor, S = brown-orange stained, R = radiolarians, D = diatoms, SS = sponge spicules, Ims = Iron monosulfides.
DOI: 10.1594/pangaea.979378
title: Foraminifera occurrences of IODP Hole 386-M0086B

description: Results of Foraminifera assemblage analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, micropaleontology samples were taken from the end of split cores at 5 m intervals. During the onshore phase approximately 2 cubic centimetres of sediment from each of these samples were analysed for foraminifera. After drying overnight in a ~40°C oven, samples were disaggregated in a solution of deionized water, Calgon, and H2O2 to ensure removal of clay-sized particles. Samples were then wet sieved through a 63 μm mesh sieve and rinsed with deionized water. The coarse fraction was placed on filter paper in an oven at ~40°C until it dried completely. Faunal identifications were made using a Meiji Techno RZ binocular light microscope. Taxonomic composition, abundance, and preservation state were observed in the &gt;63 μm size fraction.For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).Preservation and other abbreviations key: VG = very good, G = good, M = moderate, P = poor, S = brown-orange stained, R = radiolarians, D = diatoms, SS = sponge spicules, Ims = Iron monosulfides.
DOI: 10.1594/pangaea.979374
title: Foraminifera occurrences of IODP Hole 386-M0085B

description: Results of Foraminifera assemblage analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, micropaleontology samples were taken from the end of split cores at 5 m intervals. During the onshore phase approximately 2 cubic centimetres of sediment from each of these samples were analysed for foraminifera. After drying overnight in a ~40°C oven, samples were disaggregated in a solution of deionized water, Calgon, and H2O2 to ensure removal of clay-sized particles. Samples were then wet sieved through a 63 μm mesh sieve and rinsed with deionized water. The coarse fraction was placed on filter paper in an oven at ~40°C until it dried completely. Faunal identifications were made using a Meiji Techno RZ binocular light microscope. Taxonomic composition, abundance, and preservation state were observed in the &gt;63 μm size fraction.For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).Preservation and other abbreviations key: VG = very good, G = good, M = moderate, P = poor, S = brown-orange stained, R = radiolarians, D = diatoms, SS = sponge spicules, Ims = Iron monosulfides.
DOI: 10.1594/pangaea.973041
title: Spatiotemporal Distribution of Archaeological Sites in Borneo Over the Last 45,000 Years, with Emphasis on the Mid-Late Holocene (Last 6,000 Years) [chronology]

description: The dataset comprises 73 archaeological and historical sites across Borneo, a valuable resource for researchers interested in regional Bornean human occupation and settlement. It covers a period of 45 ka before the present (BP) to 0 BP (1950 CE), with a specific focus on the last 6 ka BP. The dataset provides detailed information on the location, timing, and duration of human occupation at each site, based on archaeological surveys. This compilation enables the study of resource use and their landscape legacies, making it an indispensable tool for understanding the regional Bornean human occupation and settlement. The archaeological site database was constructed based on a review of published reports and articles (see Perez-Cardenas et al., 2024). We reviewed and categorized each record between i) no radiocarbon data, such as U-series and U-Th dating, ii) calibrated radiocarbon, and iii) uncalibrated radiocarbon. Then, calibrated and uncalibrated radiocarbon were recalibrated to 95.4% confidence using the atmospheric curve IntCal20, OxCal 4.4 (Reimer et al., 2020). The dates obtained using Uranium were not calibrated. The lab code used in the original reference is provided for each record. We subset the dataset, obtaining 47 archaeological sites, by selecting sites with records over the last 6 ka BP to extract environmental characteristics. We created a matrix with the time and duration of occupation of archaeological evidence in 100-year intervals from 6 ka BP to 0 BP (1950 CE) for each site.
DOI: 10.1594/pangaea.973044
title: Spatiotemporal Distribution of Archaeological Sites in Borneo Over the Last 45,000 Years, with Emphasis on the Mid-Late Holocene (Last 6,000 Years) [environment]

