cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.772659
title: Distribution of lithologic units from IODP Hole 315-C0002B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.881968
title: Basic and other measurements of radiation at station Barrow (2007-10)

description: Version 2, 2017-10-18 with corrected Short-wave downward (GLOBAL) radiation values. Please note that relative humidity values might be off and are therefore to be handled with caution.
DOI: 10.1594/pangaea.754809
title: Hourly meteorological observations at mooring station FGGE_MET1S
DOI: 10.1594/pangaea.602480
title: Grayscale data of multicorer GeoB7805-1, tube 1

description: Depth sediment 10.87 cm - 18.21 cm: hiatus due to turbidite
DOI: 10.1594/pangaea.775873
title: Radiosonde measurements from station Ishigakijima (2011-11)
DOI: 10.1594/pangaea.750810
title: Meteorological observations during MIÑO cruise from La Habana to Cádiz started at 1794-07-18
DOI: 10.1594/pangaea.772396
title: Hydrochemistry measured on water bottle samples during cruise Lena1956

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.746575
title: Meteorological observations during FAVORITE cruise started at 1769-02-02
DOI: 10.1594/pangaea.824945
title: (Table S1) Geochemistry Cenomanian-Turonian sediments from DSDP Hole 11-105
DOI: 10.1594/pangaea.664964
title: Oceanography at CTD/bottle station IFREMER_1804
DOI: 10.1594/pangaea.772017
title: Shear strength measurements from IODP Hole 315-C0001E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.748925
title: Meteorological observations during El Gallego cruise from La Habana to La Coruña started at 1794-10-03
DOI: 10.1594/pangaea.751616
title: Meteorological observations during PYLADES cruise from New London to Carlisle Bay started at 1815-02-21
DOI: 10.1594/pangaea.727325
title: Planktic foraminifera counts of sediment core RC14-29
DOI: 10.1594/pangaea.873596
title: Ultra-violet measurements from station Toravere (2017-02)
DOI: 10.1594/pangaea.665223
title: Oceanography at CTD/bottle station IFREMER_2063
DOI: 10.1594/pangaea.477276
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/2-1

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.602481
title: Stable oxygen isotope ratios of Globigerinoides ruber (white) from multicorer GeoB7803-2, tube 1
DOI: 10.1594/pangaea.664251
title: Oceanography at CTD/bottle station IFREMER_1092
DOI: 10.1594/pangaea.751240
title: Meteorological observations during PLUTO cruise from Batavia to Samarang started at 1805-11-07
DOI: 10.1594/pangaea.671453
title: Carbonate and diatom contents of sediment core ELT05.024-PC from the West Antarctic continental margin
DOI: 10.1594/pangaea.907218
title: Track of GPS very-near surface drifter ISMER_20141021_spot213
DOI: 10.1594/pangaea.602499
title: X-ray fluorescence data of multicorer GeoB7804-4, tube 1

description: Depth sediment 18.60 cm - 29.20 cm: hiatus due to turbidite
DOI: 10.1594/pangaea.772013
title: (Table S1) Age model of ODP Hole 130-806B

description: Sediment depth is the official ODP depth (mbsf). Coring gaps between 16.17 and 16.02 mbsf, and between 25.72 and 25.52 mbsf. Based on visual alignment to the ODP Hole 677 benthic foraminiferal d18O (Shackleton et al., 1990). Coring gaps refer to losses due to sediment expansion (Berger et al., 1993, doi:10.2973/odp.proc.sr.130.023.1993) and sampling gaps refer to gaps in sections due to sample collection for organic geochemistry, interstitial water or smear slide analyses.
DOI: 10.1594/pangaea.665011
title: Oceanography at CTD/bottle station IFREMER_1851
DOI: 10.1594/pangaea.772124
title: Table 2: Stream flow measurements at the gauge station Vernagtbach

