cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.872522
title: Meteorological measurements in Cordoba, Argentina from September 1873- December 1888, digitized version

description: At the end of 1877 installed automatic instruments. Temperature: The thermometer was hanging in a wooden box with shutters in the east and west face and open the south face. The box was at the exterior or a window oriented to the south located 1.5m above the ground and 50cm distant from the window. The thermometer was constructed by the Negrtti and Zambra. About the Monthly mean temperature, during the first five Years the thermometer was observed at 7, 14, 21 these observations have been corrected by the automatic observations during 1878-1887. The correction were January (-0.5), February (-0.26), March (-0.1), April (-0.07), May (-0.25), June (-0.24), July (-0.18), August (-0.07), September (-0.19), October (-0.45), November (-0.57) and December (-0.58). Solar irradiation: Measured with thermometers in a black storage and vacuum, constructed by Negretti and Zambra, the thermometer was 0.25 cm above the grass and it is exposed from 9 to 16 the non-completely covered Days. We have rescued the Monthly max observed. Barometer: From 1873 to 1877 the mean is the result of the three observations taken at 7h, 14h, 21h. The instrument used during this period was: i) from the 1872 to 31st May 1875 a Fortin barometer that's required a correction of +0.64mm, ii) from 1st June 1875 to end of 1877 used another fortin barometer that needs a correction of +0.01mm. From 1878 to 1883 used an automatic aneroid barometer that recorded the pressure each hour. During 1886 and 1887 used the Sprung barograph. The 20th of May 1885 the barometer was moved to a different place. All the correction for the use of the different barometers and the change of location have been corrected by the author. Solar Brightness: Monthly hours of sun registered by the heliograph from March 1886 to December 1888. The heliograph was constructed by Negretti and Zambra. Precipitation [mm]: The rain gauge has a 12cm diameter and is located 1.7m above the ground. The stronger snowfall was 1st August 1877 from the 5 to 10 in the morning arriving to 26 cm depth. Evaporation: Two evaporimeters with a circumference of 314cm and 10cm height one at sun and one at shade.---The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.724107
title: Other measurements at 10 m from station Southern Great Plains (2002-03)

description: Version 2, 2009-07-07
DOI: 10.1594/pangaea.872756
title: Ultra-violet measurements from station Boulder, SURFRAD (2014-07)
DOI: 10.1594/pangaea.785948
title: (Table 3) List of samples assigned to different larger benthic foraminifer associations in ODP Leg 133 holes
DOI: 10.1594/pangaea.742546
title: (Table 2) Chemical element contents in the surface sediment layer on the submeridional section through the Eastern Pacific

description: Paper devoted to geochemistry of antimony in metalliferous and transitional sediments from the Southeast Pacific.
description: Contents are given on carbonate-free biogenic silica-free basis.
description: Supplement to: Gurvich, Evgeny G; Bogdanov, Yury A; Kurinov, Anatoly D; Katargin, Nikolay V (1976): Antimony in metalliferous sediments of the Pacific Ocean. Oceanology, 16, 279-283
DOI: 10.1594/pangaea.552438
title: Nutrients measured on water samples at stations E1 and E2, Atenas, Independence Bay, Peru (2004)
DOI: 10.1594/pangaea.872523
title: Meteorological measurements in Nassau, Bahamas from September 1852- December 1854, digitized version

description: March: Observations from 22 to 31 discontinued on account of the very serious illness of Captain Rimmintogton. April: Observations very much interrupted by sickness among the officers of the department. May: Observations interrupted between 4-9 by sickness. October: A most tremendous hurricane, lasting from the 21-24 of this Month. November: 22 the wind increased to a hurricane; the barometer fell very low, and the mercury oscillated very much, between the hours of 5 p.m., on the 22 and 1 a.m. on the 23. The night was excessively dark, and the wind came in squalls. Observations for November, December (1853) and January (1854) not quite full, on account of the instruments not being in good condition.---The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.944532
title: Biomarker data of Core CB1 from the Cygnet Bay, north-western Australia

