cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.26341099
title: Data on the effect of combined pruning and thinning treatment on the phenotypes and biomass of selected trees and shrubs under exclosure management in Tigray, Ethiopia

description: This study investigated the effects of combined pruning and thinning on the phenotype and biomass of four tree and shrub species (Vachellia etbaica, Juniperus procera, Olea europaea subsp. cuspidata, and Euclea racemosa) in exclosures in Tigray, Ethiopia. The study aimed to evaluate the impact of pruning and thinning on the growth and biomass of these species, as well as the regeneration of vegetation, including grass cover and new plant species.<br>The researchers applied four treatments: control (no treatment), 25% pruning and thinning, 35% pruning and thinning, and 50% pruning and thinning. Measurements were taken over a period of three years to assess the effects on diameter at breast height and stump height, height, crown diameter, biomass, and seedling growth.<br>The results showed that pruning and thinning at varying intensities (25% and 35%) led to increased biomass of trees and shrubs, particularly for V. etbaica and O. europaea. O. europaea and J. procera showed larger seedling heights in the 25% pruning and thinning treatments compared to the other treatments. Additionally, grass cover was significantly increased in two of the study sites (Kihen and Tukul) following pruning and thinning treatments compared to the control.<br>The study concludes that pruning and thinning can have a positive impact on forest health and productivity by increasing biomass, growth of regenerated seedlings, and grass cover. The results suggest that tailored silvicultural management practices can improve productivity and biomass through selective pruning and thinning of tree and shrub species in exclosures.
DOI: 10.1594/pangaea.676994
title: Ozone measurements from station Barrow (1995-06)
DOI: 10.1594/pangaea.673435
title: Radiosonde measurements from station Barrow (2001-04)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.875845
title: Ozone measurements from station Lindenberg (2011-08)
DOI: 10.1594/pangaea.771330
title: (Table 2) Trace element composition of seleceted clast and matrix materials from ODP Site 125-786

description: Shipboard examination of volcanic and sedimentary strata at Site 786 suggested that at least four types of breccias are present: flow-top breccias, associated with cooling and breakup on the upper surface of lava flows; autobreccias, formed by in-situ alteration at the base of flows; fault-gouge breccias; and true sedimentary breccias derived from weathering and erosion of underlying flows. It is virtually impossible to assess the origin of breccia matrix by textural and mineralogical analyses alone. However, it is fundamental for our understanding of breccia provenance to determine the source component of the matrix material. Whether the matrix is uniquely clastderived can be determined by geochemical fingerprinting. Trace elements that are immobile during weathering and alteration do not change their relative abundances. A contribution to the matrix from any source with an immobile trace element signature different from that of the clasts would appear as a perturbation of the trace element signature of the matrix.Trace element analysis of bulk samples from clasts and matrix material in individual breccia units was undertaken in a fashion similar to that used by Brimhall and Dietrich (1987, doi:10.1016/0016-7037(87)90070-6) in analyzing soil provenance: (1) to help distinguish between sedimentary and volcanic breccias, (2) to determine the degree of mixing and depth of erosion in sedimentary breccias, and (3) to analyze the local provenance of the individual breccia components (matrix and clasts).The following elements were analyzed by X-ray fluorescence (XRF): Rb, Sr, Ba, U, Zr, Cu, Zn, Ti, Cr, and V. Of these elements, Zr and Ti probably exhibit truly immobile behavior (Humphris and Thompson, 1978, doi:10.1016/0016-7037(78)90222-3 ). The remaining elements are useful as a reference for the extent of compositional change during the formation of matrix material (Brimhall and Dietrich, 1987, doi:10.1016/0016-7037(87)90070-6).
description: Supplement to: Rigsby, Catherine A (1992): Data report: Trace element analysis of clasts and matrix in sedimentary and volcaniclastic breccias at Site 786. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 681-682
DOI: 10.1594/pangaea.858667
title: Spliced sequence of planktic foraminifera including POS287_26-1B, POS287_26-3G and D13902 samples
DOI: 10.1594/pangaea.676997
title: Ozone measurements from station Barrow (1995-09)
DOI: 10.1594/pangaea.677020
title: Ozone measurements from station Barrow (1998-07)
DOI: 10.1594/pangaea.776095
title: MSCL measurements from IODP Hole 331-C0013D

