cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.26022/ieda/111941
title: Major and trace elemental analyses of fine-grained mafic igneous rock from Stephenson et al (2021): “Cenozoic Dynamic Topography of Madagascar”

description: Ten samples of fine-grained mafic igneous rock collected from northern Madagascar (i.e. Nosy Be and Bobaomby peninsula) in 2012 and 2015. Samples were analyzed for major, trace and rare earth elemental (REE) compositions using inductively-coupled plasma-mass spectrometry (ICP-MS) and X-ray fluorescence (XRF) at the universities of Cambridge and Edinburgh, respectively.
description: Stephenson, S. N., White, N. J., Carter, A., Seward, D., Ball, P. W. and Klöcking, M. (2021). "Cenozoic Dynamic Topography of Madagascar", G3.
DOI: 10.26022/ieda/111948
title: δ13C, δ18O and Δ47 records in biogenic, pedogenic and geogenic carbonate types in Nussloch paleosol-loess sequence

description: δ13C, δ18O, and clumped isotope-derived paleotemperatures [T(Δ47)] from the Quaternary Nussloch paleosol-loess sequence (Rhine Valley, SW Germany). δ13C,δ18O, and T(Δ47) values of co-occurring rhizoliths, loess dolls, land-snail shells, earthworm biospheroliths, and “bulk” (geogenic) carbonates from three sediment layers. Range in sample age ~40 to 20 ka.
description: Zamanian, K., Lechler, A.R., Schauer, A.J., Kuzyakov, Y. and Huntington, K.W., 2021. "The δ13C, δ18O and Δ47 records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning." Quaternary Research, pp.1-17.
DOI: 10.26022/ieda/111938
title: Helium, neon and argon raw data of the Washington County iron meteorite

description: Helium, neon and argon were measured in six bulk samples and one acid residue of the Washington County iron meteorite to detect solar noble gas signatures in interior parts of the meteorite. We list raw data of the seven splits of Washington County, made with three different spectrometers. Raw data encompass the signals extrapolated to gas inlet time, and in case of Heidelberg data are netto signals after subtraction of spectrometer background (including interference corrections on neon isotopes).
description: Vogt, Manfred; Trieloff, Mario; Ott, Ulrich; Hopp, Jens; Schwarz, Winfried H., (in review), "Solar noble gases in an iron meteorite indicate terrestrial mantle signatures derive from Earth’s core". Communications Earth & Environment
DOI: 10.26022/ieda/111939
title: Pressure, temperature, P- and S-wave velocities and density of MgSiO3 majorite

description: Pressure, Temperature, P- and S-wave velocities and density of MgSiO3 majorite obtained simultaneously from travel time, X-ray radiography length, and X-ray diffraction measurements on polycristalline aggregates up to 18.4 Gpa and 2000 K, in the multianvil apparatus at the beamline BL04B1 in SPring-8.
description: The manuscript is under review at the journal "Geophysical Research Letter"
DOI: 10.26022/ieda/111936
title: Iron isotope measurements of mineral separates in partially serpentinized peridotite from the New Caledonia Ophiolite

description: This dataset contains Fe isotope measurements of mineral separates in partially serpentinized peridotite from the New Caledonia Ophiolite. These results demonstrate that magnetite and awaruite are isotopically heavy relative to relict minerals (olivine, pyroxene), while serpentinite is isotopically heavy relative to relict grains. This finding is consistent with the predicted sense of fractionation from chemical modeling.
description: Scott, S.R., Sims, K.W.W., Frost, B.R.; Keleman, P.B., Evans, K.A., Swapp, S.M.,(2017), "On the hydration of olivine in ultramafic rocks: Implications from Fe isotopes in serpentinites." Geochimica et Cosmochimica Acta, 215:105-121
DOI: 10.26022/ieda/111920
title: Clumped isotopes measured in planktonic foraminifera species T. trilobus and G. tumida from IODP Site U1488 (Meinicke et al., 2021)

description: This dataset contains D47, d18O and d13C data from Site U1488 in the central Western Pacific Warm Pool measured in two species of plantonic foraminifera, Trilobatus trilobus and Globorotalia tumida. The data covers several time intervals from the last 6 Myrs. In addition to the mean sample data used in the publication, replicate-level raw data is provided to allow for reprocessing of the data.
description: Meinicke, N., Reimi, M. A., Ravelo, A. C., & Meckler, A. N. (2021). Coupled Mg/Ca and clumped isotope measurements indicate lack of substantial mixed layer cooling in the Wes! tern Pacific Warm Pool during the last ∼5 million years. Paleoceanography and Paleoclimatology, 36, e2020PA004115.
DOI: 10.26022/ieda/111932
title: Elemental analyses and cosmogenic 3He measurements of bulk soil and detrital minerals from a soil near Whitewater, California, USA

