cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.935171
title: Grain-size analysis and geochemical data of several event deposits in Lake Iznik (NW Turkey)

description: Grain-size analysis can help to discuss the energy of an event deposit and characterize its transport and depositional mechanism. The grain-size distribution at the event-deposit locations was analysed at a 5 mm vertical sampling interval on 7 cores (IZN19-13, IZN19-20, IZN19-21, IZN19-22, IZN19-24, IZN19-27, IZN19-29). A Beckman Coulter Life Science 13 230 XR laser particle-size analyser was used (EDYTEM Laboratory, University Savoie Mont-Blanc) with sonication to avoid particle flocculation. Two runs with a 30 s-long measurement were applied without any pre-treatment. Grain-size parameters were directly extracted from the Adapt software V. 1.3.337 and Gradistat V9.1 (Blott & Pye, 2001; doi:10.1002/esp.261). The sorting index was calculated according to Folk & Ward (1957; doi:10.1306/74D70646-2B21-11D7-8648000102C1865D).
DOI: 10.1594/pangaea.935182
title: Geochemistry of tephra from sediment core IZN19-15 from Lake Iznik (NW Turkey)

description: The occurrence of previously geochemically identified tephra allowed refinement of the age-depth model by comparison with previously established volcanic eruption history (Roeser et al., 2012). Tephra layers were polished on thin sections and the glass shards were geochemically characterized using a JEOL JXA-8230 Electron Probe X-ray Micro Analyzer (EMPA; ISTerre Laboratory, University Grenoble Alpes) equipped with 5 wavelength dispersive spectrometers (WDS) and one energy dispersive spectrometer (EDS) detector. The measurements used the following conditions: 15 kV voltage, 2 nA beam current, and 5 to 7 µm beam size. For standardization, MPI-DING glasses (StHs6/80-G, GOR132-G) (http://georem.mpch-mainz.gwdg.de; Jochum et al., 2000), natural minerals, and synthetic oxides were used. Two glasses, Atho-G (http://georem.mpch-mainz.gwdg.de; Jochum et al., 2000) and KE-12 (Metrich & Rutherford, 1992), were analyzed together with the samples to verify analytical accuracy and to exclude the loss of alkalis. Analyses of glass shards yielding a total oxide sum less than 96% or suggesting mineral impurities were not included in this study. Analytical data were normalized to 100% total oxide values to enable comparison.
DOI: 10.1594/pangaea.867835
title: Concentrations of anions in fluid samples from IODP Hole 357-M0072B

description: Sample precisions were ±3.9% for Cl, ±2.2% for Br, and ±4.3% for SO4, whereas both NO3 and F were at the limit of detection.
DOI: 10.1594/pangaea.935177
title: Geochemistry of tephra from sediment core IZN19-09 from Lake Iznik (NW Turkey)

description: The occurrence of previously geochemically identified tephra allowed refinement of the age-depth model by comparison with previously established volcanic eruption history (Roeser et al., 2012). Tephra layers were polished on thin sections and the glass shards were geochemically characterized using a JEOL JXA-8230 Electron Probe X-ray Micro Analyzer (EMPA; ISTerre Laboratory, University Grenoble Alpes) equipped with 5 wavelength dispersive spectrometers (WDS) and one energy dispersive spectrometer (EDS) detector. The measurements used the following conditions: 15 kV voltage, 2 nA beam current, and 5 to 7 µm beam size. For standardization, MPI-DING glasses (StHs6/80-G, GOR132-G) (http://georem.mpch-mainz.gwdg.de; Jochum et al., 2000), natural minerals, and synthetic oxides were used. Two glasses, Atho-G (http://georem.mpch-mainz.gwdg.de; Jochum et al., 2000) and KE-12 (Metrich & Rutherford, 1992), were analyzed together with the samples to verify analytical accuracy and to exclude the loss of alkalis. Analyses of glass shards yielding a total oxide sum less than 96% or suggesting mineral impurities were not included in this study. Analytical data were normalized to 100% total oxide values to enable comparison.
DOI: 10.1594/pangaea.868707
title: Natural gamma radiation from IODP Hole 357-M0076B
DOI: 10.1594/pangaea.965192
title: Monthly interpolated geochemical data from IODP Expedition 310 Tahiti coral, profile 310-5A-12R-1 (44-60 cm)

