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description Publicationkeyboard_double_arrow_right Article 2024 ItalyPublisher:Elsevier BV Arienti, G; Bistacchi, A; Caumon, G; Dal Piaz, G; Monopoli, B; Bertolo, D;International audience; Leveraging a high resolution geological and structural dataset acquired over decades of fieldwork, we build the 3D structural model of a portion of the highly deformed core of the Alpine orogen, in the Northern Aosta Valley. The model represents tectonic contacts separating the tectono-metamorphic units outcropping along the section between Mont Blanc and Monte Rosa, and it covers an area of ca. 1500 km2. The input source data include original 1:10,000 geological surveys synthetised in a 1:75,000 tectonic map, and a dense database of structural stations. After a first orientation statistics study of the structural field database, our workflow develops through structural interpretation in vertical cross-sections that allow including in the modelling process structural drivers such as crosscutting relationships, interference patterns, kinematic constraints and fold morphology from detailed field studies. Three-dimensional interpolation on a tetrahedral mesh using the implicit Discrete Smooth Interpolator method follows, using also foliation and fold axes data as interpolation constraints. After describing the workflow and the model, we discuss the difficulties of modelling in polydeformed metamorphic complexes. In particular, we address the issue of modelling shear zones, refolded, isoclinal and/or recumbent folds and dense networks of faults, that characterise the geology of the Northern Aosta Valley.
Journal of Structura... arrow_drop_down Journal of Structural Geology; BOA - Bicocca Open ArchiveArticle . 2024 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la CommunicationArticle . 2024Full-Text: https://hal.science/hal-04388453/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.jsg.2023.105045&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Journal of Structura... arrow_drop_down Journal of Structural Geology; BOA - Bicocca Open ArchiveArticle . 2024 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la CommunicationArticle . 2024Full-Text: https://hal.science/hal-04388453/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2024Publisher:Geological Society of London Dominique Cluzel; Alessandra Montanini; Arianna Secchiari; Elisa Ferrari; Matt Heizler; Fred Jourdan; Sebastien Meffre; Renjie Zhou; Christian Teyssier;The New Caledonia Ophiolite is cross-cut by coarse- to medium-grained pyroxenite and hornblende gabbro/diorite dykes intruded between 55.5 and 50 Ma (U–Pb zircon and 40 Ar/ 39 Ar hornblende), whereas the finer grained dolerites of tholeiitic affinity are younger (50–47 Ma). The production of hornblende gabbros/diorites was modelled by moderate degrees (20–40%) of partial melting of the high-temperature amphibolites of the metamorphic sole. The end-member compositions (hornblendites and anorthosites) resulted from solid-state phase segregation of crystal mushes within tectonically active magmatic conduits. Cascade reactions of the slab melts with mantle wedge peridotites successively formed clinoenstatite-bearing boninite magmas, which fed gabbronorite cumulate lenses at the mantle–crust transition; in turn, the clinoenstatite-bearing boninite melts reacted with peridotites to form websterites. The youngest magmas (of tholeiitic affinity) appeared c. 6 Myr after the inception of subduction when the cooler subducting slab plunged more steeply. Incipient slab retreat allowed corner flow, triggering low-pressure hydrous melting of the uplifted asthenosphere. The early stages of forearc magmatism were closely associated with transcurrent shear zones, which recorded oblique subduction inception. The early Eocene tectonic and magmatic features of the New Caledonia Ophiolite provide evidence for a north- or NE-dipping hot (forced) subduction zone in the SW Pacific, notably distinct from the slightly younger west-dipping Izu-Bonin–Marianna cold (spontaneous) subduction system. Supplementary material: Field pictures, additional diagrams, GPS location of dated samples, whole-rock geochemical and isotope data, Ar/Ar data, U–Pb zircon data, and distribution coefficients ( K d ) of trace elements used for modelling are available at https://doi.org/10.6084/m9.figshare.c.6949265 Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists
figshare arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2024add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1144/jgs2023-145&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert figshare arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2024add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Preprint , Other literature type 2023 FrancePublisher:American Physical Society (APS) Funded by:SNSF | Experimental Particle and..., ANR | SUNCORE, NSERC +6 projectsSNSF| Experimental Particle and Astroparticle Physics Beyond The Standard Model ,ANR| SUNCORE ,NSERC ,EC| INPhINIT ,EC| SK2HK ,SNSF| Towards neutrino CP violation: Strengthening the Japanese neutrino program T2K and Hyper-Kamiokande ,EC| JENNIFER2 ,EC| FELLINI ,SNSF| TOWARDS THE IMPROVEMENT OF NEUTRINO OSCILLATION MEASUREMENTS: T2K AND THE JAPANESE PROGRAMK. Abe; N. Akhlaq; R. Akutsu; H. Alarakia-Charles; A. Ali; Y. I. Alj Hakim; S. Alonso