cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.711534
title: Age determination of sediment core V14 in the Tai O Bay (Table 1)

description: High-resolution boomer profiles from Tai O Bay, Hong Kong SAR, were ground-truthed using ten discontinuously sampled boreholes penetrating bedrock with a maximum length of 82.1 m. The relationship between depth below seabed and seismic profiles was established through the measurement of two borehole compressional-wave velocity profiles. In departure from previous interpretations, nine Quaternary seismic units were identified, which can be divided into eight systems tracts formed by cycles of fourth-order sea-level fluctuations dating back at least to marine isotope stage (MIS) 7 (ca. 190-245 ka). These consist of two lowstand systems tracts, two transgressive systems tracts, and four highstand systems tracts. Secondary unconformities within the highstand deposits are interpreted to document fifth-order sea-level fluctuations. Lowstand deposits are less common because, as soon as the sea level drops by a few metres, Tai O Bay becomes sub-aerially exposed, leading to widespread non-deposition or erosion. At the same time, extensive fluvial erosion and channel incision take place. Filling of the fluvial channels occurs during rising sea level. Lowstand sediments (if present) are generally landslide deposits laid down on a basal alluvial plain. Uncorrected accelerator mass spectrometry (AMS) radiocarbon dates of mollusc shells show that the depositional environment was marine since 6.2 ka, becoming gradually more brackish as a result of progradation of the Pearl River delta. The computed average sedimentation rate for the period 6.2-4.1 ka is 4.4 m/1,000 year, and approximately 1 m/1,000 year since 4.1 ka.
description: Supplement to: Bahr, André; Wong, H K; Yim, Wyss W-S; Huang, G; Lüdmann, Thomas; Chan, L S; Ridley Thomas, W N (2005): Stratigraphy of Quaternary inner-shelf sediments in Tai O Bay, Hong Kong, based on ground-truthed seismic profiles. Geo-Marine Letters, 25(1), 20-33
DOI: 10.1594/pangaea.880437
title: (Table S1.2) Geographic distance between each pair of 36 study islands in the Thousand Island Lake, China

description: Geographic distance was estimated as the shortest shore-to-shore distance between island pairs.
DOI: 10.1594/pangaea.495431
title: Water temperature XBT profiles from cruise U31XX45172_1973
DOI: 10.1594/pangaea.748704
title: Meteorological observations during DRUID cruise from Torbay to Antigua started at 1768-03-03
DOI: 10.1594/pangaea.750032
title: Meteorological observations during La Atrevida cruise from Desconocido to Acapulco started at 1791-01-07
DOI: 10.1594/pangaea.880438
title: (Table S1.3) Occupancy data of winter residents by species (45 species) on 36 islands in the Thousand Island Lake, China
DOI: 10.1594/pangaea.880439
title: (Table S1.4) Occupancy data of winter visitors by species (20 species) on 36 islands in the Thousand Island Lake, China
DOI: 10.1594/pangaea.880440
title: (Table S1.5) Occupancy data of summer residents by species (43 species) on 36 islands in the Thousand Island Lake, China
DOI: 10.1594/pangaea.710845
title: Isotopic analyses of DSDP Hole 45-395A samples from veins containing gypsum (Table 1)

description: Gypsum and halite crystals, together with saponite and phillipsite, were found in a vein in a basalt sill 625 m below the sea floor at DSDP Site 395A, located 190 km west of the crest of the Mid-Atlantic Ridge. The delta34S value of the gypsum (+19.4‰) indicates a seawater source for the sulfate. The delta18O values of the saponite (+19.9‰) and phillipsite (+18.1‰) indicate either formation from normal seawater at about 55°C or formation from delta18O-depleted seawater at a lower temperature.The gypsum (which could be secondary after anhydrite) was formed by reaction between Ca[2+] released from basalt and SO4[2-] in circulating seawater. The halite could have formed when water was consumed by hydration of basalt under conditions of extremely restricted circulation. A more probable mechanism is that the gypsum was originally precipitated as anhydrite at temperatures above 60°C. As the temperature dropped the anhydrite converted to gypsum. The conversion would consume water, which could cause halite precipitation, and would cause an increase in the volume of solids, which would plug the vein and prevent subsequent dissolution of the halite.
description: Supplement to: Drever, James I; Lawrence, James R; Antweiler, Ronald C (1979): Gypsium and halite from the Mid-Atlantic Ridge, DSDP Site 395. Earth and Planetary Science Letters, 42(1), 98-102
DOI: 10.1594/pangaea.877706
title: (Table 2) Stable hydrogen and carbon isotopes of C37 alkenones during Termination I and II of sediment core MD02-2594
DOI: 10.1594/pangaea.694646
title: Temperature and salinity in the water column of the Ionian Sea at Station SEPT-2000-IRI45

