cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.mwmce5
title: Occurrence Download

description: A dataset containing 85905 species occurrences available in GBIF matching the query:
{
 "and" : [
 "InstitutionCode ~TPWD",
 "BasisOfRecord is one of (Human Observation, Specimen)",
 "HasGeospatialIssue is false",
 "HasCoordinate is true",
 "TaxonKey is one of (Alpheidae, Panopeidae)"
 ]
}

 The dataset includes 85905 records from 21 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031286-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.876486
title: Annotated record of the detailed examination of an Mn deposit surveyed in the North Atlantic Ocean (R/V Robert Conrad, Cruise 15)

description: he proposed mining of ferromanganese deposits from the deep sea will affect benthic and pelagic environments depending to a great extent on the method of nodule retrieval and separation. Three basic deep-ocean mining systems have been proposed, each of which will effect the removal under varying conditions of water, sediment and nodules from the ocean floor. This report summarizes existing oceanographhic information on potential manganese nodule mining areas at the date of publication and presents the results of field observations in a manganese nodule area of the North Atlantic Ocean surveyed during Cruise 15 of the R/V Robert Conrad.
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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: Amos, A F; Garside, Christopher; Gerard, Robert D; Levitus, Sydney; Malone, T C; Paul, Allen Z; Roels, Oswald A (1973): Study of the impact of manganese nodule mining on the seabed and water column. In: Phase I Report - Inter-University Program of Research on Ferromanganese Deposits of the Ocean Floor. Seabed Assessment Program, International Decade of Ocean Exploration, National Science Foundation, Washington D.C., USA, 221-264
DOI: 10.1594/pangaea.808638
title: (Table 1) Carbonate, organic carbon and nitrogen at DSDP Sites 79-547 and 79-545
DOI: 10.1594/pangaea.664820
title: Oceanography at CTD/bottle station IFREMER_1660
DOI: 10.1594/pangaea.777125
title: Section images from IODP Hole 331-C0013D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.871468
title: (Table 2) Pore water geochemistry and bulk sample carbon content from the Troll gas fieldin the Norwegian North Sea
DOI: 10.1594/pangaea.915970
title: CESM coupled simulation dataset with new (Mod_cp) and original (F09) dynamical coupling scheme between atmosphere and ocean

description: 1. Coupled models simulate air-sea interaction by coupling components models together. However, in state-of-the-art models such as CESM, the atmospheric model contains dynamic core and physic parameterization that are not differentiated during air-sea interaction. The dynamics-physics (D-P) coupling in CAM causes the prognostic winds of the dynamic core be interpolated onto non-staggered locations. We propose a new dynamical coupling scheme (denoted as Mod_cp) that eliminates the extra interpolation during D-P coupling for the atmosphere-ocean interaction, reducing the numerical diffusion during the dynamics-physics coupling for air-sea interactions.2. Using new and original dynamical coupling scheme, two coupled simulations (100 years) were conducted. Climatology of atmosphere (cam), ocean (ocn) and sea ice (ice) model simulations are archived here (last 50 years). The resolution is around 1 latitude x 1 longitude.3. B1850_mod_cp denotes the simulation with new dynamical coupling scheme, B1850_f09_g16 denotes the simulation with original scheme.
DOI: 10.1594/pangaea.777126
title: Section images from IODP Hole 331-C0013E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.668054
title: Basic measurements of radiation at station Boulder (2005-05)
DOI: 10.1594/pangaea.816432
title: (Table 1) Sulfur and oxygen isotopes from two anhydrite samples recovered from DSDP Hole 70-504B

