cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.tj328j
title: Occurrence Download

description: A dataset containing 117 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "POLYGON ((147.354401 -33.802053, 147.354401 -33.815527, 147.356646 -33.815527, 147.356646 -33.80879, 147.361138 -33.80879, 147.361138 -33.806544, 147.356646 -33.806544, 147.356646 -33.802053, 147.354401 -33.802053))"
 ]
}

 The dataset includes 117 records from 2 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069713-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.6084/m9.figshare.26724692.v1
title: Additional file 1 of Characterization and screening of cotton (Gossypium hirsutum L.) germplasm for leafhopper (Amrasca biguttula biguttula (Ishida)) resistance

description: Additional file 1: Table S1. Biochemical parameters and hopper injury status of the different genotypes.  Table S2. Multiple comparisons within resistant grades.
DOI: 10.1594/pangaea.112003
title: Basic hydrographic, nutrient and carbon/nitrogen chemistries at station AT_II-119/5_38-11
DOI: 10.1594/pangaea.111970
title: Basic hydrographic, nutrient and carbon/nitrogen chemistries at station AT_II-119/5_30-10
DOI: 10.1594/pangaea.55892
title: Stable isotopes measured on Globigerina bulloides of sediment core PS2498-1
DOI: 10.1594/pangaea.115069
title: (Table 3) Barium barite and excess comparison, accumulation rates and productivity from surface sediments

description: Since Dymond et al. (1992, doi:10.1029/92PA00181) proposed the paleoproductivity algorithm based on “Bio-Ba”, which relies on a strong correlation between Ba and organic carbon fluxes in sediment traps, this proxy has been applied in many paleoproductivity studies. Barite, the main carrier of particulate barium in the water column and the phase associated with carbon export, has also been suggested as a reliable paleoproductivity proxy in some locations. We demonstrate that Ba(excess) (total barium minus the fraction associated with terrigenous material) frequently overestimates Ba(barite) (barium associated with the mineral barite), most likely due to the inclusion of barium from phases other than barite and terrigenous silicates (e.g., carbonate, organic matter, opal, Fe-Mn oxides, and hydroxides). A comparison between overlying oceanic carbon export and carbon export derived from Ba(excess) shows that the Dymond et al. (1992) algorithm frequently underestimates carbon export but is still a useful carbon export indicator if all caveats are considered before the algorithm is applied. Ba(barite) accumulation rates from a wide range of core top sediments from different oceanic settings are highly correlated to surface ocean 14C and Chlorophyll a measurements of primary production. This relationship varies by ocean basin, but with the application of the appropriate f ratio to 14C and Chlorophyll a primary production estimates, the plot of Ba(barite) accumulation and carbon export for the equatorial Pacific, Atlantic, and Southern Ocean converges to a global relationship that can be used to reconstruct paleo carbon export.
description: This data set gives table 3 as reported in the Erratum. Ba total and Al total analyses of TT013 samples from Schroeder et al. (1997) and Murray et al. (2000), PS samples from Nürnberg et al. (1995).
description: Supplement to: Eagle, Meagan; Paytan, Adina; Arrigo, Kevin R; van Dijken, Gert L; Murray, Richard W (2003): A comparison between excess barium and barite as indicators of carbon export. Paleoceanography, 18(1), 1021
DOI: 10.1594/pangaea.665608
title: Oceanography at CTD/bottle station IFREMER_2448
DOI: 10.1594/pangaea.87279
title: Susceptibility raw data of sediment core PS2493-1

description: data given in 10**-5 SI units
DOI: 10.1594/pangaea.98665
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2492-2
DOI: 10.1594/pangaea.54949
title: Quartz and opal of sediment core PS2499-5
DOI: 10.6084/m9.figshare.26762809
title: DUSP22-FASN

description: Induction of fatty acid synthase (FASN) occurs in obesity and obesity-related diseases. Dual-specificity phosphatase 22 (DUSP22) is a negative regulator of cancer progression and inflammatory diseases; however, the <i>in vivo</i> role of DUSP22 in metabolic syndrome remains unclear. We found that Dusp22 KO mice spontaneously developed obesity and displayed high FASN levels in insulin-responsive tissues. Mechanistically, DUSP22 dephosphorylated FASN protein at three residues, resulting in degradation of FASN and subsequent suppression of adipogenesis.
DOI: 10.1594/pangaea.115350
title: Documentation of sediment core PS2499-5
DOI: 10.1594/pangaea.57908
title: (Table 2) Radionuclides in terrigenous sand-, silt- and clay-sized fraction

