cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.905813
title: Stable carbon isotopic composition of methane (δ¹³C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in core GeoB21613-1
DOI: 10.1594/pangaea.905814
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (δ¹³C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in core GeoB21616-1
DOI: 10.1594/pangaea.905815
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (δ¹³C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in core GeoB21621-1
DOI: 10.1594/pangaea.905849
title: Lowered ADCP data during METEOR cruise M96
DOI: 10.1594/pangaea.905855
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21601-1
DOI: 10.1594/pangaea.905856
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21605-1
DOI: 10.1594/pangaea.905857
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21610-1
DOI: 10.1594/pangaea.905858
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21612-1
DOI: 10.1594/pangaea.905859
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21613-1
DOI: 10.1594/pangaea.905860
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21619-1
DOI: 10.1594/pangaea.905861
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21621-1
DOI: 10.1594/pangaea.905869
title: Coral mound aggradation rate
DOI: 10.1594/pangaea.905874
title: Coral clast angle of sediment core GeoB18127-1
DOI: 10.1594/pangaea.905875
title: Coral clast size of sediment core GeoB18127-1
DOI: 10.1594/pangaea.905876
title: Coral content of sediment core GeoB18127-1
DOI: 10.1594/pangaea.905877
title: Coral clast angle of sediment core GeoB18130-1
DOI: 10.1594/pangaea.905371
title: Stable isotope record of benthic foraminifera of sediment cores M125-55-7/8
DOI: 10.1594/pangaea.905878
title: Coral clast size of sediment core GeoB18130-1
DOI: 10.1594/pangaea.905879
title: Coral content of sediment core GeoB18130-1
DOI: 10.1594/pangaea.905372
title: Mg/Ca ratios and SST reconstruction from sediment cores M125-55-7/8
DOI: 10.1594/pangaea.905373
title: Stable isotope record of planktonic foraminifera of sediment cores M125-55-7/8
DOI: 10.1594/pangaea.905374
title: Seawater stable oxygen isotope reconstruction from sediment cores M125-55-7/8
DOI: 10.1594/pangaea.905375
title: Sedimentation rates of sediment cores M125-55-7/8
DOI: 10.1594/pangaea.905413
title: Bulk parameters determined in sediment core PS93/025
DOI: 10.1594/pangaea.905608
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS118
DOI: 10.1594/pangaea.905610
title: Continuous thermosalinograph oceanography along POLARSTERN cruise track PS119
DOI: 10.1594/pangaea.905697
title: M70/3 raw data of EM120 multibeam echosounder (bathymetry & beam time series)

description: Between 26.11.2006 and 08.12.2006, bathymetric data was acquired in the Eastern Mediterranean Sea during the R/V METEOR cruise M70/3, which was aimed at key processes at cold seeps in the Anaximander Mountains south of Turkey. The cruise addressed factors controlling fluid escape at cold seeps, precipitates and their mineral composition, the quantification of gas and gas hydrates that exist in the sediments or escape as gas bubbles into the water column, as well as seep-related ecology. The multibeam echosounder (MBES) SIMRAD EM120 was utilized to survey the working area and produce detailed bathymetric maps, specifically of the mud volcanoes. Furthermore, hydroacoustic mapping provided the basis for dive planning of the Remotely Operated Vehicle (ROV) MARUM-QUEST and flare-imaging profiles with the sub-bottom profiler PARASOUND. Further sampling was carried out with the moving lander MOVE, an Autoclave tool and several sediment coring devices.CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval.Description of the data source:During the M70/3 cruise, the hull-mounted SIMRAD 120 multibeam ecosounder (MBES) was utilized to perform bathymetric mapping, which transmits a nominal sounding frequency of 12 kHz. During the cruise, the opening angle of the multibeam echosounder was set to 140° (for one profile 150°). The 191 generated beams were set to yield an equidistant spacing on the seafloor and yaw correction was applied. For further information, contact: https://www.kongsberg.com/maritime/support/During large scale surveys, the ship speed was 8 knots. For detailed surveying of mud volcanoes, the beam angle was adjusted to cover a swath width of about one nautical mile on the seafloor and ship speed was reduced to 5 knots. The EM120 was running during station work and ROV dives as long as it did not disturb the flare detection of the sub-bottom profiler. A sound velocity profile generated from the Levitus database was applied. The depth of the water column is estimated through the two-way-travel time, beam angle and ray bending due to refraction in the water column by sound speed variations.Responsible person during this cruise / PI: Markus BrüningChief Scientist: Gerhard Bohrmann (gbohrmann@marum.de)CR: https://www.tib.eu/en/search/id/awi%3Adoi~10.2312%252Fcr_m70/CSR: https://www2.bsh.de/aktdat/dod/fahrtergebnis/2006/20060222.htm
DOI: 10.1594/pangaea.905713
title: Sea ice drift, surface temperature, barometric pressure, humidity, wind speed and wind direction from autonomous measurements from buoy 2018A2, deployed during AKADEMIK TRYOSHNIKOV cruise TRANSDRIFT XXIV (TICE)

