cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.917363
title: 1-Hz PPP displacements at GEONET station 3016 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.747353
title: Meteorological observations during AMPHION cruise from Spithead to Martinico started at 1798-12-24
DOI: 10.1594/pangaea.677335
title: Ozone measurements from Neumayer Station (2004-06)

description: Ozone values are integrated from measured ozone profiles
DOI: 10.1594/pangaea.804514
title: Table 1: Abundance of meroplankton in the Kara Sea
DOI: 10.1594/pangaea.869987
title: Links to master tracks in different resolutions from POLAR 5 flight ANT_2008/09_15
DOI: 10.1594/pangaea.917446
title: 1-Hz PPP displacements at GEONET station 3102 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.752012
title: Meteorological observations during SCHIEDAM cruise from Spitsbergen to Schiedam started at 1778-07-14
DOI: 10.1594/pangaea.752514
title: Meteorological observations during TREMENDOUS cruise from Flat Island, Mauritius to St. Marys started at 1804-11-01
DOI: 10.1594/pangaea.749552
title: Meteorological observations during HECTOR cruise from St. Helena to Blackwall started at 1754-01-16
DOI: 10.1594/pangaea.757712
title: Velocity, attenuation, confidence interval and Seki parameter of ODP Hole 118-735B gabbros (Appendix)

description: Compressional velocity and attenuation were measured as a function of depth in layer 3 gabbros from the recovered core at Ocean Drilling Program Site 735. High-frequency (400 kHz) acoustic transmission experiments were conducted on 117 minicore samples under room conditions of temperature and pressure on board the JOIDES Resolution. Although experimental errors were large in some deformed samples, the average of our measurements of 1000/Qp on these samples is 49 ± 32. Ultrasonic tests on a 1% porosity sample at elevated effective pressures from 10 up to 500 MPa showed an increase in Vp from 6.8 to 7.0 km/s and a decrease in 1000/Qp from 26 to 23. The small pressure dependence of attenuation in these low-porosity gabbros enables one to use measurements at room conditions for relative interpretation as a function of depth.These measurements of 1000/Qp vs. depth show (1) an overall decrease in attenuation from lithologic Units II through V as a function of depth, (2) a 10-fold decrease in the average variance in the measurement in lithologic Unit II, and (3) an inverse relationship between average velocity and average attenuation. An explanation for these results is that tectonized rock fabrics have a significant effect on the measurement of attenuation and velocity. The future use of this simple shipboard operation to measure trends in attenuation as a function of depth may be effective to determine the degree of alteration and tectonism in similar, nonpressure-sensitive rocks.
description: Supplement to: Goldberg, David; Badri, Mohammed; Wepfer, William W (1991): Ultrasonic attenuation measurements in gabbros from Hole 735B. In: Von Herzen, RP; Robinson, PT; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 118, 253-259
DOI: 10.1594/pangaea.917364
title: 1-Hz PPP displacements at GEONET station 3018 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.693913
title: Sedimentology and geochemical analyses of Pliocene to Holocene sediments of ODP Hole 160-964A in the eastern Mediterranean Sea (Appendix)

