cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.927993
title: M/S Silja Serenade (Helsinki-Stockholm) pCO2 underway measurements in 2018-04

description: Quality control:Measurements during calibration, cleaning, maintenance and low discharge have been removed.-----Flag system:A flag system is applied to the data. Good data that passes the flag control, gets the flag of 11111111. If the raw CO2 partial pressure (not calibration corrected) is out of boundaries (20-1200 ppm), the first digit changes to 9, i.e. if this is only abnormality, the flag would be 9111111. All flags and their boundary limits are listed in the table below.--Flag =&gt; Parameter =&gt; Lower boundary to Upper boundary91111111 =&gt; CO2_ppm_wet =&gt; 20 ppm to 2000 ppm19111111 =&gt; T equ =&gt; -1 °C to 30 °C11911111 =&gt; T tech =&gt; -1 °C to 30 °C11191111 =&gt; Salinity =&gt; 5 to 811119111 =&gt; Pressure =&gt; 0.9 to 1.111111911 =&gt; coeff_A/coeff_B/coeff_C =&gt; -50/0.9/-0.0001 to 100/1.3/0.000111111191 =&gt; SHEQ_flow_LPM/LICOR_flow =&gt; 1.0/50 to N/A/N/A11111119 =&gt; Visually inspected bad data-----Calculations:The CO2 molar fraction observed by the LI-840A is denoted as wet CO2 molar fraction (CO2_ppm_wet).--The molar fraction with respect to dry air is calculated as,CO2_ppm_dry = CO2_ppm_wet / (1 - H2O_ppt/1000),where H2O_ppt is the H2O molar fraction measured by the LI-840A.--For each calibration sequence every 4 hour, a 2nd order polynomial function is fitted to the observed and real molar fractions:CO2_ppm_dry_cal_cor = coeff_A + coeff_B * CO2_ppm_dry + coeff_C * (CO2_ppm_dry)^2Polynomial coefficients (coeff_A, coeff_B and coeff_C) are interpolated between the calibrations.--CO2 partial pressure in dry air is calculated as,pCO2_uatm_dry = CO2_ppm_dry_cal_cor * P_eq_atm--The CO2 partial pressure in wet air (Dickson and Goyet, 1994),pCO2_uatm = pCO2_uatm_dry * (1 - Pws_eq_atm)where saturation water vapor pressure, Pws_eq_atm, is calculated from equilibratortemperature, T_eq_degC (Wagner and PruB, 2002, Eq. 2.5).--Temperature corrected CO2 partial pressure is given for the inlet,pCO2_uatm_temp_corr = pCO2_uatm * exp [ A* (T_in_degC - T_eq_degC)]where A = 0.0423 (Takahashi et al., 1993).
DOI: 10.1594/pangaea.271708
title: Splice table (interval listing) of Site 202-1242

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.916030
title: CIM-ECIMAT ocean meteorological station time-series - physical oceanography data

description: We present a six years length ocean meteorological dataset collected at the automatic station at the CIM-ECIMAT station of the University of Vigo. The data includes time-series of seawater temperature, conductivity, and dissolved oxygen along with air temperature, humidity, and wind data. The sampling interval was ten minutes.
DOI: 10.25549/annis-ouc17133665
title: Templo de Santa Teresa la Nueva, Mexico City, Mexico, 1933

description: Church with side-by-side façades marking it as a former convent, Mexico City, Distrito Federal, Mexico, 1933.
DOI: 10.1594/pangaea.271653
title: Splice table (interval listing) of Site 175-1086

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271690
title: Splice table (interval listing) of Site 198-1212

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271634
title: Splice table (interval listing) of Site 172-1055

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.774719
title: (Table T4) Deuterium composition of methane in void gas of ODP Leg 204 sites
DOI: 10.25549/annis-ouc17130497
title: Templo de Santa Teresa la Nueva, Mexico City, Mexico, 1933

description: Church with side-by-side façades marking it as a former convent, Mexico City, Distrito Federal, Mexico, 1933.
DOI: 10.1594/pangaea.271616
title: Splice table (interval listing) of Site 162-983