description: Sea ice drift, surface temperature, barometric pressure, humidity, wind speed and wind direction were measured by the Polar Area Weather Station (PAWS) 2018A2 drifting on Arctic sea ice. The buoy was deployed on multi year ice during AKADEMIK TRYOSHNIKOV cruise TRANSDRIFT XXIV (TICE). The time series describes the position and additional parameters of the buoy between 13 Sep 2018 and 15 Oct 2018 in sample intervals of 3 hours. The data set has been processed, including the removal of obvious inconsistencies (missing values).
DOI: 10.1594/pangaea.905725
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2018S76, deployed during AKADEMIK TRYOSHNIKOV cruise TRANSDRIFT XXIV (TICE)

description: Snow height was measured by the Snow Depth Buoy 2018S76, an autonomous platform, drifting on Arctic sea ice, deployed during AKADEMIK TRYOSHNIKOV cruise TRANSDRIFT XXIV (TICE). The resulting time series describes the evolution of snow depth as a function of place and time between 15 September 2018 and 27 April 2019 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on multi year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.905768
title: Physical properties of sediments and stable carbon isotopic composition of organic matter in core GeoB21605-1
DOI: 10.1594/pangaea.905769
title: Physical properties of sediments and stable carbon isotopic composition of organic matter in core GeoB21612-1
DOI: 10.1594/pangaea.905770
title: Physical properties of sediments and stable carbon isotopic composition of organic matter in core GeoB21613-1
DOI: 10.1594/pangaea.905771
title: Physical properties of sediments and stable carbon isotopic composition of organic matter in core GeoB21616-1
DOI: 10.1594/pangaea.905772
title: Physical properties of sediments and stable carbon isotopic composition of organic matter in core GeoB21619-1
DOI: 10.1594/pangaea.905773
title: Physical properties of sediments and stable carbon isotopic composition of organic matter in core GeoB21621-1
DOI: 10.1594/pangaea.905774
title: Physical properties of sediments and stable carbon isotopic composition of organic matter in core GeoB21637-1
DOI: 10.1594/pangaea.905793
title: M74/2 raw data of EM120 multibeam echosounder (bathymetry & beam time)

