cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.929749
title: A Global Atlas of Artificial Light At Night Under the Sea

description: Coastlines globally are increasingly being illuminated with Artificial Light At Night (ALAN) from various urban infrastructures such as houses, offices, piers, roads, ports and dockyards. Artificial sky glow can now be detected above 22% of the world's coasts nightly and will dramatically increase as coastal human populations more than double by the year 2060. One of the clearest demonstrations that we have entered another epoch, the urbanocene, is the prevalence of ALAN visible from space. Photobiological life history adaptations to the moon and sun are near ubiquitous in the surface ocean (0-200m), such that cycles and gradients of light intensity and spectra are major structuring factors in marine ecosystems. The potential for ALAN to reshape the ecology of coastal habitats by interfering with natural light cycles and the biological processes they inform is increasingly recognized and is an emergent focus for research.This dataset is derived from two primary satellite data sources: an artificial night sky brightness world atlas (Falchi et al., 2016) and an in-water Inherent Optical Property (Lee et al., 2002) dataset derived from ESA's Ocean Colour Climate Change Initiative (OC-CCI https://www.oceancolour.org/).These primary datasets are both used in conjunction with in-situ derived measurements and radiative transfer modelling in order to quantify the critical depth (Zc) to which biologically relevant ALAN penetrates throughout the global ocean's estuarine, coastal and near shore regions, in particular the area defined by an individual country's Exclusive Economic Zone.The critical depth is defined as the depth at which the modelled light level in the water column, illuminated by ALAN, drops below 0.102 µWm-2, the minimum irradiance of white light that elicits diel vertical migration in adult female Calanus copepods (Batnes et al., 2015). This is function of incident ALAN irradiance at the surface as well as the in-water transparency (governed by in-water optically active constituents).This dataset is an updated version of https://doi.pangaea.de/10.1594/PANGAEA.922885.
description: Filenaming conventions:(1) In-water_clear-sky_ALAN_Zc_Month-MM_aaS_bbN_ccW_ddE_AAA.ncwhere MM is month of the year (01 - January)aa, bb, cc, dd define the regional box of interest where:aa is the minimum latitudebb is the maximum latitudecc is the minimum longitudedd is the maximum longitudeAAA is a free-form descriptor of the geographical region of interest(2)Derived dataset from the primary data by Lee et al., 2002 publication algorithm using the primary dataset of Sathyendranath et al., 2019 (the CCI dataset):ESACCI-OC-MAPPED-CLIMATOLOGY-1M_MONTHLY_4km_GEO_PML_OCx_QAA-Kd-mm-fv4.0.ncwhere mm is the month of the year (01 - January).They contain the diffuse attenuation coefficient Kd at three broadband wavelengths, global, at 4 km resolution in geometric projection.
DOI: 10.1594/pangaea.868657
title: Annotated record of the detailed examination of Mn deposits from DSDP Site 113, Leg 12 (Cores 113-3, 113-11)

description: Seismic reflection profiles across the Labrador Sea by Vema-19 and Charcot-S had revealed a rugged basement topography almost entirely buried by sediments up to 2000 meters thick. It was first suggested that this was the median valley of a mid-Labrador Sea ridge where oceanic crust was generated during the last phase of opening of the Labrador Sea but which is now virtually inactive and covered by sediment. The choice of a site where basement could be dated by sampling sediments that were believed to be the same age as the basement was difficult. Site 113 was eventually chosen in a local valley 8 kilometers south of a small knoll believed, from the Vema-ll record, to be a basement high.
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: Laughton, Anthony S; Berggren, William A; Benson, Richard N; Davies, Thomas A; Franz, Ulrich; Musich, L F; Perch-Nielsen, Katharina; Ruffman, A; van Hinte, Jan E; Whitmarsh, Robert B; Bukry, David (1972): Site 113. In: Laughton, A.S.; Berggren, W.A.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XII, 255-311
DOI: 10.1594/pangaea.222793
title: Carbon analysis of Hole 26-257
DOI: 10.1594/pangaea.230527
title: Smear slide analysis of Hole 26-256
DOI: 10.1594/pangaea.224643
title: Wet bulk density (GRAPE) of Hole 26-253
DOI: 10.1594/pangaea.224642
title: Wet bulk density (GRAPE) of Hole 26-252
DOI: 10.1594/pangaea.221278
title: Physical properties of Hole 26-256
DOI: 10.1594/pangaea.962659
title: Raw data from Triaxus topAWI (towed ocean profiler of the AWI) during RV POLARSTERN cruise PS131

