cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.916608
title: 1-Hz PPP displacements at GEONET station 0411 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.749606
title: Meteorological observations during HIPPOMENES cruise from Tafelbaai to Batavia started at 1838-02-10
DOI: 10.1594/pangaea.822641
title: Meteorological measurements in the upper air at station Fouad Airport, 1948-06-10 to 1951-12-31, ERA-CLIM ID 4964

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.587199
title: Physical oceanography at CTD station M1_CTD316 of the Persian Gulf
DOI: 10.1594/pangaea.752332
title: Meteorological observations during STANDVASTIGHEID cruise from Rammekens to Kust van Afrika started at 1791-03-12
DOI: 10.1594/pangaea.495711
title: Water temperature XBT profiles from cruise U74X079430_1982
DOI: 10.1594/pangaea.757698
title: Calcium carbonate content in surface sediments on Antarctic shelves

description: Ref. data cited as Archer 1996: "Historical data for the distribution of calcium carbonate in coretop sediments was compiled from the literature. The data was presented by Biscaye et al. (1976, doi:10.1029/JC081i015p02595), Berger et al. (1976, doi:10.1029/JC081i015p02617), Cweink (1986), and Kolla et al. (1976, doi:10.1029/JC081i015p02605). Much of the data originated in the Scripps sedimentological data set, compiled by Gustaf Arhenius and colleagues". See doi:10.1594/PANGAEA.56017 for the Archer data-compilation. Antarctic shelf data were extracted and quality controlled from the global data compilation by Seiter et al. (2004, doi:10.1016/j.dsr.2004.06.014).
DOI: 10.1594/pangaea.681390
title: Radiosonde measurements from Georg-von-Neumayer Station (1988-10)
DOI: 10.1594/pangaea.916687
title: 1-Hz PPP displacements at GEONET station 0491 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916689
title: 1-Hz PPP displacements at GEONET station 0493 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.496660
title: Water temperature XBT profiles from cruise UNZ_1987
DOI: 10.1594/pangaea.497022
title: Physical oceanography from BT during cruise M90BY00052B_1989
DOI: 10.1594/pangaea.664184
title: Oceanography at CTD/bottle station IFREMER_1025
DOI: 10.1594/pangaea.916621
title: 1-Hz PPP displacements at GEONET station 0424 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916721
title: 1-Hz PPP displacements at GEONET station 0526 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916632
title: 1-Hz PPP displacements at GEONET station 0435 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.665925
title: Oceanography at CTD/bottle station IFREMER_2751
DOI: 10.1594/pangaea.854940
title: (Tables, page 14 and 15) Chemical composition of manganese nodules embedded in the grey shales of the Pasquia Hills, Saskatchewan

description: The basal few hundred feet of grey shales from the Ruling Mountain formation in the Pasquia Hills, Saskatchewan contain nodular concretions rich in iron and manganese. The nodules are resistant to erosion and are abundant in stream beds thereby providing a ready guide to prospecting for their outcrops. The manganiferous horizon is exposed on the Wakei, Whitepoplar and Bainbridge rivers and in several of the canyons on the north slope of the hills as far west as the Man River. The nodules occur in layers as long as 20 to 30 feet and never greater than one nodule thick. In dividual concretions are egg-shaped or disk-shaped with a thickness a one 1 to 6 inches and equivalent diameters although rare specimen are 20 inches in diameter. Being light grey to greenish grey they are often covered by athin (5mm or less) black or light brown skin. The Pasquia nodules are similar geologically and mineralogically to a vast deposit of manganese nodules which occurs near Chamberlain, South Dakota.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Beck, L S (1974): Geological Investigations in the Pasquia Hills Area. Geological Report. Saskatchewan Geological Survey, Canada; http://economy.gov.sk.ca/Default.aspx?DN=992f1309-df71-40b5-b7ce-8279197a1ed9, 158, 16 pp
DOI: 10.1594/pangaea.894146
title: Pollen profile of sediment core SETESGR, Grostjørna, Norway