description: The sediment core was collected from a pearl aquaculture area, northwest Australia using a push corer by SCUBA divers in 2011. After collections, the core was sectioned into sub-samples at 1 cm intervals, weighed and freeze dried before being reweighed and then stored in a freezer at -20°C before biomarker analysis. The chronology used 210Pb and 137Cs radiometric-dating techniques, which generated a sedimentation rate of 1.11 cm/yr. The sterol and long chain n-alkane contents were determined by GC (Agilent 7890 A) with an FID detector and a HP-1 column . The GDGTs contents used for calculating TEX86H index were determined by HPLC-MS (Agilent 1200/Waters Micromass-Quattro UltimaTM Pt) with APCI probe and Prevail Cyano Column.
DOI: 10.1594/pangaea.691154
title: Nutrient concentrations in water samples collected at Station JUNE-94-GN3619940280200420 in the Aegean Sea
DOI: 10.1594/pangaea.783351
title: (Table S2) XRF core scanning Fe intensity data from ODP Site 1262

description: DEPTH, sediment = Depth (mbsf)
DOI: 10.1594/pangaea.674115
title: Radiosonde measurements from station De Aar (2000-11)
DOI: 10.1594/pangaea.943610
title: Holocene diatom data from Lake Tavatui (Russia): diatom abundances and quantitative reconstructions of lake water parameters
DOI: 10.1594/pangaea.872183
title: Water temperature at time series station Soledad, Paso Comau, Patagonia, Chile in 2015/2017

description: This dataset was generated in the frame of the co-operation between the Huinay Scientific Field Station (http://www.huinay.cl) and the Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research (http://www.awi.de).
DOI: 10.1594/pangaea.687214
title: Chlorophyll a in three size fractions from bottle APRIL-2000-K4

description: Separate filtration through polycarbonate Millipore filters having porosities 0.2 (total stock), 1.2 and 3.0µm.
DOI: 10.1594/pangaea.780319
title: (Table T1) Stratigraphic distribution of phytoliths at ODP Site 188-1165 and 188-1166 sediments (continental slope)

description: Rare phytoliths are described from Late Cretaceous to Quaternary deep-sea sediments from Sites 1165 and 1166, Prydz Bay, East Antarctica. The phytoliths are comparable to modern tree/shrub, grass, and fern forms, although some may be modern contaminants. Spherical tree/shrub phytoliths are the most common, occurring particularly in the lower middle to middle Miocene core sections at Site 1165. All phytolith forms observed (except irregular and folded sphericals) have been previously described in other Antarctic sediments. The low phytolith abundances in the cores probably result from a combination of factors including the substantial distance offshore of the drill sites, taphonomic influences (low source production, soil dissolution, and dilution of terrigenous material during transport and deposition), and silica diagenesis downhole.
description: Sediment depth is given in mbsf. X = present, R = rare and poorly preserved fragments, - = not found. # = possible contaminant. Numbers represent counts of distinctive phytoliths.
description: Supplement to: Thorn, Vanessa C (2004): Data report: Phytoliths in drill core sediments from Sites 1165 and 1166, Leg 188, Prydz Bay, East Antarctica. In: Cooper, AK; O'Brien, PE; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 188, 1-12
DOI: 10.1594/pangaea.477443
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/94-1

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.777048
title: Nematode 13C isotope values from in situ feeding experiments in the Nazare Canyon conducted with sediments from ROV push-core JC10-131-PUC06

description: Nematode 13C isotope values (ca. 100 ind., per mil relative to PVDB standard)
DOI: 10.1594/pangaea.782626
title: (Table 32) Chemical composition of minerals from crystalline rocks of the Vernadsky Fracture Zone
DOI: 10.1594/pangaea.694131
title: Nutrient concentrations in water samples from the Aegean Sea at Station JUNE-1998-IR10
DOI: 10.1594/pangaea.746223
title: (Table 5) Stable oxygen isotope record of Globigerinoides ruber from ODP Site 108-662

