cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.xay6wh
title: Occurrence Download

description: A dataset containing 1705 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((0.42834 42.36269,1.75796 42.36269,1.75796 43.4624,0.42834 43.4624,0.42834 42.36269))",
 "TaxonKey is Ursus arctos"
 ]
}

 The dataset includes 1705 records from 69 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006585-260120142942310/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.5281/zenodo.15425805
title: Phenotypic evolutionary response to temporally limited pollinator access in Brassica rapa

description: Dataset 1: raw data pollinator abundance and diversity

Dataset 2: result of multi-ways ANOVAs (models 1 and 2) – experimental evolution

Dataset 3: raw data individual traits – experimental evolution

Dataset 4: raw data flower morphology – experimental evolution

Dataset 5: raw data fruit length – experimental evolution

Dataset 6: temperature and light recording – experimental evolution

Dataset 7: raw data individual traits – second resurrection

Dataset 8: raw data flower morphology – second resurrection

Dataset 9: raw data fruit length – second resurrection

Dataset 10: raw data individual traits – third resurrection

Dataset 11: raw data fruit length – third resurrection

R script used to produce the results of Authier et al. (unpublished)
DOI: 10.5281/zenodo.18347038
title: Phenotypic evolutionary response to temporally limited pollinator access in Brassica rapa

description: Dataset 1: raw data pollinator abundance and diversity

Dataset 2: result of multi-ways ANOVAs (models 1 and 2) – experimental evolution

Dataset 3: raw data individual traits – experimental evolution

Dataset 4: raw data flower morphology – experimental evolution

Dataset 5: raw data fruit length – experimental evolution

Dataset 6: temperature and light recording – experimental evolution

Dataset 7: raw data individual traits – second resurrection

Dataset 8: raw data flower morphology – second resurrection

Dataset 9: raw data fruit length – second resurrection

Dataset 10: raw data individual traits – third resurrection

Dataset 11: raw data fruit length – third resurrection

R script used to produce the results of Authier et al. (unpublished)
DOI: 10.1285/i15900932v45s1p83
title: BGG Sequences | A Riemannian perspective

description: BGG resolutions and generalized BGG resolutions from representation theory of semisimple Lie algebras have been generalized to sequences of invariant differential operators on manifolds endowed with a geometric structure belonging to the family of parabolic geometries. Two of these structures, occur as conformal structures and projective structures occur as weakenings of a Riemannian metric respectively of a specified torsion-free connection on the tangent bundle. In particular, one obtains BGG sequences on open subsets of $\Bbb R^n$ as very special cases of the construction. It turned out that several examples of the latter sequences are of interest in applied mathematics, since they can be used to construct numerical methods to study operators relevant for elasticity theory, numerical relativity and related fields. This article is intended to provide an intermediate level between BGG sequences for parabolic geometries and the case of domains in $\Bbb R^n$. We provide a construction of conformal BGG sequences on Riemannian manifolds and of projective BGG sequences on manifolds endowed with a volume preserving linear connection on their tangent bundle. These constructions do not need any input from parabolic geometries. Except from standard differential geometry methods the only deeper input comes from representation theory. So one can either view the results as a simplified version of the constructions for parabolic geometries in an explicit form. Alternatively, one can view them as providing an extension of the simplified constructions for domains in $\Bbb R^n$ to general Riemannian manifolds or to manifolds endowed with an appropriate connection on the tangent bundle.
DOI: 10.5281/zenodo.10202927
title: Accelerated lignocellulosic molecule adsorption structure determination dataset

description: Dataset containing all structures from the accelerated structure search for lignocellulosic molecules. Part of the data corresponds to DFT data, while the largest portion of structures correspond to data acquired using a machine learned interatomic potential (NequIP) trained on the former. The energies attached to each structure are atomisation energies. Contains both isolated adsorbates and adsorption structures. The dataset also contains configuration files for the NequIP training.
DOI: 10.5281/zenodo.10202926
title: Accelerated lignocellulosic molecule adsorption structure determination dataset

description: Dataset containing all structures from the accelerated structure search for lignocellulosic molecules. Part of the data corresponds to DFT data, while the largest portion of structures correspond to data acquired using a machine learned interatomic potential (NequIP) trained on the former. The energies attached to each structure are atomisation energies. Contains both isolated adsorbates and adsorption structures. The dataset also contains configuration files for the NequIP training.
DOI: 10.5281/zenodo.18346458
title: LDSC test data and reference data

