cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.787107
title: (Table 1) Granulometry, soil pH, carbonate content and color description of soil profiles obtained in Xinghai, Tibet

description: Large parts of the eastern half of the Tibetan Plateau are covered between (3,500) 4,000 and nearly 6,000 m a.s.l. by alpine sedge mats (key species Kobresia pygmea), which attain an extension of ca. 450,000 km**2. It is considered to be the world's largest alpine ecosystem. Moreover, there exist isolated (relic) forests in the same area up to an altitude of 4,700 m a.s.l. mainly consisting of juniper (Juniperus) and spruce (Picea). Large parts of the Kobresia ecosystem are expected to be a grazing-resistant replacement formation, replacing forests and grass-dominated plant communities due to human and/or climatic impact. Recently, a research project was launched to increase knowledge about the properties and genesis of these forests and sedge mats (Present-day dynamics and Holocene landscape history of fragmented forest biocoenoses in Tibet; headed by G. Miehe, Marburg).
description: Supplement to: Kaiser, Knut (2004): Pedogeomorphological transect studies in Tibet: implications for landscape history and present-day dynamics. Prace Geograficzne, 200, 147-165
DOI: 10.1594/pangaea.807449
title: Nutrients measured on water bottle samples during AGHYAR cruise NASEER-1
DOI: 10.1594/pangaea.863930
title: Basic measurements of radiation at station Lerwick (2012-12)
DOI: 10.1594/pangaea.663573
title: Oceanography at CTD/bottle station IFREMER_0413
DOI: 10.1594/pangaea.780181
title: (Table S1) Stable carbon isotope composition of dissolved inorganic carbon and Ion activity product of dolomite of IODP Exp 323 sites

description: We studied microbially mediated diagenetic processes driven by carbon mineralization in subseafloor sediment of the northeastern Bering Sea Slope to a depth of 745 meters below seafloor (mbsf). Sites U1343, U1344 and U1345 were drilled during Integrated Ocean Drilling Program (IODP) Expedition 323 at water depths of 1008 to 3172 m. They are situated in the high productivity “Green Belt” region, with organic carbon burial rates typical of the high-productivity upwelling domains on western continental margins. The three sites show strong geochemical similarities. The downward sequence of microbially mediated processes in the sediment encompasses (1) organoclastic sulfate reduction, (2) anaerobic oxidation of methane (AOM) coupled to sulfate reduction, and (3) methanogenesis. The sediment contains two distinct zones of diagenetic carbonate formation, located at the sulfate–methane transition zone (SMTZ) and between 300 and 400 mbsf. The SMTZ at the three sites is located between 6 and 9 mbsf. The upward methane fluxes into the SMTZ are similar to fluxes in SMTZs underlying high-productivity surface waters off Chile and Namibia. Our Bering Sea results show that intense organic carbon mineralization drives high ammonium and dissolved inorganic carbon (DIC) production rates (&gt; 4.2 mmol/m**3/y1) in the uppermost 10 mbsf and strongly imprints on the stable carbon isotope composition of DIC, driving it to a minimum value of -27 per mil (VPDB) at the SMTZ. Pore-water calcium and magnesium profiles demonstrate formation of diagenetic Mg-rich calcite in the SMTZ. Below the SMTZ, methanogenesis results in 13C-enrichment of pore-water DIC, with a maximum value of +11.9 per mil. The imprint of methanogenesis on the DIC carbon isotope composition is evident down to a depth of 150 mbsf. Below this depth, slow or absent microbially mediated carbon mineralization leaves DIC isotope composition unaffected. Ongoing carbonate formation between 300 and 400 mbsf strongly influences pore-water DIC and magnesium concentration profiles. The linked succession of organic carbon mineralization and carbonate dissolution and precipitation patterns that we observe in the Bering Sea Slope sediment may be representative of passive continental margin settings in high-productivity areas of the world's ocean.
description: Supplement to: Wehrmann, Laura Mariana; Risgaard-Petersen, Nils; Schrum, Heather N; Walsh, Emily A; Huh, Youngsook; Ikehara, Minoru; Pierre, Catherine; d'Hondt, Steven L; Ferdelman, Timothy G; Ravelo, Ana Christina; Takahashi, Kozo; Zarikian, Carlos Alvarez (2011): Coupled organic and inorganic carbon cycling in the deep subseafloor sediment of the northeastern Bering Sea Slope (IODP Exp. 323). Chemical Geology, 284(3-4), 251-261
DOI: 10.1594/pangaea.876912
title: Continuous sediment temperature observations at station BEFmate_I3pio (2014-10)
DOI: 10.1594/pangaea.782631
title: (Table 40) Chemical composition of Fe-Mn nodules from the Romanche Fracture Zone
DOI: 10.1594/pangaea.908425
title: Continuous sediment temperature observations at station BEFmate_S2upp (2017-11)
DOI: 10.1594/pangaea.782660
title: (Table S8) Amphibole-plagioclase thermometry reconstruction for Pito Deep samples
DOI: 10.1594/pangaea.754866
title: Strontium-90 concentration in waters of the eastern Carribbean Sea at Station AV6-SR-2
DOI: 10.1594/pangaea.757448
title: (Table 1) Abundance of bacterioplankton and cyanobacteria in waters of the East Atlantic and Mediterranean Sea

