cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.761359
title: (Table 1) Age and depth of reflectors of the 3.5-kHz and airgun seismic record and their corresponding depth of ash layers, carbonate peaks, and transition zones from DSDP Hole 83-504B

description: DSDP cores from areas of low (Site 505) and high heat flow (Site 504 B) near the Costa Rica Rift, together with seismic profiles from the Panama Basin, have been studied to determine the relationship between: (1) carbonate content and physical and acoustic properties; and (2) carbonate content, carbonate diagenesis and acoustic stratigraphy. Except for ash and chert layers, bulk density correlates strongly and linearly with carbonate content. Velocity is uniform downcore and only small variations at a small scale are measured. Thus an abrupt change in carbonate content will cause abrupt changes in acoustic impedance and should cause reflectors that can be detected acoustically. A comparison of seismic profiler reflection records with physical properties, carbonate content and reflection coefficients indicates that the main reflectors can be identified with ash layers, diagenetic boundaries, and carbonate content variations. Diagenesis of carbonate sediments is present at Site 504B in a 260 m-thick ooze-chalk-limestone/chert sequence. These diagenetic sequences occur in areas of higher heat flow (200 mW/m**2). Seismic profiler records can be used to map the extent and depth of these diagenetic boundaries.
description: Approximate depth, Vp = 1.53 km/s.
description: Supplement to: Mienert, Jürgen (1984): The importance of carbonate content in the acoustic stratigraphy of Panama Basin. Marine Geology, 54(3-4), 237-247
DOI: 10.1594/pangaea.497106
title: Physical oceanography from BT during cruise M90HQB_1989
DOI: 10.1594/pangaea.760279
title: Basic measurements of radiation at station Kwajalein (2006-03)
DOI: 10.1594/pangaea.762142
title: Tab. 1: Direct beam solar radiation measurements for selected stations in Polar regions

description: As part of a larger experiment, atmospheric turbidity measurements were carried out during the austral summer 1985/86 in Adelie Land, Eastern Antarctica at 1560 m elevation. A comparison of our measurements of the solar beam with those of other areas in the Arctic and Antarctic was carried out. Our values were higher than all measurements from the Arctic. For Antarctica, Plateau and Mizuho Stations, both higher in altitude, had somewhat higher values, while the value of the coastal stations were lower. We calculated also turbidity indexes such as Unke's turbidity factor T and Angstrom's turbidity coefficient ß. Mean values of T were around 2.0, which are low values indeed. Beta values were around 0.04, a rather typical value for polar regions. No trend in turbidity could be observed for the time of observation. Further, it could be shown that the decrease in intensity with increasing optical air mass was less pronounced for larger wavelengths than for shorter ones.
description: Supplement to: Wendler, Gerd; Ishikawa, Nobuyoshi (1988): Measurements of the atmospheric turbidity at D47, Adelie Land, Antarctica. Polarforschung, 58(1), 41-46
DOI: 10.1594/pangaea.817242
title: Mean grain size from IODP Hole 343-C0019E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.759325
title: Basic and other measurements of radiation at Neumayer Station (1997-03)
DOI: 10.1594/pangaea.759366
title: (Table 4) Depth location of oxygen isotope stages in the Ficarazzi section
DOI: 10.1594/pangaea.759445
title: (Table 1) Sample description of ODP Leg 121
DOI: 10.21227/g06c-yh08
title: A Multispectral Automated Transfer Technique (MATT) for machine-driven image labeling utilizing the Segment Anything Model (SAM)

description: Segment Anything Model (SAM) is drastically accelerating the speed and accuracy ofautomatically segmenting and labeling large Red-Green-Blue (RGB) imagery datasets. However, SAM isunable to segment and label images outside of the visible light spectrum, for example, for multispectral orhyperspectral imagery. Therefore, this paper outlines a method we call the Multispectral Automated TransferTechnique (MATT). By transposing SAM segmentation masks from RGB images we can automaticallysegment and label multispectral imagery with high precision and efficiency. For example, the resultsdemonstrate that segmenting and labeling a 2,400-image dataset utilizing MATT achieves a time reductionof 87.8% in developing a trained model, reducing roughly 20 hours of manual labeling, to only 2.4 hours.This efficiency gain is associated with only a 6.7% decrease in overall mean average precision (mAP) whentraining multispectral models via MATT, compared to a manually labeled dataset. We consider this anacceptable level of precision loss when considering the time saved during training, especially for rapidlyprototyping experimental modeling methods. This research greatly contributes to the study of multispectralobject detection by providing a novel and open-source method to rapidly segment, label, and trainmultispectral object detection models with minimal human interaction. Future research needs to focus onapplying these methods to (i) space-based multispectral, and (ii) drone-based hyperspectral imagery.
DOI: 10.1594/pangaea.855269
title: Annotated record of the detailed examination of Mn deposits from the GEORSTOM III CENTRE stations