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.778822
title: (Table 1b) Microprobe analyses of websterites from the ophiolite complex in the Hunter Fracture Zone
DOI: 10.1594/pangaea.817824
title: (Table 3) Trace elements at DSDP Hole 66-487

description: Empty cells mean no data.
DOI: 10.1594/pangaea.677026
title: Ozone measurements from station Barrow (1999-05)
DOI: 10.1594/pangaea.875909
title: Basic and other measurements of radiation at station Toravere (2017-05)

description: Please note, that SWD, DIR, DIF and SWU nighttime negatives are set manually to zero (until end of August 2018).
DOI: 10.1594/pangaea.920050
title: Basic and other measurements of radiation at Neumayer Station (2019-10)
DOI: 10.1594/pangaea.676979
title: Ozone measurements from station Barrow (1993-06)
DOI: 10.1594/pangaea.677010
title: Ozone measurements from station Barrow (1997-05)
DOI: 10.1594/pangaea.676980
title: Ozone measurements from station Barrow (1993-07)
DOI: 10.1594/pangaea.875673
title: Other measurements at 10 m from station Bondville (2015-09)
DOI: 10.1594/pangaea.775584
title: Continuous meteorological observations at station Ny-Ålesund (2001-02)
DOI: 10.1594/pangaea.824741
title: P-Wave velocity (PWL) from IODP Hole 324-U1348A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.722263
title: Ultra-violet measurements from station Goodwin Creek (1998-11)

description: Version 2, 2009-06-24. UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-03.
DOI: 10.1594/pangaea.875659
title: Ultra-violet measurements from station Bondville (2015-02)
DOI: 10.1594/pangaea.719231
title: Radiosonde measurements from station Bondville (1995-12)

description: Version 2, 2009-06-15; Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.860748
title: Other measurements at 10 m from station Goodwin Creek (2009-07)
DOI: 10.1594/pangaea.775227
title: Thermal conductivity of IODP Hole 322-C0012A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.775279
title: (Table C1) 210Pb concentrations and age model of Baltic sea sediments

description: All sediment parameters corrected for salt dilution. Assumed background values: LF1 = 15.5 Bq/kg, LF1.5 = 16.0 Bq/kg, LF3 = 27.0 Bq/kg.
DOI: 10.1594/pangaea.888881
title: Daily gridded hail risk estimates on a global scale (1979 to 2015), link to netCDF files

description: This dataset contains daily gridded hail risk 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 0.75°x075° grid spacing. The hail risk varies between zero and one where one means a high probability that the location will experience large hail on the corresponding day.
description: VERSION 1, please refer to newer version ("Replaced by" reference)
DOI: 10.1594/pangaea.860400
title: Ultra-violet measurements from station Desert Rock (2009-12)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-08.
DOI: 10.1594/pangaea.824965
title: Penetrometer shear strength from IODP Hole 334-U1379C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.875678
title: Other measurements at 10 m from station Bondville (2015-11)
DOI: 10.1594/pangaea.859249
title: (Table 1, page 1376) Chemical Analyses of Manganese Nodules from the South-western Pacific

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.825078
title: Age determination results from site La_Flachere
DOI: 10.1594/pangaea.825081
title: Age determination results from site Padul
DOI: 10.1594/pangaea.701700
title: Basic and other measurements of radiation at station Barrow (2005-08), 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.719100
title: Ultra-violet measurements from station Bondville (2007-09)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.860394
title: Radiosonde measurements from station Desert Rock (2009-10)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.875614
title: BSIOM model results for the period 1971-2010: Frequency of available juvenile cod habitat (Fig. 3) and distribution of virtual drifters (Fig. 8)
DOI: 10.1594/pangaea.552374
title: Thick-section images of the EDML ice core from 0400 to 0500 m depth
DOI: 10.1594/pangaea.875703
title: Seasonal variations of Fucus vesiculosus fertility - tissue development in the Benthocosms (receptacles)
DOI: 10.1594/pangaea.875704
title: Seasonal variations of Fucus vesiculosus fertility - tissue development in the Benthocosms (reproductive allocation)
DOI: 10.1594/pangaea.701701
title: Basic and other measurements of radiation at station Barrow (2005-09), 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.875630
title: Hopane of sediment core PG2303-1
DOI: 10.1594/pangaea.875281
title: Sea ice drift, surface temperature, and barometric pressure from autonomous measurements from buoy 2015P5, deployed during POLARSTERN cruise PS89 (ANT-XXX/2)

description: Sea ice drift, surface temperature, and barometric pressure were measured by Surface Velocity Profiler 2015P5 drifting on Antarctic sea ice. The buoy was deployed on first year ice without drogue during POLARSTERN cruise PS89 (ANT-XXX/2). The time series describes the position and additional parameters of the buoy between 13 Jan 2015 and 06 Sep 2015 in sample intervals of 1 hour. The data set has been processed, including the removal of obvious inconsistencies (missing values).
DOI: 10.1594/pangaea.825671
title: Gas measurements from IODP Hole 329-U1365A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.875618
title: BSIOM model results for the period 1971-2010: Annually averaged available and occupied juvenile cod habitat and annually averaged number of virtual drifters representing successfully settled Baltic cod juveniles (survivors) (Figures 4-7)