description: The 911plus set has been used. It consists of the 9plus underwater CTD unit and the 11plus V2 deck unit. It has high resolution sampling (24 Hz), pump-controlled T-C ducted flow, up to 10500 meter (15,000 psia) depth capability, maximum auxiliary sensor flexibility, and modem channel for water sampling control. The 911plus set has eight 12-bit A/D channels and supports redundant C&T sensors or custom auxiliary digital inputs.
DOI: 10.1594/pangaea.884325
title: Plankton arsenic content in urban lakes in the Puget Sound lowland from September 2015 to August 2016
DOI: 10.1594/pangaea.915051
title: Planktonic archaeal phosphorus affinity and apportionment (PAPAA)

description: Complete cell count, nutrient concentration, and radiotracer data for culture incubations and results presented in the manuscript "Carbon recycling efficiency and phosphate turnover by marine nitrifying archaea". This includes measurement of the following parameters for up to nine time points in cultures of N. maritimus strains NAOA6 and SCM1:For each culture incubation, the time points where C and P uptake rates were considered to be first-order are identified by a value of 1 in the column "Linear Y/N".Columns headed by "SD" provide the standard deviation of the value listed in the column to the immediate left.
DOI: 10.1594/pangaea.887588
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2005408
DOI: 10.1594/pangaea.887605
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2009403
DOI: 10.1594/pangaea.887234
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2008402

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.773227
title: Distribution of lithologic units from IODP Hole 316-C0004C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.887714
title: Meteorological observations from automatic weather station Filchner, Antarctica, 2017

description: The mounting heights given in the comment section for each parameter are those at the time of deployment (2015-12-28). Questionable data has been flagged. Main limitations are seen in: 1) Long-wave radiation measurements are affected by rime at least in the period from 2017-04-05 until 2017-09-06; 2) Wind speed measurements are affected by rime at least from 2017-05-02 until 2017-09-06; 3) The thermometer/hygrometer are rimed from the 2017-03-06 until 2017-11-11. Humidity measurements in this time need to be disregarded. Temperature measurements will be affected as well, e.g. inertia due to the rime cover of the instrument. 4) Datalogger issues with the internal voltage reference caused peaks in pressure and wind direction measurements. These are marked as invalid data.
DOI: 10.1594/pangaea.778479
title: (Table 2) Sample description and accumulation rates of ODP Hole 129-801
DOI: 10.1594/pangaea.711424
title: Basic measurements of radiation at station Regina (2006-02)
DOI: 10.1594/pangaea.887747
title: Continuous meteorological observations at Neumayer station (2017-07)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.711437
title: Basic measurements of radiation at station Regina (2007-03)
DOI: 10.1594/pangaea.887752
title: Continuous meteorological observations at Neumayer station (2017-12)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.870831
title: Experiment on effects of elevated pCO2 on bivalve dominated communities: Tissue concentration of malondialdehyde
DOI: 10.1594/pangaea.887214
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2005404