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.759773
title: Basic measurements of radiation at station Carpentras (2011-03)
DOI: 10.1594/pangaea.761710
title: (Table 2) Particulate organic carbon concentrations in the water column of the Barents Sea in August-September 1997

description: A comparative estimation of particulate organic matter concentration in seawater in various regions of the Barents Sea was carried out on the basis of materials collected by authors in August-September 1997. It is shown that the major feature of near-bottom distribution of particulate organic matter is distinct decrease in its concentration from off-shore areas of the Murman and Novaya Zemlya coasts and the Franz Josef Land Archipelago toward the central part of the Barents Sea. Using a method of mean and maximum concentrations of particulate organic matter, an attempt was made to estimate its fluxes from the surface to the bottom.
description: UML = upper mixed layer; NBL = near-bottom layer.
description: Supplement to: Romankevich, Evgeny A; Korneeva, Galina A; Shevchenko, Vladimir P; Gordeev, Vladimir Yu; Belyaev, Nikolay A (2000): Suspended organic matter in the Barents Sea. Translated from Okeanologiya, 2000, 409(2), 208-216, Oceanology, 40(2), 192-200
DOI: 10.1594/pangaea.762219
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0195

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.6084/m9.figshare.24082158
title: Travel Times and Distances between DAs and closest 24-hr EDs (csv)

description: Reported estimated travel time and distance from the DA centroid to closest identified hospital. Labels with "From_" relate to the DA centroid and labels with "To_" relate to the hospital.
DOI: 10.6084/m9.figshare.24082158.v3
title: Travel Times and Distances between DAs and closest 24-hr EDs (csv)

description: Reported estimated travel time and distance from the DA centroid to closest identified hospital. Labels with "From_" relate to the DA centroid and labels with "To_" relate to the hospital.
DOI: 10.1594/pangaea.808816
title: (Table 1) Major-oxides and trace-elements of basalts at DSDP Hole 78-543A
DOI: 10.1594/pangaea.760074
title: (Fig. 4) Active metabolic rate and pleopod beat rate in megalopa of the kelp crab Taliepus dentatus at site CC, Chile
DOI: 10.1594/pangaea.759811
title: (Table 1) Sand and 40-63 µm fraction in from ODP Hole 113-690B
DOI: 10.1594/pangaea.759812
title: (Table 2) Composition of the sand fraction from ODP Hole 113-690B

description: Sediment depth is given in mbsf. Originally given as cumulative plot.
DOI: 10.1594/pangaea.760754
title: (Table 2) Carbonate content of selected samples of DSDP Hole 27-261
DOI: 10.1594/pangaea.921985
title: Average variation in calcium and titanium from sediment core ICDP 5017-1 (Dead Sea)

description: The surface of the archived half of the core was scanned with the ITRAX core scanner at a resolution of 1 mm, an exposure time of 1 s, and a Chromium tube at 30 kV voltage and 30 mA current at the GFZ (Potsdam) (Neugebauer et al., 2014).
DOI: 10.1594/pangaea.760837
title: Basic and other measurements of radiation at station Ny-Ålesund (2001-03)
DOI: 10.1594/pangaea.757834
title: Basic and other measurements of radiation at station Barrow (1996-03), Version 1

description: Ellsworth G. Dutton discovered a calibration glitch in the SWD "Short-wave downward (GLOBAL) radiation" data for Barrow, Alaska. SWD data was therefore removed from this dataset. Please refer to the updated Version 2 (see replaced by reference) with correct calibration.
DOI: 10.1594/pangaea.760759
title: (Table 3) Single-particle composition of aerosol samples collected in the Western Russian Arctic in August-September 1991
DOI: 10.1594/pangaea.758420
title: (Table 5) Distribution of diatoms in Oligocene to early Miocene sediments of DSDP Hole 7-66

