cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.893265
title: Influence of past archipelago configuration on present-day insular biodiversity patterns

description: Aim: To quantify the influence of past archipelago configuration on present-day insular biodiversity patterns, and to compare the role of long-lasting archipelago configurations over the Pleistocene to configurations of short duration such as at the Last Glacial Maximum (LGM) and the present-day. Location: 53 volcanic oceanic islands from 12 archipelagos worldwide - Azores, Canary Islands, Cook Islands, Galápagos, Gulf of Guinea, Hawaii, Madeira, Mascarenes, Pitcairn, Revillagigedo, Samoan Islands, and Tristan da Cunha. Time period: The last 800 Kyr, representing the nine most recent glacial-interglacial cycles. Major taxa studied: Land snails and angiosperms. Methods: Species richness data for land snails and angiosperms were compiled from existing literature and species checklists. We reconstructed archipelago configurations at the following sea-levels: the present-day high interglacial sea-level, the intermediate sea-levels that are representative of the Pleistocene, and the low sea-levels of the LGM. We fitted two alternative linear mixed models for each archipelago configuration on the number of single-island endemic, multiple-island endemic, and native non-endemic species. Model performance was assessed based on the goodness-of-fit of the full model, the variance explained by archipelago configuration, and model parsimony. Results: Single-island endemic richness in both taxonomic groups was best explained by intermediate palaeo-configuration (positively by area change, and negatively by palaeo-connectedness), whereas non-endemic native species richness was poorly explained by palaeo-configuration. Single-island endemic richness was better explained by intermediate archipelago configurations than by the archipelago configurations of the LGM or present-day. Main conclusions: Archipelago configurations at intermediate sea-levels - which are representative of the Pleistocene - have left a stronger imprint on single-island endemic richness patterns on volcanic oceanic islands than extreme archipelago configurations that persisted for only a few thousand years (such as the LGM). In understanding ecological and evolutionary dynamics of insular biota it is essential to consider longer-lasting environmental conditions, rather than extreme situations alone.
description: Supplement to: Norder, Sietze Johannes; Proios, Kostas V; Whittaker, Robert J; Alonso, María R; Borges, Paulo A V; Borregaard, Michael K; Cowie, Robert H; Florens, F B Vincent; de Frias Martins, António M; Ibáñez, Miguel; Kissling, W Daniel; de Nascimento, Lea; Otto, Rüdiger; Parent, Christine E; Rigal, François; Warren, Ben H; Fernández-Palacios, José María; van Loon, E Emiel; Triantis, Kostas A; Rijsdijk, Kenneth F (2018): Beyond the Last Glacial Maximum: Island endemism is best explained by long-lasting archipelago configurations. Global Ecology and Biogeography
DOI: 10.1594/pangaea.895810
title: (Table S2) Data for compositional traverses perpendicular to olivine rims, and results of diffusion modelling

description: C0 and C1 are the compositions of olivine cores and rims, respectively, for the one-dimensional diffusion model.Dt is calculated from the best-fit of an analyzed traverse by an error function; L is the profile length calculated as L = 4*sqrt(Dt);t is the calculated diffusion time using a diffusion coefficient of 1.6*10-17 m2s-1.
DOI: 10.1594/pangaea.764310
title: (Table 1) Upper Carboniferous spores abundances from ODP Holes 172-1062B, 172-1063A and 172-1063B

description: Color variations were interpreted in paleoceanographic terms for the late Pliocene-Pleistocene sediments recovered by ODP Leg 172 on deep-sea drifts at Blake-Bahama Outer Ridge and northeastern Bermuda Rise. The color-derived parameters used in interpretation included predicted carbonate content, terrigenous fluxes, and hematite content. Abundance of Upper Carboniferous spores indicates that the hematite is probably derived from the Permo-Carboniferous red beds of the Canadian Maritimes. In the last 800 kyr sedimentation pattern changes on the Blake-Bahama Outer Ridge were determined by the sediment delivery to the deep basin as well as circulation changes. Sediment delivery increased during glacials (especially during the last 500 kyr and particularly since Stage 6). A fundamental change in the thermohaline circulation occurred at about 500 ka corresponding to the end of the Mid-Pleistocene Transition period at the onset of the predominant 100-kyr climate cyclicity. Sedimentation related to WBUC had intensified at that time and had become more focused at depths below 3000 m. Changes in hematite content and sedimentation rate show a pulse of sediment via the St. Lawrence outlet at the Pliocene-Pleistocene boundary suggesting that a likely change in the hydrography/physiography of the Laurentide Ice Sheet could have been involved in the climatic and ocean circulation changes at that time.
description: Supplement to: Giosan, Liviu; Flood, Roger D; Gruetzner, Jens; Mudie, Peta J (2002): Paleoceanographic significance of sediment color on western North Atlantic Drifts: II. Late Pliocene-Pleistocene sedimentation. Marine Geology, 189(1-2), 43-61
DOI: 10.1594/pangaea.837494
title: (Table 2) Spore density, diversity and evenness of different arbuscular mycorrhizal fungi morphotaxa 29 months after experimental removal of plant functional types, central Argentina