Monsalve; C. Alt; C. Andreopoulos; M. Antonova; S. Aoki; T. Arihara; Y. Asada; Y. Ashida; E. T. Atkin; M. Barbi; G. J. Barker; G. Barr; D. Barrow; M. Batkiewicz-Kwasniak; F. Bench; V. Berardi; L. Berns; S. Bhadra; A. Blanchet; A. Blondel; S. Bolognesi; T. Bonus; S. Bordoni; S. B. Boyd; A. Bravar; C. Bronner; S. Bron; A. Bubak; M. Buizza Avanzini; J. A. Caballero; N. F. Calabria; S. Cao; D. Carabadjac; A. J. Carter; S. L. Cartwright; M. P. Casado; M. G. Catanesi; A. Cervera; J. Chakrani; D. Cherdack; P. S. Chong; G. Christodoulou; A. Chvirova; M. Cicerchia; J. Coleman; G. Collazuol; L. Cook; A. Cudd; C. Dalmazzone; T. Daret; P. Dasgupta; Yu. I. Davydov; A. De Roeck; G. De Rosa; T. Dealtry; C. C. Delogu; C. Densham; A. Dergacheva; F. Di Lodovico; S. Dolan; D. Douqa; T. A. Doyle; O. Drapier; J. Dumarchez; P. Dunne; K. Dygnarowicz; A. Eguchi; S. Emery-Schrenk; G. Erofeev; A. Ershova; G. Eurin; D. Fedorova; S. Fedotov; M. Feltre; A. J. Finch; G. A. Fiorentini Aguirre; G. Fiorillo; M. D. Fitton; J. M. Franco Patiño; M. Friend; Y. Fujii; Y. Fukuda; Y. Furui; K. Fusshoeller; L. Giannessi; C. Giganti; V. Glagolev; M. Gonin; J. González Rosa; E. A. G. Goodman; A. Gorin; M. Grassi; M. Guigue; D. R. Hadley; J. T. Haigh; P. Hamacher-Baumann; D. A. Harris; M. Hartz; T. Hasegawa; S. Hassani; N. C. Hastings; Y. Hayato; D. Henaff; A. Hiramoto; M. Hogan; J. Holeczek; A. Holin; T. Holvey; N. T. Hong Van; T. Honjo; F. Iacob; A. K. Ichikawa; M. Ikeda; T. Ishida; M. Ishitsuka; H. T. Israel; A. Izmaylov; N. Izumi; M. Jakkapu; B. Jamieson; S. J. Jenkins; C. Jesús-Valls; J. J. Jiang; J. Y. Ji; P. Jonsson; S. Joshi; C. K. Jung; P. B. Jurj; M. Kabirnezhad; A. C. Kaboth; T. Kajita; H. Kakuno; J. Kameda; S. P. Kasetti; Y. Kataoka; T. Katori; M. Kawaue; E. Kearns; M. Khabibullin; A. Khotjantsev; T. Kikawa; S. King; V. Kiseeva; J. Kisiel; T. Kobata; H. Kobayashi; T. Kobayashi; L. Koch; S. Kodama; A. Konaka; L. L. Kormos; Y. Koshio; A. Kostin; T. Koto; K. Kowalik; Y. Kudenko; Y. Kudo; S. Kuribayashi; R. Kurjata; T. Kutter; M. Kuze; M. La Commara; L. Labarga; K. Lachner; J. Lagoda; S. M. Lakshmi; M. Lamers James; M. Lamoureux; A. Langella; J.-F. Laporte; D. Last; N. Latham; M. Laveder; L. Lavitola; M. Lawe; Y. Lee; C. Lin; S.-K. Lin; R. P. Litchfield; S. L. Liu; W. Li; A. Longhin; K. R. Long; A. Lopez Moreno; L. Ludovici; X. Lu; T. Lux; L. N. Machado; L. Magaletti; K. Mahn; M. Malek; M. Mandal; S. Manly; A. D. Marino;This paper reports the first measurement of muon neutrino charged-current interactions without pions in the final state using multiple detectors with correlated energy spectra at T2K. The data was collected on hydrocarbon targets using the off-axis T2K near detector (ND280) and the on-axis T2K near detector (INGRID) with neutrino energy spectra peaked at 0.6 GeV and 1.1 GeV respectively. The correlated neutrino flux presents an opportunity to reduce the impact of the flux uncertainty and to study the energy dependence of neutrino interactions. The extracted double-differential cross sections are compared to several Monte Carlo neutrino-nucleus interaction event generators showing the agreement between both detectors individually and with the correlated result. Updated discussion in Sec. V-A; Updated author list
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1103/physre...Article . 2023 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . Preprint . 2023add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1103/physrevd.108.112009&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.euAccess RoutesGreen 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1103/physre...Article . 2023 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . Preprint . 2023add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1103/physrevd.108.112009&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 France, ItalyPublisher:Springer Science and Business Media LLC Mike Burton; Alessandro Aiuppa; Patrick Allard; María Asensio-Ramos; Ana Pardo Cofrades; Alessandro La Spina; Emma J. Nicholson; Vittorio Zanon; José Barrancos; Marcello Bitetto; Margaret Hartley; Jorge E. Romero; Emma Waters; Alex Stewart; Pedro A. Hernández; João Pedro Lages; Eleazar Padrón; Kieran Wood; Benjamin Esse; Catherine Hayer; Klaudia Cyrzan; Estelle F. Rose-Koga; Federica Schiavi; Luca D’Auria; Nemesio M. Pérez;handle: 10447/621695
AbstractAlkaline mafic magmas forming intra-plate oceanic islands are believed to be strongly enriched in CO2 due to low-degree partial melting of enriched mantle sources. However, until now, such CO2 enhancement has not been verified by measuring CO2 degassing during a subaerial eruption. Here, we provide evidence of highly CO2-rich gas emissions during the 86-day 2021 Tajogaite eruption of Cumbre Vieja volcano on La Palma Island, in the Canary archipelago. Our results reveal sustained high plume CO2/SO2 ratios, which, when combined with SO2 fluxes, melt inclusion volatile contents and magma production rates at explosive and effusive vents, imply a magmatic CO2 content of 4.5 ± 1.5 wt%. The amount of CO2 released during the 2021 eruptive activity was 28 ± 14 Mt CO2. Extrapolating to the volume of alkaline mafic magmas forming La Palma alone (estimated as 4000 km3 erupted over 11 Ma), we infer a maximum CO2 emission into the ocean and atmosphere of 1016 moles of CO2, equivalent to 20% of the eruptive CO2 emissions from a large igneous province eruption, suggesting that the formation of the Canary volcanic archipelago produced a CO2 emission of similar magnitude as a large igneous province.