description: The first anhydrite reported from oceanic basalts occurs in altered basalts drilled during DSDP Leg 70 from Hole 504B. Anhydrite has been identified in several samples, two of which were studied in detail.Anhydrite in Sample 504B-40-3 (130-135 cm), which was acquired at 310 meters sub-basement, occurs in a dolerite at the center of a vug rimmed by saponite and calcite. Red iron-hydroxide-rich alteration halos occur from 0 to 310 meters sub-basement; primary sulfides in these halos are oxidized, and the rocks have lost large amounts of sulfur. The anhydrite in this sample has a d34S value of 18.5 per mil, and it is interpreted to have formed from a fluid containing a mixture of seawater sulfate (20.9 per mil) and basaltic sulfur (0 per mil) released during the oxidation of primary sulfides.Anhydrite in Sample 504B-48-3 (14-18 cm), which was found at 376 meters sub-basement, occurs intergrown with gyrolite at the center of a 1-cm-wide vein that is rimmed by saponite and quartz. At sub-basement depths below 310 meters to the bottom of the Leg 70 section (562 m sub-basement), the rocks exhibit the effects of anoxic alteration with common secondary pyrite. Anhydrite in Sample 504B-48-3 (14-18 cm) has a d34S value of 36.7 per mil, and it is interpreted to have formed from seawater-derived fluids enriched in 34S through sulfate reduction. Temperatures of alteration calculated from oxygen isotope data range from 60 to 100°C. Sulfate reduction may have occurred in situ, or elsewhere at higher temperature, possibly deeper in the crust.The secondary mineral paragenetic sequence indicates a progressive decrease in Mg and increase in Ca in the circulating fluids. This eventually led to anhydrite formation late in the alteration process.
description: Supplement to: Alt, Jeffrey C; Honnorez, Jose J; Hubberten, Hans-Wolfgang; Saltzman, Eric S (1983): Occurrence and origin of anhydrite from Deep Sea Drilling Project Leg 70, Hole 504B, Costa Rica Rift. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 547-550
DOI: 10.1594/pangaea.772098
title: Magnetometer measurements from IODP Hole 315-C0001F

description: Geocode = [m CSF-A] Top Core depth (below sea floor). Measurements data just above (negative section depth) and below (depth exceed section length) a core section are utilized in the deconvolution (http://en.wikipedia.org/wiki/Deconvolution).
DOI: 10.1594/pangaea.836027
title: (Table 3) Grain size of surface sediments of three bays n Hurricane Hole, U.S. Virgin Islands
DOI: 10.1594/pangaea.836077
title: Links to SEM photographs of ostracoda from the Paleocene-Eocene samples at ODP Site 865

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.671870
title: Basic measurements of radiation at station Regina (2002-07)
DOI: 10.1594/pangaea.816458
title: (Table 6, page 577) Chemical composition of Mn-rich mineral deposit from basalt of Costa Rica Rift, Site 501, DSDP Leg 68

description: Basalt samples recovered during DSDP Legs 68, 69, and 70 from a 550-meter-thick section in two holes near the Costa Rica Rift (Holes 501 and 504B) were found to contain the following secondary minerals: trioctahedral and dioctahedral smectite, chlorite, mixed-layer clays, talc, hematite, pyrite, foujasite, phillipsite, analcime, natrolite, thomsonite, gyrolite, aragonite, calcite, anhydrite, chalcocite, Fe-hydrosilicate, okenite, apophyllite, actinolite, cristobalite, quartz, and magnesite. A less positive identification of bismutite was made. A mineral rich in Mn and minerals with strong reflections at 12.9 Å and 3.20 Å remain unidentified. Trioctahedral smectite replaces glass and olivine in the basalt groundmass. The other secondary minerals occur in veins. The distribution of the secondary minerals in the basalt section shows both hydrothermal and oxidizing-nonoxidizing zonation. Most of the secondary minerals formed under alkaline, nonoxidizing conditions at temperatures up to 120° C. An acidic regime probably existed in the lowest portion of basalt. Oxidative diagenesis followed nonoxidative diagenesis in the upper part of the section. Oxidative diagenesis is characterized by the absence of celadonite, rare occurrences of dioctahedral smectite, and widespread hematite and phillipsite.
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.747356
title: Meteorological observations during AMPHITRITE cruise from Nieuwediep to Guinee started at 1838-04-21
DOI: 10.1594/pangaea.833898
title: SYNOPS: Synoptical observations from meteorological stations of West Africa, with links to data sets

