cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.778761
title: Interstitial water analysis from IODP Hole 317-U1354A

description: Geocode = Top depth CSF-A (m). Chemical methods for interstitial water analysis aboard JOIDES Resolution; ODP Technical Note 15: http://www-odp.tamu.edu/publications/tnotes/tn15/technote15.pdf Analysis of major and trace elements in rocks, sediments, and interstitial waters by ICP-AES; ODP Technical Note 29 : http://www-odp.tamu.edu/publications/tnotes/tn29/TNOTE_29.PDF Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30: http://www-odp.tamu.edu/publications/tnotes/tn30/TNOTE_30.PDF
DOI: 10.1594/pangaea.805872
title: Geochemistry of sediment core PC-K40, Potter Cove, King George Island
DOI: 10.1594/pangaea.666894
title: Physical oceanography of CTD station 50 off Independencia Bay, 2005, Peru
DOI: 10.1594/pangaea.670248
title: Basic and other measurements of radiation at Neumayer Station (1999-05)
DOI: 10.1594/pangaea.909076
title: Daily mean visibility (1983-2018) at the Arctic meteorological station Hornsund, Spitsbergen

description: The horizontal visibility is quantified using observations made by meteorologists in the surroundings of the Hornsund Station with a marine scale that range from 1 to 9. The visual observations are performed using known distances to the surrounding mountains and other objects. Values 1 and 2 correspond to very bad visibility, 0-50 m and 50-200 m, respectively. Bad visibility (200 m - 1 km) is represented by value 3. Weak horizontal visibility represents conditions with 1-2 km and 2-4 km that are quantified as 4 and 5 in the applied scale. Moderate horizontal visibility, described as 6 in the scale, represent conditions when an object or light can be clearly discerned from 4-10 km. Good horizontal visibility (7 in the scale) is 10-20 km, very good (8) 20-50 km and extremely good (9) is for horizontal visibility larger than 50 km.
DOI: 10.1594/pangaea.729894
title: Meteorological synoptical observations from station Tateno (2009-07)
DOI: 10.1594/pangaea.887964
title: (Table 1, page 155) 10Be analysis of TECHNO-1 ferromanganese crust recovered from the Pacific Ocean

description: Before analysis the samples were scraped out from the Mn crust and leached in 6MHCl and the part analysed was further separated by complete dissolution in HF. Aluminium was then precipitated with NH4OH and Fe, Mn and Th were removed by further dissolution in NaOH.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.871149
title: Biomass water content at Zackenberg valley, NE Greenland, 2013-07

description: The purpose of this work was to determine the biomass water content.Biomass was harvested at Zackenberg valley, NE Greenland, at 27-29 July 2013 at 20 locations. At every location, 3 replicates were taken with a size of 20x20cm each. All above-ground biomass was harvested and packed in plastic bags with zippers. Immediately after harvesting, the biomass was brought to the lab, weighted and oven dried until the weight did not change for 24 hours.Soil moisture was measured at each location. The moisture value is integrated from surface to 12cm depth. If no soil moisture value is given, standing water was present at the surface and the soils were saturated.
DOI: 10.1594/pangaea.670249
title: Basic and other measurements of radiation at Neumayer Station (1999-06)
DOI: 10.1594/pangaea.670256
title: Basic and other measurements of radiation at Neumayer Station (2000-02)
DOI: 10.1594/pangaea.763609
title: Light reflectance (RGB) of Hole 325-M0050A
DOI: 10.1594/pangaea.738963
title: Pollen profile AMSOPO1, Amsoldingersee, Switzerland