description: The dataset comprises 73 archaeological and historical sites across Borneo, a valuable resource for researchers interested in regional Bornean human occupation and settlement. It covers a period of 45 ka before the present (BP) to 0 BP (1950 CE), with a specific focus on the last 6 ka BP. The dataset provides detailed information on the location, timing, and duration of human occupation at each site, based on archaeological surveys. This compilation enables the study of resource use and their landscape legacies, making it an indispensable tool for understanding the regional Bornean human occupation and settlement. The archaeological site database was constructed based on a review of published reports and articles (see Perez-Cardenas et al., 2024). We reviewed and categorized each record between i) no radiocarbon data, such as U-series and U-Th dating, ii) calibrated radiocarbon, and iii) uncalibrated radiocarbon. Then, calibrated and uncalibrated radiocarbon were recalibrated to 95.4% confidence using the atmospheric curve IntCal20, OxCal 4.4 (Reimer et al., 2020). The dates obtained using Uranium were not calibrated. The lab code used in the original reference is provided for each record. We subset the dataset, obtaining 47 archaeological sites, by selecting sites with records over the last 6 ka BP to extract environmental characteristics. We created a matrix with the time and duration of occupation of archaeological evidence in 100-year intervals from 6 ka BP to 0 BP (1950 CE) for each site.
DOI: 10.1594/pangaea.973108
title: Hydrography of Lake Grevelingen during MARIX cruises 2022-2023

description: The dataset comprises hydrographic observations collected during several cruises to Lake Grevelingen (The Netherlands) between 2022 and 2023 on board the R/V Navicula. The major aim in collecting CTD-data was to acquire information on the basic, sensor-based underlying physical and chemical conditions at the time of sampling, allowing an assessment of their spatial and temporal variability, as well as their role in controlling the biogeochemical cycling of several compounds (including climate-relevant trace gases). Data was collected by means of a SeaBird CTD system (SBE11) equipped with double sensors for temperature (SBE3), conductivity (SBE4), pressure (SBE9), oxygen (SBE43) and turbidity/fluorescence (FLNTU). . Data collection was carried out via a SeaBird Electronics deck unit using the Seasave software (version 7.26.7.107) software. Data processing was carried out by means of the Seasoft V2 software (https://www.seabird.com/software).
DOI: 10.1594/pangaea.973046
title: Spatiotemporal Distribution of Archaeological Sites in Borneo Over the Last 45,000 Years, with Emphasis on the Mid-Late Holocene (Last 6,000 Years) [archaeology]

description: The dataset comprises 73 archaeological and historical sites across Borneo, a valuable resource for researchers interested in regional Bornean human occupation and settlement. It covers a period of 45 ka before the present (BP) to 0 BP (1950 CE), with a specific focus on the last 6 ka BP. The dataset provides detailed information on the location, timing, and duration of human occupation at each site, based on archaeological surveys. This compilation enables the study of resource use and their landscape legacies, making it an indispensable tool for understanding the regional Bornean human occupation and settlement. The archaeological site database was constructed based on a review of published reports and articles (see Perez-Cardenas et al., 2024). We reviewed and categorized each record between i) no radiocarbon data, such as U-series and U-Th dating, ii) calibrated radiocarbon, and iii) uncalibrated radiocarbon. Then, calibrated and uncalibrated radiocarbon were recalibrated to 95.4% confidence using the atmospheric curve IntCal20, OxCal 4.4 (Reimer et al., 2020). The dates obtained using Uranium were not calibrated. The lab code used in the original reference is provided for each record. We subset the dataset, obtaining 47 archaeological sites, by selecting sites with records over the last 6 ka BP to extract environmental characteristics. We created a matrix with the time and duration of occupation of archaeological evidence in 100-year intervals from 6 ka BP to 0 BP (1950 CE) for each site.
description: binary value represents presence/absence: 1 represents presence and 0 absence, 2 represents records without a calibrated radiocarbon records
DOI: 10.1594/pangaea.983112
title: The HalOcAt-database of volatile short-lived halogenated hydrocarbons in ocean and atmosphere (1990 -2018)