description: A multiproxy geochemical study of nine sapropel layers from ODP Hole 964A, ODP Leg 160 in the eastern Mediterranean spanning the Pliocene-Holocene time interval provides new insights into the evolution of sapropel deposition. Paleoenvironmental proxies were used for reconstruction of productivity (Ba derived from marine barite), oxygen conditions (trace metal ratios) and sedimentary regime (clay minerals, detrital elements). These proxies reveal a significant increase in river runoff relative to decreasing aeolian input during sapropel deposition over the whole time interval. Ba excess supports the argument that a significant increase in export productivity is the main triggering mechanism for sapropel deposition, although preservation also played an important role. Furthermore, major differences exist in depositional conditions, including both oxygenation and productivity since the Pliocene. Productivity fluctuated substantially and was higher during the Pliocene and Pleistocene than during the Holocene; at the same time decreasing oxygen availability parallels the enhanced productivity. Dysoxic to anoxic conditions appear to coincide with marine productivity maxima, thus suggesting that oxygen depletion may be linked to greater consumption rather than restricted circulation. This correspondence supports the hypothesis that productivity fluctuations resulting from climate oscillations were the main cause of enhanced organic matter contents and also a main controlling factor for reduced oxygen availability.
description: Supplement to: Gallego-Torres, David; Martinez-Ruiz, Francisca C; Paytan, Adina; Jiménez-Espejo, Francisco Jose; Ortega-Huertas, M (2007): Pliocene-Holocene evolution of depositional conditions in the eastern Mediterranean: Role of anoxia vs. productivity at time of sapropel deposition. Palaeogeography, Palaeoclimatology, Palaeoecology, 246(2-4), 424-439
DOI: 10.1594/pangaea.917381
title: 1-Hz PPP displacements at GEONET station 3035 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.695371
title: Strontium isotope ratios of planktonic foraminifera from ODP Site 119-744 on the Kerguelen Plateau, Indian Ocean (Table 1)

description: 87Sr/86Sr ratios of well-preserved early Miocene-Oligocene planktonic foraminifers from Site 744 in the southern Indian Ocean provide the highest southern latitude Sr isotope record of this age. The isotopic data have been calibrated with the site magnetostratigraphy. 87Sr/86Sr ages were also determined using the Sr isotope-age equations of Miller et al. (1988, doi:10.1029/PA003i002p00223) and Hess et al. (1989, doi:10.1029/PA004i006p00655). There is good agreement between the calculated ages from 87Sr/86Sr measurements using these equations and those derived from magnetobiostratigraphy. In addition, these equations were useful for inference of sediment ages in intervals where the paleomagnetic record is not well resolved and the biostratigraphy is inconclusive. The Site 744 87Sr/86Sr record can be used for correlation of Antarctic and low-latitude sequences and biostratigraphical zonation of foraminifers, radiolarians, diatoms, and calcareous nannofossils. This record will assist in the development of the high southern latitude biochronology.
description: Supplement to: Barrera, Enriqueta C; Barron, John A; Halliday, Alex N (1991): Strontium isotope stratigraphy of the Oligocene - lower Miocene section at Site 744, Southern Indian Ocean. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 731-738
DOI: 10.1594/pangaea.845254
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE401, Bremerhaven - Helgoland, 2013-05-27 - 2013-06-09
DOI: 10.1594/pangaea.917422
title: 1-Hz PPP displacements at GEONET station 3072 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.772408
title: Hydrochemistry measured on water bottle samples during cruise Lomonosov1959

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.790403
title: (Table 2) Sapropel and age model of ODP Site 160-967

description: DEPTH, sediment [m] is given in mcd. The table shows age tie-lines by astronomical calibration of the color reflectance record (and thus the sapropels). The mid-depths of the sapropels were taken for the age tie-lines. A 3-k.y. precession lag was assumed based on the age difference between the youngest, Holocene sapropel S1 and the correlative precession minimum. The user is referred to Lourens et al. (1996, doi:10.1029/96PA01125) for details of the tuning method. A correlation is made with the assigned ages of sapropels observed in the southern Italian land section. + = the Pacific Site 849 d18O record (Mix et al., 1984, doi:10.2973/odp.proc.sr.138.120.1995) was used to produce additional age tie-lines for the last 1 m.y. ++ = The Italian sections are Punta Piccola, Sicily (Italy), Vrica, and Singa, Calabria (Italy) (see Lourens et al., 1996, doi:10.1029/96PA01125; 1996, doi:10.1029/96PA02691).
DOI: 10.1594/pangaea.477272
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/16-1

