cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.879464
title: Annotated record of the detailed examination of Mn deposits from DOMES sites 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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.879674
title: Ultra-violet measurements from station Sioux Falls (2015-12)
DOI: 10.1594/pangaea.879683
title: Other measurements at 10 m from station Sioux Falls (2015-09)
DOI: 10.1594/pangaea.879685
title: Other measurements at 10 m from station Sioux Falls (2015-11)
DOI: 10.1594/pangaea.879316
title: Densities of benthic organisms close to the Fourcade glacier front at Potter Cove, South Shetland Islands, Antarctica, from December 2009 to February 2010
DOI: 10.1594/pangaea.879686
title: Other measurements at 10 m from station Sioux Falls (2015-12)
DOI: 10.1594/pangaea.879488
title: Daily mean stream temperatures at station Cabrillas, Central Spain
DOI: 10.1594/pangaea.879656
title: Annotated record of the detailed examination of Mn nodules from the Baja California Seamount Province

description: Internal growth features of manganese nodules reveal that many nodules are structurally, chemically, and mineralogically non-uniform, largely as a result of a complex growth history. If numerous investigators are to study the mineralogical and textural features of manganese nodules, the laboratories concerned must standardize procedures to some extent so that work is not duplicated and so that results can be compared fairly. In particular, we suggest that all investigators, for example, geochemists, mineralogists, and biologists who work with individual nodules, should pay due attention to the internal complexity of nodules while pursuing their individual specialized research. Detailed investigation of the relationships between the internal structure of manganese nodules and the mineralogy and chemical composition is essential to an understanding of nodule origin and of possible problems in economic use of nodules. Research of this kind is best controlled by use of good polished sections of whole manganese nodules.
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: Sorem, Ronald K; Foster, Allan R (1973): Mineralogical, chemical and optical procedures and standards for study of growth features and economic potential of manganese nodules. in: Phase I Report - Inter-University Program of Research on Ferromanganese Deposits of the Ocean Floor. Seabed Assessment Program, IDOE, NSF, Washington D.C., USA, 23-38
DOI: 10.1594/pangaea.879759
title: Annotated record of the detailed examination of manganese nodules from around the world oceans

description: Manganese nodules collected off Baja California have layers (zones) which are texturally and compositionally distinct. Massive and mottled zones consist mostly of cryptocrystalline todorokite and birnessite containing relatively high concentrations of Mn, Ni and Cu. Compact, columnar and laminated zones consist mostly of more iron- rich opaque amorphous material. Within these two groups the individual zones can be distinguished in part by their clay content. These results indicate that systematic research on nodule chemistry, mineralogy, growth rates and beneficiation should include careful analysis of individual layers within the nodules.
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: Sorem, Ronald K; Foster, Allan R (1972): Marine manganese nodules: importance of structural analysis. in: Proceedings of the the 24th International Geological Congress, Montreal, 192-200
DOI: 10.1594/pangaea.879490
title: Daily mean stream temperatures at station Cega2, Central Spain
DOI: 10.1594/pangaea.872721
title: (Supplement Table S4) Final ChRM of IODP Site 321-U1337
DOI: 10.1594/pangaea.879521
title: Basic measurements of radiation at station Sapporo (2017-06)
DOI: 10.1594/pangaea.872704
title: (Supplement Table S2) Paleomagnetic raw data of IODP Site 321-U1337
DOI: 10.1594/pangaea.877918
title: Simulated mean climate response to expanded Greenland Ice Sheet in the Kiel Climate Model