description: From 1974 to 1982 repeated tracer tests using fluorescent dyes were carried out in the highly glaciated drainage basin of Vernagtbach. These tests enabled the quantitative determination of the runoff in the forefield of the Vernagtferner, the calculation of travel times of the stream water and estimations of the relative contributions to the entire runoff originating from individual streams. In addition, tracer tests were carried out in the firn area of the glacier resulting in data concerning the storage and travel time of meltwater inside the glacier.
description: Supplement to: Behrens, Horst; Oerter, Hans; Reinwarth, Oskar (1982): Results of tracer experiments with fluorescent dyes on Vernagtferner (Oetztal Alps, Austria) from 1974 to 1982. Zeitschrift für Gletscherkunde und Glazialgeologie, 18(1), 65-83
DOI: 10.1594/pangaea.831693
title: TABLE 2. - Number of Asellota isopods collected in the Beagle Channel

description: The shallow-water Asellota from the Beagle Channel were investigated, based on material collected at four localities in 2001-2002. A total of 3,124 asellotes were sorted, and three new species and 12 new records of distribution were reported. The Paramunnidae showed the highest species diversity and abundance (11 species and 1,463 specimens). The present research raises the number of species known from the Beagle Channel to 23; of these, 16 were previously reported from the Magellan Straits, representing 69% of similarity. Based on the present results and published data, the faunistic affinities for the shallow-water Asellota was 30% between the Magellan region and the Scotia Arc, and 26% between the Magellan region and the Antarctic Peninsula.
description: Supplement to: Doti, Brenda Lia; Roccatagliata, Daniel; Zelaya, Diego Gabriel (2005): The shallow-water Asellota (Crustacea: Isopoda) from the Beagle Channel: Preliminary taxonomic and zoogeographical results. Arntz, Wolf E, Lovrich, Gustavo A & Thatje, Sven (eds.) The Magellan-Antarctic connection: links and frontiers at southern high latitudes, Scientia Marina, 69 (Suppl. 2), 159-166
DOI: 10.1594/pangaea.750412
title: Meteorological observations during LEOPARD cruise from Mocha to Bombay started at 1801-07-28
DOI: 10.1594/pangaea.771967
title: CNS-analysis from IODP Hole 315-C0001E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.905631
title: Meteorological synoptical observations from station Fukuoka (2019-07)
DOI: 10.1594/pangaea.680517
title: Other measurements at 10 m from station Payerne (2006-10)
DOI: 10.1594/pangaea.873414
title: Ultra-violet measurements from station Fort Peck (2014-08)
DOI: 10.1594/pangaea.752479
title: Meteorological observations during THETIS cruise from St. Helena to Plymouth started at 1777-07-21
DOI: 10.1594/pangaea.771958
title: (Table T8) Calcareous nannofossil events of ODP Site 199-1219

description: Sediment depth is given in rmcd.
DOI: 10.1594/pangaea.775872
title: Meteorological synoptical observations from station Ishigakijima (2011-11)
DOI: 10.1594/pangaea.873420
title: Ultra-violet measurements from station Fort Peck (2014-10)
DOI: 10.1594/pangaea.858810
title: Expanded measurements from Neumayer Station (2015-03)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.870255
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_X_17
DOI: 10.15468/dl.2mpbcj
title: Occurrence Download

description: A dataset listing the 4015634 species recorded in GBIF matching the query:
{ }

 The dataset's 4015634 records were derived from 75100 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031084-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.842823
title: Organic geochemistry of Lake Anterne sediments
DOI: 10.1594/pangaea.907941
title: (Table 2) X-ray micro-CT scanning of planktic foraminiferal from sediment cores
DOI: 10.1594/pangaea.739811
title: Pollen profile SIGVALDE, Sigvalde Trask, Sweden

