cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.867994
title: Basic and other measurements of radiation at station Tiksi (2012-11)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868081
title: Basic and other measurements of radiation at station Tiksi (2013-07)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868082
title: Basic and other measurements of radiation at station Tiksi (2013-08)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.867987
title: Basic and other measurements of radiation at station Tiksi (2012-05)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868076
title: Basic and other measurements of radiation at station Tiksi (2013-02)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.867983
title: Basic and other measurements of radiation at station Tiksi (2012-01)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.867995
title: Basic and other measurements of radiation at station Tiksi (2012-12)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868078
title: Basic and other measurements of radiation at station Tiksi (2013-04)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868079
title: Basic and other measurements of radiation at station Tiksi (2013-05)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.871048
title: Annotated record of the detailed examination of Mn deposits observed in the Pacific Ocean by the USC&GS Ship Explorer in 2 February-27 April, 1960

description: This report contains the field data obtained during the February to April 1960 oceanographic expedition of the USC&GS ship Explorer, together with such results from the analyses of these data as are completed to date. As additional studies are completed, the results will be published by the U.S. Coast and Geodetic Survey or by the other Government agencies, private oceanographic institutions, or individual scientists who are primarily concerned. The USC&GSS Explorer is a 1,900-ton, 220-foot Ocean Survey Ship (OSS 28). During the winter of 1960, the ship was scheduled for a routine transfer from her original home port of Seattle, Wash., to be based in the future out of Norfolk, Va. With the current accelerated demand for oceanographic information, it was felt that this transfer offered a unique opportunity to obtain useful oceanographic information along the route from Seattle to Norfolk.
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: Stewart, Harris B (1962): Oceanographic Cruise Report, USC & GS Ship Explorer - 1960, Seattle, Washington, to Norfolk, Virginia, 2 February-27 April. U.S. Department of Commerce, Coast and Geodetic Survey, Washington D.C., USA, 28 pp
DOI: 10.1594/pangaea.867992
title: Basic and other measurements of radiation at station Tiksi (2012-09)

description: New version (2016-11-10), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868075
title: Basic and other measurements of radiation at station Tiksi (2013-01)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.868077
title: Basic and other measurements of radiation at station Tiksi (2013-03)

description: New version (2016-11-11), data recalculated with corrected calibration coefficients.
DOI: 10.1594/pangaea.872096
title: Factors controlling the spatial distribution of landslides in the Zagros region (Iran)

description: We investigated 335 landslides (including rockslides, rock avalanches, soil slides, and slides) in the Zagros mountain belt of southwest Iran using a digital elevation model (DEM) with 30 m resolution, Google EarthTM images, and field investigation. Individual landslides have volumes ranging from 10**4 (the lower limit of resolution) to 3 × 10**10 m**3 and cover surface areas ranging from 10**3 to 10**8 m**2. The relationship between landslide volume (VL) and area (AL) is well described by a power law of the form VL = AL**alpha, where alpha = 1.49 over five orders of magnitude of AL and seven orders of magnitude of VL. We also show that the frequency-size (i.e., volume) distribution is heavy tailed, following a power law for the largest landslides (&gt;10**7 m**3) with a scaling exponent beta = 1.51. Non-power-law behavior for smaller landslides is probably an artifact due to the relatively low resolution of our data, such that we are essentially missing many small landslides. Comparison of these results with the other published data sets around the globe shows that the Zagros landslides are relatively larger, and they show similar scaling behavior to those observed in other regions, especially with regard to data sets where landslides are deep-seated or relatively large and occur in relatively resistant materials (e.g., consolidated rocks, as opposed to soil). In addition, we used principal component analysis (PCA) to investigate links between the size of landslides and causative factors (e.g., geological, geomorphological, and physical factors). Our results highlight that although the size of landslides is not controlled by any single factor, their geographic distribution is strongly influenced by lithology, elevation, and slope.
description: Supplement to: Ghazipour, Neda; Simpson, Guy (2016): Size distribution and controls of landslides in the Zagros mountain belt (Iran). Geological Society of America, Special Papers, 525, SPE525-13
DOI: 10.1594/pangaea.872154
title: Water temperature profiles of Piburger See (2003-2014)
DOI: 10.1594/pangaea.869783
title: Temperature and salinity measurements in the southern Weddell Sea at mooring site M2

