cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25582/data.2022-07.2556062/2116822
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558023/2116823
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2554811/2116824
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558096/2116825
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2557191/2116826
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2557133/2116827
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2555659/2116828
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558068/2116829
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2555561/2116830
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2554267/2116831
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2556253/2116832
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2555721/2116833
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2554512/2116834
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2557495/2116835
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2552570/2116836
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2555890/2116837
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2554785/2116838
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558127/2116839
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2557403/2116840
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2556086/2116841
title: Data for EMSL Project 51287 from July 2022
DOI: 10.6084/m9.figshare.22579684
title: Supplementary materials for: Sidorov 2023

description: <b>Supplementary materials for: Sidorov, 2023, Trans-Japan Sea land-bridge disjunction: A case of vicariance in the </b><b>subterranean genus Nipponasellus (Crustacea, Isopoda, Asellidae) in a large-</b><b>scale biogeographical context. Zootaxa 5357 (3): 342–374. doi: https://doi.org/10.11646/zootaxa.5357.3.2</b><br>SUPPLEMENTARY FILE 1. Characteristics of groundwater sampling sites in Primorye in 2009-2010.SUPPLEMENTARY FILE 2. Geolocation information.SUPPLEMENTARY FILE 3. Additional information about the literature survey and geographic distribution data of <i>Asellus</i>, <i>Calasellus</i>-<i>Columbasellus</i> and <i>Caecidotea</i>-<i>Proasellus</i> macro-groups on Figure 2.SUPPLEMENTARY FILE 4. SEM microphotographs displaying relevant morphological features of a new species.SUPPLEMENTARY FILE 5. Taxonomic list of macro- and meiofauna found in this study, and stations (sample codes as in Electronic Supplement 1) where it was collected, with the available data on species distributional ecology.SUPPLEMENTARY FILE 6. NEXUS file including character matrix for Asellidae used in analysis.--scripts.zip other supporting materials
DOI: 10.6084/m9.figshare.22579684.v1
title: Supplementary materials for: Sidorov 2023

description: <b>Supplementary materials for: Sidorov, 2023, Trans-Japan Sea land-bridge disjunction: A case of vicariance in the </b><b>subterranean genus Nipponasellus (Crustacea, Isopoda, Asellidae) in a large-</b><b>scale biogeographical context. Zootaxa 5357 (3): 342–374. doi: https://doi.org/10.11646/zootaxa.5357.3.2</b><br>SUPPLEMENTARY FILE 1. Characteristics of groundwater sampling sites in Primorye in 2009-2010.SUPPLEMENTARY FILE 2. Geolocation information.SUPPLEMENTARY FILE 3. Additional information about the literature survey and geographic distribution data of <i>Asellus</i>, <i>Calasellus</i>-<i>Columbasellus</i> and <i>Caecidotea</i>-<i>Proasellus</i> macro-groups on Figure 2.SUPPLEMENTARY FILE 4. SEM microphotographs displaying relevant morphological features of a new species.SUPPLEMENTARY FILE 5. Taxonomic list of macro- and meiofauna found in this study, and stations (sample codes as in Electronic Supplement 1) where it was collected, with the available data on species distributional ecology.SUPPLEMENTARY FILE 6. NEXUS file including character matrix for Asellidae used in analysis.--scripts.zip other supporting materials
DOI: 10.25582/data.2022-07.2555469/2116842
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2555410/2116843
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2554810/2116844
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2552819/2116845
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2555536/2116846
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2554765/2116847
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558208/2116848
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558017/2116849
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2557212/2116850
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558555/2116851
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2558229/2116852
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2555465/2116853
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2557653/2116854
title: Data for EMSL Project 51287 from July 2022
DOI: 10.25582/data.2022-07.2556767/2116855
title: Data for EMSL Project 51287 from July 2022
DOI: 10.1594/pangaea.757577
title: Physical oceanography measurements at the Håkon Mosby mud volcano (LOOME)

description: The deployment of LOOME was performed by lowering the LOOME frame by winch, followed by positioning of the surface sensors across the most active site by ROV. The frame was placed on an inactive slab of hydrates, eastwards and adjacent to the hot spot. As part of the LOOME-frame Sun & Sea multi parameter probe CTD 60M was deployed approximately 3 m above the seafloor. The device was rated to 2000 m water depth. As energy supply a DeepSea Power & Light SeaBattery (12V) was used, which allows a run time of the CTD 60M of more than a year. The memory capacity of the probe is sufficient to allow data storage for more than a year as well, applying a time resolution of better than one measurement per minute. The probe was configured to start running when the energy supply is connected and a magnetic switch is closed. An LED on top of CTD is indicating the current state of the probe. The major aim was to record the temperature and pressure regime in the bottom water at the Håkon Mosby Mud Volcano.
description: Depth calculated from pressure.
DOI: 10.1594/pangaea.757579
title: Chemical sensor measurements at the sediment surface of the Håkon Mosby mud volcano (LOOME)