description: The data set was used for ldsc analysis, which included test data and reference (download from https://zenodo.org/records/7768714).
DOI: 10.5281/zenodo.18346459
title: LDSC test data and reference data

description: The data set was used for ldsc analysis, which included test data and reference (download from https://zenodo.org/records/7768714).
DOI: 10.1285/i15900932v45s1p117
title: Canonical Reductive Decomposition of Extrinsic Homogeneous Submanifolds

description: Let $\overline{M}=\overline{G}/\overline{H}$ be a homogeneous Riemannian manifold. Given a Lie subgroup $G\subset \overline{G}$ and a reductive decomposition of the homogeneous structure of $\overline{M}$, we analyze a canonical reductive decomposition for the orbits of the action of $G$. These leaves of the $G$-action are extrinsic homogeneous submanifolds and the analysis of the reductive decomposition of them is related with their extrinsic properties. We connect the study with works in the literature and initiate the relationship with the Ambrose-Singer theorem and homogeneous structures of submanifolds.
DOI: 10.15468/dl.r2cq6g
title: Occurrence Download

description: A dataset containing 2 species occurrences available in GBIF matching the query:
{"type":"and","predicates":[{"type":"within","geometry":"POLYGON ((89.24907 24.4579, 89.17192799999999 24.452323, 89.096706 24.435731, 89.025272 24.408536, 88.959401 24.371414, 88.900724 24.325289, 88.85068699999999 24.271303, 88.81052 24.210796, 88.781201 24.145265, 88.76344 24.07633, 88.757655 24.005692, 88.76397 23.935093, 88.78220899999999 23.866268, 88.81190700000001 23.800908, 88.852318 23.740617, 88.902438 23.686871, 88.961032 23.640984, 89.02666000000001 23.604078, 89.097713 23.577055, 89.17245800000001 23.560573, 89.24907 23.555033, 89.325682 23.560573, 89.40042699999999 23.577055, 89.47148 23.604078, 89.537108 23.640984, 89.595702 23.686871, 89.645822 23.740617, 89.686233 23.800908, 89.715931 23.866268, 89.73417000000001 23.935093, 89.74048500000001 24.005692, 89.7347 24.07633, 89.716939 24.145265, 89.68762 24.210796, 89.647453 24.271303, 89.597416 24.325289, 89.53873900000001 24.371414, 89.47286800000001 24.408536, 89.40143399999999 24.435731, 89.326212 24.452323, 89.24907 24.4579))"},{"type":"equals","key":"CLASS_KEY","value":"212","matchCase":false},{"type":"greaterThanOrEquals","key":"YEAR","value":"2015","matchCase":false},{"type":"not","predicate":{"type":"in","key":"BASIS_OF_RECORD","values":["MATERIAL_CITATION","MATERIAL_SAMPLE","PRESERVED_SPECIMEN"],"matchCase":false}},{"type":"lessThanOrEquals","key":"COORDINATE_UNCERTAINTY_IN_METERS","value":"10000","matchCase":false},{"type":"equals","key":"LICENSE","value":"CC BY 4.0","matchCase":false}]}

 The dataset includes 2 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006587-260120142942310/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1285/i15900932v45s1p129
title: Analysis of the harmonic flow of geometric structures

