cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.889161
title: Metabolic prioritizations of Polar cod (Boreogadus saida) at ambient and elevated water temperatures

description: Two groups (n = 8, n = 5) of Polar cod (Boreogadus saida) were acclimated to both 0 and 6°C. The smaller groups were used to investigate specific dynamic action (SDA) (treatment "digestion"). Each fish of the larger groups was used for exercise tests in an unfed and fed state (treatment "exercise" and "exercise & digestion", respectively) at their respective acclimation temperatures as well as in a fed state acutely exposed to an intermediate temperature (3°C). SDA measurements lasted for 18 and 9 days at 0 and 6°C, identical to the food-deprivation period of B. saida in the exercise approach. Feeding was conducted in the common tank. Accordingly, daily rations reflect the mean food consumption per treatment. Each fish was allowed to feed for at least 2h before the start of the experiments.The acclimation time refers to the first day of the respective experiment. The SDA response is characterized by the maximum metabolic rate (MMR) evoked by digestion (defined as second record of oxygen consumption ṀO₂) and terminated by the standard metabolic rate (SMR) (20% quantile among ṀO₂ values obtained on the 18th day at 0°C and the 9th day at 6°C, respectively). Subsequently, the individual duration and the magnitude of the postprandial response (integral below the curve generated by aid of a specific script within the program R (R Core Team 2013)) was calculated.Fish used during exercise treatments were weaned to a Brett-type swimming tunnel for exactly two hours, before the onset of the exercise protocol. The exercise protocol involved a settling period of 5 min at a baseline swimming velocity, before the speed was carefully increased by 1.4 cm/s once per minute. Like this, the transition speed to partly anaerobic swimming (Ugait), as well as the critical swimming speed (Ucrit) was determined for every specimen. At each velocity step, burst-type swimming behavior was counted for 50 sec. The maximum burst count (max. BC) was used to estimate anaerobic capacities. As soon as Ucrit was reached, fish were placed in a separate respiration setup for the determination of MMR evoked by exercise and the MMR evoked by concomitant exercise and digestion (first ṀO₂ record after placement in respiration chamber) for 48 h. The respective SMR of unfed fish were calculated as 20% quantiles among all ṀO₂ records after 24 h. The difference between MMR and SMR values of exercised and postprandial fish represent the individual aerobic scopes (AS). The ṀO₂ at Ucrit (MMR) was used to calculate the energetic efficiency of maximum swimming performance (Emax).
DOI: 10.1594/pangaea.891264
title: Measurements of routine metabolic rates, metabolites (in blood), and cellular stress markers (in muscle) of invasive damselfish Neopomacentrus cyanomos, after acute decreasing changes of temperature; and after 45-days acclimation at colder regimes

description: The damselfish Neopomacentrus cyanomos were collected twice under an oil-loading platform 1.5 km from the Cayo Arcas reef (20.21°N, −91.98°W), in August 2016 (n = 16) and August 2017 (n = 30). All fish sampled in August 2016 were submitted to an acute-thermal-decline protocol (−4 °C over a period of 1 h, and maintaining the temperature for 23 h), while the ones collected in August were acclimated 45 days at 18, 20, 22, and 26 °C. Finally, half of the acclimated fish were submitted to a high temperature challenge to assess the effect of cold thermal acclimation on heat tolerance scope. Data of routine metabolic rates, blood metabolites and biochemical stress indicators from each fish are provided in this data set.
description: Version 2 (2020-01-09):- Remove parameters: Triglycerides; Cholesterol; RedOx potential; Metabolic rate of oxygen per wet mass, high-Change title: previously "Measurements of respiratory metabolism, metabolites (in blood), and cellular stress markers (in muscle) of invasive damselfish Neopomacentrus cyanomos, after acute decreasing changes of temperature; and after 45-days acclimation at colder regimes"
DOI: 10.1594/pangaea.898913
title: Effect of atorvastatin on whole organism respiration of the blue mussels, Mytilus edulis

description: Increasing concentration of biologically active pharmaceutical compounds can affect marine organisms. The bioavailability and environmental stability of these compounds make them potential threat to these organisms, specially the sessile organisms. We have examined the effects of atorvastatin, a globally prescribed drug, on the blue mussels – Mytilus edulis. In this data set, we presents the effect of atorvastatin (ATO) on the whole organism respiration of Mytilus edulis.
DOI: 10.1594/pangaea.942976
title: Potassium, rubidium, and cesium contents in soil along a continental transect in the Chilean Coastal Cordillera

