cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.25549/inscriptifact-ouc110820243
title: Persepolis Fortification Elamite Tablet 2267.101, Fort 2267.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2267.101 ❧ [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 right edge. ❧ [Physical Object Note:] Left side of tablet missing.
DOI: 10.25549/inscriptifact-ouc110820121
title: Persepolis Fortification Elamite Tablet 2267.101, Fort 2267.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2267.101 ❧ [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 right edge. ❧ [Physical Object Note:] Left side of tablet missing.
DOI: 10.25549/inscriptifact-ouc110820139
title: Persepolis Fortification Elamite Tablet 2267.101, Fort 2267.101

description: [Text Description:] Administrative text with seal ❧ [Text or Publication Number Note:] Fort 2267.101 ❧ [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 right edge. ❧ [Physical Object Note:] Left side of tablet missing.
DOI: 10.25549/inscriptifact-ouc110820165
title: Persepolis Fortification Elamite Tablet 2272.101, Fort 2272.101

description: [Text Description:] Administrative text ❧ [Text or Publication Number Note:] Fort 2272.101 ❧ [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:] Upper left, upper right and lower right corners broken off. Damage on obverse, reverse.
DOI: 10.25549/inscriptifact-ouc110820108
title: Persepolis Fortification Elamite Tablet 2272.101, Fort 2272.101

description: [Text Description:] Administrative text ❧ [Text or Publication Number Note:] Fort 2272.101 ❧ [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:] Upper left, upper right and lower right corners broken off. Damage on obverse, reverse.
DOI: 10.15468/dl.hb3td5
title: Occurrence Download

description: A dataset containing 959 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Kokkocynips rileyi (Nieves-Aldrey, Nicholls, Tang, Melika, Stone, Pujade-Villar, Buffington, Maldonado & Medianero, 1896) Nieves-Aldrey, Nicholls, Tang, Melika, Stone, Pujade-Villar, Buffington, Maldonado & Medianero, 2021"
 ]
}

 The dataset includes 959 records from 3 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006868-250525065834625/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25403/upresearchdata.28436366
title: Three constructs among leaders in corporate South Africa

description: The study investigates the relationship between personality, emotional intelligence, and spiritual intelligence with six (6) physiological drivers, namely brain fitness, stress coping, nutrition, mindset, sleep, and exercise, which are all key parts of leadership excellence.Phase I, the quantitative phase, involved the administration of three (3) questionnaires, namely the Hogan Personality Inventory (HPI), the EQi2.0 (an emotional intelligence assessment tool), and the Neuro Agility Profile (NAP). A sequential explanatory mixed methods research design was used during the course of the study. Seventy participants volunteered to participate in the study. Phase II of the study, the qualitative phase, consisted of semi-structured, in-depth interviews in which six (6) participants partook. Quantitative data were analysed using IBM SPSS version 26©. Descriptive statistics were used to describe the sample and to report on the prevalence of personality, emotional intelligence, and spiritual intelligence.Qualitative data were thematically analysed using Braun and Clarke’s six-phase approach for thematic analysis. Six (6) themes were identified, namely, individual leadership attributes, interaction with others, personal intent to make an impact, line of sight between the leaders and society, organizational obligations, and finally, awareness of the macro context within which leadership occurs.
DOI: 10.1594/pangaea.815931
title: (Table S4b) Major and trace element compositions of ODP Hole 181-1123B tephras

description: All standard deviations = 2sd.
DOI: 10.1594/pangaea.908574
title: (Figure 7p2) LA-ICP-MS Fe56 measurements (1315-1365) on ice core KCC from Colle Gnifetti

description: Dataset corresponds to Figure 7 in the final manuscript. LAICPMS Fe56 measurements from 1315-1365 C.E.
DOI: 10.1594/pangaea.782397
title: (Table S11) Representative trace element composition of different garnet zones of sample VT08129

description: #0 = below detection limit.
DOI: 10.1594/pangaea.929859
title: Seawater carbonate chemistry and enzymatic antioxidant defense, protein repair and removal of temperate shark (Scyliorhinus canicula)

