cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.52610
title: (Table 4) Sediment composition, d15N, and Th-normalized paleoflux and ex. 231Pa 0/ex. 230Th 0 activity ratio in core MD84-527

description: AGE (ka) is based on accelerator mass spectrometry 14C dates (Labracherie et al., 1989) dataset: doi:10.1594/PANGAEA.358352. Paleofluxes and ex. 231Pa 0/ex. 230Th 0 activity ratios computed with the assumption that authigenic U was added to these sediment sections at 14 ka B.P.
DOI: 10.1594/pangaea.52431
title: (Table A5) Opal content and stable oxygen isotope ratios of foramninifera from sediment core RC15-93
DOI: 10.1594/pangaea.198771
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1077B
DOI: 10.1594/pangaea.726525
title: (Table A1) Major element and biogenic silica concentrations in ODP Hole 127-797A sediments
DOI: 10.1594/pangaea.361510
title: (Table 2) Silica analysis on Holocene surface sediment samples
DOI: 10.1594/pangaea.117006
title: Pore water composition of sediment core TN047-4G-MC
DOI: 10.1594/pangaea.116997
title: Pore water composition of sediment core TN041-5E-MC
DOI: 10.1594/pangaea.117003
title: Pore water composition of sediment core TN041-16B-MC
DOI: 10.1594/pangaea.93468
title: Particle fluxes of SO51_CBBT-87/88_trap
DOI: 10.1594/pangaea.93483
title: Particle fluxes of AB5_trap
DOI: 10.1594/pangaea.52394
title: Geochemistry of surface sediments from the Indian Ocean
DOI: 10.1594/pangaea.52430
title: (Table A4) CaCO3, opal, and stable oxygen isotope ratios of Neogloboquadrina pachyderma from sediment core RC13-254
DOI: 10.1594/pangaea.845896
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core Y71-09-101

description: Stable isotopes by Mix for this paper and Pisias and Mix (1997)
DOI: 10.1594/pangaea.198776
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1082A
DOI: 10.1594/pangaea.52437
title: (Table A12) Opal content of sediment core ELT49.023-PC
DOI: 10.1594/pangaea.52369
title: (Table 4) Ge/Si ratio, Si, opal, and age model of Site ELT17.009-PC
DOI: 10.1594/pangaea.52463
title: (Table A1) CaCO3 and opal content of sediment core RC11-120
DOI: 10.1594/pangaea.198772
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1078A
DOI: 10.15468/dl.gzb7fn
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
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 "Geometry POLYGON((170 20, 170 50, 120 50, 120 20, 170 20))",
 "HasCoordinate is true"
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 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000877-250127130748423/datasets/export for details.
DOI: 10.1594/pangaea.198773
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1079B
DOI: 10.1594/pangaea.198775
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1081A
DOI: 10.1594/pangaea.52434
title: (Table A8) Opal content of sediment core ELT45.029-TC
DOI: 10.1594/pangaea.52609
title: (Table 2) Bulk sedimentology and stable isotopes on ODP Hole 114-704A
DOI: 10.1594/pangaea.93482
title: Particle fluxes of AB3_trap
DOI: 10.1594/pangaea.52432
title: (Table A6) Opal content and stable oxygen isotope ratios of foraminifera from sediment core RC15-94
DOI: 10.1594/pangaea.845865
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core W8402A-14
DOI: 10.1594/pangaea.116999
title: Pore water composition of sediment core TN047-13B-MC
DOI: 10.1594/pangaea.753094
title: (Table 1) Calcium carbonate and Si-opal concentrations of samples from ODP Site 111-677
DOI: 10.1594/pangaea.845893
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core Y69-106P

