Execution du pipeline. Actualisation des dois et des graphes.

1-enrich-with-datacite/all_datacite_clients_for_uga.csv

 client,count,name,year,url
-cern.zenodo,818,Zenodo,2013,https://zenodo.org/
+cern.zenodo,823,Zenodo,2013,https://zenodo.org/
 inist.sshade,498,Solid Spectroscopy Hosting Architecture of Databases and Expertise,2019,https://www.sshade.eu/
 figshare.ars,366,figshare Academic Research System,2016,http://figshare.com/
 inist.osug,238,Observatoire des Sciences de l'Univers de Grenoble,2014,http://doi.osug.fr
-dryad.dryad,166,DRYAD,2018,https://datadryad.org
+dryad.dryad,167,DRYAD,2018,https://datadryad.org
 inist.resif,93,Réseau sismologique et géodésique français,2014,https://www.resif.fr/
 rdg.prod,74,Recherche Data Gouv France,2022,https://recherche.data.gouv.fr/en
 inist.humanum,69,NAKALA,2020,https://nakala.fr
 inist.persyval,62,PERSYVAL-Lab : Pervasive Systems and Algorithms Lab,2016,
 fmsh.prod,28,Fondation Maison des sciences de l'homme,2023,
 inist.ccj,22,Centre Camille Jullian – UMR 7299,2020,
+pangaea.repository,18,PANGAEA,2020,https://www.pangaea.de/
 mcdy.dohrmi,12,dggv-e-publications,2020,https://www.dggv.de/publikationen/dggv-e-publikationen.html
-pangaea.repository,9,PANGAEA,2020,https://www.pangaea.de/
 figshare.sage,6,figshare SAGE Publications,2018,
+inist.cirm,6,Centre International de Rencontres Mathématiques,2017,
 iris.iris,5,Incorporated Research Institutions for Seismology,2018,http://www.iris.edu/hq/
 cnic.sciencedb,3,ScienceDB,2022,https://www.scidb.cn/en
-vqpf.dris,3,Direction des ressources et de l'information scientifique,2021,
-tib.gfzbib,3,GFZpublic,2011,https://gfzpublic.gfz-potsdam.de
 tib.repod,3,RepOD,2015,https://repod.icm.edu.pl/
-inist.eost,2,Ecole et Observatoire des Sciences de la Terre,2017,https://eost.unistra.fr/en/
+tib.gfzbib,3,GFZpublic,2011,https://gfzpublic.gfz-potsdam.de
+vqpf.dris,3,Direction des ressources et de l'information scientifique,2021,
 ugraz.unipub,2,unipub,2019,http://unipub.uni-graz.at
-bl.nerc,2,NERC Environmental Data Service,2011,https://eds.ukri.org
+inist.eost,2,Ecole et Observatoire des Sciences de la Terre,2017,https://eost.unistra.fr/en/
 ethz.sed,2,"Swiss Seismological Service, national earthquake monitoring and hazard center",2013,http://www.seismo.ethz.ch
-ethz.zora,1,"Universität Zürich, ZORA",2013,https://www.zora.uzh.ch/
+bl.nerc,2,NERC Environmental Data Service,2011,https://eds.ukri.org
 inist.ird,1,IRD,2016,
-estdoi.ttu,1,TalTech,2019,https://digikogu.taltech.ee
-crui.ingv,1,Istituto Nazionale di Geofisica e Vulcanologia (INGV),2013,http://data.ingv.it/
+ethz.zora,1,"Universität Zürich, ZORA",2013,https://www.zora.uzh.ch/
 repod.dbuw,1,University of Warsaw Research Data Repository,2023,https://danebadawcze.uw.edu.pl/
+estdoi.ttu,1,TalTech,2019,https://digikogu.taltech.ee
 tug.openlib,1,TU Graz OPEN Library,2020,https://openlib.tugraz.at/
-inist.opgc,1,Observatoire de Physique du Globe de Clermont-Ferrand,2017,
+crui.ingv,1,Istituto Nazionale di Geofisica e Vulcanologia (INGV),2013,http://data.ingv.it/
 ethz.da-rd,1,ETHZ Data Archive - Research Data,2013,http://data-archive.ethz.ch
+inist.opgc,1,Observatoire de Physique du Globe de Clermont-Ferrand,2017,
+tib.gfz,1,GFZ Data Services,2011,https://dataservices.gfz-potsdam.de/portal/
 ardcx.nci,1,National Computational Infrastructure,2020,
 inist.omp,1,Observatoire Midi-Pyrénées,2011,
 ihumi.pub,1,IHU Méditerranée Infection,2020,
 bl.mendeley,1,Mendeley Data,2015,https://data.mendeley.com/
 umass.uma,1,University of Massachusetts (UMass) Amherst,2018,https://scholarworks.umass.edu/
-edi.edi,1,Environmental Data Initiative,2017,https://portal.edirepository.org/nis/home.jsp
 bl.iita,1,International Institute of Tropical Agriculture datasets,2017,http://data.iita.org/
-tib.gfz,1,GFZ Data Services,2011,https://dataservices.gfz-potsdam.de/portal/
+edi.edi,1,Environmental Data Initiative,2017,https://portal.edirepository.org/nis/home.jsp

1-enrich-with-datacite/nb-dois.txt

-2502
+2523
\ No newline at end of file

dois-uga--last-500.csv

 doi,client,resourceTypeGeneral,created,publisher,rights,sizes
+10.5281/zenodo.14167823,cern.zenodo,Other,2024-12-13,Zenodo,Creative Commons Attribution 4.0 International,
+10.5281/zenodo.14410833,cern.zenodo,Dataset,2024-12-12,Zenodo,Creative Commons Attribution 4.0 International,
+10.1594/pangaea.971995,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['19211 data points']
+10.1594/pangaea.971993,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['16415 data points']
+10.1594/pangaea.971990,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['14951 data points']
+10.1594/pangaea.971989,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['30792 data points']
+10.1594/pangaea.971988,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['27433 data points']
+10.1594/pangaea.971920,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['26808 data points']
+10.1594/pangaea.971919,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['176 data points']
+10.1594/pangaea.971918,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['210 data points']
+10.1594/pangaea.971916,pangaea.repository,Dataset,2024-12-11,PANGAEA,Creative Commons Attribution 4.0 International,['188 data points']
+10.5281/zenodo.14339958,cern.zenodo,Image,2024-12-09,Zenodo,Creative Commons Attribution 4.0 International,
+10.5061/dryad.280gb5mvx,dryad.dryad,Dataset,2024-12-09,Dryad,Creative Commons Zero v1.0 Universal,['12624044 bytes']
 10.5281/zenodo.14280087,cern.zenodo,Dataset,2024-12-08,Zenodo,Creative Commons Attribution 4.0 International,
 10.5281/zenodo.14291987,cern.zenodo,Software,2024-12-07,Zenodo,MIT License,
-10.6084/m9.figshare.27958021,figshare.ars,Text,2024-12-04,figshare,Creative Commons Attribution 4.0 International,['149756 Bytes']
 10.6084/m9.figshare.c.7569397,figshare.ars,Collection,2024-12-04,figshare,Creative Commons Attribution 4.0 International,
+10.6084/m9.figshare.27958021,figshare.ars,Text,2024-12-04,figshare,Creative Commons Attribution 4.0 International,['149756 Bytes']
 10.6084/m9.figshare.27958018,figshare.ars,Text,2024-12-04,figshare,Creative Commons Attribution 4.0 International,['369386 Bytes']
 10.6084/m9.figshare.c.7569352,figshare.ars,Collection,2024-12-04,figshare,Creative Commons Attribution 4.0 International,
 10.6084/m9.figshare.27957940,figshare.ars,Text,2024-12-04,figshare,Creative Commons Attribution 4.0 International,['18680 Bytes']