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.828230
title: Spatially explicit estimates of stock size, structure and biomass of North Atlantic albacore tuna (Thunnus alalunga) in the North Atlantic for the period 1987-2011, compiled from statistics about ICCAT fishery region L6

description: The development of the ecosystem approach and models for the management of ocean marine resources requires easy access to standard validated datasets of historical catch data for the main exploited species. They are used to measure the impact of biomass removal by fisheries and to evaluate the models skills, while the use of standard dataset facilitates models inter-comparison. North Atlantic albacore tuna is exploited all year round by longline and in summer and autumn by surface fisheries and fishery statistics compiled by the International Commission for the Conservation of Atlantic Tunas (ICCAT). Catch and effort with geographical coordinates at monthly spatial resolution of 1° or 5° squares were extracted for this species with a careful definition of fisheries and data screening. In total, thirteen fisheries were defined for the period 1956-2010, with fishing gears longline, troll, mid-water trawl and bait fishing. However, the spatialized catch effort data available in ICCAT database represent a fraction of the entire total catch. Length frequencies of catch were also extracted according to the definition of fisheries above for the period 1956-2010 with a quarterly temporal resolution and spatial resolutions varying from 1°x 1° to 10°x 20°. The resolution used to measure the fish also varies with size-bins of 1, 2 or 5 cm (Fork Length). The screening of data allowed detecting inconsistencies with a relatively large number of samples larger than 150 cm while all studies on the growth of albacore suggest that fish rarely grow up over 130 cm. Therefore, a threshold value of 130 cm has been arbitrarily fixed and all length frequency data above this value removed from the original data set.
description: This work was funded in part by the European project EURO-BASIN, funded by Framework Programme 7 (Contract 264933). Special thanks to ICCAT for the access to its public fishing database and Carlos Palma (ICCAT) and Alain Fonteneau (IRD) for their helpful advice on these data.
DOI: 10.1594/pangaea.495074
title: Water temperature MBT profiles from cruise K74EHM_1953
DOI: 10.1594/pangaea.733349
title: (Fig. 5c) Remanent coercive field Bcr of IODP Hole 308-U1319A
DOI: 10.1594/pangaea.887975
title: Thecamoeba counts from polygon core AWI_12P-2107-2 in the Siberian Arctic
DOI: 10.1594/pangaea.664394
title: Oceanography at CTD/bottle station IFREMER_1235
DOI: 10.1594/pangaea.673455
title: Radiosonde measurements from station Barrow (2004-12)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.730225
title: Documentation of sediment core GIK14183
DOI: 10.1594/pangaea.828834
title: Gas measurements from IODP Hole 339-U1391A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.730241
title: Documentation of sediment core GIK15147-1
DOI: 10.1594/pangaea.734974
title: (Table 5) Middle Eocene to late Cretaceous biostratigraphic datums of ODP Hole 144-699A
DOI: 10.1594/pangaea.730212
title: Documentation of sediment core GIK10092-1
DOI: 10.1594/pangaea.763645
title: Light reflectance (RGB) of Hole 325-M0037A
DOI: 10.1594/pangaea.728412
title: (Appendix A, Table 12) Occurrence of stratigraphically important radiolaria species in ODP Hole 117-731A

description: Species occurrence: P = present, + = rare (one or two specimens), - = searched for and found to be absent
DOI: 10.1594/pangaea.786210
title: Basic measurements of radiation at station Xianghe (2008-12)
DOI: 10.1594/pangaea.728487
title: (Table 8) Occurrence of selected diatom species in ODP Hole 119-744B

description: Species abundance: A = abundant (&gt;2 specimens in one field of view (X1800)), C = common (1 specimen in 2 fields), F = few (1 specimen in each horizontal transect), R = rare (&lt;1 specimen in each horizontal transect), - = absent, lowercase letters indicate reworking
DOI: 10.1594/pangaea.734647
title: (Table 1) Summary statistics of taxa in samples of ODP Hole 181-1123B

