cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.737938
title: Physical oceanography during DISCOVERY cruise 74DI102 on section ISS02

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.664269
title: Oceanography at CTD/bottle station IFREMER_1110
DOI: 10.1594/pangaea.722321
title: Other measurements at 10 m from station Goodwin Creek (2000-06)

description: Version 2, 2009-06-24
DOI: 10.1594/pangaea.830966
title: Satellite-based daily mean lake surface water temperatures from Lake_Mond, 1989-2013

description: The daily mean Lake Surface Water Temperature (LSWT) has been extracted from all available satellite observations of a particular day by using the data from a 3x3 pixel array at the center of the lake. See "Events(s)" for Lake/pixel co-ordinates.
DOI: 10.1594/pangaea.836116
title: Alkenone stable carbon isotopes, planktic foraminfera stable carbon isotopes, alkenone unsaturation indices and calculated sea surface temperatures and atmospheric pCO2 for ODP Site 165-999

description: Temperature reconstructions indicate that the Pliocene was ~3 °C warmer globally than today, and several recent reconstructions of Pliocene atmospheric CO2 indicate that it was above pre-industrial levels and similar to those likely to be seen this century. However, many of these reconstructions have been of relatively low temporal resolution, meaning that these records may have failed to capture variations associated with the 41 Kyr glacial-interglacial cycles thought to operate in the Pliocene. Here we present a new, high temporal resolution alkenone carbon isotope based record of pCO2 spanning 2.8 to 3.3 million years ago from ODP Site 999. Our record is of high enough resolution (~19 Kyrs) to resolve glacial-interglacial changes beyond the intrinsic uncertainty of the proxy method. The record suggests that Pliocene CO2 levels were relatively stable, exhibiting variation less than 55 ppm. We perform sensitivity studies to investigate the possible effect of changing sea surface temperature, which highlights the importance of accurate and precise SST reconstructions for alkenone palaeobarometry, but demonstrate that these uncertainties do not affect our conclusions of relatively stable pCO2 levels during this interval.
description: Supplement to: Badger, Marcus P S; Schmidt, Daniela N; Mackensen, Andreas; Pancost, Richard D (2013): High-resolution alkenone palaeobarometry indicates relatively stable pCO2 during the Pliocene (3.3-2.8 Ma). Philosophical Transactions of the Royal Society A-Mathematical Physical and Engineering Sciences, 371(2001), 20130094
DOI: 10.1594/pangaea.722275
title: Ultra-violet measurements from station Goodwin Creek (1999-03)

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.916727
title: 1-Hz PPP displacements at GEONET station 0532 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.749074
title: Meteorological observations during El Pizarro cruise from La Coruña to La Habana started at 1767-01-06
DOI: 10.1594/pangaea.752555
title: Meteorological observations during TWEED cruise from Madeira to New York started at 1770-09-10
DOI: 10.1594/pangaea.770125
title: (Table 1) Stable carbon and oxygen isotope composition of foraminifera of DSDP Hole 13-132

description: The pelagic sedimentary sequences recovered by the Deep Sea Drilling Project (DSDP) from the Mediterranean are important because of their proximity to the classical shallow-water Neogene marine-type sections in Europe and because they may help correlations between the type sections and marine sequences outside the Mediterranean basin. We have studied the middle Pliocene (2.7–3.6 Myr ago) histories of surface-water temperature and oxygen isotopic composition at DSDP Site 132 in the Tyrrhenian Sea and here we compare these with another approach to estimating palaeotemperatures (Thunell, 1979, doi:10.1016/0377-8398(79)90013-6) based on the transfer function technique (Imbrie and Kipp, 1971). The record clearly shows a climatic cooling commencing between 3.2 and 3.0 Myr ago. An oxygen isotopic curve derived from the planktonic foraminiferan Globigerinoides ruber significantly correlates with a palaeotemperature record estimated from a transfer function palaeotemperature equation on planktonic foraminiferal data. Transfer functions may therefore be of value in interpreting palaeoclimatic history in sequences at least as old as the middle Pliocene.
description: Supplement to: Keigwin, Lloyd D; Thunell, Robert C (1979): Middle Pliocene climatic change in the western Mediterranean from faunal and oxygen isotopic trends. Nature, 282(5736), 294-296
DOI: 10.1594/pangaea.822613
title: Meteorological measurements in the upper air at station Helwan, 1920-01-01 to 1956-10-29, ERA-CLIM ID 4935