@@ -112,8 +125,8 @@ doi,client,resourceTypeGeneral,created,publisher,rights,sizes
 10.5281/zenodo.13785330,cern.zenodo,Dataset,2024-09-18,Zenodo,Creative Commons Attribution 4.0 International,
 10.26302/sshade/experiment_op_20050205_001,inist.sshade,Dataset,2024-09-13,SSHADE/FAME (OSUG Data Center),"Any use of downloaded SSHADE data in a scientific or technical paper or a presentation is free but you should cite both SSHADE and the used data in the text ( 'first author' et al., year) with its full reference (with its DOI) in the main reference section of the paper (or in a special 'data citation' section) and, when available, the original paper(s) presenting the data.",['1 spectrum']
 10.26302/sshade/experiment_op_20170206_001,inist.sshade,Dataset,2024-09-13,SSHADE/FAME (OSUG Data Center),"Any use of downloaded SSHADE data in a scientific or technical paper or a presentation is free but you should cite both SSHADE and the used data in the text ( 'first author' et al., year) with its full reference (with its DOI) in the main reference section of the paper (or in a special 'data citation' section) and, when available, the original paper(s) presenting the data.",['1 spectrum']
-10.6084/m9.figshare.27012151,figshare.ars,Text,2024-09-13,figshare,Creative Commons Attribution 4.0 International,['450818 Bytes']
 10.6084/m9.figshare.c.7447186,figshare.ars,Collection,2024-09-13,figshare,Creative Commons Attribution 4.0 International,
+10.6084/m9.figshare.27012151,figshare.ars,Text,2024-09-13,figshare,Creative Commons Attribution 4.0 International,['450818 Bytes']
 10.5281/zenodo.13748961,cern.zenodo,Text,2024-09-11,Zenodo,"Creative Commons Attribution 4.0 International,Creative Commons Attribution Share Alike 4.0 International",
 10.6084/m9.figshare.26985715,figshare.ars,Text,2024-09-11,figshare,Creative Commons Attribution 4.0 International,['25284 Bytes']
 10.6084/m9.figshare.c.6585842,figshare.ars,Collection,2024-09-11,figshare,Creative Commons Attribution 4.0 International,
@@ -159,8 +172,8 @@ doi,client,resourceTypeGeneral,created,publisher,rights,sizes
 10.57760/sciencedb.11705,cnic.sciencedb,Dataset,2024-08-15,Science Data Bank,Creative Commons Attribution Non Commercial Share Alike 4.0 International,"['99398887984 bytes', '14 files']"
 10.6084/m9.figshare.26722614,figshare.ars,Text,2024-08-15,figshare,Creative Commons Attribution 4.0 International,['12341 Bytes']
 10.6084/m9.figshare.25854698,figshare.ars,Image,2024-08-15,figshare,Creative Commons Attribution 4.0 International,['464136 Bytes']
-10.6084/m9.figshare.26713777,figshare.ars,Dataset,2024-08-15,figshare,Creative Commons Attribution 4.0 International,['553168 Bytes']
 10.6084/m9.figshare.c.7204785,figshare.ars,Collection,2024-08-15,figshare,Creative Commons Attribution 4.0 International,
+10.6084/m9.figshare.26713777,figshare.ars,Dataset,2024-08-15,figshare,Creative Commons Attribution 4.0 International,['553168 Bytes']
 10.6084/m9.figshare.25711209,figshare.ars,Text,2024-08-15,figshare,Creative Commons Attribution 4.0 International,['33449 Bytes']
 10.6084/m9.figshare.c.7116481,figshare.ars,Collection,2024-08-15,figshare,Creative Commons Attribution 4.0 International,
 10.6084/m9.figshare.26691925,figshare.ars,Text,2024-08-15,figshare,Creative Commons Attribution 4.0 International,['2061125 Bytes']
@@ -234,10 +247,10 @@ doi,client,resourceTypeGeneral,created,publisher,rights,sizes
 10.6084/m9.figshare.26585829,figshare.ars,Text,2024-08-13,figshare,Creative Commons Attribution 4.0 International,['279842 Bytes']
 10.6084/m9.figshare.26585826,figshare.ars,Text,2024-08-13,figshare,Creative Commons Attribution 4.0 International,['105007 Bytes']
 10.6084/m9.figshare.26585823,figshare.ars,Text,2024-08-13,figshare,Creative Commons Attribution 4.0 International,['11099 Bytes']
-10.6084/m9.figshare.c.6596504,figshare.ars,Collection,2024-08-13,figshare,Creative Commons Attribution 4.0 International,
 10.6084/m9.figshare.26577821,figshare.ars,Dataset,2024-08-13,figshare,Creative Commons Attribution 4.0 International,['56397 Bytes']
-10.6084/m9.figshare.c.6586928,figshare.ars,Collection,2024-08-13,figshare,Creative Commons Attribution 4.0 International,
+10.6084/m9.figshare.c.6596504,figshare.ars,Collection,2024-08-13,figshare,Creative Commons Attribution 4.0 International,
 10.6084/m9.figshare.26567603,figshare.ars,Text,2024-08-13,figshare,Creative Commons Attribution 4.0 International,['360541 Bytes']
+10.6084/m9.figshare.c.6586928,figshare.ars,Collection,2024-08-13,figshare,Creative Commons Attribution 4.0 International,
 10.15778/resif.z42022,inist.resif,Dataset,2024-08-12,RESIF - Réseau Sismologique et géodésique Français,,"['98 stations, 280Go (miniseed format)']"
 10.12686/eshm20-output,ethz.sed,Dataset,2024-08-12,EFEHR (European Facilities of Earthquake Hazard and Risk),Creative Commons Attribution 4.0 International,['529MB']
 10.5281/zenodo.7447726,cern.zenodo,Dataset,2024-08-12,Zenodo,Creative Commons Attribution 4.0 International,
@@ -391,6 +404,7 @@ doi,client,resourceTypeGeneral,created,publisher,rights,sizes
 10.5281/zenodo.11058212,cern.zenodo,Dataset,2024-04-24,Zenodo,Creative Commons Attribution 4.0 International,
 10.5061/dryad.qz612jmps,dryad.dryad,Dataset,2024-04-23,Dryad,Creative Commons Zero v1.0 Universal,['358827 bytes']
 10.5281/zenodo.10886304,cern.zenodo,Dataset,2024-04-23,Zenodo,Creative Commons Attribution 4.0 International,
+10.24350/cirm.v.20153203,inist.cirm,Audiovisual,2024-04-22,CIRM,Creative Commons Attribution Non Commercial No Derivatives 4.0 International,
 10.58132/bpyo1c,repod.dbuw,Dataset,2024-04-21,Dane Badawcze UW,,
 10.5281/zenodo.10568798,cern.zenodo,Dataset,2024-04-19,Zenodo,ODC Open Database License v1.0,
 10.5281/zenodo.10991301,cern.zenodo,Other,2024-04-19,Zenodo,Creative Commons Attribution 4.0 International,
@@ -403,10 +417,12 @@ doi,client,resourceTypeGeneral,created,publisher,rights,sizes
 10.5281/zenodo.10958418,cern.zenodo,Dataset,2024-04-11,Zenodo,Creative Commons Attribution 4.0 International,
 10.26302/sshade/experiment_zed_20230103_02,inist.sshade,Dataset,2024-04-10,SSHADE/DAYSY (OSUG Data Center),"Any use of downloaded SSHADE data in a scientific or technical paper or a presentation is free but you should cite both SSHADE and the used data in the text ( 'first author' et al., year) with its full reference (with its DOI) in the main reference section of the paper (or in a special 'data citation' section) and, when available, the original paper(s) presenting the data.",['9 spectra']