description: Positions can be identified by the WMO station number. Dataset created by IMPETUS subproject A1. IMPETUS data set ID: 812
DOI: 10.1594/pangaea.511745
title: Physical oceanography and CFC measured on water bottle samples at station M59/2_553
DOI: 10.1594/pangaea.511746
title: Physical oceanography and CFC measured on water bottle samples at station M59/2_554
DOI: 10.1594/pangaea.830631
title: Microphotos from IODP Hole 338-C0002K

description: Geocode = [m CSF-A]
DOI: 10.1594/pangaea.834398
title: Reconstructed surface ocean CO2 in 1990-2011 with link to a feed-forward neural network model in NetCDF format
DOI: 10.1594/pangaea.786512
title: Profile of sediment echo sounding during METEOR cruise M84/2 with links to Parasound data files

description: File format description see: Data Acquisition of ATLAS PARASTORE, Atlas Hydrographic (2007), Operator Manual ATLAS PARASTORE, Doc. Id.: ED 6006 G 212:/Version: 4.0/Edition: 05/2007, hdl:10013/epic.35589.d001.
DOI: 10.1594/pangaea.706790
title: Documentation of sediment core GeoB9916-1
DOI: 10.1594/pangaea.872542
title: (Table 08a) Raw data of reflectance spectrophotometer (RSC) from different holes of IODP Site 342-U1406
DOI: 10.1594/pangaea.710752
title: (Table 7) Oxygen isotope ratio and calculated mineral formation temperature of clay and quartz samples from ODP Hole 193-1189A
DOI: 10.1594/pangaea.725485
title: (Table 2) Magnetic hysteresis properties of DSDP Hole 85-575
DOI: 10.1594/pangaea.803153
title: (Table 1) Rock-magnetic properties of basalts from ODP Holes 135-834B and 135-835B
DOI: 10.1594/pangaea.859710
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE339
DOI: 10.1594/pangaea.705776
title: Documentation of sediment core GIK13554-1
DOI: 10.1594/pangaea.907958
title: Microscopic images and 2D-MALDI-images of the sponge Aplysina aerophoba in response to grazing and video recording of grazing behavior

description: We aimed to investigate the cellular and chemical response of the chemically defended sponge Aplysina aerophoba (Phylum Porifera: Class Demospongiae) to grazing by its specialist Tylodina perversa (Phylum Mollusca: Class Opistobranchia). Three treatments were applied: control, grazing, and mechanical damage. Samples were collected 3 hours, 1 day, 3 days, and 6 days after treatment. The behavior of sea slugs after directly contact with sponge specimen was recorded by using a GoPro Hero 4 camera with the program time lapse (1 picture every 5 sec) for 1.5 to 2 hours. Our results showed that spherulous cells were recruited to the wounded site in a time-dependent manner. MALDI-imaging MS showed that both brominated compounds (aerophobin-2 and aeroplysinin-1) localized usually at the sponge surface and accumulated at the damaged surface upon wounding. As spherulous cells are common in many members of the class Demospongiae, the recruitment of defensive cells may also occur in other sponges for protecting these filter-feeders. Our study contributes to understanding the evolutionary mechanisms in sponges for facing grazing and wounding.
DOI: 10.1594/pangaea.695067
title: Concentrations of total organic carbon in water of the Ionian Sea at Station SEPT-2000-IRI45
DOI: 10.1594/pangaea.821219
title: Abundance of pteropods in the Hilutangan Channel, Cebu Islands in January and Febuary 1972
DOI: 10.1594/pangaea.872718
title: Nutrients in porewater from German Bight during HEINCKE cruise HE304 in May and June 2009
DOI: 10.1594/pangaea.877558
title: Georeferenced photographs of benthic photoquadrats acquired along transects from Endeavour Reef in the Cairns to Cooktown region of the Great Barrier Reef (2017-05)
DOI: 10.1594/pangaea.758465
title: (Table 5) Distribution of radiolaria in Miocene to Pleistocene sediments of DSDP Hole 7-63B

description: Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent.
DOI: 10.1594/pangaea.741887
title: SeaWiFS absorption results due to detritus and yellow substances measured at 412 nm