description: ICES subdivisions in the central and eastern Baltic Sea Arkona Basin (ICES SD 24)Bornholm Basin (ICES SD 25)Gdansk Deep (ICES SD 26)Gotland Basin (ICES SD 28)
DOI: 10.1594/pangaea.897753
title: Other measurements at 30 m from station Payerne (2017-02)
DOI: 10.1594/pangaea.722066
title: Other measurements at 10 m from station Goodwin Creek (2007-10)
DOI: 10.1594/pangaea.770845
title: (Table 1) Strontium isotopic ratios of interstitial waters from ODP Leg 125 holes

description: The strontium isotopic data presented here are from interstitial waters squeezed from unconsolidated serpentine, an unusual type of substrate that was recovered from Mariana and Bonin forearc seamounts and has not been previously drilled by the Deep Sea Drilling Project or Ocean Drilling Program. The texture and composition of some of these serpentine deposits from Conical Seamount, located on the Mariana forearc, indicate emplacement as low- or high-viscosity, cold gravitational flows, which are therefore neither sediment nor igneous rock.The strontium isotopic ratios of the interstitial waters from the unconsolidated serpentine range from 0.70912 to 0.70525 and trend toward a relatively less radiogenic composition with increasing sub-bottom depth. These strontium isotopic ratios are derived from at least two strontium sources: seawater and igneous. The strontium isotopic gradients from the interstitial waters from the Leg 125 sites are probably the result of diffusive transport of strontium from an igneous source deep within the lithosphere that may be contaminated with subducted or underplated sediment.
description: Supplement to: Haggerty, Janet A; Chaudhuri, Sambhudas (1992): Strontium isotopic composition of the interstitial waters from Leg 125: Mariana and Bonin Forearcs. In: Fryer, P; Pearce, JA; Stokking, LB; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 125, 397-400
DOI: 10.1594/pangaea.668030
title: Basic measurements of radiation at station Boulder (2003-05)
DOI: 10.1594/pangaea.826285
title: Magnetic remanence from IODP Hole 330-U1372A

description: Geocode = Depth CSF-A (m)
DOI: 10.15468/dl.yydb88
title: Occurrence Download

description: A dataset containing 835 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is one of (Ciliosemina pedunculata (H.Karst.) Antonelli, Cinchona pedunculata H.Karst., Ladenbergia pedunculata (H.Karst.) K.Schum., Remijia pedunculata André, Remijia peruviana Standl.)"
 ]
}

 The dataset includes 835 records from 64 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031092-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.826416
title: P-Wave velocity (PWB) from IODP Hole 329-U1367B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.875631
title: Hopane in surface sediments off Herschel Island
DOI: 10.1594/pangaea.775582
title: Continuous meteorological observations at station Ny-Ålesund (2000-12)
DOI: 10.1594/pangaea.821517
title: Glacier mass balance Übergossene Alm, Austria, 1965-1975

description: The mass balance at the glacier Übergossene Alm has been measured with the direct/glaciological method during the Hydrological Decade IHD 1965-1975. The Übergossene Alm glacier (also: Hochköniggletscher) is a flat plateau glacier located between 2860 and 2480 m a.s.l. in the Northern Limestone Alps which showed signifcant retreat in the last decades. At Übergossene Alm, the intensive monitoring during the IHD included meteorological and hydrological measurements as well as ice thickness measurements. Until 1996, snow heights and surface elevation changes have been measured, which have been used to estimate mass balance. The surveys have been stopped as the glacier disintegrated in several smaller parts. Measuring mass balance at Übergossene Alm has been sophisticated, as the total area of this flat glacier was accumulation area in some years and ablation area in others. In addition to that, the glacier surface is exposed to wind drift, so that finding stable ablation or accumulation patterns for placing ablation stakes or snow pits have been difficult.
DOI: 10.1594/pangaea.860398
title: Radiosonde measurements from station Desert Rock (2009-11)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.875735
title: Stable isotopes of Globigerinoides ruber of sediment core MS21PC
DOI: 10.1594/pangaea.674093
title: Radiosonde measurements from station Camborne (2005-06)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.701702
title: Basic and other measurements of radiation at station Barrow (2005-10), 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.494740
title: Physical oceanography during cruise K90PO_1963
DOI: 10.1594/pangaea.719232
title: Other measurements at 10 m from station Bondville (1995-12)

