cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.977769
title: Water column raw data (Kongsberg EM 122 entire dataset) of RV SONNE during cruise SO308/1

description: Raw multibeam bathymetry data were collected aboard RV SONNE during cruise SO308 (GEOTRACES SIO) using a 12kHz Kongsberg EM 122 multibeam echosounder with 2x2 beam width. The expedition took place during 2024-10-31 – 2024-12-22 from Durban (South Africa) to Fremantle (Australia) in the South Indian Ocean. The main scientific aim of the cruise was to establish the distributions of trace elements and their isotopes (TEIs), quantify their sources from the four major ocean boundaries (rivers, atmosphere, exchange with sediments, ocean crust), and determine their biogeochemical cycling and relationships to large scale ocean circulation along a cruise track in the South Indian Ocean. Data were recorded in the EEZs of Mozambique, Europa Island (France), Bassas da India (France) and outside EEZs. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Data acquisition was done by GEOMAR Helmholtz Centre for Ocean Research, provision of the data is supported by the DAM Underway Project and published according to the FAIR principles.
description: Do not misuse data for exploitation reasons (e.g. fishing).Do not use for navigation.
DOI: 10.5281/zenodo.17836159
title: Raw data

description: Researcher
description: Raw data available to compute as statistic provided
DOI: 10.1594/pangaea.980741
title: Shipboard ADCP current measurements (38 kHz) during RV MARIA S. MERIAN cruise MSM130

description: Current velocities of the upper water column along the cruise track of R/V Maria S. Merian cruise MSM130 were collected by a vessel-mounted 38 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in two different configurations: 1) broadband mode (WM1) with a bin size of 16.00 m, a blanking distance of 16.00 m, and a total of 80 bins, 2) narrowband mode (WM10) with a bin size of 16.00 m, a blanking distance of 16.00 m, and a total of 80 bins. The depth range covered was from 38.0 m to 1302.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data processing included water track calibration of the misalignment angle (configuration 1: 0.5087° +/- 0.6034°, configuration 2: 0.5297° +/- 0.6703°) and scale factor (configuration 1: 0.9989 +/- 0.0101, configuration 2: 0.9966 +/- 0.0115) of the measured velocities. The velocity data were averaged in time using an average interval of 120 s (configuration 1) and 60 s (configuration 2). Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'. Furthermore, the time series of cell 1 to 7 (configuration 1) and cell 1 to 2 (configuration 2) are flagged as 'potentially correctable bad data' because of velocities biases most likely caused by transducer ringing.
DOI: 10.1594/pangaea.980762
title: Shipboard ADCP current measurements (75 kHz) during RV METEOR cruise M206

description: Current velocities of the upper water column along the cruise track of R/V Meteor cruise M206 were collected by a vessel-mounted 75 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 5.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 8.00 m, a blanking distance of 4.00 m, and a total of 100 bins, covering the depth range between 17.0 m and 809.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.2) was used for data post-processing. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline.Data processing included water track calibration of the misalignment angle (-46.3362° +/- 0.6125°) and scale factor (1.0051 +/- 0.0113) of the measured velocities. The velocity data were averaged in time using an average interval of 60 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.5281/zenodo.17836158
title: Raw data

description: Researcher
description: Raw data available to compute as statistic provided
DOI: 10.1594/pangaea.969313
title: Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV SONNE during cruise SO303

description: Raw multibeam bathymetry data were collected aboard RV SONNE during cruise SO303 BIOGIN using a 12 kHz Kongsberg EM 122 multibeam echosounder. The expedition took place during 21.01.2024 - 19.02.2024 from La Réunion (France) to Colombo (Sri Lanka) in the Indian Ocean. The aim of SO303 BIOGIN (BIOGeochemistry in the equatorial INdian Ocean and the northern Arabian Sea) was to to sample a transect from 15°S to 9°N at 67°30'E to 69°E to study the southern extent of the Arabian Sea oxygen minimum zone. Important note: Due to a political situation, the foregoing cruise SO302 had been cancelled and the expedition dates of SO303 shifted. Hence data that would have originally been within the time range of SO302 are now within SO303. See cruise report for further details. Data were recorded outside EEZs. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Data acquisition was done by University of Hamburg, provision of the data is supported by the DAM Underway Project and published according to the FAIR principles.
description: These data should not be used for navigational purposes.
DOI: 10.1594/pangaea.980751
title: Shipboard ADCP current measurements (38 kHz) during RV SONNE cruise SO308/1

description: Current velocities of the upper water column along the cruise track of R/V Sonne cruise SO308/1 were collected by a vessel-mounted 38 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 32.00 m, a blanking distance of 16.00 m, and a total of 50 bins, covering the depth range between 54.0 m and 1622.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.2) was used for data post-processing. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data processing included water track calibration of the misalignment angle (-0.0851° +/- 0.5905°) and scale factor (1.0027 +/- 0.0096) of the measured velocities. The velocity data were averaged in time using an average interval of 60 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.1594/pangaea.980752
title: Shipboard ADCP current measurements (75 kHz) during RV SONNE cruise SO308/1