description: We develop an analysis of the flow of harmonic $H$-structures with the strategy introduced by Chen-Struwe for the harmonic map heat equation when the target does not necessarily have negative sectional curvature, so the Eells-Sampson Theorem cannot apply. In particular, this flow method enables us to find theoretical hypotheses under which the existence of a torsion-free $H$-structure is guaranteed and conditions for which the flow must blow up in finite time. This extends results already known for some specific groups like $\mathrm{U}(n)$, $\mathrm{G}_2$ or $\mathrm{Spin}(7)$.
DOI: 10.15468/dl.kehrtz
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
{"type":"and","predicates":[{"type":"within","geometry":"POLYGON ((89.84317299999999 25.090672, 89.76563899999999 25.085095, 89.69003499999999 25.068502, 89.618241 25.041307, 89.552038 25.004186, 89.493067 24.95806, 89.44278300000001 24.904075, 89.40241899999999 24.84357, 89.372961 24.778042, 89.355119 24.709111, 89.349313 24.638479, 89.355667 24.567886, 89.374004 24.499068, 89.40385499999999 24.433717, 89.44447099999999 24.373434, 89.49484200000001 24.319695, 89.553726 24.273816, 89.619677 24.236917, 89.691078 24.209898, 89.766188 24.193419, 89.84317299999999 24.187881, 89.920159 24.193419, 89.995268 24.209898, 90.06667 24.236917, 90.13262 24.273816, 90.19150399999999 24.319695, 90.241876 24.373434, 90.28249099999999 24.433717, 90.312342 24.499068, 90.330679 24.567886, 90.33703300000001 24.638479, 90.331228 24.709111, 90.313385 24.778042, 90.28392700000001 24.84357, 90.24356400000001 24.904075, 90.193279 24.95806, 90.134308 25.004186, 90.068106 25.041307, 89.99631100000001 25.068502, 89.92070699999999 25.085095, 89.84317299999999 25.090672))"},{"type":"equals","key":"CLASS_KEY","value":"212","matchCase":false},{"type":"greaterThanOrEquals","key":"YEAR","value":"2015","matchCase":false},{"type":"not","predicate":{"type":"in","key":"BASIS_OF_RECORD","values":["MATERIAL_CITATION","MATERIAL_SAMPLE","PRESERVED_SPECIMEN"],"matchCase":false}},{"type":"lessThanOrEquals","key":"COORDINATE_UNCERTAINTY_IN_METERS","value":"10000","matchCase":false},{"type":"equals","key":"LICENSE","value":"CC BY 4.0","matchCase":false}]}

 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006591-260120142942310/datasets/export for details.
DOI: 10.1285/i15900932v45s1p147
title: Potential theory and applications in conformal geometry

description: In this paper, we want to give an exposition of our recent work on linear and nonlinear potential theory and their applications in conformal geometry. We use potential theory to study linear and quasilinear equations arising from conformal geometry. We establish the asymptotic behavior near singularities and derive applications in conformal geometry. In particular, we establish some Huber's type theorems and Hausdorff dimension estimates of the ends in conformal geometry in general dimensions.
DOI: 10.48425/yj4xsopg
title: S_climate_snow_depth_ground_ice_coastal_areas

description: Snow depth and basal gorund ice measurements in coastal areas (Brøggerhalvøya and Sarsøyra) on the western coast of Spitsbergen.

The dataset consists of three types of files: 
- One data file per year (S_climate_snow_depth_ground_ice_coastal_areas_YEAR.txt) 
- One coordinate file containing the coordinates of all sites (S_climate_snow_depth_ground_ice_coastal_areas_coordinates.txt) 
- One auxiliary file with additional information about all sites (S_climate_snow_depth_ground_ice_coastal_areas_aux.txt)

In addition, there is a README file (S_climate_snow_depth_ground_ice_coastal_areas_readme.pdf) with further information regarding the dataset.
DOI: 10.15468/dl.d8c6y8
title: Occurrence Download

description: A dataset containing 480 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Geometry POLYGON((-9.97563 35.68358,42.14347 35.68358,42.14347 55.91977,-9.97563 55.91977,-9.97563 35.68358))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Octodrilus transpadanus"
 ]
}

 The dataset includes 480 records from 15 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006592-260120142942310/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1285/i15900932v45s1p169
title: On exact locally conformally Kähler manifolds

description: In this article, we explore a distinguished class of complex manifolds known as $\( d_\theta \)$-exact locally conformally Kähler (LCK) manifolds. These manifolds are characterized by the property that their fundamental 2-form $\( \omega \)$ can be expressed as $\( \omega = d_\theta \alpha \)$, where $\( \alpha \)$ is a 1-form on $\( M \)$ and $\( d_\theta = d + \theta \wedge \)$. We establish a key result: if the 1-form $\( \alpha \)$ is holomorphic, then the Morse-Novikov cohomology $\( H_\theta^*(M) \)$ vanishes. Furthermore, we provide sufficient conditions under which a $\( d_\theta \)$-exact LCK manifold admits a Vaisman structure. This work deepens the understanding of the interplay between geometric structures, cohomological properties, and special classes of LCK manifolds.
DOI: 10.48425/kb33fz5c
title: S_climate_snow_depth_ground_ice_nordenskioldland

description: Snow depth and basal ground ice measurements in Gangdalen, Reindalen, Semmeldalen, Istjørndalen, Medalen, Fardalen, and Colesdalen, located in Nordenskiöld Land in the central part of Spitsbergen.

