cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.923679
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek WY3, Wyoming
DOI: 10.1594/pangaea.923671
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek CO2, Colorado
DOI: 10.1594/pangaea.913408
title: Magnetic parameters of sediment core MD01-2393
DOI: 10.1594/pangaea.925988
title: Solid phase trace metal analyses and organic carbon of sediment core GeoB8455-2

description: In this publication, only values down to a depth of 9.00 m are mentioned.
DOI: 10.1594/pangaea.626575
title: Chemical composition of sedimentary rocks from Hole VNIIO-1983-81 drilled in the Barents Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.626564
DOI: 10.1594/pangaea.938213
title: Long-term CCNC measurements at the central European ACTRIS research station Melpitz, Germany, 2012-2016

description: Atmospheric aerosol measurements were conducted at the Melpitz observatory, Germany. The data was collected during 2012 to 2016, measured by Droplet Measurement Technologies Cloud Condensation Nucleus Counter (DMT-CCNC).
description: Columns #9-12 contain the fit parameters "D_c", "a", "b" and "sigma_s" of following sigmoid function, where "AF" means activated fraction of aerosol particles, "a" and "b" are the lower and upper limits of the sigmoid function, "D_c" is the critical diameter of dry particles, and "sigma_s" means the shape of the sigmoid function:AF = a + b / ( 1 + exp(-(D-D_c)/sigma_s) )Column #15: The ratio "(D75-D25)/D50" represents the degree of external mixing of aerosol particles. The definations of D75, D50, D25, DX are the diameter (D) at which 75%, 50%, 25, X% of particles are activated at the given supersaturation condition. See Jurányi et al. (2013, doi:10.5194/acp-13-6431-2013) for details.Columns #16-61 contain the particle size distribution for 46 size bins. The mid-diameter of each bin (i.e. the geometric mean of the bin interval) is given in the Parameter Comment.
DOI: 10.1594/pangaea.913410
title: Magnetic parameters of sediment core MD05-2898
DOI: 10.1594/pangaea.923672
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek CO3, Colorado
DOI: 10.1594/pangaea.923673
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek CO4, Colorado
DOI: 10.1594/pangaea.925989
title: Solid phase trace metal analyses and organic carbon of sediment core GeoB8470-4

description: In this publication, only values down to a depth of 4.10 m are mentioned.
DOI: 10.1594/pangaea.913409
title: Magnetic parameters of sediment core MD05-2896-97
DOI: 10.1594/pangaea.923674
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek ID1, Idaho
DOI: 10.1594/pangaea.923675
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek ID2, Idaho
DOI: 10.1594/pangaea.937670
title: Clumped and oxygen isotope data of calcite veins from ultramafic and mafic rocks recovered from the Wadi Tayin Massif, Samail Ophiolite, Oman Drilling Project Phase II

description: The clumped and oxygen isotopes of calcite from ultramafic, and mafic rocks recovered during ICDP Expedition 5057, Oman Drilling Project Phase II (November 2017 to February 2018) on the Wadi Tayin Massif, Samail Ophiolite, was examined to characterize carbon sources, speciation, and the fate of organic and inorganic carbon during natural large-scale hydration and carbonization. The measurements were performed at the ETH Zurich from 2017 to 2020 using a Kiel IV carbonate device interfaced with a ThermoFisher Scientific MAT253 isotope ratio mass spectrometer.
DOI: 10.1594/pangaea.923676
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek OR1, Oregon
DOI: 10.1594/pangaea.937671
title: Clumped and oxygen isotope data of dolomite veins from ultramafic rocks recovered from the Wadi Tayin Massif, Samail Ophiolite, Oman Drilling Project Phase II

description: The clumped and oxygen isotopes of dolomite from ultramafic rocks recovered during ICDP Expedition 5057, Oman Drilling Project Phase II (November 2017 to February 2018) on the Wadi Tayin Massif, Samail Ophiolite, was examined to characterize carbon sources, speciation, and the fate of organic and inorganic carbon during natural large-scale hydration and carbonization. The measurements were performed at the ETH Zurich from 2017 to 2020 using a Kiel IV carbonate device interfaced with a ThermoFisher Scientific MAT253 isotope ratio mass spectrometer.
DOI: 10.1594/pangaea.923677
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek WY1, Wyoming
DOI: 10.1594/pangaea.926000
title: Mass accumulation rates of sediment core GeoB8426-3

description: In this publication, only values down to a depth of 8.40 m are mentioned.
DOI: 10.1594/pangaea.874468
title: XANES spectra at micro-sites of increase P intensity in Bad Brueckenau subsoil sample, P12

