cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.863983
title: Annotated record of the detailed examination of ferromanganese concretions from the Bothnia Gulf, the Baltic Sea and the Barents sea collected by Boström, K. and Ingri, J. (Technical University of Lulea)

description: The collection of ferromanganese nodules at Naturhistoriska Riksmuseet, Stockholm, Sweden has been donated by Pr. Boström, K. and Ingri, J. from the Technical University of Lulea. They have been collected in the Bothnia Gulf, the Baltic Sea anfd the Barents sea from 1976 until 1985. In 1997 it is was put to the care custody of the Laboratory for Isotope Geology (LIG) of NRM. As part of the Access Project at LIG, Curt Boman has gone through the collection and established a database with detailed information about the samples it contains. Ferromanganese nodules typically display a rounded shape and are formed by redox processes at the interface between the seabed sediment and water. In addition to iron and manganese they also contain other metal elements. Nodules chemical composition reflects the substances found in the sediment to which they are associated. Since the nodules grow continuously, they reflect changes in the sedimentary environment chemistry on a yearly basis, which makes them very interesting as environmental archives. The nodules can be found locally in large quantities and due to their metal content they are also economically interesting as a source of raw materials.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Boman, Curt (1997): The iron and manganese collection of the Swedish Museum of Natural History, Stockholm. Naturhistoriska Riksmuseet - NRM
DOI: 10.1594/pangaea.864214
title: Radiosonde measurements from station Tateno (2016-05)
DOI: 10.1594/pangaea.863996
title: Other measurements at 10 m from station Goodwin Creek (2010-04)
DOI: 10.1594/pangaea.864277
title: Other measurements at 10 m from station Rock Springs (2010-04)
DOI: 10.1594/pangaea.863897
title: Ultra-violet measurements from station Fort Peck (2010-10)

description: 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 2017-02-03.
DOI: 10.1594/pangaea.863838
title: Compressive-strength tests of Corvio Sandstone
DOI: 10.1594/pangaea.864258
title: Other measurements at 10 m from station Goodwin Creek (2010-02)
DOI: 10.1594/pangaea.863898
title: Other measurements at 10 m from station Fort Peck (2010-10)
DOI: 10.1594/pangaea.863853
title: Anisotropy-Y direction of Corvio Sandstone, sample Y4
DOI: 10.1594/pangaea.863854
title: Anisotropy-Z direction of Corvio Sandstone, sample Z3
DOI: 10.1594/pangaea.864491
title: Other measurements at 10 m from station Desert Rock (2011-11)
DOI: 10.1594/pangaea.864222
title: Ultra-violet measurements from station Carpentras (2016-07)

description: 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.864107
title: (Table EA3) Concentrations of n-alcohols, average chain lengths, and carbon preference indices in a 34-month time series of suspended sediments from the outflow of the Congo River

description: n-alcohol concentration (µg/gOC), mean values.
DOI: 10.1594/pangaea.860619
title: 1. Scale average variance of dune class small dunes (1-5 m) from Knudedyb, Danish Wadden Sea
DOI: 10.1594/pangaea.863904
title: Other measurements at 10 m from station Fort Peck (2010-12)
DOI: 10.1594/pangaea.864224
title: Meteorological synoptical observations from station Tateno (2016-06)
DOI: 10.1594/pangaea.864513
title: Ultra-violet measurements from station Fort Peck (2011-01)

description: 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 2017-02-03.
DOI: 10.1594/pangaea.860668
title: 2. Scale average variance of dune class medium dunes (5-10 m) from Knudedyb, Danish Wadden Sea
DOI: 10.1594/pangaea.864293
title: Other measurements at 10 m from station Rock Springs (2010-09)
DOI: 10.1594/pangaea.864200
title: Met Office Rain Radar Data from the NIMROD System, NCAS British Atmospheric Data Centre
DOI: 10.1594/pangaea.863924
title: Landscape status of the Ousteri Wetland, Puducherry, India