The dataset consists of three types of files: 
- One data file per year (S_climate_snow_depth_ground_ice_nordenskioldland_YEAR.txt) 
- One coordinate file containing the coordinates of all sites (S_climate_snow_depth_ground_ice_nordenskioldland_coordinates.txt) 
- One auxiliary file with additional information about all sites (S_climate_snow_depth_ground_ice_nordenskioldland_aux.txt)

In addition, there is a README file (S_climate_snow_depth_ground_ice_nordenskioldland_readme.pdf) with further information regarding the dataset.

Note: Due to the COVID-19 situation in 2020, no snow depth or basal ground ice measurements were conducted. Consequently, this file is missing
DOI: 10.15468/dl.35ddad
title: Occurrence Download

description: A dataset containing 7335 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Pan troglodytes"
 ]
}

 The dataset includes 7335 records from 125 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006590-260120142942310/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.xzy52h
title: Occurrence Download

description: A dataset containing 78 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Trithuria filamentosa",
 "HasCoordinate is true",
 "BasisOfRecord is one of (Specimen)"
 ]
}

 The dataset includes 78 records from 8 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006593-260120142942310/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.34740/kaggle/dsv/14591029
title: Peer-to-Peer Boliviano (BOB) Exchange Data
DOI: 10.15468/dl.73mdyj
title: Occurrence Download

description: A dataset containing 232 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is Asia",
 "Country is China",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "TaxonKey is Poa annua",
 "Year 1970-2000"
 ]
}

 The dataset includes 232 records from 14 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0006594-260120142942310/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1285/i15900932v45s1p181
title: Commuting statistical Jacobi operators

description: This paper extends the classical theory of Jacobi operators to statistical manifolds, integrating concepts from differential and information geometry. We analyze the commutation properties of statistical Jacobi operators and establish their implications for the geometry of statistical hypersurfaces. By generalizing results on commuting curvature operators, we derive new insights into the structure of statistical manifolds. Our findings contribute to a deeper understanding of the interplay between curvature, shape operators, and statistical connections.
DOI: 10.25326/859
title: ACROSS_LISA_PRG_NOx_1-Min_L2

description: The nitrogen oxide (NO), nitrogen dioxide (NO2) and their sum (NOx) was measured by a commercial chemiluminescence NOx analyzer (AC32M Environment SA, detection limit 0.4 ppb) at the PRG urban site. Air was taken from the sampling point (located on the roof of the Lamark B building of Paris Cité university at about 30 m height above the ground) to a common glass manifold of 4.3 dm3 volume (located about 10 m below, in the main building) by a teflon tube inlet of 17.5 mm inner diameter and 12 m length. The flow in this main line was fixed at 40 L min-1. The gas phase instruments sampled air from this common manifold. The NOx monitor flow rate was set at 1 l min–1. Data were acquired continuously at 1-sec time resolution and averaged over 1-minute. The NOx monitor was calibrated before the ACROSS campaign and the calibration was verified both before and after the campaign. A zero check was performed both before and after the campaign, to evaluate and correct possible offset baseline. The uncertainties given in the data file (5%) account for instrumental (linearity, instrumental drift) and calibration uncertainties. Raw data were controlled manually to remove periods where the manifold was not connected to the sampling line or when specific conditions affected the quality of the data. Invalid data are reported as -9999.999. Valid data are reported with a “O” flag (operation) and invalidated data are reported with a “M” flag (missing). Different periods were affected by rain on the 19–23, 24–27 and 30 June and 4, 19–20 and 22 July. Detailed information on the rainy periods can provided upon request to the principal investigators.
DOI: 10.1285/i15900932v45s1p193
title: An Invitation to Biharmonic and Biconservative Submanifolds

description: This note is based on a lecture delivered by the author at the Second Conference on Differential Geometry, held in Fez in October 2024. It offers an accessible introduction to biharmonic and biconservative submanifolds, exploring the motivations for their study and highlighting some key facts and open problems in the field.
DOI: 10.25326/860
title: ACROSS_LISA_PRG_O3_1-Min_L2