description: Methodology followed Faegri and Iverson (1964) with the following modifications: samples were left to stand in cold HF for several weeks; after acetolysis, clay rich samples sieved through a 7 micrometre sieve.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.771324
title: (Table 9) Constituents of sand-size fraction of ODP Holes 127-794A and 127-197B
DOI: 10.1594/pangaea.858838
title: Radiosonde measurements from Neumayer Station (2015-09)
DOI: 10.1594/pangaea.747328
title: Meteorological observations during AMAZON cruise from Spithead to Funchal started at 1806-01-29
DOI: 10.1594/pangaea.771964
title: Core summary for IODP Hole 315-C0001E
DOI: 10.1594/pangaea.750903
title: Meteorological observations during NEREIDE cruise from Falmouth to Maldonado started at 1806-11-13
DOI: 10.1594/pangaea.881981
title: Radiosonde measurements from station Barrow (2008-04)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.15468/dl.fy5xyu
title: Occurrence Download

description: A dataset containing 238 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is one of (Myrcia ferruginea G.Don, Marlierea ferruginea (Poir.) McVaugh, Eugeniopsis richardiana O.Berg, Krugia elliptica (Griseb.) Urb., Krugia ferruginea (Poir.) Urb., Marlierea acuminata O.Berg, Marlierea elliptica Griseb., Marlierea guyanensis D.Legrand, Myrtus ferruginea (Poir.) Spreng.)"
 ]
}

 The dataset includes 238 records from 46 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031094-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.771965
title: Core-section summary from IODP Hole 315-C0001E
DOI: 10.1594/pangaea.858753
title: Ultra-violet measurements from station Izaña (2016-02)
DOI: 10.1594/pangaea.858908
title: Continuous meteorological observations at Neumayer station (2015-07)
DOI: 10.1594/pangaea.782782
title: Radiosonde measurements from station Southern Great Plains (2010-08)

description: Launches at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.782896
title: Basic measurements of radiation at station Billings (2010-11)
DOI: 10.1594/pangaea.782901
title: Basic measurements of radiation at station Billings (2011-04)
DOI: 10.1594/pangaea.782907
title: Basic measurements of radiation at station Billings (2011-10)
DOI: 10.1594/pangaea.832097
title: (Table 2) Age determination of sediment core FR01/97-12

description: Measured on Globigerinoides saccullifer &gt;300 µm size fraction. Calibrated ages: Calibration up to 20 kyr BP calculated using Calib 4.3, Marine 98 database (Stuiver et al., 1998). Dates beyond 20 kyr calibrated using the Bard et al. (1998) polynomial.
DOI: 10.1594/pangaea.881983
title: Radiosonde measurements from station Barrow (2008-05)

description: Start location: Barrow, Alaska, USA; Distance from radiation site: 7 km
DOI: 10.1594/pangaea.748675
title: Meteorological observations during DRAKE cruise from Cape Breton to New York started at 1782-12-01
DOI: 10.1594/pangaea.751149
title: Meteorological observations during PENZANCE cruise from Sandy Hook to Barbados started at 1761-11-20
DOI: 10.1594/pangaea.836949
title: The Gepatschferner from 1850 - 2006, with links to digital elevation models and glacier margins

description: This theses investigates changes at Gepatschferner in length, area and volume since the last glacier maximum in 1850. Changes are discussed for the following time periods: 1850-1922, 1922-1971, 1971-1997, 1997-2006. Digital elevation models were created for 1850 from geomorphological data and for 1922 and 1971 from historical maps. Existing DEMs for 1997 and 2006 were further analysed. Since 1850 Gepatschferner has retreated by 2 km in length and has lost 32% of its area and 36% of its volume. The rate of loss of volume is increasing faster than the rate of loss of area and losses in the upper regions of the glacier are becoming increasingly more important to overall losses. The largest losses per 50 m elevation increment occur at the tongue. These losses are greatest in the most recent time step studied, 1997-2006, and exceed previous values by 40% and more. The data base includes the glacier margins, elevations models as they have been compiled within the thesis (DEMs of 1997 and 2006 are part of the glacier inventories, length changes are part of the length change data base of the Austrian Alpine Club).
description: Supplement to: Hartl, Lea (2010): The Gepatschferner from 1850 - 2006 - Changes in length, area and volume in relation to climate. Diploma Thesis, Institute for Meteorology and Geophysics, University of Innsbruck, 79 pp
DOI: 10.1594/pangaea.903384
title: Calcareous nannofossils absolute abundance and accumulation rates from Carajuan, France
DOI: 10.1594/pangaea.908812
title: Meteorological synoptical observations from station Minamitorishima (2019-09)
DOI: 10.1594/pangaea.770790
title: Mineralogy of nonclay components of Hole 325-M0058A
DOI: 10.1594/pangaea.901615
title: Beach profile data for the Elwha River Delta, 2016-10-16