description: The MacArtney Triaxus extended version is a remotely operated towed vehicle (ROTV). It is towed behind the ship between 2 and 10 knots and can undulate in a saw tooth pattern between a few meters below the surface and 350m depth. The umbilical provides power and a fiber optic link to sensors that are mounted on the Triaxus (see SensorWeb). The data collected by the sensors were recorded on separate computers, one computer per sensor (including the flight information from the Triaxus itself). Thus, there are 7 separate data streams saved in separate folders plus a folder with metadata information about the different dives. During long Triaxus operations, new data files would be started approximately every 4 hours, because some of the employed software programs do not allow for backing up of the files while they are still being written to. A heavy weight (depressor) was employed directly behind the ship to pull the umbilical below the water line before sea ice can close in behind the ship. In addition to a few test dives, three transects across the marginal ice zone north of Svalbard (Yermak Plateau) were collected on PS131 in July/August 2022.
DOI: 10.1594/pangaea.964030
title: Raw physical oceanography and ocean current velocity data from mooring SCO2-1 in Scoresby Sound, East Greenland, Aug 2018 – Aug 2022

description: Time-series data of physical oceanography and ocean current velocities were obtained from mooring SCO2-1 in the Fram Strait from Aug 2018 to Aug 2022. The mooring was deployed during RV MARIA S. MERIAN expedition MSM76 and recovered during RV POLARSTERN expedition PS131. The attached archive contains raw data files of two Seabird SBE16 SeaCATs (nominal depths: 595m, 800m; sampling interval 1h), two SBE37 MicroCATs (nominal depths: 666m, 726m; sampling interval 10m), three SBE56 temperature logger (nominal depths: 626m, 696m, 766m; sampling interval 20s), one RDI Longranger ADCP (nominal depth: 796m; sampling interval 2h) and one AADI RCM11 current meter (nominal depth: 801m; sampling interval 2h). Auxiliary information such as sensor calibration sheets, mooring diagrams, and schedule files are also provided, if applicable. The ADCP had issues and only recorded data at irregular intervals up to several days.
description: The file SCO2-1.zip includes all available sensor raw data from mooring SCO2-1. The structure of the unzipped folders is mooring-&gt;sensor/sampler type-&gt;serial number-&gt;instrument files. All instruments were synched to UTC before deployment, and the offset after the recovery is supplied in the respective instrument folder, if available. The archive also contains the sensor calibration sheets/files and relevant sampler schedule files, if available. Finally, mooring schematics are also attached as pdfs in the root folder.The authors are grateful to the captains, crews and technical/scientific staff of the expeditions MSM76 onboard RV Maria S. Merian and PS131 onboard RV Polarstern. Many individuals have contributed to the conception of the research, the preparation of the instruments, the deployment and recoveries, as well as to the retrieval of the data, which we greatly appreciate.
DOI: 10.1594/pangaea.224645
title: Wet bulk density (GRAPE) of Hole 26-256
DOI: 10.1594/pangaea.222041
title: Grain size analysis of Hole 26-250A
DOI: 10.1594/pangaea.222790
title: Carbon analysis of Hole 26-254
DOI: 10.1594/pangaea.222045
title: Grain size analysis of Hole 26-253
DOI: 10.1594/pangaea.262387
title: Major-element chemical analyses of Hole 26-256
DOI: 10.1594/pangaea.220151
title: Mineral composition of silt fraction from Hole 26-257
DOI: 10.1594/pangaea.229361
title: Sound velocity of Hole 26-250
DOI: 10.1594/pangaea.224640
title: Wet bulk density (GRAPE) of Hole 26-251
DOI: 10.1594/pangaea.261353
title: Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 26-256
DOI: 10.1594/pangaea.230523
title: Smear slide analysis of Hole 26-252
DOI: 10.1594/pangaea.261350
title: Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 26-251A
DOI: 10.1594/pangaea.220525
title: Mineral composition of bulk sediment from Hole 26-256
DOI: 10.1594/pangaea.230521
title: Smear slide analysis of Hole 26-251
DOI: 10.1594/pangaea.230528
title: Smear slide analysis of Hole 26-257
DOI: 10.1594/pangaea.230529
title: Smear slide analysis of Hole 26-258
DOI: 10.1594/pangaea.230530
title: Smear slide analysis of Hole 26-258A
DOI: 10.1594/pangaea.230531
title: Smear slide analysis of Hole 26-258B
DOI: 10.1594/pangaea.230519
title: Smear slide analysis of Hole 26-250
DOI: 10.1594/pangaea.230525
title: Smear slide analysis of Hole 26-254
DOI: 10.1594/pangaea.221277
title: Physical properties of Hole 26-254
DOI: 10.1594/pangaea.220150
title: Mineral composition of silt fraction from Hole 26-256
DOI: 10.1594/pangaea.909588
title: Annual glacier elevation change rate raster dataset, South Georgia 2000 and 2013
DOI: 10.1594/pangaea.220527
title: Mineral composition of bulk sediment from Hole 26-258
DOI: 10.1594/pangaea.222048
title: Grain size analysis of Hole 26-256
DOI: 10.1594/pangaea.221271
title: Physical properties of Hole 26-250
DOI: 10.1594/pangaea.249329
title: Nannofossil abundance of Hole 26-253