 10.26302/sshade/experiment_zed_20230103_01,inist.sshade,Dataset,2024-04-10,SSHADE/DAYSY (OSUG Data Center),"Any use of downloaded SSHADE data in a scientific or technical paper or a presentation is free but you should cite both SSHADE and the used data in the text ( 'first author' et al., year) with its full reference (with its DOI) in the main reference section of the paper (or in a special 'data citation' section) and, when available, the original paper(s) presenting the data.",['9 spectra']
+10.5281/zenodo.10949879,cern.zenodo,Software,2024-04-10,Inria,Apache License 2.0,
 10.5281/zenodo.10949807,cern.zenodo,Dataset,2024-04-09,Inria,Creative Commons Attribution 4.0 International,
 10.5281/zenodo.10912814,cern.zenodo,Dataset,2024-04-03,Zenodo,Creative Commons Attribution 4.0 International,
 10.57745/aqno8d,rdg.prod,Dataset,2024-04-03,Recherche Data Gouv,,
 10.5905/ethz-1007-760,ethz.da-rd,Software,2024-04-03,"ETH Zurich; GIPSA-lab, Univ. Grenoble Alpes, CNRS, Grenoble INP, LAAS-CNRS, Czech Technical University",,
+10.5281/zenodo.10906790,cern.zenodo,Dataset,2024-04-02,Zenodo,Creative Commons Attribution Share Alike 4.0 International,
 10.5281/zenodo.10896138,cern.zenodo,Dataset,2024-03-30,Zenodo,Creative Commons Attribution 4.0 International,
 10.5281/zenodo.10896121,cern.zenodo,ComputationalNotebook,2024-03-30,Zenodo,Creative Commons Attribution 4.0 International,
 10.5281/zenodo.10895010,cern.zenodo,Dataset,2024-03-29,Zenodo,Creative Commons Attribution 4.0 International,
@@ -460,8 +476,8 @@ doi,client,resourceTypeGeneral,created,publisher,rights,sizes
 10.60527/fpa9-1718,fmsh.prod,Other,2024-03-06,"Univ. Grenoble Alpes, GRESEC",,
 10.60527/zxn9-6b90,fmsh.prod,Audiovisual,2024-03-06,"Univ. Grenoble Alpes, GRESEC",Droit commun de la propriété intellectuelle,
 10.5281/zenodo.10788911,cern.zenodo,Dataset,2024-03-06,Zenodo,Creative Commons Attribution 4.0 International,
-10.6084/m9.figshare.25341247,figshare.ars,Dataset,2024-03-05,figshare,Creative Commons Attribution 4.0 International,['29389796 Bytes']
 10.6084/m9.figshare.c.7105606,figshare.ars,Collection,2024-03-05,figshare,Creative Commons Attribution 4.0 International,
+10.6084/m9.figshare.25341247,figshare.ars,Dataset,2024-03-05,figshare,Creative Commons Attribution 4.0 International,['29389796 Bytes']
 10.6084/m9.figshare.25329673,figshare.ars,Text,2024-03-02,figshare,Creative Commons Attribution 4.0 International,['15066 Bytes']
 10.6084/m9.figshare.c.7097182,figshare.ars,Collection,2024-02-29,figshare,Creative Commons Attribution 4.0 International,
 10.6084/m9.figshare.25309966,figshare.ars,Text,2024-02-29,figshare,Creative Commons Attribution 4.0 International,['584702 Bytes']
@@ -483,19 +499,3 @@ doi,client,resourceTypeGeneral,created,publisher,rights,sizes
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-10.57745/tzdeih,rdg.prod,Dataset,2024-02-16,Recherche Data Gouv,,
-10.5061/dryad.xpnvx0knw,dryad.dryad,Dataset,2024-02-15,Dryad,Creative Commons Zero v1.0 Universal,['212839 bytes']
-10.5281/zenodo.4292167,cern.zenodo,Dataset,2024-02-15,Zenodo,Creative Commons Attribution 4.0 International,
-10.5281/zenodo.10654575,cern.zenodo,InteractiveResource,2024-02-13,Zenodo,Creative Commons Attribution 4.0 International,
-10.5281/zenodo.10265625,cern.zenodo,Dataset,2024-02-13,Zenodo,Creative Commons Attribution 4.0 International,
-10.5281/zenodo.10652455,cern.zenodo,Software,2024-02-13,Zenodo,MIT License,
-10.5281/zenodo.10650736,cern.zenodo,Dataset,2024-02-12,Zenodo,Creative Commons Attribution No Derivatives 4.0 International,
-10.5281/zenodo.10634156,cern.zenodo,Dataset,2024-02-12,Zenodo,Creative Commons Attribution 4.0 International,
-10.6084/m9.figshare.c.7068560,figshare.ars,Collection,2024-02-10,figshare,Creative Commons Attribution 4.0 International,
-10.6084/m9.figshare.25200581,figshare.ars,Text,2024-02-10,figshare,Creative Commons Attribution 4.0 International,['1025399 Bytes']
-10.18709/perscido.2024.02.ds406,inist.persyval,Dataset,2024-02-09,PerSCiDO,,['100 Mo']
-10.5281/zenodo.10640565,cern.zenodo,Dataset,2024-02-09,Zenodo,Creative Commons Attribution 4.0 International,
-10.5281/zenodo.10423906,cern.zenodo,Dataset,2024-02-09,Zenodo,Creative Commons Attribution Non Commercial 4.0 International,
-10.5281/zenodo.10635624,cern.zenodo,Text,2024-02-09,Unite! Alliance Publications,Creative Commons Attribution 4.0 International,
-10.5061/dryad.b2rbnzsp7,dryad.dryad,Dataset,2024-02-07,Dryad,Creative Commons Zero v1.0 Universal,['1103297 bytes']
-10.5281/zenodo.10619441,cern.zenodo,Software,2024-02-05,Zenodo,Creative Commons Attribution 4.0 International,

dois-uga.csv

@@ -12055,3 +12055,55 @@ The complete output files for the AlphaFold2 multimer prediciotn of the pairwise
 10.57745/4vsxwh,Replication data for : Pointillism Wall Painting Drone Using Bouncing Frequency Control,Recherche Data Gouv,2024,,Dataset,,"This study presents an new robotic airborne solution for autonomous wall painting using a pointillism technique. The proposed dot-painting drone is a quadcopter equipped with an additional forward propulsion unit and a spring-mounted painting pad. It is designed to bounce on a vertical wall in order to print dots at a controlled frequency along a predefined trajectory. A dynamic model of the system is derived and used to control accurately the bouncing frequency as well as the position of the robot. The performance of the system is validated experimentally, demonstrating successful indoor painting capability of pointillism drawing on vertical walls. This work represents a first step toward fully autonomous, large-scale mural reproduction using aerial robotics.",mds,True,findable,10,1,0,0,0,2024-10-09T09:05:07.000Z,2024-12-02T09:05:19.000Z,rdg.prod,rdg,,,,,,,"['HasPart', 'HasPart', 'HasPart', 'HasPart', 'HasPart', 'HasPart', 'HasPart', 'HasPart', 'HasPart', 'HasPart']",