description: Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites skeletons recovered during IODP Expedition 310 "Tahiti Sea Level". These coral colonies have been U-Th dated and cover an age between 9.06 and 15.15 ka BP.
DOI: 10.1594/pangaea.965188
title: Monthly interpolated geochemical data from IODP Expedition 310 Tahiti coral, profile 310-9E-9R-1 (32-36 cm)

description: Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites skeletons recovered during IODP Expedition 310 "Tahiti Sea Level". These coral colonies have been U-Th dated and cover an age between 9.06 and 15.15 ka BP.
DOI: 10.1594/pangaea.965189
title: Monthly interpolated geochemical data from IODP Expedition 310 Tahiti coral, profile 310-9A-6R-1 (11-26 cm)

description: Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites skeletons recovered during IODP Expedition 310 "Tahiti Sea Level". These coral colonies have been U-Th dated and cover an age between 9.06 and 15.15 ka BP.
DOI: 10.1594/pangaea.873524
title: Sea floor drill rig videos of IODP Hole 357-M0076A
DOI: 10.1594/pangaea.935140
title: High-resolution XRF analysis of sediment core IZN19-11 from Lake Iznik (NW Turkey)

description: High-resolution XRF analysis of sediment cores (IZN19-05, IZN19-07, IZN19-09, IZN19-11, IZN19-13, IZN19-15, IZN19-20, IZN19-21, IZN19-22, IZN19-23, IZN19-24, IZN19-27, IZN19-28 and IZN19-29) from Lake Iznik, NW Turkey. The relative contents of major and trace elements were analysed with an X-Ray Fluorescence (XRF) Avaatech Core Scanner (EDYTEM Laboratory). The split-core surface was first covered with a 4-μm-thick Ultralene film to avoid contamination and desiccation of the sediment. All cores are registered in the French national cyber-core repository https://www.cybercarotheque.fr and the International Geo Sample Number (IGSN) service https://www.igsn.cnrs.fr/#/search. All cores were collected in April and July, 2019.
DOI: 10.1594/pangaea.965136
title: Monthly interpolated geochemical data from modern Tahiti coral MARAA-8

description: Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites modern corals ecovered at Tahiti that grew between 1996 and 2008 and serve as a modern-day benchmark.
DOI: 10.1594/pangaea.838278
title: Natural gamma radiation of IODP Hole 347-M0061C
DOI: 10.1594/pangaea.965137
title: Monthly interpolated geochemical data from modern Tahiti coral TIAREI-3B

description: Here we present monthly resolved geochemical proxy data (Sr/Ca, Mg/Ca, δ18O, δ13C) extracted along the growth axes of Porites modern corals ecovered at Tahiti that grew between 1996 and 2008 and serve as a modern-day benchmark.
DOI: 10.1594/pangaea.838283
title: Natural gamma radiation of IODP Hole 347-M0063A
DOI: 10.1594/pangaea.869858
title: Concentrations of major elements in fluid samples from IODP Hole 357-M0075X
DOI: 10.1594/pangaea.837843
title: Visual core description and core images IODP Hole 347-M0059A
DOI: 10.1594/pangaea.838282
title: Natural gamma radiation of IODP Hole 347-M0062D
DOI: 10.1594/pangaea.935141
title: High-resolution XRF analysis of sediment core IZN19-13 from Lake Iznik (NW Turkey)

description: High-resolution XRF analysis of sediment cores (IZN19-05, IZN19-07, IZN19-09, IZN19-11, IZN19-13, IZN19-15, IZN19-20, IZN19-21, IZN19-22, IZN19-23, IZN19-24, IZN19-27, IZN19-28 and IZN19-29) from Lake Iznik, NW Turkey. The relative contents of major and trace elements were analysed with an X-Ray Fluorescence (XRF) Avaatech Core Scanner (EDYTEM Laboratory). The split-core surface was first covered with a 4-μm-thick Ultralene film to avoid contamination and desiccation of the sediment. All cores are registered in the French national cyber-core repository https://www.cybercarotheque.fr and the International Geo Sample Number (IGSN) service https://www.igsn.cnrs.fr/#/search. All cores were collected in April and July, 2019.
DOI: 10.1594/pangaea.935154
title: High-resolution XRF analysis of sediment core IZN19-29 from Lake Iznik (NW Turkey)