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.221281
title: Physical properties of Hole 26-258A
DOI: 10.1594/pangaea.220524
title: Mineral composition of bulk sediment from Hole 26-255
DOI: 10.1594/pangaea.221280
title: Physical properties of Hole 26-258
DOI: 10.1594/pangaea.224639
title: Wet bulk density (GRAPE) of Hole 26-250A
DOI: 10.1594/pangaea.263122
title: Minor-element chemical analyses of Hole 26-253
DOI: 10.1594/pangaea.219851
title: Mineral composition of clay fraction from Hole 26-253
DOI: 10.1594/pangaea.261352
title: Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 26-254
DOI: 10.1594/pangaea.219856
title: Mineral composition of clay fraction from Hole 26-258
DOI: 10.1594/pangaea.219853
title: Mineral composition of clay fraction from Hole 26-255
DOI: 10.1594/pangaea.220147
title: Mineral composition of silt fraction from Hole 26-253
DOI: 10.1594/pangaea.261351
title: Paleomagnetic and rock magnetic measurements of igneous and metamorphic rocks of Hole 26-253
DOI: 10.1594/pangaea.868631
title: Annotated record of the detailed examination of Mn deposits from DSDP Site 111, Leg 12 (Core 111-3, 111A-12)

description: Orphan Knoll is a pronounced submarine feature at the foot of the continental rise and bounded on its northeast side by the 4000-meter deep abyssal plain of the Labrador Basin. It lies isolated on the ocean floor some 550 kilometers northeast of Newfoundland and 350 kilometers north of Flemish Cape. The DSDP drilling site 111 was originally chosen by the Atlantic Advisory Panel on the basis of Charcot's Flexotir continuous seismic profile provided by CNEXO.
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: Laughton, Anthony S; Berggren, William A; Benson, Richard N; Davies, Thomas A; Franz, A; Musich, L F; Perch-Nielsen, Katharina; Ruffman, A; van Hinte, Jan E; Whitmarsh, Robert B (1972): Site 111. In: Laughton, A.S.; Berggren, W.A.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XII, 33-159
DOI: 10.1594/pangaea.249264
title: Planktic foraminifera abundance of Hole 26-250

