cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.792648
title: (Appendix A2) Paleomagnetic of ODP Hole 172-1062D

description: DEPTH, sediment [m] is given in mbsf.
DOI: 10.1594/pangaea.749396
title: Meteorological observations during General Elliot cruise from Downs to Bombay started at 1789-03-24
DOI: 10.1594/pangaea.511369
title: Miocene macroflora of Akmola (Kazakhstan)
DOI: 10.1594/pangaea.786705
title: (Appendix) Carbon and nitrogen isotope ratios of ODP Site 160-964

description: Nitrogen isotopes of chlorins, degradation products of chlorophyll, reflect the isotopic composition of nutrient N utilized by marine phytoplankton communities. Here we show that in sediments of the eastern Mediterranean Pleistocene and Holocene, values of d15N for chlorins and total nitrogen vary in concert, with a consistent offset of ~5 per mil reflecting the fractionation imparted during chlorophyll biosynthesis. Samples from the Integrated Ocean Drilling Program Sites 964 and 969 were analyzed at a sampling resolution of ~4-10 cm, clustered around sapropel events 2, 3, 4 and 5 (~100-170 ka). In low organic content sediments, chlorin values of ~0 per mil coincident with total nitrogen values of ~+ 5 per mil indicate that the latter reflects the original biomass and is not a consequence of diagenetic isotope enrichment. In sapropel horizons, the chlorin and total nitrogen values are 5 per mil more negative (~-5 per mil and ~ 0 per mil, respectively), resembling previously-reported, modern-day water-column particulates (~0 per mil). We suggest that nutrient conditions in the Eastern Mediterranean correspond to three scenarios and that the similarity between sapropel and modern-day bulk d15N is coincidental. Organic-poor marl sediments formed under oligotrophic conditions where surface productivity resulted from upwelling of Atlantic-sourced nitrate. Sapropels were characterized by enhanced diazotrophy that was likely fueled by increased riverine P fluxes to surface waters. Present-day conditions are dominated by anthropogenic N sources. These scenarios agree with a model of sapropel formation in which stratification caused by increased fresh-water inputs led to N fixation due to P:N nutrient imbalance. Enhanced production combined with stratification promoted and maintained anoxic deep waters, consequently increasing organic matter preservation. Such a model may be relevant to interpreting other episodes of intense organic matter deposition in past oceans.
description: Supplement to: Higgins, Meytal B; Robinson, Rebecca S; Carter, Susan J; Pearson, Ann (2010): Evidence from chlorin nitrogen isotopes for alternating nutrient regimes in the Eastern Mediterranean Sea. Earth and Planetary Science Letters, 290(1-2), 102-107
DOI: 10.1594/pangaea.788832
title: Basic and other measurements of radiation at station Alert (2010-12)
DOI: 10.1594/pangaea.775266
title: Visual core description (VCD) from IODP Hole 322-C0012A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.788715
title: (Table 3D) DSDP Site 82-563 age from model 2
DOI: 10.1594/pangaea.878180
title: Earlywood width of Pinus sylvestris at site SJU
DOI: 10.1594/pangaea.787949
title: (Table T5) Anisotropy of magnetic susceptibility for ODP Site 172-1057

description: DEPTH, sediment is given in mbsf.
DOI: 10.1594/pangaea.747705
title: (Table 3) Abundance distribution of the 'clavate' subspecies of the genus Globigerinelloides and Pseudoschackoina saundersi in the upper part of the Cismon core

description: Frequency classes (washed samples), vr, very rare (1 specimen); r, rare (2-3 specimens); r/f, rare to few (4-5 specimens); f, few (6-8 specimens); f/c, few to common (9-12 specimens); c, common (13-16 specimens); c/a, common to abundant (17-20 specimens); a, abundant (21-25 specimens); va, very abundant (&gt;25 specimens); x occurrence in thin section. - = absent. Depth, sediment is meters below well head.
DOI: 10.1594/pangaea.892274
title: Simulated net primary productivity (NPP) in the southern North Sea 2003-2013 for a simulation with and without consideration of benthic filtration by Mytilus edulis