description: High-resolution XRF analysis of sediment cores (IZN19-05, IZN19-07, IZN19-09, IZN19-11, IZN19-13, IZN19-15, IZN19-20, IZN19-21, IZN19-22, IZN19-23, IZN19-24, IZN19-27, IZN19-28 and IZN19-29) from Lake Iznik, NW Turkey. The relative contents of major and trace elements were analysed with an X-Ray Fluorescence (XRF) Avaatech Core Scanner (EDYTEM Laboratory). The split-core surface was first covered with a 4-μm-thick Ultralene film to avoid contamination and desiccation of the sediment. All cores are registered in the French national cyber-core repository https://www.cybercarotheque.fr and the International Geo Sample Number (IGSN) service https://www.igsn.cnrs.fr/#/search. All cores were collected in April and July, 2019.
DOI: 10.1594/pangaea.838286
title: Natural gamma radiation of IODP Hole 347-M0063D
DOI: 10.1594/pangaea.838824
title: Thermal conductivity of IODP Hole 347-M0064C
DOI: 10.1594/pangaea.837855
title: Visual core description and core images IODP Hole 347-M0062C
DOI: 10.1594/pangaea.915887
title: Description of lithologic section units of IODP Hole 381-M0079A

description: Drilling deformation intensity: 0 = undisturbed, 1 = slight, 2 = moderate, 3 = high, 4 = severe.
DOI: 10.15468/dl.auznrk
title: Occurrence Download

description: A dataset containing 1019552 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-71.62 -13.12,-69.27 -13.12,-69.27 -12.83,-71.62 -12.83,-71.62 -13.12))",
 "OccurrenceStatus is Present"
 ]
}

 The dataset includes 1019552 records from 279 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0014182-251025141854904/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.839780
title: Calculated salinity and elemental ratios of interstitial water of IODP Hole 347-M0063C
DOI: 10.1594/pangaea.868489
title: Normalized, volatile-free major element concentrations and trace element compositions of representative lithologies from IODP Hole 357-M0076B
DOI: 10.1594/pangaea.753975
title: Core-section summary for Hole 313-M0028A
DOI: 10.1594/pangaea.837845
title: Visual core description and core images IODP Hole 347-M0059C
DOI: 10.1594/pangaea.870616
title: Thin sections from IODP Hole 357-M0072B
DOI: 10.1594/pangaea.786017
title: (Table T1-3) Stable carbon and oxygen isotope ratios of cool-water Bryozoa Idmidronea spp. from ODP Leg 182 sites
DOI: 10.1594/pangaea.914115
title: Nonmarine diatom counts for IODP Hole 381-M0078A
DOI: 10.1594/pangaea.838348
title: Moisture and density (MAD) measured on IODP Hole 347-M0059E
DOI: 10.1594/pangaea.839843
title: Composite depth scale of IODP Hole 347-M0063A
DOI: 10.1594/pangaea.708732
title: Light reflectance (RGB) of Hole 302-M0004C
DOI: 10.1594/pangaea.868127
title: Sensor signal time log from IODP Hole 357-M0068A
DOI: 10.1594/pangaea.754299
title: X-ray diffraction analysis and quantification of minerals of Hole 313-M0028A
DOI: 10.1594/pangaea.914948
title: Nitrous oxide production rates in the eastern tropical South Pacific during METEOR cruise M138

description: N2O production rates from ammonium, nitrite and nitrate and nitrate reduction rates and ammonium oxidation rates from the top 400 m water depth off the coast of Peru sampled from R/V Meteor during M138 in June 2017.
DOI: 10.1594/pangaea.754233
title: Thermal conductivity of IODP Hole 313-M0028A
DOI: 10.1594/pangaea.914493
title: X-Ray fluorescence (XRF) scanning results (30kV run) of IODP Hole 381-M0079A
DOI: 10.1594/pangaea.351435
title: Pore water samples and chemistry of Hole 302-M0003A
DOI: 10.1594/pangaea.753972
title: Core summary for Hole 313-M0028A