description: Proxy data suggest that the Plio-Pleistocene transition from ~3.2 - 3.0 to 2.5 Ma featured the onset of Northern Hemisphere glaciation and enhanced climate variability on obliquity timescale. Here, we investigate the influence of the expanding Greenland ice sheet (GrIS) on the mean climate and obliquity-related variability. Special attention is given to the Atlantic Meridional Overturning Circulation (AMOC). A series of climate model simulations suggest that the expanding GrIS weakens the AMOC by ~1 Sv, which is mainly due to reduced heat loss of the Greenland-Iceland-Norwegian Sea. Moreover, the expanded GrIS amplifies the Hadley circulation response to obliquity forcing. This drives enhanced obliquity-forced variations in freshwater export from the tropical Atlantic and in turn variations of the AMOC that increase by about a factor. The stronger AMOC response to obliquity forcing in turn drives a stronger global-mean near-surface temperature response. We conclude that the AMOC response to obliquity forcing is important to understand the enhanced climate variability on obliquity timescale during the Plio-Pleistocene transition.
description: Supplement to: Song, Zhaoyang; Latif, Mojib; Park, Wonsun (2017): Expanding Greenland Ice Sheet Enhances Sensitivity of Plio-Pleistocene Climate to Obliquity Forcing in the Kiel Climate Model. Geophysical Research Letters
DOI: 10.1594/pangaea.879827
title: Radiosonde measurements from station Tateno (2017-06)
DOI: 10.1594/pangaea.879832
title: Ultra-violet measurements from station Boulder, SURFRAD (2016-02)
DOI: 10.1594/pangaea.871248
title: Table S6 - ODP Site 208-1267 X-ray fluorescence Fe intensities
DOI: 10.1594/pangaea.871277
title: Table S7 - Calibration data for ODP Site 208-1267 X-ray fluorescence Fe intensities
DOI: 10.1594/pangaea.879833
title: Other measurements at 10 m from station Boulder, SURFRAD (2016-02)
DOI: 10.1594/pangaea.878089
title: Ultra-violet measurements from station Toravere (2017-06)
DOI: 10.1594/pangaea.879503
title: Daily mean stream temperatures at station Tagus-Peralejos, Central Spain
DOI: 10.1594/pangaea.879505
title: Daily mean stream temperatures at station Tormes1, Central Spain
DOI: 10.1594/pangaea.879841
title: Ultra-violet measurements from station Boulder, SURFRAD (2016-05)
DOI: 10.1594/pangaea.879843
title: Basic measurements of radiation at station Boulder, SURFRAD (2016-06)
DOI: 10.1594/pangaea.879243
title: Other measurements at 10 m from station Rock Springs (2015-02)
DOI: 10.1594/pangaea.879710
title: Illite content of sediment core M40/4_SL71
DOI: 10.1594/pangaea.879846
title: Basic measurements of radiation at station Boulder, SURFRAD (2016-07)
DOI: 10.1594/pangaea.879570
title: Closed versus total porosity for ice core B49, 73-90 m
DOI: 10.1594/pangaea.879853
title: Ultra-violet measurements from station Boulder, SURFRAD (2016-09)
DOI: 10.1594/pangaea.879571
title: Closed versus total porosity for ice core B53, 76-106 m, with cut-bubble effect
DOI: 10.1594/pangaea.871328
title: Table S22 - Paleomagnetic data interpretation from ODP Site 208-1263
DOI: 10.1594/pangaea.879572
title: Closed versus total porosity for ice core B53, 76-106 m
DOI: 10.1594/pangaea.879486
title: Daily mean stream temperatures at station Aravalle, Central Spain
DOI: 10.1594/pangaea.879575
title: Coordination number versus total porosity for ice core B53, 76-106 m
DOI: 10.1594/pangaea.871394
title: Table S36 - Mapping pairs for ODP Site 208-1262 to correlate intervals outside the splice to the splice
DOI: 10.1594/pangaea.871396
title: Table S38 - Mapping pairs for ODP Site 208-1265 to correlate intervals outside the splice to the splice
DOI: 10.1594/pangaea.879449
title: Radon 222 and meteorological time series at Jang Bogo Station, Antarctica, in 2015-2016
DOI: 10.1594/pangaea.879673
title: Ultra-violet measurements from station Sioux Falls (2015-11)
DOI: 10.1594/pangaea.879489
title: Daily mean stream temperatures at station Cega1, Central Spain
DOI: 10.1594/pangaea.879573
title: Closed versus total porosity for ice core RECAP_S2, 49-73 m
DOI: 10.1594/pangaea.879676
title: Other measurements at 10 m from station Sioux Falls (2015-02)
DOI: 10.1594/pangaea.879373
title: Table S48 - Comparison of durations of magnetochrons in million years including uncertainties in magnetic anomaly width
DOI: 10.1594/pangaea.879576
title: Coordination number versus total porosity for ice core RECAP_S2, 49-73 m
DOI: 10.1594/pangaea.879245
title: Ultra-violet measurements from station Rock Springs (2015-03)
DOI: 10.1594/pangaea.879491
title: Daily mean stream temperatures at station Cega3, Central Spain
DOI: 10.1594/pangaea.879677
title: Other measurements at 10 m from station Sioux Falls (2015-03)
DOI: 10.1594/pangaea.879493
title: Daily mean stream temperatures at station Cega5, Central Spain
DOI: 10.1594/pangaea.879684
title: Other measurements at 10 m from station Sioux Falls (2015-10)
DOI: 10.1594/pangaea.879249
title: Other measurements at 10 m from station Rock Springs (2015-04)
DOI: 10.1594/pangaea.879260
title: Ultra-violet measurements from station Rock Springs (2015-08)
DOI: 10.1594/pangaea.879589
title: Heavy mineral composition at site Byk_98_North_B-S
DOI: 10.1594/pangaea.879747
title: Carbon, nitrogen and hydrocarbons contents in soil after a diesel spill at Carlini Base, King George Island (Isla 25 de Mayo)
DOI: 10.1594/pangaea.879157
title: Radiosonde measurements from station Kwajalein (2017-04)
DOI: 10.1594/pangaea.879496
title: Daily mean stream temperatures at station Gallo, Central Spain
DOI: 10.1594/pangaea.879161
title: Radiosonde measurements from station Kwajalein (2017-06)
DOI: 10.1594/pangaea.879497
title: Daily mean stream temperatures at station Gredos_Gorge, Central Spain
DOI: 10.1594/pangaea.879831
title: Basic measurements of radiation at station Boulder, SURFRAD (2016-02)
DOI: 10.1594/pangaea.879835
title: Ultra-violet measurements from station Boulder, SURFRAD (2016-03)
DOI: 10.1594/pangaea.880277
title: Ultra-violet measurements from station Fort Peck (2016-08)
DOI: 10.1594/pangaea.880772
title: Simulation of benthic δ¹⁸O, CO2, ice-volume-equivalent sea level and temperature over the past 38 million years