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.887716
title: Meteorological observations from an automatic weather station 1km northwest of Neumayer Station, Antarctica, 2017

description: The mounting heights given in the comment section for each parameter are those at the time of deployment (2017-03-15). The data has been validated against the measurements at the Neumayer Station. Questionable and non-valid data has been flagged.
DOI: 10.1594/pangaea.887746
title: Continuous meteorological observations at Neumayer station (2017-06)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.887749
title: Continuous meteorological observations at Neumayer station (2017-09)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.887720
title: (Table 1) Fractional abundances of GDGTs in DSDP Hole 94-608
DOI: 10.1594/pangaea.887750
title: Continuous meteorological observations at Neumayer station (2017-10)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.887751
title: Continuous meteorological observations at Neumayer station (2017-11)

description: The meteorological observatory Neumayer continuously acquires meteorological parameters. Measurements are taken on or near the meteorological 10m-mast, located some 300m south-east of the main station building. Co-located there are BSRN (Baseline Surface Radiation Network) measurements taken. The measurement interval of the raw data is approximately 6s. Data is quality controlled: All measurements are checked daily on site and again prior to publication according to BSRN standards. Knowingly affected or erroneous data is removed.
DOI: 10.1594/pangaea.887763
title: Water vapor mixing ratio from MLS/GEOSCCM/trajectory model simulations and tropical average time series of regressors from ERAi/MERRA-2/GEOSCCM, link to netCDF files

description: The zip contains the following files:MLS_traj_water_vapor_100hpa.nc and GEOSCCM_traj_water_vapor_100hpa.nc are netCDF files of the water vapor mixing ratio from MLS/GEOSCCM/trajectory model simulations. All data are lon/lat/time at 100 hPa in parts per million by volume.Reanalyses_regressors.nc and GEOSCCM_regressors.nc contain the tropical average time series of regressors from ERAi/MERRA-2/GEOSCCM. These regressors are indices for BDC, tropospheric temperature and/or QBO.
description: Supplement to: Ye, Hao; Dessler, Andrew; Yu, Wandi (2018): Effects of convective ice evaporation on interannual variability of tropical tropopause layer water vapor. Atmospheric Chemistry and Physics, 18(7), 4425-4437
DOI: 10.1594/pangaea.750191
title: Meteorological observations during La Loir cruise from Brest to Martinique started at 1786-03-06
DOI: 10.1594/pangaea.750701
title: Meteorological observations during MEERMIN cruise from Curaçao to Vlissingen started at 1849-09-04
DOI: 10.1594/pangaea.549207
title: Atmospheric carbon dioxide in the Atlantic Ocean of Quima cruise QUIMA20060604

description: Atmospheric measurements refer to a height of 45 m.a.s.l
DOI: 10.1594/pangaea.819132
title: (Table 1) Oxygen and carbon isotopes for planktonic foraminifers at DSDP Hole 64-480

description: During the cleaning of the HPC core surfaces from Hole 480 for photography, the material removed was conserved carefully in approximately 10 cm intervals (by K. Kelts); this material was made available to us in the hope that it would be possible to obtain oxygen isotope stratigraphy for the site. The samples were, of course, somewhat variable in size, but the majority were probably between 5 and 10 cm**3. Had this been a normal marine environment, such sample sizes would have contained abundant planktonic foraminifers together with a small number of benthics. However, this is clearly not the case, for many samples contained no foraminifers, whereas others contained more benthics than planktonics. Among the planktonic foraminifers the commonest species are Globigerina bulloides, Neogloboquadrina dutertrei, and N. pachyderma. A few samples contain a more normal fauna with Globigerinoides spp. and occasional Globorotalia spp. Sample 480-3-3, 20-30 cm contained Globigerina rubescens, isolated specimens of which were noted in a few other samples in Cores 3,4, and 5. This is a particularly solution-sensitive species; in the open Pacific it is only found widely distributed at horizons of exceptionally low carbonate dissolution, such as. the last glacial-to-interglacial transition.
description: Sediment depth is given in mbsf. The analyses with # were made immediately after a machine breakdown; it seems likely, in the light of their plotted position in Figure 1, that they are unreliable. It is our normal procedure to vacuum-roast samples immediately before analysis (in batches of 10 samples); these samples had been roasted before the machine breakdown, which was only fully cured after three weeks. We suspect that vacuum-roasting may decompose a small percentage of the calcite of the foraminifers to CaO, which would be expected to take up atmospheric moisture and CO2 to give a small amount of carbonate of a different isotopic composition. Whether or not this is the correct explanation, we consider that the asterisked analyses should be disregarded.
description: Supplement to: Shackleton, Nicholas J; Hall, Michael A (1982): Oxygen isotope study of continuous scrape samples from Site 480. In: Curray, JR; Moore, DG; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 64, 1251-1254
DOI: 10.1594/pangaea.898669
title: Surface water Dissolved Organic Matter (DOC, CDOM) in the Lena River (2013)
DOI: 10.1594/pangaea.898705
title: Surface water Dissolved Organic Matter (DOC, CDOM) in the Lena River (2010)
DOI: 10.1594/pangaea.742622
title: Physical oceanography during LANCE cruise LA97/2
DOI: 10.1594/pangaea.771516
title: Physical oceanography during Walther Herwig II cruise WH094
DOI: 10.1594/pangaea.887787
title: Physical oceanography of CARIOCA buoy at station HL2 at the Scotain Shelf in 2014
DOI: 10.1594/pangaea.773652
title: MSCL measurements from IODP Hole 316-C0006E