description: Six sensor units each having a pH, dissolved oxygen (DO) and oxidation reduction potential (ORP) sensor, plus a central logger, and connection cables were purchased from RBR (Ottawa). The sensing loggers were placed at a transect across the hot spot. Unfortunately, 5 of the 7 loggers were drowned. Only the central logger, that collected the data from the 6 sensor loggers, and one of the sensor loggers remained dry and functional. The sensor was positioned at 50 m south of the frame, in the center of the hot spot. The ORP did not show interpretable signals. The DO and pH signals showed good correlation (. At the end of October 2009 both signals decreased, the pH became as low as 4, possibly indicating increased seepage, or burial in expelled sediments. In December both sensors regained seawater values and then decreased again until the end of May 2010. A pH of 4 can only be reached by very high carbondioxide levels. The dynamics of the signals indicate eruptions and sediment movements from October 2009 till the end of the deployment.
DOI: 10.1594/pangaea.757632
title: Sediment temperatures of the Håkon Mosby mud volcano measured continuously with a long temperature lance (LOOME)

description: The Ifremer T-lance comprises of a coring pipe (outer diameter of 0.115 m) on which in total of 7 temperature sensors (NKE-THP) had been attached. Please note, a complementary upper probe (lest probe ) was attached above the weight of the corer (275 kg, outer diameter of 0.365 m) was intended for bottom water temperature monitoring during the duration of the experiment. However, it was actually driven into the sediment down to an estimated sub-bottom depth of 6.7 m due to over-penetration into soft crater mud. The coring pipe had a plug at its lower end, preventing mud penetration into the pipe. After the recovery of the T-lance, it was checked that there was no mud in the pipe. The T-Lance was deployed at the seafloor at the 26.07.2009 (N 72.0041 E 014.726833,) and recovered at the 30.09.2010 (N 72.0026 E 014.72685). The difference between the two positions is approximately 160 m and the instrument had been moved towards south by mud flows. The temperature probes measured and recorded data every 30 minutes over a time period of 430 days 21 hours 30 minutes, resulting into a total number of 20684 single measurements.
DOI: 10.1594/pangaea.758001
title: Basic measurements of radiation at station Lindenberg (2005-02)
DOI: 10.1594/pangaea.757461
title: Sediment temperatures of the Håkon Mosby mud volcano measured continuously with a short temperature lance (LOOME)

description: The short sediment temperature probe were deployed and recovered with the LOOME observatory in 2009 and 2010, respectively. In addition to temperature, the loggers also recorded bottom water pressure at a sampling interval of 20 minutes. Even though the data obtained from the short temperature probe was strongly disturbed by leakage through a corroded connector, the data shows clearly that the probe was pulled out of the sediment on October 26, 2009, presumably by advancing mud flows.
DOI: 10.1594/pangaea.758006
title: Basic measurements of radiation at station Lindenberg (2005-03)
DOI: 10.1594/pangaea.757662
title: Temperatures at the sediment surface of the Håkon Mosby mud volcano measured continuously with a thermistor string (LOOME)