description: This dataset was archived on 2018-09-14 from the EPD database. (http://www.europeanpollendatabase.net). Date analyzed: 1999
DOI: 10.1594/pangaea.817093
title: Physical oceanography during PELAGIA cruise MERLIM98
DOI: 10.1594/pangaea.825968
title: Core summary for IODP Hole 329-U1366D
DOI: 10.1594/pangaea.774606
title: (Table 1) Radiolarian accumulation rates and geochemistry of ODP Site 184-1143

description: Late Miocene–Recent micropaleontological and geochemical records from Ocean Drilling Program (ODP) Site 1143 in the southern South China Sea (SCS) indicate that increase and decrease in abundance of siliceous plankton may be controlled mainly by the input of nutrients derived from land and provided by upwelling. A high export production event - a “biogenic bloom” event - occurred in the southern SCS between 12 and 6 Ma. During this period, high ratios of smectite/(illite + chlorite), smectite/quartz and Al/K indicate a high weathering intensity of the Asian continent, possibly due to the intensification of the East Asian Summer Monsoon (EASM), which may have increased the net flux of nutrients to the ocean, both directly through terrestrial input and indirectly through upwelling activity. A drop in Ba/Ti, Al/Ti and Ca/Ti values around 6 Ma may indicate a lowering of productivity, possibly due to the large consumption of sea surface nutrients by the “biogenic bloom”. Alternatively, it may indicate a shift in terrigenous input source area. At about 5.4 Ma, a decrease in weathering intensity, as indicated by a sudden decrease in the values of smectite/(illite + chlorite), smectite/quartz and Al/K, might have led to a sudden decrease of terrestrial nutrient input to the SCS. We suggest that the biogenic bloom ended when nutrients in surface waters were exhausted, because of a decrease in supply as well as a decrease in upwelling intensity due to weakening of the EASM. As a result, radiolarians were absent in the studied area between ~6 and 3.2 Ma. At ~3.2 Ma, radiolarians began to recover, possibly because the start of Northern Hemispheric glaciation and the rapid uplift of the Tibet Plateau led to intensification of the East Asian monsoon. After the Mid-Pleistocene Climate Transition at 0.9 Ma, the abundance and mass accumulation rates of radiolarians increased, probably as a result of increased upwelling activity driven by the increasing intensity of the summer monsoon.
description: Sediment depth is given in mcd.
description: Supplement to: Zhang, Lili; Chen, Muhong; Xiang, Rong; Zhang, Lanlan; Lu, Jun (2009): Productivity and continental denudation history from the South China Sea since the late Miocene. Marine Micropaleontology, 72(1-2), 76-85
DOI: 10.1594/pangaea.785854
title: (Table 2) Stable isotope record of foraminifera from ODP Hole 133-817A
DOI: 10.1594/pangaea.828606
title: Magnetic remanence from IODP Hole 323-U1345A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829258
title: P-Wave velocity (PWC) from IODP Hole 340-U1397B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.825973
title: Pass-through measurements of magnetic susceptibility from IODP Hole 329-U1366D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.916620
title: 1-Hz PPP displacements at GEONET station 0423 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916652
title: 1-Hz PPP displacements at GEONET station 0456 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916665
title: 1-Hz PPP displacements at GEONET station 0469 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.825987
title: Pass-through measurements of magnetic susceptibility from IODP Hole 329-U1366E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.916760
title: 1-Hz PPP displacements at GEONET station 0569 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.825991
title: P-Wave velocity (PWC) from IODP Hole 329-U1366E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.499381
title: Physical oceanography from BT during cruise U90XX07681B_1987
DOI: 10.1594/pangaea.691184
title: Nutrient concentrations in water samples collected at Station MARCH-94-GN3619940280100430 in the Aegean Sea
DOI: 10.1594/pangaea.818221
title: (Table 1) Relative abundances of biphytanediols and biphytanes in IODP Site 315-C0001