description: Species abundaces: D = dominant, A = abundant, C = common, F = few, R = rare, - = absent.
DOI: 10.1594/pangaea.757450
title: Tab.1: Composition of salt crusts and host rocks

description: Gypsum and calcite crusts were found on many outcrops of the metamorphic basement and on moraines in Dronning Maud Land. For the first time the copper mineral connellite was found in such crusts. Salt crust and efflorescences indicate an important role of chemical weathering even in a cold and arid climate such as the Antarctic interior. Findings of salt efflorescenees few centimetres beneath the rock surface suggest the contribution of salt crystallization to the formation of the typical Antarctic cavernous or honeycomb weathering features.
description: Supplement to: Bauer, Wilfried; Fitzner, Bernd (2005): Salt crusts on bedrock exposures in Dronning Maud Land, East Antarctica. Polarforschung, 73(1), 1-4
DOI: 10.1594/pangaea.758474
title: (Table 12) Distribution of radiolaria in Oligocene to Miocene sediments of DSDP Hole 30-289

description: Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent.
DOI: 10.1594/pangaea.759133
title: (Table 2) Hydrogen index and soluble organic matter in selected samples of ODP Leg 121 holes
DOI: 10.1594/pangaea.748302
title: Hydrography on standard level calculated from water bottle samples of RV Atlantis II from 1963 to 1980
DOI: 10.1594/pangaea.497628
title: Physical oceanography from BT during cruise U58JH00053B_1960
DOI: 10.1594/pangaea.757346
title: (Table 2) Carbon chemistry of DSDP Leg 62 samples
DOI: 10.1594/pangaea.757347
title: (Table 3) Summary of extractable organic matter contents of limestones from DSDP Holes 62-463 and 62-465A
DOI: 10.1594/pangaea.734237
title: (Figure F2) Orthogonal vector plots of AF demagnetization steps of IODP Hole 308-U1320A (163.96 mbsf)
DOI: 10.1594/pangaea.757209
title: (Table 4) Occurrence and arbitrary relative abundances of organic sulfur compounds in ODP Leg 117 samples

description: + = present, - = not detected
DOI: 10.1594/pangaea.756866
title: Meteorological synoptical observations from station Lindenberg (2004-02)
DOI: 10.1594/pangaea.756548
title: (Table 1) Concentrations of organic carbon, nitrogen, sulfur and carbonate in Samples of ODP Hole 116-717C
DOI: 10.1594/pangaea.841974
title: Flow and suspended sediment concentration fields over tidal bedforms, ADCP profile 17
DOI: 10.1594/pangaea.756873
title: Ozone measurements from station Lindenberg (2004-03)
DOI: 10.1594/pangaea.745555
title: (Table 2) In-situ sediment temperatures of gravity corer stations from the Dvurechenskii mud volcano

description: For each sensor, the distance Dz between the sensor and the tip of the gravity corer is given in the last row of the table. The estimated penetration depth also refers to the tip of the gravity corer, such that the sensor depth may be calculated by subtracting Dz from the penetration depth.
DOI: 10.1594/pangaea.756876
title: Meteorological synoptical observations from station Lindenberg (2004-04)
DOI: 10.1594/pangaea.756879
title: Expanded measurements from station Lindenberg (2004-04)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.755768
title: (Table 2) Magnetic properties of ODP Leg 115 basalt samples
DOI: 10.1594/pangaea.757499
title: (Table 2) Stable carbon isotopic composition of biomarkers of DSDP Hole 41-367

description: carbon isotope in per mil vs. VPDB
DOI: 10.1594/pangaea.868602
title: Water level from CTD pressure sensor 2 m above seabed at station HE441/07-1 from the German Bight
DOI: 10.1594/pangaea.755862
title: Ozone measurements from station Tamanrasset (2010-11)
DOI: 10.1594/pangaea.755943
title: (Table 2) Cd/Ca ratios of Uvigerina hispidocostata of ODP Hole 115-709C
DOI: 10.1594/pangaea.667469
title: Radiocarbon age of sediment core GeoB7608-1