description: Sr and Nd isotopic data for the terrigenous sand-, silt-, and clay-size fractions of sediments from the S Atlantic and SE Pacific, and adjacent continental regions
DOI: 10.1594/pangaea.55890
title: Isotopes (N. pachyderma, dextral) of sediment core PS2495-3
DOI: 10.1594/pangaea.87282
title: Susceptibility raw data of sediment core PS2498-1

description: data given in 10**-5 SI units
DOI: 10.1594/pangaea.65923
title: (Table 2a) Age, TOC, primary production, and isotopes (Cibicidoides spp.) of sediment core PS2495-3
DOI: 10.1594/pangaea.399829
title: Characteristics of benthic foraminifera assemblage in sediment core PS2498-2
DOI: 10.1594/pangaea.399830
title: Characteristics of benthic foraminifera assemblage in sediment core PS2499-1
DOI: 10.1594/pangaea.399836
title: Q-mode varimax factor loadings matrix of benthic foraminifera assemblage of sediment core PS2499-1
DOI: 10.1594/pangaea.77191
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2496-3
DOI: 10.1594/pangaea.55887
title: Distribution of planktic foraminifera, factor analysis, SST of sediment core PS2498-1
DOI: 10.1594/pangaea.820709
title: Documentation of sediment core PS2493-3
DOI: 10.1594/pangaea.847191
title: Documentation of sediment core PS2499-1
DOI: 10.1594/pangaea.323422
title: Water temperature and salinity CTD profiles from cruise 18TL96008 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.782732
title: (S2, Fig. 4) Biometric measurements of Fragilariopsis kerguelensis on sediment core PS2498-1
DOI: 10.1594/pangaea.323411
title: Water temperature and salinity CTD profiles from cruise 18OK96008 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.124468
title: Documentation of sediment core PS2500-2
DOI: 10.1594/pangaea.320671
title: Water temperature real-time profiles from cruise FNQD91 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.322126
title: Water temperature real-time profiles from cruise 4154098 (DCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.378378
title: Radiosonde PS14/04435 during POLARSTERN cruise ANT-VII/1 on 1988-09-29 03:27h

description: Height of tropopause 16228 m, precipitable water content 3.9852 cm
DOI: 10.1594/pangaea.376713
title: Radiosonde PS18/06198 during POLARSTERN cruise ANT-IX/1 on 1990-10-28 14:13h

description: Height of tropopause 16396 m, precipitable water content 2.7871 cm
DOI: 10.1594/pangaea.377543
title: Radiosonde PS16/04361 during POLARSTERN cruise ANT-VIII/1 on 1989-08-21 00:22h

description: Precipitable water content 4.3233 cm
DOI: 10.1594/pangaea.221045
title: Mineral composition of the less than 2 µm fraction from Hole 66-493
DOI: 10.1594/pangaea.779345
title: (Table T2) Stable carbon and oxygen isotopes of DSDP Leg 30, Leg 33, ODP Leg 130 and Leg 192 sites, Ontong Java Plateau

description: Stable isotopic analyses of bulk carbonates recovered from Ontong Java Plateau during Ocean Drilling Program (ODP) Leg 192 (Holes 1183A and 1186A) show an ~0.5 per mil increase in d18O values from the upper Campanian/lower Maastrichtian to the upper Maastrichtian. This shift is consistent with widespread evidence for cooling at this time. Similar shifts were found at other localities on Ontong Java Plateau (Deep Sea Drilling Project [DSDP] Sites 288 and 289 and ODP Site 807) and at DSDP Site 317 on Manihiki Plateau. These data extend evidence for Maastrichtian cooling into the southwestern tropical and subtropical Pacific. The record of apparent cooling survives despite a significant diagenetic overprint at all sites. Comparing average Maastrichtian d18O values among sites suggests that diagenesis caused d18O to first be shifted toward higher values and then back toward lower values as burial depth increased. Carbon isotopes at the six sites show no apparent primary shifts, but at four sites, the Cretaceous/Tertiary boundary interval coincides with a negative excursion attributed to alteration of sediments near the boundary.
description: Sediment depth is given in mbsf. External precision is &lt;0.03 per mil for d13C and &lt;0.05 per mil for d18O (1 sigma). For nannofossil datums and depths of holes 30-288A and 30-289 see Andrews, Packham, et al. (1975, doi:10.2973/dsdp.proc.30.1975), for Hole 33-317A see Schlanger, Jackson, et al. (1976, doi:10.2973/dsdp.proc.33.1976), for Hole 130-807C see Mao and Wise (1993, doi:10.2973/odp.proc.sr.130.054.1993), and for holes 192-1183A and 192-1186A see Bergen (2004, doi:10.1144/GSL.SP.2004.229.01.08).
DOI: 10.1594/pangaea.377116
title: Radiosonde PS20/07557 during POLARSTERN cruise ANT-X/1a on 1991-11-18 06:02h