description: Depth, sediment (m) is composite depth (mcd).
DOI: 10.1594/pangaea.778781
title: (Table T1) Ages and initial porosities of ODP Hole 194-1194A and 194-1198A sediments
DOI: 10.1594/pangaea.782698
title: Other measurements at 10 m from station Southern Great Plains (2010-09)
DOI: 10.1594/pangaea.859437
title: Stable carbon isotopes of core lipids from the Orca Basin, northern Gulf of Mexico
DOI: 10.1594/pangaea.669542
title: Underway carbon dioxide in the Indian Ocean of Marion-Dufresne cruise 35MF20050919
DOI: 10.1594/pangaea.672154
title: Radiosonde measurements from station South Pole (1997-03)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.674085
title: Radiosonde measurements from station Camborne (2004-10)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.829556
title: Dissolution rate spectra data of calcite single crystal and micrite material

description: The large discrepancy between field and laboratory measurements of mineral reaction rates is a long-standing problem in earth sciences, often attributed to factors extrinsic to the mineral itself. Nevertheless, differences in reaction rate are also observed within laboratory measurements, raising the possibility of intrinsic variations as well. Critical insight is available from analysis of the relationship between the reaction rate and its distribution over the mineral surface. This analysis recognizes the fundamental variance of the rate. The resulting anisotropic rate distributions are completely obscured by the common practice of surface area normalization. In a simple experiment using a single crystal and its polycrystalline counterpart, we demonstrate the sensitivity of dissolution rate to grain size, results that undermine the use of "classical" rate constants. Comparison of selected published crystal surface step retreat velocities (Jordan and Rammensee, 1998) as well as large single crystal dissolution data (Busenberg and Plummer, 1986) provide further evidence of this fundamental variability. Our key finding highlights the unsubstantiated use of a single-valued "mean" rate or rate constant as a function of environmental conditions. Reactivity predictions and long-term reservoir stability calculations based on laboratory measurements are thus not directly applicable to natural settings without a probabilistic approach. Such a probabilistic approach must incorporate both the variation of surface energy as a general range (intrinsic variation) as well as constraints to this variation owing to the heterogeneity of complex material (e.g., density of domain borders). We suggest the introduction of surface energy spectra (or the resulting rate spectra) containing information about the probability of existing rate ranges and the critical modes of surface energy.
description: Comparison of VSI rate data (histograms for dt = 4 h) with published calcite dissolution rates. Our (new) rate data are not simple means, but instead preserve the contribution of certain height step retreats that constitute a total rate spectrum.BP (Busenberg and Plummer, 1986).JR (Jordan and Rammensee, 1998).SC: single crystal
description: Supplement to: Fischer, Cornelius; Arvidson, Rolf S; Lüttge, Andreas (2012): How predictable are dissolution rates of crystalline material? Geochimica et Cosmochimica Acta, 98, 177-185
DOI: 10.1594/pangaea.902107
title: Expanded measurements from station Ny-Ålesund (2018-08)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.484900
title: Sea surface temperature data during cruise Harald_Hearfoger_18890228

description: Values of air and water temperature are corrected if corrections are given. If correction value is missing, it is taken 0.0. If correction is given for a range of temperature, particular value is computed by linear interpolation.
DOI: 10.1594/pangaea.677389
title: Ozone measurements from station Ny-Ålesund (1994-10)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.848814
title: Abundance of mesozooplankton during the long-tern mesozooplankton analysis in Sevastopol Bay from 1976 to 2003

description: The present dataset includes results of analysis of 227 zooplankton samples taken in and off the Sevastopol Bay in the Black Sea in 1976, 1979-1980, 1989-1990, 1995-1996 and 2002-2003. Exact coordinates for stations 1, 4, 5 and 6 are unknown and were calculated using Google-earth program. Data on Ctenophora Mnemiopsis leidyi and Beroe ovata are not included. Juday net: Vertical tows of a Juday net, with mouth area 0.1 m**2, mesh size 150µm. Tows were performed at layers. Towing speed: about 0.5 m/s. Samples were preserved by a 4% formaldehyde sea water buffered solution. Sampling volume was estimated by multiplying the mouth area with the wire length. The collected material was analysed using the method of portions (Yashnov, 1939). Samples were brought to volume of 50 - 100 ml depending upon zooplankton density and mixed intensively until all organisms were distributed randomly in the sample volume. After that 1 ml of sample was taken by calibrated Stempel-pipette. This operation was produced twice. If divergence between two examined subsamples was more than 30% one more subsample was examined. Large (&gt; 1 mm body length) and not abundant species were calculated in 1/2, 1/4, 1/8, 1/16 or 1/32 part of sample. Counting and measuring of organisms were made in the Bogorov chamber under the stereomicroscope to the lowest taxon possible. Number of organisms per sample was calculated as simple average of two subsamples meanings multiplied on subsample volume. Total abundance of mesozooplankton was calculated as sum of taxon-specific abundances and total abundance of Copepods was calculated as sum of copepods taxon-specific abundances.
DOI: 10.1594/pangaea.674095
title: Radiosonde measurements from station Camborne (2005-08)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.777622
title: 11) Revised age model of sediment core EW9302-JPC2 for the Last Interglacial (period 134-110 ka)
DOI: 10.1594/pangaea.674080
title: Radiosonde measurements from station Camborne (2004-05)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.872426
title: Daily meteorological measurements in Corral, Chile from January 1871- December 1872, digitized version