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271646
title: Splice table (interval listing) of Site 175-1079

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.706967
title: (Table T2) Iodine isotopic composition and minimum ages in pore water of ODP Hole 204-1250C
DOI: 10.1594/pangaea.706969
title: (Table T2) Iodine isotopic composition and minimum ages in pore water of ODP Hole 204-1252A
DOI: 10.1594/pangaea.774725
title: (Table T7) Isotope composition of dissolved inorganic carbon from interstitial waters of ODP Leg 204 sites
DOI: 10.1594/pangaea.774720
title: (Table T5) Carbon isotope composition of methane and carbon dioxide in PCS gas of ODP Leg 204 sites
DOI: 10.25549/annis-ouc17088065
title: Templo de Santa Teresa la Nueva, Mexico City, Mexico, 1933

description: Church with side-by-side façades marking it as a former convent, Mexico City, Distrito Federal, Mexico, 1933.
DOI: 10.1594/pangaea.271710
title: Splice table (interval listing) of Site 207-1258

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.763251
title: (Table 1) Molecular properties of void gases at ODP Leg 204 sites
DOI: 10.1594/pangaea.783635
title: FISH analysis of biofilm samples from five CANON reactors in Beijing

description: Completely autotrophic nitrogen removal over nitrite (CANON) has been regarded as an efficient and economical process for nitrogen removal from wastewater. The distribution and genetic diversity of the functional microorganisms in five lab-scale CANON reactors have been investigated by using some molecular biology methods. Nitrosomonas-like aerobic ammonium oxidizing bacteria (AerAOB) and Candidatus Brocadia-related anaerobic ammonium oxidizing bacteria (AnAOB) were detected as predominant functional microbes in the five reactors while Nitrobacter-like nitrite oxidizing bacteria (NOB) existed only in the systems operated at ambient temperature. Communities of AerAOB and AnAOB were almost similar among the five reactors while the distribution of the functional microbes was either scattered or densely packed. Meanwhile, this study has demonstrated the feasibility of starting up CANON by inoculating conventional activated sludge in low ammonium content at ambient temperature.
description: Picture of a FISH analysis of biofilm samples from five CANON reactors. Left: Optical photomicrographs; Right: FISH micrographs: hybridization of biomass with Cy3-labelled NOS190 (red, targeting AerAOB), AMCA-labelled AMX368 (blue, targeting AnAOB) and HEX-labelled NIT3 (green, targeting Nitrobacter). AerAOB appears purple because of the overlapping of red and blue backgrounds. Bar: 50 µm.
description: Supplement to: Liu, Tao; Li, Dong; Zeng, Huiping; Li, Xiangkun; Liang, Yuhai; Chang, Xiaoyan; Jie, Zhang (2012): Distribution and genetic diversity of functional microorganisms in different CANON reactors. Bioresource Technology, 123, 574-580
DOI: 10.1594/pangaea.271617
title: Splice table (interval listing) of Site 162-984

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271630
title: Splice table (interval listing) of Site 167-1021

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.763252
title: (Table 2) Molecular properties of gas from decomposed gas hydrates of ODP Leg 204 sites

description: Sediment depth is given in mbsf. 0 ist 0 or below detection limit.
DOI: 10.25549/annis-ouc17131626
title: Catedral de Azcapotzalco, Mexico City, Mexico, 1936

description: The Catedral de Azcapotzalco, Mexico City, Distrito Federal, Mexico, 1936 June 25.
DOI: 10.1594/pangaea.271607
title: Splice table (interval listing) of Site 160-969

