cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.865253
title: Annotated record of the detailed examination of Mn deposits from DSDP Hole 3-13 and Hole 3-15

description: The preliminary planning and approach to site 13 were taken from the JOIDES Atlantic Advisory Panel Report and from a previous detailed survey of the site by R/V Vema of the Lamont Geological Observatory. Several CSP profiles crossing the selected site in various directions show an uplifted portion of the sea floor roughly circular in shape of about 10 kilometers in diameter. In contrast to the smooth bottom of the surrounding abyssal plain, the topography of the small rise selected for the site has a small-scale roughness of amplitude of 40 to 80 meters. The work reported here is a biostratigraphic summary of available samples. Only the most important and biostratigraphically significant components of the faunas have been noted. No attempt has been made to give an exhaustive faunal analysis of the samples seen.
description: The sediment properties and epoch are extracted from: Maxwell, A.E., et al., (1970) 3. Site 13, In: Maxwell, A.E., et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Government Print Office), p. 27-70, doi:10.2973/dsdp.proc.3.103.1970; and from: Maxwell, E., Von Herzen, R. P., Andrews, J. E., Boyce, R. E., Millow, E. D., Hsu, K. J., Percival, S. and Saito, T., (1970) 5. Site 15, In: Maxwell, A.E., et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Government Print Office), p. 113-152, doi:10.2973/dsdp.proc.3.105.1970.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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.
DOI: 10.1594/pangaea.872185
title: Non-metric multidimensional scaling analyses of ostracode taxa from the Maastrichtian-Thanetian samples at IODP Site 342-U1407
DOI: 10.1594/pangaea.671848
title: Basic measurements of radiation at station Regina (2000-09)
DOI: 10.1594/pangaea.498203
title: Physical oceanography from BT during cruise U74EH00361B_1949
DOI: 10.1594/pangaea.762622
title: Core-section summary for Hole 325-M0039A
DOI: 10.1594/pangaea.859730
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE362
DOI: 10.1594/pangaea.498292
title: Physical oceanography from BT during cruise U901007636B_1984
DOI: 10.1594/pangaea.691153
title: Nutrient concentrations in water samples collected at Station JUNE-94-GN3619940280200360 in the Aegean Sea
DOI: 10.1594/pangaea.755627
title: (Table 1p) Concentrations of particulate protein and organic phosphorus in waters of the East Pacific at Station Agat-3614
DOI: 10.1594/pangaea.762982
title: Tab. 2: Chemical composition of saline lakes in the coastal region
DOI: 10.1594/pangaea.761767
title: Macroalgal communities of gas vents near Ischia island in the Medterranean sea, 2011

description: There are high levels of uncertainty about how coastal ecosystems will be affected by rapid ocean acidification caused by anthropogenic CO2, due to a lack of data. The few experiments to date have been short-term (&lt; 1 year) and reveal mixed responses depending on the species examined and the culture conditions used. It is difficult to carry out long-term manipulations of CO2 levels, therefore areas with naturally high CO2 levels are being used to help understand which species, habitats and processes are resilient to the effects of ocean acidification, and which are adversely affected. Here we describe the effects of increasing CO2 levels on macroalgal communities along a pH gradient caused by volcanic vents.Macroalgal habitat differed at taxonomic and morphological group levels along a pH gradient. The vast majority of the 101 macroalgal species studied were able to grow with only a 5% decrease in species richness as the mean pH fell from 8.1 to 7.8. However, this small fall in species richness was associated with shifts in community structure as the cover of turf algae decreased disproportionately. Calcitic species were significantly reduced in cover and species richness whereas a few non-calcified species became dominant. At mean pH 6.7, where carbonate saturation levels were &lt; 1, calcareous species were absent and there was a 72% fall in species richness. Under these extremely high CO2 conditions a few species dominated the simplified macroalgal assemblage and a very few exhibited enhanced reproduction, although high CO2 levels seemed to inhibit reproduction in others.Our data show that many macroalgal species are tolerant of long-term elevations in CO2 levels but that macroalgal habitats are altered significantly as pH drops, contributing to a scant but growing body of evidence concerning the long-term effects of CO2 emissions in vegetated marine systems. Further study is now needed to investigate whether the observed response of macroalgal communities can be replicated in different seasons and from a range of geographical regions for incorporation into global modelling studies to predict effects of CO2 emissions on Earth's ecosystems.
description: Supplement to: Porzio, Lucia; Buia, Maria-Cristina; Hall-Spencer, Jason M (2011): Effects of ocean acidification on macroalgal communities. Journal of Experimental Marine Biology and Ecology, 400(1-2), 278-287
DOI: 10.1594/pangaea.778102
title: (Table 1) Trace metal content of Pliocene to Pleistocene sediments of ODP Hole 127-794A
DOI: 10.1594/pangaea.872188
title: Annotated record of the detailed examination of Mn deposits in the Atlantic Ocean from cruises from R/V Atlantis, R/V Atlantis II, R/V Chain, R/V Gosnold and R/V Knorr in 1961-1977