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.722296
title: Ultra-violet measurements from station Goodwin Creek (1999-10)

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.885983
title: Basic measurements of radiation at station Billings (2012-01)

description: Version 2, 2018-02-06, including temperature, humidity and pressure data.
DOI: 10.6084/m9.figshare.25787580
title: <b> </b><b>Experimental data of Hypotrachyna cirrhata (Fr.) Hale ex Sipman</b>

description: In general, the methanolic extract obtained from <i>H. cirrhata</i> contains diverse phytochemical compounds that contribute to treating various diseases. This study revealed notable antioxidant, anti-diabetic, and anti-bacterial attributes, displaying impressive IC<sub>50</sub> values and zones of inhibition in comparison to prior research. The anti-oxidant and alpha-glucosidase inhibition activities of the ethyl acetate extract of <i>H. cirrhata </i>were noteworthy, demonstrating an IC<sub>50</sub> value of 10.37 ± 0.62 for anti-oxidant activity and 1.17 ± 0.50 for alpha-glucosidase inhibition. The current investigation consolidates information on the bioactive elements in <i>H. cirrhata</i>, identified through LC-MS, facilitating the identification of eight lichen substances. A comprehensive molecular modeling analysis of the primary components, involving five compounds functioning as α-glucosidase binders, was conducted by considering both active and allosteric pockets as a result high binding energy was showed by salazinic acid with -9.9 kcal/mole. Computational analysis reveals the potent anti-diabetic properties of salazinic acid, as demonstrated through molecular docking, molecular dynamics simulations, ADMET analysis, and free energy calculations.
DOI: 10.1594/pangaea.748781
title: Meteorological observations during EENDRACHT cruise from Curacao to Porto Rico started at 1823-11-11
DOI: 10.6084/m9.figshare.25787580.v3
title: <b> </b><b>Experimental data of Hypotrachyna cirrhata (Fr.) Hale ex Sipman</b>

description: In general, the methanolic extract obtained from <i>H. cirrhata</i> contains diverse phytochemical compounds that contribute to treating various diseases. This study revealed notable antioxidant, anti-diabetic, and anti-bacterial attributes, displaying impressive IC<sub>50</sub> values and zones of inhibition in comparison to prior research. The anti-oxidant and alpha-glucosidase inhibition activities of the ethyl acetate extract of <i>H. cirrhata </i>were noteworthy, demonstrating an IC<sub>50</sub> value of 10.37 ± 0.62 for anti-oxidant activity and 1.17 ± 0.50 for alpha-glucosidase inhibition. The current investigation consolidates information on the bioactive elements in <i>H. cirrhata</i>, identified through LC-MS, facilitating the identification of eight lichen substances. A comprehensive molecular modeling analysis of the primary components, involving five compounds functioning as α-glucosidase binders, was conducted by considering both active and allosteric pockets as a result high binding energy was showed by salazinic acid with -9.9 kcal/mole. Computational analysis reveals the potent anti-diabetic properties of salazinic acid, as demonstrated through molecular docking, molecular dynamics simulations, ADMET analysis, and free energy calculations.
DOI: 10.1594/pangaea.750692
title: Meteorological observations during MEERMIN cruise from Suriname to St. Maarten started at 1848-03-15
DOI: 10.1594/pangaea.824541
title: (Table 1) Main constituents of coccolith size fractions expressed as carbonate contribution at Bass River during the PETM

