cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.935321
title: Density development of Carcinus maenas and Hemigrapsus takanoi between 2017-2020 in the Northfrisian Wadden Sea

description: Field and Laboratory experiments were performed to study the feeding ecology of Hemigrpasus takanoi and C. maenas. Experiments were done between 2017-2020 on oyster reefs near the island of Sylt (Wadden Sea, North Sea). Data were collected to investigate the effect of a non-native crab species on native community. We used exclusion experiments in the field and feeding experiments under controlled conditions at the lab.
DOI: 10.1594/pangaea.823162
title: Biomarker record and temperature reconstruction across the Eocene-Oligocene boundary of ODP Hole 151-913B
DOI: 10.1594/pangaea.497858
title: Physical oceanography from BT during cruise U58X001083B_1934
DOI: 10.1594/pangaea.908230
title: Ice rafted debris flux to sediment core FOX12-02R

description: The samples were wet-sieved, separating them into grain-size fractions , (63-150 µm, and &gt;150 µm). For the &gt;150 µm fraction, individual grains that weighed more than 0.01 g were discarded in order to reduce distortion of the grain size signal resulting from the occurrence of singular large grains. Weight percentages of the sand fraction were calculated relatively to the total dry weight. Sediment weight percentages were converted to IRD fluxes.
DOI: 10.1594/pangaea.677388
title: Ozone measurements from station Ny-Ålesund (1994-09)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.891113
title: Meteorological synoptical observations from station Tateno (2018-01)
DOI: 10.1594/pangaea.935459
title: Meteorological synoptical observations from station Fukuoka (2021-06)
DOI: 10.1594/pangaea.730005
title: Mud volcanism related investigations of sediment core VKGD277/PC-7
DOI: 10.1594/pangaea.891272
title: Radiolarian abundances from IODP Hole 349-U1433A
DOI: 10.1594/pangaea.819294
title: (Table 4) Distribution and abundance of Cretaceous nannofossils in DSDP Hole 89-585

description: DEPTH, sediment [m] is given in mbsf. Species abundance: A = abundant (&gt;10 specimens per field ov view at 780 X), C = common (1 specimen per field), F = few (1 specimen per 10 fields), R = rare (1 specimen per 100 fields), P = present (1 specimen per &gt;100 fields), - = absent.
DOI: 10.1594/pangaea.498489
title: Physical oceanography from BT during cruise U90OG08778B_1970
DOI: 10.1594/pangaea.826311
title: Solids analysis from IODP Hole 330-U1373A

description: Geocode = Top depth CSF-A (m)#0 = bdl (below detection limit)
DOI: 10.1594/pangaea.676865
title: Contents of total organic carbon and bitumen in sedimentary rocks of Hole VNIIO-1985-Kur-01 drilled in the Barents Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.676866
DOI: 10.1594/pangaea.495894
title: Water temperature IBT profiles from cruise U90CT88083I_1988
DOI: 10.1594/pangaea.856864
title: (Table 1) Sample description from ODP Hole 206-1256D and IODP Hole 335-U1256D

description: # = "Ghost core": rock debris collected from the junk basket during hole-cleaning operation (Teagle et al., 2006).
DOI: 10.1594/pangaea.856658
title: (Table 4, page 94) Chemical composition of ferromanganese encrustations from the Equatorial Atlantic

description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
DOI: 10.1594/pangaea.749557
title: Meteorological observations during HELDIN cruise from Rio de Janeiro to Batavia started at 1832-02-14
DOI: 10.1594/pangaea.828768
title: Reflectance spectroscopy and colorimetry from IODP Hole 336-U1384A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.755992
title: (Table 3f) Mercury concentrations in waters of the Mediterranean Sea at Station VB30-288
DOI: 10.1594/pangaea.935324
title: Number of consumed Gammarus locusta in a feeding experiment with Hemigrapsus takanoi and Carcinus maenas

description: Field and Laboratory experiments were performed to study the feeding ecology of Hemigrpasus takanoi and C. maenas. Experiments were done between 2017-2020 on oyster reefs near the island of Sylt (Wadden Sea, North Sea). Data were collected to investigate the effect of a non-native crab species on native community. We used exclusion experiments in the field and feeding experiments under controlled conditions at the lab.
DOI: 10.1594/pangaea.497655
title: Physical oceanography from BT during cruise U58JH01056B_1943
DOI: 10.1594/pangaea.842508
title: Other measurements at 10 m from station Darwin (2005-12)