description: ICP-MS elemental analyses and helium isotope measurements of bulk soil samples and detrital magnetite grains to measure the cosmogenic 3He exposure age of a soil offset by the Banning Strand of the San Andreas Fault near Whitewater (CA). Magnetite separates were extracted by a neodymium magnet and then microCT scanned to detect mineral inclusions before helium measurement. Some samples contain inclusions, while others are inclusion-free.
DOI: 10.26022/ieda/111930
title: Geochemical data from carbonates of the Chuanlinggou-Tuanshanzi formations, North China

description: Samples were collected along newly exposed road cuts at the Dalongmen village, Miyun area (Beijing, China). A total of 99 carbonate samples from a ~200 m succession spanning the lower Chuanlinggou Formation and the Tuanshanzi Formation were analyzed. This file contains I, Ca, Mg, Mn, Sr, P, Al, TOC, d13Ccarb, d18O and d13Corg of these samples.
description: Wei Beilei, Tang Dongjie, Shi Xiaoyin, et al., "A pulsed oxygenation in terminal Paleoproterozoic ocean: Evidence from the transition between the Chuanlinggou and Tuanshanzi formations, North China." Geochemistry, Geophysics, Geosystems, in review
DOI: 10.26022/ieda/111922
title: Raw clumped isotope sample and standard data of modern and fossil Cittarium pica from Bermuda for manuscript submission titled "Seasonally Variable Aquifer Discharge and Cooler Climate in Bermuda during the Last Interglacial Revealed by Subannual Clumped Isotope Analysis"

description: In this dataset, we present new, subannual-scale clumped isotope measurements on five of the ten C. pica shells from the original Winkelstern et al., 2017 study (1 modern, 2 fossils from DB/RB, 2 fossils from GB) to investigate the seasonal persistence and timing of interglacial cooling in Bermuda and determine whether inter-site differences may have been the result of seasonal sampling bias. Published clumped isotope data from Winkelstern et al. (2017) were recalculated using improved data processing techniques (IUPAC/Brand parameters; see Petersen et al. 2019) for more accuracy and to enable better comparison with new data.
DOI: 10.26022/ieda/111910
title: Samail ophiolite ID-TIMS U-Pb zircon geochronology from Rioux et al. (JGR, 2021)

description: ID-TIMS U-Pb zircon data from the Samail ophiolite, Oman and the United Arab Emirates. Data collected in the Isotope Laboratory at MIT.
description: Matthew Rioux, Joshua M. Garber, Michael Searle, Peter Kelemen, Sumio Miyashita, Yoshiko Adachi, Samuel Bowring, in press, "High-precision U-Pb zircon dating of late magmatism in the Samail ophiolite: A record of subduction initiation" Journal of Geophysical Research. Matthew Rioux, Mathieu Benoit, Isma Amri, Georges Ceuleneer, Joshua M. Garber, Michael Searle, Kayla Leal, in press, "The origin of felsic intrusions within the mantle section of the Samail ophiolite: Geochemical evidence for three distinct mixing and fractionation trends" Journal of Geophysical Research.;
DOI: 10.26022/ieda/111917
title: Polycyclic aromatic hydrocarbons (PAHs) concentration in particulate matter (PM) from Tyumen City, Russia

description: This dataset contain the results of our study of polycyclic aromatic hydrocarbons (PAHs) deposited with the particulate matter (PM) of snow in the city of Tyumen (Russia) and in nearby background areas. Tyumen is one of the most rapidly developing cities in Siberia due to oil and gas extraction in the north of the Tyumen Region. The aim of the study was to evaluate the concentrations of PAHs in the PM phase of snow within the city of Tyumen and to identify their sources and any adverse environmental effects. 14 U.S. Environmental Protection Agency priority-listed PAHs were detected in snow solid phase samples: naphthalene (NaP), fluorene (Flu), phenanthrene (Phe), anthracene (Ant), fluoranthene (Flt), pyrene (Pyr), benzo(a)anthracene (BaA), chrysene (Chr), benzo(b)fluoranthene (BbF), benzo(k)fluoranthene (BkF), benzo(a)pyrene (BaP), dibenzo(a,h)anthracene (DahA), benzo(ghi)perylene (BghiP), indeno[1,2,3-cd]pyrene (IcdP)
description: Dmitriy Moskovchenko, Roman Pozhitkov, Aleksandr Tigeev and Evgeny Lodygin (2021) "Polycyclic aromatic hydrocarbons (PAHs) in atmospheric particulate depositions in Tyumen, Russia" (submitted)
DOI: 10.26022/ieda/111901
title: Mineral Analyses of Eucrite-type Achondrites