description: Between 07.10.2007 and 28.10.2007, bathymetric data was acquired in the Makran region during the R/V METEOR cruise M74/2. The subduction of the Eurasian plate beneath the Arab plate in the Makran Region is associated with continuous sediment input, active mud volcanism and fluid venting. The expedition was dedicated to the investigation of known seeps and the location of new venting sites. Furthermore, the scientists focused on the influence of extreme sediment thickness on the nature of vents and the relationship between local tectonics and spatial distribution of seeps. The multibeam echosounders (MBES) KONGSBERG SIMRAD EM120 and EM710 were utilized for large-scale mapping of vent-related structures on the seafloor. In order to visualize vent-related structures in the shallow subsurface, a deep-tow sidescan sonar, sediment echosounder and high resolution multichannel equipment were utilized. These acoustic methods were supplemented by video observations, gravity corer and multicorer samples, which yielded detailed information at many locations.CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval.Description of the data source:During the M74/2 cruise, the hull-mounted KONGSBERG SIMRAD EM120 multibeam ecosounder (MBES) was utilized to perform bathymetric mapping. The system covers full ocean depth and transmits a nominal sounding frequency of 12 kHz. It generates 191 beams with a 1°(Tx)/2°(Rx) footprint and a maximum opening angle of 140°. For further information consult: https://epic.awi.de/26725/1/Kon2007a.pdfThe acquisition mode was set to obtain equally spaced soundings on the sea floor. Yaw movements of the ship were compensated automatically by transmitting the swath perpendicular to the track rather than to the ship's axis. The opening angle was limited by either the maximum angle possible, a maximum angle set or a maximum coverage on the sea floor. Those values were adjusted to the requirements of the special surveys. For TOBI lines, which were 5.5 km apart, coverage was limited to obtain overlap at the edges of profiles. During transits in areas, which were covered before by the SIMRAD, swath widths were usually 6 km wide, on surveys over areas covered by data from previous cruises 7 km. Where no data were available at all, the full opening angle of 140° was set. Ship speed varied between 2.5 kn during TOBI profiles, 5 kn during seismic profiling, 8 kn for bathymetric surveys, and up to 12 kn during transits. A sound velocity profile for the cruise was delivered during the first CTD station. The depth of the water column is estimated through the two-way-travel time, beam angle and ray bending due to refraction in the water column by sound speed variations.Responsible person during this cruise / PI: Markus BrüningChief Scientist: Volkhard Spiess (vspiess@uni-bremen.de)CR: https://www.tib.eu/en/search/id/awi%3Adoi~10.2312%252Fcr_m74/CSR: https://www2.bsh.de/aktdat/dod/fahrtergebnis/2007/20080085.htm
DOI: 10.1594/pangaea.905801
title: Stable carbon isotopic composition of methane (δ¹³C-CH4) in core GeoB21601-1
DOI: 10.1594/pangaea.905802
title: Stable carbon isotopic composition of methane (δ¹³C-CH4) in core GeoB21605-1
DOI: 10.1594/pangaea.905803
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (δ¹³C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in core GeoB21609-2
DOI: 10.1594/pangaea.905805
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (δ¹³C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in core GeoB21612-1
DOI: 10.1594/pangaea.905808
title: Hydrocarbon composition (C1/(C2-C5), stable carbon isotopic composition of methane (δ¹³C-CH4), and stable hydrogen isotopic composition of methane (d2H-CH4) in core GeoB21619-1
DOI: 10.1594/pangaea.905810
title: Hydrocarbon composition (C1/(C2-C5) and stable carbon isotopic composition of methane (δ¹³C-CH4) in core GeoB21637-1
DOI: 10.1594/pangaea.905811
title: Stable carbon isotopic composition of methane (δ¹³C-CH4) in core GeoB21638-1
DOI: 10.1594/pangaea.905812
title: Hydrocarbon composition (C1/(C2-C5) and stable carbon isotopic composition of methane (δ¹³C-CH4) in core GeoB21610-1
DOI: 10.1594/pangaea.905172
title: Isoprene concentrations in the surface South Atlantic waters during during Marion Dufresne cruise MD160 (OOMPH MD07 leg 2) in March 2007

description: Isoprene concentrations in the surface South Atlantic waters, measured during the OOMPH (Leg 2) cruise in March 2007 on board the R/V Marion Dufresne. Measurements were made on-line with water extracted from the "ship's membrane pump" (~8m under the surface).
description: #0.00 = below detection limit
DOI: 10.1594/pangaea.905212
title: CARD-FISH cell counts of taxonomic bacterial and archaeal groups in Fram Strait during PS99.2

description: With CARD-FISH we quantified 16 microbial taxonomic groups in different water depths, from surface to the deep sea. We investigated 11 stations in LTER-HAUSGARTEN and adjacent stations in Fram Strait.
DOI: 10.1594/pangaea.905244
title: Seismic refraction data from the Mid-Cayman-Spreading-Centre from profiles P05 and P06 during METEOR cruise M115 with links to data files