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.718941
title: (Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP Hole 2-10 sediments
DOI: 10.1594/pangaea.772155
title: Structure description (VCD) from IODP Hole 315-C0001F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.494840
title: Physical oceanography during cruise U67X001026C
DOI: 10.1594/pangaea.825564
title: Natural gamma radiation from IODP Hole 329-U1371D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.746942
title: Meteorological observations during HOUND cruise from Cape Sambrough to Woolwich started at 1752-10-22
DOI: 10.1594/pangaea.840886
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE316
DOI: 10.1594/pangaea.750481
title: Meteorological observations during LIVERPOOL cruise from St. Jago to Madagascar started at 1763-03-18
DOI: 10.1594/pangaea.822848
title: Meteorological measurements in the upper air at station Poznan, 1920-01-14 to 1920-07-21, ERA-CLIM ID 5726

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.860004
title: Bulk mineralogy of Heihai lake sediment core PG2060-1
DOI: 10.1594/pangaea.771006
title: Turbidity (MAPR) YoYos and Tow-yo from L Atalante cruise MARSUED lV
DOI: 10.1594/pangaea.894101
title: Pollen profile of sediment core OTTMAS, Måsåtjørnet, Norway

description: This dataset was archived on 2018-09-14 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 2000
DOI: 10.1594/pangaea.835828
title: Pollen profile KLICAVA, Klícava, Czech Republic

description: This dataset was archived on 2014-09-12 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.499492
title: Physical oceanography from BT during cruise U90XX08260B_1978
DOI: 10.1594/pangaea.747132
title: Meteorological observations during Vrouwe Johanna Cores cruise from Middelburg to Gulf of Guinea started at 1751-04-17
DOI: 10.1594/pangaea.747107
title: Meteorological observations during TARTAR cruise from Bombay to Carnar started at 1751-01-18
DOI: 10.1594/pangaea.917555
title: Course of ice phenomena on the rivers of Poland 1981-2010

description: This dataset contains information on the course of ice phenomena on rivers in Poland (137 stations) during 1981-2010: station, river, latitude, longitude, season, date start (ice on), date (freeze up), date (break up), date end (ice off), days of ice phenomena, days of ice cover. These are processed raw data from the Institute of Meteorology and Water Management National Research Institute (Poland).
DOI: 10.1594/pangaea.744509
title: (Table 1) Chemical composition of Fe-Mn nodules, crusts and host sediments at the section from the Wake Atoll to the Hawaiian Islands
DOI: 10.1594/pangaea.811734
title: (Table 1) Isotopic composition of organic compinents of DSDP Hole 24-231

description: Plant leaf wax hydrogen isotope (dDwax) reconstructions are increasingly being used to reconstruct hydrological change. This approach is based upon the assumption that variations in hydroclimatic variables, and in particular, the isotopic composition of precipitation (dDP), dominate dDwax. However modern calibration studies suggest that offsets between plant types may bias the dDwax hydrological proxy at times of vegetation change. In this study, I pair leaf wax analyses with published pollen data to quantify this effect and construct the first vegetation-corrected hydrogen isotopic evidence for precipitation (dDcorrP). In marine sediments from Deep Sea Drilling Program Site 231 in the Gulf of Aden spanning 11.4-3.8 Ma (late Miocene and earliest Pliocene), I find 77 per mil swings in dDwax that correspond to pollen evidence for substantial vegetation change. Similarities between dDP and dDcorrP imply that the hydrological tracer is qualitatively robust to vegetation change. However, computed vegetation corrections can be as large as 31 per mil indicating substantial quantitative uncertainty in the raw hydrological proxy. The resulting dDcorrP values quantify hydrological change and allow us to identify times considerably wetter than modern at 11.09, 7.26, 5.71 and 3.89 Ma. More generally, this novel interpretative framework builds the foundations of improved quantitative paleohydrological reconstructions with the dDwax proxy, in contexts where vegetation change may bias the plant-based proxy. The vegetation corrected paleoprecipitation reconstruction dDcorrP, represents the best available estimate as proof-of-concept, for an approach that I hope will be refined and more broadly applied.
description: Supplement to: Feakins, Sarah J (2013): Pollen-corrected leaf wax D/H reconstructions of northeast African hydrological changes during the late Miocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 374, 62-71
DOI: 10.1594/pangaea.498433
title: Physical oceanography from BT during cruise U90BY08522B_1985
DOI: 10.1594/pangaea.837322
title: (Table 1) Age determination and calendar agesf ODP Hole 117-723A