description: Blue mussels filter water and transport material to the ocean floor. I investigate with a computer model the effect of such filtration and transport in the southern North Sea and find that up to 10% of the net annually produced biomass is filtered. This effect is not the same everywhere: near-shore, it is up to 50% and it is negligible offshore. Considering filtration is important for understanding the spatial patterns of coastal ecosystems.
description: The data set contains spatially resolved annual values of net primary production (NPP) for the years 2003-2013 for two scenarios from simulations that include the ecosystem model MAECS (Model for Adaptive Ecosystems in Coastal Seas), the hydrodynamic model GETM (General Estuarine Transport Model), the biochemical model OMEXDia (Ocean Margin Experiment Diagenesis) and reconstructed blue mussel distribution, all coupled through MOSSCO (Modular System for Shelves and Coasts). Besides the reference scenario (REF), a NONE scenario evaluates the ecosystem without the presence of filter feeders.
description: Supplement to: Lemmen, Carsten (2018): North Sea ecosystem-scale model-based quantification of net primary productivity changes by the benthic filter feeder Mytilus edulis. Water, 10(11), 1527
DOI: 10.1594/pangaea.747968
title: Meteorological observations during CRESCENT cruise from Table Bay to Spithead started at 1798-03-15
DOI: 10.1594/pangaea.701029
title: Monthly landings of marine products, Region VI, Chile, 2002
DOI: 10.1594/pangaea.898440
title: Other measurements at 10 m from station Bondville (2017-11)
DOI: 10.1594/pangaea.898451
title: Radiosonde measurements from station Bondville (2018-02)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.619072
title: Soil temperature and soil moisture at different sites during expedition LENA 2002 (Table A 5.2.4)
DOI: 10.1594/pangaea.477142
title: Hydrochemistry measured on water bottle samples at station NPac_1974_RY_136E/4470

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.758238
title: (Table 5) Distribution of Neogene planktonic foraminifers in sediments of ODP Hole 115-707A

description: Abundances: planktonic foraminifera x = occurrence, / extremely rare or presents some taxonomic ambiguity. Components other than planktonic foraminifera: R = rare, F = few, C = common, A = abundant. - = not observed.
DOI: 10.1594/pangaea.898442
title: Ultra-violet measurements from station Bondville (2017-12)
DOI: 10.1594/pangaea.677991
title: Expanded measurements from Neumayer Station (2000-02)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.750581
title: Meteorological observations during MAGDALENA cruise from Batavia to London started at 1852-08-22
DOI: 10.1594/pangaea.716630
title: Radiosonde measurements from Neumayer Station (2008-08)
DOI: 10.1594/pangaea.898450
title: Ultra-violet measurements from station Bondville (2018-02)
DOI: 10.1594/pangaea.869948
title: 10Be measured on Akademii Nauk ice core, Russian Arctic, for the period 1590-1950 CE

description: Global variations of the radionuclide 10Be that are almost simultaneous provide a powerful tool to synchronize 10Be records from different locations. We compared the 10Be record of the Akademii Nauk (AN) ice core (Russian Arctic) for the time period CE 1590-1950 to the 10Be records of two well-dated Greenland ice cores (Dye3 and NGRIP). A high correlation (r=0.60) was found between the AN and Dye3 records, which increases up to 0.78 in certain intervals, whereas the correlation to NGRIP was distinctly lower. Sources of deviations may include local fluctuations in the deposition of 10Be due to changes in the precipitation patterns, artefacts due to the core-sampling strategy and a general bias in the age model. In general, the existing age model was validated confirming the AN ice core to be a unique and well-dated source of palaeoclimate parameters for the Russian Arctic. Because of a possible minor bias in the earliest part of the studied ice-core section, the influence of the core-sampling strategy was studied, based on a numerical model that simulates sampling in a discrete and continuous mode with varying sample lengths. Based on the results of the model to sample continuously with individual samples lengths covering a time span of 4-8 years we developed a new sample strategy for the deeper layers.
description: Supplement to: von Albedyll, Luisa; Opel, Thomas; Fritzsche, Diedrich; Merchel, Silke; Laepple, Thomas; Rugel, Georg (2017): 10Be in the Akademii Nauk ice core – first results for CE 1590–1950 and implications for future chronology validation. Journal of Glaciology, 1-9
DOI: 10.1594/pangaea.898471
title: Radiosonde measurements from station Bondville (2018-07)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.810948
title: (Table 1) Interstitial water chemistry at DSDP Leg 73 Holes

description: Interstitial waters obtained from a transect east from the Mid-Atlantic Ridge on progressively older oceanic crust (Sites 519-522) indicate a general absence of concentration gradients in calcium and magnesium. The lack of gradients indicates little or no exchange of these seawater constituents with the underlying basalts. Only at Site 520, where there are increases in calcium and decreases in magnesium, do reactions in the silica-enriched zone appear to have affected interstitial water composition. At Site 524, on the eastern flank of the Walvis Ridge, large changes in calcium and magnesium occur as a result of reactions involving the volcanic materials that are both dispersed in the sediment column and present in the underlying basalts.
description: Supplement to: Gieskes, Joris M; Sirocky, Frank X; LaKind, Judy (1984): Interstitial water studies, Leg 73. In: Hsü, KJ; LaBrecque, JL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 73, 539-541
DOI: 10.1594/pangaea.776114
title: (Table T1) Distribution of selected calcareous nannofossils at the Paleocene/Eocene boundary, ODP Hole 208-1266C