description: Ocean acidification is a consequence of chemical changes driven mainly by a continuous uptake of carbon dioxide, resulting in pH decrease. This phenomenon represents an additional threat to marine life, with expected effects ranging from changes in behavioral responses and calcification rates to the potential promotion of oxidative stress. To unravel the impacts of ocean acidification on the antioxidant system of sharks, we performed a long-term exposure (9 months, since early embryogenesis) to high CO2 conditions (pCO2 900 μatm) on a temperate shark (Scyliorhinus canicula). The following biomarkers were measured: enzymatic antioxidant defense (superoxide dismutase, catalase and glutathione peroxidase), protein repair and removal (heat shock proteins and ubiquitin), and oxidative damage on lipids (malondialdehyde) and DNA (8-hydroxy-2′-deoxyguanosine). Changes in the antioxidant enzyme defense were restricted to an increase in catalase activity in the muscle, an enzyme that plays a major role in oxidative stress mitigation. On the other hand, no evidence of oxidative damage was found, indicating that the observed increase in catalase activity may be enough to neutralize the effects of potentially higher reactive oxygen species. These results further indicate that these sharks' antioxidant system can successfully cope with the levels of carbon dioxide projected for the end of the century. Nonetheless, the interaction between ocean acidification and the rise in temperature expected to occur in a near future may disturb their antioxidant capacity, requiring further investigation.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2021) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2021-03-23.
DOI: 10.1594/pangaea.910312
title: (Table S1) Laser ablation strontium isotope analysis for hardgrounds
DOI: 10.1594/pangaea.810351
title: Element composition of clinopyroxenes from gabbroic rocks of the Tiger Gabbro complex, Spatulate Ridge and Apostrophe Island, Antarctica
DOI: 10.1594/pangaea.586871
title: Mg/Ca ratio, Sr/Ca ratio and stable isotopes of the foraminifera Oridorsalis umbonatus in surface sediment samples

description: We investigate the influence of carbonate system parameters (carbonate ion concentration, [CO3**2-]; carbonate ion saturation, Delta [CO3**2-]) on the trace element and stable isotope ratios in the endobenthic foraminifera Oridorsalis umbonatus. Data from modern core top samples from the Namibian continental slope suggest that the shell composition of this species is influenced by the chemistry of the pore-water. For these organic-rich sediments, the impact of ocean bottom water properties on both pore-water and shell chemistry is surprisingly small. Sr/Ca correlates positively with [CO3**2-] and to a lesser extent with Delta [CO3**2-], which is opposed to previous results. A [CO3**2-] decrease of 10 µmol/kg leads to an increase of 0.05 mmol/mol in Sr/Ca. We observe a correlation between shell d18O (corrected for temperature and d18O seawater) and [CO3**2-], however, the variability of the corrected d18O is close to the analytical limit. No clear dependences were observed for d13C and Mg/Ca.
description: Supplement to: Rathmann, Söhnke; Kuhnert, Henning (2008): Carbonate ion effect on Mg/Ca, Sr/Ca and stable isotopes on the benthic foraminifera Oridorsalis umbonatus off Namibia. Marine Micropaleontology, 66(2), 120-133
DOI: 10.1594/pangaea.767497
title: Oxide concentrations of zircons in ODP Hole 188-1166A upper level sample
DOI: 10.1594/pangaea.829831
title: Experiment: Elevated temperature and PCO2 affect enzyme activities in differentially oxidative tissues of Notothenia rossii