Communications Earth... arrow_drop_down Communications Earth & Environment; Archivio istituzionale della ricerca - Università di PalermoArticle . 2023 . Peer-reviewedLicense: CC BYHAL Clermont Université; Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert Communications Earth... arrow_drop_down Communications Earth & Environment; Archivio istituzionale della ricerca - Università di PalermoArticle . 2023 . Peer-reviewedLicense: CC BYHAL Clermont Université; Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.All Research productsarrow_drop_down <script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://www.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/s43247-023-01103-x&type=result"></script>'); --> </script>
For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Spain, Italy, GermanyPublisher:American Meteorological Society Funded by:EC | A-LIFE, EC | EUNADICS-AV, EC | FRAGMENT +1 projectsEC| A-LIFE ,EC| EUNADICS-AV ,EC| FRAGMENT ,EC| ACTRIS IMPMona, Licia; Amiridis, Vassilis; Cuevas, Emilio; Gkikas, Antonis; Trippetta, Serena; Vandenbussche, Sophie; Benedetti, Angela; Dagsson-Waldhauserova, Pavla; Formenti, Paola; Haefele, Alexander; Kazadzis, Stelios; Knippertz, Peter; Laurent, Benoit; Madonna, Fabio; Nickovic, S.; Papagiannopoulos, Nikolaos; Pappalardo, Gelsomina; Perez Garcia-Pando, Carlos; Popp, Thomas; Rodriguez, Sergio; Sealy, Andrea; Sugimoto, Nobuo; Terradellas, Enric; Vukovic Vimic, Ana; Weinzierl, Bernadett; Basart, Sara;handle: 10261/339009 , 20.500.11765/15177 , 2117/393050
Authors acknowledge dr Sangboom Ryoo of Korean Meteorological Administration in Seoul for his help and support.The research leading to these results has received funding from the COST ActionCA16202, supported by COST Association (European Cooperation in Science and Technology), from DustClim Project as part of ERA4CS, an ERA-NET initiated by JPI Climate, and funded by FORMAS (SE), DLR (DE), BMWFW (AT), IFD (DK), MINECO (ES), ANR (FR) with co-funding by the European Union (Grant 690462) and by the European Union’s Horizon 2020 research program for societal challenges – smart, green and integrated transport under grant agreement no.723986 (project EUNADICS-AV – European Natural Disaster Coordination and Information System for Aviation). L. Mona acknowledges the ACTRIS-IMP (Implementation project), funded by the European Union’s Horizon 2020 research and innovation programme (Grant no 871115) and the contribution of the ACTRIS-ITALIA JRU (CNR prot. n. 0067310/2017). S. Basart acknowledges CAMS-84 and CAMS2-82 (part of the Copernicus Atmospheric Monitoring Services, CAMS) and the Spanish Jose Castillejo mobility programme (CAS18/0033). V. Amiridis acknowledges support from the European Research Council (grant no. 725698, D-TECT). A. Gkikas acknowledges support by the Hellenic Foundation for Research and Innovation (H.F.R.I.) under the “2nd Call for H.F.R.I. Research Projects to support Post-Doctoral Researchers” (project acronym: ATLANTAS, project number: 544). S. Kazadzis acknowledges the ACTRIS-CH (Aerosol, Clouds and Trace Gases Research Infrastructure–- Swiss contribution) funded by the State Secretariat for Education, Research, and Innovation, Switzerland. Work of P. Dagsson-Waldhauserova was partly funded by the Czech Science Foundation (HLD-CHANGE project, no. 20-06168Y). C. Pérez García-Pando acknowledges the long-term support from the AXA Research Fund, as well as the support received through the Ramón y Cajal programme (grant RYC-2015-18690) of the Spanish Ministry of Economy and Competitiveness, and the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (grant agreement No. 773051).B. Weinzierl acknowledges funding under the European Union’s Horizon 2020 research and innovation programme (grant agreement No. 640458, A‐LIFE). Mineral dust produced by wind erosion of arid and semi-arid surfaces is a major component of atmospheric aerosol that affects climate, weather, ecosystems, and socio-economic sectors such as human health, transportation, solar energy, and air quality. Understanding these effects and ultimately improving the resilience of affected countries requires a reliable, dense, and diverse set of dust observations, fundamental for the development and the provision of skillful dust forecasts tailored products. The last decade has seen a notable improvement of dust observational capabilities in terms of considered parameters, geographical coverage, and delivery