description: Planktonic foraminifera are used to identify late Pliocene-Quaternary near surface water masses on the northeastern flank of Chatham Rise by comparison with faunas in core-tops east of New Zealand. In an overview study, distance measures, ordinations, and discriminant analysis are applied to 32 faunas from Site 1123B to identify similar faunas among 35 core-tops between 35 and 61°S east of New Zealand. Many Site 1123B faunas in the 2.72 myr interval sampled compare with those in core-tops on the northern side of Chatham Rise from a similar latitude, and are identified as transitional zone assemblages now associated with the subtropical gyre. This result is consistent with studies of late Quaternary planktonic foraminifera from this region and suggests that, typically, the Subtropical Front was locked to Chatham Rise through glacial and interglacial periods, at least back to the late Pliocene. However, a fauna at ca. 1.17 Ma compares with subpolar assemblages in core-tops between 44 and 48°S and identifies cooler surface water. Expectedly, closer sampling may reveal additional periods when southern water moved over the northeastern flank of Chatham Rise. Although the dominance of Globorotalia inflata, a species typical of the southern margin of subtropical gyres, is a principal feature of Site 1123B faunas, in a minority it is replaced as the most abundant species by dextral populations of Neogloboquadrina pachyderma, particularly about the time of the middle Pleistocene transition. Close analogues of these variant transitional assemblages are not present in core-tops about Chatham Rise but sediment trap and coretop data from other regions suggest that they identify high fertility in the mixed layer associated with upwelling or mixing of water masses. The proportion of sinistrally coiled Neogloboquadrina pachyderma rises to ca. 0.6 between ca. 2.45 and 2.57 Ma, soon after the intensification of Northern Hemisphere glaciation. Although the coiling data indicate subantarctic near surface water, the species remains rare. As the faunas retain their transitional zone character, only minor entrainment of subantarctic water may have occurred.
description: Globorotalia inflata includes 19 specimens of Globorotalia puncticuloides and Globorotalia puncticulata? from 4 samples below 8H-5-100. Globorotalia oceanica (no peripheral keel) from 10H-2-100-10H-7-5 is included in Globorotalia crassaformis. Globigerinita glutinata includes Globigerinita juvenilis. Globigerina falconensis includes tentative identifications. Neogloboquadrina dutertrei s.l. comprises forms intermediate between Neogloboquadrina dutertrei and Neogloboquadrina pachyderma; no typical specimens of the former were found.
description: Supplement to: Scott, George H; Hall, Ian R (2004): Planktonic foraminiferal evidence on late Pliocene-Quaternary near surface water masses at ODP Site 1123B, northern Chatham Rise, east of New Zealand. Marine Geology, 205(1-4), 127-145
DOI: 10.1594/pangaea.740692
title: Age determination of sediment core RL305, Rotsee, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.888099
title: Total water vapor retrieval data in the Arctic in December 2008 using microwave humidity sounders (F-all retrieval)
DOI: 10.1594/pangaea.716613
title: Basic and other measurements of radiation at Neumayer Station (2008-04)
DOI: 10.1594/pangaea.728229
title: (Appendix B) Late Neogene radiolarian events in ODP Hole 115-710A
DOI: 10.1594/pangaea.770120
title: (Appendix 5) Stable isotope ratios of foraminifera of ODP Hole 113-689B and 113-690B
DOI: 10.1594/pangaea.717995
title: Ultra-violet measurements from station Boulder, SURFRAD (2006-05)

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.718205
title: Radiosonde measurements from station Boulder, SURFRAD (2008-06)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.728406
title: (Appendix A, Table 6) Occurrence of stratigraphically important radiolaria species in ODP Hole 117-726A

description: Species occurrence: P = present, + = rare (one or two specimens), - = searched for and found to be absent
DOI: 10.1594/pangaea.909602
title: Cloud Chemistry Monitoring at Mt. Brocken, Germany - 2005