description: Coccoliths, calcite plates produced by the marine phytoplankton coccolithophores, have previously shown a large array of carbon and oxygen stable isotope fractionations (termed “vital effects”), correlated to cell size and hypothesized to reflect the varying importance of active carbon acquisition strategies. Culture studies show a reduced range of vital effects between large and small coccolithophores under high CO2, consistent with previous observations of a smaller range of interspecific vital effects in Paleocene coccoliths. We present new fossil data examining coccolithophore vital effects over three key Cenozoic intervals reflecting changing climate and atmospheric partial pressure of CO2 (pCO2). Oxygen and carbon stable isotopes of size-separated coccolith fractions dominated by different species from well preserved Paleocene-Eocene thermal maximum (PETM, ~56 Ma) samples show reduced interspecific differences within the greenhouse boundary conditions of the PETM. Conversely, isotope data from the Plio-Pleistocene transition (PPT; 3.5-2 Ma) and the last glacial maximum (LGM; ~22 ka) show persistent vital effects of ~2 per mil. PPT and LGM data show a clear positive trend between coccolith (cell) size and isotopic enrichment in coccolith carbonate, as seen in laboratory cultures. On geological timescales, the degree of expression of vital effects in coccoliths appears to be insensitive topCO2 changes over the range ~350 ppm (Pliocene) to ~180 ppm (LGM). The modern array of coccolith vital effects arose after the PETM but before the late Pliocene and may reflect the operation of more diverse carbon acquisition strategies in coccolithophores in response to decreasing Cenozoic pCO2.
description: Supplement to: Bolton, Clara T; Stoll, Heather M; Mendez-Vicente, Ana (2012): Vital effects in coccolith calcite: Cenozoic climate-pCO2 drove the diversity of carbon acquisition strategies in coccolithophores? Paleoceanography, 27(4), PA4204
DOI: 10.1594/pangaea.803148
title: (Table 1) Organic acid analyses from Leg 135 interstitial waters

description: For the first time, short-chain organic acids are described in interstitial waters from sediments and lithified materials in a backarc setting. Organic acids in interstitial waters from the Tonga forearc region were also analyzed and compared with previous organic acid analyses from the Mariana and Bonin forearc interstitial waters.In the Tonga backarc setting, propionate typically dominates the organic acid assemblage, and organic acids are a consistent feature of these interstitial waters. The persistent presence of ammonia and the dominance of propionate over formate in the backarc interstitial waters suggest that the organic acids in this setting have their origin in reductive deamination of amino acids derived from sedimentary proteinaceous material.The organic acid assemblage revealed in the samples from Hole 841B in the Tonga forearc are similar to the organic acid assemblage detected in the Mariana forearc, that is, formate dominates the assemblage over acetate or propionate. These forearc organic acid assemblages may both have formed by a similar mechanism.
description: Supplement to: Haggerty, Janet A; Fisher, J Berton (1994): Short-chain organic acids in interstitial waters from the Tonga Arc-Trench System, Leg 135. In: Hawkins, J; Parson, L; Allan, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 135, 709-714
DOI: 10.1594/pangaea.916792
title: 1-Hz PPP displacements at GEONET station 0601 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.664878
title: Oceanography at CTD/bottle station IFREMER_1718
DOI: 10.1594/pangaea.916796
title: 1-Hz PPP displacements at GEONET station 0607 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.722257
title: Ultra-violet measurements from station Goodwin Creek (1998-09)

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.484610
title: Physical oceanography at CTD station SN97/15-1

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.825077
title: Age determination results from site La_Croix_Rouge
DOI: 10.1594/pangaea.785124
title: (Table 2) Absolute age of Magellan Seamount Guyots