times, as well as of tailored products of interest to both the scientific community and the various end-users. Given this progress, here we review the current state of observational capabilities including in-situ, ground-based and satellite remote sensing observations, in Northern Africa, the Middle East and Europe for the provision of dust information considering the needs of various users. We also critically discuss observational gaps and related unresolved questions while providing suggestions for overcoming the current limitations. Our review aims to be a milestone for discussing dust observational gaps at a global level to address the needs of users, from research communities to nonscientific stakeholders "Article signat per 26 autors/es: Lucia Mona, Vassilis Amiridis, Emilio Cuevas, Antonis Gkikas, Serena Trippetta, Sophie Vandenbussche, Angela Benedetti, Pavla Dagsson-Waldhauserova, Paola Formenti, Alexander Haefele, Stelios Kazadzis, Peter Knippertz, Benoit Laurent, Fabio Madonna, Slobodan Nickovic, Nikolaos Papagiannopoulos, Gelsomina Pappalardo, Carlos Pérez García-Pando, Thomas Popp, Sergio Rodríguez, Andrea Sealy, Nobuo Sugimoto, Enric Terradellas, Ana Vukovic Vimic, Bernadette Weinzierl, and Sara Basart " Peer Reviewed
CNR ExploRA arrow_drop_down Bulletin of the American Meteorological Society; UPCommons. Portal del coneixement obert de la UPC; DLR publication serverOther literature type . Article . 2023 . Peer-reviewedUPCommons. Portal del coneixement obert de la UPCArticle . 2023Data sources: UPCommons. Portal del coneixement obert de la UPCRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2023 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!visibility 140visibility views 140 download downloads 146 Powered bymore_vert CNR ExploRA arrow_drop_down Bulletin of the American Meteorological Society; UPCommons. Portal del coneixement obert de la UPC; DLR publication serverOther literature type . Article . 2023 . Peer-reviewedUPCommons. Portal del coneixement obert de la UPCArticle . 2023Data sources: UPCommons. Portal del coneixement obert de la UPCRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2023 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Preprint 2023 Germany, France, Spain, Italy, FrancePublisher:Springer Science and Business Media LLC Abe, S.; Adams, J.; Allard, D.; Alldredge, P.; Anchordoqui, L.; Anzalone, A.; Arnone, E.; Baret, B.; Barghini, D.; Battisti, M.; Bayer, J.; Bellotti, R.; Belov, A.; Bertaina, M.; Bertone, P.; Bianciotto, M.; Biermann, P.; Bisconti, F.; Blaksley, C.; Blin-Bondil, S.; Bobik, P.; Bolmgren, K.; Briz, S.; Burton, J.; Cafagna, F.; Cambié, G.; Campana, D.; Capel, F.; Caruso, R.; Casolino, M.; Cassardo, C.; Castellina, A.; Černý, K.; Christl, M.; Colalillo, R.; Conti, L.; Cotto, G.; Crawford, H.; Cremonini, R.; Creusot, A.; Cummings, A.; Castro Gónzalez, A.; Taille, C.; Peral, L.; Diesing, R.; Dinaucourt, P.; Nola, A.; Ebersoldt, A.; Ebisuzaki, T.; Eser, J.; Fenu, F.; Ferrarese, S.; Filippatos, G.; Finch, W.; Flaminio, F.; Fornaro, C.; Fuehne, D.; Fuglesang, C.; Fukushima, M.; Gardiol, D.; Garipov, G.; Golzio, A.; Gorodetzky, P.; Guarino, F.; Guépin, C.; Guzmán, A.; Haungs, A.; Heibges, T.; Hernández-Carretero, J.; Isgrò, F.; Judd, E.; Kajino, F.; Kaneko, I.; Kawasaki, Y.; Kleifges, M.; Klimov, P.; Kreykenbohm, I.; Krizmanic, J.; Kungel, V.; Kuznetsov, E.; López Martínez, F.; Mackovjak, S.; Mandát, D.; Manfrin, M.; Marcelli, A.; Marcelli, L.; Marszał, W.; Matthews, J.; Menshikov, A.; Mernik, T.; Mese, M.; Meyer, S.; Mimouni, J.; Miyamoto, H.; Mizumoto, Y.; Monaco, A.; Morales de los Ríos, J.A; Nagataki, S.; Nachtman, J.; Naumov, D.; Neronov, A.; Nonaka, T.; Ogawa, T.; Ogio, S.; Ohmori, H.; Olinto, A.; Onel, Y.; Osteria, G.; Pagliaro, A.; Panico, B.; Parizot, E.; Park, I.; Pastircak, B.; Paul, T.; Pech, M.; Perfetto, F.; Picozza, P.; Piotrowski, L.; Plebaniak, Z.; Posligua, J.; Prevete, R.; Prévôt, G.; Prieto, H.; Przybylak, M.; Putis, M.; Reali, E.; Reardon, P.; Reno, M.; Ricci, M.; Rodríguez Frías, M.; Romoli, G.; Sáez Cano, G.; Sagawa, H.; Sakaki, N.; Santangelo, A.; Saprykin, O.; Sarazin, F.; Sato, M.; Schieler, H.; Schovánek, P.; Scotti, V.; Selmane, S.; Sharakin, S.; Shinozaki, K.; Soriano, J.; Szabelski, J.; Tajima, N.; Tajima, T.; Takahashi, Y.; Takeda, M.; Takizawa, Y.; Tenzer, C.; Thomas, S.; Tkachev, L.; Tomida, T.; Toscano, S.; Traïche, M.; Trofimov, D.; Tsuno, K.; Vallania, P.; Valore, L.; Venters, T.; Vigorito, C.; Ballmoos, P.; Vrabel, M.; Wada, S.; Watts, J.; Weindl, A.; Wiencke, L.; Wilms, J.; Winn, D.; Wistrand, H.; Yashin, I.; Young, R.; Zotov, M.;JEM-EUSO