description: Treatments were applied in November/December 1998. Density is given per kg dry weight. Data was originally given in #/100 g soil dry weight but was converted to #/kg by multiplying by 10.
DOI: 10.1594/pangaea.774624
title: (Table T1) Composition of clay minerals from ODP Leg 204 sediments

description: This report describes the results of semiquantitative analysis of clay mineral composition by X-ray diffraction. The samples consist of hemipelagic mud and mudstone cored from Hydrate Ridge during Leg 204 of the Ocean Drilling Program. We analyzed oriented aggregates of the clay-sized fractions (&lt;2 µm) to estimate relative percentages of smectite, illite, and chlorite (+ kaolinite). For the most part, stratigraphic variations in clay mineral composition are modest and there are no significant differences among the seven sites that were included in the study. On average, early Pleistocene to Holocene trench slope and slope basin deposits contain 29% smectite, 31% illite, and 40% chlorite (+ kaolinite). Late Pliocene to early Pleistocene strata from the underlying accretionary prism contain moderately larger proportions of smectite with average values of 38% smectite, 27% illite, and 35% chlorite (+ kaolinite). There is no evidence of clay mineral diagenesis at the depths sampled. The expandability of smectite is, on average, equal to 64%, and there are no systematic variations in expandability as a function of burial depth or depositional age. The absence of clay mineral diagenesis is consistent with the relatively shallow sample depths and corresponding maximum temperatures of only 24°-33°C.
DOI: 10.1594/pangaea.847425
title: (Table S3) Geochemical analysis of Site 3, Omkyk

description: highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyrite).
DOI: 10.1594/pangaea.778257
title: (Table T1) Paleomagnetic characterization of sedimentary rocks from ODP Hole 198-1213B

description: Coring in Hole 1213B on the south flank of Shatsky Rise recovered sedimentary rocks (chalk and claystone) of earliest Cretaceous (Berriasian) age. Because few samples of this age are available for the Pacific plate, this recovery provides an opportunity to use paleomagnetism to determine a value for the paleolatitude of the site and of the Pacific plate for Berriasian time. A total of 22 vertically oriented samples were measured, yielding consistent alternating-field demagnetization results and low paleoinclination values consistent with magnetization near the equator. Samples can be grouped by inclination sign to produce a magnetic stratigraphy. If negative inclinations are assumed to represent reversed polarity (i.e., the site was magnetized north of the equator), the result is consistent with the Berriasian reversal timescale, which contains more reversed polarity (Chrons M16r-M18r) than normal polarity. Likewise, the assumption of a Northern Hemisphere magnetization produces a paleoinclination (9.1° + 13.6°/-14.2°; N = 17) and paleolatitude (4.6° + 7.2°/-6.9°) that is consistent with independent Pacific paleomagnetic data of Late Jurassic and Early Cretaceous age. This paleolatitude implies that the Pacific Apparent Polar Wander Path trends southward from this time until the mid-Cretaceous.
description: Supplement to: Sager, William W; Evans, Helen F; Channell, James E T (2005): Paleomagnetism of Early Cretaceous (Berriasian) sedimentary rocks, Hole 1213B, Shatsky Rise. In: Bralower, TJ; Premoli Silva, I; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 198, 1-14
DOI: 10.1594/pangaea.896231
title: CICE output from Navy Earth System Model (NESM) for 2018111712

description: INITIALIZATION: 2018111712FORECASTS:daily at 00Z out to 45 days (t1068)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.780486
title: (Table T2) Biogenic silica content of ODP Site 188-1165 sediments
DOI: 10.1594/pangaea.887962
title: Description of lithologic units (VCD) from IODP Hole 370-C0023A
DOI: 10.1594/pangaea.847428
title: (Table S5) Geochemical analysis of Site 4, Driedoornvlagte
DOI: 10.1594/pangaea.896232
title: CICE output from Navy Earth System Model (NESM) for 2018111812