description: Version 2, 2009-06-15
DOI: 10.1594/pangaea.775317
title: Color data from IODP Hole 331-C0013E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.701705
title: Ozone measurements from station Barrow (2005-10)
DOI: 10.1594/pangaea.775444
title: Continuous meteorological observations at station Ny-Ålesund (1995-10)
DOI: 10.1594/pangaea.792709
title: (Table 1) Magnetic hysteresis parameters for samples from ODP Hole 119-738C
DOI: 10.1594/pangaea.675479
title: Radiosonde measurements from station Payerne (2006-02)
DOI: 10.1594/pangaea.875326
title: Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2015S21, deployed during POLARSTERN cruise PS94 (ARK-XXIX/3)

description: Snow height was measured by the Snow Depth Buoy 2015S21, an autonomous platform, drifting on Arctic sea ice, deployed during POLARSTERN cruise PS94 (ARK-XXIX/3). The resulting time series describes the evolution of snow depth as a function of place and time between 25 Sep 2015 and 10 Aug 2016 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on first year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.
DOI: 10.1594/pangaea.711890
title: Pollen profile GOLHISH, Gölhisar Gölü, Turkey

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.890665
title: Diatom counts from sediment core MLC from the center of the Moss Lake, Washington, USA

description: Core collection was at Moss Lake, which is located within the Tolt River basin in King County in the Cascade foothills, approximately 530 km north east of Crater Lake (Mount Mazama). Moss Lake has a diameter of approximately 200 m with a maximum depth of 4.5 m. Data has been obtained from lake sediment cores from Moss Lake, Washington. Two cores were taken, one from the centre (MLC) and one from the fringe (MLF).
description: This data set provides raw count diatom abundances from the central core of Moss Lake. Depths are provided in the top row.Radiocarbon dates are provided in Egan et al (2016).
DOI: 10.1594/pangaea.774858
title: (Table 50) Chemical composition of calcareous crusts and nodules from the Mediterranean Sea
DOI: 10.1594/pangaea.774425
title: (Table 13) Representative Fe-Ti oxide analyses of ODP Hole 126-791B and Alvin samples

description: Cations based on 4 oxygens.
DOI: 10.1594/pangaea.789732
title: Basic and other measurements of radiation at station Barrow (1994-07)

description: Version 2, 2012-10-08
DOI: 10.1594/pangaea.708194
title: (Table 3) Chemical composition of strip samples from ODP Hole 118-735B
DOI: 10.1594/pangaea.496131
title: Water temperature MBT profiles from cruise U90X089162M_1973
DOI: 10.1594/pangaea.717335
title: Bioavailable carbohydrates, lipids, and proteins in sediment core 13368-026
DOI: 10.1594/pangaea.749748
title: Meteorological observations during IRENE cruise from Suriname to Barbados started at 1816-05-26
DOI: 10.1594/pangaea.901600
title: Beach profile data for the Elwha River Delta, 2016-02-18

description: Data were collected using GNSS survey methods, with a differential GPS operating in Real Time Kinematic (RTK) mode. Data from prior to 2013 were typically collected with a Magellan ProMark 3 traditional RKT-DGPS system (i.e. local base station and rover), with the base station sited on survey control markers installed in 1996, with survey control coordinates referenced to NAD83(CORS91). Starting in 2013 survey data were typically collected with an AshTech ProMark 200 RTK-DGPS system connected to the Washington State Reference Network. Survey data collected between January and November 2013 are referenced to NAD83(CORS96), and after November 2013 to NAD83(2011). Vertical data for surveys in 2012 and 2013 are referenced to NAVD88, presumably using Geoid96 (the survey control documentation does not specific a geoid). For all subsequent surveys the vertical data are referenced to NAVD88(Geoid09). No conversion were applied to these data to account for variations in horizontal or vertical coordinate system adjustments through time, but an error analysis suggests a standard deviation for the elevation data of between 0.03 and 0.05 m across the entire sampling period (2011-2018). All survey data were collected with the GNSS system mounted on a 2.05 m rover pole, held level as a transect line was traced in a cross-shore orientation on the beach. The associated text files include the horizontal (HRMS) and vertical (VRMS) root-mean-square errors estimated by the GNSS system, as well as the RTK-DGPS status reported by the GNSS system at the time each point was collected. Times are referenced to local Pacific time (either PST or PDT).
DOI: 10.1594/pangaea.789020
title: Basic and other measurements of radiation at station Alert (2008-02)

description: Temperature measurements not reliable!
DOI: 10.1594/pangaea.701706
title: Radiosonde measurements from station Barrow (2005-08)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.758288
title: Meteorological data from Jubany Station, King George Island, Western Antarctic Peninsula, 1987
DOI: 10.1594/pangaea.789731
title: Basic and other measurements of radiation at station Barrow (1994-06)

description: Version 2, 2012-10-08
DOI: 10.1594/pangaea.701707
title: Radiosonde measurements from station Barrow (2005-09)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km