cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25549/inscriptifact-ouc110213509
title: Persepolis Fortification Elamite Tablet 2261.102, Fort 2261.102

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2261.102 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform, Aramaic ❧ [Physical Object Description:] Clay tablet with cuneiform text and Aramaic gloss. Seal impression on left edge. ❧ [Physical Object Note:] Damage or cracks on left edge, right edge, reverse and upper edge.
DOI: 10.25549/kada-ouc11399lk24
title: Clippings on Japanese rule in Korea, 1918-1919

description: Clippings on Japanese rule in Korea, 1918-1919
DOI: 10.1594/pangaea.667184
title: Biomass of in- and epibenthic invertebrate macrofauna in the German Bight at site MZB-WB
DOI: 10.25549/inscriptifact-ouc110217421
title: Persepolis Fortification Elamite Tablet 0576.101, Fort 0576.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 0576.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on left edge. ❧ [Physical Object Note:] Wear on right side of obverse, right edge broken off.
DOI: 10.1594/pangaea.401198
title: Figure 2: Chemical measurements from the EPICA Dome C core, on an age scale

description: The timescale is EDC2, and the accumulation rates used to calculate flux also derive from EDC2. Non-sea-salt concentrations were calculated. We calculated ssNa and nssCa assuming a Ca/Na weight ratio of 0.038 for marine aerosols and 1.78 for the average crust. nssSO42- was derived assuming a SO42-/Na ratio in marine aerosol of 0.1 (appropriate for a sea ice surface, but note that the use of a traditional sea water ratio of 0.25 would not affect the results significantly).Data presented in Wolff et al. (2006) were all too high by 8.3% because of an error with the accumulation rates: these are the corrected values.
DOI: 10.1594/pangaea.927458
title: Phycotoxin contents during a long-term mesocosm study in Gullmar Fjord Sweden in 2013

description: The phycotoxin contents were measured in 2013 during a long-term mesocosm CO2 experiment in Gullmar Fjord (Sweden). The natural plankton community was enclosed in ten pelagic mesocosms and five of the mesocosms were enriched with CO2 to simulate end-of the century ocean acidification while the others served as controls. The data set was used to assess the impact of ocean acidification on harmful algal bloom species and toxins. The Fjord-sample data were taken in close proximity of the mesocosms and were used to assess the phycotoxin contents in the surrounding waters.
DOI: 10.25549/inscriptifact-ouc1sto1540423
title: Persepolis Fortification Elamite Tablet 2171.102, Fort 2171.102

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2171.102 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform, Aramaic ❧ [Physical Object Description:] Clay tablet with cuneiform text and Aramaic gloss. Seal impressions on left edge and reverse. ❧ [Physical Object Note:] Damage or cracks on right edge and reverse.
DOI: 10.15468/dl.pnkzfr
title: Occurrence Download

description: A dataset containing 429 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Brazil",
 "TaxonKey is Cheiracanthium inclusum"
 ]
}

 The dataset includes 429 records from 9 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0027878-251025141854904/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.716789
title: (Table 1) Radiocarbon age determination on sediment core Lz1101 from the Melles Lake, 0-190 cm
DOI: 10.1594/pangaea.864101
title: Radiocarbon dates of peatland initiation across the northern high latitudes

description: A compilation of basal dates of peatland initiation across the northern high latitudes, associated metadata including location, age, raw and calibrated radiocarbon ages, and associated references.Includes previously published datasets from sources below as well as 365 new data points.
description: Supplement to: Treat, Claire C; Jones, Miriam C; Brosius, Laura Susan; Grosse, Guido; Walter Anthony, Katey M (in prep.): High latitude lake and wetland methane emissions lag abrupt early Holocene increases in atmospheric methane.
DOI: 10.25549/inscriptifact-ouc110217411
title: Persepolis Fortification Elamite Tablet 0314.104, Fort 0314.104