description: Element: P; Element Edge: K; Athena.e0: 2152.49321
DOI: 10.1594/pangaea.926002
title: Mass accumulation rates of sediment core GeoB8470-4

description: In this publication, only values down to a depth of 4.10 m are mentioned.
DOI: 10.1594/pangaea.926012
title: Age model of sediment core GeoB8426-3

description: In this publication, only values down to a depth of 8.40 m are mentioned.
DOI: 10.1594/pangaea.498251
title: Physical oceanography from BT during cruise U74X008750B_1962
DOI: 10.1594/pangaea.783211
title: Documentation of sediment core M66/3a_140
DOI: 10.1594/pangaea.807444
title: Fractionated primary productivity in the water column during AGHYAR cruise NASEER-1
DOI: 10.1594/pangaea.938211
title: Long-term ACSM and MAAP measurements at the central European ACTRIS research station Melpitz, Germany, 2012-2016

description: Atmospheric aerosol measurements were conducted at the Melpitz observatory, Germany. The data was collected during 2012 to 2016, measured by Aerosol Chemical Speciation Monitor (ACSM) and Multi-angle absorption photometer (MAAP).
description: Negative values are a within the measurement uncertainty and can be interpreted as 'below detection limit'.
DOI: 10.1594/pangaea.926014
title: Age model of sediment core GeoB8470-4

description: In this publication, only values down to a depth of 4.10 m are mentioned.
DOI: 10.1594/pangaea.926018
title: Radiocarbon age determination of sediment core GeoB8426-3
DOI: 10.1594/pangaea.843917
title: Physical oceanography (microcat) from mooring KPO_1061 lower instruments

description: Quality flags:0 --&gt; unknown1 --&gt; good data2 --&gt; probably good data3 --&gt; potentially correctable bad data4 --&gt; bad data7 --&gt; nominal value8 --&gt; interpolated value9 --&gt; missing value
DOI: 10.1594/pangaea.782583
title: (Appendix A) Sulphur isotope ratios of upper crust samples of the sheeted dyke complex at Pito Deep

description: The behaviour of seawater sulphate in hydrothermal systems at intermediate- to fast-spreading ridges is investigated using new analyses of the d34S, sulphur concentration and Fe2O3/Fe2O3total, combined with existing 87Sr/86Sr, of sheeted dykes from the Pito Deep tectonic window. The Pito Deep sheeted dyke complex has a similar composition to the sheeted dykes drilled at ODP Hole 504B suggesting that the measured compositions are representative of sheeted dyke complexes at intermediate- to fast-spreading ridges. The dykes show only small increases in ?34S which, combined with the rock dominated d34S of vent fluids, requires the majority of seawater sulphate to be precipitated as anhydrite before the fluid reacts with the sheeted dyke complex. This loss of sulphate from the fluid means that a much higher Fe2O3 in the sheeted dyke complex than in fresh MORB glasses cannot be explained by oxidation due to seawater sulphate reduction during fluid–rock reaction. Instead, oxidation probably occurs due to degassing of reduced species, largely H2, during dyke emplacement and solidification. A mass balance model that accounts for anhydrite precipitation and Sr partitioning into the anhydrite, as well as fitting the concentration and isotopic ratios of S and Sr in the sheeted dykes and vent fluids, suggests water/rock ratios of ?1. For a 1 km thick sheeted dyke complex this is equivalent to a fluid flux of ?3 * 10**6 kg/m**2, sufficient to remove ? 60% of the latent heat of crystallization from the lower crust
description: For major element data (except Fe2O3) see Pollock et al (2009) datasets doi:10.1594/PANGAEA.782597 and Heft et al (2008) datasets: doi:10.1594/PANGAEA.782661. For Sr isotope and trace element data see Barker et al (2008) dataset: doi:10.1594/PANGAEA.782664.
description: Supplement to: Barker, A K; Coogan, Laurence A; Gillis, Kathryn M (2010): Insights into the behaviour of sulphur in mid-ocean ridge axial hydrothermal systems from the composition of the sheeted dyke complex at Pito Deep. Chemical Geology, 275(1-2), 105-115
DOI: 10.1594/pangaea.601894
title: (Table S2) Volcano-stratigraphic synchronisation B32 vs. EDML vs. EDC, Antarctica