 10.6084/m9.figshare.c.7569397,The impact of a dedicated checklist on the quality of onsite management of critically buried avalanche victims in cardiac arrest in a Swiss helicopter emergency medical service,figshare,2024,,Collection,Creative Commons Attribution 4.0 International,"Abstract Background The management of avalanche victims in cardiac arrest (CA) is a challenging situation for rescuers. Despite existing specific management algorithms, previous studies have reported poor compliance with international guidelines and incomplete documentation and transmission of the information required for patient management. The Avalanche Victim Resuscitation Checklist (AVRC) was developed in 2014 in response by the International Commission for Mountain Emergency Medicine. Our aim was to assess the impact of the AVRC on the quality of onsite management of critically buried avalanche victims in CA, i.e. the compliance of management with international guidelines and the completeness of documentation of avalanche specific information. Methods We assessed compliance and documentation in a Swiss helicopter emergency medical service (HEMS) between January 2010 and April 2020. Victims buried for more than 24 h were excluded. Results In the 10-year study period, 87 critically buried avalanche victims in CA were treated by the HEMS, 44 of them after the introduction of the AVRC. Enough information was available to assess management compliance in over 90% of cases (n = 79). Inadequate management (n = 25, 32%) and incomplete documentation occurred more often in patients with a long burial duration. After the introduction of the AVRC, the compliance of patient management with the guidelines increased by 36% (from 59 to 95%, p < 0.05) and led to complete documentation of the required information for patient management. Conclusions The use of the AVRC improves the quality of management of critically buried avalanche victims in CA and ensures complete documentation of avalanche specific information. Quality improvement efforts should focus on the management of avalanche victims with a long burial duration. The use of the AVRC enables identification and appropriate treatment of patients with hypothermic cardiac arrest.",mds,True,findable,0,0,0,0,0,2024-12-04T04:38:09.000Z,2024-12-04T04:38:10.000Z,figshare.ars,otjm,"Medicine,Cell Biology,Biotechnology,Environmental Sciences not elsewhere classified,Biological Sciences not elsewhere classified,Cancer,Science Policy","[{'subject': 'Medicine'}, {'subject': 'Cell Biology'}, {'subject': 'Biotechnology'}, {'subject': 'Environmental Sciences not elsewhere classified'}, {'subject': 'Biological Sciences not elsewhere classified'}, {'subject': 'Cancer'}, {'subject': 'Science Policy'}]",,,,,['IsIdenticalTo'],"[['IsIdenticalTo', '10.6084/m9.figshare.c.7569397']]"
 10.57745/jjwoys,Explore2 dataset : A large transient multi-scenario multi-model ensemble of future streamflows and groundwater projections in France,Recherche Data Gouv,2024,,Dataset,,"A large transient multi-scenario and multi-model ensemble of future streamflows and groundwater projections in France developed in a national project named Explore2 was recently published. The main objective of Explore2 is to provide rich and spatially consistent information for the future evolution of hydrological (surface and groundwater) resources and extremes in France to support adaptation strategies. The Explore2 dataset was obtained using a nested multi-scenario multi-model approach to estimate future uncertainty and to access local climate and catchment scales: 3 greenhouse gases (GHG) emission scenarios, with a set of 17 combinations of Global Climate Models and Regional Climate Models (GCM-RCM) and 2 bias correction methods provide the meteorological forcings for 9 surface hydrology models and 4 groundwater hydrology models (1 to simulate groundwater recharge and 3 to simulate groundwater level). The associated datapaper, present the methodology underlying the dataset, the assessment of the hydrological models we applied against daily observations of discharge and groundwater level, the data availability and the ways of accessing the data and understanding the results (mainly through visualisation tools).",mds,True,findable,11,1,0,0,0,2024-11-06T16:57:58.000Z,2024-12-03T12:27:07.000Z,rdg.prod,rdg,,,,,,,"['HasPart', 'HasPart', 'HasPart', 'HasPart', 'HasPart']",
+10.1594/pangaea.971988,Elemental geochemistry of sediment core MD03-2679,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,"All elemental data were obtained with a X-Ray Fluorescence (XRF) core-scanner Avaatech 4th generation at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE), and calibrated using the Weltje et al., (2015) Multivariate Log-ratio Calibration (MLC).",mds,True,findable,0,0,2,0,0,2024-12-11T01:12:24.000Z,2024-12-11T01:12:25.000Z,pangaea.repository,pangaea,"Deep current intensity,North Atlantic circulation,XRF,Event label,DEPTH, sediment/rock,Depth, corrected,AGE,Iron,Titanium,ln-Titanium/Potassium ratio,ln-Zirconium/Rubidium ratio,ln-Calcium/Titanium ratio,ln-Calcium/Iron ratio,Calypso Corer,X-ray fluorescence core scanner (XRF), Avaatech,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'North Atlantic circulation'}, {'subject': 'XRF'}, {'subject': 'Event label', 'subjectScheme': 'Parameter'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'Depth, corrected', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Iron', 'subjectScheme': 'Parameter'}, {'subject': 'Titanium', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Titanium/Potassium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Zirconium/Rubidium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Calcium/Titanium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Calcium/Iron ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'X-ray fluorescence core scanner (XRF), Avaatech', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['27433 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References', 'References']",
+10.24350/cirm.v.20036503,Contact flows and Birkhoff sections - Part 1,CIRM,2023,ENG,Audiovisual,Creative Commons Attribution Non Commercial No Derivatives 4.0 International,"This course is devoted to the interplay of several topological and dynamical notions, namely contact forms and their Reeb flows, open book decompositions, and Anosov flows. We will spend some time explaining the basic definitions and several important examples. The rough plan is (1) Contact forms, Reeb flows, and open book decomposition (2) Birkhoff sections, Anosov flows, and Reeb-Anosov flows.",mds,True,findable,0,0,0,0,0,2023-05-02T09:52:31.000Z,2023-05-02T09:52:31.000Z,inist.cirm,jbru,"37C10,53D10,57R65,Dynamical Systems & ODE,Topology","[{'subject': '37C10', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '53D10', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '57R65', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': 'Dynamical Systems & ODE', 'subjectScheme': 'Area(s)'}, {'subject': 'Topology', 'subjectScheme': 'Area(s)'}]",,['MP4'],,,"['IsSupplementTo', 'IsPartOf']",