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 0314.104 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on reverse. ❧ [Physical Object Note:] Broken left edge, upper edge. Large crack on reverse.
DOI: 10.25549/kada-ouc11399lk23
title: Clippings on Japanese rule in Korea, 1918-1919

description: Clippings on Japanese rule in Korea, 1918-1919
DOI: 10.1594/pangaea.671367
title: EPICA Dome C Ice Core Timescales EDC3

description: The EPICA (European Project for Ice Coring in Antarctica) Dome C drilling in East Antarctica has now been completed to a depth of 3260 m, at only a few meters above bedrock. Here we present the new EDC3 chronology, which is based on the use of 1) a snow accumulation and mechanical flow model, and 2) a set of independent age markers along the core. These are obtained by pattern matching of recorded parameters to either absolutely dated paleoclimatic records, or to insolation variations. We show that this new time scale is in excellent agreement with the Dome Fuji and Vostok ice core time scales back to 100 kyr within 1 kyr. Discrepancies larger than 3 kyr arise during MIS 5.4, 5.5 and 6, which points to anomalies in either snow accumulation or mechanical flow during these time periods. We estimate that EDC3 gives accurate event durations within 20% (2 sigma) back to MIS11 and accurate absolute ages with a maximum uncertainty of 6 kyr back to 800 kyr.
description: Timescale EDC3 for the EPICA Dome C ice core, both for the ice matrix and gas bubbles. The dataset gives the depth versus age timescale that has been adopted as official for the EPICA Dome C ice core. Depth refers to the official log depth of the drilling. EDC3 for the ice matrix (EDC3_ice) is described fully in Parrenin et al. (Climate of the Past, 3, 485-497, 2007). This timescale is based on an snow accumulation / ice flow model, which is further tuned with independent age markers. Gas ages are derived using a firn densification model, and are fully described in Loulergue et al. (Climate of the Past, 3, 527-540, 2007). The ages given here correspond to the scenario 4 of Loulergue et al. and where necessary can be referred to as EDC3_gas_a.
description: Supplement to: Parrenin, Frédéric; Barnola, Jean-Marc; Beer, Jürg; Blunier, Thomas; Castellano, Emiliano; Chappellaz, Jérôme A; Dreyfus, Gabrielle; Fischer, Hubertus; Fujita, Shuji; Jouzel, Jean; Kawamura, Kenji; Lemieux-Dudon, Bénédicte; Loulergue, Laetitia; Masson-Delmotte, Valerie; Narcisi, Biancamaria; Petit, Jean Robert; Raisbeck, Grant M; Raynaud, Dominique; Ruth, Urs; Schwander, Jakob; Severi, Mirko; Spahni, Renato; Steffensen, Jørgen Peder; Svensson, Anders M; Udisti, Roberto; Waelbroeck, Claire; Wolff, Eric William (2007): The EDC3 chronology for the EPICA Dome C ice core. Climate of the Past, 3, 485-497
DOI: 10.25549/inscriptifact-ouc110213287
title: Scans

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2047.001 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impression on reverse. ❧ [Physical Object Note:] Damage or cracks on bottom edge, left edge, obverse, right edge and reverse.
DOI: 10.1594/pangaea.683641
title: EPICA Dome C chemical concentrations and fluxes

description: Sea salt Na+ and nss Ca2+ data from the EPICA Dome C (EDC) ice core over the last 150000 yr in 1 m resolution (revised version). Data has been calculated from raw data as described in the manuscript. Negative concentrations after correcting for crustal sodium and sea salt calcium, respectively, have been replaced by zeros. Missing values occur due to sample loss, bad core quality or contamination during sample preparation.
DOI: 10.1594/pangaea.696109
title: Rare earth elements determined in ice core EDC by inductively coupled plasma quadrupole mass spectrometry (ICP-Q-MS)

description: Number of replicates: 3
DOI: 10.25549/inscriptifact-ouc110186827
title: Scans

description: [Text Description:] Administrative text ❧ [Text or Publication Number Note:] Fort 1267.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform, Aramaic ❧ [Physical Object Description:] Clay tablet with cuneiform text, Aramaic ink inscription. ❧ [Physical Object Note:] Bottom left corner, top right corner triangular section broken off.
DOI: 10.25549/kada-ouc11399lk60
title: Clippings on Japanese rule in Korea, 1918-1919