description: Seismic profiles p05 and p06 were shot during the cruise M115 of the German RV METEOR in the vicinity of the Mid-Cayman-Spreading-Centre off the median valley in flow line direction of seafloor spreading. Shots fired with a seismic airgun array (volume 5250 cubic-inch) towed behind the METEOR were recorded at Ocean-Bottom-Seismometers (OBS) and Ocean-Bottom-Hydrophones (OBH). Here, segy-data of all OBS and OBH providing data for geophysical data analyis are presented.
description: List of shot positions contain: Longitude, Latitude, Profile Number, Shot Number, Depth, water [m]
description: Supplement to: Grevemeyer, Ingo; Hayman, Nicholas W; Peirce, Christine; Schwardt, Michaela; van Avendonk, Harm; Dannowski, Anke; Papenberg, Cord (2018): Episodic magmatism and serpentinized mantle exhumation at an ultraslow-spreading centre. Nature Geoscience, 11(6), 444-448
DOI: 10.1594/pangaea.905300
title: Age model of sediment cores M125-55-7/8
DOI: 10.1594/pangaea.905886
title: Stable carbon isotopic composition of dissolved inorganic carbon (δ¹³C-DIC) in sediment core GeoB21637-1
DOI: 10.1594/pangaea.905895
title: Stable oxygen and carbon isotope from mixed benthic foraminifera Cibicoides mundulus and Cibicoides pachyderma of sediment core GeoB18131-1
DOI: 10.1594/pangaea.905896
title: Stable oxygen and carbon isotope from the benthic foraminfiera C. mundulus and C. pachydrema of sediment core GeoB18131-1
DOI: 10.1594/pangaea.905897
title: Mean grain size of sediment core GeoB18131-1
DOI: 10.1594/pangaea.905900
title: Benthic foraminifera accumulation rate of sediment core GeoB18131-1
DOI: 10.1594/pangaea.905903
title: Stable carbon isotopes of C. kullenbergi from sediment core GeoB13731-1
DOI: 10.1594/pangaea.905988
title: Sortable silt records of sediment core PS97/093-2
DOI: 10.1594/pangaea.905994
title: High resolution sortable silt records of sediment core PS97/093-2
DOI: 10.1594/pangaea.906081
title: Clay minerals of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.905996
title: Ca, Fe, Ti, K measurement and Zr/Rb ratios of sediment core PS97/093-2
DOI: 10.1594/pangaea.906082
title: C/N ratio of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906479
title: Hydrochemistry of water samples from SONNE cruise SO241
DOI: 10.1594/pangaea.906083
title: Grain size distribution of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906084
title: Halite concentration of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906085
title: Iron carbonate concentration of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906481
title: Porewater geochemistry of sediment cores from SONNE cruise SO241
DOI: 10.1594/pangaea.906087
title: Sr and Nd isotopic record of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906088
title: Palaeomagnetism of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906089
title: Pollen groups record of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906504
title: Geochemistry of sediment cores from SONNE cruise SO241
DOI: 10.1594/pangaea.906091
title: TOC concentration of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906099
title: Documentation of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.906890
title: Heterocyst glycolipids and SWT reconstruction of sediment cores 9R and 10R at site PS104_20-2
DOI: 10.1594/pangaea.907389
title: Trace metal concentration from surface water samples of METEOR cruise M116
DOI: 10.1594/pangaea.907393
title: Incubation experiments during METEOR cruise M116
DOI: 10.1594/pangaea.907748
title: Macrofauna abundance and biomass at the LTER observatory HAUSGARTEN in 2016

description: Macrofauna data was collected using a box corer (0.25m² sampling area). The sampled sediment from each box corer was divided into eight subsamples (pseudoreplicates). The uppermost 12 cm of these subsamples were analyzed. Each subsample was processed through a 500-µm mesh size sieve. After sieving, residuals were fixed with 100% ethanol and stored at room temperature. Macrofaunal organisms were identified to the lowest possible taxonomical level. Whenever identification to species level was not possible, the sample was identified to the next identifiable taxonomical category and assigned a putative species name (e.g., 'Hesionidae genus sp. 1', 'Hesionidae genus sp. 2'). Posterior fragments, exuviae, xenobionts, meiofauna taxa (Nematoda, Ostracoda, Harpacticoida) and empty tubes were excluded from the analysis. Biomass (blotted wet weight, ww) was determined by weighing each specimen. Shelled organisms, such as mollusks, were weight in their shells.
description: Supplement to: Käß, Melissa; Vedenin, Andrey; Hasemann, Christiane; Brandt, Angelika; Soltwedel, Thomas (2019): Community structure of macrofauna in the deep Fram Strait: A comparison between two bathymetric gradients in ice-covered and ice-free areas. Deep Sea Research Part I: Oceanographic Research Papers, 103102
DOI: 10.1594/pangaea.907764
title: Surface oceanographic data (TSG) during METEOR cruise M116/1

description: Temp Sensor ID 1 = THERMOSALINOGRAPH TSTempSecondary Spot °CTemp Correction 1 = -0.0027463Temp Uncertainty 1 = +/-0.0034895Temp Sensor ID 2 = Weather WaterTempPort Spot °CTemp Correction 2 = 0.071896Temp Uncertainty 2 = +/-0.017842Temp Sensor ID 3 = Weather WaterTempStarboard Spot °CTemp Correction 3 = 0.13168Temp Uncertainty 3 = +/-0.024874Temp Sensor ID 4 = THERMOSALINOGRAPH TsTempPrimary Spot °CTemp Correction 4 = -0.1548Temp Uncertainty 4 = +/-0.0049359Salt Sensor ID 1 = THERMOSALINOGRAPH TsSalinityPri Spot PSUSalt Correction 1 = 0.0078439+7.3755e-05*tim+3.7246e-05*tim.*timSalt Uncertainty 1 = +/-0.00074428Comment = The above calibrations have been added to the raw data.Comment = Multiple calibrations for a single sensor are valid only for the times given in Range.Comment = The calibration time data 'tim' and the time ranges have been referenced to the Expocode date for this cruise is 736085 in Matlab datenum.The data has been compared with CTD data from 5 dbar .
DOI: 10.1594/pangaea.908073
title: HCRF measurements (Ibsen Freedom VIS FSV-305) of bare Arctic sea ice acquired during POLARSTERN cruise PS106/2