description: Annual, summer, and winter sea surface temperatures (SSTs) in the western Arabian Sea were reconstructed through the last 22 kyr using artificial neural networks (ANNs) based on quantitative analyses of planktic foraminifera. Down-core SST estimates reveal that annual, summer, and winter SSTs were 2, 1.2, and 2.6°C cooler, respectively, during the last glacial period than in the Holocene. A 2.5°C SST increase during Termination 1A (hereinafter referred as glacial to Holocene transition) in the western Arabian Sea. The study reveals a strong seasonal SST contrast between winter and summer from 18 to 14 calendar kyr owing to the combined effect of weak upwelling and strong cold northeasterly winds. Minor or no seasonal SST changes were noticed within the Holocene period, which is attributed to the intense upwelling during the summer monsoon. This causes a lowering of SST to values similar to those of the winter season in analogy with the present day. A 3°C rise in winter SSTs during the glacial to Holocene transition coincides with a strengthening of the monsoon, suggesting a link between winter SST and monsoon initiation from the beginning of the Holocene. Strikingly, annual, summer, and winter SSTs show a cooling trend from ~8 ka to the present day, implying tropical cooling in the late Holocene.
description: Supplement to: Naidu, Pothuri Divakar; Malmgren, Bjorn (2005): Seasonal sea surface temperature contrast between the Holocene and last glacial period in the western Arabian Sea (Ocean Drilling Project Site 723A): Modulated by monsoon upwelling. Paleoceanography, 20(1), PA1004
DOI: 10.1594/pangaea.465029
title: (Fig. 2) Stable oxygen and carbon isotopes of Cibicidoides robertsonianus from sediment core MD99-2339
DOI: 10.1594/pangaea.498927
title: Physical oceanography from BT during cruise U90X008069B_1984
DOI: 10.1594/pangaea.705285
title: (Table 3) Sr, Nd and Pb isotopic composition of whole rock samples from ODP Hole 176-735B

description: Pb isotope analyses were corrected for mass fractionation using measured values of NBS981 and amounted to 0.12+/-0.02 (1 S.D.) %/AMU. The strontium isotope analyses were corrected for Rb interference, the ratios normalised to 86Sr/88Sr=0.1194 and corrected for fractionation by the exponential law and the results monitored by the international standard NBS987: 87Sr/86Sr=0.710257+/-0.000008 (1 S.D.), N=16. Neodymium was corrected for interference of Sm and fractionation by normalizing to 146Nd/144Nd=0.7219. Laboratory standard JM Nd yielded: 143Nd/144Nd=0.511123+/-0.000016 (1 S.D.), N=10, in the period of measurement. Within run precision was always insignificant compared to reproducibility of the reference materials.
DOI: 10.1594/pangaea.711907
title: Pollen profile KOILADHA, Koiladha, Greece

description: Method: Heavy-liquid separation (Bromoform-Alcohol mixture s.g. 2.0) followed by standard procedure as described by Faegri and Iversen (1973).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.494927
title: Physical oceanography during cruise U90XX00137C
DOI: 10.1594/pangaea.746043
title: Pleistocene-Pliocene strontium-isotope ratios of ODP Site 107-653 (Table 1)