description: Gear ID 1: sbe39, SN 3571; Gear ID 2: microcat, SN 5452; Gear ID 3: rcm7, SN 12313
DOI: 10.1594/pangaea.869789
title: Current measurements in the southern Weddell Sea at mooring site M3

description: Gear ID 1: rcm7, SN 6798; Gear ID 2: rdi_down, SN 10149; Gear ID 3: continental_up, SN 624
DOI: 10.1594/pangaea.871826
title: Photographs taken the intertidal zone at Georgina Cay (Lihou Reef National Marine Park, Coral Sea Territory, Australia), links to photographs
DOI: 10.1594/pangaea.871989
title: Wind speed and direction, temperature, relative humity and pressure at time series station Wollongong, 2012-12-21 to 2013-01-25
DOI: 10.1594/pangaea.871827
title: Photographs taken the terrestrial zone at Georgina Cay (Lihou Reef National Marine Park, Coral Sea Territory, Australia), links to photographs
DOI: 10.1594/pangaea.876218
title: Surface velocities of Columbia Glacier, Alaska during 2011-2016, Links to GeoTIFF files
DOI: 10.1594/pangaea.873256
title: Beach seine fish survey along the coast of Newfoundland from 1960-1964 (Fleming Survey) and from 1992-1996 (Resurrected Fleming Survey)

description: The collapse of the Northwest Atlantic cod (Gadus morhua) stocks in the early 1990s led to widespread ecological changes offshore. Changes in coastal fish communities are less known, largely due to the lack of historical records and long-term, standardized research surveys in coastal ecosystems. We aimed to overcome this with a unique dataset known as the Fleming survey. From 1959 to 1964, a systematic beach-seine survey was conducted to examine juvenile cod abundance in 84 bays (42 of which were consistently sampled and therefore analysed) along the east coast of Newfoundland. In addition to cod, all other fish collected in the seines were recorded. These surveys were repeated from 1992 to 1996 after the cod collapse, and document a substantial reduction in a dominant inshore species - juvenile Atlantic cod. We show that total fish abundance declined significantly with the decrease of cod, whereas Shannon diversity and species evenness significantly increased. Species richness increased in some regions but decreased in others. We also found significant changes in the composition of the fish community likely due to a combination of release from predation from fewer large cod feeding in inshore areas as well as a release from competition from fewer juvenile cod occupying the coastal habitat. Region and the presence of vegetated habitats also significantly influenced the fish community. This study shows a strong reorganization of coastal fish communities after a large-scale fisheries collapse with implications for ecosystem-based and cross-ecosystem management.
description: Supplement to: McCain, James Scott Patrick; Cull, Daneen J; Schneider, David C; Lotze, Heike K (2016): Long-term shift in coastal fish communities before and after the collapse of Atlantic cod (Gadus morhua). ICES Journal of Marine Science, 73(5), 1415-1426
DOI: 10.1594/pangaea.876217
title: TanDEM-X digital elevation models of Columbia Glacier, Alaska during 2011-2016, Links to GeoTIFF files
DOI: 10.1594/pangaea.876224
title: Abrupt Climate Transition from Snowball to Moist or Runaway Greenhouse, links to model results in NetCDF format