description: Clippings on Japanese rule in Korea, 1918-1919
DOI: 10.1594/pangaea.929680
title: Amospheric carbon dioxide of the Marine Isotope Stage 6 period (190-135 ka) from the EPICA Dome C ice core

description: We measured 177 new data points of atmospheric CO2 concentrations from the EPICA Dome C (EDC) ice core (75°06'S, 123°24'E) spanning MIS 6 (190 to 135 kyr BP) at the Institut des Géosciences de l'Environnement (IGE), France and Climate and Environmental Physics (CEP), Physics Institute, University of Bern, Switzerland. The majority of all atmospheric CO2 samples (i.e. 150) were measured using the ball mill dry-extraction system which is coupled to a gas chromatograph at IGE (Schaefer et al., 2011). We measured 65 samples from 27 depth intervals using the Centrifugal Ice Microtome (CIM) (Bereiter et al., 2013) at CEP. This new CO2 data measured within the scope of this study is complemented with two published datasets (Lourantou et al., 2010; Schneider et al., 2013) and one unpublished CO2 dataset measured in 2003. We use all of the available data from the EDC ice core to compile a composite dataset of atmospheric CO2 covering MIS 6 in doi:10.1594/PANGAEA.929693.
DOI: 10.1594/pangaea.696111
title: Rare earth elements determined in ice core EDC by inductively coupled plasma sector field mass spectrometry (ICP-SF-MS)

description: Number of replicates: 40
DOI: 10.1594/pangaea.780541
title: EDC dust laser signal (24-769.5 m)

description: The file "EDC_KPHdust_1cm.dat" contains the EPICA Dome C insoluble dust measured with the Copenhavn laser sensor on a depth and EDC3 age scale. Below 769.5m depth insoluble dust was measured with the Bern sensor, data available in the file "EDC_CaDustConc_1cm.dat".
DOI: 10.25549/inscriptifact-ouc110213284
title: Persepolis Fortification Elamite Tablet 2041.101, Fort 2041.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2041.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impressions on right edge, reverse. ❧ [Physical Object Note:] Damage or cracks on bottom edge, left edge, reverse and upper edge.
DOI: 10.1594/pangaea.784003
title: (Appendix 2) Diatom biostratigraphy of sediment core GA306-GC4 obtained during Galathea 3 cruise
DOI: 10.25549/inscriptifact-ouc110186822
title: Scans

description: [Text Description:] Administrative text with seals ❧ [Text or Publication Number Note:] Fort 1223.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform, Aramaic ❧ [Physical Object Description:] Clay tablet with cuneiform text, Aramaic ink inscription. Seal impression left edge. ❧ [Physical Object Note:] Broken right edge.
DOI: 10.25549/kada-ouc11399lk3f
title: Clippings on Japanese rule in Korea, 1918-1919

description: Clippings on Japanese rule in Korea, 1918-1919
DOI: 10.1594/pangaea.728699
title: Carbon isotopic record of CO2 from the Holocene of the Dome C ice core