description: Version 2, 2015-02-06
DOI: 10.1594/pangaea.893776
title: Pollen profile of sediment core KON, Lake Konsu, Estonia

description: This dataset was archived on 2018-09-10 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.677325
title: Ozone measurements from Neumayer Station (2003-07)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.935326
title: Number of consumed Mytilus edulis in a feeding experiment with Hemigrapsus takanoi and Carcinus maenas

description: Field and Laboratory experiments were performed to study the feeding ecology of Hemigrpasus takanoi and C. maenas. Experiments were done between 2017-2020 on oyster reefs near the island of Sylt (Wadden Sea, North Sea). Data were collected to investigate the effect of a non-native crab species on native community. We used exclusion experiments in the field and feeding experiments under controlled conditions at the lab.
DOI: 10.1594/pangaea.497103
title: Physical oceanography from BT during cruise M90HPB_1986
DOI: 10.1594/pangaea.497547
title: Physical oceanography from BT during cruise U58GS01304B_1955
DOI: 10.1594/pangaea.935327
title: Number of polychaetes in field experiments with and without native and non-native shore crab inclusion
DOI: 10.1594/pangaea.477369
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/14-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.908394
title: Continuous sediment temperature observations at station BEFmate_S2low (2018-10)
DOI: 10.1594/pangaea.908413
title: Continuous sediment temperature observations at station BEFmate_S3low (2018-08)
DOI: 10.1594/pangaea.498240
title: Physical oceanography from BT during cruise U74X000735B_1956
DOI: 10.1594/pangaea.829711
title: (Table 6) Strontium isotope ratios of foraminifera from ODP Hole 171-1049C

description: DEPTH, sediment/rock [m] is given in mbsf.
DOI: 10.1594/pangaea.494999
title: Water temperature MBT profiles from cruise K7401M_1967
DOI: 10.1594/pangaea.908537
title: Microsensor analyses of oxygen and pH at sediment surface in core LZUG_1 from Lake Zug
DOI: 10.1594/pangaea.752550
title: Meteorological observations during Twee Cornelissen cruise from Texel to Batavia started at 1836-10-31
DOI: 10.1594/pangaea.892386
title: Methane and carbon dioxide concentrations measured in subglacial air, Isunnguate Sermia glacier, Western Greenland, 2016-08-23
DOI: 10.1594/pangaea.842763
title: Radiosonde measurements from station Darwin (2005-04)

description: Version 3, 2015-02-13; Launches at irregular time intervals
DOI: 10.1594/pangaea.496519
title: Water temperature XBT profiles from cruise U99X114135_1993
DOI: 10.1594/pangaea.755740
title: (Table 1j) Nutrient concentrations and primary production at Station Sap-92-2129 in the Bering Sea
DOI: 10.1594/pangaea.842481
title: Basic measurements of radiation at station Darwin (2005-01)

description: Version 3, 2015-02-06
DOI: 10.1594/pangaea.823072
title: (Table 1) Description, organic/carbon, and external characteristics at DSDP Legs 56-57 Holes

description: Sediment depth is given in mbsf. Empty cells = no data. # = Values questionable because of extremely low weight of fractions.
DOI: 10.1594/pangaea.823097
title: (Table 3) ESR of kerogen and humic acids at DSDP Leg 57 Holes

description: Sediment depth is given in mbsf. Empty cells = no data.
DOI: 10.1594/pangaea.761005
title: (Supplementary Table 1) Phylogenetic affiliation of particle-associated bacterial isolates
DOI: 10.1594/pangaea.771635
title: Physical oceanography during Walther Herwig III cruise WH219
DOI: 10.1594/pangaea.893775
title: Age determination of sediment core KON, Lake Konsu, Estonia

description: This dataset was archived on 2018-09-10 from the EPD database. (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.803981
title: Surface wind stress modeled for the Panama Seaway with the Community Climate System Model 3