description: Drillers log: hdl:10013/epic.36807.d001
DOI: 10.1594/pangaea.913460
title: Core Catcher images (processed) of IODP Hole 381-M0078A
DOI: 10.1594/pangaea.912540
title: Location, morphometry, lithology and land-use in the watersheds of reservoirs in Southern Spain

description: We collected data of reservoir area, capacity, age, and location from open databases: Infraestructura de Datos Espaciales de Andalucía (IDEAndalucia; http://www.ideandalucia.es/portal/web/ideandalucia/) and the Ministerio para la Transición Ecológica (https://www.embalses.net/). The reservoir capacity (m3) divided by its surface area (m2) will yield the mean depth (m).We obtained the lithology and land-use maps using ArcGIS® 10.2 software (ESRI 2012) under the Universidad de Granada license. First, we delimited the watershed of each reservoir using the rivers and hydrographical demarcations, and, second, we calculated the area for each different type of lithology and land-use within watersheds. We used the databases: Infraestructura de Datos Espaciales (IDE) from the Ministerio de Agricultura, Pesca y Alimentación (MAPA; https://www.mapa.gob.es/es/cartografia-y-sig/ide/default.aspx); the Infraestructura de Datos Espaciales de Andalucía(IDEAndalucia; http://www.ideandalucia.es/portal/web/ideandalucia/); the Instituto Geológico y Minero de España (IGME; http://www.igme.es/default.asp); the Confederación Hidrográfica del Segura (CHSEGURA; https://www.chsegura.es/chs/); and The Junta de Comunidades de Castilla-La Mancha (IDE-JCCM; https://castillalamancha.maps.arcgis.com/home/index.html). We defined the next categories: water-covered area; carbonate-rich rocks; limestones, marls, and dolomites; gravels, conglomerates, sands and silts; and non-calcareous rocks. The soils with high capacity to solubilize dissolved inorganic carbon are carbonate-rich rocks and limestones, marls, and dolomites. In contrast, non-calcareous rocks include igneous rocks like basalt and metamorphic rocks like marble, schist, quartzite, phyllite, gneiss, and slate have less capacity to leach dissolved inorganic carbon. The land-use categories were: crops, forest, urban, treeless area, and water covered area. The forestry area includes trees, plantation trees, sparse trees, and dispersed trees.
DOI: 10.1594/pangaea.754153
title: Natural remanent magnetization polarity estimation of Hole 313-M0028A
DOI: 10.1594/pangaea.870622
title: Visual core description and core images from IODP Hole 357-M0068A
DOI: 10.1594/pangaea.870623
title: Visual core description and core images from IODP Hole 357-M0068B
DOI: 10.1594/pangaea.870620
title: Thin sections from IODP Hole 357-M0076B
DOI: 10.1594/pangaea.870625
title: Visual core description and core images from IODP Hole 357-M0070A
DOI: 10.1594/pangaea.870619
title: Thin sections from IODP Hole 357-M0076A
DOI: 10.1594/pangaea.886115
title: Foraminifers of IODP Hole 364-M0077A
DOI: 10.1594/pangaea.962223
title: Dissolved methane concentration variability along freshwater-sea continuum at Geesthacht, northern Germany, 2021

description: The dataset is about temporal variability of dissolved methane along the freshwater-sea continuum in northern Germany. Sensors were installed at fixed stations at in total three sites at different water depths. This dataset is from the station in Geesthacht (53.4112 N, 10.4032 E) at about 2 meter depth. The data was obtained between 14 April and 29 September 2021) in high frequency measurements (1 min) with a methane sensor from Kongsberg (4H Jena model CONTROS HydroC CH4,). Methane concentrations were calculated according to manufacturer's instructions. Data on temperature were provided by from Vattenfall, Kernkraftwerk Krümel, a salinity of 0.01 was assumed. Special thanks to the colleagues from Vattenfall for the logistic and technical support. For the quality control of the data a local range of 0.1 – 5000 nmol/L was set, a technical range for the pump power 2 – 8. Watt, a spike and gradient value of 1. For a more detailed description see the article cited in References.
DOI: 10.1594/pangaea.867539
title: Chemical compositions of representative lithologies from IODP Hole 357-M0071A
DOI: 10.1594/pangaea.870629
title: Visual core description and core images from IODP Hole 357-M0071B
DOI: 10.1594/pangaea.870631
title: Visual core description and core images from IODP Hole 357-M0072A
DOI: 10.1594/pangaea.962224
title: Dissolved methane concentration variability along freshwater-sea continuum at Heligoland, Southern North Sea, 2021