description: The liquid water content of clouds (LWC) has been continuously measured using forward scattering of laser beams by cloud droplets with a Particulate Volume Monitor PVM-100 (Gerber Scientific Inc.). This instrument was also used to control an automated „wet-only” sampling unit that opens up and moves a passive string collector (ASRC type) into sampling position when the LWC level exceeds a 25mg/m**3 threshold. The samples were analysed by ion chromatography (DIONEX suppressor, SYKAM pump and conductivity detector, JASCO sampler) for anions ([Cl]-, [NO3]-, [SO4]2-) and cations ([Na]+, [NH4]+, [K]+, [Ca]2+, [Mg]2+), pH and conductivity. The acceptance criteria for ion balance and for conductivity (measured/calculated), respectively, are defined in the Reports 85 (1992) and 102 (1994) of the WMO for all activities within the GAW program and also we did follow rigorously these standard practices. The whole measurement and analytical procedure was laid down in standard operating procedures. Overall data check: Karin Acker
DOI: 10.1594/pangaea.603898
title: Hydrographic and chemical measurements at anchor station M8_065-6b of the eastern North Atlantic (Table 1)
DOI: 10.1594/pangaea.759059
title: (Table 3) Composition of major oxides of plagioclase crystals in tephra layers at ODP Site 121-758
DOI: 10.1594/pangaea.716614
title: Radiosonde measurements from Neumayer Station (2008-04)
DOI: 10.1594/pangaea.759340
title: Basic and other measurements of radiation at Neumayer Station (2002-03)
DOI: 10.1594/pangaea.717903
title: Ultra-violet measurements from station Sioux Falls (2004-04)

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 2017-02-03.
DOI: 10.1594/pangaea.728952
title: (Table 5) Varimax factor loadings from factor analysis of ODP Site 121-756
DOI: 10.1594/pangaea.830105
title: Basic measurements of radiation at station Palaiseau (2005-11)

description: Version 3, 2014-02-27
DOI: 10.1594/pangaea.718170
title: Radiosonde measurements from station Boulder, SURFRAD (2007-10)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.727710
title: Documentation of ice wedge L7-11
DOI: 10.1594/pangaea.718296
title: Radiosonde measurements from station Boulder, SURFRAD (1996-04)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown; Version 2, 2009-06-12
DOI: 10.1594/pangaea.718150
title: Radiosonde measurements from station Boulder, SURFRAD (2007-05)

description: Start location: Denver, CO; Distance from radiation site: 40 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.728231
title: (Appendix C) Paleogene radiolarian events in ODP Hole 115-709A
DOI: 10.1594/pangaea.807360
title: Basic measurements of radiation at station Nauru Island (2004-06)

description: Version 3, 2013-02-15
DOI: 10.1594/pangaea.718318
title: Basic measurements of radiation at station Boulder, SURFRAD (1996-10)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.787365
title: (Table T1) Isotopic ratios of vein minerals from ODP Hole 176-735B

description: DEPTH, sediment is given in mbsf.
DOI: 10.1594/pangaea.819007
title: (Figure 7B) Biogenic opal of sediment core GeoB13862-1
DOI: 10.1594/pangaea.717927
title: Ultra-violet measurements from station Sioux Falls (2004-12)

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 2017-02-03.
DOI: 10.1594/pangaea.759936
title: Calcareous nannofossil biomagneochronology of ODP Hole 122-762B (Tables 1, 2)

description: Drilling on the Exmouth Plateau during Ocean Drilling Program Leg 122 recovered an almost complete Cenozoic sequence at Site 762. Sediments at this site contain abundant, diverse, and generally well-preserved calcareous nannofossils. The continuity of the stratigraphic sequence, preservation of the taxa, and availability of magnetostratigraphy offered an opportunity to construct a first-order biomagnetochronologic history for late Miocene-Quaternary calcareous nannofossils at Site 762. Magnetochronologically dated FADs/LADs for 23 different nannofossils are given in this study. FADs or LADs for five of these species (Discoaster blackstockae, D. calcaris, Rhabdosphaera claviger, R. longistylis, and R. procera) have never been presented before. In addition, a LAD for Ceratolithus rugosus is new. We believe these new age datums, and the complementary information on previous datums, will add to the growing refinement of Cenozoic biomagnetochronology.
description: Supplement to: Siesser, William G; Bralower, Timothy J; Tang, Cheng; Galbrun, Bruno (1992): Late Miocene-Quaternary calcareous nannofossil biomagnetochronology on the Exmouth Plateau, Northwest Australia. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 677-681
DOI: 10.1594/pangaea.718088
title: Ultra-violet measurements from station Sioux Falls (2005-12)