description: The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.845363
title: Radiosonde measurements from station Ny-Ålesund (2014-03)

description: The Ny-Ålesund radiosonde program is part of the GCOS Reference Upper-Air Network (GRUAN). Please consider using the Ny-Alesund reference radiosonde data with higher temporal resolution and uncertainty values for all height levels, available via http://www.gruan.org.
DOI: 10.1594/pangaea.902111
title: Expanded measurements from station Ny-Ålesund (2018-10)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.674090
title: Radiosonde measurements from station Camborne (2005-03)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.677390
title: Ozone measurements from station Ny-Ålesund (1994-11)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.772476
title: Hydrochemistry measured on water bottle samples during cruise SEVER05

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.752908
title: Meteorological observations during Witte Cornelisz de Wit cruise from New York to Rotterdam started at 1853-01-27
DOI: 10.1594/pangaea.477432
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/84-1

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.779006
title: (Tables T3-T6) Chemical composition of pyrite in ODP sites 193-1188 and 193-1189
DOI: 10.1594/pangaea.767491
title: Rare earth element concentrations of zircons in ODP Hole 188-1167A sample 1167 A-37
DOI: 10.1594/pangaea.777638
title: 1) Revised age model of sediment core MD02-2488 for the Last Interglacial (period 136-108 ka)

description: Depth, sediment: Composite depth (corrected for voids within the sediment sections).
DOI: 10.1594/pangaea.934148
title: Physical oceanography during HEINCKE cruise HE574

description: Conductivity-temperature-depth profiles were measured using a Seabird SBE 911plus CTD during RV Heincke cruise HE574 between 12.04.2021 and 17.04.2021. Additional sensors included a WET Labs C-Star transmissometer and a WET Labs ECO-AFL fluorometer. Data were connected to the station book of the specific cruise as available in the DSHIP database. Processing of the data including removal of obvious outliers followed the procedures described in CTD Processing Logbook of RV Heincke (hdl:10013/epic.47427). A detailed report on the CTD data of HE574 is available at https://hdl.handle.net/10013/epic.7e2aff22-0a3b-4945-a6b4-4796811bb77e.
DOI: 10.1594/pangaea.779061
title: (Table 1) Mineral phases in selected samples of dolerites and basalts from ODP Leg 129 holes

description: + = analyzed, - = not analyzed
DOI: 10.1594/pangaea.807334
title: (Figure 3) Methane concentration profile and isotopic composition of sediment core M72/5_574-1 (14-GC1)
DOI: 10.1594/pangaea.807336
title: (Figure 3) Methane concentration profile and isotopic composition of sediment core M72/5_620-1 (22-GC4)
DOI: 10.1594/pangaea.872022
title: Changes in body mass of individual summer flounder juveniles
DOI: 10.1594/pangaea.759741
title: (Table 2) Age determination of ODP Hole 120-747A
DOI: 10.1594/pangaea.477428
title: Hydrochemistry measured on water bottle samples at station SAtl_1983-84_6N_0E/80-1