description: Mineral analyses and mineral composition diagrams for 42 eucrites and eucrite-type achondrites determined by electron microprobe analyses at NASA-Johnson Space Center are presented. The data were collected to support petrologic interpretations of the meteorites as given in the related publications identified in the datafiles. Full analytical protocols for the analyses are presented in related publication #2.
DOI: 10.26022/ieda/111913
title: Experimental Determination of Mantle Solidi and Melt Compositions for Two Likely Rocky Exoplanet Compositions

description: This dataset presents the conditions and run product compositions for partial mantle melting experiments performed in a piston-cylinder on hypothetical silicate exoplanet mantle compositions. All analyses and experiments were conducted at Arizona State University except for analysis of experiment R137 which was done at the Earth & Planets Laboratory, Carnegie Institution for Science.
description: Brugman, K. K., Phillips, M. G., & Till, C. B. (in review). "Experimental Determination of Mantle Solidi and Melt Compositions for Two Likely Rocky Exoplanet Compositions." Journal of Geophysical Research: Planets.
DOI: 10.26022/ieda/111911
title: Radiometric ages from faulted volcanic units of Silali volcano, Kenya Rift.

description: Ar40_Ar39 Ages of volcanic rocks from Silali volcano, Kenya. The volcano is located in the actively spreading East African Rift. Its volcanic units show normal faulting and were sampled to constrain the timing of the fault activity at the volcano. We present 4 radiometric ages (3x step heating, 1x total fusion).
description: Riedl, S., Melnick, D., Njue, L., Sudo, M., & Strecker, M. R. (2022). Mid-Pleistocene to recent crustal extension in the inner graben of the Northern Kenya Rift. Geochemistry, Geophysics, Geosystems, 23, e2021GC010123. https://doi.org/10.1029/2021GC010123
DOI: 10.26022/ieda/111905
title: Major, trace element and U, Li isotope analyses of river water from the Kaoping River, Taiwan

description: River water samples collected from Kaoping River, Taiwan on a seasonal basis during 2006, 2009, and 2010 are analyzed for major and trace elemental concentrations, as well as U and Li isotopes, to understand the water chemistry and weathering processes.
description: Wang, R.M., You, C.F., Chung, C.H., Huang, K.F., Hsu, Y.J. (Submitted 2021). Uranium isotopes in a subtropical mountainous river of Taiwan: Insight into the physical and chemical weathering processes. Submitted to Geochemistry, Geophysics, Geosystems.
DOI: 10.26022/ieda/111900
title: The Effects of Phosphorus on Partial Melting of the Martian Mantle and Compositions of the Martian Crust

description: This dataset presents the experimental bulk composition and the phase composition and abundances for the piston-cylinder experiments detailed in the The Effects of Phosphorus on Partial Melting of the Martian Mantle and Compositions of the Martian Crust paper. Experiments correspond to two set of partial melting experiments on a martian primitive mantle composition at 2 GPa with P2O5 = 0 wt.% and 0.5 wt.%.
description: Payré & Dasgupta, The Effects of Phosphorus on Partial Melting of the Martian Mantle and Compositions of the Martian Crust, GCA, submitted
DOI: 10.26022/ieda/111904
title: Microbeam analyses of glasses and minerals in Karoo picrites

description: Magmatic products of the Karoo Large Igneous Province can be divided into a volumetrically dominant, compositionally uniform low-Ti tholeiitic suite, and a subordinate, geographically restricted, compositionally diverse, incompatible-rich high-Ti suite. High-Ti picrites contain up to 2400 ppm Sr, 1900 ppm Ba and 550 ppm Zr, which seems unusual for olivine-enriched rocks. We studied six Karoo picrites to determine the phase(s) in which Sr resides. Samples consist of 10–30 % olivine phenocrysts in a groundmass of brown glass, augite, feldspar, ilmenite and apatite. Glass compositions vary, but are generally evolved, ranging from basaltic trachyandesite to dacite. X-ray intensity maps demonstrate that most of the Sr resides in the glasses, and to a lesser extent, in feldspars, if present. Some samples contain two texturally and compositionally distinct glasses, best modelled in terms of magma hybridization: variably accumulated olivine phenocrysts surrounded by evolved Sr-rich (to 9470 ppm) Type 2 melts formed by extensive olivine fractionation were infiltrated by chemically distinct Type 1 melts. Upon eruption, Type 2 melt quenched to minor glass around olivine phenocrysts, and the dominant Type 1 glass acquired its evolved composition by quench-crystallization of groundmass mineral phases. Both glasses are rich in H2O (up to 3.8 wt. %) but are nearly devoid of CO2. Calculated parental melts have much higher K2O and incompatible trace elements (e.g. Sr or Ba &gt;1200 ppm) relative to low-Ti tholeiites. The unusual parental melt compositions imply derivation by small degrees of partial melting from SCLM mantle sources enriched in Sr and other incompatibles.
DOI: 10.26022/ieda/111899
title: Oxygen Fugacity Across Tectonic Settings