description: The distribution of acyclic and cyclic biphytanediols, the putative breakdown products of glycerol dialkyl glycerol tetraethers (GDGTs), was investigated for recent marine sediments from Nankai Trough, offshore Kii Peninsula. The most abundant diol is tricyclic biphytanediol, whose relative abundance is in the range 32–46%. Its carbon skeleton, with two cyclopentane rings and one cyclohexane ring, is the same as would be expected via a crenarchaeol origin. Based on the structure of crenarchaeol, the tricyclic biphytanediol is considered to be derived not only from crenarchaeol but also from other unknown sources. The ring distributions of the biphytanediols are different from those of the biphytanes obtained from intact polar lipids by way of chemical treatment, suggesting that biphytanediols are not solely the diagenetic products of in situ GDGTs.
description: Supplement to: Saito, Hiroyuki; Suzuki, Noriyuki (2010): Distribution of acyclic and cyclic biphytanediols in recent marine sediments from IODP Site C0001, Nankai Trough. Organic Geochemistry, 41(9), 1001-1004
DOI: 10.1594/pangaea.691185
title: Nutrient concentrations in water samples collected at Station MARCH-94-GN3619940280100440 in the Aegean Sea
DOI: 10.1594/pangaea.739591
title: Pollen profile NERO489, Lake Nero, Russia

description: Method: KOH, Erdtman's 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.822867
title: Meteorological measurements in the upper air at station Ostrov Chetyrekhstolbovoy, 1924-09-21 to 1925-06-03, ERA-CLIM ID 5771

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.663482
title: Oceanography at CTD/bottle station IFREMER_0322
DOI: 10.1594/pangaea.916924
title: 1-Hz PPP displacements at GEONET station 0741 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.841354
title: (Table 2) Radiocarbon ages of eastern equatorial Pacific sediment cores

description: We use planktonic oxygen isotope (d18O) records spanning the last 30,000 years (kyr) to constrain the magnitude and spatial pattern of glacial cooling in the upwelling environment of the eastern equatorial Pacific (EEP). Fourteen new downcore d18O records were obtained from surface-dwelling planktonic foraminifera Globigerinoides sacculifer and Globigerinoides ruber in eight cores from the upwelling tongue of the EEP. All sites have sedimentation rates exceeding 5 cm/kyr and, with one exception, lie above the modern depth of the foraminiferal lysocline. Sites directly underlying the cool band of upwelling immediately south of the equator record mean late Holocene (LH)-Last Glacial Maximum (LGM) d18O amplitudes ranging between 1.0 and 1.3 per mil. We estimate that mean sea surface temperatures (SST) in this region during the LGM were on average 1.5 ± 0.5°C lower than the LH. Larger d18O amplitudes are observed in sites north of the equator, indicating a spatial pattern of reduced meridional SST gradient across the equator during the LGM. This result is supported by comparison of Mg/Ca SST reconstructions from two sites straddling the equator. We interpret the reduction of this gradient during the LGM as evidence for a less intense cold tongue-Intertropical Convergence Zone (ITCZ) frontal system, a more southerly position of the ITCZ, and weaker southeast equatorial trades in the EEP.
description: Data of RC11-238 previously published in Faul et al. (2000). All measurements were made on monospecific foraminiferal samples comprised of N. dutertrei shells, except the 400 cm sample from core V21-30 where a mix of N. dutertrei and O. universa was used.
description: Supplement to: Koutavas, Athanasios; Lynch-Stieglitz, Jean (2003): Glacial-interglacial dynamics of the eastern equatorial Pacific cold tongue-Intertropical Convergence Zone system reconstructed from oxygen isotope records. Paleoceanography, 18(4), 1089
DOI: 10.1594/pangaea.916857
title: 1-Hz PPP displacements at GEONET station 0670 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.496736
title: Physical oceanography from BT during cruise K35AIB_1956
DOI: 10.1594/pangaea.786440
title: (Table 2) Geochemistry of basalt glass of ODP Hole 206-1256D
DOI: 10.1594/pangaea.741836
title: Lithology of sediment core WIGGENHA, Wiggenhall St. Germans, United Kingdom