description: A tracer experiment was conducted in three study sites along a continental transect from arid to humid-temperate conditions in the Chilean Coastal Cordillera. The objective was to determine the short-term (&lt;1 year) plant nitrogen (N) and potassium (K) acquisition from topsoil (A-Bw horizons), subsoil (Bw-BCw horizons), and saprolite (below BCw horizon). In February and March 2016, ¹⁵N (as Na¹⁵NO₃, 99 at%) and the K analogs rubidium (as RbCl) and cesium (as CsCl) were injected in three soil depths around the focal plants: Gutierrezia resinosa (H.&A.) B. in the northernmost site (arid shrubland), Aristeguietia salvia (C.) K.&R. in the intermediate site (mediterranean woodland), and Araucaria araucana (M.) K. in the southernmost site (temperate rainforest). The injection holes were drilled with an auger and the excavated soil material was collected to determine soil N, K, Rb, and Cs contents. In November 2016, shoot and root material of labeled and unlabeled plants was collected. The N, K, Rb, and Cs contents and the stable isotope ratios of δ¹⁵N (expressed as δ¹⁵N) in plant tissue were measured. The tracer recovery by plants was determined by the ¹⁵N enrichment and the shift of Rb and Cs contents normalized to the K content between reference plants and labeled plants. The data set contains the K, Rb, and Cs contents in soil.
DOI: 10.1594/pangaea.942978
title: Element contents and stable isotope analysis in plants from a nitrogen and potassium tracer experiment in the Chilean Coastal Cordillera

description: A tracer experiment was conducted in three study sites along a continental transect from arid to humid-temperate conditions in the Chilean Coastal Cordillera. The objective was to determine the short-term (&lt;1 year) plant nitrogen (N) and potassium (K) acquisition from topsoil (A-Bw horizons), subsoil (Bw-BCw horizons), and saprolite (below BCw horizon). In February and March 2016, δ¹⁵N (as Na¹⁵NO₃, 99 at%) and the K analogs rubidium (as RbCl) and cesium (as CsCl) were injected in three soil depths around the focal plants: Gutierrezia resinosa (H.&A.) B. in the northernmost site (arid shrubland), Aristeguietia salvia (C.) K.&R. in the intermediate site (mediterranean woodland), and Araucaria araucana (M.) K. in the southernmost site (temperate rainforest). The injection holes were drilled with an auger and the excavated soil material was collected to determine soil N, K, Rb, and Cs contents. In November 2016, shoot and root material of labeled and unlabeled plants was collected. The N, K, Rb, and Cs contents and the stable isotope ratios of N (expressed as δ¹⁵N) in plant tissue were measured. The tracer recovery by plants was determined by the δ¹⁵N enrichment and the shift of Rb and Cs contents normalized to the K content between reference plants and labeled plants.The data set contains the N, K, Rb, and Cs contents as well as the stable isotope ratios of N in plant biomass.
DOI: 10.1594/pangaea.965557
title: Sediment core description of GeoB24303-1 (GC02) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24303-1 (GC02) was collected during R/V Sonne expedition SO278 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the gravity core was longitudinally split directly after recovery on board of cruise SO278 and the archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965558
title: Sediment core description of GeoB24366-1 (GC32) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24366-1 (GC32) was collected during R/V Sonne expedition SO278 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the gravity core was longitudinally split directly after recovery on board of cruise SO278 and the archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965559
title: Sediment core description of GeoB24366-2 (MUC24) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24366-2 (MUC24) was collected during R/V Sonne expedition SO278 using a multi corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the multi core was longitudinally split and the archive halve was photographed using a camera at a 300-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965560
title: Sediment core description of GeoB24367-1 (MUC25) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24367-1 (MUC25) was collected during R/V Sonne expedition SO278 using a multi corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the multi core was longitudinally split and the archive halve was photographed using a camera at a 300-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965561
title: Sediment core description of GeoB24373-1 (GC35) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24373-1 (GC35) was collected during R/V Sonne expedition SO278 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the gravity core was longitudinally split directly after recovery on board of cruise SO278 and the archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965562
title: Sediment core description of GeoB24374-1 (GC36) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24374-1 (GC36) was collected during R/V Sonne expedition SO278 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the gravity core was longitudinally split directly after recovery on board of cruise SO278 and the archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965563
title: Sediment core description of GeoB24374-2 (MUC29) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24374-2 (MUC29) was collected during R/V Sonne expedition SO278 using a multi corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the multi core was longitudinally split and the archive halve was photographed using a camera at a 300-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965564
title: Sediment core description of GeoB24375-1 (GC37) recovered during R/V Sonne expedition SO278 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB24375-1 (GC37) was collected during R/V Sonne expedition SO278 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the gravity core was longitudinally split directly after recovery on board of cruise SO278 and the archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965679
title: Sediment core description of gravity core GeoB21366-1 (GC22) recovered during R/V Poseidon expedition POS499 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB21366-1 (GC22) was collected during R/V Poseidon expedition POS499 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). The gravity core was longitudinally split directly after recovery on board of cruise POS499. The archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution in 2019. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965680
title: Sediment core description of gravity core GeoB21367-1 (GC23) recovered during R/V Poseidon expedition POS499 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB21367-1 (GC23) was collected during R/V Poseidon expedition POS499 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). The gravity core was longitudinally split directly after recovery on board of cruise POS499. The archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution in 2019. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965694
title: Sediment core description of gravity core GeoB19289-1 (GC37) recovered during R/V Meteor expedition M112 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB19289-1 (GC37) was collected during R/V Meteor expedition M112 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). The gravity core was longitudinally split directly after recovery on board of cruise M112. The archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution in 2019. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.1594/pangaea.965709
title: Sediment core description of gravity core GeoB19290-1 (GC38) recovered during R/V Meteor expedition M112 at Sartori MV in the Calabrian Arc, Mediterranean Sea