description: Update on 2018-01-19: Parameter 'Susceptibility, volume' has been converted from [10**-5 SI] to [10**-6 SI]. All values were previously given in the wrong unit.
DOI: 10.1594/pangaea.774547
title: Physical oceanography from mooring TR_Micro6 at Tisler Cold-Water Coral Reef, Norway
DOI: 10.1594/pangaea.772815
title: Core-section summary from IODP Hole 315-C0002C
DOI: 10.1594/pangaea.772816
title: (Table 5) Averaged hydrocarbon compositions of gas hydrates sampled at GC185 and GC415 and the standard deviation encountered in the samples
DOI: 10.1594/pangaea.773506
title: Fossil occurrence of calcareous nannofossils from IODP Hole 316-C0006E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.708676
title: (Table 2) K and Cs contents of smectites and analcites from DSDP Hole 51-417A

description: For Rb and Sr data see Hart and Staudigel (1978) data sets: doi:10.1594/PANGAEA.708668, and Richardson et al. (1980) data sets: doi:10.1594/PANGAEA.708671
DOI: 10.1594/pangaea.708724
title: Mineralogy and oxygen isotope values of silicified claystone and porcelanite from DSDP Hole 35-323

description: Discrepancies between predicted and observed interstitial water profiles for sites 322 and 323, Leg 35, Bellingshausen Abyssal Plain, were used to identify sites of reaction for further mineralogical and chemical investigations. Two major reaction sites were identified at site 323:(1) In the silicification zone between 410 and 505 m depth, where dissolution of biogenic (opaline) silica, plagioclase and a few coccoliths and the formation of opal-CT, Mg-rich smectite and K-feldspar are responsible for the observed silica, Ca[2+], Mg[2+], and K[+] interstitial water gradients. Dissolution of biogenic silica provided most of the silica for the porcelanites.(2) In the basalt, weathering of pyroxene and plagioclase and the formation of celadonite, smectite, calcite, and goethite are probably responsible for the observed Ca[2+], Mg[2+], and K[+] interstitial water gradients below the silicification zone.The chemistry of authigenic smectites reflects the composition of their precursor(s).
description: Supplement to: Kastner, Miriam; Gieskes, Joris M (1976): Interstitial water profiles and sites of diagenetic reactions, Leg 35, DSDP, Bellingshausen abyssal plain. Earth and Planetary Science Letters, 33(1), 11-20
DOI: 10.1594/pangaea.708736
title: (Table 2) Chemical composition of the DSDP Hole 42-373A basalts
DOI: 10.1594/pangaea.696147
title: Yearly production of stewed marine products in 1992, Chile
DOI: 10.1594/pangaea.696150
title: Yearly production of stewed marine products in 1995, Chile
DOI: 10.1594/pangaea.695638
title: Radiosonde measurements from station Sede Boqer (2007-01)

description: Wind speed was multiplied by a factor of 0.1 (2009-08-28). Start location: Bet-Dagan, Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.784260
title: Laser profiles of sea ice surface roughness during ARANDA cruise IRIS 2005 from flight IRIS2005_200503131346
DOI: 10.1594/pangaea.706294
title: Weighted mean depth of zooplankton during Alexander von Humboldt cruise AvH44/02/03