description: This report is Volume 1 in the series of reports entitled "Descriptions of W.H.O.I. rock dredge samples". This series represents a major effort to catalog and prepare initial descriptions for all rock dredge samples in the W.H.O.I. Sea Floor Samples Collection, and to distribute this information throughout the scientific community. Volume 1 contains sample descriptions from approximately 382 dredging stations executed during the period 1960 through 1977. It also represents a digitized listing of all dredge station data for the entire W.H.O.I. Dredge Collection through 1980. This data is sorted by Marsden Square and can serve as a regional index for all rock descriptions included in Volumes 1-3.
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.
DOI: 10.1594/pangaea.736132
title: Ozone measurements from station Lindenberg (1998-03)
DOI: 10.1594/pangaea.816916
title: Hydrochemistry measured on water bottle samples during PARIZEAU cruise IOS_91-08
DOI: 10.1594/pangaea.762018
title: Other measurements at 10 m from station Payerne (2004-03)
DOI: 10.1594/pangaea.778103
title: (Table 2) Trace metal content of Pliocene to Pleistocene sediments of ODP Hole 127-795A
DOI: 10.1594/pangaea.762227
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0203

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.923546
title: Hourly electricity generation of Yarwun gas power plant, Australia, 2010 - 2019
DOI: 10.1594/pangaea.548891
title: Nutrients and bacteria measured on water bottle samples at station Chan_2003-01-09_12, Chanavallita, Chile
DOI: 10.1594/pangaea.496746
title: Physical oceanography from BT during cruise K58BOB_1933
DOI: 10.1594/pangaea.762243
title: Counts and mass of different fish species from beam trawl samples in the Eastfrisian Wadden Sea during POLARIS cruise PO0299

description: Depth, water was calculated as mean from bathymetric depths at start/end of trawl
DOI: 10.1594/pangaea.762257
title: Full tide and low tides recorded at gauge station St. Martin

description: Tide gauges were deployed at three stations around the Cap de la Hague. They operated at a depth range of 0?10 m, accurate to 3 cm and with a resolution of 0.3 cm every 15 s. They were deployed from the coast, at depths close to the lowest low water level. A total of 685 tidal cycles were measured; the dates and levels of high and low waters were extracted.
DOI: 10.1594/pangaea.800322
title: Physical oceanography and current meter data from mooring F16-6

description: Gear ID: 1, SN 11892; Gear ID: 2 SBE37, SN 227; Gear ID: 3, SN 311; Gear ID: 4, SN 462; Gear ID: 5, SN 506; Gear ID: 6, SN 509
DOI: 10.1594/pangaea.498137
title: Physical oceanography from BT during cruise U58XX01071B_1946
DOI: 10.1594/pangaea.778077
title: Reflectance spectroscopy and colorimetry from IODP Hole 317-U1351B

description: Geocode = Depth CSF-A (m). Technical Note 26 Chapter 7: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP7.PDF
DOI: 10.1594/pangaea.713603
title: Population density of radiolaria at station UT99-4-2
DOI: 10.1594/pangaea.747941
title: Meteorological observations during CONQUEROR cruise from Lagos Bay to Gibraltar started at 1805-05-12
DOI: 10.1594/pangaea.498420
title: Physical oceanography from BT during cruise U90AZ00435B_1973
DOI: 10.1594/pangaea.755589
title: Meteorological synoptical observations from station Lindenberg (2003-11)
DOI: 10.1594/pangaea.495553
title: Water temperature MBT profiles from cruise U7403038M_1951
DOI: 10.1594/pangaea.917795
title: Other measurements at 10 m from station Southern Great Plains (2019-07)
DOI: 10.1594/pangaea.916975
title: 1-Hz PPP displacements at GEONET station 0795 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.919682
title: Exemplary FOFS output data of experiments on simultaneous recording of filtration and respiration in marine organisms