+10.1594/pangaea.971918,Tie-points used to construct the chronology of sediment core MD03-2685,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,Method Numberklf 1RPI 2ln(Ca/Fe) 3Laschamp excursion 4,mds,True,findable,0,0,4,0,0,2024-12-11T01:12:21.000Z,2024-12-11T01:12:21.000Z,pangaea.repository,pangaea,"Deep current intensity,magnetism,North Atlantic circulation,XRF,DEPTH, sediment/rock,AGE,Method comment,Reference/source,Calypso Corer,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'magnetism'}, {'subject': 'North Atlantic circulation'}, {'subject': 'XRF'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Method comment', 'subjectScheme': 'Parameter'}, {'subject': 'Reference/source', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['210 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References', 'References', 'References', 'References']",
+10.1594/pangaea.971920,Elemental geochemistry of sediment core MD03-2673,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,"All elemental data were obtained with a X-Ray Fluorescence (XRF) core-scanner Avaatech 4th generation at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE), and calibrated using the Weltje et al., (2015) Multivariate Log-ratio Calibration (MLC).",mds,True,findable,0,0,2,0,0,2024-12-11T01:12:23.000Z,2024-12-11T01:12:24.000Z,pangaea.repository,pangaea,"Deep current intensity,North Atlantic circulation,XRF,Event label,DEPTH, sediment/rock,AGE,Iron,Titanium,ln-Titanium/Potassium ratio,ln-Zirconium/Rubidium ratio,ln-Calcium/Titanium ratio,ln-Calcium/Iron ratio,Calypso Corer,X-ray fluorescence core scanner (XRF), Avaatech,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'North Atlantic circulation'}, {'subject': 'XRF'}, {'subject': 'Event label', 'subjectScheme': 'Parameter'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Iron', 'subjectScheme': 'Parameter'}, {'subject': 'Titanium', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Titanium/Potassium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Zirconium/Rubidium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Calcium/Titanium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Calcium/Iron ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'X-ray fluorescence core scanner (XRF), Avaatech', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['26808 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References', 'References']",
+10.5281/zenodo.14167823,Rapport d'activité 2023 des BU de l'Université Grenoble Alpes,Zenodo,2024,,Other,Creative Commons Attribution 4.0 International,"Rapport d’activité de la DGD Bibliothèques et Appui à la Science Ouverte pour l’année 2023.
+
+Une année de travail, de projets, de réalisations, pour l’ensemble de l’équipe de la DGD BAPSO, regroupant l’ensembledes bibliothèques universitaires de l’UGA.",api,True,findable,0,0,0,0,0,2024-12-13T10:42:40.000Z,2024-12-13T10:42:40.000Z,cern.zenodo,cern,,,,,,,['HasVersion'],"[['IsVersionOf', '10.5281/zenodo.14167823']]"
+10.1594/pangaea.971990,Magnetic data of sediment core MD03-2673,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,"The low-field magnetic susceptibility was measured on u-channels using a 45 mm inner diameter Bartington coil.NRM, IRM and ARM were measured on u-channels using 755R DC-SQUIDS cryogenic magnetometers from 2G Enterprise and demagnetized with 12 steps.",mds,True,findable,0,0,1,0,0,2024-12-11T01:12:27.000Z,2024-12-11T01:12:27.000Z,pangaea.repository,pangaea,"Deep current intensity,magnetism,North Atlantic circulation,Event label,DEPTH, sediment/rock,AGE,Magnetic susceptibility, low-field,Anhysteretic remanent magnetization,Anhysteretic remanent magnetization/isothermal remanent magnetization ratio,Remanent magnetization, normalized/magnetic susceptibility, low-field, ratio,Remanent magnetization, normalized/anhysteretic remanent magnetization ratio,Remanent magnetization, normalized/isothermal remanent magnetization ratio,Principal component analysis inclination,Mean angular deviation,Geocentric axial dipole field inclination,Calypso Corer,Bartington MS2 magnetic susceptibility meter,Magnetometer [U-channel], 2G Enterprises, Model 755R,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'magnetism'}, {'subject': 'North Atlantic circulation'}, {'subject': 'Event label', 'subjectScheme': 'Parameter'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Magnetic susceptibility, low-field', 'subjectScheme': 'Parameter'}, {'subject': 'Anhysteretic remanent magnetization', 'subjectScheme': 'Parameter'}, {'subject': 'Anhysteretic remanent magnetization/isothermal remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/magnetic susceptibility, low-field, ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/anhysteretic remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/isothermal remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Principal component analysis inclination', 'subjectScheme': 'Parameter'}, {'subject': 'Mean angular deviation', 'subjectScheme': 'Parameter'}, {'subject': 'Geocentric axial dipole field inclination', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'Bartington MS2 magnetic susceptibility meter', 'subjectScheme': 'Method'}, {'subject': 'Magnetometer [U-channel], 2G Enterprises, Model 755R', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['14951 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References']",
+10.5281/zenodo.14339958,Supplementary material of ALMA-IMF XVI (Motte et al. 2025),Zenodo,2024,en,Image,Creative Commons Attribution 4.0 International,"Figure entitled ""ALMA-IMF-XVI_FigureD3.png"" displays the distribution of the mass-averaged dust temperature of prestellar cores located within luminosity peaks (orange histogram) and far away from them (green histogram), as indicated by their correspondence in Figs. 1 and D.1 of Motte et al. (2025). The prestellar cores in the immediate vicinity of luminous protostellar cores have higher dust temperatures.  It is a supplementary plot that complements the Astronomy & Astrophysics article Motte et al. (2025).",api,True,findable,0,0,0,0,1,2024-12-09T19:35:55.000Z,2024-12-09T19:35:55.000Z,cern.zenodo,cern,,,,,,,"['IsPartOf', 'HasVersion', 'IsPartOf']",
