cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.751161
title: Meteorological observations during PERSEVERENCE cruise from Java Head to The Downs started at 1803-01-08
DOI: 10.1594/pangaea.916276
title: 1-Hz PPP displacements at GEONET station 0066 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.822649
title: Meteorological measurements in the upper air at station Marsa Matrouh, 1955-02-01 to 1956-10-25, ERA-CLIM ID 4972

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.821397
title: Meteorological measurements in the upper air during the 'Deutschen Atlantischen Expediton' of research vessel Meteor in 1925-1927, ERA-CLIM ID 0073C
DOI: 10.1594/pangaea.821626
title: Meteorological measurements in the upper air during ballon flight ERA-CLIM ID 0100

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.752469
title: Meteorological observations during THAMES cruise from Cape Spartel to Plymouth started at 1771-03-21
DOI: 10.1594/pangaea.739839
title: Pollen profile SPAJALLS, Spjällsjön, Sweden

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.682884
title: Continuous meteorological observations at Georg-von-Neumayer station (1983-06)

description: Geocode DATE/TIME has centered values.
DOI: 10.1594/pangaea.762110
title: (Table 1A) Stable carbon and oxygen isotope ratios of planktonic foraminifera of ODP Hole 124-769A
DOI: 10.1594/pangaea.907525
title: Geochemistry of permafrost core Grondalen_9
DOI: 10.1594/pangaea.774192
title: (Table T1) Stable carbon and oxygen isotopes of foraminifers from ODP Site 202-1237

description: Depth (sediment) is given in mbsf. Correction of C. wuellerstorfi d18O values to 'Uvigerina' scale by adding 0.64 per mil.
DOI: 10.1594/pangaea.719198
title: Ultra-violet measurements from station Bondville (1995-04)

description: Version 2, 2009-06-15. 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 2017-02-09.
DOI: 10.1594/pangaea.916296
title: 1-Hz PPP displacements at GEONET station 0088 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.476033
title: Physical oceanography at CTD station AOS94/17-1

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.771683
title: Physical oceanography during Walther Herwig III cruise WH269
DOI: 10.1594/pangaea.805882
title: Geochemistry of sediment core PC-K49, Potter Cove, King George Island
DOI: 10.1594/pangaea.744335
title: Physical oceanography during Scotia cruise Scotia72/1 to the North Sea
DOI: 10.1594/pangaea.746599
title: Meteorological observations during Le Bizarre cruise from Brest to Louisbourg started at 1753-05-04
DOI: 10.1594/pangaea.747026
title: Meteorological observations during POLANEN cruise from Batavia to Kaap de Goede Hoop started at 1749-01-26
DOI: 10.1594/pangaea.747121
title: Meteorological observations during True Briton cruise from Canton to Tillicherry started at 1750-11-07
DOI: 10.1594/pangaea.750409
title: Meteorological observations during LEOPARD cruise from Surat to Aden started at 1800-03-09
DOI: 10.1594/pangaea.756841
title: Stable isotope record, organic geochemistry and sea surface temperature estimation of ODP Hole 117-721B (Table 1)

description: Late Pleistocene sea surface water temperatures (SST) offshore Oman were calculated from the UK'37 ratio measured in sediment extracts from ODP holes drilled on the Oman Margin (723B, 728B) and on the Owen Ridge (721B, 731A). The data revealed a complex history of SST variations with a temperature range of 18°/19°C-27°/28°C, which is in accord with the present-day SST range in the western Arabian Sea. We found that, notably, in the glacial periods of isotopic stages 3 and 8 the SST was lower than during the interglacials. The lowest SST values occurred during isotopic stage 3. A mechanism involving a strong influence of cold northeasterly winds during glacial periods, with the southwestern monsoon being less effective at the same time, explains cold SST during glacial periods. However, further research is necessary to approve or disapprove this mechanism, because in the present study not all glacial periods were clearly marked by low SST values.
description: Supplement to: ten Haven, H Lo; Kroon, Dick (1991): Late Pleistocene sea surface water temperature variations off Oman as revealed by the distribution of long-chain alkenones. In: Prell, WL; Niitsuma, N; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 117, 445-452
DOI: 10.1594/pangaea.746972
title: Meteorological observations during L'AQUILLON cruise started at 1753-01-30
DOI: 10.1594/pangaea.747326
title: Meteorological observations during AMAZON cruise from Cape St Vincent to Barbados started at 1805-05-12
DOI: 10.1594/pangaea.484064
title: Geochemical analysis of sediment core GIK12327-4, West African continental shelf (Table 3)
DOI: 10.1594/pangaea.916317
title: 1-Hz PPP displacements at GEONET station 0110 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.744181
title: Physical oceanography during Dana II cruise Dana04/2 to the North Sea
DOI: 10.1594/pangaea.916319
title: 1-Hz PPP displacements at GEONET station 0112 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916351
title: 1-Hz PPP displacements at GEONET station 0144 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.750911
title: Meteorological observations during NEWCASTLE cruise from Halifax to Quebec started at 1820-06-09
DOI: 10.1594/pangaea.817764
title: (Table 1) Geochemistry of Cocos Plate hemipelagic-pelagic sediments in DSDP Hole 66-487