description: Distribution of cyanobacteria as compared with total bacterioplankton was studied in the Mediterranean Sea and off the west coast of Africa in November 1985 - January 1986. Fluorescent microscopy indicated that abund¬ance of chroococcoid cyanobacteria was 2 to 3 orders of magnitude lower than that of non-fluorescent bacteria. Cyanobacteria cells were larger than other bacterial cells and had in average 4 times larger volume. Biomass of cyanobacteria was significant percentage (5-15%) of total bacterioplankton biomass only in the surface interval (0-30 m).
description: Supplement to: Chepurnova, E A; Gutveyb, L G (1988): Distribution and size structure of phototrophic bacterioplankton (cyanobacteria) in the Mediterranean Sea and Atlantic Ocean. Oceanology, 28(5), 643-647
DOI: 10.1594/pangaea.712855
title: (Appendix 1) Chemical concentration in particulate matter measured on water bottle samples at station BP97-17
DOI: 10.1594/pangaea.817271
title: Hydochemistry measured on water bottle samples during TYRO cruise NIOP-D1
DOI: 10.1594/pangaea.778160
title: (Table 1) Grain size composition and heavy metal speciations in bottom sediments of the Ussuri Bay, Sea of Japan

description: Changes in concentration levels and speciation of heavy metals during sedimentation on example of a typical semi-closed bay, where bottom sediments have formed due to river run-off, are under consideration. It is shown that due to desorption of mobile manganese, zinc and copper entered the bay with river suspended matter, their total contents in bottom sediments decrease and percentages of lithogenic forms increase. Contents and speciation of iron in bottom sediments are determined by its participation in coagulation of river colloids in the mixing zone and by mechanical differentiation of sedimentary material.
description: Supplement to: Shul'kin, Vladimir M; Bogdanova, Natalia N (1984): Geochemistry of iron, manganese, zinc, and copper in nearshore sedimentation (on example of the Ussuri Bay). Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 19(6), 105-117
DOI: 10.1594/pangaea.763747
title: (Table 1) Chemical composition of basalts from boards of the Hess Deep
DOI: 10.1594/pangaea.780140
title: Biogeochemical analysis in sediments of the Var turbidity system from ENVAR6_MTB_33

description: The data set describes biogeochemical composition of sediment samples from the Var turbidite system.
DOI: 10.1594/pangaea.848495
title: Abundance and biomass of gelatinous plankton in the Black Sea in April 1993
DOI: 10.1594/pangaea.777783
title: (Table 1) Sulfur speciation in bottom sediments of the Pacific Ocean to the east of Japan
DOI: 10.1594/pangaea.857311
title: Colored dissolved organic matter (cDOM) absorption measurements during Yamal-Arctic Expedition in 2014
DOI: 10.1594/pangaea.698991
title: Abundance of ichthyoplankton during HEINCKE cruise HE211/1

description: Mesh size: 500 µm; ship speed: 3 kn; heave speed: 0.5 m/sec; fier speed: 0.7 m/sec
DOI: 10.1594/pangaea.733147
title: Physical oceanography during Kaimalino cruise HOT-10 on section PRS2
DOI: 10.1594/pangaea.733169
title: Physical oceanography during Alpha Helix cruise HOT-27 on section PRS2
DOI: 10.1594/pangaea.927037
title: Comparison of disaggregation techniques for indurated carbonates
DOI: 10.1594/pangaea.723254
title: Description of profile 7139-202
DOI: 10.1594/pangaea.477360
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/96-1