description: Mitochondrial plasticity plays a central role in setting the capacity for acclimation of aerobic metabolism in ectotherms in response to environmental changes. We still lack a clear picture if and to what extent the energy metabolism and mitochondrial enzymes of Antarctic fish can compensate for changing temperatures or PCO2 and whether capacities for compensation differ between tissues. We therefore measured activities of key mitochondrial enzymes (citrate synthase (CS), cytochrome c oxidase (COX)) from heart, red muscle, white muscle and liver in the Antarctic fish Notothenia rossii after warm- (7 °C) and hypercapnia- (0.2 kPa CO2) acclimation vs. control conditions (1 °C, 0.04 kPa CO2). In heart, enzymes showed elevated activities after cold-hypercapnia acclimation, and a warm-acclimation-induced upward shift in thermal optima. The strongest increase in enzyme activities in response to hypercapnia occurred in red muscle. In white muscle, enzyme activities were temperature-compensated. CS activity in liver decreased after warm-normocapnia acclimation (temperature-compensation), while COX activities were lower after cold- and warm-hypercapnia exposure, but increased after warm-normocapnia acclimation. In conclusion, warm-acclimated N. rossii display low thermal compensation in response to rising energy demand in highly aerobic tissues, such as heart and red muscle. Chronic environmental hypercapnia elicits increased enzyme activities in these tissues, possibly to compensate for an elevated energy demand for acid-base regulation or a compromised mitochondrial metabolism, that is predicted to occur in response to hypercapnia exposure. This might be supported by enhanced metabolisation of liver energy stores. These patterns reflect a limited capacity of N. rossii to reorganise energy metabolism in response to rising temperature and PCO2.
description: Notothenia rossii acclimated to higher temperature and PCO2; Citrate synthase (CS) and cytochrome c oxidase (COX) activities are given in nmol per minute and mg protein (CS/protein; COX/protein) or mg tissue fresh mass (CS/MW; COX/MW) at the assay temperatures of 0, 6, 9, 12 °C in heart, liver, red muscle & white muscle tissue of all acclimated animals and the control.
description: Supplement to: Strobel, Anneli; Leo, Elettra; Pörtner, Hans-Otto; Mark, Felix Christopher (2013): Elevated temperature and PCO2 shift metabolic pathways in differentially oxidative tissues of Notothenia rossii. Comparative Biochemistry and Physiology Part B: Biochemistry & Molecular Biology, 166(1), 48-57
DOI: 10.1594/pangaea.782389
title: (Table S8) Representative trace element composition of garnet 1, sample VT08102

description: #0 = below detection limit.
DOI: 10.1594/pangaea.885145
title: Mn/Ca, Mg/Ca and Sr/Ca ratios of multiple chambers of specimens of Ammonia tepida from Lake Grevelingen

description: The adaptation of some benthic foraminiferal species to low-oxygen conditions provides the prospect of using the chemical composition of their tests as proxies for bottom water oxygenation. Manganese may be particularly suitable as such a geochemical proxy because this redox element is soluble in reduced form (Mn2+) and hence can be incorporated into benthic foraminiferal tests under low-oxygen conditions. Therefore, intra- and inter-test differences in foraminiferal Mn/Ca ratios may hold important information about short-term variability in pore water Mn2+ concentrations and sediment redox conditions. Here, we studied Mn/Ca intra- and inter-test variability in living individuals of the shallow infaunal foraminifer Ammonia tepida sampled in Lake Grevelingen (the Netherlands) in three different months of 2012. The deeper parts of this lake are characterized by seasonal hypoxia/anoxia with associated shifts in microbial activity and sediment geochemistry, leading to seasonal Mn2+ accumulation in the pore water. Earlier laboratory experiments with similar seawater Mn2+ concentrations as encountered in the pore waters of Lake Grevelingen suggest that intra-test variability due to ontogenetic trends (i.e. size-related effects) and/or other vital effects occurring during calcification in A. tepida (11-25% relative SD, RSD) is responsible for part of the observed variability in Mn/Ca. Our present results show that the seasonally highly dynamic environmental conditions in the study area lead to a strongly increased Mn/Ca intra- and inter-test variability (average of 45% RSD). Within single specimens, both increasing and decreasing trends in Mn/Ca ratios with size are observed. Our results suggest that the variability in successive single-chamber Mn/Ca ratios reflects the temporal variability in pore water Mn2+. Additionally, active or passive migration of the foraminifera in the surface sediment may explain part of the observed Mn/Ca variability.
description: Supplement to: Petersen, Jassin; Barras, Christine; Bézos, Antoine; La, Carole; de Nooijer, Lennart Jan; Meysman, Filip J R; Mouret, Aurélia; Slomp, Caroline P; Jorissen, Frans J (2018): Mn/Ca intra- and inter-test variability in the benthic foraminifer Ammonia tepida. Biogeosciences, 15(1), 331-348
DOI: 10.1594/pangaea.941335
title: Pollution mask for the continuous corrected particle number concentration data in 1 min resolution, measured in the Swiss aerosol container during MOSAiC 2019/2020