description: Model output of a coupled ice sheet-climate model, inversely forced by benthic d18O over the past 38 million years. Sheet 1 contains the main results from the reference simulation: benthic d18O, CO2, ice-volume-equivalent sea level and global temperature. Sheet 2 contains global, Northern Hemisphere (40-80 deg N), and Antarctic (60-90 deg S) temperatures, from the reference run and the run with ice uncoupled, only albedo coupled, and only surface height coupled. Sheet 3 contains global temperature, from the reference run, and the runs with fixed PD ice, fixed LGM ice, and no ice. Details are given in the publication. More information or data can be obtained by contacting L.B. Stap (lennert.stap@awi.de).
description: Supplement to: Stap, Lennert Bastiaan; van de Wal, Roderik S W; de Boer, Bas; Bintanja, Richard; Lourens, Lucas Joost (2017): The influence of ice sheets on temperature during the past 38 million years inferred from a one-dimensional ice sheet-climate model. Climate of the Past, 13(9), 1243-1257
DOI: 10.1594/pangaea.879838
title: Ultra-violet measurements from station Boulder, SURFRAD (2016-04)
DOI: 10.1594/pangaea.879840
title: Basic measurements of radiation at station Boulder, SURFRAD (2016-05)
DOI: 10.1594/pangaea.879842
title: Other measurements at 10 m from station Boulder, SURFRAD (2016-05)
DOI: 10.1594/pangaea.879848
title: Other measurements at 10 m from station Boulder, SURFRAD (2016-07)
DOI: 10.1594/pangaea.879849
title: Basic measurements of radiation at station Boulder, SURFRAD (2016-08)
DOI: 10.1594/pangaea.879850
title: Ultra-violet measurements from station Boulder, SURFRAD (2016-08)
DOI: 10.1594/pangaea.880283
title: Other measurements at 10 m from station Fort Peck (2016-09)
DOI: 10.6084/m9.figshare.26342293
title: OsMADS20.pro

description: OsMADS20 protein sequence
DOI: 10.6084/m9.figshare.26342293.v2
title: OsMADS20.pro

description: OsMADS20 protein sequence
DOI: 10.1594/pangaea.879255
title: Other measurements at 10 m from station Rock Springs (2015-06)
DOI: 10.6084/m9.figshare.26342293.v1
title: OsMADS20.pro