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.988026
title: Multibeam bathymetry processed data (Atlas Hydrosweep DS 3 echo sounder entire dataset) of RV POLARSTERN during cruise PS150, Arctic Ocean

description: Multibeam data were collected during RV Polarstern cruise PS150 (2025-09-04 to 2025-10-24). Multibeam sonar system was Atlas Hydrographic Hydrosweep DS 3 multibeam echo sounder. Data are processed with Caris HIPS, including sound velocity correction with SV data from CTDs and World Ocean Atlas 23 (https://www.ncei.noaa.gov/archive/accession/NCEI-WOA23), tidal correction with TPXO9_atlas_v5 (https://www.tpxo.net), and manual cleaning. The soundings are combined in daily files, the format is XYZ ASCII ( ). Additional grids have been computed with depth dependent cell size to visualize the data. These grids are not meant for scientific analysis or navigation, but for overview purposes only.
description: These data should not be used for navigational purposes.
DOI: 10.15468/dl.wghmpj
title: Occurrence Download

description: A dataset containing 13 species occurrences available in GBIF matching the query:
{
 "and" : [
 "GadmGid is CHN.29_1",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Chlidonias hybrida"
 ]
}

 The dataset includes 13 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000899-260221153910048/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.271613
title: Splice table (interval listing) of Site 162-980

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.706964
title: (Table T2) Iodine isotopic composition and minimum ages in pore water of ODP Hole 204-1247B
DOI: 10.1594/pangaea.271645
title: Splice table (interval listing) of Site 175-1078

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.706965
title: (Table T2) Iodine isotopic composition and minimum ages in pore water of ODP Hole 204-1248C
DOI: 10.25549/annis-ouc17129814
title: Catedral de Azcapotzalco, Mexico City, Mexico, 1936

description: The Catedral de Azcapotzalco, Mexico City, Distrito Federal, Mexico, 1936 June 25.
DOI: 10.1594/pangaea.706952
title: (Table T1) Concentrations of iodine, bromine, and chlorine in pore water of ODP Site 204-1244
DOI: 10.1594/pangaea.706966
title: (Table T2) Iodine isotopic composition and minimum ages in pore water of ODP Hole 204-1249C
DOI: 10.1594/pangaea.706954
title: (Table T1) Concentrations of iodine, bromine, and chlorine in pore water of ODP Site 204-1246
DOI: 10.1594/pangaea.271608
title: Splice table (interval listing) of Site 160-973

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271683
title: Splice table (interval listing) of Site 189-1168

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.25549/annis-ouc17128018
title: Cloister with murals, other decoration of Parroquía y Ex-convento San Agustin de Hipona, Acolman, Mexico, 1936

description: Partially restored murals on walls of cloister, and decoration on Parroquía y Ex-convento San Agustin de Hipona, Acolman, Mexico, Mexico, 1936 June 30.
DOI: 10.1594/pangaea.271685
title: Splice table (interval listing) of Site 189-1171

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271691
title: Splice table (interval listing) of Site 199-1215

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271680
title: Splice table (interval listing) of Site 184-1147

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.706957
title: (Table T1) Concentrations of iodine, bromine, and chlorine in pore water of ODP Site 204-1249
DOI: 10.1594/pangaea.271611
title: Splice table (interval listing) of Site 161-976

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271716
title: Splice table (interval listing) of Site 208-1265

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.25549/annis-ouc17132481
title: "Acolman church and monastery," Acolman, Mexico, 1936

description: Acolman church and monastery exteriors, Acolman, Mexico, Mexico, 1936 June 30.
DOI: 10.1594/pangaea.271681
title: Splice table (interval listing) of Site 184-1148

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271718
title: Splice table (interval listing) of Site 208-1267

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271609
title: Splice table (interval listing) of Site 161-974

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271713
title: Splice table (interval listing) of Site 208-1262

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271605
title: Splice table (interval listing) of Site 160-966

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.1594/pangaea.271712
title: Splice table (interval listing) of Site 207-1261

description: Data derives from the downhole depth-shifting and correlation of multiple core and logging datasets. Splicer and Sagan are the tools used to depth-shift and correlate the input datasets. A custom tool, SplicerIntegrator, is used to record the affine and splice lookup tables in the central database.
DOI: 10.25549/annis-ouc17129230
title: "Acolman church and monastery," Acolman, Mexico, 1936