description: The sedimentary sequence recovered from Hole 487 documents northeast seafloor spreading on the Cocos Plate. A basal 65-meter unit of upper Miocene-Pliocene brown clay was deposited on the subsiding east flank of the East Pacific Rise. The overlying 105-meter unit of gray hemipelagic silt and mud was deposited when Site 487 drifted within reach of terrigenous sediment derived from the Mexican continental margin. Analyses of 21 elements in 45 samples, taken at regular intervals up Hole 487, give a geochemical profile which shows metal enrichment in basal sediment similar to that observed in previously recovered basal sediment sections in the Eastern Pacific (e.g., von der Borch & Rex, 1970; von der Borch et al., 1971). This verifies that the basalt cored at the base the hole is oceanic basement, since the first sediment to be deposited on newly formed ocean crust is characteristically enriched in metals, particularly Fe and Mn. The metals precipitate from circulating hydrothermal-exhalative solutions which are an integral part of active ridge volcanism (summary in Jenkyns, 1978). In this chapter I discuss the geochemistry of the basal metalliferous sediment from Hole 487. The geochemical data may also prove useful in studies of onshore volcanism: mass-balance calculations show that much (possibly all) of the incoming Cocos Plate sediment has been subducted since the Miocene (Watkins et al., this volume). It may have contributed to the genesis of magmas erupted in the Mexican volcanic arc
description: Supplement to: Leggett, Jeremy K (1982): Geochemistry of Cocos Plate pelagic-hemipelagic sediments in Hole 487, Deep Sea Drilling Project Leg 66. In: Watkins, JS; Casey Moore, J; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 66, 683-686
DOI: 10.1594/pangaea.752082
title: Meteorological observations during SEAHORSE cruise from Gravesend to York Factory started at 1792-06-25
DOI: 10.1594/pangaea.751146
title: Meteorological observations during PENZANCE cruise from River Tagus to Portsmouth started at 1755-12-13
DOI: 10.1594/pangaea.822227
title: Meteorological measurements in the upper air at station Mys Vasilieva, 1954-04-20 to 1954-09-22, ERA-CLIM ID 4571
DOI: 10.1594/pangaea.887195
title: Physical oceanography (CTD) during Fridtjof Nansen cruise FN2002404

description: Manufacture calibration were used for conductivity, temperature, pressure and oxygen sensor calibration.
DOI: 10.1594/pangaea.496708
title: Physical oceanography from BT during cruise K06ADB_1956
DOI: 10.1594/pangaea.615307
title: Description of the soil of core LD98_t4b

description: For the position of the transects t, v, and w see also figure 3-1
DOI: 10.1594/pangaea.751160
title: Meteorological observations during PERSEVERENCE cruise from Portsmouth to Madras started at 1802-02-26
DOI: 10.1594/pangaea.752038
title: Meteorological observations during SCORPION cruise from Port Royal to The Downs started at 1796-07-01
DOI: 10.1594/pangaea.777940
title: (Table 9) Factor loading matrix for benthic foraminifera of Northwest Indian Ocean surface sediments
DOI: 10.1594/pangaea.664415
title: Oceanography at CTD/bottle station IFREMER_1255
DOI: 10.1594/pangaea.752809
title: Meteorological observations during WALPOLE cruise from Java Head to Portsmouth started at 1793-01-08
DOI: 10.1594/pangaea.751733
title: Meteorological observations during Rembrandt van Rhijn cruise from Coromandel to Batavia started at 1853-05-07
DOI: 10.1594/pangaea.495054
title: Water temperature XBT profiles from cruise K7442_1974
DOI: 10.1594/pangaea.752395
title: Meteorological observations during SWALLOW cruise from St. Helena to Madras started at 1771-05-06
DOI: 10.1594/pangaea.671389
title: Major and trace element composition of clinopyroxenes from an olivine gabbro of ODP Hole 176-735B (Table 1)