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 2017-02-03.
DOI: 10.1594/pangaea.496874
title: Physical oceanography from BT during cruise K90OTB_1956
DOI: 10.15468/dl.2xzrjf
title: Occurrence Download

description: A dataset containing 1517 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Egypt",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Culex pipiens Linnaeus, 1758"
 ]
}

 The dataset includes 1517 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031155-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.718474
title: Other measurements at 10 m from station Boulder, SURFRAD (1999-12)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.718519
title: Other measurements at 10 m from station Boulder, SURFRAD (2000-11)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.748036
title: Hydrography on standard level calculated from water bottle samples of RV Akademik Kurchatov in 1982
DOI: 10.1594/pangaea.674384
title: Radiosonde measurements from Neumayer Station (1994-12)
DOI: 10.1594/pangaea.726445
title: (Table 4) Visual kerogen data and vitrinite reflectance measurement of ODP Hole 113-696B
DOI: 10.1594/pangaea.754900
title: (Appendix D) Siliceous microfossil abundance in ODP Hole 114-699A
DOI: 10.1594/pangaea.755335
title: (Table 3) Absolute abundance of silicoflagellates from ODP Hole 114-700B
DOI: 10.1594/pangaea.712029
title: (Table 1) Ostracode assemblage parameters in sediments of ODP Hole 113-689

description: During the late Paleocene thermal maximum (ca. 55.50 Ma) mid-bathyal ostracodes at Maud Rise in the Southern Ocean (Ocean Drilling Program Site 689) underwent a sudden, dramatic turnover synchronous with a global extinction in deep-sea benthic foraminifers and with large-scale, short-lived negative excursions in the stable isotope record of foraminiferal calcite. A previously stable and long-lived ostracode assemblage, dominated by heavily calcified, chiefly epifaunal taxa, was replaced within ~10 k.y. by a taxonomically novel association of small, thin-walled opportunistic and generalist forms that persisted for ~25-40 k.y. Thereafter, ostracode faunas recovered and common bathyal forms returned, although species were smaller and/or less-heavily calcified than before the turnover. The complex fabric of change in ostracode shell morphology and assemblage composition and structure reflects both long-term and sudden perturbations in seawater chemistry at this site. Ostracode data are in agreement with the hypothesis that the latest Paleocene extinctions in the deep sea were caused by a change in the dominant source area of intermediate water mass from high altitudes to the subtropics. These data also suggest that warm saline waters persisted at Maud Rise for the next 100 k.y.
description: Age model after Thomas et al. (1990; http://www-odp.tamu.edu/publications/113_SR/VOLUME/CHAPTERS/sr113_51.pdf), as adapted by Thomas and Shackleton (1996; DOI: 10.1144/GSL.SP.1996.101.01.20) to the stratigraphic interpretation of Aubry et al. (1996; DOI: 10.1144/GSL.SP.1996.101.01.18).
DOI: 10.1594/pangaea.718200
title: Ultra-violet measurements from station Boulder, SURFRAD (2008-05)

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.903901
title: Meteorological synoptical observations from station Tamanrasset (2019-06)
DOI: 10.1594/pangaea.719176
title: Ultra-violet measurements from station Bondville (2009-04)

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.728191
title: (Appendix B1) Radiolaria abundance of ODP Hole 112-682A

description: P = present, - = absent
DOI: 10.1594/pangaea.719113
title: Radiosonde measurements from station Bondville (2007-12)

description: 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.718199
title: Basic measurements of radiation at station Boulder, SURFRAD (2008-05)
DOI: 10.1594/pangaea.718787
title: Other measurements at 10 m from station Sioux Falls (2007-12)
DOI: 10.1594/pangaea.718485
title: Ultra-violet measurements from station Boulder, SURFRAD (2000-03)

description: Version 2, 2009-06-12. 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.696193
title: Total organic carbon in waters of the Arabian Sea in sommer 1995 at Station M32/5_433