description: This paper generalizes both original data and all available materials obtained by home and foreign researchers when studying guyots of the Magellan seamounts. The Magellan seamounts represent an extended arc-like chain of seamounts, mainly guyots within the middle part of the East-Mariana Trough. The guyots rise above the relatively flat floor of the East-Mariana Trough with depths about 5500-6000 m to the height up to 4500-4800 m and reach depth level from 1300 to 1200 m. In 1980s-1990s the Magellan seamounts become objects of permanent studies for both home and foreign researchers. First of all it is connected with the fact that considerable accumulations of Fe/Mn crusts and nodules were found at slopes and tops of the Magellan seamounts. Though having some similar features, the guyots of the Magellan seamounts differ considerably in their geological structure, time of formation and duration of volcanic activity. They were studied rather non-uniformly. The Ita-Maitai, Dalmorgeo, Roskomnedra, Vulkanolog, TIG, Hemler guyots and the Himu seamount were studied in detail, while the Nakhodka, IMGiG, TOI, DVGI guyots and the D-4 and Golden Dragonseamounts are less studied. The MA-3, MA-4, MA-10, MA-11, MA-27, MA-29, MA-31 and MA-38 guyots are very poorly studied.
description: Supplement to: Rashidov, V A; Nevretdinov, E B; Selyangin, O B; Nevretdinov, Er B (2003): Geologic-geophysical investigations of Magellan Seamount Guyots, Pacific Ocean. Vestnik KRAUNC (Bulletin of Kamchanka Regional Association "Educational-Scientific Center"). Earth Sciences, No 1, 103-126
DOI: 10.1594/pangaea.834358
title: Ceilometer raw data measured at Neumayer Station (2011-04), links to files
DOI: 10.1594/pangaea.477105
title: Hydrochemistry measured on water bottle samples at station NPac_1974_RY_130E/4504

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.682256
title: Transparency of surface water during Akademik Vernadsky cruise AV10
DOI: 10.1594/pangaea.885913
title: Basic measurements of radiation at station Billings (2015-01)
DOI: 10.1594/pangaea.885987
title: Basic measurements of radiation at station Billings (2012-09)
DOI: 10.1594/pangaea.885988
title: Basic measurements of radiation at station Billings (2012-10)
DOI: 10.1594/pangaea.615261
title: Observation of birds in the Lena Delta Region, mid-July to August 1998 (Table A3-4)

description: Br = breeding species; + = species was observed with unknown status; - = no observation of the species
DOI: 10.1594/pangaea.777990
title: (Table T6a) Chronological list of radiolarian events from ODP Site 199-1218

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.828860
title: Gamma ray attenuation bulk density from IODP Hole 339-U1387A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.916825
title: 1-Hz PPP displacements at GEONET station 0636 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.484514
title: Hydrochemistry measured on water bottle samples at station SAVE3/152-1

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.680759
title: Bitumen contents in sedimentary rocks from Hole VNIIO-1983-Bel-01 drilled in the Kara Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.680748
DOI: 10.1594/pangaea.633956
title: Sea-bed images of permanent plots of rocky benthos at Medes, site Pota de Llop, plot V6E

description: Area monitored at each permanent plot: 310 cm²
DOI: 10.1594/pangaea.916831
title: 1-Hz PPP displacements at GEONET station 0642 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.678324
title: Litostratigraphic units of the ANDRILL AND1-1B drill core
DOI: 10.1594/pangaea.916845
title: 1-Hz PPP displacements at GEONET station 0657 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.740711
title: Age determination of sediment core SABBION1, Sabbion, France

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.916837
title: 1-Hz PPP displacements at GEONET station 0648 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.664710
title: Oceanography at CTD/bottle station IFREMER_1550
DOI: 10.1594/pangaea.671620
title: Diatom distribution and carbonate content of sediment core PC108 from the continental rise west of the Antarctic Peninsula
DOI: 10.1594/pangaea.916866
title: 1-Hz PPP displacements at GEONET station 0680 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.763774
title: (Table 2) Fauna Harpacticoida and its distribution in the Kandalaksha Bay (White Sea) in July 1998 and 1999

description: Dependence of the faunal composition and species structure of the White Sea littoral Harpacticoida on sediment properties was studied. Three groups of species could be distinguished according to their relationship with sediment properties: (1) species typical of silty sediments, (2) species preferring sediments with high gravel content, and (3) species inhabiting well-sorted washed sands. Vertical distribution of crustaceans within sediments of different types was studied. Vertical migrations of harpacticoids (3) during the tidal cycle were described. Data on interannual variability of harpacticoid fauna are presented.
description: Supplement to: Rybnikov, P V; Kondar', D V; Azovskii, A I (2003): Properties of the White Sea littoral sediments and their influence on the fauna and distribution of Harpacticoida. Translated from Okeanologiya, 2003, 43(1), 97-108, Oceanology, 43(1), 91-102
DOI: 10.1594/pangaea.494707
title: Physical oceanography during cruise K9018_1962
DOI: 10.1594/pangaea.911901
title: Benthic foraminifera of sediment core NBP1502A-KC49
DOI: 10.1594/pangaea.740762
title: Age determination of sediment core SOSVIATS, Mire Sosvyatskoe, Russia