description: Data used: B32-SO4 (Traufetter et al 2004), EDML-DEP (Wilhelms), EDC96-SO4 (Udisti).EDML-Depth assignments: Some depth assignents for the same volcanic events deviated in the the EDML data sets of DEP, IC-SO4 and FIC-SO4. To overcome this, the average depth was calculated from DEP and IC-SO4, thus omitting the FIC-SO4, which in 2002 did not yet consider missing core at breaks. All three depths are listed here for documentation.B32-Year: The date was manually chosen from Traufetter et al 2004 (see DOI:10.1594/PANGAEA.601853), H. Fischer pers com 2005-10-12, F. Fundel pers com, R. Udisti pers com; usually there was only a small discrepancy between the 3 dates given, and usually the average date was taken. The selection of events and assignments of dates to be used as primary dating information for EDML1/EDC3 was agreed upon by AWI and Florence.
DOI: 10.1594/pangaea.823285
title: Nimrod (dynamic penetrometer) measurements of a sandbar at Raglan, New Zealand in 2009

description: Dynamic penetrometer data obtained with the Nimrod penetrometer (MARUM). Data is presented as (i) penetration depth (including for different layers if present), (ii) measured deceleration and (iv) estimated quasi-static bearing capacity including range of uncertainty due to the processing method. Lat/Long coordinates are given.
description: Supplement to: Stark, Nina; Kopf, Achim J (2013): In-situ geotechnical investigation of sediment remobilitzation processes utilizing geotechnical measurement techniques to detect, quantify and describe sediment erosion and deposition. Sea Technology, 54
DOI: 10.1594/pangaea.552232
title: Methane of ice core EDML

description: Time scale: GICC05 age scale for the NGRIP ice core
DOI: 10.1594/pangaea.745600
title: Penetration velocity and deceleration of penetrometer stations N1 to N97 during cruise Senckenberg_11_2008

description: In-situ geotechnical measurements of surface sediments were carried out along large subaqueous dunes in the Knudedyb tidal inlet channel in the Danish Wadden Sea using a small free-falling penetrometer. Vertical profiles showed a typical stratification pattern with a resolution of ~1 cm depicting a thin surface layer of low sediment strength and a stiffer substratum below (quasi-static bearing capacity equivalent: 1–3 kPa in the top layer, 20–140 kPa in the underlying sediment; thickness of the top layer ca. 5–8 cm). Observed variations in the thickness and strength of the surface layer during a tidal cycle were compared to mean current velocities (measured using an acoustic Doppler current profiler, ADCP), high-resolution bathymetry (based on multibeam echo sounding, MBES) and qualitative estimates of suspended sediment distributions in the water column (estimated from ADCP backscatter intensity). The results revealed an ebb dominance in sediment remobilization, and a general accretion of the bed towards low water. A loose top layer occurred throughout the tidal cycle, likely influenced by bedload transport and small events of suspended sediment resettlement (thickness: 6 +-2 cm). Furthermore, this layer showed a significant increase in thickness (e.g. from 8 cm to 16 cm) related to periods of overall deposition. These findings imply that dynamic penetrometers can conveniently serve to (1) quantify potentially mobile sediments by determining the thickness of a loose sediment surface layer, (2) unravel sediment strength development in potentially mobile sediments and (3) identify sediment accumulation. Such data are an important complement and add a new geotechnical perspective during investigations of sediment remobilization processes in highly dynamic coastal environments.
description: Supplement to: Stark, Nina; Hanff, Hendrik; Svenson, C; Ernstsen, Verner Brandbyge; Lefebvre, Alice; Winter, Christian; Kopf, Achim J (2011): Coupled penetrometer, MBES and ADCP assessments of tidal variations in surface sediment layer characteristics along active subaqueous dunes, Danish Wadden Sea. Geo-Marine Letters, 31(4), 249-258
DOI: 10.1594/pangaea.938214
title: Long-term MPSS measurements at the central European ACTRIS research station Melpitz, Germany, 2012-2016

description: Atmospheric aerosol measurements were conducted at the Melpitz observatory, Germany. The data was collected during 2012 to 2016, measured by Mobility Particle Size Spectrometer (T-MPSS).
description: Columns #2-56 contain the particle size distribution for 55 size bins. The mid-diameter of each bin (i.e. the geometric mean of the bin interval) is given in the Parameter Comment.Negative values are a within the measurement uncertainty and can be interpreted as 'below detection limit'.
DOI: 10.1594/pangaea.782619
title: (Appendix 1) Contents, coefficients of roundness and flatness and their variations of rock fragments in 25-50 mm size fraction from shelf bottom sediments of the Sea of Okhotsk
DOI: 10.1594/pangaea.784350
title: Color data from IODP Hole 333-C0012C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.923678
title: Pre/during/post-fire Normalized Difference Vegetation Index along creek WY2, Wyoming
DOI: 10.1594/pangaea.552327
title: Physical properties of Hole 310-M0015B
DOI: 10.1594/pangaea.913405
title: Magnetic parameters of ODP Site 184-1145
DOI: 10.1594/pangaea.824505
title: Magnetic remanence on discrete pieces from IODP Hole 318-U1359A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.497059
title: Physical oceanography from BT during cruise M90DI00007B_1953
DOI: 10.1594/pangaea.913407
title: Magnetic parameters of ODP Site 184-1147
DOI: 10.1594/pangaea.868371
title: Physical water column characteristics from April to June 2014 in Kongsfjorden (Spitsbergen)
DOI: 10.1594/pangaea.913411
title: Magnetic parameters of sediment core MD05-2900
DOI: 10.1594/pangaea.786009
title: Description and distribution of lithologic units (VCD) from IODP Hole 333-C0012G