description: The seabed thermistor string was deployed and recovered with the LOOME observatory in 2009 and 2010, respectivly. In addition to temperature, the loggers also recorded bottom water pressure at a sampling interval of 20 minutes. All 24 channels of the seabed thermistor string worked without failure during the entire observation. The data shows numerous small events recorded by individual sensors as well as a few larger scale events detected by several neighboring sensors.
DOI: 10.1594/pangaea.760630
title: Basic measurements of radiation at station Lindenberg (1998-03)
DOI: 10.1594/pangaea.758583
title: Basic measurements of radiation at station Lindenberg (2005-05)
DOI: 10.1594/pangaea.758588
title: Basic measurements of radiation at station Lindenberg (2005-06)
DOI: 10.1594/pangaea.758593
title: Basic measurements of radiation at station Lindenberg (2005-07)
DOI: 10.1594/pangaea.758598
title: Basic measurements of radiation at station Lindenberg (2005-08)
DOI: 10.1594/pangaea.758011
title: Basic measurements of radiation at station Lindenberg (2005-04)
DOI: 10.1594/pangaea.760633
title: Basic measurements of radiation at station Lindenberg (1999-03)
DOI: 10.1594/pangaea.760636
title: Basic measurements of radiation at station Lindenberg (2000-03)
DOI: 10.1594/pangaea.760639
title: Basic measurements of radiation at station Lindenberg (2001-03)
DOI: 10.1594/pangaea.760722
title: Basic measurements of radiation at station Lindenberg (1996-03)
DOI: 10.1594/pangaea.760725
title: Basic measurements of radiation at station Lindenberg (1997-03)
DOI: 10.1594/pangaea.761317
title: Basic measurements of radiation at station Lindenberg (2006-05)
DOI: 10.1594/pangaea.761322
title: Basic measurements of radiation at station Lindenberg (2006-06)
DOI: 10.1594/pangaea.761327
title: Basic measurements of radiation at station Lindenberg (2006-07)
DOI: 10.1594/pangaea.761333
title: Basic measurements of radiation at station Lindenberg (2006-08)
DOI: 10.1594/pangaea.761338
title: Basic measurements of radiation at station Lindenberg (2006-09)
DOI: 10.1594/pangaea.761344
title: Basic measurements of radiation at station Lindenberg (2006-10)
DOI: 10.1594/pangaea.761349
title: Basic measurements of radiation at station Lindenberg (2006-11)
DOI: 10.1594/pangaea.761489
title: Basic measurements of radiation at station Lindenberg (2006-12)
DOI: 10.1594/pangaea.778343
title: Basic measurements of radiation at station Lindenberg (2005-12)
DOI: 10.1594/pangaea.779132
title: FerryBox measurements at the Namibian upwelling system during the Africana II cruise AFR258
DOI: 10.1594/pangaea.779133
title: Nutrients measured with a FerryBox at Namibian upwelling system during the Africana II cruise AFR258
DOI: 10.1594/pangaea.779134
title: FerryBox measurements at the Namibian upwelling system during Discovery 356
DOI: 10.1594/pangaea.779135
title: FerryBox measurements at the Namibian upwelling system during Maria S. Merain cruise MSM17/3
DOI: 10.1594/pangaea.761278
title: Basic measurements of radiation at station Lindenberg (2005-09)
DOI: 10.1594/pangaea.761287
title: Basic measurements of radiation at station Lindenberg (2005-10)
DOI: 10.1594/pangaea.761292
title: Basic measurements of radiation at station Lindenberg (2005-11)
DOI: 10.1594/pangaea.761297
title: Basic measurements of radiation at station Lindenberg (2006-01)
DOI: 10.1594/pangaea.761302
title: Basic measurements of radiation at station Lindenberg (2006-02)
DOI: 10.1594/pangaea.761307
title: Basic measurements of radiation at station Lindenberg (2006-03)
DOI: 10.1594/pangaea.761312
title: Basic measurements of radiation at station Lindenberg (2006-04)
DOI: 10.1594/pangaea.773204
title: Chlorophyll pigments from the Namibian upwelling system during Discovery 356