description: Sediment core GeoB19290-1 (GC38) was collected during R/V Meteor expedition M112 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). The gravity core was longitudinally split directly after recovery on board of cruise M112. The archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution in 2019. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
DOI: 10.34740/kaggle/dsv/7900093
title: WallStreetBets 2022
DOI: 10.6084/m9.figshare.25442404
title: MATLAB resource for DFN model

description: Quantitative framework for predicting radon flux through open-mode fractures and the influence of rock geo-mechanical properties.
DOI: 10.5281/zenodo.10829156
title: Data for 'Careful selection of forest types in afforestation can increase carbon sequestration without compromising sustainability'
DOI: 10.5281/zenodo.10829157
title: Data for 'Careful selection of forest types in afforestation can increase carbon sequestration without compromising sustainability'
DOI: 10.5281/zenodo.10846289
title: Data for 'Careful selection of forest types in afforestation can increase carbon sequestration without compromising sustainability'
DOI: 10.5281/zenodo.10846304
title: Data for 'Careful selection of forest types in afforestation can increase carbon sequestration without compromising sustainability'
DOI: 10.26179/w56q-je48
title: Aurora Australis Voyage 1 2011/12 Track and Underway Data
DOI: 10.5517/ccdc.csd.cc2jg8kv
title: CCDC 2337417: Experimental Crystal Structure Determination

description: Related Article: K. SureshKumar, T. Khamrang, M. Hemamalini, D. Saravanan, G.J.M. Antony|2024|IUCrData|9|x240207|doi:10.1107/S2414314624002074
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.6084/m9.figshare.16699519
title: Improving geological logging of drill holes using geochemical data and data analytics for mineral exploration in the Gawler Ranges, South Australia

description: Geochemical data are frequently collected from mineral exploration drill-hole samples to more accurately define and characterise the geological units intersected by the drill hole. However, large multi-element data sets are slow and challenging to interpret without using some form of automated analysis, such as mathematical, statistical or machine learning techniques. Automated analysis techniques also have the advantage in that they are repeatable and can provide consistent results, even for very large data sets. In this paper, an automated litho-geochemical interpretation workflow is demonstrated, which includes data exploration and data preparation using appropriate compositional data-analysis techniques. Multiscale analysis using a modified wavelet tessellation has been applied to the data to provide coherent geological domains. Unsupervised machine learning (clustering) has been used to provide a first-pass classification. The results are compared with the detailed geologist’s logs. The comparison shows how the integration of automated analysis of geochemical data can be used to enhance traditional geological logging and demonstrates the identification of new geological units from the automated litho-geochemical logging that were not apparent from visual logging but are geochemically distinct. To reduce computational complexity and facilitate interpretation, a subset of geochemical elements is selected, and then a centred log-ratio transform is applied. The wavelet tessellation method is used to domain the drill holes into rock units at a range of scales. Several clustering methods were tested to identify distinct rock units in the samples and multiscale domains for classification. Results are compared with geologist’s logs to assess how geochemical data analysis can inform and improve traditional geology logs.