cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.904028
title: Physical oceanography from mooring KPO_1177

description: instrument = Label:kpo_1177_02 File:kpo_1177_instr_02.nc Type:GEOMAR TD-Logger SN:79instrument = Label:kpo_1177_03 File:kpo_1177_instr_03.nc Type:Seabird MicroCat 37-IM mit P SN:03754instrument = Label:kpo_1177_04 File:kpo_1177_instr_04.nc Type:Aanderaa Optode 4330 SN:00216 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_05 File:kpo_1177_instr_05.nc Type:Seabird MicroCat 37-IM SN:01722 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_06 File:kpo_1177_instr_06.nc Type:Aanderaa Optode 3830 SN:01463 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_07 File:kpo_1177_instr_07.nc Type:Seabird MicroCat 37-SM mit P SN:10709instrument = Label:kpo_1177_08 File:kpo_1177_instr_08.nc Type:Aanderaa Optode 3830 SN:01469 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_09 File:kpo_1177_instr_09.nc Type:Seabird MicroCat 37-IM SN:01721 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_10 File:kpo_1177_instr_10.nc Type:Aanderaa Optode 4330 SN:00215 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_11 File:kpo_1177_instr_11.nc Type:Seabird MicroCat 37-SM SN:02247 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_12 File:kpo_1177_instr_12.nc Type:Aanderaa Optode 3830 SN:00206 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_13 File:kpo_1177_instr_13.nc Type:Seabird MicroCat 37-SM mit P SN:10609instrument = Label:kpo_1177_14 File:kpo_1177_instr_14.nc Type:Aanderaa Optode 3830 SN:00944 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_15 File:kpo_1177_instr_15.nc Type:Seabird MicroCat 37-IM SN:02933 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_16 File:kpo_1177_instr_16.nc Type:Aanderaa Optode 3830 SN:01074 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_17 File:kpo_1177_instr_17.nc Type:Teledyne RDI LongRanger 75 SN:02330instrument = Label:kpo_1177_18 File:kpo_1177_instr_18.nc Type:Seabird MicroCat 37-IM mit P SN:10696instrument = Label:kpo_1177_19 File:kpo_1177_instr_19.nc Type:Aanderaa Optode 4330 SN:00375 depth/pressure data was derived not measuredinstrument = Label:kpo_1177_20 File:kpo_1177_instr_20.nc Type:Seabird MicroCat 37-IMP mit P SN:10641
DOI: 10.1594/pangaea.917981
title: LOI of profile GRN-I

description: The sampling site was in an extensive blanket bog, 16 km south of Céide Fields Visitor Centre, where peat cutting had revealed many pine timbers and also oak timbers. This provided the opportunity to carry out a palaeoecological study that included pollen analysis and dendrochronological investigations. In the study area, the bedrock is Carboniferous sandstone which, to the east of the sampling area, gives way to Carboniferous limestone of the Moy valley. Here there are thick glacial deposits including well-developed drumlin fields, and the land is fertile and bogs are few.Core GRN I was taken where what appeared to be an isolated small pine stump (P2/W1) was present at ca. 58 cm in a turf bank (depth from the cutover surface; the uppermost peat (≥1 m) had been removed by peat cutters). At a lower level and in a drainage channel below the peat face, there were several pine timbers. A pine stump P1/W2) at this level from beside the core was 14C dated; pine stump P2 was also 14C dated. The age/depth model (Clam v. 2.2) for the pollen profile derives from a smooth spline curve (smooth factor = 0.4) fitted to ten 14C dates which includes two pine timber dates. The uppermost peat-derived 14C date, 1170±30 BP (10–8 cm; at least 1 m of peat had been removed by peat cutters), was regarded as unrealistically young and was not used.The pollen profile GRN I spans the interval ca. 5700–1800 BC. The pollen profile indicates that pine grew in the mire from the beginning of the record (5700 BC) to at least 2600 BC ('pine flush' recorded at 2700–2600 BC). This is supported by a Pinus stomatal record and also dendrochronological investigations of pine in the extensive bog at Garrynagran.The dendrochronological investigations enabled two floating chronologies to be constructed spanning the intervals 4530-4350 BC and 3135–2700 BC (fixed by 14C dates from dendro-matched pines). These data, together with the pollen data, serve to emphasise the importance of bog-pine in the region at ca. 3000 BC. Profile GRN I shows a distinct Elm Decline (but little P. lanceolata) that is followed by a Neolithic Landnam (3700–3300 BC). After a long lull in activity, farming impact begins to register again in a substantial way in the early Bronze Age (2300 BC). The macrofossil data provide evidence for mire development including a substantial role for Sphagnum austinii from ca. 2750 BC onwards.LOI and tephra investigations were also carried out. A distinct tephra layer was present (9–4 cm; highest tephra concentration at 6–5 cm; ca. 1450 BC based on age/depth model). The results of the tephra investigations have yet to be published.The research, most of which was carried out as a PhD project by Eneda Jennings (1997), was supported by Forbairt/Eolas (Irish Research Council) and NUIG Postgraduate Fellowship scheme.
DOI: 10.1594/pangaea.848434
title: Radiosonde measurements from station Sapporo (2015-05)
DOI: 10.1594/pangaea.917992
title: Macrofossils of profile BHY_V

