cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.804553
title: Table 1: Station list with macrobenthos biomass results from the ocean floor

description: Among the Siberian shelf seas the Kara Sea is most strongly influenced by riverine runoff with nearly 1500 km fresh water discharge per year. This fresh water, discharged mainly by Ob and Yenisei, contains about 3.1 * 106 and 4.6 * 106 tons of total organic carbon per year, respectively (Gordeev et al. 1996). Little is known about the relevance of this organic material for biological communities, neither for the Kara Sea nor for the adjacent deep basins of the central Arctic Ocean. Aiming at elucidating the fate of fluvial matter transported from the rivers via estuaries into the central Arctic Ocean and the relative importance of marine organic matter being produced such information is crucial. Here we present calculations on the organic carbon demand of the Kara Sea macrozoobenthos based on measured biomass (total wet weight [ww] per 0.25 m ) from quantitative box corer samples and empirical relationships between biomass, annual production, annual respiration, and carbon remineralisation. This bottom-up approach may serve as a first estimate of the carbon remineralization potential of a given zoobenthos community (or area) as long as no data on in situ respiration rates are available. Our data basis comprises 54 stations sampled in summer seasons 1997, 1999 and 2000 in the Kara Sea at water depths between 10 and 68 m. The geographical area represented by stations analysed covers roughly 178 000 km**2, which is about one fifth of the total Kara Sea area. In this area, 290 species of invertebrate macrozoobenthos were identified with polychaeta, Crustacea, mollusca and echinodermata being the most abundant. For all stations analysed, mean biomass values ranged between 4.3 and 778.1 g ww/m**2 with organic carbon demands between 3.5 and 43.2 mg C/m**2/d. For the area of 178 000 km2 a preliminary total consumption of 1.4 * 10**6t Corg/y (equivalent to 21.5 mg C/m**2/d) was calculated for the macrozoobenthos. An extrapolation of our data would lead to an annual carbon demand of about 5-7 * 106 t for the whole Kara Sea macrozoobenthos (or 15.5-21.7 mg C/m2/d).
description: Supplement to: Klages, Michael; Deubel, Hendrik; Rachor, Eike (2003): Organic carbon consumption of the Kara Sea macrozoobenthos: A first assessment. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 267-280
DOI: 10.1594/pangaea.910954
title: Continuous thermosalinograph oceanography along Heincke cruise track HE534
DOI: 10.1594/pangaea.675018
title: Radiosonde measurements from station Ny-Ålesund (2002-12)
DOI: 10.1594/pangaea.800408
title: Physical oceanography and current meter data from mooring F9-1

description: Gear ID: 1, SN 10530; Gear ID: 2, SN 12328; Gear ID: 3, SN 1474; Gear ID: 4, SN 8403
DOI: 10.1594/pangaea.818806
title: Glacier mass balance Hintereisferner, Ötztal Alps, Austria, 1984/1985
DOI: 10.1594/pangaea.747806
title: Meteorological observations during CARYSFORT cruise from Spithead to Bic Road started at 1777-07-16
DOI: 10.1594/pangaea.675076
title: Radiosonde measurements from station Sede Boqer (2004-06)

description: Wind speed was multiplied by a factor of 0.1 (2009-08-28). Start location: Bet-Dagan, Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.751666
title: Meteorological observations during RACEHORSE cruise from Smeerenberg to Deptford started at 1773-08-20
DOI: 10.1594/pangaea.496651
title: Water temperature XBT profiles from cruise UNO_1985
DOI: 10.1594/pangaea.811704
title: (Table 1) Concentrations of BDE congeners, PBDEs, and HBCD in marine species, Norwegian North-East Atlantic

description: Sample tissues: blubber/adipose tissue from seals, whole eggs from terns, whole samples of zooplankton and cod. Concentrations are given per gram lipid weight.
DOI: 10.1594/pangaea.858435
title: Time series of atmospheric water vapour at station TAMP_S1
DOI: 10.1594/pangaea.760688
title: Statistics of radar altitude estimates of plume-top over time intervals of 12 hours