description: KIA 21460, KIA 21866, KIA 21459, KIA 21457: Dates were not used because of the adoption of the stratigraphy from MD04-2760 [Kwiecien et al., Radiocarbon, 50(1), 2008, 99-118] / KIA 21460: Sample was discarded because of its high amount of broken and probably reworked shells [Bahr et al., 2006, doi:10.1016/j.epsl.2005.10.036]
DOI: 10.1594/pangaea.688782
title: Total organic carbon at bottle station SEPT-1999-K8

description: The samples (10 ml) were obtained in pre-combusted (480∞C, 12h) glass ampoules, acidified with HCl to 0.1% by volume and flame-sealed immediately on board. High Temperature Catalytic Oxidation HTCO using a Shimadzu 5000 TOC analyzer. Sugimura, Y & Y. Suzuki, 1988. Cauwet, G., 1994.
DOI: 10.1594/pangaea.754682
title: (Table 1) Stable isotopic measurements of left-coild Neogloboquadrina pachyderma from ODP Hole 114-704B
DOI: 10.1594/pangaea.755564
title: (Table 1) Range chart of relative abundances of selected diatoms and silicoflagellates from ODP Hole 114-699A

description: Species abundances: X = very rare (only one observed specimen); R = rare (several specimens/slide); S = sparse (one specimen/20 fields of view); F = frequent (one specimen/10 fields); C = common (one specimen/5 fields); A = abundant (an average of one specimen/field); D = dominant (more than one specimen/field); ? = questionably present; - = not present. () = reworked/displaced (?).
DOI: 10.1594/pangaea.755410
title: (Table 3) Distribution of Paleocene calcareous nannofossils in ODP Hole 114-700B

description: Species abundances: A = abundant (&gt;30 %), C = common (30-15 %), F = few (15-3 %), R = rare (&lt;3%), - = not present.
DOI: 10.1594/pangaea.855091
title: (Table 2, page 239), Trace elements and REEs from Mn rich deposits recovered during the NODCO 1 expedition

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.868604
title: Significant wave height and peak period at station HE441/07-1 from the German Bight
DOI: 10.1594/pangaea.755229
title: Tab. 2: Geochemical analyses (with XRF) of some selected volcanic rocks
DOI: 10.1594/pangaea.754373
title: Electron microprobe results of clay minerals from samples of the Frankenwald and the Thüringer Wald

description: Late Devonian (Frasnian) pillow basalts from the Frankenwald and Thüringer Wald within the Saxothuringian zone in Germany were found to contain abundant putative biogenic filaments, indicating that the volcanic rocks once harbored microbial life. The mineralized filaments are found in calcite-filled amygdules (former vesicles), where they started to form on internal surfaces of vesicles after seawater ingress. The filaments postdate an early fibrous carbonate cement but predate later equant calcite spar, revealing syngenetic formation. A biogenic origin of filaments is indicated by their size and morphology resembling modern microorganisms, their independence of crystal faces and cleavage plans, complex branching patterns, and internal segmentation. The filamentous microorganisms represent cryptoendoliths that lived in structural cavities of the basalt. They became preserved upon microbial clay authigenesis similar to the encrustation of modern prokaryotes in iron-rich environments. Filaments consist of clay minerals with the endmember composition berthierine-chamosite and illite-glauconite. Based on the discovery of fossilized filamentous microorganisms in Late Devonian pillow basalts of the Saxothurigian zone that are similar to filaments previously found in Middle Devonian pillow basalts of the Rhenohercynian zone, it is apparent that cryptoendolithic life was more widespread than previously recognized. Structural cavities within seafloor basalt may thus represent a common, perhaps universal niche for life in the oceanic crust.
description: Supplement to: Eickmann, Benjamin; Bach, Wolfgang; Kiel, Steffen; Reitner, Joachim; Peckmann, Jörn (2009): Evidence for cryptoendolithic life in Devonian pillow basalts of Variscan orogens, Germany. Palaeogeography, Palaeoclimatology, Palaeoecology, 283, 120-125
DOI: 10.1594/pangaea.747838
title: Meteorological observations during CASTOR cruise from Nederland to Batavia started at 1836-10-07
DOI: 10.1594/pangaea.755761
title: (Appendix) Thin sections probed on samples from ODP Leg 115
DOI: 10.1594/pangaea.755404
title: (Table 3b) Distribution of planktonic foraminiferal tests in sediments from Core NKA-3T
DOI: 10.1594/pangaea.753471
title: (Table 9) Abundance of silicoflagellates in ODP Hole 113-696A
DOI: 10.1594/pangaea.911411
title: Oxygen profiles across the sediment-water interface in three different habitats in salt marshes