is an international program for the development of space-based Ultra-High Energy Cosmic Ray observatories. The program consists of a series of missions which are either under development or in the data analysis phase. All instruments are based on a wide-field-of-view telescope, which operates in the near-UV range, designed to detect the fluorescence light emitted by extensive air showers in the atmosphere. We describe the simulation software ESAF in the framework of the JEM-EUSO program and explain the physical assumptions used. We present here the implementation of the JEM-EUSO, POEMMA, K-EUSO, TUS, Mini-EUSO, EUSO-SPB1 and EUSO-TA configurations in ESAF. For the first time ESAF simulation outputs are compared with experimental data. Comunidad de Madrid
Archivio Istituziona... arrow_drop_down Archivio Istituzionale (AperTO); European Physical Journal C: Particles and Fields; Biblioteca Digital de la Universidad de AlcaláOther literature type . Article . 2023 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.science/hal-04288595/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 3 citations 3 popularity Average influence Average impulse Average Powered by BIP!more_vert Archivio Istituziona... arrow_drop_down Archivio Istituzionale (AperTO); European Physical Journal C: Particles and Fields; Biblioteca Digital de la Universidad de AlcaláOther literature type . Article . 2023 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.science/hal-04288595/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 France, Belgium, Italy, Spain, Sweden, United Kingdom, Sweden, PolandPublisher:Elsevier BV Funded by:EC | ALECEC| ALECTianyu Zhao; Iana Markevych; Elaine Fuertes; Kees de Hoogh; Simone Accordini; Anne Boudier; Lidia Casas; Bertil Forsberg; Judith Garcia Aymerich; Marco Gnesi; Mathias Holm; Christer Janson; Deborah Jarvis; Ane Johannessen; Rudolf A. Jörres; Stefan Karrasch; Benedicte Leynaert; José Antonio Maldonado Perez; Andrei Malinovschi; Jesús Martínez-Moratalla; Lars Modig; Dennis Nowak; James Potts; Nicole Probst-Hensch; José Luis Sánchez-Ramos; Valerie Siroux; Isabel Urrutia Landa; Danielle Vienneau; Simona Villani; Bénédicte Jacquemin; Joachim Heinrich;Background: While the adverse effects of short-term ambient ozone exposure on lung function are well-documented, the impact of long-term exposure remains poorly understood, especially in adults. Methods: We aimed to investigate the association between long-term ozone exposure and lung function decline. The 3014 participants were drawn from 17 centers across eight countries, all of which were from the European Community Respiratory Health Survey (ECRHS). Spirometry was conducted to measure pre-bronchodilation forced expiratory volume in 1 s (FEV1) and forced vital capacity (FVC) at approximately 35, 44, and 55 years of age. We assigned annual mean values of daily maximum running 8-h average ozone concentrations to individual residential addresses. Adjustments were made for PM2.5, NO2, and greenness. To capture the ozone-related change in spirometric parameters, our linear mixed effects regression models included an interaction term between long-term ozone exposure and age. Findings: Mean ambient ozone concentrations were approximately 65 μg/m³. A one interquartile range increase of 7 μg/m³ in ozone was associated with a faster decline in FEV1 of -2.08 mL/year (95% confidence interval: -2.79, -1.36) and in FVC of -2.86 mL/year (-3.73, -1.99) mL/year over the study period. Associations were robust after adjusting for PM2.5, NO2, and greenness. The associations were more pronounced in residents of northern Europe and individuals who were older at baseline. No consistent associations were detected with the FEV1/FVC ratio. Interpretation: Long-term exposure to elevated ambient ozone concentrations was associated with a faster decline of spirometric lung function among middle-aged European adults over a 20-year period. Funding: German Research Foundation. The present analyses are part of the Ageing Lungs in European Cohorts (ALEC) Study (www.alecstudy.org), which has also received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 633212. The local investigators and funding agencies for the European Community Respiratory Health are reported in the Supplementary Material.