description: The early Pliocene warm phase was characterized by high sea surface temperatures and a deep thermocline in the eastern equatorial Pacific. A new hypothesis suggests that the progressive closure of the Panamanian seaway contributed substantially to the termination of this zonally symmetric state in the equatorial Pacific. According to this hypothesis, intensification of the Atlantic meridional overturning circulation (AMOC) - induced by the closure of the gateway - was the principal cause of equatorial Pacific thermocline shoaling during the Pliocene. In this study, twelve Panama seaway sensitivity experiments from eight ocean/climate models of different complexity are analyzed to examine the effect of an open gateway on AMOC strength and thermocline depth. All models show an eastward Panamanian net throughflow, leading to a reduction in AMOC strength compared to the corresponding closed-Panama case. In those models that do not include a dynamic atmosphere, deepening of the equatorial Pacific thermocline appears to scale almost linearly with the throughflow-induced reduction in AMOC strength. Models with dynamic atmosphere do not follow this simple relation. There are indications that in four out of five models equatorial wind-stress anomalies amplify the tropical Pacific thermocline deepening. In summary, the models provide strong support for the hypothesized relationship between Panama closure and equatorial Pacific thermocline shoaling.
description: Data are averaged from the last 100 model years of the simulation (Model year 911 - 1001).
description: Supplement to: Zhang, Xiao; Prange, Matthias; Steph, Silke; Butzin, Martin; Krebs, Uta; Lunt, Daniel J; Nisancioglu, Kerim H; Park, Wonsun; Schmittner, Andreas; Schneider, Birgit; Schulz, Michael (2012): Changes in equatorial Pacific thermocline depth in response to Panamanian seaway closure: Insights from a multi-model study. Earth and Planetary Science Letters, 317-318, 76-84
DOI: 10.1594/pangaea.807087
title: (Table 6) Geochemistry and minerals at DSDP Leg 81 Holes

description: CIPW norms are calculated with 85% of total iron as FeO and 15% as Fe2O3.
DOI: 10.1594/pangaea.842764
title: Radiosonde measurements from station Darwin (2005-05)

description: Version 3, 2015-02-13; Launches at irregular time intervals
DOI: 10.1594/pangaea.934178
title: Consumption rates in sand from the Janssand, Germany intertidal flat

description: The mpbvdnf_consumption_rates.csv file contains data in the following columns:event_label - the latitude from which samples were collected. Units = degrees and decimal minutes North latitude.season - the nominal season in which the sediment cores used in each measurement were collected.core - the identification number for each unique sediment core used in these measurements.light - a factor identifying whether measurements were made in the dark or the light. rate_nox - the net NOx (nitrate + nitrite) consumption rate. Units = mmol NOx (m3 sediment)-1 h-1. Positive values indicate net consumption, negative values indicate net production. rate_o2 - the net oxygen (O2) production rate. Units = mmol O2 (m3 sediment)-1 h-1. Positive values indicate net production, negative values indicate net consumption. Methods: Prior to rate measurements, steady state oxygen depth profiles were measured in the light in each sediment core to identify the depth of maximum net oxygen production (0.1–0.2 cm). Oxygen micro sensors and NOx micro biosensors were positioned in parallel at this depth. Site seawater containing ambient oxygen and nitrate concentrations were gravity drained through the core. Oxygen and NOx concentrations were measured for 10 minutes. Net production and consumption rates were calculated as the linear rate of change in concentration with respect to time.
DOI: 10.1594/pangaea.935314
title: Number of consumed Gammarus locusta in a feeding experiment with Hemigrapsus takanoi

description: Field and Laboratory experiments were performed to study the feeding ecology of Hemigrpasus takanoi and C. maenas. Experiments were done between 2017-2020 on oyster reefs near the island of Sylt (Wadden Sea, North Sea). Data were collected to investigate the effect of a non-native crab species on native community. We used exclusion experiments in the field and feeding experiments under controlled conditions at the lab.
DOI: 10.6084/m9.figshare.26340226
title: miniImageNet.zip

description: The Mini-ImageNet dataset of Few-Shot learning.
DOI: 10.1594/pangaea.755207
title: (Table 2b) Accumulation of glucose and protein hydrolysate by natural populations of microorganisms at Stations ML27_2124-1, 2125-1, 2126-1, and 2151-1

description: Glucose - 0.5-2.0 mg/l; protein hydrolysate - 0.5 mg/l.
DOI: 10.1594/pangaea.675383
title: Radiosonde measurements from station Payerne (1998-02)
DOI: 10.1594/pangaea.762534
title: Description of lithologic section units of IODP Hole 325-M0057A
DOI: 10.1594/pangaea.755208
title: (Table 2c) Accumulation of glucose and protein hydrolysate by natural populations of microorganisms at Station ML27_2159