description: Current velocities of the upper water column along the cruise track of R/V Sonne cruise SO308/1 were collected by a vessel-mounted 75 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 8.00 m, a blanking distance of 8.00 m, and a total of 100 bins, covering the depth range between 22.0 m and 814.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.2) was used for data post-processing. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data processing included water track calibration of the misalignment angle (-45.1182° +/- 0.7007°) and scale factor (0.9984 +/- 0.0105) of the measured velocities. The velocity data were averaged in time using an average interval of 60 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.1594/pangaea.937223
title: Multibeam bathymetry raw data (Kongsberg EM710 entire dataset) of RV METEOR during cruise M154/1

description: Multibeam bathymetry raw data was recorded in the Atlantic during cruise M154/1 that took place between 2019-04-03 and 2019-04-25. The data was collected using the ship's own Kongsberg EM 710. This data is part of the DAM (German Marine Research Alliance) project Underway Research Data. Sound velocity profiles (SVP) were applied on the data for calibration. SVP data from this cruise can be found here (https://doi.org/10.1594/PANGAEA.935598). Please see the cruise report for details.
description: These data should not be used for navigational purposes.
DOI: 10.1594/pangaea.969316
title: Water column raw data (Kongsberg EM 122 entire dataset) of RV SONNE during cruise SO303

description: Raw water column data were collected aboard RV SONNE during cruise SO303 BIOGIN using a 12 kHz Kongsberg EM 122 multibeam echosounder. The expedition took place during 21.01.2024 - 19.02.2024 from La Réunion (France) to Colombo (Sri Lanka) in the Indian Ocean. The aim of SO303 BIOGIN (BIOGeochemistry in the equatorial INdian Ocean and the northern Arabian Sea) was to to sample a transect from 15°S to 9°N at 67°30'E to 69°E to study the southern extent of the Arabian Sea oxygen minimum zone. Important note: Due to a political situation, the foregoing cruise SO302 had been cancelled and the expedition dates of SO303 shifted. Hence data that would have originally been within the time range of SO302 are now within SO303. See cruise report for further details. Data were recorded outside EEZs. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Data acquisition was done by University of Hamburg, provision of the data is supported by the DAM Underway Project and published according to the FAIR principles.
description: These data should not be used for navigational purposes.
DOI: 10.1594/pangaea.973610
title: Water column raw data (Kongsberg EM 122 entire dataset) of RV METEOR during cruise M204

description: Raw water column data were collected aboard RV METEOR during cruise M204 using a 12kHz Kongsberg EM 122 multibeam echosounder. The expedition took place during 2024-09-27 – 2024-10-20 from Bridgetown (Barbados) to Las Palmas (Spain) in the Central Atlantic. The major aims of M204 Transformers III is to gain new insights into the seismic activity and geological processes at this largely unexplored plate boundary.Data were recorded outside EEZ in international waters. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Data acquisition was done by GEOMAR Helmholtz Centre for Ocean Research, provision of the data is supported by the DAM Underway Project and published according to the FAIR principles.
description: These data should not be used for navigational purposes or exploitation.
DOI: 10.1594/pangaea.968509
title: Water column raw data (Kongsberg EM710 entire dataset) of RV METEOR during cruise M192/2

description: Raw water column data were collected aboard RV METEOR during cruise M192/2 using a 40-100kHz Kongsberg EM 710 multibeam echosounder. The expedition took place during 20.8.23 - 5.9.23 from Piraeus (Greece) to Limassol (Cyprus) in the Mediterranean Sea. The major aims of the second leg of the M192 BRIDGEHELL cruise was to systematically sample the hydrothermal vent areas identified during the first leg by multicorer, Van Veen grab and with the remotely operated vehicle ROV MARUM-SQUID. Data were recorded in the Greek EEZ. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Data acquisition was done by MARUM and the Faculty of Geology and Geo-Environment of University of Athens, provision of the data is supported by the DAM Underway Project and published according to the FAIR principles.
description: These data should not be used for navigational purposes.These data should not be used for exploitation, e.g. fishing.Data publishing was realised by Mia Schumacher, GEOMAR.
DOI: 10.1594/pangaea.974157
title: Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV SONNE during cruise SO307

description: Raw multibeam bathymetry data were collected aboard RV SONNE during cruise SO307 Madagaskar/Indico using a 12kHz Kongsberg EM 122 multibeam echosounder with 2x2 beam width. The expedition took place during 2024-09-12 – 2024-10-28 from Durban to Durban (South Africa) in the Indian Ocean. During the SONNE expedition SO307, scientific work was carried out for the geological main project (MADAGASCAR), a biological oceanography sub-project (INDICOM) and a biological sub-project (MADAGASCAR-BIO). The Madagascar Ridge (Southwest Indian Ocean) is ideal to explore the cause(s) of seafloor bathymetric anomalies, because it formed during the breakup of Gondwana, but the process behind its emplacement is controversial. Proposed origins include thinned continental crust, a hotspot-generated aseismic ridge or uplift due to buoyant, melt- depleted mantle. The overall aim of INDICOM is to investigate biological and biogeochemical processes that affect the turnover of organic matter in the deep Indian Ocean. The investigations of MADAGASCAR-Bio aim at: (1) Recording and describing the diversity of selected groups of the benthic communities of the Madagascar Ridge, (2) Uncovering cryptic species, (3) Testing the hypothesis about the function of oceanic ridges and their parallel running currents as corridors for the dispersal of benthic species, (4) Studying the availability of nutrients into the study area by sediment analyses ('total carbon', TC and 'total organic carbon', TOC). Data were recorded outside EEZs. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Data acquisition was done by GEOMAR Helmholtz Centre for Ocean Research, provision of the data is supported by the DAM Underway Project and published according to the FAIR principles.
description: These data should not be used for navigational purposes.
DOI: 10.1594/pangaea.965746
title: Water column raw data (Kongsberg EM712 entire dataset) of RV MARIA S. MERIAN during cruise MSM112