description: The dataset is about temporal variability of dissolved methane along the freshwater-sea continuum in northern Germany. Sensors were installed at fixed stations at in total three sites at different water depths. This dataset is from the station in Heligoland (54.1833 N, 7.8667 E) at about 9-12m depth (depending on the tide). The data was obtained between 27 April and 28 October in high frequency measurements (1 min) with a methane sensor from Kongsberg (4H Jena model CONTROS HydroC CH4,). Methane concentrations were calculated according to manufacturer's instructions, based on temperature and salinity values from UW-node Heligoland (Fischer, Philipp; Happel, Lea; Brand, Markus; Eickelmann, Laura; Lienkämper, Miriam; Bussmann, Ingeborg; Anselm, Norbert; Brix, Holger (2022): Hydrographical time series data of Helgoland, Southern North Sea, 2021. PANGAEA, https://doi.org/10.1594/PANGAEA.950173). A gap in the salinity data was replaced with the median value of the observed time span (31.66). For the quality control of the data a local range of 0.1 – 1000 nmol/L was set, a technical range for the pump power 2 – 8. Watt, a spike and gradient value of 1. For a more detailed description see the article cited in References.
DOI: 10.1594/pangaea.943832
title: Data from a multi-proxy comparison from the Little Belt (IODP Expedition 347, Site M0059: palynomorph, diatom, geochemical data)

description: The data published here were gathered in the framework of a multi-proxy-based study of paleotemperature (both marine and terrestrial), -salinity, and -ecosystem changes from the Little Belt (Site M0059). They cover the past ~8,000 years and contain only material from the uppermost subunits 1a and 1b encountered at Site M0059 (see e.g. Andrén et al. 2015). Four environmental zones (EZ1: oldest, freshwater conditions; EZ2 to EZ4 reflecting following salinity and ecosystem changes in the region) were identified in Kotthoff et al. (2017). The age model and the sedimentology are discussed in Kotthoff et al. (2017). The datasets comprise data for salinity proxies (diatoms, aquatic palynomorphs, diol index) and for water temperature proxies (foraminiferal Mg/Ca-ratios, long chain diol index and TEXL86) as well as temperature reconstruction based on pollen grains. It is discussed in Kotthoff et al. (2017) that applying and interpreting proxies in coastal environments and marginal seas needs particular caution. For example, foraminiferal Mg/Ca-ratios may have been influenced by contamination by authigenic coatings in the deeper intervals of the record. Lipid paleothermometers were probably influenced by significant changes in depositional settings in the Little Belt. References: Andrén, T., Jørgensen, B.B., Cotterill, C., and the Expedition 347 Scientists: Baltic Sea Paleoenvironment. Proceedings IODP, 347. College Station, TX (Integrated Ocean Drilling Program), https://doi.org/10.2204/iodp.proc.347.101.2015, 2015. Kotthoff, U., Groeneveld, J., Ash, J. L., Fanget, A.-S., Krupinski, N. Q., Peyron, O., Stepanova, A., Warnock, J., Van Helmond, N. A. G. M., Passey, B. H., Clausen, O. R., Bennike, O., Andrén, E., Granoszewski, W., Andrén, T., Filipsson, H. L., Seidenkrantz, M.-S., Slomp, C. P., and Bauersachs, T.: Reconstructing Holocene temperature and salinity variations in the western Baltic Sea region: a multi-proxy comparison from the Little Belt (IODP Expedition 347, Site M0059), Biogeosciences, 14, 5607–5632, https://doi.org/10.5194/bg-14-5607-2017, 2017.
DOI: 10.1594/pangaea.962221
title: Dissolved methane concentration variability along freshwater-sea continuum at Cuxhaven, northern Germany, 2021