description: Major and trace element profiles of clinopyroxene grains in oceanic gabbros from ODP Hole 735B have been investigated by a combined in situ analytical study with ion probe, and electron microprobe. In contrast to the homogeneous major element compositions, trace elements (REE, Y, Cr, Sr, and Zr) show continuous core to rim zoning profiles. The observed trace element systematics in clinopyroxene cannot be explained by a simple diffusive exchange between melts and gabbros along grain boundaries. A simultaneous modification of the melt composition is required to generate the zoning, although Rayleigh fractional crystallization modelling could mimic the general shape of the profiles. Simultaneous metasomatism between the cumulate crystal and the porous melt during crystal accumulation is the most likely process to explain the zoning. Deformation during solidification of the crystal mush could have caused squeezing out of the incompatible element enriched residual melts (interstitial liquid). Migration of the melt along grain boundaries might carry these melt out of the system. This process named as synkinematic differentiation or differentiation by deformation (Natland and Dick, 2001, doi:10.1016/S0377-0273(01)00211-6) may act as an important magma evolution mechanism in the oceanic crust, at least at slow-spreading ridges.
description: Numbers of ions were calculated on the basis of six O, and assume two cations on T site, Al (IV) and Al (VI) denote the Al in T and M1 site, respectively
description: Supplement to: Gao, Yongjun; Hoefs, Jochen; Hellebrand, Eric; von der Hand, Anette; Snow, Jonathan E (2007): Trace element zoning in pyroxenes from ODP Hole 735B gabbros: diffusive exchange or synkinematic crystal fractionation? Contributions to Mineralogy and Petrology, 153, 429-442
DOI: 10.1594/pangaea.705254
title: (Table 2) Control Points and sedimentation rates for the ODP Site 181-1119 age model

description: Depth is composite depth (mcd) from Weedon and Harris, in: Carter et al, 1999, doi:10.2973/odp.proc.ir.181.2000, 0.45 mcd and 47.58 mcd Diasten, 86.62 mcd unconformity. The model is based upon radiocarbon age control down to ~39 ka (18.67 mcd), and prior to that by matching individualistic features of the climatic record between the 1119 onboard MST natural Q radiation curve (a proxy for mud delivery to the site) and the deuterium record from the Vostok ice core (a proxy for Antarctic air temperature; Petit et al.,1999, doi:10.1038/20859 ), using the Vostok time scale tuned to insolation at 65°N by Shackleton (2000, doi:10.1126/science.289.5486.1897). To reduce arbitrary changes in sedimentation rate, a linear age model was fitted to the six AMS dates between 2.07 and 14.95 (age=13700+710*mcd; R2 =0.96). Because of the marine reservoir correction uncertainties, the radiocarbon-controlled part of the age model is provisional. Age errors up to +/-1 kyr are possible back to ~25 ka, and up to +/-3 kyr between 25 and 40 ka.
DOI: 10.1594/pangaea.752397
title: Meteorological observations during SWALLOW cruise from Surat to Muscat started at 1773-02-24
DOI: 10.1594/pangaea.694399
title: Temperature and salinity in the water column of the Aegean Sea at Station FEBR-1999-IR03

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.753058
title: Meteorological observations during SALTASH cruise started at 1757-07-14
DOI: 10.1594/pangaea.759417
title: (Table 2) Oxygen isotope data from sediment core well 6407/1-2
DOI: 10.1594/pangaea.838607
title: Lithology of sediment core FANGEAS, Fangeas, France

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.477879
title: Hydrochemistry measured on water bottle samples at station SPac_1971_HH_150-100W/21

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.484517
title: Hydrochemistry measured on water bottle samples at station SAVE3/155-2

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.739640
title: Pollen profile PALLUNG, Palü Lunga ob Ramosch, Switzerland