description: Chlorophyll-a data from the cruise number D-356 with research vessel "Discovery" from 10.9.-13.10.2010 in front of Namibia. Samples taken by CTD- rosette sampler from different depths. Filtration through GF/F filters immediately on board, filters frozen, transported to the institute.Procedure as described by WASMUND et al. (2006, http://www.iopan.gda.pl/oceanologia/481wasmu.pdf). However, a new fluorometer was used which measured according to the principle of WELSCHMEYER (1994, http://www.jstor.org/stable/2838404). Therefore, the chlorophyll a data were corrected for chlorophyll b, but not for pheopigments.Formula:Chl.a-tot [mg*m-3] = F0 * KX * VE * VPr**-1KX = linear calibration factor [µg chl.a/L per fluorescence unit]F0 = rel. fluorescenceVE = extraction volume [ml]VPr = filtration volume of the sample [ml]
DOI: 10.1594/pangaea.779586
title: Biogeochemical characteristics of the Northern Benguela upwelling system with emphasis on the carbonate system and nutrient dynamics during AFR258
DOI: 10.1594/pangaea.779634
title: Biogeochemical characteristics of the Northern Benguela upwelling system with emphasis on the carbonate system and nutrient dynamics during Discovery 356
DOI: 10.1594/pangaea.779638
title: Biogeochemical characteristics of the Northern Benguela upwelling system with emphasis on the carbonate system and nutrient dynamics during Discovery MSM17/3
DOI: 10.1594/pangaea.810723
title: Single cell abundances of Håkon Mosby mud volcano sediments measured at station MSM16/2_823-1 (Sample 9, old flow surface)
DOI: 10.1594/pangaea.810724
title: Single cell abundances of Håkon Mosby mud volcano sediments measured at station MSM16/2_838-1 (Sample 3, new flow surface)
DOI: 10.1594/pangaea.810725
title: Single cell abundances of Håkon Mosby mud volcano sediments measured at station MSM16/2_847-1 (Sample 5, aged flow surface)
DOI: 10.1594/pangaea.810726
title: Single cell abundances of Håkon Mosby mud volcano sediments measured at station MSM16/2_855-1 (Sample 6, aged flow surface)
DOI: 10.1594/pangaea.810728
title: Single cell abundances of Håkon Mosby mud volcano sediments measured at station PS74/168-1 (Sample 2, new flow surface)
DOI: 10.1594/pangaea.810729
title: Single cell abundances of Håkon Mosby mud volcano sediments measured at station PS74/169-1_PUC-1 (Sample 1, new flow surface)
DOI: 10.1594/pangaea.810730
title: Single cell abundances of Håkon Mosby mud volcano sediments measured at station PS74/172-1_PUC-131 (Sample 8, old flow surface)
DOI: 10.1594/pangaea.810732
title: Sulphate reduction rates of Håkon Mosby mud volcano sediments measured at station MSM16/2_823-1 (Sample 9, old flow surface)

description: Turnover rates were determined for surface sediment cores obtained in 2009 and 2010. Sulfate reduction (SR) were measured ex situ by the whole core injection method (doi:10.1080/01490457809377722). We incubated the samples at in situ temperature (1.0°C) for 12 hours with carrier-free 35**SO4 (dissolved in water, 50 kBq). Sediment was fixed in 20 ml 20% ZnAc solution for AOM or SR, respectively. Turnover rates were measured as previously described (doi:10.4319/lom.2004.2.171).
DOI: 10.1594/pangaea.810736
title: Sulphate reduction and methane oxidation rates of Håkon Mosby mud volcano sediments measured at station MSM16/2_838-1 (Sample 3, new flow surface)

description: Sulfate reduction (SR) and anaerobic oxidation of methane (AOM) were measured ex situ by the whole core injection method (doi:10.1080/01490457809377722). We incubated the samples at in situ temperature (1.0°C) for 12 hours with either 14** CH4 (dissolved in water, 2.5 kBq) or carrier-free 35** SO4 (dissolved in water, 50 kBq). Sediment was fixed in 25 ml 2.5% sodium hydroxide (NaOH) solution or 20 ml 20% ZnAc solution for AOM or SR, respectively. Turnover rates were measured as previously described (http://edoc.mpg.de/177065; doi:10.4319/lom.2004.2.171).
DOI: 10.1594/pangaea.810737
title: Sulphate reduction and methane oxidation rates of Håkon Mosby mud volcano sediments measured at station MSM16/2_847-1 (Sample 5, aged flow surface)

description: Sulfate reduction (SR) and anaerobic oxidation of methane (AOM) were measured ex situ by the whole core injection method (doi:10.1080/01490457809377722). We incubated the samples at in situ temperature (1.0°C) for 12 hours with either 14** CH4 (dissolved in water, 2.5 kBq) or carrier-free 35** SO4 (dissolved in water, 50 kBq). Sediment was fixed in 25 ml 2.5% sodium hydroxide (NaOH) solution or 20 ml 20% ZnAc solution for AOM or SR, respectively. Turnover rates were measured as previously described (http://edoc.mpg.de/177065; doi:10.4319/lom.2004.2.171).
DOI: 10.1594/pangaea.810738
title: Sulphate reduction and methane oxidation rates of Håkon Mosby mud volcano sediments measured at station MSM16/2_855-1 (Sample 6, aged flow surface)