description: Ongoing and future space missions aim to identify potentially habitable planets in our Solar System and beyond. Planetary habitability is determined not only by a planet's current stellar insolation and atmospheric properties, but also by the evolutionary history of its climate. It has been suggested that icy planets and moons become habitable after their initial ice shield melts as their host stars brighten. Here we show from global climate model simulations that a habitable state is not achieved in the climatic evolution of those icy planets and moons that possess an inactive carbonate-silicate cycle and low concentrations of greenhouse gases. Examples for such planetary bodies are the icy moons Europa and Enceladus, and certain icy exoplanets orbiting G and F stars. We find that the stellar fluxes that are required to overcome a planet's initial snowball state are so large that they lead to significant water loss and preclude a habitable planet. Specifically, they exceed the moist greenhouse limit, at which water vapour accumulates at high altitudes where it can readily escape, or the runaway greenhouse limit, at which the strength of the greenhouse increases until the oceans boil away. We suggest that some icy planetary bodies may transit directly to a moist or runaway greenhouse without passing through a habitable Earth-like state.
description: Supplement to: Yang, Jun; Ding, Feng; Ramirez, Ramses M; Peltier, W R; Hu, Yongyun; Liu, Yonggang (2017): Abrupt climate transition of icy worlds from snowball to moist or runaway greenhouse. Nature Geoscience, 10(8), 556-560
DOI: 10.1594/pangaea.880486
title: Observation of manganese deposits on Kaikata Seamount, Izu-Ogasawara (Bonin) Arc by the Shikai 2000 submersible

description: During Dive 408 of Shinkai 2000 on the flank of the Kaikata Seamount located on the volcanic front of the Izu-Ogasawara (Bonin) Arc, possibly recent hydrothermal manganese deposits were observed on sandy volcanic sediments at water depths of between 800 and 1200 m. The deposits cover almost the entire surface sediment across the manganese belt on the northwestern flank on the seamount on a scale of kilometers. The occurrence of the deposits, seafloor morphology and temperature of the sediments, together with previous shipboard results, lead to a possible model for the formation of the manganese deposits: A low-temperature hydrothermal solution ascends through fractures or faults in the volcanic substrate into permeable volcanic sands and precipitates manganate minerals which cement several centimeters of surface sand as hardpan. More intense and probably intermittent discharge of hydrothermal solution follows and forms many typical ridge-like vents and mounds on the seafloor. Subsequently, pure dense manganate layers developed beneath the semi-consolidated volcanic sandstone and act as a cap to the ascending fluids. The proposed mechanism may be the dominant type of low-temperature hydrothermal mineralization in submarine island-arc volcanoes and rifts. Similar hydrothermal manganese deopsits most probably occur in other active areas of the modern seafloors and in inactive island arcs.
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: Usui, Akira; Nishimura, Akira (1992): Submersible observations of hydrothermal manganese deposits on the Kaikata Seamount, Izu-Ogasawara (Bonin) Arc. Marine Geology, 106(3-4), 203-216
DOI: 10.1594/pangaea.319787
title: Shipboard acoustic doppler current profiling during cruise HOT-116 (SAC ID 00495)

description: Absolute currents at hourly and 10m intervals
DOI: 10.1594/pangaea.879195
title: (Table 20, page 55) Chemical composition of layers inside a manganese nodule from the Gulf of California in the Pacific Ocean

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.398388
title: Water temperature and current velocity from RAFOS float DBW286

description: Velocity algorithm: splined. Data have been checked by the WOCE Subsurface Float Data Assembly Center. See hdl:10013/epic.32931.d001 for further information.
DOI: 10.1594/pangaea.356222
title: Water temperature XBT profiles from cruise WTES93 (SCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.250508
title: (Figure 2) Planktonic foraminifera abundance in DSDP Hole 93-603C

description: Three holes were drilled at Site 603 on the continental rise off the U.S. east coast during DSDP Leg 93. A thick Pliocene section and a few meters of lowermost Quaternary sediments were recovered in Hole 603C. A detailed biostratigraphic analysis, based on planktonic foraminiferal distribution, allowed us to delineate precisely all the Pliocene zones (sensu Berggren, 1977). The Quaternary sequence was eroded beyond Ericson's Zone P. The calculated sediment accumulation rate remained relatively high during most of the Pliocene, reaching a maximum of 150 m/Ma in Zone PL4. Quantitative micropaleontological methods enabled us to delineate several paleoclimatic and paleoceanographic events, including those at 4.3 and 3.4 Ma.
description: Species abundance: A = abundant (&gt;10 %); C = common (5-10 %), F = few (3-5 %), R = rare (1-2 %), VR = very rare (0-1 %), - = absent.
description: Supplement to: Maalouleh, Kayed; Moullade, Michel (1987): Biostratigraphic and paleoenvironmental study of Neogene and Quaternary planktonic foraminifers from the lower continental eise of the New Jersey Margin (western North Atlantic), Deep Sea Drilling Project Leg 93, Site 603. In: van Hinte, JE; Wise, SW Jr; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 93, 481-491
DOI: 10.1594/pangaea.206804
title: Production at station CD47_0506G#4