description: The sampling site lies 25 m east of chamber of Behy court tomb where a small patch of intact uncut peat remained.A monolith 44 cm long was removed. Total depth of peat at sampling point (TDP; adjust for shrinkage) 180 cm.The pollen spectra (16 in all) start at 3 cm (i.e. 3–4 cm: mineral soil immediately beneath the peat) to -30 cm, i.e. 30 to 29 cm ABOVE the peat/mineral soil interface. Peat near the base (-7 to -19 cm) was charcoal-rich. The age/depth model gives the following chronology:[≥2600, pre-bog development]; pollen profile: 2520-210 BC, i.e. late Neolithic/Chalcolithic to mid-Iron Age. LOI and tephra investigations were also carried out. A distinct tephra layer at -28 cm (ca. 280 BC according to age/depth model). Tephra geochemically characterised. The results of the tephra investigations have yet to be published.The age/depth curve for BHY V is a smooth spline curve (smooth factor = 0.2) that is based on the five available 14C dates and a surface age estimate (peat thickness: 180 cm, i.e. 50 cm added to compensate for peat shrinkage. Surface peat is regarded as dating to AD 1950). This is the age/depth model used in the EGQSJ publication (in press, 12/2019).A 'pine flush' is not recorded but ca. 2% Pinus in mineral soil and basal peat samples; these samples dominated by Betula; little Calluna. Very sharp Betula to Poaceae switch near base (cf. hiatus). These investigations relating to Céide Fields were carried out in PRU, NUIG, part-funded by The Heritage Council (of Ireland). The aim was to provide an environmental context for the establishment and use of the prehistoric stone-wall field system, and an overall chronological framework and an environmental history of the area.
description: Macroremains recorded in sievings from pollen samples. Abundance of macro-remains as follows: 3, abundant; 2, frequent; 1, occasional; 0.5, rare, i.e. +
DOI: 10.1594/pangaea.912694
title: Multichannel reflection seismic data of profile GeoB08-065
DOI: 10.1594/pangaea.937089
title: Soil health indicators for Central Washington Orchards

description: The objective of this study was to initiate the steps to develop a soil assessment tool for irrigated orchard soils in Central Washington, United States including defining objectives, gathering baseline data and selecting target indicators.A total of 97 apple (Malus domestica) orchard fields were sampled in Washington, United States between 2015 and 2020. Of these plots there were 30 matched pairs (60 plots) on the same or similar soil type with matching cultivar/rootstock, tree age and training system type. One field in each pair was high performing and the other underperforming based on grower description. A subset of 32 plots (16 matched pairs) were sampled for fruit yield and fruit quality. Soil samples were collected as 50 to 100-soil core composite samples (2.5 cm core) to a depth of 20 cm in the tree root zone (15-60 cm from trunk) where 10 to 20 random samples were taken in each of five locations of the 2 to 16 hectare field. Four 100 cm3 intact soil cores were used for bulk density analysis. Five 120 cm3 intact cores were taken for micro-arthropod analysis. All soil sampling was conducted during June and July after soils had warmed (&gt;13 °C) and 1 to 3 months before apple harvest. Water supply for each orchard site was determined using a grower survey of irrigation practices and on-site irrigation measurements and demand was estimated from evapotranspiration estimates based on meteorological data from the nearest weather station [1]. On site irrigation measurements included measurements of water volume per emitter per hour at ten locations within a block which was then multiplied by emitters per acre. Fields with insufficient irrigation were not included in matched plot analysis.Fruit yield and quality were determined by collecting grower reported packing house yield data for the previous two to four years where available. For orchards where packing house data was not collected, a subset of five representative trees were selected for each orchard. At harvest, fruit per tree were counted and 20 fruit per tree collected to determine mean fruit weight and to estimate total yield. Yield was normalized to a 0-100 scale (percent yield goal) where the reported yield was divided by the yield goal identified by the grower in order to account for the yield potential of individual varieties and growing systems.
description: Empty cells = NAPenetration resistance = Measured using a penetrometer in pounds per square inch (psi) (Dicky-john Corp, Auburn, IL) at field capacity. Slow even pressure was applied. The highest pressure reading was recorded for the surface 0-15 cm and proximate 15-45 cm.
DOI: 10.1594/pangaea.825491
title: P-Wave velocity (PWL) from IODP Hole 329-U1370D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.633951
title: Sea-bed images of permanent plots of rocky benthos at Medes, site Pota de Llop, plot V4D