description: Ocean Drilling Program Leg 208 Hole 1266C (28°32.55'S, 2°20.61'E) is located along the northwestern flank of Walvis Ridge (South Atlantic Ocean). The location of Site 1266, at 3.798 km water depth, corresponds to a mid-depth site of the Leg 208 transect. A stratigraphically continuous and expanded sequence of upper Paleocene and lower Eocene pelagic nannofossil ooze was recovered. Three holes were cored at Site 1266, and from Hole 1266C, an expanded and continuous Paleocene/Eocene (P/E) transition was recovered using the advanced piston corer system. The successful recovery and well-preserved nannofossil assemblages make Hole 1266C a reference section for improving the knowledge of the Paleocene/Eocene Thermal Maximum. The P/E transition is one of the most remarkable and intensively investigated time intervals. Significant and dramatic changes in climate and oceanography occurred at this transition. The P/E boundary is linked with an important turnover in benthic foraminifers and planktonic marine communities (Thomas and Shackleton, 1996, doi:10.1144/GSL.SP.1996.101.01.20; Kelly et al., 1998, doi:10.1016/S0031-0182(98)00017-0; Monechi et al., 2000, doi:10.2113/171.4.477; Bralower, 2002, doi:10.1029/2001PA000662). This report documents the calcareous nannofossil assemblage fluctuations at the P/E boundary in Hole 1266C based on semiquantitative and quantitative investigations.
description: Sediment depth is given in mcd. Relative abundance defined as: A = abundant (&gt;30% of the total assemblages), C = common (&gt;10%-30% of the total assemblages), F = few (&gt;3%-10% of the total assemblages), R = rare (1%-3% of the total assemblages), and RR = very rare (&lt;1% of the total assemblages); cf = compare. Dissolution interval between 306.63 and 306.76 mcd.
description: Supplement to: Monechi, Simonetta; Angori, Eugenia (2006): Data report: Calcareous nannofossil biostratigraphy of the Paleocene/Eocene boundary, Ocean Drilling Program Leg 208 Hole 1266C. In: Kroon, D; Zachos, JC; Richter, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 208, 1-9
DOI: 10.1594/pangaea.667420
title: (Table 4) Mineral composition of magnesium oxide depleted basalt phenocrysts, microphenocrysts, and matrix from DSDP Hole 52-418A
DOI: 10.1594/pangaea.727130
title: Geological map of Heimefrontfjella, Dronning Maud Land, Antarctica (Scale 1:250,000)

description: The geological overview map was compiled from 15 geological maps (1 : 25,000) and is based on Jacobs et al. 1996. The topographic basemaps were adapted from unpublished 1:250,000 provisional topographic maps, Institut f. Angewandte Geodäsie, Frankfurt, 1983. Part of the contour lines are from Radarsat (Liu et al. 2001).
DOI: 10.1594/pangaea.820391
title: Lucky Strike record of hydrothermal outflow temperature at vent MS_C04_101011_110706_LW00002

description: The temperature record include ambient temperatures (onboard the ship), water column temperatures (going up and down) and the hydrothermal temperatures.
DOI: 10.1594/pangaea.828474
title: Pass-through measurements of magnetic susceptibility from IODP Hole 323-U1341C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.495581
title: Water temperature MBT profiles from cruise U7426244M_1954
DOI: 10.1594/pangaea.920196
title: Ozone measurements from station Tamanrasset (2020-06)
DOI: 10.1594/pangaea.674069
title: Radiosonde measurements from station Camborne (2003-06)

description: Start location: Denver, Colorado, USA; Distance from radiation site: 30 km
DOI: 10.1594/pangaea.692293
title: Particulate organic carbon and nitrogen concentrations in water samples collected at Station SEPT-1997-GN36199704606MNB02 in the Aegean Sea