description: Here we compile published analytical data from lithologies that constrain fO2 (n=860 volcanic rocks - lavas and tephras and n=326 mantle lithologies- the majority peridotites) from ridges, back-arc basins, forearcs, arcs, and plumes. Because calculated fO2 varies with choice of activity model, we re-calculate fO2 for each dataset from compositional data, applying the same set of activity models and methodologies for each data type. Additionally, we compile trace element concentrations (e.g. vanadium) which serve as an additional fO2-proxy. The compiled data show that, on average, volcanic rocks and mantle rocks from the same tectonic setting yield similar fO2s, but mantle lithologies span a much larger range in fO2 than volcanics. Multiple Fe-based oxybarometric methods and vanadium partitioning vary with statistical significance as a function of tectonic setting, with fO2 ridges &lt; back arcs &lt; arcs. Plume lithologies are more nuanced to interpret, but indicate fO2s &gt;= ridges.
description: Cottrell, E., S. Birner, M. Brounce, F. A. Davis, L. E. Waters and K. A. Kelley (In Press). Oxygen Fugacity Across Tectonic Settings. AGU Geophysical Monograph Redox variables and mechanisms in magmatism and volcanism. D. R. Neuville and R. Moretti, Wiley. 2020. DOI: 10.1002/essoar.10502445.1
DOI: 10.22008/fk2/sd56cb/nq0lgj
title: snow_specific_surface_area-2.tif

description: SICE NRT
DOI: 10.22008/fk2/sd56cb/tuj3fv
title: r_TOA_06-2.tif

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DOI: 10.22008/fk2/sd56cb/01p7mi
title: snow_specific_surface_area-2.tif

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DOI: 10.22008/fk2/sd56cb/a43xym
title: r_TOA_17-2.tif

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DOI: 10.22008/fk2/sd56cb/gig9wa
title: SCDA_final-2.tif

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DOI: 10.22008/fk2/sd56cb/mmaj7u
title: SCDA_v20-2.tif

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title: albedo_bb_planar_sw-2.tif

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title: r_TOA_21-2.tif

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title: r_TOA_21-2.tif

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title: r_TOA_17-2.tif

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title: r_TOA_06-2.tif

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title: r_TOA_01-2.tif

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DOI: 10.22008/fk2/sd56cb/t9bucb
title: BBA_combination-2.tif

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DOI: 10.22008/fk2/sd56cb/2exmxh
title: SCDA_v20-2.tif

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title: albedo_bb_planar_sw-2.tif

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DOI: 10.22008/fk2/sd56cb/gu0p90
title: SCDA_final-2.tif

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DOI: 10.22008/fk2/sd56cb/oba4ps
title: snow_specific_surface_area-2.tif

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title: BBA_combination-2.tif

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title: r_TOA_21-2.tif

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title: r_TOA_17-2.tif

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title: r_TOA_01-2.tif

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title: r_TOA_06-2.tif

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title: SCDA_final-2.tif

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title: r_TOA_01-2.tif

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DOI: 10.22008/fk2/sd56cb/ffzsvk
title: snow_specific_surface_area-2.tif

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DOI: 10.22008/fk2/sd56cb/h0hkqq
title: albedo_bb_planar_sw-2.tif

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DOI: 10.22008/fk2/sd56cb/rmgr2q
title: SCDA_v20-2.tif

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DOI: 10.22008/fk2/sd56cb/rtpl7s
title: BBA_combination-2.tif

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DOI: 10.22008/fk2/sd56cb/07vnxi
title: SCDA_final-2.tif

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DOI: 10.22008/fk2/sd56cb/3pwly6
title: r_TOA_06-2.tif

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DOI: 10.22008/fk2/sd56cb/gboydc
title: r_TOA_17-2.tif