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.934954
title: Biology and morphometrics of dominant salp species in the subarctic Northeast Pacific

description: Salps are ubiquitous members of shelf break and offshore zooplankton communities in the subarctic Northeast Pacific. However, little is known about their species composition and biology compared to other regions in the Pacific. Seven salp species occur more or less frequently, whereas three of them numerically dominate: Cyclosalpa bakeri, Salpa aspera, and S. fusiformis. Two more southern salp taxa, Thalia democratica and Thetys vagina, not sampled since 2016, re-invaded the subarctic Northeast Pacific likely due to a series of marine heat waves. Specimens were collected during 1985–2020 using various gear types (BIONESS, Bongo net, midwater trawl, Multinet, neuston net, ring net, Tucker trawl) in the top 250 m (occasionally down to 1500 m) off the west coast of British Columbia, Canada. In total, approximately 1200 salp specimens were analysed. General salp biology, including life cycle stage and development stage compositions as well as body morphometrics (i.e., total length, oral-atrial length, embryo length, stolon properties, gut diameter) were measured. Species, size-, and stage-specific differences were compared. For the three dominant species and T. democratica, first biological and morphometric measurements in the subarctic Northeast Pacific are provided.
DOI: 10.1594/pangaea.859048
title: Stem radius change of Pine 396 at Site VISP in 2012
DOI: 10.1594/pangaea.871964
title: Soil moisture at Zackenberg valley, NE Greenland, July 2014

description: In July 2014, soil moisture (VWC %) was measured at Zackenberg valley, NE Greenland, at more than 4500 points. The measurements were conducted with a Hydrosense 2 Water content sensor with 12 cm rods (CS659). Many locations were revisited and measured again after some days / weeks. Many locations were already measured in 2013 (see "Related to:") and revisited in 2014. In general, it was a wet year at Zackenberg valley with late snowmelt.
DOI: 10.1594/pangaea.929011
title: Calibrated ages of Kimana (KIM) peat core from Kimana Game Reserve, Kenya

description: Calibrated ages of a high-resolution peat core from the Past Global Changes - Carbon in Peat on EArth through Time (PAGES_C-PEAT) Project.
DOI: 10.1594/pangaea.871717
title: Principles of ammonia excretion in mussels

description: The excretion of nitrogenous waste products in the form of ammonia (NH3) and ammonium (NH4+) is a fundamental process in aquatic organisms. For mytilid bivalves little is known about the mechanisms and sites of excretion. This study investigated the localization and the mechanisms of ammonia excretion in mytilid mussels. A Rh protein was found to be abundantly expressed in the apical cell membrane of the plicate organ which was previously described as a solely respiratory organ. The Rh protein was also expressed in the gill, although at significantly lower concentrations, but was not detectable in mussel kidney. Furthermore, NH3/NH4+ was not enriched in the urine suggesting that kidneys are not involved in active NH3/NH4+ excretion. Exposure to elevated seawater pH of 8.5 transiently reduced NH3/NH4+ excretion rates, but they returned to control values following 24h acclimation. This mussels had increased abundance of V-type H+-ATPase in the apical membranes of plicate organ cells: however, NH3/NH4+ excretion rates were not affected by the V-type H+-ATPase specific inhibitor concanamycin A (100 nM). On the other hand, inhibition of ciliary beating with dopamine and increased seawater viscosity significantly reduced NH3 excretion rates under control pH (8.0). These results suggest that NH3/NH4+ excretion in mytilid mussels takes place by passive NH3 diffusion across respiratory epithelia via the Rh protein, facilitated by the water current produced for filter feeding which prevents accumulation of NH3 in the boundary layer. This mechanism would be energy efficient for sessile organisms, since they already generate water currents for filter feeding.
description: Supplement to: Thomsen, Jörn; Himmerkus, Nina; Holland, Nicolas; Sartoris, Franz-Josef; Bleich, Markus; Tresguerres, Martin (2016): Ammonia excretion in mytilid mussels is facilitated by ciliary beating. Journal of Experimental Biology, 219(15), 2300-2310
DOI: 10.1594/pangaea.873877
title: (Table S2) Gamma ray log of the Wang-1 well
DOI: 10.1594/pangaea.926410
title: Calibrated ages of VM2-5 peat core
DOI: 10.1594/pangaea.477361
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/97-1

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.