description: Data sets are outputs of two experiments (each experiment includes two or more temporally replicated trials - named by date) that were conducted using a newly developed Fluorometer and Oximeter equipped Flow-through Setup (FOFS).The corresponding method paper is titled 'Simultaneous recording of filtration and respiration in marine organisms in response to short-term environmental variability'. The paper is under review by Limnology and Oceanography: Methods.The main directory of experimental data (e.g., FOFS_test/blank_trials) contain subdirectories termed raw_data_temperature (including °C-temperature .xlsx files), raw_data_Chl, and raw_data_Oxygen, the two latter contains folders named after the starting dates of the trials (e.g., 04_nov).Each of these folders has three subfolders named after the three stages of the trial (i.e., pre, main, and post). Each subfolder includes data sheets of mV-Chl (.CSV) or %air-saturation (.xlxs, which are outputs of the DO calulator.py) that were collected in the corresponding stage and trial.The data can be processed through the Python scripts accompanying the method paper, providing time-series of filtration, respiration, and scope for growth along daily thermal cycles for the studied blue mussel Mytilus spp. specimens (see the paper for details).
DOI: 10.1594/pangaea.778091
title: (Table 1) Physical properties of ODP Hole 127-794C samples
DOI: 10.1594/pangaea.778094
title: (Table 3) Correction of previously applied stress for the pore-pressure effect, ODP Hole 127-794C samples
DOI: 10.1594/pangaea.499308
title: Physical oceanography from BT during cruise U90XX00308B_1970
DOI: 10.1594/pangaea.711558
title: Radiosonde measurements from station Tamanrasset (2008-12)

description: Start location: Tamanrasset; Distance from radiation site: 10 km
DOI: 10.1594/pangaea.892744
title: Ultra-violet measurements from station Toravere (2018-06)
DOI: 10.1594/pangaea.912660
title: Radiosonde measurements from station Ishigakijima (2019-12)
DOI: 10.1594/pangaea.675367
title: Radiosonde measurements from station Payerne (1996-10)
DOI: 10.1594/pangaea.917743
title: Radiosonde measurements from station Southern Great Plains (2018-06)

description: Launches may be at irregular time intervals. The radiosonde measurements from station Southern Great Plains are used for Billings and E13
DOI: 10.1594/pangaea.750899
title: Meteorological observations during NEPTUNE cruise from Torbay to Basse Terre started at 1808-01-15
DOI: 10.1594/pangaea.734907
title: Meteorological synoptical observations from station Lindenberg (1994-11)
DOI: 10.1594/pangaea.759510
title: Tab. 1: Trace-element concentrations in ore samples collected from mercury mines and deposits in southwestern Alaska