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.262388
title: Major-element chemical analyses of Hole 26-257
DOI: 10.1594/pangaea.220526
title: Mineral composition of bulk sediment from Hole 26-257
DOI: 10.1594/pangaea.221276
title: Physical properties of Hole 26-253
DOI: 10.1594/pangaea.229364
title: Sound velocity of Hole 26-251A
DOI: 10.1594/pangaea.219852
title: Mineral composition of clay fraction from Hole 26-254
DOI: 10.1594/pangaea.219855
title: Mineral composition of clay fraction from Hole 26-257
DOI: 10.1594/pangaea.249272
title: Planktic foraminifera abundance of Hole 26-258A

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.263251
title: Minor-element chemical analyses of Hole 26-250A
DOI: 10.1594/pangaea.743991
title: Clay mineralogy of ODP Leg 103 sites (Table 1)

description: Samples from Cenozoic and Mesozoic sediments drilled during ODP Leg 103 were analyzed for clay mineralogy. Kaolinite, chlorite, illite, and smectite occur in most of the samples studied; palygorskite and sepiolite occur principally in Paleogene and Eocene brown clays. In general, throughout the section deposited in the syn- and post-rift period, the more calcareous-rich pelagic sediments contain greater amounts of smectite and lesser amounts of kaolinite and chlorite than do the calcareous-poor terrigenous sediments. The clay data presented here also lend support to the general paleoenvironmental interpretation of a relatively warm climate throughout the Cretaceous and early Tertiary and a relatively cooler climate from the Oligocene to the present day.
description: Supplement to: Meyer, Audrey W; Davies, Thomas A (1988): Clay mineralogy of sediments from the Galicia margin, ODP Leg 103. In: Boillot, G; Winterer, EL; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 103, 461-475
DOI: 10.1594/pangaea.263252
title: Minor-element chemical analyses of Hole 26-254
DOI: 10.1594/pangaea.263123
title: Minor-element chemical analyses of Hole 26-254
DOI: 10.1594/pangaea.263253
title: Minor-element chemical analyses of Hole 26-256
DOI: 10.1594/pangaea.263240
title: Minor-element chemical analyses of Hole 26-251A
DOI: 10.1594/pangaea.263254
title: Minor-element chemical analyses of Hole 26-257
DOI: 10.1594/pangaea.263241
title: Minor-element chemical analyses of Hole 26-253
DOI: 10.1594/pangaea.263242
title: Minor-element chemical analyses of Hole 26-254
DOI: 10.1594/pangaea.263243
title: Minor-element chemical analyses of Hole 26-256
DOI: 10.1594/pangaea.263239
title: Minor-element chemical analyses of Hole 26-250A
DOI: 10.1594/pangaea.263244
title: Minor-element chemical analyses of Hole 26-257
DOI: 10.1594/pangaea.249267
title: Planktic foraminifera abundance of Hole 26-251A

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.222047
title: Grain size analysis of Hole 26-255
DOI: 10.1594/pangaea.249268
title: Planktic foraminifera abundance of Hole 26-253