description: Area monitored at each permanent plot: 310 cm²
DOI: 10.1594/pangaea.711082
title: (Supp. Fig.) Shear strength of sediment core JR104-GC362
DOI: 10.1594/pangaea.775705
title: Continuous meteorological observations at station Ny-Ålesund (2010-12)
DOI: 10.1594/pangaea.912692
title: Multichannel reflection seismic data of profile GeoB08-032
DOI: 10.1594/pangaea.633990
title: Sea-bed images of permanent plots of rocky benthos at Marseille, site Riou Sud, plot R1E

description: Area monitored at each permanent plot: 310 cm²
DOI: 10.1594/pangaea.912693
title: Multichannel reflection seismic data of profile GeoB08-050
DOI: 10.1594/pangaea.912695
title: Multichannel reflection seismic data of profile GeoB08-070
DOI: 10.1594/pangaea.846708
title: Radiosonde measurements from station Boulder (2015-03)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.684643
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station MARCH-1997-GN36199704603MNB04 in the Aegean Sea

description: For determining POC and PON concentrations 1 to 5 litres (depending on the distance of the station from the coast and the depth layer sampled) were filtered through Whatman GF/F filters (2.5 cm diam.). Then these filters were wrapped in aluminium foil and stored at -22°C until analysing in the laboratory.
DOI: 10.1594/pangaea.496684
title: Physical oceanography from BT during cruise IHUXXB_1982
DOI: 10.1594/pangaea.711086
title: (Supp. Fig.) Shear strength of sediment core JR104-GC370
DOI: 10.1594/pangaea.922409
title: Water levels reconstructed and measured by H.C. Russell (1820–1886)

description: Lake George water levels for the period 1820–1886, reproduced from the reconstruction and measurements of Henry Chamberlain Russell. The data were digitised from the hydrograph diagrams presented in Russell (1886). Dates are given as the 15th day of the month but should only be treated as indicative because no dates were given in the original publication. The levels were surveyed based on sites located at several locations around Lake George. From February 1885, Russell collected monthly measurements from a site located on the SW shore (approximately 35.184°S, 149.400°E).
DOI: 10.1594/pangaea.922445
title: Water levels measured by ACTEW/Icon Water (2006–2013)

description: Lake George water levels for the period 2006–2013, provided courtesy of, and with approval from (pers. com. T. Purves, Icon water, to M. Short, 2020) Icon Water (formerly ACTEW). The values are daily averages of measurements collected at an hourly frequency. The data are freely-available from the National Collaborative Research Infrastructure Strategy (NCRIS) Super Science Groundwater Portal (NCRIS, 2019). The Icon Water measurements were collected from a sensor located on the lakebed near Rocky Point (35.092°S, 149.465°E). The surface water sensor could only detect water above a depth of 0.45 m.The full dataset on the NCRIS website also includes water levels for the period 2013-2015 but they are not included here because measurements collected from August 2013 by researchers at the Australian National University were able to detect lower levels, as well as record temperature and electrical conductivity.
DOI: 10.1594/pangaea.775686
title: Continuous meteorological observations at station Ny-Ålesund (2009-05)
DOI: 10.1594/pangaea.830238
title: Core summary for IODP Hole 338-C0021B
DOI: 10.1594/pangaea.824583
title: Point measurements of magnetic susceptibility from IODP Hole 318-U1361A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.913417
title: Collected tsetse tissue and tsetse species (Glossina sp.) collected in protected and tsetse invested areas in Nigeria