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title: r_TOA_21-2.tif

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DOI: 10.22008/fk2/sd56cb/xcaw88
title: SCDA_v20-2.tif

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title: r_TOA_17-2.tif

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DOI: 10.22008/fk2/sd56cb/huudxk
title: r_TOA_01-2.tif

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title: albedo_bb_planar_sw-2.tif

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DOI: 10.22008/fk2/sd56cb/pwom8j
title: r_TOA_06-2.tif

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DOI: 10.22008/fk2/sd56cb/rxxlnt
title: snow_specific_surface_area-2.tif

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DOI: 10.22008/fk2/sd56cb/yulz8m
title: BBA_combination-2.tif

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title: albedo_bb_planar_sw-2.tif

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DOI: 10.22008/fk2/sd56cb/fcv2if
title: SCDA_v20-2.tif

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DOI: 10.22008/fk2/sd56cb/rgafod
title: SCDA_final-2.tif

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DOI: 10.22008/fk2/sd56cb/uwbhl2
title: r_TOA_21-2.tif

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DOI: 10.22008/fk2/sd56cb/zn7gar
title: snow_specific_surface_area-2.tif

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title: r_TOA_06-2.tif

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title: r_TOA_01-2.tif

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DOI: 10.22008/fk2/sd56cb/mqsmmu
title: BBA_combination-2.tif

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title: r_TOA_17-2.tif

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DOI: 10.22008/fk2/sd56cb/vbphaj
title: r_TOA_21-2.tif

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title: albedo_bb_planar_sw-2.tif

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DOI: 10.22008/fk2/sd56cb/esrsv5
title: albedo_bb_planar_sw-1.tif

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title: snow_specific_surface_area-2.tif

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DOI: 10.22008/fk2/sd56cb/tlawft
title: SCDA_v20-2.tif

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DOI: 10.22008/fk2/sd56cb/zu4bgk
title: SCDA_final-2.tif

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title: r_TOA_06-2.tif

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title: BBA_combination-1.tif

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title: r_TOA_01-1.tif

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title: r_TOA_06-1.tif

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title: BBA_combination-2.tif

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title: SCDA_final-1.tif

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title: r_TOA_17-2.tif

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title: r_TOA_17-1.tif

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title: r_TOA_21-2.tif

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title: r_TOA_21-1.tif

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title: SCDA_final-1.tif

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title: SCDA_v20-1.tif

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title: SCDA_v20-1.tif

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DOI: 10.22008/fk2/sd56cb/vtp2vj
title: snow_specific_surface_area-1.tif

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DOI: 10.22008/fk2/sd56cb/w1ccnm
title: snow_specific_surface_area-2.tif

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DOI: 10.22008/fk2/sd56cb/hohvwl
title: albedo_bb_planar_sw-3.tif

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DOI: 10.22008/fk2/sd56cb/ig1ms6
title: r_TOA_06-3.tif

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title: r_TOA_01-1.tif

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DOI: 10.22008/fk2/sd56cb/ktavuu
title: BBA_combination-3.tif

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title: r_TOA_17-3.tif

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title: BBA_combination-1.tif

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title: albedo_bb_planar_sw-1.tif

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DOI: 10.22008/fk2/sd56cb/a9wlil
title: r_TOA_01-1.tif

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DOI: 10.22008/fk2/sd56cb/pkvoym
title: r_TOA_21-3.tif

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DOI: 10.22008/fk2/sd56cb/ws5xfw
title: snow_specific_surface_area-3.tif

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DOI: 10.22008/fk2/sd56cb/j6bbhi
title: SCDA_v20-1.tif

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DOI: 10.22008/fk2/sd56cb/keqxou
title: r_TOA_06-1.tif

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DOI: 10.22008/fk2/sd56cb/m74zo7
title: SCDA_final-1.tif

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DOI: 10.22008/fk2/sd56cb/pjnxf7
title: r_TOA_21-1.tif

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DOI: 10.22008/fk2/sd56cb/xc2aza
title: r_TOA_17-1.tif

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DOI: 10.22008/fk2/sd56cb/5osuc2
title: albedo_bb_planar_sw-1.tif

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DOI: 10.22008/fk2/sd56cb/hx3v1o
title: BBA_combination-1.tif

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title: albedo_bb_planar_sw-1.tif

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DOI: 10.22008/fk2/sd56cb/p3xo82
title: BBA_combination-1.tif

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DOI: 10.22008/fk2/sd56cb/pmisqk
title: snow_specific_surface_area-1.tif

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DOI: 10.22008/fk2/sd56cb/56huob
title: r_TOA_06-1.tif

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