description: Glucose - 0.5-2.0 mg/l; protein hydrolysate - 0.5 mg/l.
DOI: 10.1594/pangaea.788942
title: (Table 2) Oxygen and iron isotope ratios of ODP Hole 504B hydrothermally altered basltic rocks
DOI: 10.1594/pangaea.755401
title: (Table 1) Late Quaternary paleotemperatures of surface waters in the North Tropical Atlantic
DOI: 10.1594/pangaea.933386
title: Geochemical measurements of Gujo-Hachiman and Ubara, Japan and Opal Creek, Canada
DOI: 10.1594/pangaea.935452
title: Meteorological synoptical observations from station Abashiri (2021-06)
DOI: 10.1594/pangaea.675375
title: Radiosonde measurements from station Payerne (1997-06)
DOI: 10.1594/pangaea.787527
title: (Table 6) Susceptibility correlation tie points for Sites 133-819 and 133-820
DOI: 10.1594/pangaea.750267
title: Meteorological observations during La Princesa cruise from La Coruña to Montevideo started at 1786-08-19
DOI: 10.1594/pangaea.823096
title: (Table 2) Visible spectroscopy and elemental analyses of humic acids at DSDP Leg 57 Holes
DOI: 10.1594/pangaea.908637
title: Geochemical parameter measured in pore water and sediment of sediment core LZUG_2 from Lake Zug

description: /0: outliers removed#0: below detectionempty cells: not determined
DOI: 10.1594/pangaea.675373
title: Radiosonde measurements from station Payerne (1997-04)
DOI: 10.1594/pangaea.695677
title: Ultra-violet measurements from station Toravere (2007-04)

description: Values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-01-17. UVB is measured with Kipp&Zonen CUVB1 narrowband radiometer (bandwidth 306 ± 0.1 nm)
DOI: 10.1594/pangaea.908813
title: Radiosonde measurements from station Minamitorishima (2019-09)
DOI: 10.1594/pangaea.499673
title: Physical oceanography from BT during cruise UXXXX00109B_1956
DOI: 10.1594/pangaea.762900
title: Occurrence and type of dolomite in ODP Site 124-768 samples (Table 1)

description: Occurrence of deep-sea dolomites has been reported from numerous settings (for discussion see Lumsden, 1988). Different authors agree that dolomite formation in the pelagic realm is a relatively early diagenetic process (e.g., Jorgensen, 1983; Shimmield and Price, 1984; Kablanow et al., 1984; Kulm et al., 1984). Baker and Burns (1985) suggest that most of the pelagic dolomites formed within a few tens of meters below the seafloor within the zone of microbial sulfate reduction. According to Fuechtbauer and Richter (1988), dolomite can form in the deep-sea at a minimum temperature of 10°C. Other deep-sea dolomites are products of fluids derived from underlying evaporites or submarine weathering of basalts (Garrison, 1981). In some cases (Mullins et al., 1985; Dix and Mullins, 1988; Mullins et al., 1988), the existence of dolomite is linked to disconformities and its formation may have resulted from circulation of seawater through the sediment during prolonged exposure (Dix and Mullins, 1988, p. 287).At Site 768 (Fig. 1), lithified carbonate layers, some containing variable amounts of dolomite, occur below 201 mbsf (Miocene). These beds alternate with unconsolidated or semi-lithified marl layers interbedded in clays and siliciclastic turbidites. The irregular depth distribution of the limestone beds and the variation in preservation and recrystallization of the calcareous microfaunas suggest that lithification of carbonates at Site 768 not only reflects burial diagenesis as described by Garrison (1981) and others, but in part may be a selective, early diagenetic process. The different types and distribution of the dolomite additionally seem to support this assumption.The purpose of this report is to document the occurrence and textural nature of the dolomite at Site 768. Methods used were analyses of stained thin sections (Alizarin S and Ferrocyanide) and studies with the scanning electron microscope. No geochemical analyses (e.g., stable isotopes) were carried out; they will be the subject of further investigations.
description: + = present, - = absent
description: Supplement to: Betzler, Christian (1991): Data report: Occurrence of dolomite at Site 768 (Sulu Sea). In: Silver, EA; Rangin, C; von Breymann, MT; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 124, 527-530
DOI: 10.1594/pangaea.879661
title: Heterotrophic prokaryotes population dynamics - Grazing and viral lysis of prokaryotes
DOI: 10.1594/pangaea.935469
title: Meteorological synoptical observations from station Ishigakijima (2021-06)
DOI: 10.1594/pangaea.675376
title: Radiosonde measurements from station Payerne (1997-07)
DOI: 10.1594/pangaea.935328
title: Survival rate of barnacles and juvenile oysters in a predation experiment with native and non-native shore crabs
DOI: 10.1594/pangaea.762512
title: Description of lithologic section units of IODP Hole 325-M0038A
DOI: 10.1594/pangaea.496342
title: Water temperature MBT profiles from cruise U90X110169M_1989
DOI: 10.1594/pangaea.841446
title: Basic measurements of radiation at station Momote (2008-02)