description: This data set includes data from a tsetse (Glossina sp.) collection carried out in Nigeria between 2014 and 2016. Traps were employed for one to three days in four different National Parks, one Game Reserve and two tsetse invested areas. Each tsetse was identified morphologically and dissected in the field. Wings were removed and stored dry. Legs were immersed in a DNA-preservation agent. Salivary glands and ovaries were dissected and stored in a DNA-preservation agent. The whole gut was dissected, homogenized in the field and partially preserved for DNA analysis and used to investigate for sialidase activity. The data table summarizes the available tissue, sex and species information for each dissected specimen.Species collected were G. morsitans submorsitans, G. tachinoides, G. palpalis palpalis and several unidentified Glossina species.
DOI: 10.1594/pangaea.936764
title: Basic measurements of radiation at station Newcastle (2019-07)
DOI: 10.1594/pangaea.665317
title: Oceanography at CTD/bottle station IFREMER_2157
DOI: 10.1594/pangaea.875897
title: Radiosonde measurements from station Ishigakijima (2017-03)
DOI: 10.1594/pangaea.824592
title: Thermal conductivity of IODP Hole 318-U1361A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.888592
title: Large area scan macroscope images of ice core samples (vertical thin sections, full bag measurements) collected from the polar ice core EDML, 2359-2380 m depth (2015)

description: 39 vertical thin sections measured with Large Area Scanning Macroscope.Size of thin sections: ca. 6.7 x 9 cm²Resolution: 2000 px/cm (LASM), images are horizontally mirrored to each other.Measured at Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany.
DOI: 10.1594/pangaea.881411
title: Radiosonde measurements from station Barrow (2013-10)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.733355
title: Documentation of sediment core MSM12/646-1
DOI: 10.1594/pangaea.834391
title: Ceilometer raw data measured at Neumayer Station (2014-01), links to files
DOI: 10.1594/pangaea.913420
title: Sialidase assay and analysis of free sialic acid in tsetse (Glossina sp.) collected in protected and tsetse invested areas in Nigeria

description: This data set includes results of a sialidase assay applied in tsetse gut tissue from a tsetse (Glossina sp.) collection carried out in Nigeria between 2014 and 2016. Traps were employed for one to three days in four different National Parks, one Game Reserve and two tsetse invested areas. Each tsetse was identified morphologically and dissected in the field, all tissues preserved and used for further analysis. The whole gut of each tsetse was homogenized in the field and partially preserved for DNA analysis and used to investigate for sialidase activity with a fluorescent substrate and a natural substrate. Analysis for sialidase activity was done by fluorescent measurement and reverse phase HPLC of processed gut samples.
DOI: 10.1594/pangaea.711079
title: (Supp. Fig.) Shear strength of sediment core JR104-GC358
DOI: 10.1594/pangaea.829968
title: XRF-core logger measurements from IODP Hole 338-C0002L

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.737279
title: Sea surface temperature reconstruction from sediment core TY93929/P using alkenones
DOI: 10.1594/pangaea.833077
title: Stable isotope ratios of foraminifera from Hole 104-642B

description: Specimens picked by Dorothee Spiegler. Isotope data measured by Kyaw Winn in 1988 with the CARBO KIEL Massenspectrometer Finnigan MAT 251, Christian-Albrechts-University, Kiel, Germany.
DOI: 10.1594/pangaea.902831
title: Profile of vertical fish echo sounding with Simrad EK60 during Jan Mayen cruise (July 2009) with links to raw data files
DOI: 10.1594/pangaea.936768
title: Basic measurements of radiation at station Newcastle (2019-11)
DOI: 10.1594/pangaea.893160
title: Daily large hail probability on a global scale (1979 to 2015), Version 2, link to netCDF files

description: This is an updated version of a dataset that contains daily gridded hail hazard estimates on a global scale for the period 1979 to 2015. It is based on the presence of environmental conditions in which large hail (diameter &gt;2.5 cm) has been observed. The data is provided on a global grid with 0.7°x07° grid spacing. The hail risk varies between zero and one where one means a high probability that the location will experience large hail on a corresponding day.
description: Supplement to: Prein, Andreas F; Holland, Greg (2018): Global estimates of damaging hail hazard. Weather and Climate Extremes, 22, 10-23
DOI: 10.1594/pangaea.758289
title: Meteorological data from Jubany Station, King George Island, Western Antarctic Peninsula, 1988
DOI: 10.1594/pangaea.611377
title: Documentation of ice wedge Mak-IW-18
DOI: 10.1594/pangaea.912345
title: Pore water sulfate and chloride concentrations of MeBo sediment core GMMB08 collected in the area of Pockmark A
DOI: 10.1594/pangaea.936761
title: Basic measurements of radiation at station Newcastle (2019-03)
DOI: 10.1594/pangaea.911674
title: Trace metal concentrations and isotope compositions from drill core OPH of the Zaonega Formation, NW-Russia