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.917175
title: 1-Hz PPP displacements at GEONET station 1001 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.822547
title: Meteorological measurements in the upper air at station Macquarie Island, 1949-01-01 to 1952-12-31, ERA-CLIM ID 4809

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.477877
title: Hydrochemistry measured on water bottle samples at station SPac_1971_HH_150-100W/19

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.917166
title: 1-Hz PPP displacements at GEONET station 0992 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.829547
title: Physical oceanography measured on water bottle samples during DISCOVERY cruise D191

description: Institute of Oceanographic Sciences Deacon Laboratory (now National Oceanography Centre, Southampton). Authorship was originally "BODC" and was changed by request of the BODC.
DOI: 10.1594/pangaea.665515
title: Oceanography at CTD/bottle station IFREMER_2355
DOI: 10.1594/pangaea.917165
title: 1-Hz PPP displacements at GEONET station 0991 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.740765
title: Age determination of sediment core SPITS, Semmeldalen, Norway

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.747530
title: Meteorological observations during ASTUTO cruise from El Callao de Lima to Cádiz started at 1778-03-13, Version 5
DOI: 10.1594/pangaea.740780
title: Age determination of sediment core SUDOBLE, Sudoble Lake, Belarus

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.748979
title: Meteorological observations during El Grimaldi cruise from La Coruña to La Habana started at 1773-06-01
DOI: 10.1594/pangaea.740632
title: Age determination of sediment core ORGE3, Lac du Mont dOrge, Sion, Switzerland

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.484437
title: Hydrochemistry measured on water bottle samples at station SAVE2/69-1

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.676852
title: Physical properties of sedimentary rocks from Hole VNIIO-1985-Arct-01 drilled in the Barents Sea

description: Types of rocks and their ages are given in the special data set; see: doi:10.1594/PANGAEA.676854
DOI: 10.1594/pangaea.744812
title: (Table 1) Depth and time of first appearance of species identified by fish remains in ODP Site 169-1034

description: Ocean Drilling Program Leg 169S retrieved a complete Holocene sequence from Saanich Inlet, British Columbia, Canada. Fish and diatom remains were extracted from sediments at Site 1034. Very small fish bones, teeth and scales were ubiquitous except in the lowermost glaciomarine clays; scales degraded with depth. In the identifiable fraction, Pacific herring were the most abundant with Pacific hake and cartilaginous fish yielding significant fractions. Fish remains appear just before 12 000 BP but greatest diversity does not occur until about 6500 BP. A smoothed abundance curve highlights two periods of maximal abundance at about 1500 and 6500 BP. Abundances in the last 1000 years are lower than the rest of the record. A correlation with abundances of seven phytoplankton taxa is significant; diatoms explain about a third of the variance. This study demonstrates the use of fish and diatoms from the same paleosedimentary matrix to examine millennia-scale correlations between primary and tertiary production.
description: Supplement to: Tunnicliffe, Verena; O'Connell, J M; McQuoid, Melissa R (2001): A Holocene record of marine fish remains from the Northeastern Pacific. Marine Geology, 174(1-4), 197-210
DOI: 10.1594/pangaea.669510
title: Horizon at station Bermuda
DOI: 10.1594/pangaea.916871
title: 1-Hz PPP displacements at GEONET station 0686 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.669530
title: Underway carbon dioxide in the Indian Ocean of Marion-Dufresne cruise 35MF20030126
DOI: 10.1594/pangaea.727045
title: (Fig. 3) Pollen concentration profile from exposure Fluderbach Ia, Samerberg

description: Horizontal sample surface 6 cm x 6 cm. Zero at the base of the profile. See doi:10.1594/PANGAEA.727046 for the percentages pollen profil.