description: Seawater samples (1-5 l depending on distance of a station from a coast and depth of sampling) were filtered through Whatman GF/F filters (diameter 2.5 cm). Then the filters were wrapped in aluminium foil and stored at 22°C until analysis according to Hedges and Stern (Hedges, J.I., Stern, J.H. 1984. Carbon and nitrogen determinations of carbonate-containing solids. Limnol. Oceanogr., 29(3), 657-663; http://www.aslo.org/lo/toc/vol_29/issue_3/0657.pdf)
DOI: 10.1594/pangaea.887497
title: Expanded measurements from station Ny-Ålesund (2017-09), Version 1

description: 99999: No clouds detected; Version 1 with some values missing at 10000m CBH, please use new version (see "Replaced by" reference)
DOI: 10.1594/pangaea.751207
title: Meteorological observations during PHOENIX cruise from Madeira to Gambia started at 1768-01-06
DOI: 10.1594/pangaea.918006
title: Mass Accumulation Rates during Floods, Turbidites, and Droughts over the past 2000 years in the Santa Barbara Basin, CA
DOI: 10.1594/pangaea.737247
title: Sea surface temperature reconstruction from sediment core MD79-257 using alkenones
DOI: 10.1594/pangaea.751209
title: Meteorological observations during PHOENIX cruise from Spithead to Madeira started at 1768-12-20
DOI: 10.1594/pangaea.719625
title: Other measurements at 10 m from station Desert Rock (2003-10)
DOI: 10.1594/pangaea.774439
title: (Table T8) Dissolved inorganic carbon isotopes in pore fluid samples of ODP Site 204-1251 sediments

description: Sediment depth is given in mbsf. Overall precision is estimated to be better than ±0.15 per mil (1 sigma).
DOI: 10.1594/pangaea.773777
title: Visual core description (VCD) from IODP Hole 316-C0006F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.887869
title: Crystal c-axes (fabric analyser G50) of ice core samples collected from the Alpine ice core VCL (2012)

description: Image data: 5 sections FA -&gt; top depth of sections "01" equals top depth of the run, e.g. "36".Resolution: 500 px/cm (FA), images are vertically mirrored to each other.Measured at Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany.
DOI: 10.1594/pangaea.719628
title: Radiosonde measurements from station Desert Rock (2003-11)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.776286
title: Linescanner images of sediment core PG2066-1

description: IMPORTANT: These data are raw data which have not been corrected for gaps in the sediment, plastic plugs or other artifacts on the core margins. Prior to use, please use the core photographs to check for these errors.RGB and Lab raw data: http://hs.pangaea.de/Raw/PG/China2011/PG2066-1_color.zip
DOI: 10.1594/pangaea.760693
title: Organic carbon and calcium carbonate concentrations of K/T boundary samples from southern Tethyan margin location (Table 1)

description: Regional consequences of the biotic extinctions and of the changes in biological productivity that occurred at the time of the Cretaceous/Tertiary (K/T) boundary were investigated by comparison of organic matter in sediments from three southern Tethyan margin locations. Organic matter characterization comprised Rock-Eval pyrolysis and organic carbon measurements. Low concentrations of organic matter precluded additional detailed determinations. At all three locations, the organic matter has been microbially reworked and evidently was deposited in oxygenated marine environments.
description: Supplement to: Meyers, Philip A (1992): Data report: The Cretaceous/Tertiary boundary at Sites 761 and 762 (Northwest Australian Margin), at El Kef (Tunisia), and in the Negev Desert (Israel): a comparison of the organic geochemical records. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 881-885
DOI: 10.1594/pangaea.918003
title: Isotopic Carbon Data for Floods, Turbidites, and Droughts over the past 2000 years in the Santa Barbara Basin, CA
DOI: 10.1594/pangaea.787757
title: Sedimentology of core PG1901
DOI: 10.1594/pangaea.676932
title: Core description of the ANDRILL AND1-1B drill core (overview)
DOI: 10.1594/pangaea.724169
title: Other measurements at 10 m from station Southern Great Plains (2004-01)

description: Version 2, 2009-07-07
DOI: 10.1594/pangaea.793283
title: (Table 3) Clay mineralogy at DSDP Site 89-585

description: VA = very abundant, A = abundant, AR = common, R = rare, - = absent, &lt;1 = traces.
DOI: 10.1594/pangaea.683066
title: (Table 1) Measurement of length, breadth, and total area on the Globorotalia (Fohsella) lineage from Middle Miocene sediments of DSDP Hole 30-289 in the western equatorial Pacific