description: Ozone mixing ratio was measured by a commercial UV absorption monitor (O3 41M Environment SA, detection limit 0.4 ppb) at the PRG urban site. Air was taken from the sampling point (located on the roof of the Lamark B building of Paris Cité university at about 30 m height above the ground) to a common glass manifold of 4.3 dm3 volume (located about 10 m below, in the main building) by a teflon tube inlet of 17.5 mm inner diameter and 12 m length. The flow in this main line was fixed at 40 L min-1. The gas phase instruments sampled air from this common manifold. The ozone monitor flow rate was set at 2 l min–1. Data were acquired continuously at 1-sec time resolution and averaged over 1-minute. The ozone monitor was calibrated before the ACROSS campaign and the calibration was verified both before and after the campaign. A zero check was performed both before and after the campaign, to evaluate and correct possible offset baseline. The uncertainties given in the data file (5%) account for instrumental (linearity, instrumental drift) and calibration uncertainties. Raw data were controlled manually to remove periods where the manifold was not connected to the sampling line or when specific conditions affected the quality of the data. Invalid data are reported as -9999.999. Valid data are reported with a “O” flag (operation) and invalidated data are reported with a “M” flag (missing). Different periods were affected by rain on the 19–23, 24–27 and 30 June and 4, 19–20 and 22 July. Detailed information on the rainy periods can be provided upon request to the principal investigators.
DOI: 10.25326/861
title: ACROSS_LISA_PRG_SO2_1-Min_L2

description: The sulfur dioxide (SO2) mixing ratio was measured by a commercial fluorescence UV monitor (AF22E Environnement SA, detection limit 0.4 ppb) at the PRG urban site. Air was taken from the sampling point (located on the roof of the Lamark B building of Paris Cité university at about 30 m height above the ground) to a common glass manifold of 4.3 dm3 volume (located about 10 m below, in the main building) by a teflon tube inlet of 17.5 mm inner diameter and 12 m length. The flow in this main line was fixed at 40 L min-1. The gas phase instruments sampled air from this common manifold. The sulfur dioxide monitor flow rate was set at 0.4 l min–1. Data were acquired continuously at 1-sec time resolution and averaged over 1-minute. The SO2 monitor was calibrated before the ACROSS campaign and the calibration was verified both before and after the campaign. A zero check was performed both before and after the campaign, to evaluate and correct possible offset baseline. The uncertainties given in the data file (5%) account for instrumental (linearity, instrumental drift) and calibration uncertainties. Raw data were controlled manually to remove periods where the manifold was not connected to the sampling line or when specific conditions affected the quality of the data. Invalid data are reported as -9999.999. Valid data are reported with a “O” flag (operation) and invalidated data are reported with a “M” flag (missing). Different periods were affected by rain on the 19–23, 24–27 and 30 June and 4, 19–20 and 22 July. Detailed information on the rainy periods can provided upon request to the principal investigators.
DOI: 10.25326/862
title: ACROSS_LISA_PRG_NH3_H2O_CH4_1-Min_L2

description: The atmospheric ammonia (NH3) concentration as volume mixing ratio was measured at the ground–based PRG urban site during ACROSS by a commercial in situ analyser (PROCEAS® NH3 from DURAG group, AP2E society, Aix-en-Provence, France), based on two technologies: Optical-Feedback Cavity-Enhanced Absorption Spectroscopy (OFCEAS) and low-pressure sampling. Air was taken from the sampling point (located on the roof of the Lamark B building of Paris Cité university at about 30 m height above the ground) to a common glass manifold of 4.3 dm3 volume (located about 10 m below, in the main building) by a teflon tube inlet of 17.5 mm inner diameter and 12 m length. The flow in this main line was fixed at 40 L min-1. The gas phase instruments sampled air from this common manifold. Data were acquired continuously at 10 sec time resolution then averaged to 1 minute. The time indicated in the datafile is the start time (UTC) of the 1-min interval. Available data started from June 12, 2022, until July 24, 2022. H2O and CH4 concentrations were simultaneously measured with ammonia as both species interfer in the NH3 spectral micro-window. They are therefore given as indicators of coherent data. Concentrations for NH3, H2O and CH4 are provided in ppb, % and ppb, respectively. Few data are missing between June 18, 2022 and June 20, 2022 due to an electrical disconnection. The data were not further calibrated since measuring ammonia with a standard is still challenging.