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.832499
title: (Table 1) CaCO3 contents at the core top and at 5 cm depth sediments below 4.0 km in the South Pacific
DOI: 10.1594/pangaea.858859
title: Ozone measurements from Neumayer Station (2016-01)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.810712
title: (Table 1) Iron, cadmium, chromium and lead concentrations in liver of wild sea bird chicks from the Norwegian arctic region

description: Concentrations are given in µg/g (mg/kg) dry weight.
DOI: 10.1594/pangaea.858858
title: Radiosonde measurements from Neumayer Station (2016-01)
DOI: 10.1594/pangaea.752929
title: Meteorological observations during WORCESTER cruise from Downs to Bombay started at 1770-02-24
DOI: 10.1594/pangaea.858860
title: Expanded measurements from Neumayer Station (2016-01)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.873315
title: Varve measurements from Eocene Lake Messel (core Messel 2001, 89.83 - 89.86 m depth)
DOI: 10.1594/pangaea.497405
title: Physical oceanography from BT during cruise U06XX01019B_1938
DOI: 10.1594/pangaea.673916
title: Radiosonde measurements from station Boulder (1992-09)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.674006
title: Radiosonde measurements from station Boulder (2000-03)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.832826
title: Continuous meteorological observations at Redcliff station, Moreton Bay, Australia, in 2011
DOI: 10.1594/pangaea.477452
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_10S/139

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.903382
title: Calcareous nannofossils absolute abundance and accumulation rates from Meussia, France
DOI: 10.1594/pangaea.832424
title: (Table S2) Stratigraphic correlation tie points between IODP Exp302 composite core, PS-2185-6 and 96/1-PC

description: DEPTH, sediment/rock [m] is given in rmcd.
DOI: 10.1594/pangaea.903435
title: Calcareous nannofossils absolute abundance and accumulation rates from ODP Hole 208-1263C and 208-1263D
DOI: 10.1594/pangaea.674012
title: Radiosonde measurements from station Boulder (2000-09)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.739878
title: Pollen profile SZYM_N, Szymbark, Poland

description: Method: 10% KOH, Erdtman acetolysis.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.770802
title: (Table 4) Stratigraphic distribution of calcareous nannofossils at ODP Site 127-796

description: Species abundances: A = Abundant, C = common, M = many, F = few, R = rare
DOI: 10.1594/pangaea.771397
title: (Appendix) Range chart of calcareous nannofossils in ODP Hole 129-802A

description: Only Site 802 has recorded appreciable Cenozoic carbonate sediments during Ocean Drilling Program Leg 129 in the central Mariana Basin of the western Pacific Ocean. Calcareous nannofossils provide the best biostratigraphic information for the 360-m Tertiary section, which consists primarily of volcaniclastic turbidites interbedded with calcareous claystone and chalk. Many samples contain significant amounts of nannofossils reworked from older sediments. An unconformity appears to be present between Cores 129-802A-32R and -33R, with upper Oligocene-lower Miocene sediments above and lower Eocene-upper Paleocene sediments below the unconformity. The sediments below the unconformity contain abundant reworked Cretaceous nannofossils. Only one sample from Site 801 yielded nannofossils, and those consist of a mixture of Campanian-Maastrichtian and Paleogene forms.
description: Species abundance: A = abundant, C = common, F = few, R = rare, - = absent
description: Supplement to: Mao, Shaozhi; Covington, James M (1992): Data Report: Cenozoic nannofossils from Leg 129. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 801-809
DOI: 10.1594/pangaea.770502
title: Visual core description (VCD) from IODP Hole 315-C0001E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.817270
title: Hydochemistry measured on water bottle samples during TYRO cruise NIOP-C2
DOI: 10.1594/pangaea.673917
title: Radiosonde measurements from station Boulder (1992-10)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.832848
title: (Table S2) Mapping meters below seafloor to corrected composite depth for ODP Site 138-851