description: Ousteri Lake is popularly called Ousteri which is a word formed out of the fusion of Tamil words Oussudu (a proper noun) and eri (meaning a lake). Ousteri is an inter-state lake about 50 percent of its waterspread lies in Puducherry and the rest in Tamil Nadu of India. The landscape survey of the entire Ousteri Lake has been collected and reported in the article. Additionally provides feedback from all category of stakeholders to identify whether the Ousteri lake is worth to be recognised under Ramsar Convention or not.
DOI: 10.1594/pangaea.864184
title: Ultra-violet measurements from station Sioux Falls (2010-08)

description: 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 2017-02-03.
DOI: 10.1594/pangaea.864373
title: Ultra-violet measurements from station Toravere (2016-08)

description: 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 2017-01-17. UVB is measured with Kipp&Zonen CUVB1 narrowband radiometer (bandwidth 306 ± 0.1 nm)
DOI: 10.1594/pangaea.863953
title: Mg/Ca ratios of Cibicidoides robertsonianus and BWT reconstruction of DSDP Hole 80-548
DOI: 10.1594/pangaea.863863
title: (Table 3) Palynology data from Seam 1 and assosciated interbeds of Schöningen

description: Oldest samples at base. Palynomorph data = relative to total palynomorph assemblage (Inglis et al., unpublished).
DOI: 10.1594/pangaea.864049
title: (Tables 4-5, page 160) REE contents in ferromanganese concretions from the Gulf of Bothnia and the Barents Sea

description: Ferromanganese concretions from the Svalbard shelf in the Barents Sea show slightly convex shale-normalized REE patterns with no Eu anomalies. Concretions from the Gulf of Bothnia, northern part of the Baltic Sea, exhibit an enrichment of light REE and negative Eu anomalies. This difference is interpreted as a consequence of different conveyor mechanisms of the REE to the sediment. It is suggested that dissolving biogenic debris contributes to the convex pattern obtained in the Barents Sea, whereas an inorganic suspended fraction with scavenged REE is the main carrier in the Gulf of Bothnia. During oxic diagenesis in the sediment, the scavenged REE are set free into the porewater and contribute to the distribution pattern in concretions found in the Gulf of Bothnia. Small Mn-rich spheroidal concretions are enriched two to five times in REE compared to average shale, whereas Mn-poor flat concretions are low in REE. Specific surface area of the concretion and the depth of burial in the oxidized surface sediment are two factors that strongly affect the enrichment of the REE. Weak Ce anomalies are present in the analysed concretions and a redox level dependence is seen.
description: All concentrations (except Insoluble residue [%]) are expressed as fraction of the soluble part of dried and ground samples in an HF-HClO4 solution.From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Ingri, J; Ponter, C (1987): Rare earth abundance patterns in ferromanganese concretions from the Gulf of Bothnia and the Barents Sea. Geochimica et Cosmochimica Acta, 51(1), 155-161
DOI: 10.1594/pangaea.864432
title: Other measurements at 10 m from station Boulder, SURFRAD (2011-12)
DOI: 10.1594/pangaea.863913
title: Hourly discharge of the San Francisco River at station ECPL (Planta), in 2007-2008

description: Please note, that in this remote and environment the hourly discharge measurement is subject to a high uncertainty. We therefore recommend to use daily averages of this dataset. Also note, that in Bücker et al. (2010), the discharge was calculated slightly differently which leads to a slight shift in daily discharge data in 2007.This work was funded by the Deutsche Forschungsgemeinschaft DFG in the frame of the project FOR816 "Biodiversity and Sustainable Management of a Megadiverse Mountain Ecosystem in South Ecuador".This station is called R2 in the connected article.
DOI: 10.1594/pangaea.864464
title: Other measurements at 10 m from station Desert Rock (2011-03)
DOI: 10.1594/pangaea.864187
title: Ultra-violet measurements from station Sioux Falls (2010-09)