description: Radar did not detect plume when below about 2.9 km due to mountain ranges and curvature of the Earth.Date/time (UTC) refer to the end of the time interval.
DOI: 10.1594/pangaea.673401
title: Radiosonde measurements from station Barrow (1998-06)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.825976
title: P-Wave velocity (PWB) from IODP Hole 329-U1366D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.675457
title: Radiosonde measurements from station Payerne (2004-04)
DOI: 10.1594/pangaea.748989
title: Meteorological observations during El Grimaldi cruise from La Coruña to La Habana started at 1776-08-03
DOI: 10.1594/pangaea.707745
title: Radiosonde measurements from station Payerne (2008-02)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.1594/pangaea.917194
title: 1-Hz PPP displacements at GEONET station 1021 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.673363
title: Radiosonde measurements from station Barrow (1995-04)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.677743
title: Ozone measurements from station South Pole (1995-03)
DOI: 10.1594/pangaea.913154
title: Pluviographic observations of rainfall at station Medvedevskaya (11111)
DOI: 10.1594/pangaea.825288
title: P-Wave velocity (PWL) from IODP Hole 329-U1368F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.499245
title: Physical oceanography from BT during cruise U90X009729B_1901
DOI: 10.1594/pangaea.911186
title: Basic measurements of radiation at station Billings (2018-02)
DOI: 10.1594/pangaea.751050
title: Meteorological observations during PALLAS cruise from Coastal Suriname started at 1827-06-23
DOI: 10.1594/pangaea.672032
title: Nanoplankton data off Chipana Bay, winter 2006, Chile
DOI: 10.1594/pangaea.793229
title: Daily polynya area in the Laptev Sea polynyas
DOI: 10.1594/pangaea.655719
title: Current meter data from mooring PEX86_M13
DOI: 10.1594/pangaea.874554
title: Radiosonde measurements from Neumayer Station (2016-10)
DOI: 10.1594/pangaea.694775
title: Temperature and salinity in the water column of the Ionian Sea at Station SEPT-2000-IRI15B

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.694776
title: Temperature and salinity in the water column of the Ionian Sea at Station SEPT-2000-IRI15ZK

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.755630
title: (Table 2b) Concentrations of particulate protein and organic phosphorus combined with mesoplankton fraction in waters of the East Pacific at Station Agat-3572
DOI: 10.1594/pangaea.725434
title: (Appendix 1) Chemistry of sediment core TT013_32
DOI: 10.1594/pangaea.774559
title: (Table 5) Chemical composition of Cu- and Fe minerals from the Rainbow hydrothermal field
DOI: 10.1594/pangaea.663554
title: Oceanography at CTD/bottle station IFREMER_0394
DOI: 10.1594/pangaea.495943
title: Water temperature MBT profiles from cruise U90M_1986
DOI: 10.1594/pangaea.499130
title: Physical oceanography from BT during cruise U90X008323B_1985
DOI: 10.1594/pangaea.548897
title: Nutrients and bacteria measured on water bottle samples at station Chan_2003-01-09_5, Chanavallita, Chile
DOI: 10.1594/pangaea.874555
title: Ozone measurements from Neumayer Station (2016-10)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.829525
title: Meteorological records from the Vernagtferner Basin - Vernagtbach station, for the year 2011
DOI: 10.1594/pangaea.849447
title: Ground-penetrating radar (GPR) point measurements of ice thickness on Gurgler Ferner in 1998
DOI: 10.1594/pangaea.496456
title: Water temperature IBT profiles from cruise U999973052I_1973
DOI: 10.1594/pangaea.668869
title: Basic measurements of radiation at station Carpentras (2001-08)
DOI: 10.1594/pangaea.785192
title: Basic measurements of radiation at station Eureka (2011-03)
DOI: 10.1594/pangaea.761107
title: (Table 1a) Contents of aluminum, manganese, iron, phosphorus, and their reactive forms in surface sediments of the Barents Sea
DOI: 10.1594/pangaea.826417
title: P-Wave velocity (PWC) from IODP Hole 329-U1367B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.694780
title: Temperature and salinity in the water column of the Ionian Sea at Station SEPT-2000-IRI20A