description: DEPTH, sediment/rock [m] gives mbsf.
DOI: 10.1594/pangaea.749410
title: Meteorological observations during GIBRALTAR cruise from Cruising started at 1756-03-01
DOI: 10.1594/pangaea.771429
title: (Table 5) Chemical composition of Cretaceous volcaniclastites from Units VIII to IX of ODP Holes 129-801A and 129-802A
DOI: 10.1594/pangaea.839147
title: Pollen profile DESVERNE

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.771434
title: (Appendix B) Recalculated chemical composition of Cretaceous volcaniclastites from Unit III of ODP Site 129-801 and Units VIII to IX of ODP Hole 129-802A

description: Sediment depth is given in mbsf. Recalculated on a volatile-free basis.
DOI: 10.1594/pangaea.857822
title: Basic measurements of radiation at station Cener (2015-10)
DOI: 10.1594/pangaea.858056
title: Pollen and non-pollen palynomorph data from Lake Iznik, NW Turkey (last 31 ka cal BP)

description: The Marmara region in northwestern Turkey provides a unique opportunity for studying the vegetation history in response to climate changes and anthropogenic impacts because of its location between different climate and vegetation zones and its long settlement history. Geochemical and mineralogical investigations of the largest lake in the region, Lake Iznik, already registered climate-related changes of the lake level and the lake mixing. However, a palynological investigation encompassing the Late Pleistocene to Middle Holocene was still missing. Here, we present the first pollen record of the last ca. 31 ka cal BP (calibrated kilo years before 1950) inferred from Lake Iznik sediments as an independent proxy for paleoecological reconstructions. Our study reveals that the vegetation in the Iznik area changed generally between (a) steppe during glacials and stadials indicating dry and cold climatic conditions, (b) forest-steppe during interstadials indicating milder and moister climatic conditions, and (c) oak-dominated mesic forest during interglacials indicating warm and moist climatic conditions. Moreover, a pronounced succession of pioneer trees, cold temperate, warm temperate, and Mediterranean trees appeared since the Lateglacial. Rapid climate changes, which are reflected by vegetation changes, can be correlated with Dansgaard-Oeschger (DO) events such as DO-4, DO-3, and DO-1, the Younger Dryas, and probably also the 8.2 event. Since the mid-Holocene, the vegetation was influenced by anthropogenic activities. During early settlement phases, the distinction between climate-induced and human-induced changes of the vegetation is challenging. Still, evidence for human activities consolidates since the Early Bronze Age (ca. 4.8 ka cal BP): cultivated trees, crops, and secondary human indicator taxa appeared, and forests were cleared. Subsequent fluctuations between extensive agricultural uses and regenerations of the natural vegetation become apparent.
description: The dataset includes counts of pollen and other palynomorphs from sediment cores of Lake Iznik, NW Turkey. The investigated time period encompasses the last 31,000 years BP. Further details are described in the corresponding publication.This dataset is also part of the EPD data base (http://www.europeanpollendatabase.net).
description: Supplement to: Miebach, Andrea; Niestrath, Phoebe; Roeser, Patricia A; Litt, Thomas (2016): Impacts of climate and humans on the vegetation in northwestern Turkey: palynological insights from Lake Iznik since the Last Glacial. Climate of the Past, 12(2), 575-593
DOI: 10.1594/pangaea.739989
title: Pollen profile ZIRBEN1, Zirbenwaldmoor, Austria

description: Method: KOH, acetolysis.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.665276
title: Oceanography at CTD/bottle station IFREMER_2116
DOI: 10.1594/pangaea.840712
title: (ES-4) Principal component analysis of surface sediments from the Trondheimsfjord, central Norway

description: Results of the PCA used to calculate the TM index. Variables are d13Corg and the fraction of terrestrial organic carbon (Fterr).