description: 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 2017-02-03.
DOI: 10.1594/pangaea.864102
title: Distal shield length, coccosphere diameter and number of coccoliths per coccosphere of Emiliania huxleyi in the South China Sea, 2014
DOI: 10.1594/pangaea.863956
title: Mg/Ca ratios of Cibicidoides wuellerstorfi and BWT reconstruction of DSDP Hole 80-548
DOI: 10.1594/pangaea.864103
title: Coccolithophore abundance in the South China Sea, 2014
DOI: 10.1594/pangaea.864191
title: Other measurements at 10 m from station Sioux Falls (2010-10)
DOI: 10.1594/pangaea.863839
title: Acoustic wave tests of Corvio Sandstone
DOI: 10.1594/pangaea.864153
title: Compilation of bigeye tuna (Thunnus obesus) fork length frequencies in 2 centimeter intervals from catches in the Indian Ocean over 1952-2014
DOI: 10.1594/pangaea.863841
title: BET Specific surface of Corvio Sandstone
DOI: 10.1594/pangaea.864196
title: Ultra-violet measurements from station Sioux Falls (2010-12)

description: 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 2017-02-03.
DOI: 10.1594/pangaea.864159
title: Knickpoint migration between 2007-14 following the channel diversion of Glaisdale Beck
DOI: 10.1594/pangaea.864264
title: Other measurements at 10 m from station Rock Springs (2010-01)
DOI: 10.1594/pangaea.864267
title: Other measurements at 10 m from station Rock Springs (2010-02)
DOI: 10.1594/pangaea.864198
title: River discharge and suspended sediment concentrations measured at Glasdale Beck (2007-09)
DOI: 10.1594/pangaea.864091
title: (Table EA1) Environmental parameters of the Congo River recorded near Brazzaville/Kinshasa during the sampling period from November 2010 to August 2013
DOI: 10.1594/pangaea.864450
title: Magnetic susceptibility dataset from the Danian Contessa Highway section, Gubbio, Italy

description: We studied a high-resolution multiproxy data set, including magnetic susceptibility (MS), CaCO3 content, and stable isotopes (d18O and d13C), from the stratigraphic interval covering the uppermost Maastrichtian and the lower Danian, represented by the pelagic limestones of the Scaglia Rossa Formation continuously exposed in the classic sections of the Bottaccione Gorge and the Contessa Highway near Gubbio, Italy. Variations in all the proxy series are periodic and reflect astronomically forced climate changes (i.e., Milankovitch cycles). In particular, the MS proxy reflects variations in the terrigenous dust input in this pelagic, deep-marine environment. We speculate that the dust is mainly eolian in origin and that the availability and transport of dust are influenced by variations in the vegetation cover on the Maastrichtian-Paleocene African or Asian zone, which were respectively located at tropical to subtropical latitudes to the south or far to the east of the western Tethyan Umbria-Marche Basin, and were characterized by monsoonal circulation. The dynamics of monsoonal circulation are known to be strongly dependent on precession-driven and obliquity-driven changes in insolation. We propose that a threshold mechanism in the vegetation coverage may explain eccentricity-related periodicities in the terrigenous eolian dust input. Other mechanisms, both oceanic and terrestrial, that depend on the precession amplitude modulated by eccentricity, can be evoked together with the variation of dust influx in the western Tethys to explain the detected eccentricity periodicity in the d13C record. Our interpretations of the d18O and MS records suggest a warming event ~400 k.y. prior to the Cretaceous-Paleogene (K-Pg) boundary, and a period of climatic and environmental instability in the earliest Danian. Based on these multiproxy phase relationships, we propose an astronomical tuning for these sections; this leads us to an estimate of the timing and duration of several late Maastrichtian and Danian biostratigraphic and magnetostratigraphic events.
description: Supplement to: Sinnesael, Matthias; De Vleeschouwer, David; Coccioni, Rodolfo; Claeys, Philippe; Frontalini, Fabrizio; Jovane, Luigi; Savian, Jairo Francisco; Montanari, Alessandro (2016): High-resolution multiproxy cyclostratigraphic analysis of environmental and climatic events across the Cretaceous-Paleogene boundary in the classic pelagic succession of Gubbio (Italy). In: Menichetti, M., Coccioni, R., and Montanari, A. (eds.): The Stratigraphic Record of Gubbio: Integrated Stratigraphy of the Late Cretaceous-Paleogene Umbria-Marche Pelagic Basin, Geological Society of America Special Papers, 524, Geological Society of America, 115-137
DOI: 10.1594/pangaea.864661
title: Ultra-violet measurements from station Goodwin Creek (2011-04)