+10.1594/pangaea.971916,Tie-points used to construct the chronology of sediment core MD03-2673,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,Method Numberklf 1RPI 2ln(Ca/Fe) 3Laschamp excursion 4AMS radiocarbon 5,mds,True,findable,0,0,4,0,0,2024-12-11T01:12:19.000Z,2024-12-11T01:12:20.000Z,pangaea.repository,pangaea,"Deep current intensity,magnetism,North Atlantic circulation,XRF,DEPTH, sediment/rock,AGE,Method comment,Reference/source,Calypso Corer,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'magnetism'}, {'subject': 'North Atlantic circulation'}, {'subject': 'XRF'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Method comment', 'subjectScheme': 'Parameter'}, {'subject': 'Reference/source', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['188 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References', 'References', 'References', 'References']",
+10.5281/zenodo.10949879,"On the Moreau–Jean scheme with the Frémond impact law: energy conservation and dissipation properties for elastodynamics with contact, impact and friction — codes",Inria,2024,en,Software,Apache License 2.0,"This deposit contains the codes of the systems described in On the Moreau–Jean scheme with the Frémond impact law. Energy conservation and dissipation properties for elastodynamics with contact impact and friction. The data outputs that are generated by this code are available in another deposit archived on Zenodo, as well as in a GitHub repository archived on Software Heritage, which is the preferred method of obtaining the codes. One of the codes in this deposit (""block_mesh_plot.py"") requires two of the files in the data deposit (""deformed_sliding_block_mesh.png"" and ""sliding_block_mesh.png"") to run successfully, with the files assumed to be located in the folder specified in the data_folder variable of the file ""path_file.py"", but the deposits are otherwise independent.",api,True,findable,0,0,0,1,0,2024-04-10T11:19:40.000Z,2024-04-10T11:19:40.000Z,cern.zenodo,cern,Solid mechanics,"[{'subject': 'Solid mechanics', 'subjectScheme': 'EuroSciVoc'}]",,,,,"['IsDescribedBy', 'IsReferencedBy', 'HasVersion', 'HasVersion']","[['IsVersionOf', '10.5281/zenodo.10949879']]"
+10.1594/pangaea.971989,Elemental geochemistry of sediment core MD03-2685,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,"All elemental data were obtained with a X-Ray Fluorescence (XRF) core-scanner Avaatech 4th generation at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE), and calibrated using the Weltje et al., (2015) Multivariate Log-ratio Calibration (MLC).",mds,True,findable,0,0,2,0,0,2024-12-11T01:12:26.000Z,2024-12-11T01:12:26.000Z,pangaea.repository,pangaea,"Deep current intensity,North Atlantic circulation,XRF,Event label,DEPTH, sediment/rock,AGE,Iron,Titanium,ln-Titanium/Potassium ratio,ln-Zirconium/Rubidium ratio,ln-Calcium/Titanium ratio,ln-Calcium/Iron ratio,Calypso Corer,X-ray fluorescence core scanner (XRF), Avaatech,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'North Atlantic circulation'}, {'subject': 'XRF'}, {'subject': 'Event label', 'subjectScheme': 'Parameter'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Iron', 'subjectScheme': 'Parameter'}, {'subject': 'Titanium', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Titanium/Potassium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Zirconium/Rubidium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Calcium/Titanium ratio', 'subjectScheme': 'Parameter'}, {'subject': 'ln-Calcium/Iron ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'X-ray fluorescence core scanner (XRF), Avaatech', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['30792 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References', 'References']",
+10.5281/zenodo.14410833,"Datasets and analysis for ""Gatemon qubit on a germanium quantum-well heterostructure""",Zenodo,2024,,Dataset,Creative Commons Attribution 4.0 International,Inside is all the analysis and scripts used to create the figures of the paper. Please see readme.txt file for an overview of what is inside.,api,True,findable,0,0,0,0,0,2024-12-12T09:30:21.000Z,2024-12-12T09:30:21.000Z,cern.zenodo,cern,,,,,,,['HasVersion'],"[['IsVersionOf', '10.5281/zenodo.14410833']]"
+10.24350/cirm.v.20036003,Contact flows and Birkhoff sections - Part 2,CIRM,2023,ENG,Audiovisual,Creative Commons Attribution Non Commercial No Derivatives 4.0 International,"This course is devoted to the interplay of several topological and dynamical notions, namely contact forms and their Reeb flows, open book decompositions, and Anosov flows. We will spend some time explaining the basic definitions and several important examples. The rough plan is (1) Contact forms, Reeb flows, and open book decomposition (2) Birkhoff sections, Anosov flows, and Reeb-Anosov flows.",mds,True,findable,0,0,0,0,0,2023-05-02T09:48:33.000Z,2023-05-02T09:48:34.000Z,inist.cirm,jbru,"37C10,53D10,57R65,Dynamical Systems & ODE,Topology","[{'subject': '37C10', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '53D10', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '57R65', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': 'Dynamical Systems & ODE', 'subjectScheme': 'Area(s)'}, {'subject': 'Topology', 'subjectScheme': 'Area(s)'}]",,['MP4'],,,"['IsSupplementTo', 'IsPartOf']",
+10.5281/zenodo.10906790,Spatiotemporally distinct responses to mechanical forces shape the developing seed of Arabidopsis,Zenodo,2024,,Dataset,Creative Commons Attribution Share Alike 4.0 International,"Source Data File related to the manuscript:
+
+ 
+
+Spatiotemporally distinct responses to mechanical forces
+
+shape the developing seed of Arabidopsis
+
+ 
+
+See Description Dataset file for full description
+
+ ",api,True,findable,0,0,0,0,0,2024-04-02T08:00:22.000Z,2024-04-02T08:00:22.000Z,cern.zenodo,cern,,,,,,,['HasVersion'],"[['IsVersionOf', '10.5281/zenodo.10906790']]"
+10.24350/cirm.v.18479303,Which geodesic flows are left-handed?,CIRM,2013,Eng,Audiovisual,Creative Commons Attribution Non Commercial No Derivatives 4.0 International,"Left-handed flows are 3-dimensional flows which have a particular topological property, namely that every pair of periodic orbits is negatively linked. This property (introduced by Ghys in 2007) implies the existence of as many Bikrhoff sections as possible, and therefore allows to reduce the flow to a suspension in many different ways. It then becomes natural to look for examples. A construction of Birkhoff (1917) suggests that geodesic flows are good candidates. In this conference we determine on which hyperbolic orbifolds is the geodesic flow left-handed: the answer is that yes if the surface is a sphere with three cone points, and no otherwise.