description: Reconstructions of atmospheric CO2 concentrations based on Antarctic ice cores reveal significant changes during the Holocene epoch, but the processes responsible for these changes in CO2 concentrations have not been unambiguously identified. Distinct characteristics in the carbon isotope signatures of the major carbon reservoirs (ocean, biosphere, sediments and atmosphere) constrain variations in the CO2 fluxes between those reservoirs. Here we present a highly resolved atmospheric d13C record for the past 11,000 years from measurements on atmospheric CO2 trapped in an Antarctic ice core. From mass-balance inverse model calculations performed with a simplified carbon cycle model, we show that the decrease in atmospheric CO2 of about 5 parts per million by volume (p.p.m.v.) and the increase in d13C of about 0.25% during the early Holocene is most probably the result of a combination of carbon uptake of about 290 gigatonnes of carbon by the land biosphere and carbon release from the ocean in response to carbonate compensation of the terrestrial uptake during the termination of the last ice age. The 20 p.p.m.v. increase of atmospheric CO2 and the small decrease in d13C of about 0.05% during the later Holocene can mostly be explained by contributions from carbonate compensation of earlier land-biosphere uptake and coral reef formation, with only a minor contribution from a small decrease of the land-biosphere carbon inventory.
description: Dome C ice core covering 0 to 11 kyr BP. The air from polar ice-core samples of about 30g (AWI/Bern) and 5-6g (Bern) is extracted under vacuum with a sublimation methode or via mechanical cracking, respectively, and the extracted gas is then analysed for d13CO2 using gas chromatographic separation and isotopic analyses on two independet mass spectrometers. The mean d13CO2 analytical uncertainty of both methods (1-sigma) is 0.07 per mille.The age scale used (in ka before 1950 AD) is EDC3 gas age scenario 4 (Loulergue et al., 2007, http://www.clim-past.net/3/527/2007).Values marked via '/', are outlies, and have not been taken into account for deconvolution calculations. The outlier depths have been measured using both extraction methods and are very likley caused by an ice core break during the drilling (see further details).
description: Supplement to: Elsig, Joachim; Schmitt, Jochen; Leuenberger, Daiana; Schneider, Robert; Eyer, Marc; Leuenberger, Markus Christian; Joos, Fortunat; Fischer, Hubertus; Stocker, Thomas F (2009): Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core. Nature, 461, 507-510
DOI: 10.1594/pangaea.887109
title: Redox sensitive metals, d15N, hydrogen index and TOC measured on a composite record (B14-G10-G14) off Peru covering the last 25 kyr

description: Oxygen minimum zones (OMZ) have expanded in all tropical oceans during the last 50 years resulting in habitat contraction and considerable changes in marine biogeochemistry. However, for a better understanding of the OMZ dynamics under the current climate change, two questions are relevant: 1) how do the magnitude and temporal changes in oceanic dissolved oxygen of the last few decades compare to the natural variability on longer timescales, and 2) what were the local and remote factors driving OMZ changes in the past. In the present study we use a stacked record covering the last 25 kyr from the Eastern Tropical South Pacific (ETSP) OMZ to reconstruct changes in oxygenation and productivity. We use a suite of proxies including the presence of laminations, redox sensitive metals (U, Mo, Re, Ni and Cu), total organic carbon and d15N measurements. Water column denitrification and sediment redox conditions show pronounced centennial to millennial-scale variability during the last 25 kyr, with oxygenation levels as low as at present. Global cold periods at different timescales such as the Last Glacial Maximum (23e19 kyr BP) and the Little Ice Age (1500e1850 AD) were associated with a weak OMZ and low export production, while warm intervals such as the deglaciation, part of the Medieval Climate Anomaly and the last 100 years are associated with a stronger OMZ and high export production. Water column denitrification and sediment redox conditions were strongly coupled during the last 25 kyr BP apart from one remarkable exception: during the Antarctic Cold Reversal, sediments were less reducing but the water column denitrification was high resulting in a strong but shallow OMZ. This may have been produced by an enhanced Antarctic Intermediate Water flow. Contrary to our expectations and modeling predictions for the next few decades, we observe a weak ETSP-OMZ during the warm mid-Holocene, which may have been the result of a stronger Walker Circulation that brought oxygen-rich waters to intermediate depths off Peru via Equatorial undercurrents. In combination with other paleoceanographic reconstructions, our results show that oxygenation variability in the ETSP-OMZ was influenced by ocean circulation changes in the Tropical Pacific, high latitude oceanographic and climatic changes, and local productivity.
description: Supplement to: Salvatteci, Renato; Gutièrrez, Dimitri; Sifeddine, Abdelfettah; Ortlieb, Luc; Druffel, Ellen R M; Boussafir, Mohammed; Schneider, Ralph R (2016): Centennial to millennial-scale changes in oxygenation and productivity in the Eastern Tropical South Pacific during the last 25,000 years. Quaternary Science Reviews, 131, 102-117
DOI: 10.25549/inscriptifact-ouc110211082
title: Scans