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.756572
title: Consolidation characteristics of outer Bengal Fan deposits (Table 1)

description: The state of consolidation of outer Bengal Fan deposits is closely related to their depositional history. Early Pleistocene sediments are underconsolidated, i.e., fabric strength is lower than under equilibrium with the present overburden stress, at depths greater than 60-80 mbsf. This may be due to rapid accumulation (&gt;15-20 cm/k.y.) and overlying low-permeability (&lt;10**-7 cm/s) deposits. The underlying Pliocene sediments are overconsolidated, i.e., fabric strength is higher than in equilibrium with the present overburden stress; at Sites 717 and 719 the sediments are slightly overconsolidated, whereas at Site 718 the overconsolidation is significant. Overconsolidation is explained by erosion that occurred during the early Pleistocene for which a stratigraphic gap was recorded in the drilled cores. The eroded section is estimated to be in the range of 10-40 m at Sites 717 and 719, respectively, and 130-150 m at Site 718. Below 250-300 mbsf the most sediments are normally consolidated. The amount of erosion seems to be related to block rotation and uplift due to intraplate deformation.
description: Supplement to: Wetzel, Andreas (1990): Consolidation characteristics and permeability of Bengal Fan sediments drilled during Leg 116. In: Cochran, JR; Stow, DAV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 116, 363-368
DOI: 10.1594/pangaea.536302
title: Accumalion rate of carbonte free sediment for sediment core V22-196 northern subtropical Atlantic (App. 4)
DOI: 10.1594/pangaea.916858
title: 1-Hz PPP displacements at GEONET station 0672 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.536305
title: Accumalion rate of carbonte free sediment for sediment core V23-100 northern subtropical Atlantic (App. 4)
DOI: 10.1594/pangaea.916784
title: 1-Hz PPP displacements at GEONET station 0593 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916811
title: 1-Hz PPP displacements at GEONET station 0622 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.816393
title: (Table 3) Nd isotopic ratios of ancient seawater fraction of ODP Sites 121-758 and 121-757 samples
DOI: 10.1594/pangaea.916864
title: 1-Hz PPP displacements at GEONET station 0678 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.904728
title: Table SM-3: Splice tie table for ODP Site 138-850

description: This is the splice tie table for Site 850 (originally preferred format for presenting the splice).Each row lists a tie point between consecutive cores, which together form the splice. The table starts with the topmost core and ends with the final core in the splice.TIE indicates where that the core is directly tied to the previous core. The revised m CCSF (revised metres core composite depth below sea floor) depth will be identical between cores at the location of the splice tie point.APPEND indicates where the core is appended to the previous core. The revised m CCSF (revised metres core composite depth below sea floor) depth may not be identical between cores at the location of the append point.
DOI: 10.1594/pangaea.916865
title: 1-Hz PPP displacements at GEONET station 0679 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.509884
title: Total organic carbon, nitrogen and phosphorus oxygen content of sediment core GIK01168, Arabian Sea, African continental margin (Appendix)
DOI: 10.1594/pangaea.495611
title: Water temperature MBT profiles from cruise U74EH26236M_1952
DOI: 10.1594/pangaea.898363
title: Interaction between warm Atlantic-sourced waters and the East Greenland Current in northern Denmark Strait (68°N) during the last 10 600 cal a BP

description: Changes in the Holocene interaction of the (i) cold/fresh East Greenland Current (EGC) and (ii) warm/saline Irminger Current (IC) in northern Denmark Strait have been reconstructed from benthic and planktic foraminifera assemblages, ice-rafted debris, grain-size analyses and quantitative X-ray diffraction. During the time from c. 10 600 to 8000 cal a BP, palaeoceanographic reconstructions reveal waning deglacial influence from the receding Greenland Ice Sheet and presence of a strong EGC caused low surface water productivity. From c. 8000 cal a BP, a predominant influence of Atlantic-sourced IC waters on subsurface water conditions became established in northern Denmark Strait, which accompanied low surface water productivity. Relatively warm surface and subsurface water conditions, i.e. reduced EGC and strong IC influence, are found from c. 6500 to 4500 cal a BP, representing Holocene optimum-like conditions. A mid- to late Holocene EGC strengthening caused increased stratification and formation of a distinct halocline. However, we recognize millennial-scale periods of reduced stratification by an enhanced influence of Atlantic-sourced IC Water on surface water conditions: (i) at c. 2500–1400 cal a BP - the time of the Roman Warm Period and (ii) at c. 300 cal a BP - the later part of the Little Ice Age. These periods of oceanic warming probably relate to changes in the Subpolar Gyre dynamics that led to enhanced entrainment of Atlantic-sourced IC Water into northern Denmark Strait.
description: Supplement to: Perner, Kerstin; Jennings, Anne E; Moros, Matthias; Andrews, John T; Wacker, Lukas (2016): Interaction between warm Atlantic-sourced waters and the East Greenland Current in northern Denmark Strait (68°N) during the last 10 600 cal a BP. Journal of Quaternary Science, 31(5), 472-483
DOI: 10.1594/pangaea.829033
title: Magnetic remanence from IODP Hole 339-U1387A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.663885
title: Oceanography at CTD/bottle station IFREMER_0725
DOI: 10.1594/pangaea.664537
title: Oceanography at CTD/bottle station IFREMER_1377
DOI: 10.1594/pangaea.916888
title: 1-Hz PPP displacements at GEONET station 0703 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.828507
title: Point measurements of magnetic susceptibility from IODP Hole 323-U1343D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.916946
title: 1-Hz PPP displacements at GEONET station 0765 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.748416
title: (Table 6) Strontium and neodymium isotope ratios of basalts from ODP Hole 111-504B
DOI: 10.1594/pangaea.779490
title: (Table T1) Element concentrations and Strontium and Neodymium isotopes of ODP Hole 191-1179D basalts