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.759198
title: Physical oceanography during LANCE cruise LA98/4
DOI: 10.1594/pangaea.778714
title: (Table 3) Stable oxygen and carbon isotopes and carbon composition of four Leg 194 site survey gravity cores

description: Smear slides were examined visually with a microscope at 1000x magnification.
DOI: 10.1594/pangaea.842625
title: Linescanner images of sediment core PG2127-1

description: RGB and Lab raw data: http://hs.pangaea.de/Raw/PG/Yakutia2013/PG2127-1_color.zip
DOI: 10.1594/pangaea.788833
title: Basic measurements of radiation at station Cener (2012-07)
DOI: 10.1594/pangaea.782628
title: (Table 34-2) Chemical composition of metamorphic minerals from metabasites of the Romanche and Vernadsky Fracture Zones, Atlantic Ocean
DOI: 10.1594/pangaea.788790
title: (Table 2) Age, biostratigraphic and paleomagnetic events at DSDP Site 94-606
DOI: 10.1594/pangaea.713600
title: Population density of radiolaria at station UT99-22-1
DOI: 10.1594/pangaea.784881
title: Physical oceanography during Le Noroit curise ECOMARGE3
DOI: 10.1594/pangaea.788794
title: (Table 6) Age, biostratigraphic and paleomagnetic events at DSDP Site 94-610
DOI: 10.1594/pangaea.788889
title: (Table T1) Major element oxides and carbonate composition of calcite from ODP Leg 168 sites

description: All concentrations given with a 'less than' sign are below detection limit.
DOI: 10.1594/pangaea.763770
title: (Table 2b) Percentages of adsorbed chemical elements of their total contents in suspended matter from the near-bottom waters of the Ob River estuary (Obskaya Guba) and Kara Sea in September 2007
DOI: 10.1594/pangaea.774545
title: Physical oceanography from mooring TR_Micro4 at Tisler Cold-Water Coral Reef, Norway
DOI: 10.1594/pangaea.896080
title: Microbiota 16s rRNA genotyping in S. typhle eggs and broodpouch

description: While originally acquired from the environment, a fraction of the microbiota is transferred from parents to offspring. The immune system shapes the microbial colonization, while commensal microbes may boost host immune defences. Parental transfer of microbes in viviparous animals remains ambiguous, as the two transfer routes (transovarial vs. pregnancy) are intermingled within the maternal body. Pipefishes and seahorses (Syngnathids) are ideally suited to disentangle transovarial microbial transfer from a contribution during pregnancy due to their maternal egg production and their unique male pregnancy.We assessed the persistency and the changes in the microbial communities of the maternal and paternal reproductive tracts over proceeding male pregnancy by sequencing microbial 16S rRNA genes of swabs from maternal gonads and brood pouches of non-pregnant and pregnant fathers. Applying parental immunological activation with heat-killed bacteria, we evaluated the impact of parental immunological status on microbial development. Our data indicate that maternal gonads and paternal brood pouches harbor distinct microbial communities, which could affect embryonal development in a sex-specific manner. Upon activation of the immune system, a shift of the microbial community was observed. The activation of the immune system induced the expansion of microbiota richness during late pregnancy, which corresponds to the time point of larval mouth opening, when initial microbial colonization must take place.
description: Supplement to: Beemelmanns, Anne; Poirier, Maude; Bayer, Till; Künzel, Sven; Roth, Olivia (2019): Microbial embryonal colonization during pipefish male pregnancy. Scientific Reports, 9(1)
DOI: 10.1594/pangaea.772475
title: Hydrochemistry measured on water bottle samples during cruise SEVER04