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.931565
title: Basic and other measurements of radiation at Neumayer Station (2020-03)
DOI: 10.1594/pangaea.937668
title: Content and carbon and oxygen isotope composition of total carbon, total non-carbonate carbon, and total inorganic carbon of mafic and ultramafic rocks from the Wadi Tayin Massif, Samail Ophiolite, Oman Drilling Project Phase II

description: The carbon geochemistry of serpentinized peridotites, and mafic rocks recovered during ICDP Expedition 5057, Oman Drilling Project Phase II (November 2017 to February 2018) on the Wadi Tayin Massif, Samail Ophiolite, was examined to characterize carbon sources, speciation, and the fate of organic and inorganic carbon during natural large-scale hydration and carbonization. The measurements were performed at the ETH Zurich, Geological Institute from 2017 to 2020 using a FlashEA 1112 Elemental Analyzer (EA) interfaced via a Conflo IV to a Delta V Plus Isotope Ratio Mass Spectrometer for total carbon (TC) and total non-carbonate carbon (NCC) content and isotope composition, and a GasBench II connected to a Delta V Mass Spectrometer for the total inorganic carbon (TIC) isotope composition. Results are reported as replicates. Analyzed samples are aliquots of samples used for microbiological studies and were collected under sterile conditions (denoted as MBio samples).
DOI: 10.1594/pangaea.937669
title: Clumped and oxygen isotope data of aragonite veins from ultramafic and mafic rocks recovered from the Wadi Tayin Massif, Samail Ophiolite, Oman Drilling Project Phase II

description: The clumped and oxygen isotopes of aragonite from ultramafic, and mafic rocks recovered during ICDP Expedition 5057, Oman Drilling Project Phase II (November 2017 to February 2018) on the Wadi Tayin Massif, Samail Ophiolite, was examined to characterize carbon sources, speciation, and the fate of organic and inorganic carbon during natural large-scale hydration and carbonization. The measurements were performed at the ETH Zurich from 2017 to 2020 using a Kiel IV carbonate device interfaced with a ThermoFisher Scientific MAT253 isotope ratio mass spectrometer.
DOI: 10.1594/pangaea.931562
title: Basic and other measurements of radiation at Neumayer Station (2020-02)
DOI: 10.1594/pangaea.924693
title: Physical oceanography from mooring KPO_1001

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019).
description: instrument = Label:kpo_1001_01 File:kpo_1001_instr_01.nc Type:Teledyne RDI Workhorse 300 SN:508instrument = Label:kpo_1001_02 File:kpo_1001_instr_02.nc Type:GEOMAR TD-Logger SN:24instrument = Label:kpo_1001_03 File:kpo_1001_instr_03.nc Type:Seabird MicroCat 37-SM SN:00052instrument = Label:kpo_1001_04 File:kpo_1001_instr_04.nc Type:Seabird MicroCat 37-SM SN:00055instrument = Label:kpo_1001_05 File:kpo_1001_instr_05.nc Type:Seabird MicroCat 37-SM SN:00278instrument = Label:kpo_1001_06 File:kpo_1001_instr_06.nc Type:Teledyne RDI LongRanger 75 SN:2395instrument = Label:kpo_1001_07 File:kpo_1001_instr_07.nc Type:Aanderaa RCM 8 SN:09930instrument = Label:kpo_1001_08 File:kpo_1001_instr_08.nc Type:Sontek Argonaut SN:182instrument = Label:kpo_1001_09 File:kpo_1001_instr_09.nc Type:Aanderaa RCM 8 SN:09964instrument = Label:kpo_1001_10 File:kpo_1001_instr_10.nc Type:WHOI Smartie MMP SN:120comment = flag_meaningscomment = 0:unknowncomment = 1:good_datacomment = 2:probably_good_datacomment = 3:potentially_correctable_bad_datacomment = 4:bad_datacomment = 5:not_usedcomment = 6:not_usedcomment = 7:nominal_valuecomment = 8:interpolated_valuecomment = 9:missing_value
DOI: 10.1594/pangaea.924782
title: Physical oceanography from mooring KPO_1201