description: OsMADS20 protein sequence
DOI: 10.1594/pangaea.879851
title: Other measurements at 10 m from station Boulder, SURFRAD (2016-08)
DOI: 10.1594/pangaea.879858
title: Basic measurements of radiation at station Boulder, SURFRAD (2016-11)
DOI: 10.1594/pangaea.879264
title: Other measurements at 10 m from station Rock Springs (2015-09)
DOI: 10.1594/pangaea.880286
title: Ultra-violet measurements from station Fort Peck (2016-10)
DOI: 10.1594/pangaea.880490
title: Basic measurements of radiation at station Sapporo (2017-07)
DOI: 10.1594/pangaea.880372
title: Clay components mineralogy and smears slides analysis for the cores of DOMES Site C, Pacific Ocean

description: DOMES area C sediment is quite heterogeneous, but most commonly is classified as mud (clay minerals, quartz, and feldspar) or siliceous ooze. However, in several samples Fe-Mn micronodules, globules and aggreqates are the major sediment components. Calcareous nannofossil ooze characterized only one sample, core 18A-1-8 and calcite (reworked limestone?) is present in several other cores, but never as a major compoment. Volcanic ash (glassy mud) is the major sediment type in several cores.
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: Hein, James R; Gutmacher, Christina; Miller, Jacquelyn (1976): DOMES Area C, General statement about mineralogy, diagenesis and sediment classification. in: Deep Ocean Mining Environmental Study, N.E. Pacific Nodule Province, Site C, Geology and Geochemistry, U.S. Geological Survey Open File Report. U.S. Geological Survey, 63-80
DOI: 10.1594/pangaea.879861
title: Basic measurements of radiation at station Boulder, SURFRAD (2016-12)
DOI: 10.1594/pangaea.879862
title: Ultra-violet measurements from station Boulder, SURFRAD (2016-12)
DOI: 10.1594/pangaea.879273
title: Other measurements at 10 m from station Rock Springs (2015-12)
DOI: 10.1594/pangaea.880187
title: Ultra-violet measurements from station Desert Rock (2016-03)
DOI: 10.1594/pangaea.880289
title: Ultra-violet measurements from station Fort Peck (2016-11)
DOI: 10.1594/pangaea.880188
title: Other measurements at 10 m from station Desert Rock (2016-03)
DOI: 10.1594/pangaea.879863
title: Other measurements at 10 m from station Boulder, SURFRAD (2016-12)
DOI: 10.1594/pangaea.880290
title: Other measurements at 10 m from station Fort Peck (2016-11)
DOI: 10.1594/pangaea.879761
title: COSMOS model Late Cretaceous surface temperature results with different CO2 levels and gateway configurations in NetCDF format
DOI: 10.1594/pangaea.880191
title: Other measurements at 10 m from station Desert Rock (2016-04)
DOI: 10.1594/pangaea.880311
title: Major, trace and rare earth elements geochemistry of manganese nodules from the DOMES, Site A area in the Pacific Ocean

description: The distribution of rare earth elements (REE) in ferromanganese nodules from DOMES Site A has been determined by instrumental neutron activation methods. The concentrations of the REE vary markedly. Low concentrations characterize samples from a depression (the valley), in which Quaternary sediments are thin or absent; high concentrations are found in samples from the surrounding abyssal hills (the highlands) where the Quaternary sediment section is relatively thick. Moreover, the valley nodules are strongly depleted in the light trivalent REE (LREE) and Ce compared with nodules from the highlands, some of the former showing negative Ce anomalies. The REE abundances in the nodules are strongly influenced by the REE abundances in coexisting bottom water. Some controls on the REE chemistry of bottom waters include: a) the more effective removal of the LREE relative to the HREE from seawater because of the greater degree of complexation of the latter elements with seawater ligands, b) the very efficient oxidative scavenging of Ce on particle surfaces in seawater, and c) the strong depletion of both Ce and the LREE in, or a larger benthic flux of the HREE into, the Antarctic Bottom Water (AABW) which flows through the valley. The distinctive REE chemistry of valley nodules is a function of their growth from geochemically evolved AABW. In contrast, the REE chemistry of highland nodules indicates growth from a local, less evolved seawater source.
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: Calvert, Stephen E; Piper, David Z; Baedecker, Philip A (1987): Geochemistry of the rare earth elements in ferromanganese nodules from DOMES Site A, northern equatorial Pacific. Geochimica et Cosmochimica Acta, 51(9), 2331-2338
DOI: 10.1594/pangaea.879885
title: Ultra-violet measurements from station Bondville (2016-02)
DOI: 10.1594/pangaea.879907
title: Ultra-violet measurements from station Bondville (2016-06)
DOI: 10.1594/pangaea.880434
title: Annotated record of the detailed examination of Mn deposits observed during a Continuous Line Bucket test done off the Tuamotu Archipelago