description: Raw water column data were collected aboard RV MARIA S. MERIAN during cruise MSM112 using a Kongsberg EM 712 multibeam echosounder. The expedition took place during 07.10.-14.11.2022 from St. John's (Canada) to Cartagena (Colombia) in the Northern and Central Atlantic Ocean. MSM112 focused on the geophysical, sedimentological, and biogeochemical processes of the delta and ROFI, and searched for connections of the river mouth to the La Guajira upwelling system. Sound velocity profiles (SVP) were applied on the data for calibration. Please see environmental data and the cruise report for details. The data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors may occur when no proper SVP is applied. Acquisition and provision of the data are part of the DAM Underway Project.
description: These data should not be used for navigational purposes.
DOI: 10.1594/pangaea.980759
title: Shipboard ADCP current measurements (38 kHz) during RV METEOR cruise M206

description: Current velocities of the upper water column along the cruise track of R/V Meteor cruise M206 were collected by a vessel-mounted 38 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 5.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 32.00 m, a blanking distance of 16.00 m, and a total of 55 bins, covering the depth range between 53.0 m and 1781.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.2) was used for data post-processing. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data processing included water track calibration of the misalignment angle (0.1421° +/- 0.6307°) and scale factor (1.0044 +/- 0.0111) of the measured velocities. The velocity data were averaged in time using an average interval of 60 s. Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'.
DOI: 10.17026/ar/epjnph
title: PAN-00110179 - coin/coin-related, Republiek, un centime

description: &lt;p&gt;This find is registered at Portable Antiquities of the Netherlands with number PAN-00110179&lt;/p&gt;
description: Modified: 2025-09-16T15:33:40+02:00
DOI: 10.1594/pangaea.980750
title: Shipboard ADCP current measurements (75 kHz) during RV MARIA S. MERIAN MSM130

description: Current velocities of the upper water column along the cruise track of R/V Maria S. Merian cruise MSM130 were collected by a vessel-mounted 75 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in two different configurations: 1) broadband mode (WM1) with a bin size of 8.00 m, a blanking distance of 8.00 m, and a total of 100 bins, 2) narrowband mode (WM10) with a bin size of 8.00 m, a blanking distance of 8.00 m, and a total of 100 bins. The covered depth range was 22.0 m to 814.0 m. Attitude data from the ship's motion reference unit were used by the data acquisition software VmDAS internally to convert ADCP beam velocities to geographic coordinates. The Python toolbox OSADCP (version 2.0.0) was used for data post-processing. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. Acoustic Interferences were identified based on outliers in the ADCP echo intensity data. Echo intensity data were cleaned accordingly and affected velocity cells were flagged to be removed prior ensemble-averaging. The ship's velocity was calculated from position fixes obtained by the Global Navigation Satellite System (GNSS), taking into account lever arms of ADCP transducer and GNSS antenna. Accuracy of the derived water velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data processing included water track calibration of the misalignment angle (configuration 1: -47.2542° +/- 0.5410°, configuration 2: -47.2217° +/- 0.7196°) and scale factor (configuration 1: 0.9983 +/- 0.0095, configuration 2: 0.9973 +/- 0.0134) of the measured velocities. The velocity data were averaged in time using an average interval of 120 s (configuration 1) and 60 s (configuration 2). Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'. Furthermore, the time series of cell 1 to 4 (configuration 1) and cell 1 to 6 (configuration 2) are flagged as 'potentially correctable bad data' because of velocities biases most likely caused by transducer ringing.
DOI: 10.1594/pangaea.948123
title: Master tracks in different resolutions of Maria S. Merian cruise MSM108, Tromsø - Tromsø, 2022-06-07 - 2022-07-02

description: Raw data acquired by position sensors on board RV MERIAN during expedition MSM108 were processed to receive a validated master track which can be used as reference of further expedition data. During MSM108 the motion reference unit Kongsberg SeaTex AS MRU-5 combined with Kongsberg SeaTex AS Seapath 320 and the GPS receivers Trimble SPS855 and SAAB R4 were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.bsh.de) with a resolution of 1 sec. Processing and evaluation of the data is outlined in the data processing report. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
description: This dataset contains the master track in 10 min resolution, for other resolutions please see "Further details" and "Other version" references.