description: Monthly coverage, 18 km on equal angle resolution.
DOI: 10.1594/pangaea.552359
title: Thick-section images of the EDML ice core from 1500 to 1600 m depth
DOI: 10.1594/pangaea.846621
title: Snow melt monitoring at Fuglebekken, around Hornsund, Svalbard, in 2014, links to images

description: Roof of a scientif container in the Fuglebekken catchment. Camera mounted 5 m above the surface, looking N over Fuglebekken catchment towards Fugleberget. 68 images in the period April-June 2014, different times of the day depending on fog cloudiness.
DOI: 10.1594/pangaea.696217
title: Organic carbon and nitrogen concentrations in waters of the Arabian Sea at Station M32/3_271
DOI: 10.1594/pangaea.859719
title: Continuous thermosalinograph oceanography along HEINCKE cruise track HE349
DOI: 10.1594/pangaea.846622
title: Snow melt monitoring at Fugleberget, around Hornsund, Svalbard, in 2014, links to images

description: Located at approx. 550 m a.s.l. looking SSW on the Fuglebekken catchment, involving the Polish Polar Station. Orthorectified images at 1 m resolution of the camera scene (in UTM zone 33), ranging from the coast at the end of Revdalen (left), Isbjørnhamna (right) to the lower slopes of Fugleberget (top). The absolute referencing accuracy is about 5m in the N (top part) and 50 - 100 m in the W (lower left part). Buildings and elevated structures cause strong distortions and image errors. We provide both geopreferenced images in the geotiff-format (readable e.g. in ArcGIS) and unreferenced jpg images for easy overview.
DOI: 10.1594/pangaea.816386
title: (Table 1) Uranium at DSDP Hole 69-504B pore water

description: Basalt formation waters collected from Hole 504B at sub-basement depths of 194, 201, 365, and 440 meters show inverse linear relationships between 87Sr/86Sr and Ca, 87Sr/86Sr and Sr, and K and Ca. If the Ca content of a fully reacted formation water end-member is assumed to be 1340 ppm, the K, Sr, and 87Sr/86Sr values for the end-member are 334 ppm, 7.67 ppm, and 0.70836, respectively. With respect to contemporary seawater at Hole 504B, K is depleted by 13%, Sr is enriched by 2.7%, and 87Sr/86Sr is depleted by 0.8%. The Sr/Ca ratio of the formation water (0.0057) is much lower than that of seawater (0.018) but is similar to the submarine hot spring waters from the Galapagos Rift and East Pacific Rise and to geothermal brines from Iceland. At the intermediate temperatures represented by the Hole 504B formation waters (70°-105°C), the interaction between seawater and the ocean crust produces large solution enrichments in Ca, the addition of a significant basalt Sr isotope component accompanied by only a minor elemental Sr component, and the removal from solution of seawater K. The Rb, Cs, and Ba contents of the formation waters appear to be affected by contamination, possibly from drilling muds.
description: Sediment depth is given in mbsf. Concentrations are corrected (+0.67%) for HCl dilution.
description: Supplement to: Hart, Stanley R; Mottl, Michael J (1983): Alkali and Sr isotope geochemistry of waters collected from basaltic basement, Deep Sea Drilling Project Hole 504B, Costa Rica Rift. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office)Government Printing Office, 69, 487-494
DOI: 10.1594/pangaea.840842
title: Mesocosm experiment on warming and acidification effects in 2012: Individual measurements of cell sizes of dominant taxa

description: low = 560 ppmhigh = 1400 ppm//
DOI: 10.1594/pangaea.915802
title: Quantifying the effect of the Drake Passage opening on the Eocene Ocean

description: This dataset combines the oceanic and atmospheric outputs from various experiments modelling the Drake Passage opening during the Eocene (Toumoulin et al. 2020, Paleoceanography and Paleoclimatology). It includes 4 simulations with a 40 Ma paleogeography, a 1120 ppm pCO2 and different depths of the Drake Passage (0, 100, 1000, 2500m). Experiments were performed with the general circulation model IPSL-CM5A2. Each of these simulations ran for 4000 years until a quasi-equilibrium state (deep ocean temperature change &lt;0.1°C/century).Data are monthly averages over the last 100 years.
DOI: 10.1594/pangaea.815781
title: (Table 3) Particle size distribution of mountainous tundra soils from the Rai-Iz Massif
DOI: 10.1594/pangaea.871889
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 42 (Holes 372 and 379A)