description: Testing of a continuous bucket-line dredging system was carried out in the South Pacific August 23 through September 14, 1970 by Japan Resources Association aboard the vessel "Chiyoda Maru No. 2". Fifteen dredge stations were occupied, and the system was tested at depths of 1080, 3755, and 1220 meters. The system is designed to recover manganese nodules, and the tests helped to verify its feasibility. A brief discussion of the merits of the continuous bucket-line compared to other continuous systems is made.
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: Masuda, Yoshio; Cruickshank, Michael J; Mero, John L (1971): Continuous Bucket-Line Dredging at 12,000 Feet. Proceedings of the 3rd Annual Offshore Technology Conference, OTC1410, 22 pp
DOI: 10.1594/pangaea.879888
title: Ultra-violet measurements from station Bondville (2016-03)
DOI: 10.1594/pangaea.880205
title: Other measurements at 10 m from station Desert Rock (2016-05)
DOI: 10.1594/pangaea.879905
title: Other measurements at 10 m from station Bondville (2016-05)
DOI: 10.1594/pangaea.840609
title: Grain size composition of sediment core MD99-2303
DOI: 10.1594/pangaea.880358
title: Ultra-violet measurements from station Toravere (2017-07)
DOI: 10.1594/pangaea.879924
title: Other measurements at 10 m from station Bondville (2016-07)
DOI: 10.1594/pangaea.879929
title: Other measurements at 10 m from station Bondville (2016-08)
DOI: 10.1594/pangaea.879185
title: Radiosonde measurements from station South Pole (2017-05)

description: Start location: Amundsen-Scott Station; Distance from radiation site: 1 km
DOI: 10.1594/pangaea.879934
title: Ultra-violet measurements from station Bondville (2016-10)
DOI: 10.1594/pangaea.880411
title: Ultra-violet measurements from station Goodwin Creek (2016-05)
DOI: 10.1594/pangaea.879931
title: Ultra-violet measurements from station Bondville (2016-09)
DOI: 10.1594/pangaea.880217
title: Other measurements at 10 m from station Desert Rock (2016-09)
DOI: 10.1594/pangaea.880412
title: Other measurements at 10 m from station Goodwin Creek (2016-05)
DOI: 10.1594/pangaea.879251
title: Ultra-violet measurements from station Rock Springs (2015-05)
DOI: 10.1594/pangaea.880415
title: Other measurements at 10 m from station Goodwin Creek (2016-06)
DOI: 10.1594/pangaea.879935
title: Other measurements at 10 m from station Bondville (2016-10)
DOI: 10.1594/pangaea.880219
title: Ultra-violet measurements from station Desert Rock (2016-10)
DOI: 10.1594/pangaea.879254
title: Ultra-violet measurements from station Rock Springs (2015-06)
DOI: 10.1594/pangaea.879937
title: Ultra-violet measurements from station Bondville (2016-11)
DOI: 10.1594/pangaea.879671
title: Ultra-violet measurements from station Sioux Falls (2015-09)
DOI: 10.1594/pangaea.880418
title: Other measurements at 10 m from station Goodwin Creek (2016-07)
DOI: 10.1594/pangaea.879258
title: Other measurements at 10 m from station Rock Springs (2015-07)
DOI: 10.1594/pangaea.880423
title: Ultra-violet measurements from station Goodwin Creek (2016-09)
DOI: 10.1594/pangaea.879450
title: Radon 222 and meteorological time series at King Sejong Station, Antarctica, in 2015-2016
DOI: 10.1594/pangaea.880430
title: Other measurements at 10 m from station Goodwin Creek (2016-11)
DOI: 10.1594/pangaea.880220
title: Other measurements at 10 m from station Desert Rock (2016-10)