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.671867
title: Basic measurements of radiation at station Regina (2002-04)
DOI: 10.1594/pangaea.793189
title: (Table 2) Geochemical composition of suspended matter samples from the northern Dvina River

description: The results of the analysis of samples of the Northern Dvina River's suspended particulate matter obtained by the sedimentation method from large water volumes in the periods of the spring high water and summer low water are presented. By the method of sequential leaching using different reagents, four fractions have been separated: the F1 is the sorbed complex and carbonates, the F2 is the amorphous hydroxides of Fe and Mn, the F3 is the form connected with the organic matter, and the F4 is the residual or silicate-detrital (inert) form. The data have shown that all ten elements determined were grouped with respect to the ratio of the distinguished forms: F4 is the predominant form for Al and Fe (73-88% of all the forms; however, the summer sample contains only 38% of this form of iron, and F2 is the predominant form for this period with 46.6%). As to Mn, the F1, F2, and F4 are nearly equally distributed in the spring high water samples, and only the F3 form is less important (5.4%). In the summer sample, the manganese sorbed complex is predominant (53.5%); for Cu, Ni, Cr, and Co, the inert F4 form is predominant (60-70%) in the sample of the spring suspended matter. The summer low water suspended matter has a lower F4 contribution (25-45%); for Zn, Pb, and Cd, the equal distribution of the forms in the spring samples is typical, while the summer suspended matter differs by the F2 form's predominance (53-61% for Zn and Pb). The main conclusion from the acquired data is that the geochemical mobility of all the studied elements, except for cadmium, in the summer low water suspended matter is higher than in the spring suspended matter. The more intensive biogeochemical processes in August, the high level of organic matter, and the higher contribution of phytoplankton lead to the intensification of the metals' geochemical activity in the Northern Dvina suspended matter in the end of the summer compared to the spring high water period when the physical processes are predominant over the biogeochemical ones due to the high speeds of the freshened waters flow.
description: Supplement to: Gordeev, Viacheslav V; Shevchenko, Vladimir P (2012): Forms of some metals in the suspended sediments of the northern Dvina River and their seasonal variations. Oceanology, 52(2), 261-270
DOI: 10.1594/pangaea.827317
title: Magnetic remanence from IODP Hole 329-U1368D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.700853
title: Medusae abundance during HEINCKE cruise HE201

description: Ship speed: 3 kn; heave speed: 0.5 m/sec; fier speed: 0.7 m/sec
DOI: 10.1594/pangaea.818637
title: (Table 1) alpha- and gamma-Hexachlorocyclohexane concentrations, salinity and temperature in brine and bulk sea-ice samples, eastern Beaufort Sea
DOI: 10.1594/pangaea.738446
title: (Table 8) Contents of foraminifera fragments, CaCO3, and mineral insoluble residue in different grain size fractions of Late Cenozoic sediments from DSDP Hole 45-395
DOI: 10.1594/pangaea.496616
title: Water temperature XBT profiles from cruise U99X122535_1996
DOI: 10.1594/pangaea.784372
title: Laser profiles of sea ice surface roughness during POL-ICE 2007 field campaign from flight POL-ICE07_200703111154
DOI: 10.1594/pangaea.678046
title: Expanded measurements from Neumayer Station (2004-09)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.793242
title: (Table 1) Oxides and carbonates at DSDP Sample 89-585A-18-6,84-88

description: DSDP Site 585 was selected for drilling the Central Old Pacific as a relic of the Mesozoic superocean Panthalassa. The basal lithologic unit recovered from Holes 585 and 585A is composed of a thick section of Aptian-Albian volcaniclastic turbidite deposits containing carbonate debris. On the basis of both microstructure and genesis, the carbonate debris consists of various shallow-water skeletal fragments, as well as at least two types of ooids. The most distinct change in the shallow-water skeletal debris observed within the unit is the type of large, benthic foraminifers. In the lower Aptian portion of the unit, forms having an affinity to Orbitolina texana (Roemer) are observed. In the upper Albian portion of the unit, these are replaced by large, benthic foraminifers of a complex, agglutinated type from the family Ataxophragmiidae. Microstructurally, the ooids have concentric laminations of micrite or radial needles. The radial needles are usually truncated by the next concentric layer. Fossil content indicates that the micritic ooids formed in two different environments. Some specimens contain shell fragments and miliolids, which provided nuclei for the formation of typical shallow- water ooids. Some ooids contain planktonic foraminifers. These planktonic foraminifers could have been washed into shallow-water environments during storms and subsequently incorporated into the development of ooids, but their presence may indicate development in a pelagic environment.
description: Sediment depth is given in mbsf. Missing values are below detection limit.
description: Supplement to: Haggerty, Janet A; Premoli Silva, Isabella (1986): Ooids and shallow-water debris in Aptian–Albian sediments from the East Mariana Basin, Deep Sea Drilling Project Site 585: Implications for the environment of deposition of the ooids. In: Moberly, R; Schlanger, SO; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 89, 399-412
DOI: 10.1594/pangaea.664855
title: Oceanography at CTD/bottle station IFREMER_1695
DOI: 10.1594/pangaea.677721
title: Ozone measurements from station South Pole (1993-02)
DOI: 10.1594/pangaea.811088
title: (Table 4) Nannoplankton occurrences in DSDP Site 90-588