description: 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 2017-02-03.
DOI: 10.1594/pangaea.863851
title: Anisotropy-X direction of Corvio Sandstone, sample X5
DOI: 10.1594/pangaea.864062
title: Mineral distribution of sediment core MD99-2256
DOI: 10.1594/pangaea.864063
title: Benthic and planktonic foraminifera abundances of sediment core MD99-2256
DOI: 10.1594/pangaea.864052
title: Carbonate content of sediment core MD99-2236
DOI: 10.1594/pangaea.864321
title: Fresh biomass of macroalgae collected at Hansneset, Kongsfjorden, Spitsbergen in 1996/1998

description: We surveyed macroalgae at Hansneset, Blomstrand in Kongsfjorden, Svalbard, down to 30 m depth between 1996 and 1998. In total, 62 species were identified: 16 Chlorophyta, 25 Phaeophyceae, and 21 Rhodophyta. The majority of species (53.5%) belonged to the Arctic cold-temperate group, followed in frequency by species distributed from the Arctic to the warm-temperate region (25.9%). Four endemic Arctic species (Laminaria solidungula, Acrosiphonia flagellata, A. incurva, and Urospora elongata) were found. Two species (Pogotrichum filiforme and Mikrosyphar polysiphoniae) were new to Svalbard. Chlorophyta, Phaeophyceae, and Rhodophyta extended from the eulittoral zone down to 11, 21, and &gt;30 m depths with maximum biomasses at 1-5 m, 5-10 m, and 5-30 m depths, respectively. Annual and pseudoperennial species had highest biomasses in the upper 5 m, while perennials were distributed deeper. The highest biomass (8600 g/m**2 wet weight) at 5 m depth comprised mainly L. digitata, Saccorhiza dermatodea, Alaria esculenta, and Saccharina latissima. The biogeographic composition of macroalgae at Hansneset was rather similar to that of northeastern Greenland, but different from that of northern Norway, which has a higher proportion of temperate species. Climate warming and ship traffic may extend some of the distribution ranges of macroalgae from mainland Norway to Svalbard.
description: replicate a: transect taken by Barbara Voegele: Late May-mid July 1996replicate b,c: transect taken by Haakon Hop: 26 August to 10 September 1996 and 14 August to 10 September 1998
description: Supplement to: Hop, Haakon; Wiencke, Christian; Vögele, Barbara; Kovaltchouk, Nikolaj A (2012): Species composition, zonation, and biomass of marine benthic macroalgae in Kongsfjorden, Svalbard. Botanica Marina, 55(4), 399-414
DOI: 10.1594/pangaea.864037
title: Survival of Perna viridis during a 91 day exposure experiment to microplastics in Bogor, Indonesia, 2014
DOI: 10.1594/pangaea.864053
title: IRD content of sediment core MD99-2236
DOI: 10.1594/pangaea.863857
title: Anisotropy-Z direction of Corvio Sandstone, sample Z5
DOI: 10.1594/pangaea.864054
title: Size fraction distribution of sediment core MD99-2236
DOI: 10.1594/pangaea.864060
title: Planktonic foraminifera distribution of sediment core MD99-2256
DOI: 10.1594/pangaea.864221
title: Basic measurements of radiation at station Carpentras (2016-07)
DOI: 10.1594/pangaea.863971
title: Standardized geo-referenced catch and fishing effort data of the bigeye tuna (T. obesus) fisheries in the Indian Ocean over 1952-2014

description: Units of effort and catch are different for each fishery. For instance, the effort and catch of fishery 1,2,3 and 4 are expressed in number of hooks and number of individual tuna, respectively. The fishery 5 and 6 have number of hooks (effort) and tonnes (catch). For the purse seine fisheries, all the catch are expressed in tonnes, but the effort unit can be different for each fishery. To obtain catch and effort unit for each fishery, users are recommended to see the article for details.PLEASE NOTE, that this dataset was updated on 2016-12-21. An additional column was added: T. obesus, mass in tons. Also, a few numbers were corrected. Please contact the PI for details.
DOI: 10.1594/pangaea.864160
title: Longitudinal change in thalweg elevation between 2009-14 in response to the channel diversion of Glaisdale Beck
DOI: 10.1594/pangaea.864572
title: Basic measurements of radiation at station Sapporo (2016-07)
DOI: 10.1594/pangaea.864055
title: Color measurement on sediment core MD99-2236
DOI: 10.1594/pangaea.864211
title: 2003 Habitat Maps derived from Grey Nurse Shark (GNS) Project of Wolf Rock, Double Island Point, Queensland, Australia