description: Strontium isotopic determinations were made on samples from the Pliocene-Pleistocene sequence recovered at ODP Hole 653A, the proposed "deep-sea type section" for the Mediterranean region. Biostratigraphic correlations can be combined with the patterns of variations in the 87Sr/86Sr values to delineate the following: (1) the earliest Pliocene (MP11 to basal MP12 zones) is distinguished by fluctuations in the ratio, probably related to the unstable paleoceanographic conditions following the Zanclean flooding and initial in-filling of the Mediterranean after the Messinian desiccation, (2) during most of the Pliocene between approximately 4.5 and 2.4 Ma (MP12 to MP15 zones) the 87Sr/86Sr values remain relatively constant, producing a plateau in the strontium isotope-depth curve for this period, and (3) beginning at approximately 2.4 Ma (across the MP15/MP16 boundary) and continuing into the latest Pleistocene, the 7Sr/86Sr values increase significantly but show fluctuations that have both positive and negative slopes.The presence of a plateau in the curve generated for the Mediterranean type section duplicates in greater detail the late Neogene results reported by DePaolo (1986, doi:10.1130/0091-7613(1986)14&lt;103:DROTNS&gt;2.0.CO;2). The virtual lack of change in the ratio between 4.5 and 2.4 Ma essentially eliminates strontium isotopes as a high-resolution correlation method for this period. The fluctuations in the ratio beginning at 2.4 Ma may be a reflection of major climatic changes occurring in the latest Pliocene-Pleistocene. The relationship between glacial-interglacial cycles and seawater 87Sr/86Sr values suggested by DePaolo (1986) and Capo and DePaolo (1987) is uncertain but should be tested as significant increases and decreases in 87Sr/86Sr of seawater have apparently occurred since 2.4 Ma.
description: Supplement to: McKenzie, Judith A; Palmer, Sarah C; Mueller, Paul A (1990): Strontium isotope stratigraphy of the Pliocene-Pleistocene ''Deep-Sea Type Section'' at ODP Hole 653A. In: Kastens, KA; Mascle, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 107, 401-404
DOI: 10.1594/pangaea.750367
title: Meteorological observations during Le Etoile cruise from Saint Pierre to Brest started at 1786-07-30
DOI: 10.1594/pangaea.753020
title: Meteorological observations during DESCONOCIDO-21 cruise from Cádiz started at 1789-09-12
DOI: 10.15468/dl.wncndd
title: Occurrence Download

description: A dataset containing 1449 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is South America",
 "TaxonKey is Leucobryum crispum Müll.Hal."
 ]
}

 The dataset includes 1449 records from 88 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031262-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.499079
title: Physical oceanography from BT during cruise U90X008270B_1979
DOI: 10.1594/pangaea.822729
title: Meteorological measurements in the upper air at station Kolkata, 1938-12-31 to 1942-03-30, ERA-CLIM ID 5452

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.831654
title: Survey on economic assessment of the improvement of the quality of environment: the case of the fight against floods in Cotonou (Benin Living Standard Survey)

description: This study aims to analyze households' attitude toward flood risk in Cotonou in the sense to identify whether they are willing or not to leave the flood-prone zones. Moreover, the attitudes toward the management of wastes and dirty water are analyzed. The data used in this study were obtained from two sources: the survey implemented during March 2011 on one hundred and fifty randomly selected households living in flood-prone areas of Cotonou, and Benin Living Standard Survey of 2006 (Part relative to Cotonou on 1,586 households). Moreover, climate data were used in this study. Multinomial probability model is used for the econometric analysis of the attitude toward flood risk. While the attitudes toward the management of wastes and dirty water are analyzed through a simple logit. The results show that 55.3% of households agreed to go elsewhere while 44.7% refused [we are better-off here (10.67%), due to the proximity of the activities (19.33), the best way is to build infrastructures that will protect against flood and family house (14.67%)]. The authorities have to rethink an alternative policy to what they have been doing such as building socio-economic houses outside Cotonou and propose to the households that are living the areas prone to inundation. Moreover, access to formal education has to be reinforced.
description: The institution that carried out the survey relative to the first data set was INSAE (Institut National de la Statistique et de l'Analyse Economique) and the second survey was carried out by the author.
DOI: 10.1594/pangaea.711958
title: Pollen profile SERRENT2, Serrent, France

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.694681
title: Temperature, salinity, and concentration of dissolved oxygen in the water column of the Cretan Sea at Station SEPTEMBER-1995-D4
DOI: 10.1594/pangaea.762874
title: (Table 7) Chemical classification of brown claystones and associated sediments from ODP Leg 124 samples