description: Height of tropopause 12748 m, precipitable water content 2.0418 cm
DOI: 10.1594/pangaea.378125
title: Radiosonde PS20/07559 during POLARSTERN cruise ANT-X/1a on 1991-11-18 14:48h

description: Height of tropopause 15131 m, precipitable water content 1.8996 cm
DOI: 10.1594/pangaea.262029
title: Major-element chemical analyses of Hole 37-335
DOI: 10.1594/pangaea.707324
title: (Table 1) Element concentrations in the carbonate fraction of DSDP Hole 92-598 sediments

description: Data on the bulk salt-free basis of sediments. The carbonate fraction was leached by 4 hours treatment by 10% acetic acid. Then chemical composition of the leachate was studied.
DOI: 10.1594/pangaea.734246
title: (Table 1) Mineralogy, geochemistry and isotopic ratios of peridotites from ODP Hole 209-1268A

description: For d18O of whole rock see Alt et al. (2007) dataset: doi:10.1594/PANGAEA.734291
DOI: 10.1594/pangaea.792830
title: (Table 7) Representative chemical composition of plagioclase crystals at DSDP Holes 89-586 and 90-587
DOI: 10.1594/pangaea.920529
title: Continuous water level observations at station BEFmate_S10pio (2019-05)
DOI: 10.1594/pangaea.745382
title: (Table 3) Chemistry of potassium-rich basalts from ODP Hole 106-648B

description: Analysis number 393, SAMF &lt; 12.1; 342-32, SAMF 12.1-12.3; 335-7, SAMF 12.3-12.5; 193-134, SAMF 12.5-12.7; 92-152, SAMF 12.7-12.9; 111-159, SAMF 12.9-13.1. Analyses are listed in depth order within each SAMF division.
DOI: 10.1594/pangaea.783666
title: (Table 3a) Geochemistry of olivine of ODP Holes 207-1272A and 207-1274A

description: Sediment depth is given in mbsf. Normalized to four oxygens.
DOI: 10.1594/pangaea.663763
title: Oceanography at CTD/bottle station IFREMER_0603
DOI: 10.1594/pangaea.665450
title: Oceanography at CTD/bottle station IFREMER_2290
DOI: 10.1594/pangaea.888721
title: The deep scattering layer micronektonic fish faunas of the Atlantic mesopelagic ecoregions

description: Three hundred and twenty-nine species of micronektonic fishes were identified in 1040 midwater trawl collections taken between 1963 and 1974 from the North and South Atlantic, the Mediterranean, the Caribbean and the Gulf of Mexico. The target of most tows was the deep scattering layer, and consequently the dominant species in the material were those that were concentrated in the layer. The results only generally confirm the 11 Atlantic mesopelagic ecoregions previously recognized. The geometric mean of the proportion of joint occurrences (GMPJO) of species with tows within each ecoregion was used to characterize the faunas of the ecoregions. The ecoregion affinities of fishes were compared to those of decapod shrimp in the same collections. The fish and shrimp faunas of ecoregions could be distinguished by GMPJO values, but the ranges of species favoring each ecoregion varied widely in extent and did not conform well to ecoregion boundaries or features of circulation. This suggests that co-occurring species respond differently to the physical properties and resulting biological factors defining mesopelagic ecoregions.
DOI: 10.1594/pangaea.665647
title: Oceanography at CTD/bottle station IFREMER_2487
DOI: 10.1594/pangaea.837299
title: Stable C and N isotopes and percent C as well as N composition of plankton from the North Atlantic