description: Version 2, 2015-01-12
DOI: 10.1594/pangaea.908616
title: (Table S5) Age model of ODP Site 208-1263
DOI: 10.1594/pangaea.908589
title: (Table S5) X-ray fluorescence (XRF) measurements of ODP Hole 114-702B
DOI: 10.1594/pangaea.484353
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_6N_7S_9N/117-1

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.750523
title: Meteorological observations during LUCIPARAS cruise from New York to Antwerpen started at 1847-05-16
DOI: 10.1594/pangaea.750750
title: Meteorological observations during MERCUUR cruise from Curacao to Marguerita started at 1821-01-17
DOI: 10.1594/pangaea.747687
title: Meteorological observations during BOREAS cruise from Banjoewangie to Texel started at 1847-02-03
DOI: 10.1594/pangaea.773720
title: MSCL measurements from IODP Hole 316-C0006F

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.828947
title: Natural gamma radiation from IODP Hole 339-U1385E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.706272
title: (Table 1) Mineral composition of clay fractions and bulk rocks, and δ¹⁸O, d2H(d1D) and δ¹³C values for clay fractions of bottom sediments from ODP Hole 139-858B

description: Mineral contents are approximate
DOI: 10.1594/pangaea.759857
title: Suspended matter and its components in the western Black Sea

description: Distribution and composition of suspended matter in the western Black Sea is examined in relation to influence of river run-off and eutrophication. Changes in suspended matter concentration and composition within the studied area are shown to be caused principally by intensity of production processes associated with different levels of eutrophication of coastal waters. Data on suspended matter obtained aboard or by remote control from space satellites are analyzed as a basis for evaluation of eutrophication scales and monitoring for evolution of marine production processes.
description: Supplement to: Vostokov, Sergey V (1996): Suspended matter as a measure of productivity in the western Black Sea. Translated from Okeanologiya, 1996, 36(2), 260-267, Oceanology, 36(2), 241-247
DOI: 10.1594/pangaea.803832
title: Ozone measurements from station Tamanrasset (2012-07)
DOI: 10.1594/pangaea.934184
title: Marine electrical resistivity profile 4 - east, Bykovsky Peninsula, Siberia

description: The data was collected with an IRIS Syscal Pro Deep Marine resistivity system that was equipped with a GPS and an echo-sounder to record water depths. The geoelectric cable had an electrode separation of 10 m and the electrodes were arranged in a reciprocal Wenner Schlumberger array. The offset between the first electrode and the boat was approximately 10 m.
description: Distance: Distance of boat position from starting point (m). This is not a cumulative distance.Water_depth: Water depth (m) from echo-sounderP1P2: Apparent resistivity (ohm-m) measured between potential electrodes P1 and P2. The remaining apparent resistivity columns have the same structure.C1: Position (m) of current electrode C1 relative to the boat position. For example, -60 m indicates that C1 is located 60 m behind the boat at the profile start.C2: Position (m) of current electrode C2 relative to the boat position. For example, -70 m indicates that C2 is located 70 m behind the boat at the profile start.P1: Position (m) of potential electrode P1 relative to the boat position. For example, -80 m indicates that P1 is located 80 m behind the boat at the profile start.P2: Position (m) of potential electrode P2 relative to the boat position. For example, -50 m indicates that P2 is located 50 m behind the boat at the profile start.The remaining electrode position columns follow the same structure.Latitude: latitude of boat position measured with GPS (WGS 1984)Longitude: longitude of boat position measured with GPS (WGS 1984)Note: Profile 4 (East) and Profile (West) were originally part of a single profile, but they were chopped into two segments for which the geoelectric cable was straight. Therefore, the initial distance of Profile (West) is listed as 357 m. Since the latter is the distance from the Profile 4 (East) origin point, the latitude and longitude coordinates should be used for more accurate estimates of distances between soundings along Profile 4 (West).
DOI: 10.1594/pangaea.688763
title: Meteorology at radiosonde positions during METEOR cruise M16

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de