description: Opal and quartz by X-ray diffraction, from Pisias MSc. thesis, 1974. benthic and planktic stable isotopes by Mix for this paper and Pisias and Mix (1997)
DOI: 10.1594/pangaea.117005
title: Pore water composition of sediment core TN041-17A-MC
DOI: 10.1594/pangaea.93466
title: Particle fluxes of SO51_SBBT-87/88_trap
DOI: 10.1594/pangaea.93472
title: Particle fluxes of NBBTs-89/90_trap
DOI: 10.1594/pangaea.93481
title: Particle fluxes of AB4_trap
DOI: 10.1594/pangaea.52429
title: (Table A3) Opal content and stable oxygen isotope ratios of Neogloboquadrina pachyderma from sediment core RC13-271
DOI: 10.1594/pangaea.845894
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core Y71-3-2

description: Planktic stable isotopes by Mix for this paper and Pisias and Mix (1997)
DOI: 10.1594/pangaea.92437
title: Particle fluxes of SBB_trap
DOI: 10.1594/pangaea.93485
title: Particle fluxes of AB1_trap
DOI: 10.1594/pangaea.93635
title: Particle fluxes of NBP96-4A_MS1_trap
DOI: 10.1594/pangaea.746235
title: (Table 4) Carbonate, opal, terrigenous fraction, and dry bulk density of ODP Hole 108-662A
DOI: 10.1594/pangaea.794530
title: (Table 1) Biogenic and terrigenous components and ages of ODP Hole 167-1020B sediments

description: The California Current and associated coastal upwelling have changed with the growth and decay of the North American ice sheets since 2.5 Ma. Because the coastal upwelling has a close relationship with biogenic productivity in surface water, analyses of biogenic components in sediments of the upwelling region enable us to reconstruct the past changes of the productivity and/or the current systems.In this study, we analyzed biogenic silica and carbonate as well as organic carbon in sediments from the northern California margin, Hole 1020B. The results show that terrigenous-free content of biogenic silica is high during interglacial periods since 800 ka and varies in correspondence with 100-k.y. glacial-interglacial cycles. On the other hand, terrigenous-free content of biogenic carbonate is high during glacial periods. These temporal variations may have been caused by changes in the origin of deep water.
description: DEPTH, sediment is given in mbsf.
description: Supplement to: Kuroda, Tomoko; Sakamoto, Tatsuhiko; Koizumi, Itaru (2000): Data Report: Temporal variations of biogenic components on the northern California margin since the late Pleistocene, Site 1020. In: Lyle, M; Koizumi, I; Richter, C; Moore, TC Jr (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 167, 1-4
DOI: 10.1594/pangaea.753820
title: (Table 2) Sediment chemistry at ODP Hole 112-682A
DOI: 10.1594/pangaea.753822
title: (Table 3) Sediment chemistry at ODP Hole 112-685A
DOI: 10.1594/pangaea.93467
title: Particle fluxes of SBBT-90/91_trap
DOI: 10.1594/pangaea.93473
title: Particle fluxes of NBBTs-90/91_trap
DOI: 10.1594/pangaea.744047
title: (Table 1) TOC, carbonate and opal concentrations from ODP Holes 175-1082A and 175-1084A

description: Depth = mcd
DOI: 10.1594/pangaea.93474
title: Particle fluxes of SO51_NBBTn-87/88_trap
DOI: 10.1594/pangaea.198777
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1084A
DOI: 10.1594/pangaea.93500
title: Particle fluxes of SCS-C_trap
DOI: 10.1594/pangaea.93501
title: Particle fluxes of SCS-N_trap
DOI: 10.1594/pangaea.52436
title: (Table A10) Opal content of sediment core ELT49.018-PC
DOI: 10.1594/pangaea.746236
title: (Table 5) Carbonate, opal, terrigenous fraction, and dry bulk density of ODP Hole 108-663A
DOI: 10.1594/pangaea.198770
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1076A
DOI: 10.1594/pangaea.726134
title: (Table 5) Geochemistry from DSDP Hole 71-514
DOI: 10.1594/pangaea.198774
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1080A
DOI: 10.1594/pangaea.726528
title: (Table A1) Major element and biogenic silica concentrations in ODP Hole 127-797B sediments
DOI: 10.1594/pangaea.845859
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core V19-27