description: Sediment depth is given in mbsf. Species abundance: A = abundant (&gt;50 specimens), C = common (25-49 specimens), and R = rare (&lt;25 specimens) - = absent, obtained by scanning an area measuring approximately 45 mm**2.
DOI: 10.1594/pangaea.771670
title: Physical oceanography during Walther Herwig III cruise WH257
DOI: 10.1594/pangaea.713880
title: Chlorophyll and Phaeopigments measured on water bottle samples at station Chipana_EW9Z2_25
DOI: 10.1594/pangaea.716637
title: Basic and other measurements of radiation at Neumayer Station (2008-10)
DOI: 10.1594/pangaea.792796
title: (Table 1) Major element oxides of glasses and basalts obtained during R/V Akademik Nikolaj Strakhov cruise ANS24
DOI: 10.1594/pangaea.498837
title: Physical oceanography from BT during cruise U90X007697B_1988
DOI: 10.1594/pangaea.800424
title: Physical oceanography and current meter data from mooring F12-1

description: Gear ID: 1, SN 10349; Gear ID: 2 CTD-SBE16, SN 1978; Gear ID: 3 CTD-SBE16, SN 2416; Gear ID: 4 AADI-ADCP, SN 47006; Gear ID: 5, SN 9219; Gear ID: 6, SN 9997
DOI: 10.1594/pangaea.779945
title: (Table 4) Quaternary calcareous nannofossil datums in ODP Hole 130-804C
DOI: 10.1594/pangaea.735573
title: Other measurements at 30 m from station Payerne (2009-10)
DOI: 10.1594/pangaea.758559
title: (Table 2) Textural analyses of the sand fraction of selected samples from lithologic Unit III glauconite sequence in ODP Hole 120-748C
DOI: 10.1594/pangaea.752925
title: Meteorological observations during WOOLWICH cruise from Carlisle Bay to Woolwich started at 1797-08-02
DOI: 10.1594/pangaea.793494
title: (Table 2) Major element composition of glasses from ODP Leg 135 basalt samples
DOI: 10.1594/pangaea.870937
title: Other measurements at 10 m from station Southern Great Plains (2013-08)
DOI: 10.1594/pangaea.548161
title: Nutrients and bacteria measured on water bottle samples at station Chip_2003-12-19_09, Chipana, Chile
DOI: 10.1594/pangaea.875860
title: Radiosonde measurements from station Lindenberg (2011-11)
DOI: 10.1594/pangaea.899019
title: Other measurements at 30 m from station Payerne (2018-11)
DOI: 10.1594/pangaea.903013
title: Continuous thermosalinograph oceanography along Heincke cruise track HE525
DOI: 10.1594/pangaea.735217
title: Other measurements at 30 m from station Payerne (2008-12)
DOI: 10.1594/pangaea.902066
title: Fraction of spectral solar radiance transmitted through snow and sea ice as measured in different depths under sea ice (transflectance) at station ALERT2018_22_1
DOI: 10.1594/pangaea.789132
title: Heat fluxes and surface radiation measurements from Samoylov Island, Lena Delta, Siberia, April to September 2007