description: This dataset contains HCRF measurements of a bare ice surface acquired during RV POLARSTERN cruise PS106.2 with a transportable field goniometer (see photo goniometer.jpg) and an Ibsen Freedom VIS FSV-305. The goniometer has been built and designed at German Aerospace Center (DLR) Oberpfaffenhofen by Thomas Schwarzmaier, Stefan Plattner and Peter Gege.The data has been acquired under clear sky conditions.The folder contains two subfolders:1) raw: raw measurements of dark current, reference (spectralon panel at nadir) and target (bare ice surface under different viewing and azimuth angles). Reference spectra were taken for every azimuth angle. 2) reflectance: reflectance data computed from the raw measurements (associated raw files are documented in each reflectance file) including information about sun and viewing zenith and azimuth angles.
DOI: 10.1594/pangaea.907866
title: CTD measurements in Vema channel of the Atlantic Ocean in 2017
DOI: 10.1594/pangaea.907140
title: Grain size and bulk composition of ocean sediments between South America and the Antarctic Peninsula
DOI: 10.1594/pangaea.907872
title: CTD measurements in Vema Fracture Zone of the Atlantic Ocean in 2006
DOI: 10.1594/pangaea.907143
title: Bulk mineral XRD peak ratios of ocean sediments between South America and the Antarctic Peninsula
DOI: 10.1594/pangaea.907144
title: Silt fraction mineral XRD peak ratios of ocean sediments between South America and the Antarctic Peninsula
DOI: 10.1594/pangaea.907145
title: Clay mineral data of ocean sediments between South America and the Antarctic Peninsula
DOI: 10.1594/pangaea.907147
title: Sortable silt data of ocean sediments between South America and the Antarctic Peninsula
DOI: 10.1594/pangaea.907913
title: CTD measurements in Vema Fracture Zone of the Atlantic Ocean in April 2016
DOI: 10.1594/pangaea.907914
title: CTD measurements in Vema Fracture Zone of the Atlantic Ocean in October 2016
DOI: 10.1594/pangaea.907933
title: LADCP measurements in Vema Channel of the Atlantic Ocean in 2017

description: Stations 2685, 2686, 2687: for technical reasons, data contain only the bottom part of the profile
DOI: 10.1594/pangaea.907962
title: LADCP measurements in Vema Fracture Zone of the Atlantic Ocean in 2006
DOI: 10.1594/pangaea.907965
title: LADCP measurements in Vema Fracture Zone of the Atlantic Ocean in April 2016
DOI: 10.1594/pangaea.907592
title: Bottom Pressure Records and current velocities from mooring KPO_1106

description: instrument = Label:kpo_1106_01 File:kpo_1106_instr_01.nc Type:Teledyne RDI LongRanger 75 SN:19397instrument = Label:kpo_1106_02 File:kpo_1106_instr_02.nc Type:Seabird SBE26plus 26plus SN:1356Flags0:unknown1:good_data2:probably_good_data3:potentially_correctable_bad_data4:bad_data5:not_used6:not_used7:nominal_value8:interpolated_value9:missing_value
DOI: 10.1594/pangaea.907966
title: LADCP measurements in Vema Fracture Zone of the Atlantic Ocean in October 2016
DOI: 10.1594/pangaea.908174
title: (Table 1) Boron concentrations and isotope ratios together with previously reported chemical and physical parameter in hydrothermal fluids and acid-sulfate fluids

description: a: Previously reported by: Tivey et al., 2006; Craddock et al., 2010; Reeves et al., 2011 ; Seewald et al (2015) for fluids from Manus Basin collected in 2006; Bach et al., 2011 and unpublished data for fluids from the EMVZ collected in 2011 and Schmidt et al., 2017 for vent fluids from Nifonea volcano.
DOI: 10.1594/pangaea.908181
title: (Table 3) SiO2, TiO2 and B concentrations and isotope ratios of fresh and altered rocks from Nifonea volcano and the Eastern Manus Volcanic Zone

description: *: Fresh volcanic rocks from the Manus Basin were previously reported by Beier et al. (2015), and fresh volcanic rocks from Nifonea volcano by Lima et al. (2017), uncertainties for B concentrations are smaller than 5% (2SD).