description: Sr and Nd isotopic compositions of 19 basalts from Hole 1179D, Leg 191 were analyzed to determine ridge and plume interaction. 87Sr/86Sr and 143Nd/144Nd ratios of the basalts ranged from 0.7029 to 0.7040 and from 0.5131 to 0.5132 (epsilon Nd0 = 9.3 ~ 10.8), respectively. Calculated initial isotopic compositions at 129 Ma, the age of magnetic Anomaly M8, are 87Sr/86Sri = 0.7026 ~ 0.7033 and epsilon NdT = 9.2 ~ 10.6. The initial Sr isotope ratio is higher than that of normal mid-ocean-ridge basalts (MORBs) from the East Pacific Rise and Mesozoic MORBs. They are similar to those of the Shatsky Rise, suggesting a plume component was involved in the formation.
description: Sediment depth is given in mbsf. K2O, Ba, Rb and Sr data are from Shipboard Scientific Party (2001, doi:10.2973/odp.proc.ir.191.104.2001) and Y. Hayasaka (unpubl. data). Epsilon Nd values at 129 Ma are estimated by 147Sm/144Nd = 0.2178, based on element data of average N-MORB (Sun and McDonough, 1989, doi:10.1144/GSL.SP.1989.042.01.19).
description: Supplement to: Sano, Sakae; Hayasaka, Yasutaka (2004): Sr and Nd geochemistry of Hole 1179D basalts. In: Sager, WW; Kanazawa, T; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 191, 1-11
DOI: 10.1594/pangaea.916883
title: 1-Hz PPP displacements at GEONET station 0698 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.775977
title: (Appendix A6) Sediment composition and accumulation rates of ODP Site 178-1095A
DOI: 10.1594/pangaea.785997
title: (Table T1) Calcium carbonate mineralogy and stable isotopic composition of ODP Hole 182-1132C sediments

description: Petrographic observation and carbonate mineralogic and stable isotopic investigation were conducted on lower Oligocene to middle Miocene sediments recovered during Ocean Drilling Program Leg 182 from Site 1132, located at a water depth of 218.5 m immediately seaward of the shelf-slope break of the eastern Eyre Terrace in the western Great Australian Bight. The middle Miocene section consists of bioclastic packstone and grainstone with an interval of partially silicified nannofossil-foraminiferal chalk and is slightly to densely dolomitized. By contrast, the lower Oligocene to lower Miocene section is characterized by a predominance of planktonic and benthic foraminifers, high porosity, absence of chert, and weak dolomitization. The carbon and oxygen isotopic composition of calcites and dolomites between two sections, however, shows no significant difference.
description: Supplement to: Matsuda, Hiroki; Machiyama, Hideaki; James, Noel P (2002): Data report: Petrography and stable isotope geochemistry of lower Oligocene to middle Miocene carbonates, Site 1132, Great Australian Bight. In: Hine, AC; Feary, DA; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 182, 1-11