description: Leg 42, Part 1 of the Deep Sea Drilling Project was scheduled to continue the geological exploration of the Mediterranean. The strategy was to search for areas where the Mediterranean Evaporite formation had been largely or completely removed by erosion, such is the case for Site 372. For Leg 42, Part 2, the project entered the Black Sea. In particular, Site 379 was located the central portion of the Black Sea.
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: Worstell, Paula J; Mélières, Frédéric; Bernoulli, Daniel; Erickson, A J; Wright, Ramil; Bizon, G; Cita, Maria Bianca; Müller, Carla; Kidd, Robert B; Fabricius, F H; Garrison, Robert E; Hsü, Kenneth J; Montadert, Lucien (1978): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XLII Pt. 1, 1249 pp + 1244 pp
DOI: 10.1594/pangaea.893244
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018081412

description: INITIALIZATION: 2018081412FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.679342
title: Grain size composition of sediments and sedimentary rocks from Hole VNIIO-1987-140 drilled in the Barents Sea
DOI: 10.1594/pangaea.689898
title: Radiosonde M58_R077 during METEOR cruise M58 on 1981-09-29 05:00h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.873565
title: Annotated record of the detailed examination of Mn deposits from R/V Eltanin Cruise 14 stations

description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 13 in 1964 by the Department of Geology, Florida State University. Cores and dredges were recovered for 17 stations along with bottom photography and are available at the Antarctic Research Facility, Florida State University for sampling and study.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.891560
title: CICE output from Global Ocean Forecast System (GOFS) 3.1 for 2018060112

description: INITIALIZATION: 2018060112FORECASTS:12-hrly out to 7.5 days (t180)GRIDS:ARCu0.08 -- poleward of 40NANTu0.08 -- poleward of 49.52SPARAMETERS:hi:standard_name = "sea_ice_thickness" ;hs:standard_name = "surface_snow_thickness" ;Tsfc:standard_name = "surface_temperature_where_sea_ice" ;aice:standard_name = "sea_ice_area_fraction" ;uvel:standard_name = "eastward_sea_ice_velocity" ;vvel:standard_name = "northward_sea_ice_velocity" ;sst:standard_name = "sea_water_temperature" ;uocn:standard_name = "eastward_sea_water_velocity" ;vocn:standard_name = "northward_sea_water_velocity" ;Tair:standard_name = "air_temperature" ;strength:standard_name = "compressive_strength_of_sea_ice" ;
DOI: 10.1594/pangaea.695022
title: Concentrations of chlorophyll-alpha in water of the Ionian Sea at Station MARCH-2000-IRI17

description: Samples from 2 l of sea water were filtered through polycarbonate Millipore filters. The filters were kept deep frozen and analyzed according to Holm-Hansen et al. (Holm-Hansen, O., Lorenzen, C.J., Holmes, R.W., Strickland, J.D.H. 1965. Fluorometric determination of chlorophyll. Journal du Conseil Permanent International Pour l'Exploration de la Mer 30, 3-15).
DOI: 10.1594/pangaea.854823
title: Carte Geologique d'Europe = Geological Map of Europe = Geologische Karte von Europa

description: In the table below, the full map is linked in jpg-format as a 37 MB file with a print size of 100 x 90 cm (Ord No 0). With ordinal numbers 1-49 detailed maps are provided in pdf-format of 2 MB each. The numbers refer to the tile numbers in the mosaic overview.
DOI: 10.1594/pangaea.818105
title: (Table 5) Comparison between unaltered interstitial glass and associated smectite, DSDP Sample 65-482C-10-1,16-18 both recalculated to 100%
DOI: 10.1594/pangaea.678239
title: Grain size composition of sediments from Hole VNIIO-1987-118 drilled in the Barents Sea