IRIS - Università de... arrow_drop_down IRIS - Università degli Studi di Verona; The Lancet Regional Health. EuropeArticle . 2023 . Peer-reviewedLicense: CC BYIRIS - Università degli Studi di VeronaArticle . 2023Data sources: IRIS - Università degli Studi di VeronaSpiral - Imperial College Digital RepositoryArticle . 2023License: CC BYData sources: Spiral - Imperial College Digital RepositoryThe Lancet Regional Health. EuropeArticle . 2023Data sources: Institutional Repository Universiteit Antwerpenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesgold 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert IRIS - Università de... arrow_drop_down IRIS - Università degli Studi di Verona; The Lancet Regional Health. EuropeArticle . 2023 . Peer-reviewedLicense: CC BYIRIS - Università degli Studi di VeronaArticle . 2023Data sources: IRIS - Università degli Studi di VeronaSpiral - Imperial College Digital RepositoryArticle . 2023License: CC BYData sources: Spiral - Imperial College Digital RepositoryThe Lancet Regional Health. EuropeArticle . 2023Data sources: Institutional Repository Universiteit Antwerpenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 ItalyPublisher:Elsevier BV Negrel P.; Ladenberger A.; Reimann C.; Demetriades A.; Birke M.; Sadeghi M.; Albanese S.; Andersson M.; Baritz R.; Batista M. J.; Bel-lan A.; Cicchella D.; De Vivo B.; De Vos W.; Dinelli E.; Duris M.; Dusza-Dobek A.; Eklund M.; Ernstsen V.; Filzmoser P.; Flem B.; Flight D. M. A.; Forrester S.; Fuchs M.; Fugedi U.; Gilucis A.; Gosar M.; Gregorauskiene V.; De Groot W.; Gulan A.; Halamic J.; Haslinger E.; Hayoz P.; Hoffmann R.; Hoogewerff J.; Hrvatovic H.; Husnjak S.; Janik L.; Jordan G.; Kaminari M.; Kirby J.; Kivisilla J.; Klos V.; Krone F.; Kwecko P.; Kuti L.; Lima A.; Locutura J.; Lucivjansky D. P.; Mann A.; Mackovych D.; Matschullat J.; McLaughlin M.; Malyuk B. I.; Maquil R.; Meuli R. G.; Mol G.; O'Connor P.; Oorts R. K.; Ottesen R. T.; Pasieczna A.; Petersell W.; Pfleiderer S.; Ponavic M.; Pramuka S.; Prazeres C.; Rauch U.; Radusinovic S.; Salpeteur I.; Scanlon R.; Schedl A.; Scheib A. J.; Schoeters I.; Sefcik P.; Sellersjo E.; Skopljak F.; Slaninka I.; Sorsa A.; Srvkota R.; Stafilov T.; Tarvainen T.; Trendavilov V.; Valera P.; Verougstraete V.; Vidojevic D.; Zissimos A.; Zomeni Z.;The chemical composition of soil represents to a large extent the primary mineralogy and geochemistry of the source bedrock, the effects of pre- and post-depositional weathering and element mobility, either by leaching or mineral sorting with the addition of secondary products such as clays. Agricultural soil in Europe (0–20 cm, 33 countries, 5.6 million km2) was sampled during the continental-scale soil mapping project (GEochemical Mapping of Agricultural and grazing land Soil - GEMAS). Total element concentrations were determined by wavelength dispersive X-ray fluorescence spectrometry. Bulk content of major elements (SiO2, TiO2, Al2O3, Fe2O3, MgO, CaO, Na2O, K2O, P2O5) in soil has been used to calculate weathering indices such as chemical index of alteration (CIA), reductive and oxidative mafic indices of alteration (MIA), the change in mass balance (τ calculation relative to immobile Nb) for soil derived from silicate bedrocks (granite, gneiss and schist) at the European continental-scale, which are useful tools for evaluating chemical weathering trends.The greatest variation of CIA values is exhibited by soil derived from granite, followed by soil derived from schist. The CIA results show clearly that Ca and Na are removed from agricultural soil (0–20 cm) during soil development. Geographical distribution of weathering indices shows that weak chemical weathering of agricultural soil samples, sourced from gneissic and granitic bedrock, occurs in the Fennoscandian Shield; intermediate chemical weathering in granite, schist and gneiss occurring in the Iberian Peninsula and France, and intense chemical weathering in schist sourced agricultural soil occurring in areas with intense rainfall and moderate temperature (Wales, England, Ireland and western Iberia). In addition, values of CIA and MIA, higher than those for standard rock compositions, suggest more active enrichment/depletion processes during soil formation and subsequent soil weathering/maturation.The range of the elemental mass transfer coefficient τ is wide for agricultural soil derived from gneiss and granite, and narrow for agricultural soil sourced from schist parent rocks. The weathering behaviour of chemical elements, assessed by using the τ mass transport model, suggests an order of susceptibility of K ≈ Na > Al > Fe > Ca > Mg > Ti.Weathering indices and gain-loss mass transfer coefficients, tested on agricultural soil samples, provide an insight to the weathering processes affecting the silicate parent rocks and their impact on soil development at the European scale. This can have further implications for evaluation of soil nutritional conditions and mitigating of soil erosion and deprivation.
Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Alma Mater Studiorum Università di Bologna; Chemical GeologyArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Alma Mater Studiorum Università di Bologna; Chemical GeologyArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023Publisher:Wiley Francesca Meneghini; Maria Di Rosa; Michele Marroni; Hugues Raimbourg; Luca Pandolfi;doi: 10.1111/ter.12694
AbstractThe Internal Ligurian units (Northern Apennine) represent deformed and metamorphosed fragments of the oceanic lithosphere of the Ligure–Piemontese oceanic basin. Different tectonic models have been proposed for the geodynamic setting in which the deformation and metamorphism have been acquired. However, the lack of updated, clear, thermo‐barometric data has made it hard to unambiguously discriminate between these different proposed models. In this article, we provide evidence for the deformation of the Palombini Shale, i.e., pelagic deposits belonging to the Internal Ligurian units, under P and T peak conditions of 230–300°C. and 0.6–0.9 GPa, respectively. These data indicate that the Internal Ligurian units were affected by a blueschist facies metamorphism achieved during the underplating within the accretionary wedge developed during the Late Cretaceous—Early Tertiary Alpine subduction. These data support the hypothesis of a unique, pre‐Oligocene orogenic system for the Alpine belt and the westernmost sector of the Northern Apennines belt.
Terra Nova arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert Terra Nova arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2023 Germany, United Kingdom, Netherlands, Italy, Denmark, Italy, Switzerland, Switzerland, Austria, Belgium, Italy, France, GermanyPublisher:Springer Science and Business Media LLC Ma, Haozhi; Crowther, Thomas W.; Crowther, Thomas W.; Mo, Lidong; Maynard, Daniel S.; Renner, Susanne S.; Van Den Hoogen, Johan; Zou, Yibiao; Liang, Jingjing; De-Miguel, Sergio; Nabuurs, Gert-Jan; Reich, Peter B.; Niinemets, Ülo; Abegg, Meinrad; Adou Yao, Yves C.; Alberti, Giorgio; Almeyda Zambrano, Angelica M.; Alvarado, Braulio Vilchez; Alvarez-Dávila, Esteban; Alvarez-Loayza, Patricia; Alves, Luciana F.; Ammer, Christian; Antón-Fernández, Clara; Araujo-Murakami, Alejandro; Arroyo, Luzmila; Avitabile, Valerio; Aymard, Gerardo A.; Baker, Timothy R.; Bałazy, Radomir; Banki, Olaf; Barroso, Jorcely G.; Bastian, Meredith L.; Bastin, Jean-Francois; Birigazzi, Luca; Birnbaum, Philippe; Bitariho, Robert; Boeckx, Pascal; Bongers, Frans; Bouriaud, Olivier; Brancalion, Pedro H. S.; Brandl, Susanne; Brearley, Francis Q.; Brienen, Roel; Broadbent, Eben N.; Bruelheide, Helge; Bussotti, Filippo; Cazzolla Gatti, Roberto; César, Ricardo G.; Cesljar, Goran; Chazdon, Robin; Chen, Han Y. H.; Chisholm, Chelsea; Cho, Hyunkook; Cienciala, Emil; Clark, Connie; Clark, David; Colletta, Gabriel D.; Coomes, David A.; Valverde, Fernando Cornejo; Corral-Rivas, José J.; Crim, Philip M.; Cumming, Jonathan R.; Dayanandan, Selvadurai; De Gasper, André L.; Decuyper, Mathieu; Derroire, Géraldine; DeVries, Ben; Djordjevic, Ilija; Dolezal, Jiri; Dourdain, Aurélie; Engone Obiang, Nestor Laurier; Enquist, Brian J.; Eyre, Teresa J.; Fandohan, Adandé Belarmain; Fayle, Tom M.; Feldpausch, Ted R.; Ferreira, Leandro V.; Finér, Leena; Fischer, Markus; Fletcher, Christine; Fridman, Jonas; Frizzera, Lorenzo; Gamarra, Javier G. P.; Gianelle, Damiano; Glick, Henry B.; Harris, David J.; Hector, Andrew; Hemp, Andreas; Hengeveld, Geerten; Hérault, Bruno; Herbohn, John L.; Herold, Martin; Hillers, Annika; Honorio Coronado, Eurídice N.; Hui, Cang; Ibanez, Thomas T.; Amaral, Iêda; Imai, Nobuo; Jagodziński, Andrzej M.; Jaroszewicz, Bogdan; Johannsen, Vivian Kvist; Joly, Carlos A.; Jucker, Tommaso; Jung, Ilbin; Karminov, Viktor; Kartawinata, Kuswata; Kearsley, Elizabeth; Kenfack, David; Kennard, Deborah K.; Kepfer-Rojas, Sebastian; Keppel, Gunnar; Khan, Mohammed Latif; Khan, Mohammed Latif; Killeen, Timothy J.; Kim, Hyun Seok; Kitayama, Kanehiro; Köhl, Michael; Korjus, Henn; Kraxner, Florian; Kucher, Dmitry; Laarmann, Diana; Lang, Mait; Lewis, Simon L.; Lu, Huicui; Lukina, Natalia V.; Maitner, Brian S.; Malhi, Yadvinder; Marcon, Eric; Marimon, Beatriz Schwantes; Marimon-Junior, Ben Hur; Marshall, Andrew R.; Martin, Emanuel H.; Meave, Jorge A.; Melo-Cruz, Omar; Mendoza, Casimiro; Merow, Cory; Monteagudo Mendoza, Abel; Moreno, Vanessa S.; Mukul, Sharif A.; Mundhenk, Philip; Nava-Miranda, María