description: Queen's University Belfast School of Biological Sciences, Plymouth Marine Laboratory. Authorship was originally taken from the JGOFS CDs (Lowry & BODC) and was changed by request of the BODC.
DOI: 10.1594/pangaea.228553
title: (Table 1) Interstitial water chemistry of DSDP Leg 96 holes
DOI: 10.1594/pangaea.117834
title: Pigments measured on water bottle samples at station TT053_22-10
DOI: 10.1594/pangaea.126135
title: Primary production of station TT007_12-PP_array
DOI: 10.1594/pangaea.761139
title: Percent cropland coverage for sub-Saharan Africa

description: The dataset contains a cropland percent coverage map for Africa created through the combination of five existing land cover products: GLC-2000, MODIS Land Cover, GlobCover, MODIS Crop Likelihood and AfriCover. A synergy map was created in which the products are ranked by experts, which reflects the likelihood or probability that a given pixel is cropland. The cropland map was calibrated with national and sub-national crop statistics using a novel approach. Preliminary validation of the map was undertaken. The resulting cropland map has an accuracy of 83%, which is higher than the accuracy of any of the individual maps. The cropland percent coverage map for Africa is available for overlay on Google Earth or for download at http://agriculture.geo-wiki.org.
description: The Erdas Imagine (.img) format is described at http://www.gdal.org/frmt_hfa.html (stable link to document hdl:10013/epic.37579.d001). Map in GeoTIFF-format see "Other version"; the format is described at http://www.gdal.org/frmt_gtiff.html.
description: Supplement to: Fritz, Steffen; You, Liangzhi; Bun, Andriy; See, Linda; McCallum, Ian; Schill, Christian; Perger, Christoph; Liu, Junguo; Hansen, Matt; Obersteiner, Michael (2011): Cropland for sub-Saharan Africa: A synergistic approach using five land cover data sets. Geophysical Research Letters, 38, L04404, 6 pp
DOI: 10.1594/pangaea.432740
title: Daily sea level from coastal tide gauge station Walvis_Bay in 1991 (Research quality database)
DOI: 10.1594/pangaea.435019
title: Hourly sea level from coastal tide gauge station Hachinohe in 1984 (Research quality database)
DOI: 10.1594/pangaea.219744
title: Mineral composition of clay fraction from Hole 15-150
DOI: 10.1594/pangaea.223197
title: Carbon analysis of Hole 68-502A
DOI: 10.1594/pangaea.885274
title: MATLAB code and raw data (mzXML) for one headwater stream, three rivers, one fjord and one seawater sample

description: Molecular complexity is an inherent feature of dissolved organic matter (DOM), confounding investigations into its nature. Recent research has suggested that this complexity may explain the persistence of DOM due to the implied low abundance of individual compounds. Here, we use chromatographic separation and collision induced dissociation of deprotonated molecules to demonstrate the extreme isomeric complexity of individual molecular formulas in DOM and show that isomeric complexity occurs across diverse aquatic environments.This raw data was generated by HPLC-Orbitrap and can be manipulated to produce the figures etc. of Hawkes et al. (2018) with the Matlab code available.
description: Supplement to: Hawkes, Jeffrey A; Patriarca, Claudia; Sjöberg, Per J R; Tranvik, Lars J; Bergquist, Jonas (2018): Extreme isomeric complexity of dissolved organic matter found across aquatic environments. Limnology and Oceanography Letters, 3(2), 21-30
DOI: 10.1594/pangaea.229201
title: (Table 1) Geochemistry of surface water samples from DSDP Leg 96 sites
DOI: 10.1594/pangaea.894608
title: Stratigraphic description of drilling core M133 from Ziskensee peatland
DOI: 10.1594/pangaea.222311
title: Grain size analysis of Hole 57-441B
DOI: 10.1594/pangaea.894612
title: Stratigraphic description of drilling core M170 from Calpenzmoor peatland
DOI: 10.1594/pangaea.894613
title: Stratigraphic description of drilling core M171 from Pastling peatland
DOI: 10.1594/pangaea.894614
title: Stratigraphic description of drilling core M172 from Kleinsee peatland
DOI: 10.1594/pangaea.183652
title: Primary production at time series station DYFAMED from date 1996-03-01