description: A belt of small but numerous mercury deposits extends for about 500 km in the Kuskokwim River region of southwestern Alaska. The southwestern Alaska mercury belt is part of widespread mercury deposits of the circum Pacific region that are similar to other mercury deposits throughout the world because they are epithermal with formation temperatures of about 200 °C, the ore is dominantly cinnabar with Hg-Sb-As±Au geochemistry, and mineralized forms include vein, vein breccias, stockworks, replacements, and disseminations. The southwestern Alaska mercury belt has produced about 1400 t of mercury, which is small on an international scale. However, additional mercury deposits are likely to be discovered because the terrain is topographically low with significant vegetation cover. Anomalous concentrations of gold in cinnabar ore suggest that gold deposits are possible in higher temperature environments below some of the Alaska mercury deposits. We correlate mineralization of the southwestern Alaska mercury deposits with Late Cretaceous and early Tertiary igneous activity. Our 40Ar/39Ar ages of 70 ±3 Ma from hydrothermal sericites in the mercury deposits indicate a temporal association of igneous activity and mineralization. Furthermore, we suggest that our geological ancl geochemical data from the mercury deposits indicate that ore fluids were generated primarily in surrounding sedimentary wall rocks when they were cut by Late Cretaceous and early Tertiary intrusions. In our ore genesis model, igneous activity provided the heat to initiate dehydration reactions and expel fluids from hydrous minerals and formational waters in the surrounding sedimentary wall rocks, causing thermal convection and hydrothermal fluid flow through permeable rocks and along fractures and faults. Our isotopic data from sulfide and alteration minerals of the mercury deposits indicate that ore fluids were derived from multiple sources, with most ore fluids originating from the sedimentary wall rocks.
description: Supplement to: Gray, John E; Gent, Carol A; Snee, Lawrence W (2000): The southwestern Alaska Mercury Belt and its relationship to the circum-Pacific metallogenic mercury province. Polarforschung, 68, 187-196
DOI: 10.1594/pangaea.759656
title: (Table 1) Composition of organic matter from sediments of the triple junction area in the Indian Ocean

description: Bituminous substances in metalliferous sediments from the region of the triple junction in the Indian Ocean were studied. Specific peculiarities of their structure confirming location in "hot conditions" were revealed. Hydrocarbons are genetically connected with hydrothermal matter, and thus they could be considered as a geochemical indicator of hydrothermal processes in the ocean.
description: Supplement to: Chernova, Tatyana G; Pykovskiy, YuI; Ogloblina, A I; Alekseeva, T A (1994): Geochemistry of bituminous substances in the sediment of triple junction ridges of the Indian Ocean. Oceanology, 33(5), 604-607
DOI: 10.1594/pangaea.760076
title: (Fig. 6) Cumulative time per month with temperatures greater than or equal to 17°C, 18°C or 19°C in Las Cruces, central Chile, during 2001 to 2008
DOI: 10.1594/pangaea.618956
title: Water temperature profile LD00-8
DOI: 10.1594/pangaea.761014
title: (Table 1) Distribution of TiO2 in DSDP Leg 22 Holes

description: The TiO2/Al2O3 ratio in the Cenozoic Bengal Abyssal Fan sediments displays decisive potential as a paleostream velocity indicator. The reason for this is that, even in the finest fan suspendates, hydrodynamic sorting determines the amounts of heavy TiO2-rich minerals relative to lighter Al2O3-rich clay minerals.In five Deep Sea Drilling Project cores (213 - 217), which have been recovered in, and south of, the Bay of Bengal, TiO2/Al2O3 ratios increase linearly with time from the Late Miocene to Recent. The increase reflects fan progradation and intensified bottom current activity on the southern Bengal Fan. These processes are related to the Himalayan elevation by factors such as the maturation of northern India river systems, evolution of orographic monsoon rains and elevation-attributed increases in denudation rates.
description: Supplement to: Schmitz, Birger (1987): The TiO2/Al2O3 ratio in the Cenozoic Bengal Abyssal Fan sediments and its use as a paleostream energy indicator. Marine Geology, 76, 195-206
DOI: 10.1594/pangaea.848242
title: Master track of Nathaniel B. Palmer cruise NBP11-03 in 1 min resolution
DOI: 10.1594/pangaea.759572
title: (Table 1) Compositional variation with depth in a nodule of sediment sample RVG-10D

description: A detailed study of a nodule from the Somali Basin dated by 230Thexcess was correlated with the paleoceanographic events recorded in Site 236 (Leg 24) Deep Sea Drilling Project (DSDP) cores. Tentative indications are that the phase of nodule accretion starting with the development of pillar structure at a depth of 20 mm in the nodule around 13 Ma coincides with increased Antarctic Bottom Water (AABW) flow and an elevated calciumcarbonate compensation depth (CCD).The Late Miocene lowering of the CCD is represented by the mottled zones between 8 and 18 mm in the nodule is characterised by an abundant silicate component (&gt;20%) of aeolian origin. The Miocene/Pliocene boundary (5 Ma) occurs at a depth of about 8 mm and is represented by the development of pillar structure and a minimum of aeolian dust (10.3%).The increased biological productivity of the Somali surface water since the Middle Miocene is demonstrated by the increasing Corg content of the nodule (from 0.11 to 0.19%) towards its surface.
description: Zero corresponds to the surface of the nodule. Nucleus residue content is 51.5 %.
description: Supplement to: Banakar, Virupaxa K; Nair, R R; Tarkian, M; Haake, Birgit (1993): Neogene oceanographic variations recorded in manganese nodules from the Somali Basin. Marine Geology, 110(3-4), 393-402
DOI: 10.1594/pangaea.760778
title: (Table 1) Distribution of 210Pb in the surface layer of shelf sediments near the Congo mouth and sedimentation rates