description: This dataset contains molybdenum and uranium concentrations; uranium isotope compositions; pertinent major element concentrations; and total organic carbon contents of black shales from the ~2 Ga upper Zaonega Formation, NW-Russia. The samples originate from the Onega Parametric Borehole (OPH). This data was collected via X-ray fluorescence spectroscopy, multi-collector inductively-coupled plasma mass spectrometry and carbon analysis.
DOI: 10.1594/pangaea.633923
title: Sea-bed images of permanent plots of rocky benthos at Medes, site Carall Bernat, plot CBB3Ecostat

description: Area monitored at each permanent plot: 310 cm²
DOI: 10.1594/pangaea.914604
title: Output velocity profile from core-log-seismic integration (CLSI) of IODP Site 381-M0078
DOI: 10.1594/pangaea.611379
title: Documentation of ice wedge Mak-IW-20
DOI: 10.1594/pangaea.496297
title: Water temperature MBT profiles from cruise U90X097112M_1976
DOI: 10.1594/pangaea.829963
title: (Table S1) Geochemistry of ODP Hole 39-356

description: Sediment depth is given in mcd. Scanned at the Center for Marine Environmental Sciences at the University of Bremen (22-23 June 2009), with 1cm**2 footprint and a 30 second count time for 10kV (100µA) and 50kV (800µA).
DOI: 10.1594/pangaea.935844
title: Resin extracted wood δ13C content and lumen length of sample NacPi20_2007_iso
DOI: 10.1594/pangaea.843684
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE375, Bremerhaven - Bremerhaven, 2012-03-30 - 2012-04-05
DOI: 10.1594/pangaea.860385
title: Radiosonde measurements from station Desert Rock (2009-08)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.552440
title: Nutrients measured on water samples at stations E1 and E2, Atenas, Independence Bay, Peru (2005)
DOI: 10.1594/pangaea.759003
title: Multibeam survey and contour maps from BELGICA cruise BG08/13a
DOI: 10.1594/pangaea.902953
title: Directional Wave Buoy at 17 m Depth at USACE Field Research Facility 1996-2018

description: USACE / FRF has maintained wave buoys around the 17 m and/or 20 m depth contour since 1980. Over the years, we have used three different types of waverider buoys manufactured by Datawell B.V. (Haarlem, Netherlands). From 1980 until 1996, we used non-directional buoys, first the 0.7 m hull diameter design and then the 0.9 m hull diameter design. The buoys operate by recording the output of an accelerometer suspended in fluid and gimbaled (Hippy-40). For data prior to September 1986, data were recorded at 2 or 4 Hz and record lengths were either 34 or 17 minutes, respectively. Collection intervals were either three hours or six hours. From September 1986 to November 1996 data was collected hourly. Frequency spectra were computed using the Welch method with 50% overlapped ensembles [1]. From the end of 1996 onward, we have maintained 0.9 m hull diameter Directional Waverider MkII and MKIII buoys [2] that, in addition to vertical acceleration, also measure two orthogonal components of horizontal acceleration. From Feb 1997 to May 2005, time series were collected at 1.28 Hz and cross-spectral analysis was performed on shore [3, 4]. Between May 2005 and May 2013, directional Fourier coefficients computed on-board the buoy and transmitted onshore. Since May 2013, data analysis has been manged through the Coastal Data Information Program (CDIP), UCSD San Diego, CA. Data are transmitted via an Iridium satellite link at half-hour intervals. Two dimensional (2D) frequency-direction spectra are computed using an Iterative Maximum Likelihood Estimator (IMLE) method [5].For more information see FRF data paper, FRF website and data portal, and CDIP website.[1] Welch, P (1967) [2] de Vries, JJ (2014) [3] Longuet-Higgins, M.S., Cartwright, D.E. and Smith, N.D. (1963)[4] Earle, M.D., Steele, K.E. and Wang, D.W.C. (1999)[5] Oltman-Shay, J. and Guza, R.T. (1984)
DOI: 10.1594/pangaea.779209
title: Corephotos from IODP Hole 317-U1351B

description: Geocode = Depth CSF-A (m). These files are stored as PNG images at 2200 X 3400 pixels.The layout displays the archive halves of an entire core laid out left to right (top of core to bottom) with color and meter rule references.
DOI: 10.1594/pangaea.821917
title: XRD raw data from IODP Exp337
DOI: 10.1594/pangaea.777216
title: Xray-ct-scanner images from IODP Hole 331-C0013D

description: Geocode = [m CSF-A] Top Core depth (below sea floor). Measurements data just above (negative section depth) and below (depth exceed section length) a core section are utilized in the deconvolution (http://en.wikipedia.org/wiki/Deconvolution).