description: Oxygen profiles across the sediment-water interface in three different habitats in salt marshes: 1) Tidal river; submerged sediment. 2) Tidal ponds; submerged sediment and 3) vegetated marsh platform; intertidal. Profiles from tidal river were measured in sediment cores in the laboratory. Profiles from tidal ponds and marsh platform were measured in situ.Instrumentation: Optode microprofiling device from PreSens GmbH (Germany, www.presens.de) with needle-type optodes (PM-PSt7) for measurements of oxygen profles.Time: Tidal river (Parker river, Ma, USA) - August 2016, Tidal Ponds (Plum Island Estuary marshes, MA, USA) July 2018,Marsh Platform (Great Sippewissett marsh, MA, USA) August 2016.
DOI: 10.1594/pangaea.855088
title: (Table 2, page 277), Major and trace elements geochemical analysis of the layers of the TECHNO crust

description: Layers A to E go outward from the inside contact with substrate (A) to the outside (E) of the TECHNO crust.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.911366
title: In situ time series of temperature in shallow salt marsh tidal ponds
DOI: 10.1594/pangaea.855090
title: Description of manganese deposits collected by R/V "Jean Charcot" during its NODCO 1 expedition

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.911370
title: In situ time series of salinity in shallow salt marsh tidal ponds
DOI: 10.1594/pangaea.744353
title: Physical oceanography during Skagerrak cruise Skagerrak72/3 to the North Sea
DOI: 10.1594/pangaea.751921
title: Meteorological observations during San Vicente cruise from Ferrol to Brest started at 1779-05-25
DOI: 10.1594/pangaea.911357
title: In situ time series of pH in shallow salt marsh tidal ponds

description: Optode microprofiling device from PreSens GmbH (Germany, www.presens.de) with an Automated Micromanipulator (AM), needle-type optodes for measurements of oxygen (PM-PSt7) and pH (PM-HP5). Temperature was measured with HOBO Pendant© Temperature/Light Datalogger. Salinity was measured with a handheld refractometer. Light data PAR was received from nearby weather-station; light sensor unknown.Oxygen and pH were measured in the water column at a distance of 2-cm from the sediment surface. Oxygen measurements are temperature compensated.
DOI: 10.1594/pangaea.911360
title: In situ time series of photosynthetically active radiation (PAR) in shallow salt marsh tidal ponds

description: Optode microprofiling device from PreSens GmbH (Germany, www.presens.de) with an Automated Micromanipulator (AM), needle-type optodes for measurements of oxygen (PM-PSt7) and pH (PM-HP5). Temperature was measured with HOBO Pendant© Temperature/Light Datalogger. Salinity was measured with a handheld refractometer. Light data PAR was received from nearby weather-station; light sensor unknown.Oxygen and pH were measured in the water column at a distance of 2-cm from the sediment surface. Oxygen measurements are temperature compensated.
DOI: 10.1594/pangaea.752476
title: Meteorological observations during Theodora en Sara cruise from Nieuwediep to Batavia started at 1841-05-26
DOI: 10.1594/pangaea.744413
title: Physical oceanography during Tridens cruise Tridens76 to the North Sea
DOI: 10.1594/pangaea.774599
title: Section images from IODP Hole 316-C0008A

description: Geocode = [m CSF-A] Top Core depth (below sea floor).
DOI: 10.1594/pangaea.752926
title: Meteorological observations during WOOLWICH cruise from Table Bay to The Downs started at 1799-04-07
DOI: 10.1594/pangaea.753009
title: Meteorological observations during BOREAS cruise from Senegal to Lisbon started at 1766-05-01