description: A constant concentration model was used in conjunction with the nonequilibrium 210Pb method in determining mean sedimentation rates of bottom sediments sampled during Cruise 20 of R/V Vityaz-II in a test range occurred on the Atlantic shelf near the Congo mouth. 210Pb distribution was analyzed at 16 stations located within a canyon, which is an extension of the Congo channel, and on its shoulders. On the canyon floor at depths 1 km within 12-15 cm sampled sediment monoliths it was possible to detect sediments re-deposited from the canyon walls characterized by high 210Pb concentrations. Sedimentation rates of the surface layer of sediments vary in the range 0.065-0.290 cm/year with the mean value 0.141+/-0.083 cm/year. At most stations the analysis of 210Pb distribution indicates presence of re-deposited matter. Integral activity of 210Pb was used to mark five stations with sediment accumulation regime close to that in the adopted model. Sedimentation rate for these five stations is 0.082+/-0.024 cm/year.
description: Supplement to: Kuptsov, Vladimir M; Sharay, Irina V (1993): Rates of recent accumulation of sediments on shelf of West Equatorial Africa near Congo mouth. Oceanology, 33(3), 353-358
DOI: 10.1594/pangaea.761173
title: Meteorological synoptical observations from station Sede Boqer (2010-10)
DOI: 10.1594/pangaea.826344
title: Moisture and density (MAD) measured on IODP Hole 330-U1377A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.897149
title: Rock magnetic properties of sediment core GeoB18514-2
DOI: 10.1594/pangaea.761174
title: Radiosonde measurements from station Sede Boqer (2010-10)

description: Start location: Bet-Dagan,Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.761177
title: Radiosonde measurements from station Sede Boqer (2010-11)

description: Start location: Bet-Dagan,Israel; Distance from radiation site: 120 km
DOI: 10.1594/pangaea.495254
title: Water temperature MBT profiles from cruise U3190213M_1950
DOI: 10.1594/pangaea.495603
title: Water temperature MBT profiles from cruise U74EH26220M_1950
DOI: 10.1594/pangaea.761283
title: Meteorological synoptical observations from station Lindenberg (2005-09)
DOI: 10.1594/pangaea.672159
title: Radiosonde measurements from station South Pole (1997-09)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.872547
title: (Table 05a) Raw data of magnetic susceptibility (MS) from different holes of IODP Site 342-U1406
DOI: 10.1594/pangaea.663321
title: Oceanography at CTD/bottle station IFREMER_0161
DOI: 10.1594/pangaea.672200
title: Radiosonde measurements from station South Pole (2001-02)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.496366
title: Water temperature MBT profiles from cruise U90X120069M_1983
DOI: 10.1594/pangaea.772383
title: Hydrochemistry measured on water bottle samples during cruise Iceberg1951

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.497844
title: Physical oceanography from BT during cruise U58X001019B_1954
DOI: 10.1594/pangaea.497042
title: Physical oceanography from BT during cruise M90CQ00014B_1986
DOI: 10.1594/pangaea.877464
title: Radiosonde measurements from station Ishigakijima (2017-05)
DOI: 10.1594/pangaea.665382
title: Oceanography at CTD/bottle station IFREMER_2222
DOI: 10.1594/pangaea.664035
title: Oceanography at CTD/bottle station IFREMER_0876
DOI: 10.1594/pangaea.896959
title: Ultra-violet measurements from station Payerne (2016-01)
DOI: 10.1594/pangaea.751681
title: Meteorological observations during RAISONABLE cruise from Montevideo to Table Bay started at 1807-08-02