description: aCO3, C-org, opal by Lyle for this paper.
DOI: 10.1594/pangaea.93470
title: Particle fluxes of CBBT-90_trap
DOI: 10.1594/pangaea.52433
title: (Table A7) CaCO3, opal, and stable isotope ratios of Cibicides spp. from sediment core V22-108

description: The ages have been derived through oxygen isotope stratigraphy with various supplemental control points from 14C and biostratigraphy and are given as calculated ages.
DOI: 10.1594/pangaea.93471
title: Particle fluxes of CBBT-91_trap
DOI: 10.1594/pangaea.52435
title: (Table A9) Opal content of sediment core ELT49.017-PC
DOI: 10.1594/pangaea.117001
title: Pore water composition of sediment core TN047-3H-MC
DOI: 10.1594/pangaea.117004
title: Pore water composition of sediment core TN041-11F-MC
DOI: 10.1594/pangaea.693923
title: Sedimentology and accumulation rates of ODP Site 184-1143 in the South China Sea (Appendix B)

description: 128 samples from Ocean Drilling Program (ODP) Site 1143 in the southern South China Sea were analyzed for grain size, clay minerals, biogenic opal content and quartz in order to reconstruct changes in East Asian monsoon climate since 8.5 Ma. An abrupt change of terrigenous mass accumulation rate (MAR), clay mineral assemblage, median grain size and biogenic opal MAR about 5.2 Ma suggests that between 8.5-5.2 Ma the source of terrigenous sediment was mainly in the region of surface uplift and basaltic volcanism in southern Vietnam. A simple model of East Asian summer monsoon evolution was based on the clay/feldspar ratio, kaolinite/chlorite ratio and biogenic opal MAR. The summer monsoon has two periods of maximum strength at 8.5-7.6 Ma and 7.1-6.2 Ma. Subsequently, there was a relatively stable period at 6.2-3.5 Ma, continued intensification about 3.5-2.5 Ma, and gradually weakening after 2.5 Ma. Since 1 Ma the monsoon has intensified, with remarkable high-frequency and amplitude variability. Simultaneous increase in sedimentation rates at ODP Sites 1143, 1146 and 1148, as well as in MAR of terrigenous materials, quartz, feldspar and clay minerals at ODP Site 1143 at 3.5-2.5 Ma, may be the erosional response to both global climatic deterioration and the strengthening of the East Asian summer monsoon after about 3-4 Ma.
description: Age model after Tian et al. 2002, doi:10.1016/S0012-821X(02)00923-8 and Li et al. 2004, doi:10.1029/2003PA000906
description: Supplement to: Wan, Shiming; Li, Anchun; Clift, Peter D; Jiang, Hengyi (2006): Development of the East Asian summer monsoon: Evidence from the sediment record in the South China Sea since 8.5 Ma. Palaeogeography, Palaeoclimatology, Palaeoecology, 241(1), 139-159
DOI: 10.1594/pangaea.115857
title: Stable isotope analysis on sediment core GIK17957-2
DOI: 10.1594/pangaea.845860
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core V19-28

description: CaCO3, C-org, opal from Lyle et al. (1988)
DOI: 10.1594/pangaea.845890
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core Y69-71P

description: Benthic and planktic stable isotopes by Mix for this paper, and Shackleton (unpublished) for isotope stage 5.
DOI: 10.1594/pangaea.204350
title: (Table T1) Biogenic opal concentrations, ODP Hole 177-1093A
DOI: 10.1594/pangaea.204353
title: (Table T1) Biogenic opal concentrations, ODP Hole 177-1094A
DOI: 10.1594/pangaea.204352
title: (Table T1) Biogenic opal concentrations, ODP Hole 177-1093C
DOI: 10.1594/pangaea.204354
title: (Table T1) Biogenic opal concentrations, ODP Hole 177-1094B
DOI: 10.1594/pangaea.845571
title: Calcium carbonate and organic carbon content, and stable isotope composition of sediment core INDM-1-14P