description: INITIALIZATION: 2018111812FORECASTS:daily at 00Z out to 45 days (t1068)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.895936
title: (Table S1a) Clinopyroxene phenocryst rims, group 1 composition (average of up to 6 single analyses) and thermobarometers applied to rim and host groundmass compositions
DOI: 10.1594/pangaea.896234
title: CICE output from Navy Earth System Model (NESM) for 2018112012

description: INITIALIZATION: 2018112012FORECASTS:daily at 00Z out to 45 days (t1068)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.780489
title: (Table T7) Age-depth tie points for ODP Site 188-1165 sediments
DOI: 10.1594/pangaea.896259
title: Ultra-violet measurements from station Carpentras (2018-08)
DOI: 10.1594/pangaea.788194
title: (Table T8) Minor element concentration of ODP Hole 171B-1049C sediments
DOI: 10.1594/pangaea.895937
title: (Table S1b) Clinopyroxene phenocryst cores, group 1 composition (average of up to 37 single analyses) and thermobarometers applied to core and host groundmass compositions
DOI: 10.1594/pangaea.847481
title: (Table S6) Geochemical analysis of Site 5, Brak

description: highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyrite).
DOI: 10.1594/pangaea.895938
title: (Table S1c) Clinopyroxene phenocryst cores, group 2 or transitional composition (average of up to 28 single analyses) and thermobarometers applied to core compositions and average corrected olivine-hosted melt inclusions
DOI: 10.1594/pangaea.889720
title: Liquid from core liner gas chemistry of IODP Hole 370-C0023A
DOI: 10.1594/pangaea.895939
title: (Table S1d) Clinopyroxene cumulus crystal rims, group 1 composition (average of up to 3 single analyses) and thermobarometers applied to rim and host groundmass compositions
DOI: 10.1594/pangaea.787914
title: (Table T1-2) Proportion of ferrous and ferric iron in ODP Hole 172-1062A sediments

description: Changes in bulk sediment Fe(II)/Fe(III) ratio and in the distribution of iron among different minerals as a result of Ocean Drilling Program archive storage in the Bremen Core Repository were investigated using Mössbauer spectroscopy. Massive Fe(II) to Fe(III) oxidation, which involved between 24% and 45% of the initial Fe(II), occurred within only 6 months of refrigerated storage. Prior to archive storage, &gt;95% of the Fe(II) in the sediment samples under investigation was structural iron in silicate minerals. Hence, virtually the entire oxidation process took place within silicate mineral lattices, and the sediment mineral assemblage was not changed in this case. Nevertheless, the observed oxidation of the comparatively shielded silicate lattice Fe(II) suggests that Fe(II) bound in authigenic carbonates, phosphates, or sulfides - such as that found in many marine sediments - would likely be oxidized at least as fast. Those minerals, however, would be replaced by Fe(III)-bearing oxides and oxyhydroxides, which implies a change of sediment composition, and thus, of various sediment properties, including the magnetic signal, within a few months of storage.Furthermore, changes in the silicate lattice Fe(II)/Fe(III) ratio during storage, such as those reported here, also signify loss of information. This is because oxidation of the structural Fe(II) upon contact with atmospheric oxygen may occur only inasmuch as the inverse Fe(III)-Fe(II) redox transition has taken place in the seabed. Therefore, the reversible shift, if it were measured under controlled reoxidation in the laboratory, may suggest the chemical stress that was suffered by the iron oxide minerals at the ocean bottom. Concerning Site 1062, this process might help to judge both the authenticity of magnetic field excursion records and the lithostratigraphic value of red lutites at given sediment depths. Although the nature and extent of information loss or alteration during storage depend on sediment type, the reported observations emphasize the need for special sample protection with respect to properties that might be affected.
description: Supplement to: König, Iris; Lougear, A; Bruns, P; Gruetzner, Jens; Trautwein, Alfred X; Dullo, Wolf-Christian (2000): Iron oxidation in sediment cores (Site 1062) during six months of storage in the Ocean Drilling Program archive. In: Keigwin, LD; Rio, D; Acton, GD; Arnold, E (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 172, 1-11
DOI: 10.1594/pangaea.788195
title: (Table T9) Elemental abundances normalized against aluminium abundance of ODP Hole 171B-1049C sediments
DOI: 10.1594/pangaea.818211
title: Chronostratigraphy for MIS 1-2 and MIS 5 of ODP Hole 172-1058C

description: DEPTH, sediment/rock = Depth (mcd)
DOI: 10.1594/pangaea.847482
title: (Table S7A) Geochemical analysis of Site 6, Arasab: Carbonates

description: highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyrite).
DOI: 10.1594/pangaea.896242
title: Raw measurement data of ice core DomeC, Core 2
DOI: 10.1594/pangaea.847484
title: (Table S8) Geochemical analysis of Site 7, Grens