description: Elemental C and N percent composition and natural abundance of stable C and N isotopes of plankton species and/or size-fractions collected in several cruises on the N Atlantic Ocean from Greenland to Norway and around Iceland. Determinations included key copepod and krill species. Lipid extraction was performed in some samples to determine carbón isotope depletion factors.
DOI: 10.1594/pangaea.816961
title: Nitrogen fixation rate of different stations in 2008, 2009 and 2010
DOI: 10.1594/pangaea.815981
title: Abundance and calculated biomass of Richelia, in association with diatoms, in the central North Pacific
DOI: 10.1594/pangaea.810471
title: (Table 4) Accumulation rate of noncarbonate fraction at DSDP Leg 74 sites
DOI: 10.1594/pangaea.777771
title: (Table 1) Diatom and silicoflagellate relative abundance in ODP Hole 207-1260A
DOI: 10.1594/pangaea.402532
title: Water temperature and current velocity from surface drifter SVP_7700485
DOI: 10.1594/pangaea.50447
title: Ice rafted debris (&gt; 2 mm gravel) distribution in sediment core PS2562-6
DOI: 10.1594/pangaea.115365
title: Documentation of sediment core PS2562-6
DOI: 10.1594/pangaea.115366
title: Documentation of sediment core PS2563-2
DOI: 10.1594/pangaea.115367
title: Documentation of sediment core PS2564-3
DOI: 10.1594/pangaea.665680
title: Oceanography at CTD/bottle station IFREMER_2520
DOI: 10.1594/pangaea.476407
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_37N/27

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.745189
title: (Table 2) Mineralogy of bulk sediments of ODP Site 105-647
DOI: 10.1594/pangaea.920416
title: Continuous water level observations at station BEFmate_I4low (2019-05)
DOI: 10.1594/pangaea.743273
title: (Table 2) Elemental and isotope analyses of isolated kerogens for ODP Hole 101-635B
DOI: 10.1594/pangaea.787790
title: (Table T7) Mass accumulation rates and bulk density of ODP Hole 173-1068A
DOI: 10.1594/pangaea.788529
title: (Table 1) Organic carbon and epoch at DSDP Hole 93-605
DOI: 10.1594/pangaea.789081
title: (Table 2) Sediment description and age at DSDP Hole 93-605
DOI: 10.1594/pangaea.476366
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_26N/219

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.789587
title: (Table 3) Age and nannofossil zone at DSDP Site 92-598
DOI: 10.1594/pangaea.476375
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_26N/228

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.476388
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_AN_37N/102

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.792910
title: (Table 2) Mass accumulation rates and grain-size fractions at DSDP Site 89-586
DOI: 10.1594/pangaea.745889
title: (Table 1) Measured and reconstructed primary modes of peridotites from ODP Hole 109-670A

description: Measured modes based on 1000 point per thin section (1215 points for 109-670A-9R-1,94-97). Grid spacing = 0.5 mm. &lt;1 = traces.
DOI: 10.1594/pangaea.900317
title: Mg/Ca ratios and SST reconstruction for sediment core MV99_GC41
DOI: 10.1594/pangaea.792729
title: (Table 1) Mass accumulation rate, linear sedimentation rate, bulk denisty and age at DSDP Leg 92 holes
DOI: 10.1594/pangaea.858000
title: (Table 1) Carbon content, carbon isotope composition such as oxygen and hydrogen isotope compositions from serpentine mineral and carbon and oxygen isotope composition on calcite and serpentine veins from Holes of ODP Site 149-897
DOI: 10.1594/pangaea.484148
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_6N_58N/176-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.434399
title: Hourly sea level from coastal tide gauge station Duck_Pier in 1983 (Research quality database)
DOI: 10.1594/pangaea.484168
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_6N_58W/237-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.484142
title: Hydrochemistry measured on water bottle samples at station NAtl_1981_6N_58N/138-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.664480
title: Oceanography at CTD/bottle station IFREMER_1320
DOI: 10.1594/pangaea.920297
title: Continuous water level observations at station BEFmate_I3upp (2018-05)
DOI: 10.1594/pangaea.920142
title: Continuous water level observations at station BEFmate_I3low (2017-05)
DOI: 10.1594/pangaea.718969
title: (Table 3) Survey of Atlantic Ocean DSDP sites for hiatuses PH and NH 1 through NH 7
DOI: 10.1594/pangaea.705524
title: (Table 4) Chemical composition of sample-residues (non-carbonate fractions) from lower Miocene sediments, ODP Site 166-1007
DOI: 10.1594/pangaea.809113
title: (Table S1) Nannofossil abundances at DSDP Hole 86-577