description: CaCO3, C-org, opal analyses are by Lyle for this paper.
DOI: 10.1594/pangaea.93475
title: Particle fluxes of NBBTn-88/89_trap
DOI: 10.1594/pangaea.778022
title: (Table T1) Carbonate and opal composition of ODP Hole 198-1208A sediments, Shatsky Rise

description: Weight percent opal and carbonate data are presented for the Miocene-Lower Pliocene interval at Site 1208 on Shatsky Rise. These data compare favorably with shipboard estimates and measurements. The opal and carbonate data confirm that the color cycles recognized in shipboard data are the result of fluctuations in carbonate content and are not related to opal productivity.
description: Supplement to: Robinson, Stuart A; Jenkyns, Hugh C (2005): Data report: Opal and carbonate data from the Miocene to Lower Pliocene, Site 1208 (Central High, Shatsky Rise). In: Bralower, TJ; Premoli Silva, I; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 198, 1-7
DOI: 10.1594/pangaea.93484
title: Particle fluxes of AB2_trap
DOI: 10.1594/pangaea.786366
title: (Table T2) Biogenic opal content of ODP Site 181-1124 sediments

description: DEPTH, sediment is given in mbsf.
DOI: 10.1594/pangaea.796220
title: (Table 1) Biogenic opal concentrations for a latitudinal transect of seven ODP Leg 167 sites along the California margin

description: Ocean Drilling Program Leg 167 drilled thirteen sites in a series of depth and latitudinal transects along the climatically sensitive California margin to reconstruct the Neogene history of deep-, intermediate-, and surface-ocean circulation changes (Lyle, Koizumi, Richter, et al., 1997, doi:10.2973/odp.proc.ir.167.1997). Significant variations occurred in sediment properties on all time scales as seen in the high-resolution nondestructive shipboard measurements (e.g., bulk density and color reflectance), high- to intermediate-resolution downhole log measurements (e.g., resistivity and magnetic susceptibility), and lower resolution discrete shipboard measurements (e.g., physical properties and carbon geochemistry). Thus, these Leg 167 sites provide an opportunity to address paleoceanographic questions about the evolution of the California Current and links between the equatorial Pacific and the high-latitude North Pacific from millennial and orbital to tectonic time scales. This data report presents the results of biogenic opal analyses from a latitudinal transect of seven sites along the California margin for the time interval from 8 Ma to the present. Site selection for opal analyses was based upon such parameters as opal content, stratigraphic continuity, and lack of coring disturbance.
description: DEPTH, sediment is given in mbsf.
description: Supplement to: Janecek, Thomas R (2000): Data Report: Late Neogene biogenic opal data for Leg 167 sites on the California margin. In: Lyle, M; Koizumi, I; Richter, C; Moore, TC Jr (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 167, 1-2
DOI: 10.1594/pangaea.198769
title: (Table T1) Calcium carbonate, total organic carbon, and biogenic opal concentrations and δ¹³Corg values for sediment samples, ODP Hole 175-1075A
DOI: 10.1594/pangaea.726132
title: (Table 5) Geochemistry from DSDP Hole 29-278
DOI: 10.1594/pangaea.786365
title: (Table T1) Biogenic opal content of ODP Site 181-1123 sediments

description: DEPTH, sediment is given in mcd.
DOI: 10.1594/pangaea.832061
title: (Table TS14) Carbonate and opal content of sediment core V34-153
DOI: 10.1594/pangaea.117000
title: Pore water composition of sediment core TN047-1E-MC
DOI: 10.1594/pangaea.116996
title: Pore water composition of sediment core TN041-4F-MC
DOI: 10.1594/pangaea.712442
title: (Table A11) Opal content and stable oxygen isotope ratios of Cibicides spp. from sediment core ELT49.019-PC
DOI: 10.1594/pangaea.683654
title: Stable oxygen isotope ratios, calcium carbonate and opal content in late Pliocene sediments of DSDP Hole 75-532 in the Southeast Atlantic (Table 1)