description: This dataset contains a pollution flag in 1 min time resolution. It is derived by the pollution detection algorithm (PDA) based on the corrected particle number concentration data (doi:10.1594/PANGAEA.941886) measured during the year long MOSAiC expedition from October 2019 to September 2020. With pollution, we refer to emission from the exhaust of the ship stack, snow groomers, diesel generators, ship vents, helicopters and other. Pollution hence reflects locally emitted particles and trace gases, which are not representative of the central Arctic ambient concentrations. The PDA identifies and flags periods of polluted data in the particle number concentration dataset five steps. The first and most important step identifies polluted periods based on the gradient (time-derivative) of a concentration over time. If this gradient exceeds a given threshold, data are flagged as polluted. Further pollution identification steps are a simple concentration threshold filter, a neighboring points filter (optional), a median and a sparse data filter (optional). The detailed methodology of the derivation of the pollution flag is described in Beck et al. (2022). A description and download link to the used particle number concentration dataset can be found here: doi:10.1594/PANGAEA.941886. The code of the PDA can be found on Zenodo (Beck et al., 2021; doi:10.5281/zenodo.5761101).Participation of the Swiss Container was co-financed by the Swiss Polar Institute and University of Helsinki.
description: This dataset contains a pollution flag in 1 min time resolution and the corresponding particle number concentration data (doi:10.1594/PANGAEA.941886). The data columns include Event, Time, Latitude, Longitude, Particle number concentration and a pollution flag to indicate polluted periods (0=not polluted, 1=polluted). The pollution flag is derived from the Pollution Detection Algorithm (PDA), a python-based open access script to automatically detect contamination in remote atmospheric time series (Beck et al., Atmos. Meas. Tech., in prep.). The following parameters were used in the PDA script to derive this pollution flag:• a= 0.5 cm-3s-1• m = 0.55 s-1• upper_threshold: 104 cm-3• lower_threshold: 60 cm-3• neighboring points filter: on• median deviation factor: 1.4• sparse window: 30• sparse threshold: 24Remark_1: The corrected particle number concentration may still contain some minor artefacts and a critical review of the data by an expert is required. The pollution flag is based on the above mentioned parameters. If needed, the PDA can be tuned to be stricter. The decision whether a single data point is affected by pollution is up to the user and requires an expert review.Remark_2: This pollution mask can be applied to other particle and trace measurements obtained during MOSAiC. Please see Beck et al., Atmos. Meas. Tech., in prep. for a detailed discussion.
DOI: 10.1594/pangaea.922248
title: Seawater carbonate chemistry and energy metabolism and survival of the juvenile recruits of the American lobster (Homarus americanus)

description: The transition from the last pelagic larval stage to the first benthic juvenile stage in the complex life cycle of marine invertebrates, such as the American lobster Homarus americanus, a species of high economic importance, represents a delicate phase in these species development. Under future elevated pCO2 conditions, ocean acidification and other elevated pCO2 events can negatively affect crustaceans. This said their effects on the benthic settlement phase are virtually unknown. This study aimed to identify the effects of elevated seawater pCO2 on stage V American lobsters exposed to seven pCO2 levels. The survival, development time, metabolic and feeding rates, carapace composition, and mitochondrial function were investigated. Results suggested an increase in mortality, slower development and a reduction in aerobic capacity with increasing pCO2. Our study points to potential reduction in juvenile recruitment success as seawater pCO2 increases, thus foreshadowing important socio-economic repercussions for the lobster fisheries and industry.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2019) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2020-07-07.
DOI: 10.1594/pangaea.879657
title: Light spectra absorption and HPLC pigments of phytoplankton in the northern Antarctic Peninsula

description: This dataset includes light absorption spectra, HPLC pigments and CHEMTAX community composition of phytoplankton collected during 2013 and 2014 austral summers in the northern Antarctic Peninsula. Our analysis in Ferreira et al, JGR (in press) showed that 1) variations in photosynthetic and photoprotective pigments are not discernible by changes in the chlorophyll-specific absorption of phytoplankton; 2) a cluster analysis identifies a regular increase in the degree of package effect of phytoplankton absorption; and 3) a regular increase in the degree of package effect is associated with an increase of fucoxanthin and decrease of photoprotective pigments relative to chlorophyll-a.
description: To download the data, please contact:amabilefr@gmail.com
description: Supplement to: Ferreira, Amabile; Ciotti, Áurea Maria; Mendes, Carlos Rafael; Uitz, Julia; Bricaud, Annick (2017): Phytoplankton light absorption and the package effect in relation to photosynthetic and photoprotective pigments in the northern tip of Antarctic Peninsula. Journal of Geophysical Research: Oceans, 122(9), 7344-7363