description: measurement of approx. 60 specimens. For the interval from 473.85 to 418.18 mbsf, ages of samples in Site 289 were assigned by applying the regression equations derived by Woodruff and Savin (1991). For the interval from 418.18 to 390.34 mbsf, ages were calculated by linear interpolation between the regressed age at 418.18 mbsf ( 13.31 Ma) and the concurrent extinction level of the G. (Fohsella) lineage at 390.34 mbsf, corresponding to an age of 11.8 Ma (Barron et al., 1985 ).
DOI: 10.1594/pangaea.870481
title: Current measurements from mooring SE in the Weddell Sea
DOI: 10.1594/pangaea.820394
title: Lucky Strike record of hydrothermal outflow temperature at vent MS_V01_090906_101004_HW0007A

description: The temperature record include ambient temperatures (onboard the ship), water column temperatures (going up and down) and the hydrothermal temperatures.
DOI: 10.1594/pangaea.820412
title: Lucky Strike record of hydrothermal outflow temperature at vent TE_AIS_090923_101010_HN29016b

description: The temperature record include ambient temperatures (onboard the ship), water column temperatures (going up and down) and the hydrothermal temperatures.
DOI: 10.1594/pangaea.730446
title: (Table 79) Chemical composition of apophyllite from basalts of the Nauru Basin, DSDP Hole 61-462A

description: Analyses have been carried out by T.N. Bortina and I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences.
DOI: 10.1594/pangaea.744584
title: (Table 4) Trace element contents in basalts and plutonic rocks from pillow lavas of the Sierra Leone fault site, MAR 5-7°N
DOI: 10.1594/pangaea.724266
title: Other measurements at 10 m from station Southern Great Plains (2007-11)
DOI: 10.1594/pangaea.724268
title: Other measurements at 10 m from station Southern Great Plains (2007-12)
DOI: 10.1594/pangaea.784667
title: XRF-core logger measurements from IODP Hole 333-C0011C

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.918063
title: Fig. 6 (top) RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and bulk susceptibility Klf

description: Fig. 6. RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and ARM (bottom), “S”IRM (middle) and bulk susceptibility Klf (top) as normalisers, respectively. The depth section between 3 and 6.5 m was re-sampled in 2009 to better describe the behaviour of the EMF in this depth/time interval.
DOI: 10.1594/pangaea.711679
title: (Table 1) Basalt density, basement age, and intrusive/extrusive relations from DSDP Site 9-79
DOI: 10.1594/pangaea.900459
title: Radiosonde raw data from Neumayer Station (2018-06), links to files
DOI: 10.1594/pangaea.868438
title: Othmarsingen, Switzerland (forest station): Long-term forest meteorological data from the Long-term Forest Ecosystem Research Programme (LWF), from 1997-2016

description: High quality meteorological data are needed for long-term forest ecosystem research, particularly in the light of global change. The long-term data series published here comprises almost 20 years of two meteorological stations in Othmarsingen in Switzerland where one station is located within a natural deciduous forest stand (OTB) with European beech (Fagus sylvatica; 120-140 yrs) and lime trees (Tilia sp.; 120-140 yrs) as dominant tree species. A second station is situated in the very vicinity outside of the forest (field station, OTF). The meteorological time series are presented in hourly time resolution of air temperature, relative humidity, precipitation, photosynthetically active radiation (PAR) and wind speed. Othmarsingen is part of the Long-term Forest Ecosystem research Programme (LWF) established and maintained by the Swiss Federal Research Institute WSL. For more information see PDF under 'Further Details'.
DOI: 10.1594/pangaea.724270
title: Other measurements at 10 m from station Southern Great Plains (2008-01)
DOI: 10.1594/pangaea.724240
title: Other measurements at 10 m from station Southern Great Plains (2006-10)
DOI: 10.1594/pangaea.741850
title: Lithology of sediment core ZABOIN94, Zaboinoe Lake, Russia

description: This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.724246
title: Other measurements at 10 m from station Southern Great Plains (2007-01)
DOI: 10.1594/pangaea.472246
title: Physical oceanography measured at different bottle stations in 1994, Bahia Independencia, Peru
DOI: 10.1594/pangaea.900463
title: Radiosonde raw data from Neumayer Station (2018-10), links to files
DOI: 10.1594/pangaea.918406
title: Ultra-violet measurements from station Toravere (2020-03)
DOI: 10.1594/pangaea.907691
title: OZ-7 Lake Eyre region in South Australia and along the Darling River up to Bourke in New South Wales sampling trip and analysis: strontium, rubidium and neodymium isotopes

description: Analyses performed by Dr Marc Norman, ANUProcedures as in: Gingele, F.X. & De Deckker, P. (2005)
DOI: 10.1594/pangaea.472252
title: Physical oceanography measured at different bottle stations in 2000, Bahia Independencia, Peru