description: Site 532 on the Walvis Ridge was sampled at 4000- to 800-year intervals from 2.24 to 2.60 Ma, spanning the three large glacial advances of the late Pliocene. An age model was created by correlating the oxygen isotope record to Site 607 with linear interpolations between tie-lines. The resultant age model differs from that in the site reports by more than 800,000 years, due to misidentification of a magnetic boundary. Sedimentation rates varied by an order of magnitude at this site, with minimum accumulation during glacial events. Interglacial intervals were charactrized by high marine production and high summer precipitation on land, while glacials had very low production and arid continental climate. During the large glacial events (Stages 96-100) conditions of low production and continental aridity reached their greatest intensity, but there is no evidence of a permanent mode shift in either marine or terrestrial records. Calcite concentration has a strong variation at obliquity frequencies, with maxima during interglacials, but occasionally shows a large amplitude at precessional frequencies as well, so that high concentrations occur in a few glacial intervals. As a result, color variation is not a reliable guide to glacial-scale cycles at this site. Composition of the phytoplankton assemblage is diverse and highly variable, and we have not been able to distinguish a clear indicator of upwelling-related production. Spectral analysis reveals obliquity and precessional signals in the pollen data, while several diatom records contain combination tones, indicating that these data represent a complicated response to both local and high-latitude forcing.
description: Age model relies upon matching the isotope record to that at DSDP Site 94-607 in the North Atlantic (Raymo et al., 1989)
description: Supplement to: Sancetta, Constance A; Heusser, Linda E; Hall, Michael A (1992): Late Pliocene climate in the Southeast Atlantic: Preliminary results from a multi-disciplinary study of DSDP Site 532. Marine Micropaleontology, 20(1), 59-75
DOI: 10.1594/pangaea.116995
title: Pore water composition of sediment core TN041-29H-MC
DOI: 10.1594/pangaea.116998
title: Pore water composition of sediment core TN047-11A-MC
DOI: 10.1594/pangaea.117002
title: Pore water composition of sediment core TN047-7B-MC
DOI: 10.1594/pangaea.786367
title: (Table T3) Biogenic opal content of ODP Site 181-1125 sediments

description: DEPTH, sediment is given in mbsf.
DOI: 10.1594/pangaea.773654
title: (Appendix A) Radiolarian abundances in ODP Hole 175-1084A

description: The changing composition of radiolarian faunas from late Neogene deep-sea sediments has been used in recent years as a proxy for changes in marine paleoproductivity. We examine radiolarian faunas, organic carbon content (TOC), opal and coarse-fraction components over the last 270,000 years in sediments from ODP Hole 1084A, drilled in a high productivity upwelling region within the Benguela Upwelling System off the west coast of Africa. Age control is provided by stable oxygen isotope measurements of benthic foraminifera. Prior research has established that late Pleistocene glacial intervals in this upwelling system generally had higher productivity than interglacials. The radiolarian WADE (water-depth ecology) paleoproductivity index correlates well with TOC and opal in these samples, and all three parameters change in synchrony with the benthic isotope curve over all but the MIS 5e–6 time interval. WADE inferred productivity is significantly higher in glacials than interglacials. We conclude that the WADE index is a useful proxy for paleoproductivity at this location, as are also opal and organic carbon accumulation rates. Carbonate and carbonate based indices such as the accumulation rate of benthic foraminifera (BFAR) by contrast do not correlate well either to productivity indices or to the glacial–interglacial cycle, and are interpreted to primarily reflect carbonate dissolution.
description: Supplement to: Lazarus, David B; Bittniok, Beatrice; Diester-Haass, Lieselotte; Billups, Katharina; Ogawa, Yujiro; Takahashi, Kozo; Meyers, Philip A (2008): Radiolarian and sedimentologic paleoproductivity proxies in late Pleistocene sediments of the Benguela Upwelling System, ODP Site 1084. Marine Micropaleontology, 68(3-4), 223-235
DOI: 10.1594/pangaea.746237
title: (Table 6) Carbonate, opal, terrigenous fraction, and dry bulk density of ODP Hole 108-664B
DOI: 10.1594/pangaea.746238
title: (Table 7) Carbonate, opal, terrigenous fraction, and dry bulk density of ODP Hole 108-664D
DOI: 10.15468/dl.a8cz8v
title: Occurrence Download