description: Sulfate reduction (SR) and anaerobic oxidation of methane (AOM) were measured ex situ by the whole core injection method (doi:10.1080/01490457809377722). We incubated the samples at in situ temperature (1.0°C) for 12 hours with either 14** CH4 (dissolved in water, 2.5 kBq) or carrier-free 35** SO4 (dissolved in water, 50 kBq). Sediment was fixed in 25 ml 2.5% sodium hydroxide (NaOH) solution or 20 ml 20% ZnAc solution for AOM or SR, respectively. Turnover rates were measured as previously described (http://edoc.mpg.de/177065; doi:10.4319/lom.2004.2.171).
DOI: 10.1594/pangaea.817289
title: Basic measurements of radiation at station Lindenberg (2007-01)
DOI: 10.1594/pangaea.817294
title: Basic measurements of radiation at station Lindenberg (2007-02)
DOI: 10.1594/pangaea.840869
title: Basic measurements of radiation at station Lindenberg (2007-03)
DOI: 10.1594/pangaea.840874
title: Basic measurements of radiation at station Lindenberg (2007-04)
DOI: 10.1594/pangaea.843216
title: Ichthyoplankton density and zooplankton biomass in the Benguela upwelling system during AFR258 in December 2009

description: IIchthyoplankton density (fish eggs and larvae) and bulk zooplankton biomass in December 2009 were determined for 22 stations in the Benguela upwelling system, based on oblique Multinet hauls during the FRS Africana cruise AFR258. A HYDROBIOS Multinet, type Midi (0.25 m**2 mouth area) was equipped with five nets of 500 µm-mesh size, temperature and oxygen probes, and an inner and outer flow meter to monitor the net's trajectory (for volume filtered calculations) as well as net clogging. The Multinet was handled over the side, towed horizontally at 2 knots. Winch speed when fearing was 0.5 or 0.3 m/s, heaving velocity 0.2 - 0.3 m/s. The Multinet was towed obliquely at 22 stations sampling the upper 200 m of the water column, which were divided into five different depth strata after inspection of temperature and oxygen concentration depth profiles. Ichthyoplankton densities and zooplankton biomass were calculated for each depth stratum (=single net) from total abundance and the volume of water filtered [individuals per m**3 and g wet weight per m**3, respectively]. Densities and biomass were integrated over the area for each station [individuals per m**2], as sum of calculations for each net: Sum ([individuals per m**3]*Delta (depth bot[m]-depth top [m]).
description: Geocode DEPTH, water is the mid depth of net range. Empty cell describes a missing sample.
DOI: 10.1594/pangaea.843278
title: Ichthyoplankton density and zooplankton biomass in the northern Benguela upwelling system during D356 September 2010

description: Ichthyoplankton density (fish eggs and larvae) and bulk zooplankton biomass in September 2010 were determined for 10 stations in the northern Benguela upwelling system, based on oblique Multinet hauls during the RRS Discovery D356 cruise. A HYDROBIOS Multinet, type Midi (0.25 m**2 mouth area) was equipped with five nets of 500 µm-mesh size, temperature and oxygen probes, and an inner and outer flow meter to monitor the net's trajectory (for volume filtered calculations) as well as net clogging. The Multinet was handled over the side, towed horizontally at 2 knots. Winch speed when fearing was 0.5 or 0.3 m/s, heaving velocity 0.2 - 0.3 m/s. The Multinet was towed obliquely at 10 stations sampling the upper 200 m of the water column, which were divided into five different depth strata after inspection of temperature and oxygen concentration depth profiles. Ichthyoplankton densities and zooplankton biomass were calculated for each depth stratum (=single net) from total abundance and the volume of water filtered [individuals per m**3 and g wet weight per m**3, respectively]. In addition, densities and biomass were integrated over the area for each station [individuals per m**2], as sum of calculations for each net: Sum ([individuals per m**3]*Delta(depth bot[m]-depth top [m]).
description: Geocode DEPTH, water is the mid depth of net range. Empty cell describes a missing sample.
DOI: 10.1594/pangaea.843325
title: Chlorophyll pigments from the Namibian upwelling system during Maria S. Merain cruise MSM17/3

description: Geocode DEPTH, water is the mid depth of the range. Procedure as described by Wasmund et al. (2006, http://www.iopan.gda.pl/oceanologia/481wasmu.pdf). However, a new fluorometer was used which measured according to the principle of Welschmeyer (1994, doi:10.4319/lo.1994.39.8.1985). Therefore, the chlorophyll a data were corrected for chlorophyll b, but not for pheopigments. This procedure is also recommended by HELCOM (2014, http://www.helcom.fi/Documents/Action%20areas/Monitoring%20and%20assessment/Manuals%20and%20Guidelines/Manual%20for%20Marine%20Monitoring%20in%20the%20COMBINE%20Programme%20of%20HELCOM.pdf).