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.220145
title: Mineral composition of silt fraction from Hole 26-251A
DOI: 10.1594/pangaea.220517
title: Mineral composition of bulk sediment from Hole 26-250
DOI: 10.1594/pangaea.219846
title: Mineral composition of clay fraction from Hole 26-250
DOI: 10.1594/pangaea.220146
title: Mineral composition of silt fraction from Hole 26-252
DOI: 10.1594/pangaea.220149
title: Mineral composition of silt fraction from Hole 26-255
DOI: 10.1594/pangaea.220152
title: Mineral composition of silt fraction from Hole 26-258
DOI: 10.1594/pangaea.220519
title: Mineral composition of bulk sediment from Hole 26-251
DOI: 10.1594/pangaea.220520
title: Mineral composition of bulk sediment from Hole 26-251A
DOI: 10.1594/pangaea.220521
title: Mineral composition of bulk sediment from Hole 26-252
DOI: 10.1594/pangaea.220523
title: Mineral composition of bulk sediment from Hole 26-254
DOI: 10.1594/pangaea.219847
title: Mineral composition of clay fraction from Hole 26-250A
DOI: 10.1594/pangaea.219848
title: Mineral composition of clay fraction from Hole 26-251
DOI: 10.1594/pangaea.219850
title: Mineral composition of clay fraction from Hole 26-252
DOI: 10.1594/pangaea.222042
title: Grain size analysis of Hole 26-251
DOI: 10.1594/pangaea.220142
title: Mineral composition of silt fraction from Hole 26-250
DOI: 10.1594/pangaea.220144
title: Mineral composition of silt fraction from Hole 26-251
DOI: 10.1594/pangaea.222043
title: Grain size analysis of Hole 26-251A
DOI: 10.1594/pangaea.222044
title: Grain size analysis of Hole 26-252
DOI: 10.1594/pangaea.222046
title: Grain size analysis of Hole 26-254
DOI: 10.1594/pangaea.222049
title: Grain size analysis of Hole 26-257
DOI: 10.1594/pangaea.222050
title: Grain size analysis of Hole 26-258
DOI: 10.1594/pangaea.222784
title: Carbon analysis of Hole 26-250A
DOI: 10.1594/pangaea.222785
title: Carbon analysis of Hole 26-250
DOI: 10.1594/pangaea.222786
title: Carbon analysis of Hole 26-251A
DOI: 10.1594/pangaea.222787
title: Carbon analysis of Hole 26-251
DOI: 10.1594/pangaea.222788
title: Carbon analysis of Hole 26-252
DOI: 10.1594/pangaea.251428
title: Nannofossil abundance of Hole 26-250

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.250228
title: Pollen and spore abundance of Hole 26-254

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.251429
title: Nannofossil abundance of Hole 26-250A

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.251430
title: Nannofossil abundance of Hole 26-251

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.251431
title: Nannofossil abundance of Hole 26-251A

description: Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
DOI: 10.1594/pangaea.221275
title: Physical properties of Hole 26-252
DOI: 10.1594/pangaea.869206
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 26 (Sites 250A, 252, 256, 257)

description: DSDP Leg 26, is the fifth cruise of D/V Glomar Challenger in the Indian Ocean, and the first cruise of Phase III of the Deep Sea Drilling Project. The Indian Ocean is the smallest of the three major ocean basins but appears to be geologically the most complex. The sites drilled on Leg 26 were selected to try to elucidate a number of specific problems of both local and broad regional significance, as well as to add to the general knowledge of the area. In particular: a) To locate the oldest sediment in the Indian Ocean and thus possibly the date of the initial breakup of Gondwanaland (Sites 250, 256, 257); b) To determine the effects of the initiation of the Circumpolar Current on southern Indian Ocean sedimentation (Sites 250, 252, 256, 257, 258); c) To determine the history of spreading of the Southwest Branch of the Indian Ocean Ridge and the history of the crust and oceanic sedimentation in that general region (Sites 250, 251, 252).
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: Doyle, Patricia S; Boltovskoy, Esteban; Herb, Rene C; Thierstein, Hans R; Hyndman, Roy D; Horvath, George J; Leidy, Rosanne D; McKelvey, Barrie C; Kempe, D R C; Rodolfo, Kelvin S; Davies, Thomas A; Luyendyk, Bruce P (1974): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVI, 1129 pp
DOI: 10.15468/dl.cj2bj7
title: Occurrence Download

description: A dataset containing 113 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Etheostoma moorei Raney & Suttkus, 1964",
 "HasGeospatialIssue is false",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Living Specimen)"
 ]
 }
 }
 ]
}

 The dataset includes 113 records from 15 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0106957-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.rzwwa2
title: Occurrence Download

description: A dataset containing 1292 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Clinopodium macrostemum (Moc. & Sessé ex Benth.) Kuntze"
 ]
}

 The dataset includes 1292 records from 75 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0106959-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.