description: In this article, we present a study on the surface energy balance of a polygonal tundra landscape in northeast Siberia. The study was performed during half-year periods from April to September in each of 2007 and 2008. The surface energy balance is obtained from independent measurements of the net radiation, the turbulent heat fluxes, and the ground heat flux at several sites. Short-wave radiation is the dominant factor controlling the magnitude of all the other components of the surface energy balance during the entire observation period. About 50% of the available net radiation is consumed by the latent heat flux, while the sensible and the ground heat flux are each around 20 to 30%. The ground heat flux is mainly consumed by active layer thawing. About 60% of the energy storage in the ground is attributed to the phase change of soil water. The remainder is used for soil warming down to a depth of 15 m. In particular, the controlling factors for the surface energy partitioning are snow cover, cloud cover, and the temperature gradient in the soil. The thin snow cover melts within a few days, during which the equivalent of about 20% of the snow-water evaporates or sublimates. Surface temperature differences of the heterogeneous landscape indicate spatial variabilities of sensible and latent heat fluxes, which are verified by measurements. However, spatial differences in the partitioning between sensible and latent heat flux are only measured during conditions of high radiative forcing, which only occur occasionally.
description: See doi:10.1594/PANGAEA.789131 for the period October 2007 to March 2008.
DOI: 10.1594/pangaea.788956
title: Documentation of sediment core M40/4_KL51
DOI: 10.1594/pangaea.706824
title: Basic and other measurements of radiation at station Barrow (2008-02), 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.867113
title: A suite of global, cross-scale topographic variables for environmental and biodiversity modeling, digital elevation model source: global 250 m GMTED, links to files in GeoTIFF format
DOI: 10.1594/pangaea.497801
title: Physical oceanography from BT during cruise U58X000053B_1960
DOI: 10.1594/pangaea.867114
title: A suite of global, cross-scale topographic variables for environmental and biodiversity modeling, digital elevation model source: near-global 90 m SRTM, links to files in GeoTIFF format
DOI: 10.1594/pangaea.499626
title: Physical oceanography from BT during cruise U99X000420B_1975
DOI: 10.1594/pangaea.673448
title: Radiosonde measurements from station Barrow (2004-04)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.587181
title: Physical oceanography at CTD station M1_CTD298 of the Persian Gulf
DOI: 10.1594/pangaea.735904
title: Radiosonde measurements from station Lindenberg (1995-12)
DOI: 10.1594/pangaea.680623
title: Other measurements at 30 m from station Payerne (2001-12)
DOI: 10.1594/pangaea.789821
title: Peatland depths and radiocarbon dates, recent decades, North America

description: Peatland ecosystems store about 500-600 Pg of organic carbon, largely accumulated since the last glaciation. Whether they continue to sequester carbon or release it as greenhouse gases, perhaps in large amounts, is important in Earth's temperature dynamics. Given both ages and depths of numerous dated sample peatlands, their rate of carbon sequestration can be estimated throughout the Holocene. Here we use average values for carbon content per unit volume, the geographical extent of peatlands, and ecological models of peatland establishment and growth, to reconstruct the time-trajectory of peatland carbon sequestration in North America and project it into the future. Peatlands there contain ~163 Pg of carbon. Ignoring effects of climate change and other major anthropogenic disturbances, the rate of carbon accumulation is projected to decline slowly over millennia as reduced net carbon accumulation in existing peatlands is largely balanced by new peatland establishment. Peatlands are one of few long-term terrestrial carbon sinks, probably important for global carbon regulation in future generations. This study contributes to a better understanding of these ecosystems that will assist their inclusion in earth-system models, and therefore their management to maintain carbon storage during climate change.
description: Supplement to: Gorham, Eville; Lehman, Clarence; Dyke, Arthur; Clymo; Janssens, Jan (2012): Long-term carbon sequestration in North American peatlands. Quaternary Science Reviews, 58, 77-82
DOI: 10.1594/pangaea.750985
title: Meteorological observations during NYMPHE cruise from Cape Verde to Simons Bay started at 1779-05-13
DOI: 10.1594/pangaea.840873
title: Expanded measurements from station Lindenberg (2007-03)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.920795
title: Age determination of sediment core LV53-19-1
DOI: 10.1594/pangaea.511180
title: Radiosonde at Georg-Forster station on 1989-08-22 12:00h

description: Height of tropopause 12171 m