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.762672
title: (Table 6) Salinity in the River Kem' estuary during the ebb tide on 30 July 2003
DOI: 10.1594/pangaea.868254
title: XRF counts of potassium and iron in composite core ICDP5045-1 (386 sections) and Co1261 (2 sections) at Lake Ohrid (Macedonia, Albania) down to 247 meter sediment depth
DOI: 10.1594/pangaea.816905
title: Physical oceanography during John P. Tully cruise IOS_94-01
DOI: 10.1594/pangaea.887467
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2005404
DOI: 10.1594/pangaea.771062
title: (Table 6) Measurements of valves of Calyptogena valdiviae

description: Vesicomya valdiviae: ZMB 101.598a (lectotype, 2 valves of the same specimen, selected by Boss (1970)); ZMB 101.598b (paralectotypes, 31 valves, same locality); ZMB 101.599 (paralectotypes, 6 valves).
DOI: 10.1594/pangaea.876198
title: Station list and links to master tracks in different resolutions of HEINCKE cruise HE476, Bremerhaven - Bremerhaven, 2017-02-09 - 2017-02-12
DOI: 10.1594/pangaea.825643
title: Physical oceanography during Hespérides cruise Fruela95
DOI: 10.1594/pangaea.749049
title: Meteorological observations during El Patagon cruise from Montevideo to La Coruña started at 1775-11-18
DOI: 10.1594/pangaea.772575
title: Hydrochemistry measured on water bottle samples during cruise WOD98_18_11445

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.778780
title: Core-section summary from IODP Hole 317-U1354B
DOI: 10.1594/pangaea.771502
title: Physical oceanography during Walther Herwig II cruise WH077A
DOI: 10.1594/pangaea.882592
title: Links to master tracks in different resolutions of HEINCKE cruise HE496/1, Bremerhaven - Bremerhaven, 2017-09-22 - 2017-09-24
DOI: 10.1594/pangaea.762037
title: (Table 1) Major and trace elements analyses from FAMOUS-Project and DSDP Site 54-424

description: Hydrothermal deposits "sensu stricto" have been recovered during the FAMOUS cruise and Leg 54 of the Deep Sea Drilling Project near the Galapagos Spreading Centre. The studied sediments, mainly composed of clay material, have very poor REE concentrations, below about ten ppm. The shale-normalized patterns are characterized by a significant enrichment in heavy rare earths and show a negative Ce anomaly. The magnitude of this anomaly fluctuates but is generally lower than the seawater Ce anomaly. The geochemical characteristics of these hydrothermal deposits are in contrast with those of metalliferous sediments which are more enriched in trace elements, especially in REE.
description: Surface data from FAMOUS-Project (Heirtzler, J.R. and Van Andel, T.H., 1977, doi:10.1130/0016-7606(1977)88&lt;481:PFIOPA&gt;2.0.CO;2), geographical position estimated from map.
description: Supplement to: Bonnot-Courtois, Chantal (1981): Distribution des terres rares dans les depots hydrothermaux de la zone FAMOUS et des galapagos-Comparaison avec les sediments metalliferes. Marine Geology, 39(1-2), 1-14
DOI: 10.1594/pangaea.778762
title: Gas measurements from IODP Hole 317-U1354A

description: Geocode = Top depth CSF-A (m).Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30: http://www-odp.tamu.edu/publications/tnotes/tn30/TNOTE_30.PDF
DOI: 10.1594/pangaea.816319
title: (Table 1) Characteristics of DSDP Site 69-504 late Miocene siliceous rocks and associated rocks
DOI: 10.1594/pangaea.759172
title: Physical oceanography during G. O. Sars cruise GS98/5
DOI: 10.1594/pangaea.788525
title: Ozone measurements from station Izaña (2012-08)
DOI: 10.1594/pangaea.858772
title: (Table 4, Page 98) Chemical composition of iron-manganese concretions from the Pacific Ocean recovered by the R/V Vityaz (Analyses carried out in the Exogene Section of the I. G. Ye. M., Academy of Sciences, U.S.S.R.)