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019).
description: instrument = Label:kpo_1201_02 File:kpo_1201_instr_02.nc Type:Teledyne RDI QuarterMaster 150 SN:21861instrument = Label:kpo_1201_03 File:kpo_1201_instr_03.nc Type:GEOMAR TD-Logger SN:70instrument = Label:kpo_1201_04 File:kpo_1201_instr_04.nc Type:Teledyne RDI LongRanger 75 SN:19398instrument = Label:kpo_1201_05 File:kpo_1201_instr_05.nc Type:Seabird MicroCat 37-SM SN:02617 depth/pressure data was at least partially derived and not directly measured, consult quality flags for detailsinstrument = Label:kpo_1201_06 File:kpo_1201_instr_06.nc Type:Aanderaa Optode 3830 SN:00219 depth/pressure data was at least partially derived and not directly measured, consult quality flags for detailsinstrument = Label:kpo_1201_07 File:kpo_1201_instr_07.nc Type:Seabird MicroCat 37-SM mit P SN:06863instrument = Label:kpo_1201_08 File:kpo_1201_instr_08.nc Type:Aanderaa Optode 3830 SN:00942 depth/pressure data was at least partially derived and not directly measured, consult quality flags for detailsinstrument = Label:kpo_1201_09 File:kpo_1201_instr_09.nc Type:Nortek Aquadopp Induktiv SN:P26209-03instrument = Label:kpo_1201_10 File:kpo_1201_instr_10.nc Type:McLane Profiler MMP SN:11617instrument = Label:kpo_1201_11 File:kpo_1201_instr_11.nc Type:Nortek Aquadopp Induktiv SN:P26209-06instrument = Label:kpo_1201_12 File:kpo_1201_instr_12.nc Type:Nortek Aquadopp Seriell SN:P25460-02instrument = Label:kpo_1201_13 File:kpo_1201_instr_13.nc Type:Seabird MicroCat 37-SM mit P SN:02485comment = flag_meaningscomment = 0:unknowncomment = 1:good_datacomment = 2:probably_good_datacomment = 3:potentially_correctable_bad_datacomment = 4:bad_datacomment = 5:not_usedcomment = 6:not_usedcomment = 7:nominal_value
DOI: 10.1594/pangaea.497480
title: Physical oceanography from BT during cruise U589900290B_1900
DOI: 10.1594/pangaea.924780
title: Physical oceanography from mooring KPO_1023

description: GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019).
description: instrument = Label:kpo_1023_02 File:kpo_1023_instr_02.nc Type:GEOMAR TD-Logger SN:58instrument = Label:kpo_1023_03 File:kpo_1023_instr_03.nc Type:Teledyne RDI QuarterMaster 150 SN:8237instrument = Label:kpo_1023_04 File:kpo_1023_instr_04.nc Type:Seabird MicroCat 37-SM SN:01284instrument = Label:kpo_1023_05 File:kpo_1023_instr_05.nc Type:Seabird MicroCat 37-SM SN:01286instrument = Label:kpo_1023_06 File:kpo_1023_instr_06.nc Type:Aanderaa Optode 3830 SN:00939instrument = Label:kpo_1023_07 File:kpo_1023_instr_07.nc Type:Seabird MicroCat 37-SM SN:01320instrument = Label:kpo_1023_08 File:kpo_1023_instr_08.nc Type:Aanderaa Optode 3830 SN:00942instrument = Label:kpo_1023_09 File:kpo_1023_instr_09.nc Type:Teledyne RDI LongRanger 75 SN:1181instrument = Label:kpo_1023_10 File:kpo_1023_instr_10.nc Type:Sontek Argonaut SN:144instrument = Label:kpo_1023_11 File:kpo_1023_instr_11.nc Type:Aanderaa RCM 8 SN:06122comment = flag_meaningscomment = 0:unknowncomment = 1:good_datacomment = 2:probably_good_datacomment = 3:potentially_correctable_bad_datacomment = 4:bad_datacomment = 5:not_usedcomment = 6:not_usedcomment = 7:nominal_value
DOI: 10.1594/pangaea.496814
title: Physical oceanography from BT during cruise K58XXB_1938
DOI: 10.1594/pangaea.874333
title: Survival of European sea bass post-larvae (Dicentrarchus labrax) after PHB administration