description: The HalOcAt- database is a data product of the HaOcAt inititative (https://halocat.geomar.de), which was active from 2010 to 2018. The HalOcAt database was compiled as part of the doctoral thesis of F. Ziska at GEOMAR from 2010 to 2018. HalOcAt brought together global oceanic and atmospheric data sets of mainly short-lived brominated, chlorinated and iodinated trace gases, as bromoform (CHBr₃), dibromomethane (CH₂Br₂), dibromochloromethane (CHBr₂Cl), bromodichloromethane (CHBrCl₂), methyl bromide (CH₃Br), methyl iodide (CH₃I), diiodomethane (CH₂I₂), chloroiodomethane (CH₂ClI), bromoiodomethane (CH₂BrI), dichloromethane (CH₂Cl₂), chloroform (CHCl₃) , trichloroethane (C2HCl3), carbon tetrachloride (CCl4), tetrachloroethene (C2Cl4), and higher iodoalkanes (R–I).Many of the data of bromoform (CHBr₃), dibromomethane (CH₂Br₂), and methyl iodide (CH₃I), included in this zip-Archive have been used in the publication of global halocarbon emissions by Ziska, F. et al, 2013. The data and data products are attached as a supplement to the publication.In this HalOcAt data product halocarbon data from ocean and atmosphere were formatted into a uniform Excel template, which consists of three sheets. The first sheet contains the Metadata , the second and third sheet seawater, respectively air data, if available, with the columns: Sample Identifier, Sampling Gear, Date (UTC) and time, (Air sampling period), Sample start latitude (+ve N), Sample end latitude (+ve N), Sample start longitude (+ve E), Sample end longitude (+ve E), Sample depth (meter), Bottom Depth (meter), Water Temperature, in situ (°C), Water Salinity, CH3I (pM), CH2I2 (pM), C2H5I (pM), C3H7I (pM), C4H9I (pM), CH3Br (pM), CHBr3 (pM), CH2Br2 (pM), C2H5Br (pM), CH3Cl (pM), CHCl3 (pM), CH2Cl2 (pM), C2HCl3 (pM), C2Cl4 (pM), CH2ICl (pM), CH2IBr (pM), CHIBr2 (pM), CHBr2Cl (pM), CHBrCl2 (pM), Quality Control CommentsThe HalOcAt- database was curated on a best-effort basis rather than for full coverage. Missing entries are expected and are outside our responsibility. More halocarbon data in ocean and atmosphere from the involved scientists can be found on PANGAEA, other public databases or directly from the scientists.
DOI: 10.1594/pangaea.933398
title: XRF and biogeochemical characteristics of sediment core PG2201 from Lake Malaya Chabyda, Central Yakutia
DOI: 10.1594/pangaea.974941
title: Physical properties (MSCL) of IODP Hole 386-M0092D

description: Multi-Sensor Core Logger (MSCL) data (P-wave velocity, gamma ray attenuation (GRA) density, magnetic susceptibility, natural gamma radiation (NGR), noncontact resistivity (NCR)) from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). These data were obtained from whole round core sections by means of a Geotek MSCL during the offshore phase of the expedition. The offshore phase of expedition 386 took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan. As the aforementioned parameters are sensitive to temperature core sections were stored for at least 6 hours after arrival on deck before measurement to allow for temperature equilibration. The core physical properties were measured at predetermined optimal instrument-based spatial and temporal sampling intervals. GRA density, P-wave velocity, NCR, and magnetic susceptibility were measured every 2 cm, and NGR measurements were obtained every 10 cm. For further methodological information see methods chapter in Strasser, M. et al., 2023 https://doi.org/10.14379/iodp.proc.386.102.2023
description: Data was submitted and proofread by Vera Barbara Bender, MARUM - Center for Marine Environmental Sciences (University Bremen) on behalf of ECORD Science Operator Data Management (https://www.ecord.org).