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.676890
title: Ages and types of rocks from Hole Northern-1 drilled in the Alexander Island, Franz Josef Land Archipelago
DOI: 10.1594/pangaea.908400
title: Continuous sediment temperature observations at station BEFmate_S3low (2017-07)
DOI: 10.1594/pangaea.746954
title: Meteorological observations during La Gironde cruise from Rochefort to Baie de Chibouctou-Rochefort started at 1746-06-20
DOI: 10.1594/pangaea.887604
title: ADCP current measurements (150 kHz) during Fridtjof Nansen cruise FN2008404
DOI: 10.1594/pangaea.759858
title: Contencentrations of reduced inorganic sulfur forms in Mediterranean Sea waters

description: The first data on content of inorganic reduced sulfur compounds [H2S, S°, S2O3(2-), SO3(2-)] were obtained at two stations in the northeastern Levant Sea (Mediterranean Basin). With lower detection limit for the mentioned sulfur forms of 30 nM, sulfide forms were not found, while thiosulfate concentration varied from 178 to 890 nM (from 24 to 78 % of total reduced S), and S° varied from 156 to 1090 nM. Vertical distribution of these compounds showed irregular character; correlation between total reduced S maxima, fluorescence, and increase of nutrient element content near the lower pycnocline boundary was observed. The maximum total sulfur concentration in the surface layer was likely due an anthropogenic influence. The ''starting'' mechanism that controls appearance and distribution of sulfur compounds in oxygen-containing water is the process of bacterial sulfate reduction in micropatches of fresh organic detritus. Reduced sulfur forms participate further in a series of chemical and biochemical processes. Contribution of hydrolysis of organic sulfur-containing compounds is insignificant for the region in study.
description: 0 = not detected.
description: Supplement to: Neretin, Lev N; Zhabina, Nina N; Demidova, Tatyana P (1996): The content of inorganic reduced sulfur forms in the water of the Mediterranean Sea. Translated from Okeanologiya, 1996, 36(1), 61-65, Oceanology, 36(1), 54-58
DOI: 10.1594/pangaea.744347
title: Physical oceanography during Scotia cruise Scotia96/1 to the North Sea
DOI: 10.1594/pangaea.788697
title: (Table T4) Composition of sulfide minerals from ODP Hole 169-1035H, ODP Mound
DOI: 10.1594/pangaea.772608
title: Tab. A8: Biomasse, Produktions- und Eliminationsberechnungen Macoma balthica &gt;500µm
DOI: 10.1594/pangaea.778543
title: Magnetic remanence on section halves of cores from IODP Hole 317-U1352D

description: Geocode = Depth CSF-A (m).Handbook for Shipboard Paleomagnetists; Technical Note 34: http://www-odp.tamu.edu/publications/tnotes/tn34/TNOTE_34.PDF
DOI: 10.1594/pangaea.788623
title: (Table A1) Taxonomic identification of IODP Hole 325-M0058A
DOI: 10.1594/pangaea.763751
title: (Table 1) Main parameters of consumption of inorganic nitrogen compounds by microplankton in the western Black Sea in April 1993

description: Parameters of provision of the phytoplankton community with inorganic nitrogen compounds in the western Black Sea in April 1993 are analyzed (specifically, dependence of rates of uptake of nitrates and ammonium by microplankton on substrate concentration, diurnal dynamics of assimilation of mineral nitrogen, values of f-ratios, and proportions of carbon and nitrogen fluxes). In most cases all the parameters of degree of phytoplankton provision with mineral nitrogen are shown to vary unidirectionally, both at the surface and in the photosynthesis zone. Individual areas of a relatively small region studied differed markedly in their level of provision of algae with inorganic nitrogen compounds - from complete saturation to high degree of limitation of phytoplankton development due to nitrogen deficiency in the environment. Obtained results allow to estimate provision of Black Sea phytoplankton with nitrogen in terms of limitation of rates of uptake of its inorganic compounds.
description: Supplement to: Krivenko, O V; Stel'makh, Lyudmila V (2003): The provision of the phytoplankton community with inorganic nitrogen compounds in the Black Sea during the spring period. Tranlated from Okeanologiya, 2003, 43(6), 862-870, Oceanology, 43(6), 811-819
DOI: 10.1594/pangaea.772564
title: Hydrochemistry measured on water bottle samples during cruise TUGMS1985

description: No original source is given by the authors of the atlas.
DOI: 10.1594/pangaea.843120
title: Dominate algeas and rare animals of Point Lookout Dive Sites, North Stradbroke Island, Queensland

description: Empty cells indicates "none recorded".
DOI: 10.1594/pangaea.908356
title: Continuous sediment temperature observations at station BEFmate_I3Pio (2017-11)
DOI: 10.1594/pangaea.778221
title: Core-section summary from IODP Hole 317-U1352B