description: highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyrite).
DOI: 10.1594/pangaea.847485
title: (Table S9A) Geochemical analysis of Site 8, Pinnacle Reefs: carbonates

description: highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyrite).
DOI: 10.1594/pangaea.895940
title: (Table S1e) Clinopyroxene cumulus crystal cores, group 1 composition (average of up to 36 single analyses) and thermobarometers applied to core and host groundmass compositions
DOI: 10.1594/pangaea.896243
title: Raw measurement data of ice core DomeC, Core 3
DOI: 10.1594/pangaea.847486
title: (Table S9B) Geochemical analysis of Site 8, Pinnacle Reefs: shales

description: highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyrite).
DOI: 10.1594/pangaea.895941
title: (Table S1f) Orthopyroxene phenocryst rims (average of up to 8 single analyses) and thermobarometers applied to rim and host groundmass compositions
DOI: 10.1594/pangaea.895943
title: (Table S1g) Plagioclase phenocryst and cumulus crystal rims (single analyses or average of 2 analyses) and thermobarometers applied to rim and host groundmass compositions
DOI: 10.1594/pangaea.895946
title: (Table S1i) Spinel inclusions in olivine phenocrysts (average of up to 14 analyses), and Fo% of host olivine
DOI: 10.1594/pangaea.818233
title: Mg/Ca-temperatures of planktonic foraminifer Globorotalia truncatulinoides sinistral from ODP Hole 172-1058C

description: DEPTH, sediment/rock = Depth (mcd)
DOI: 10.1594/pangaea.896244
title: Raw measurement data of ice core DomeC, Core 4
DOI: 10.1594/pangaea.896245
title: Raw measurement data of ice core DomeC, Core 5
DOI: 10.1594/pangaea.896257
title: Basic measurements of radiation at station Carpentras (2018-08)
DOI: 10.1594/pangaea.896334
title: Phytoplankton Composition in the KOSMOS Experiment Bergen 2015

description: Treatment: high = pCO2 aiming at 2000 µatm
DOI: 10.1594/pangaea.896336
title: Fatty acid Composition in the KOSMOS Experiment Bergen 2015

description: Treatment: high = pCO2 aiming at 2000 µatm
DOI: 10.1594/pangaea.896338
title: CICE output from Navy Earth System Model (NESM) for 2018112412

description: INITIALIZATION: 2018112412FORECASTS:daily at 00Z out to 45 days (t1068)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.896339
title: CICE output from Navy Earth System Model (NESM) for 2018112512

description: INITIALIZATION: 2018112512FORECASTS:daily at 00Z out to 45 days (t1068)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.896340
title: CICE output from Navy Earth System Model (NESM) for 2018112612

description: INITIALIZATION: 2018112612FORECASTS:daily at 00Z out to 45 days (t1068)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.896341
title: CICE output from Navy Earth System Model (NESM) for 2018112712

description: INITIALIZATION: 2018112712FORECASTS:daily at 00Z out to 45 days (t1068)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.711569
title: Ozone measurements from station Tamanrasset (2008-04)
DOI: 10.1594/pangaea.817936
title: (Table 2) Bacterial abundance, carbon production and respiration in samples obtained during a CCGS Amundsen cruise in 2008

description: Averages of stations depicted in Table 1. Respiration parameter all Q10 corrected. Potential and specific bacterial respiration and respiration rate based on the equation BR = 0.45CR**0.93 (Robinson 2008).
DOI: 10.1594/pangaea.896313
title: Air temperature data from the Serra da Estrela (Central Portugal) from January to December 2000, station Alto da Pedrice
DOI: 10.1594/pangaea.788196
title: (Table T10) Elemental ratios, biogenic barium and phosphorus excess of ODP Hole 171B-1049C sediments
DOI: 10.1594/pangaea.896347
title: Ultra-violet measurements from station Toravere (2018-10)
DOI: 10.1594/pangaea.896314
title: Air temperature data from the Serra da Estrela (Central Portugal) from January to December 2000, station Candieira
DOI: 10.1594/pangaea.896315
title: Air temperature data from the Serra da Estrela (Central Portugal) from January to December 2000, station Cantaro Gordo
DOI: 10.1594/pangaea.896349
title: Ultra-violet measurements from station Payerne (2015-01)
DOI: 10.1594/pangaea.896316
title: Air temperature data from the Serra da Estrela (Central Portugal) from January to December 2000, station Curral Nave
DOI: 10.1594/pangaea.896350
title: Meteorological synoptical observations from station Payerne (2015-01)