description: Surveying habitats critical to the survival of grey nurse sharks in South-East Queensland has mapped critical habitats, gathered species inventories and developed protocols for ecological monitoring of critical habitats in southern Queensland. This information has assisted stakeholders with habitat definition and effective management. In 2002 members of UniDive applied successfully for World Wide Fund for Nature, Threatened Species Network funds to map the critical Grey Nurse Shark Habitats in south east Queensland.UniDive members used the funding to survey, from the boats of local dive operators, Wolf Rock at Double Island Point, Gotham, Cherub's Cave, Henderson's Rock and China Wall at North Moreton and Flat Rock at Point Look Out during 2002 and 2003. These sites are situated along the south east Queensland coast and are known to be key Grey Nurse Shark aggregation sites.During the project UniDive members were trained in mapping and survey techniques that include identification of fish, invertebrates and substrate types. Training was conducted by experts from the University of Queensland (Centre of Marine Studies, Biophysical Remote Sensing) and the Queensland Parks and Wildlife Service who are also UniDive members. The monitoring methods (see methods) are based upon results of the UniDive Coastcare project from 2002, the international established Reef Check program and research conducted by Biophysical Remote Sensing and the Centre of Marine Studies.Habitats were mapped using a combination of towed GPS photo transects, aerial photography, bathymetry surveys and expert knowledge. This data provides georeferenced information regarding the major features of each of Sites mapped including Wolf Rock
DOI: 10.1594/pangaea.864199
title: River levels for the River Esk at Lealholm (1998 - 2016)
DOI: 10.1594/pangaea.864549
title: Annotated record of the detailed examination of Mn deposits in the Atlantic Ocean from cruises from R/V Atlantis II, R/V Knorr, R/V Melvin and R/V James M. Gilliss in 1980-1981

description: This report is Volume 3 of Descriptions of WHOI rock dredge samples. This series represents a major effort to catalog the rock dredge samples in the WHOI Sea Floor samples collection, and to disseminate this information throughout the scientific community. Volume 3 contains sample descriptions and station data for the dredge stations from five cruises during the period September 1978 through December 1980. The material in this and subsequent volumes of rock descriptions was largely prepared onboard ship by the participating scientists. Volume 3 was printed prior to volumes 1 and 2 because of the excellent documentation of the samples represented in this volume.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: Farmer, H G; Dick, H (1981): Descriptions of WHOI rock dredge samples: volume 3. Woods Hole Oceanographic Institution, No. WHOI-81-48, 81-48, 324 pp
DOI: 10.1594/pangaea.864671
title: PanCount - an Excel-sheet to use the keyboard as a counting device
DOI: 10.1594/pangaea.864095
title: Moored current and temperature measurements in the Faroe Bank Channel overflow region at mooring site C1, June 2012-June 2013

description: The temperature measurements were made by accurate temperature sensors on Sea-Bird Electronics SBE39 and SBE56, and SBE37 instruments, as well as by the temperature sensors on current meters. Current measurements were made by Anderaa current meters (RCM7/8), a Nortek current meter (Aquadopp), and various ADCPs (RD-Instruments 75/150/300 kHz Workhorse, Anderaa 600 kHz RDCP, and Nortek Continental). Instrumentation and other details of the moorings can be found in Ullgren et al. (2016). The sampling rate was 15 s for SBE56s, 5 min for SBE37s and SBE39s, 5-60 min for ADCPs, 1 h for RCMs, and 20 min for the Aquadopp. Time series of the vertical position and tilt of the instruments were calculated using hourly mean measured currents, and the Mooring Design and Dynamics software (Dewey, 1999). Hourly velocity and temperature records at corrected depths were then linearly interpolated to 1 m vertical resolution. The data for this data set is extracted at 5-m vertical separation without loss of vertical resolution (the smallest vertical bin separation of the ADCPs 4 m).