description: Weighted mean depth calculated with OST 1.4.1.232a
DOI: 10.1594/pangaea.706811
title: (Table 4-6) Chemical composition of interstitial solutions from sediments of DSDP Hole 12-116
DOI: 10.1594/pangaea.706812
title: (Table 4-6) Chemical composition of interstitial solutions from sediments of DSDP Hole 12-119
DOI: 10.1594/pangaea.706814
title: (Table 4-6) Chemical composition of interstitial solutions from sediments of DSDP Hole 15-147
DOI: 10.1594/pangaea.706818
title: (Table 7) Chemical composition of interstitial solutions from sediments of DSDP Hole 22-214
DOI: 10.1594/pangaea.706820
title: (Table 7) Chemical composition of interstitial solutions from sediments of DSDP Hole 22-217
DOI: 10.1594/pangaea.706156
title: (Page 118-119) Description of surface sediments during the drift of Vessel Varna

description: The Netherlands expedition intended to establish a station at Port Dikson, at the mouth of the Ienissei (Yenisey) river, but their ship was beset in heavy sea ice in the Kara Sea. The Varna, along with the Danish vessel Dijmphna, drifted with the ice for the entire IPY year. A station was built on the sea ice in October, near the two trapped ships. The Varna was crushed and finally sank on July 24, 1883.
DOI: 10.1594/pangaea.706826
title: Basic and other measurements of radiation at station Barrow (2008-04), Version 1

description: Ellsworth G. Dutton discovered a calibration glitch in the SWD "Short-wave downward (GLOBAL) radiation" data for Barrow, Alaska. SWD data was therefore removed from this dataset. Please refer to the updated Version 2 (see replaced by reference) with correct calibration.
DOI: 10.1594/pangaea.706851
title: Basic measurements of radiation at station Kwajalein (2008-05)
DOI: 10.1594/pangaea.706591
title: (Table 2) Rhenium and platinum-group element concentrations and Os isotope data for Philippine Sea Plate basalts from DSDP Hole 58-446A
DOI: 10.1594/pangaea.706997
title: (Appendix 2) Chemical composition of bulk sediments from DSDP Hole 38-336

description: Data have been corrected for pore fluid contents
DOI: 10.1594/pangaea.695838
title: Yearly production of fresh frozen marine products in 1997, Chile
DOI: 10.1594/pangaea.729662
title: (Table 1) Cretaceous calcareous nannofossils from ODP Hole 123-765C

description: species abundance: RE = reworked, R = rare (1 specimen per 101-100 fields of view at 1500 X), F = few (1 specimen per 11-100 fields), C = common (1 specimen per 2-10 fields), A = abundant (1-10 specimens per field), ? = questionable present, - = not present
DOI: 10.1594/pangaea.775169
title: Continuous meteorological observations at Neumayer station (2010-09)
DOI: 10.1594/pangaea.695809
title: Documentation of sediment core GIK12560-1
DOI: 10.1594/pangaea.695811
title: Documentation of sediment core GIK12567-1
DOI: 10.1594/pangaea.817202
title: Core-section summary from IODP Hole 343-C0019E
DOI: 10.1594/pangaea.817203
title: Anisotropy-magnetic susceptibility from IODP Hole 343-C0019E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.751378
title: (Table 6) Analyses of epidote from ODP Hole 111-504B
DOI: 10.1594/pangaea.695648
title: Radiosonde measurements from station Tateno (2007-11)
DOI: 10.1594/pangaea.737426
title: (Table 22) Concentrations of methane, carbon dioxide, and C2-C5 hydrocarbon gases in samples from DSDP Holes 50-415 and 50-415A
DOI: 10.1594/pangaea.856895
title: (Table 1) Stratigraphy of sediment core Voulkaria_1966
DOI: 10.1594/pangaea.807760
title: (Table 2) Oxygen- and carbon-isotopes of Globigerina bulloides and Neogloboquadrina pachyderma at DSDP Hole 80-549A
DOI: 10.1594/pangaea.829700
title: Core summary for IODP Hole 338-C0002L

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.879312
title: Total organic carbon content, calcium carbonate and the stable carbon isotope collected from East Tributary section