description: The dataset is about temporal variability of dissolved methane along the freshwater-sea continuum in northern Germany. Sensors were installed at fixed stations at in total three sites at different water depths. This dataset is from the station in Cuxhaven (53.8771 N, 8.7048 E) taken at about 2-7m depth (depending on the tide). The data was obtained between 11 April and 28 August 2021 in high frequency measurements (1 min) with a methane sensor from Kongsberg (4H Jena model CONTROS HydroC CH4). Methane concentrations were calculated according to manufacturer's instructions, based on temperature and salinity values from COSYNA Container Cuxhaven. For the quality control of the data a local range of 0.1 – 1000 nmol/L was set, a technical range for the pump power 2 – 8 Watt, a spike and gradient value of 1. Due to heavy biofouling the external pump of the sensor failed, resulting in data gaps. For a more detailed description see the article cited in References.
DOI: 10.1594/pangaea.837810
title: Core-section summary for IODP Hole 347-M0059D
DOI: 10.1594/pangaea.869853
title: Concentrations of major elements in fluid samples from IODP Hole 357-M0072Z
DOI: 10.1594/pangaea.869852
title: Concentrations of major elements in fluid samples from IODP Hole 357-M0072X
DOI: 10.1594/pangaea.837833
title: Core-section summary for IODP Hole 347-M0064C
DOI: 10.1594/pangaea.869851
title: Concentrations of major elements in fluid samples from IODP Hole 357-M0072B
DOI: 10.1594/pangaea.838443
title: Physical properties (Fast Track) of IODP Hole 347-M0059E
DOI: 10.1594/pangaea.839795
title: Calculated salinity and elemental ratios of interstitial water of IODP Hole 347-M0062A
DOI: 10.1594/pangaea.838820
title: Thermal conductivity of IODP Hole 347-M0061B
DOI: 10.1594/pangaea.838825
title: Thermal conductivity of IODP Hole 347-M0065A
DOI: 10.1594/pangaea.873533
title: (Table 1) Description of IODP rock samples from the Atlantis Massif, near the Mid-Atlantic Ridge
DOI: 10.1594/pangaea.913468
title: X-ray diffraction results from IODP Hole 381-M0078B

description: Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™.
DOI: 10.1594/pangaea.837991
title: Light reflectance (RGB) of IODP Hole 347-M0064B
DOI: 10.1594/pangaea.868719
title: Light reflectance (RGB) of IODP Hole 357-M0070B
DOI: 10.1594/pangaea.881450
title: Planktonic foraminifera in sediment core CH69-K09
DOI: 10.1594/pangaea.840568
title: Distribution and abundance of benthic foraminifera from IODP Hole 347-M0059B

description: Abundance: A = abundant, C = common, F = few, R = rare, B = barren, V = very high.
DOI: 10.1594/pangaea.867526
title: Magnetic susceptibility and demagnetized inclinations measured on discrete samples from IODP Hole 357-M0069A
DOI: 10.1594/pangaea.838468
title: Physical properties of IODP Hole 347-M0060A
DOI: 10.1594/pangaea.913291
title: Shear strength (handheld penetrometer) from IODP Hole 381-M0079A
DOI: 10.1594/pangaea.959134
title: Benthic macrofauna and foraminifera (&gt;500 µm) diversity, abundance and biomass on the Northeast Greenland (NEG) shelf sediments during POLARSTERN cruise PS109

description: The samples have been collected with R/V Polarstern during PS109 between September and October 2017. Sediment was collected with a camera-equipped MUC (TV-MUC; diameter of 93mm; circle area 0.007 m2) or with a benthic lander (dimensions 20 cmx20 cm; square area 0.04 m²), sliced into 0-5 cm and 5-10 cm layers and subsequently sieved over a 500 µm mesh. Afterwards, the samples were fixed with 4 % seawater-buffered formaldehyde in Kautex bottles at room temperature. In the lab, samples were stained with Rose Bengal and macrofauna and foraminifera individuals were identified to the lowest taxonomic level possible, and the blotted wet formalin weight of macrofauna individuals was measured with a precision balance (DeltaRange XP56 or AX205; Mettler Toledo, Ohio, USA).
DOI: 10.1594/pangaea.913297
title: Shear strength (shear vane and fall cone) from IODP Hole 381-M0080A