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 1852.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. ❧ [Physical Object Note:] Damage or cracks on left edge, obverse, right edge and reverse.
DOI: 10.1594/pangaea.863152
title: Prosome length of Pseudocalanus acuspes (females), KOSMOS 2013, Kristineberg, Sweden
DOI: 10.25549/inscriptifact-ouc110186658
title: Scans

description: [Text Description:] Administrative text with seals ❧ [Text or Publication Number Note:] Fort 1223.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform, Aramaic ❧ [Physical Object Description:] Clay tablet with cuneiform text, Aramaic ink inscription. Seal impression left edge. ❧ [Physical Object Note:] Broken right edge.
DOI: 10.1594/pangaea.548513
title: Annual means of density, δ¹⁸O, deuterium, and accumulation rates of firn core FRI34C95_03
DOI: 10.1594/pangaea.82275
title: (Fig. 5) Pollen analysis of the Furo do Chato core

description: Age: Radiocarbon dates
DOI: 10.25549/kada-ouc11399lk50
title: Clippings on Japanese rule in Korea, 1918-1919

description: Clippings on Japanese rule in Korea, 1918-1919
DOI: 10.1594/pangaea.548659
title: Density and δ¹⁸O of snow pit FRI15S90_131

description: Temperature of ice at 10 m depth: -23.3 deg C
DOI: 10.1594/pangaea.81339
title: (Table 2) AMS radiocarbon dates for Bosque de Avicennia records
DOI: 10.25549/inscriptifact-ouc110211047
title: Scans

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 1738.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform ❧ [Physical Object Description:] Clay tablet with cuneiform text. Seal impressions on reverse and upper edge. ❧ [Physical Object Note:] Damage or cracks on bottom edge, left edge, obverse, right edge and reverse.
DOI: 10.1594/pangaea.548664
title: Annual means of density, δ¹⁸O, and accumulation rates of snow pit FRI11S90_235

description: Temperature of ice at 10 m depth: -24.3 deg C
DOI: 10.1594/pangaea.548746
title: Conductivity and oxygen isotope measured on ice core FRI09C90_13 (B13) from the Filchner-Ronne ice shelf, Antarctica

description: The Filchner-Ronne ice shelf, which drains most of the marine-based portions of the West Antarctic ice sheet, is the largest ice shelf on Earth by volume. The origin and properties of the ice that constitutes this shelf are poorly understood, because a strong reflecting interface within the ice and the diffuse nature of the ice?ocean interface make seismic and radio echo sounding data difficult to interpret. Ice in the upper part of the shelf is of meteoric origin, but it has been proposed that a basal layer of saline ice accumulates from below. Here we present the results of an analysis of the physical and chemical characteristics of an ice core drilled almost to the bottom of the Ronne ice shelf. We observe a change in ice properties at about 150 m depth, which we ascribe to a change from meteoric ice to basal marine ice. The basal ice is very different from sea ice formed at the ocean surface and we propose a formation mechanism in which ice platelets in the water column accrete to the bottom of the ice shelf.
description: Temperature of ice at 10 m depth: -23.5 deg C
description: Supplement to: Oerter, Hans; Kipfstuhl, Sepp; Determann, Jürgen; Miller, Heinrich; Wagenbach, Dietmar; Minikin, Andreas; Graf, Wolfgang (1992): Evidence for basal marine ice in the Filchner-Ronne ice shelf. Nature, 358, 399-401
DOI: 10.25549/inscriptifact-ouc110186655
title: Scans

description: [Text Description:] Administrative text ❧ [Text or Publication Number Note:] Fort 1258.101 ❧ [Excavation Description:] Found during Oriental Institute's excavations in Spring, 1933, near the northeastern corner of the stone platform of Persepolis, in two small rooms of a bastion in the fortification wall ❧ [Medium:] Clay ❧ [Script Note:] Non-Alphabetic Cuneiform, Aramaic ❧ [Physical Object Description:] Clay tablet with cuneiform text, Aramaic ink inscription. ❧ [Physical Object Note:] Top left edge broken, bottom right triangular section broken off.