description: A dataset containing 428 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Sebastes inermis Cuvier, 1829",
 "Geometry POLYGON((170 20, 170 50, 120 50, 120 20, 170 20))",
 "HasCoordinate is true"
 ]
}

 The dataset includes 428 records from 23 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000879-250127130748423/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.92861
title: Particle Flux of EAST-86/90_trap
DOI: 10.1594/pangaea.92863
title: Particle Flux of KL71_trap
DOI: 10.1594/pangaea.52396
title: Geochemistry of core SO42-74KL
DOI: 10.1594/pangaea.754799
title: (Appendix) Carbonate, opal and other sediment components of ODP Site 114-704A
DOI: 10.1594/pangaea.92747
title: Particle fluxes of L2-B-92_trap
DOI: 10.1594/pangaea.92859
title: Particle Flux of CENTRAL_trap
DOI: 10.1594/pangaea.92862
title: Particle Flux of KL26_trap
DOI: 10.25903/w2f4-bx25
title: Data: Who gets the ventilator? A survey of Australian intensivists’ opinions and experiences of triage during the COVID-19 pandemic

description: <p><b>Background:</b> Global responses to the COVID-19 pandemic in the critical care setting were varied and inconsistent, exposing flaws in health systems as immense pressure was put on intensivists when disaster triage was enacted. This study explored experiences and opinions of Australian intensivists working during Coronavirus disease 2019 (COVID-19) regarding triage in disaster scenarios and views on the availability and role of guidelines to support triage decision-making.</p>

<p><b>Methods: </b> An online questionnaire, adapted from a European study, was distributed to Australian intensivists in 2023. Participants were College of Intensive Care Medicine of Australia and New Zealand (CICM) trainees and consultants working in Australian hospitals during the COVID-19 pandemic. We examined the respondents’ preferred grounds and considerations of Intensive Care Unit (ICU) triage in five case scenarios. Respondents were given various options exploring ventilator allocation decisions, consulting others and extreme expansion of ICU capacity. Preferences were examined using a 5-point Likert scale and open-ended questions with free-text responses. We performed group comparisons based on age, gender, seniority and explored alignment of decisions with ethical frameworks. Secondary outcomes included explorations of moral distress and opinions on guidelines.</p>

<p><b>This data record contains:</b></p>
<p>1 MS Excel (.xslx) file (also saved in Open Document Format) containing all 32 survey responses to questions as exported from Qualtrics, with related unique consultant (C) and trainee (T) codes as referred to in the main text for this paper. This data was analysed in SPSS, with Likert data for Questions 12-16 presented using the R studio package Likert. Some demographic fields are redacted to reduce risk of identifying respondents. </p>
DOI: 10.1594/pangaea.92748
title: Particle fluxes of OMEX3_trap
DOI: 10.1594/pangaea.92860
title: Particle Flux of KL15_trap
DOI: 10.1594/pangaea.92745
title: Particle Flux of SEEP-10_trap
DOI: 10.1594/pangaea.92749
title: Particle fluxes of OMEX2_trap
DOI: 10.1594/pangaea.92746
title: Particle fluxes of SEEP-7_trap