+
+dynamical system - geodesic flow - knot - periodic orbit - global section - linking number - fibered knot",mds,True,findable,0,0,0,0,0,2017-04-28T15:19:05.000Z,2017-04-28T15:19:06.000Z,inist.cirm,jbru,"37C10,37C15,37C27,57M25,Topology,Dynamical Systems & ODE","[{'subject': '37C10', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '37C15', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '37C27', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '57M25', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': 'Topology', 'subjectScheme': 'Area(s)'}, {'subject': 'Dynamical Systems & ODE', 'subjectScheme': 'Area(s)'}]",,['quicktime;audio/x-aac'],,,"['IsSupplementTo', 'IsPartOf']",
+10.24350/cirm.v.20153203,Complex analysis in Lean,CIRM,2024,ENG,Audiovisual,Creative Commons Attribution Non Commercial No Derivatives 4.0 International,"I present a formalization of the Riemann Mapping Theorem in the Lean 4 proof assistant, and a few related topics.",mds,True,findable,0,0,0,0,0,2024-04-22T11:49:33.000Z,2024-04-22T11:49:34.000Z,inist.cirm,jbru,"30-04,30C35,30H05,Analysis and its Applications,Logic and Foundations","[{'subject': '30-04', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '30C35', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '30H05', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': 'Analysis and its Applications', 'subjectScheme': 'Area(s)'}, {'subject': 'Logic and Foundations', 'subjectScheme': 'Area(s)'}]",,['MP4'],,,"['IsSupplementTo', 'IsPartOf']",
+10.1594/pangaea.971993,Magnetic data of sediment core MD03-2679,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,"The low-field magnetic susceptibility was measured on u-channels using a 45 mm inner diameter Bartington coil.NRM, IRM and ARM were measured on u-channels using 755R DC-SQUIDS cryogenic magnetometers from 2G Enterprise and demagnetized with 12 steps.",mds,True,findable,0,0,1,0,0,2024-12-11T01:12:28.000Z,2024-12-11T01:12:29.000Z,pangaea.repository,pangaea,"Deep current intensity,magnetism,North Atlantic circulation,Event label,DEPTH, sediment/rock,Depth, corrected,AGE,Magnetic susceptibility, low-field,Anhysteretic remanent magnetization,Anhysteretic remanent magnetization/isothermal remanent magnetization ratio,Remanent magnetization, normalized/magnetic susceptibility, low-field, ratio,Remanent magnetization, normalized/anhysteretic remanent magnetization ratio,Remanent magnetization, normalized/isothermal remanent magnetization ratio,Principal component analysis inclination,Mean angular deviation,Geocentric axial dipole field inclination,Calypso Corer,Bartington MS2 magnetic susceptibility meter,Magnetometer [U-channel], 2G Enterprises, Model 755R,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'magnetism'}, {'subject': 'North Atlantic circulation'}, {'subject': 'Event label', 'subjectScheme': 'Parameter'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'Depth, corrected', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Magnetic susceptibility, low-field', 'subjectScheme': 'Parameter'}, {'subject': 'Anhysteretic remanent magnetization', 'subjectScheme': 'Parameter'}, {'subject': 'Anhysteretic remanent magnetization/isothermal remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/magnetic susceptibility, low-field, ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/anhysteretic remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/isothermal remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Principal component analysis inclination', 'subjectScheme': 'Parameter'}, {'subject': 'Mean angular deviation', 'subjectScheme': 'Parameter'}, {'subject': 'Geocentric axial dipole field inclination', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'Bartington MS2 magnetic susceptibility meter', 'subjectScheme': 'Method'}, {'subject': 'Magnetometer [U-channel], 2G Enterprises, Model 755R', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['16415 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References']",
+10.24350/cirm.v.19983203,Asymptotic behaviour of rational curves,CIRM,2022,ENG,Audiovisual,Creative Commons Attribution Non Commercial No Derivatives 4.0 International,"In diophantine geometry, the Batyrev-Manin-Peyre conjecture originally concerns rational points on Fano varieties. It describes the asymptotic behaviour of the number of rational points of bounded height, when the bound becomes arbitrary large.
+
+A geometric analogue of this conjecture deals with the asymptotic behaviour of the moduli space of rational curves on a complex Fano variety, when the 'degree' of the curves 'goes to infinity'. Various examples support the claim that, after renormalisation in a relevant ring of motivic integration, the class of this moduli space may converge to a constant which has an interpretation as a motivic Euler product.