description: Incubation time: 4 h
DOI: 10.1594/pangaea.222565
title: Carbon analysis of Hole 1-6A
DOI: 10.1594/pangaea.262822
title: Major-element chemical analyses of Hole 59-449
DOI: 10.1594/pangaea.894617
title: Stratigraphic description of drilling core M175 from Die Laie peatland
DOI: 10.1594/pangaea.894618
title: Stratigraphic description of drilling core M176 from Weisses Lauch peatland
DOI: 10.1594/pangaea.894627
title: Stratigraphic description of drilling core M29 from Kesselmoor N Ziskensee peatland
DOI: 10.1594/pangaea.357400
title: Water temperature XBT profiles from cruise MQLN798 (SCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.430780
title: Daily sea level from coastal tide gauge station Panama_City_Beach in 1998 (Research quality database)
DOI: 10.1594/pangaea.894629
title: Stratigraphic description of drilling core M296 from Seilensee peatland
DOI: 10.1594/pangaea.431762
title: Daily sea level from coastal tide gauge station San_Diego in 1980 (Research quality database)
DOI: 10.1594/pangaea.894630
title: Stratigraphic description of drilling core M31 from Moor SO Kruegersee peatland
DOI: 10.1594/pangaea.894632
title: Stratigraphic description of drilling core M350 from Kleiner Wiedel peatland
DOI: 10.1594/pangaea.894645
title: Stratigraphic description of drilling core M51 from Grosser Wiedel 2 peatland
DOI: 10.1594/pangaea.894648
title: Stratigraphic description of drilling core M521 from Staakower Lauche peatland
DOI: 10.1594/pangaea.439143
title: Hourly sea level from coastal tide gauge station Loreto in 1983 (Research quality database)
DOI: 10.1594/pangaea.894650
title: Stratigraphic description of drilling core M524 from Grabkower Seewiesen peatland
DOI: 10.1594/pangaea.894651
title: Stratigraphic description of drilling core M619 from Moor O Calpenz (Hasenluch) peatland
DOI: 10.1594/pangaea.358073
title: Water temperature real-time profiles from cruise NYGG90 (SCQC)

description: For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.360238
title: Water temperature real-time profiles from cruise UOT_4300194 (SCQC)

description: SCQC=quality controlled by Science Center. For definition of quality flags see hdl:10013/epic.31518.d001
DOI: 10.1594/pangaea.894534
title: Stratigraphic description of drilling core M116 from Kleine Zehme peatland
DOI: 10.1594/pangaea.894536
title: Stratigraphic description of drilling core M131 from Meierei peatland
DOI: 10.1594/pangaea.820954
title: Ozone measurements from station Boulder (2011-05)

description: Location: Boulder, Colorado, USA; Distance from radiation site: 16 km
DOI: 10.1594/pangaea.821503
title: Radiosonde measurements from station Ishigakijima (2013-08)
DOI: 10.1594/pangaea.820955
title: Other measurements at 300 m from station Boulder (2011-05)
DOI: 10.1594/pangaea.820957
title: Radiosonde measurements from station Boulder (2011-06)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.820958
title: Ozone measurements from station Boulder (2011-06)

description: Location: Boulder, Colorado, USA; Distance from radiation site: 16 km