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.778651
title: (Table 1) Bulk carbonate content of ODP Hole 194-1198A sediments, east of the Great Barrier Reef

description: Upper Quaternary sediment sequences east of the Great Barrier Reef are characterized by alternating siliciclastic- and carbonate-rich horizons caused by changes in the input of various sedimentary components and reflected in cores by variations in bulk carbonate content. A total of 153 measurements of bulk carbonate content were determined using the carbonate-bomb technique for late Pleistocene sediments between 0 and 23.69 meters below sea floor (mbsf) in Ocean Drilling Program Hole 1198A. Average sample resolution was 15 cm and multiple analyses were performed on each sample. Bulk carbonate content ranges from a maximum of 94 wt% at 13.63 mbsf to a minimum of 73 wt% at 14.54 mbsf. Five cyclic trends are observed that may relate to five major glacial events during the last 500 k.y. of the Quaternary.
description: Supplement to: Page, Michael C (2004): Data report: Variations in bulk carbonate content, Hole 1198A, 0-23.69 mbsf. In: Anselmetti, FS; Isern, AR; Blum, P; Betzler, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 194, 1-9
DOI: 10.1594/pangaea.829052
title: Magnetic remanence on discrete pieces from IODP Hole 339-U1386A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.916387
title: 1-Hz PPP displacements at GEONET station 0182 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916393
title: 1-Hz PPP displacements at GEONET station 0188 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.776260
title: (Table T1) Depth of target horizons at all ODP Leg 208 sites

description: Walvis Ridge, located in the eastern South Atlantic Ocean, is one of the few known locations where it is possible to recover undisturbed, complete, and possibly expanded Paleogene sediments over a wide range of water depths. The main objective of Ocean Drilling Program (ODP) Leg 208, realized on outer Walvis Ridge in the summer of 2003, was recovery of intact composite sequences of "critical" transitions like the Cretaceous/Tertiary (K/T) boundary, Eocene/Oligocene (E/O) boundary, Paleocene/Eocene Thermal Maximum (PETM), and the Elmo event.Meteor Cruise M49/1, in early 2001, was the main seismic presite survey for Leg 208. The high-resolution multichannel seismic system of the University of Bremen was used to identify drill sites at outer Walvis Ridge that promised recovery of undisturbed, complete, and possibly expanded Cenozoic sequences. Based on these new seismic data, six sites were drilled at water depths between 2500 and 4755 m on the northeastern flank of Walvis Ridge during Leg 208.To ground truth the seismic record, synthetic seismograms were calculated from closely spaced core logging density measurements of Leg 208 cores. The high quality of both seismic and core logging data allows good correlation between synthetic seismograms and recorded seismic data. These results allow identification and characterization of target reflection horizons like the E/O boundary, Elmo horizon, PETM, and K/T boundary in seismic images and dating of individual reflectors.Total sediment thickness in the survey area varies between 200 and 530 m, and the study area can be separated into three zones that have different deposition conditions. In general, seismic data show a decrease in total sediment thickness with increasing distance from the ridge crest, but lateral variations in sedimentation rates were found across the entire survey area. Especially close to the crest of the ridge, these lateral variations in sedimentation rates might indicate the influence of bottom water currents on sedimentation at the outer Walvis Ridge.
description: Supplement to: Bartels, Thomas; Krastel, Sebastian; Spieß, Volkhard (2007): Correlation of high-resolution seismic data with ODP Leg 208 borehole measurements. In: Kroon, D; Zachos, JC; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 208, 1-27
DOI: 10.1594/pangaea.916410
title: 1-Hz PPP displacements at GEONET station 0205 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916444
title: 1-Hz PPP displacements at GEONET station 0240 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.759203
title: Physical oceanography during LANCE cruise LA99/3
DOI: 10.1594/pangaea.916554
title: 1-Hz PPP displacements at GEONET station 0356 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.870156
title: Links to master tracks in different resolutions from POLAR 2 flight EPICA_IX_20
DOI: 10.1594/pangaea.497228
title: Physical oceanography from BT during cruise M90TC00017B_1984
DOI: 10.1594/pangaea.691232
title: Nutrient concentrations in water samples collected at Station SEPT-94-GN3619940280300300 in the Aegean Sea
DOI: 10.1594/pangaea.793277
title: (Table 3) Paleogene radiolarians in DSDP Hole 93-603B