description: Acolman church and monastery exteriors, Acolman, Mexico, Mexico, 1936 June 30.
DOI: 10.1594/pangaea.706955
title: (Table T1) Concentrations of iodine, bromine, and chlorine in pore water of ODP Site 204-1247
DOI: 10.1594/pangaea.774700
title: (Table T1) Deuterium and oxygen isotope composition of interstitial waters from ODP Leg 204 sediments

description: The isotopic compositions of interstitial waters collected from Hydrate Ridge during Ocean Drilling Program Leg 204 were measured to evaluate the fluid evolution of this accretionary prism. At shallow depths, the dissolved Cl- concentrations and dD and d18O values of the interstitial water reflect changes in the salinity and the isotopic compositions of seawater from the Last Glacial Maximum to the present. The presence of disseminated gas hydrates, which is well identified by discrete low Cl- anomalies within the gas hydrate stability zone, is accompanied by high dD and d18O values of the freshened fluids. This is consistent with incorporation of heavy isotopes into the gas hydrate lattice, which is also apparent in the signals observed at the ridge summit. Here, massive gas hydrate formation in the upper 20 meters below seafloor leads the formation of brines with dissolved Cl- concentrations as high as 1400 mM. The interstitial waters sampled near massive gas hydrates at the ridge summit are extremely depleted in D and 18O. Clay mineral dehydration within the deep prism results in a progressive decrease in Cl- and dD with depth. Dehydration temperature estimates based on those data likely suggest a progressive increase in the temperature of isotopic fractionation between clay and water with distance from the prism toe. The oxygen isotope data probably reflect the combined effects of clay dehydration, carbonate precipitation, and alteration of oceanic basement; however, there are not enough data to constrain the relative contribution of these processes to the observed signals.
description: Supplement to: Tomaru, Hitoshi; Matsumoto, R; Torres, Marta E; Borowski, Walter S (2006): Geological and geochemical constraints on the isotopic composition of interstitial waters from the Hydrate Ridge region, Cascadia Continental Margin. In: Tréhu, AM; Bohrmann, G; Torres, ME; Colwell, FS (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 204, 1-20
DOI: 10.1594/pangaea.706968
title: (Table T2) Iodine isotopic composition and minimum ages in pore water of ODP Site 204-1251
DOI: 10.1594/pangaea.770069
title: (Table 1) Depth to basement, accreted melange, bottom simulating reflector and sediment penetration in meters below seafloor

description: Drilling in the Cascadia accretionary complex enable us to evaluate the contribution of dehydration reactions and gas hydrate dissociation to pore water freshening. The observed freshening with depth and distance from the prism toe is consistent with enhanced conversion of smectite to illite, driven by increase in temperature and age of accreted sediments. Although they contain gas hydrate -as evidenced by discrete low chloride spikes- the westernmost sites drilled on Hydrate Ridge show no freshening trend with depth. Strontium data reveal that all the mélange samples contain deep fluids modified by reaction with the subducting oceanic crust. Thus we infer that, at the westernmost sites, accretion is too recent for the sediments to have undergone significant illitization. Our data demonstrate that a smooth decrease in dissolved chloride with depth cannot generally be used to infer the presence or to estimate the amount of gas hydrate in accretionary margins.
description: Distance to the prism toe in kilometers +-1.
description: Supplement to: Torres, Marta E; Teichert, Barbara M A; Tréhu, Anne M; Borowski, Walter S; Tomaru, Hitoshi (2004): Relationship of pore water freshening to accretionary processes in the Cascadia margin: Fluid sources and gas hydrate abundance. Geophysical Research Letters, 31(22), 1-4
DOI: 10.1594/pangaea.706975
title: (Table 1) Iodine isotopic composition and minimum ages in pore water of ODP Hole 204-1251B

description: Iodine concentrations see Fehn et al., 2006, data set: doi:10.1594/PANGAEA.706959, further 129I/I ratios Fehn et al., 2006, data set: doi:10.1594/PANGAEA.706968
DOI: 10.25549/annis-ouc17130885
title: "Interior of Acolman Monastery Church," Acolman, Mexico, 1936

description: Interior of Parroquía y Ex-convento San Agustin de Hipona, Acolman, Mexico, Mexico, 1936 June 30.