description: DEPTH, sediment is given in mbsf. Most data from Backman (1986).
DOI: 10.1594/pangaea.844820
title: Radiosonde PS88/36317 during POLARSTERN cruise PS88.1 (ANT-XXX/1.1) on 2014-10-31T11

description: Height of tropopause 14912 m, precipitable water content 3.0102 cm
DOI: 10.1594/pangaea.868395
title: Annotated record of the detailed examination of Mn deposits from DSDP Site 67, Leg 7 (Cores 67-1, 67A-2)

description: Site 67 is on the Hawaiian Arch, in the general region selected for one of the Mohole Project sites. Therefore, intensive geophysical surveys have been made in the area. The objectives were to penetrate the entire sedimentary sequence to basement in order to learn the petrology and ages of the sediments and of the seismic reflectors, and to obtain samples of the underlying basement rocks. Well consolidated and bedded volcanic sandstone and mudstone, and claystone were found to extend from the sea floor to a depth of 60 meters, where a layer of hard brown porcelanite stopped the bit. Displaced radiolarians in mud from a core at 60 meters indicate sediments of early Eocene or late Paleocene age are present somewhere above that depth.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Winterer, Edward L; Riedel, William R; Moberly, Ralph; Resig, Johanna M; Kroenke, Loren W; Gealy, E L; Heath, G Ross; Bronnimann, P; Martini, E; Worsley, Thomas R (1971): Site 67. In: Winterer, E.L.; et al., Initial Reports of the Deep Sea Drilling Project, 7, Initial Reports of the Deep Sea Drilling Project, 7, U.S. Government Printing Office, VII, 821-841
DOI: 10.1594/pangaea.679398
title: Physical oceanography at CTD station CE0506_47
DOI: 10.1594/pangaea.802134
title: (Table 1) Late Cenozoic silicoflagellate biostratigraphy, relative paleotemperature, and distribution of various genera and morphologic subgroups with remarks on noteworthy occurrences at DSDP Hole 86-577
DOI: 10.1594/pangaea.679379
title: Physical oceanography at CTD station CE0506_28
DOI: 10.1594/pangaea.864678
title: Age, 232Th, 230Th, 238U, CaCO3, organic carbon, lithogenic fraction, opal, and iron concentrations of 4 sediment cores from the southwest Pacific, with calculated 230Th-normalized mass flux

description: Increased export production (EP) in the Subantarctic Zone (SAZ) of the Southern Ocean due to iron fertilisation has been proposed as a key mechanism for explaining carbon drawdown during the last glacial maximum (LGM). This work reconstructs marine EP since the LGM at four sites around New Zealand. For the first time in this region, 230-Thorium-normalised fluxes of biogenic opal, carbonate, excess barium, and organic carbon are presented. In Subtropical Waters and the SAZ, these flux variations show that EP has not changed markedly since the LGM. The only exception is a site currently north of the subtropical front. Here we suggest the subtropical front shifted over the core site between 18 and 12 ka, driving increased EP. To understand why EP remained mostly low and constant elsewhere, lithogenic fluxes at the four sites were measured to investigate changes in dust deposition. At all sites, lithogenic fluxes were greater during the LGM compared to the Holocene. The positive temporal correlation between the Antarctic dust record and lithogenic flux at a site in the Tasman Sea shows that regionally, increased dust deposition contributed to the high glacial lithogenic fluxes. Additionally, it is inferred that lithogenic material from erosion and glacier melting deposited on the Campbell Plateau during the deglaciation (18-12 ka). From these observations, it is proposed that even though increased glacial dust deposition may have relieved iron limitation within the SAZ around New Zealand, the availability of silicic acid limited diatom growth and thus any resultant increase in carbon export during the LGM. Therefore, silicic acid concentrations have remained low since the LGM. This result suggests that both silicic acid and iron co-limit EP in the SAZ around New Zealand, consistent with modern process studies.
description: Supplement to: Durand, Axel; Chase, Zanna; Noble, Taryn L; Bostock, Helen C; Jaccard, Samuel L; Kitchener, Priya; Townsend, Ashley T; Jansen, Nils; Kinsley, Les; Jacobsen, Geraldine; Johnson, Sean; Neil, Helen L (2017): Export production in the New-Zealand region since the Last Glacial Maximum. Earth and Planetary Science Letters, 469, 110-122