description: Species abundance: C = common (20-30 specimens), F = few (10-20 specimens), R = rare (3-10 specimens), VR= very rare (1-2 specimens), ? = questionable, - = absent.
DOI: 10.1594/pangaea.826105
title: Thermal conductivity of IODP Hole 327-U1363F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.499600
title: Physical oceanography from BT during cruise U90ZB00469B_1974
DOI: 10.1594/pangaea.916576
title: 1-Hz PPP displacements at GEONET station 0378 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.906900
title: Carbon and sulfur content of Lake Hovsgol sediments during the last 18.9 kyrs
DOI: 10.1594/pangaea.822509
title: Meteorological measurements in the upper air at station Buhta Tiksi, 1948-01-03 to 1948-06-29, ERA-CLIM ID 4767
DOI: 10.1594/pangaea.826119
title: P-Wave velocity (PWB) from IODP Hole 327-U1363G

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826124
title: Basic measurements of radiation at station Nauru Island (2007-03)

description: Version 2, 2014-01-15
DOI: 10.1594/pangaea.497050
title: Physical oceanography from BT during cruise M90CQB_1989_1989
DOI: 10.1594/pangaea.916468
title: 1-Hz PPP displacements at GEONET station 0265 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916471
title: 1-Hz PPP displacements at GEONET station 0268 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.916580
title: 1-Hz PPP displacements at GEONET station 0382 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.744363
title: Physical oceanography during Thalassa cruise Thalassa07/1 to the North Sea
DOI: 10.1594/pangaea.916497
title: 1-Hz PPP displacements at GEONET station 0295 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.691235
title: Nutrient concentrations in water samples collected at Station SEPT-94-GN3619940280300321 in the Aegean Sea
DOI: 10.1594/pangaea.822783
title: Meteorological measurements in the upper air at station Sodankylä, 1920-01-23 to 1935-12-14, ERA-CLIM ID 5517

description: Altitude = Height above sea-level
DOI: 10.1594/pangaea.916489
title: 1-Hz PPP displacements at GEONET station 0286 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.745087
title: Tab. 1+2 Sites and depth of reference level 1963 and mean annual net balance since 1963

description: Measurements of the gross beta activity of firn samples taken from drillings in the region of the North Water polynya allow us to identify deposits of the radioactive Fall-out of 1963, due to a maximum of gross beta activity in a vertical profile. Drillings were made in the lower region of the accumulation area (Percolation Zone). The reference horizon of 1963 in this area is well marked by a concentration of deposits of radioactive fall out. This method of dating still enables us to determine the mean annual net accumulation since 1963.
description: Supplement to: Ambach, Walter; Müller, Fritz (1980): Determination of net accumulations from gross beta activity measurements in the North Water region. Polarforschung, 50(1/2), 1-7
DOI: 10.1594/pangaea.830866
title: (Table S3) Geochemical traces measured before reductive cleaning, ODP Site 208-1263

description: DEPTH, sediment/rock [m] is given in mbsf. Enrichments are calculated as (metal/Ti)sample/(metal/Ti)crust where Mn/Ticrust = 0.156, U/Ticrust = 0.061 (Rudnick and Gao, 2004)
DOI: 10.1594/pangaea.726647
title: Main and trace element composition of rocks from the Mid Atlantic Ridge at MARSUED-IV stations (Inside Corner High)
DOI: 10.1594/pangaea.739958
title: Pollen profile WAXECK, Waxeckalm, Austria

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.691234
title: Nutrient concentrations in water samples collected at Station SEPT-94-GN3619940280300320 in the Aegean Sea
DOI: 10.1594/pangaea.771653
title: Physical oceanography during Walther Herwig III cruise WH233
DOI: 10.1594/pangaea.822192
title: Meteorological measurements in the upper air at station Moscow Dolgoprudnii, 1943-01-01 to 1943-12-31, ERA-CLIM ID 4536
DOI: 10.1594/pangaea.747217
title: Meteorological observations during Admiral Pocock cruise from Mohilla Island to Bombay started at 1762-09-27
DOI: 10.1594/pangaea.497584
title: Physical oceanography from BT during cruise U58GS01869B_1977
DOI: 10.1594/pangaea.587151
title: Physical oceanography at CTD station M1_CTD269 of the Persian Gulf