+
+In this talk, we will state this motivic version of the Batyrev-Manin-Peyre conjecture and give some examples for which it is known to hold : projective space, more generally toric varieties, and equivariant compactifications of vector spaces. In a second part we will introduce the notion of equidistribution of curves and show that it opens a path to new types of results.",mds,True,findable,0,0,0,0,0,2022-12-16T11:30:52.000Z,2022-12-16T11:30:53.000Z,inist.cirm,jbru,"14H50,14J45,Algebraic & Complex Geometry","[{'subject': '14H50', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '14J45', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': 'Algebraic & Complex Geometry', 'subjectScheme': 'Area(s)'}]",,['MP4'],,,"['IsSupplementTo', 'IsPartOf']",
+10.1594/pangaea.971919,Tie-points used to construct the chronology of sediment core MD03-2679,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,Method Numberklf 1RPI 2ln(Ca/Fe) 3Laschamp excursion 4AMS radiocarbon 5,mds,True,findable,0,0,4,0,0,2024-12-11T01:12:22.000Z,2024-12-11T01:12:22.000Z,pangaea.repository,pangaea,"Deep current intensity,magnetism,North Atlantic circulation,XRF,DEPTH, sediment/rock,AGE,Method comment,Reference/source,Calypso Corer,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'magnetism'}, {'subject': 'North Atlantic circulation'}, {'subject': 'XRF'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Method comment', 'subjectScheme': 'Parameter'}, {'subject': 'Reference/source', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['176 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References', 'References', 'References', 'References']",
+10.24350/cirm.v.20036903,Contact flows and Birkhoff sections - Part 3,CIRM,2023,ENG,Audiovisual,Creative Commons Attribution Non Commercial No Derivatives 4.0 International,"This course is devoted to the interplay of several topological and dynamical notions, namely contact forms and their Reeb flows, open book decompositions, and Anosov flows. We will spend some time explaining the basic definitions and several important examples. The rough plan is (1) Contact forms, Reeb flows, and open book decomposition (2) Birkhoff sections, Anosov flows, and Reeb-Anosov flows.",mds,True,findable,0,0,0,0,0,2023-05-02T09:52:35.000Z,2023-05-02T09:52:35.000Z,inist.cirm,jbru,"37C10,53D10,57R65,Dynamical Systems & ODE,Topology","[{'subject': '37C10', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '53D10', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': '57R65', 'schemeUri': 'https://mathscinet.ams.org/msc/msc2020.html', 'subjectScheme': 'MSC2020'}, {'subject': 'Dynamical Systems & ODE', 'subjectScheme': 'Area(s)'}, {'subject': 'Topology', 'subjectScheme': 'Area(s)'}]",,['MP4'],,,"['IsSupplementTo', 'IsPartOf']",
+10.5061/dryad.280gb5mvx,Local incomplete combustion emissions define the PM2.5 oxidative potential in Northern India,Dryad,2023,en,Dataset,Creative Commons Zero v1.0 Universal,"The oxidative potential (OP) of particulate matter (PM) is a major driver
+ of PM-associated health effects. In India, the emission sources defining
+ PM-OP, and their local/regional nature, have yet to be established. To
+ address this gap, we determined the geographical origin, sources of PM,
+ and its OP at five Indo-Gangetic Plain (IGP) sites inside and outside
+ Delhi. Our findings reveal that although uniformly high PM concentrations
+ were recorded across the entire region, local emission sources and
+ formation processes dominate PM pollution. PM-OP is overwhelmingly driven
+ by OA from incomplete combustion of biomass and fossil fuels, including
+ traffic. These findings suggest that addressing local inefficient
+ combustion processes can effectively mitigate PM health exposure in
+ Northern India.",mds,True,findable,0,1,0,1,0,2024-12-09T08:25:45.000Z,2024-12-09T08:25:46.000Z,dryad.dryad,dryad,"Oxidative Potential,Positive Matrix Factorization,Mass spectrometry,FOS: Earth and related environmental sciences,FOS: Earth and related environmental sciences","[{'subject': 'Oxidative Potential'}, {'subject': 'Positive Matrix Factorization'}, {'subject': 'Mass spectrometry', 'schemeUri': 'https://github.com/PLOS/plos-thesaurus', 'subjectScheme': 'PLOS Subject Area Thesaurus'}, {'subject': 'FOS: Earth and related environmental sciences', 'subjectScheme': 'fos'}, {'subject': 'FOS: Earth and related environmental sciences', 'schemeUri': 'http://www.oecd.org/science/inno/38235147.pdf', 'subjectScheme': 'Fields of Science and Technology (FOS)'}]",['12624044 bytes'],,,,['IsCitedBy'],
+10.1594/pangaea.971995,Magnetic data of sediment core MD03-2685,PANGAEA,2024,,Dataset,Creative Commons Attribution 4.0 International,"The low-field magnetic susceptibility was measured on u-channels using a 45 mm inner diameter Bartington coil.NRM, IRM and ARM were measured on u-channels using 755R DC-SQUIDS cryogenic magnetometers from 2G Enterprise and demagnetized with 12 steps.",mds,True,findable,0,0,1,0,0,2024-12-11T01:12:30.000Z,2024-12-11T01:12:30.000Z,pangaea.repository,pangaea,"Deep current intensity,magnetism,North Atlantic circulation,Event label,DEPTH, sediment/rock,AGE,Magnetic susceptibility, low-field,Anhysteretic remanent magnetization,Anhysteretic remanent magnetization/isothermal remanent magnetization ratio,Remanent magnetization, normalized/magnetic susceptibility, low-field, ratio,Remanent magnetization, normalized/anhysteretic remanent magnetization ratio,Remanent magnetization, normalized/isothermal remanent magnetization ratio,Principal component analysis inclination,Mean angular deviation,Geocentric axial dipole field inclination,Calypso Corer,Bartington MS2 magnetic susceptibility meter,Magnetometer [U-channel], 2G Enterprises, Model 755R,MD132,Marion Dufresne (1995)","[{'subject': 'Deep current intensity'}, {'subject': 'magnetism'}, {'subject': 'North Atlantic circulation'}, {'subject': 'Event label', 'subjectScheme': 'Parameter'}, {'subject': 'DEPTH, sediment/rock', 'subjectScheme': 'Parameter'}, {'subject': 'AGE', 'subjectScheme': 'Parameter'}, {'subject': 'Magnetic susceptibility, low-field', 'subjectScheme': 'Parameter'}, {'subject': 'Anhysteretic remanent magnetization', 'subjectScheme': 'Parameter'}, {'subject': 'Anhysteretic remanent magnetization/isothermal remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/magnetic susceptibility, low-field, ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/anhysteretic remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Remanent magnetization, normalized/isothermal remanent magnetization ratio', 'subjectScheme': 'Parameter'}, {'subject': 'Principal component analysis inclination', 'subjectScheme': 'Parameter'}, {'subject': 'Mean angular deviation', 'subjectScheme': 'Parameter'}, {'subject': 'Geocentric axial dipole field inclination', 'subjectScheme': 'Parameter'}, {'subject': 'Calypso Corer', 'subjectScheme': 'Method'}, {'subject': 'Bartington MS2 magnetic susceptibility meter', 'subjectScheme': 'Method'}, {'subject': 'Magnetometer [U-channel], 2G Enterprises, Model 755R', 'subjectScheme': 'Method'}, {'subject': 'MD132', 'subjectScheme': 'Campaign'}, {'subject': 'Marion Dufresne (1995)', 'subjectScheme': 'Basis'}]",['19211 data points'],['text/tab-separated-values'],,,"['IsPartOf', 'References']",