Guadalupe; Neill, David; Neldner, Victor J.; Nevenic, Radovan V.; Ngugi, Michael R.; Niklaus, Pascal A.; Oleksyn, Jacek; Ontikov, Petr; Ortiz-Malavasi, Edgar; Pan, Yude; Paquette, Alain; Parada-Gutierrez, Alexander; Parfenova, Elena I.; Park, Minjee; Parren, Marc; Parthasarathy, Narayanaswamy; Peri, Pablo L.; Pfautsch, Sebastian; Phillips, Oliver L.; Picard, Nicolas; Piedade, Maria Teresa F.; Piotto, Daniel; Pitman, Nigel C. A.; Mendoza-Polo, Irina; Poulsen, Axel D.; Poulsen, John R.; Pretzsch, Hans; Ramirez Arevalo, Freddy; Restrepo-Correa, Zorayda; Rodeghiero, Mirco; Rolim, Samir G.; Roopsind, Anand; Rovero, Francesco; Rutishauser, Ervan; Saikia, Purabi; Salas-Eljatib, Christian; Saner, Philippe; Schall, Peter; Schelhaas, Mart-Jan; Schepaschenko, Dmitry; Scherer-Lorenzen, Michael; Schmid, Bernhard; Schöngart, Jochen; Searle, Eric B.; Seben, Vladimír; Serra-Diaz, Josep M.; Sheil, Douglas; Shvidenko, Anatoly Z.; Silva-Espejo, Javier E.; Silveira, Marcos; Singh, James; Sist, Plinio; Slik, Ferry; Sonké, Bonaventure; Souza, Alexandre F.; Miścicki, Stanislaw; Stereńczak, Krzysztof J.; Svenning, Jens-Christian; Svoboda, Miroslav; Swanepoel, Ben; Tchebakova, Nadja; Ter Steege, Hans; Umunay, Peter M.; Van Der Plas, Fons; Van Do, Tran; Verbeeck, Hans; Viana, Helder; Vibrans, Alexander C.; Vieira, Simone; Westerlund, Bertil; Wiser, Susan K.; Zo-Bi, Irie C.; Zohner, Constantin M.;doi: 10.1038/s41477-023-01543-5 , 10.3929/ethz-b-000643725 , 10.5445/ir/1000163924 , 10.48350/187399
pmid: 37872262
pmc: PMC10654052
Understanding what controls global leaf type variation in trees is crucial for comprehending their role in terrestrial ecosystems, including carbon, water and nutrient dynamics. Yet our understanding of the factors influencing forest leaf types remains incomplete, leaving us uncertain about the global proportions of needle-leaved, broadleaved, evergreen and deciduous trees. To address these gaps, we conducted a global, ground-sourced assessment of forest leaf-type variation by integrating forest inventory data with comprehensive leaf form (broadleaf vs needle-leaf) and habit (evergreen vs deciduous) records. We found that global variation in leaf habit is primarily driven by isothermality and soil characteristics, while leaf form is predominantly driven by temperature. Given these relationships, we estimate that 38% of global tree individuals are needle-leaved evergreen, 29% are broadleaved evergreen, 27% are broadleaved deciduous and 5% are needle-leaved deciduous. The aboveground biomass distribution among these tree types is approximately 21% (126.4 Gt), 54% (335.7 Gt), 22% (136.2 Gt) and 3% (18.7 Gt), respectively. We further project that, depending on future emissions pathways, 17–34% of forested areas will experience climate conditions by the end of the century that currently support a different forest type, highlighting the intensification of climatic stress on existing forests. By quantifying the distribution of tree leaf types and their corresponding biomass, and identifying regions where climate change will exert greatest pressure on current leaf types, our results can help improve predictions of future terrestrial ecosystem functioning and carbon cycling. Nature Plants, 9 (11) ISSN:2055-026X ISSN:2055-0278
Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Fondazione Edmund MachArticle . 9999 . 2023Nature Plants; PURE Aarhus University; IRIS - Institutional Research Information System of the University of TrentoArticle . 2023 . Peer-reviewedLicense: CC BYGFZ German Research Centre for GeosciencesArticle . 2023License: CC BYData sources: GFZ German Research Centre for GeosciencesGhent University Academic BibliographyArticle . 2023Data sources: Ghent University Academic BibliographyCopenhagen University Research Information SystemArticle . 2023Data sources: Copenhagen University Research Information SystemBern Open Repository and Information System (BORIS)Article . 2023 . Peer-reviewedData sources: Bern Open Repository and Information System (BORIS)Flore (Florence Research Repository)Article . 2023Data sources: Flore (Florence Research Repository)Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.inrae.fr/hal-04288936/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Fondazione Edmund MachArticle . 9999 . 2023Nature Plants; PURE Aarhus University; IRIS - Institutional Research Information System of the University of TrentoArticle . 2023 . Peer-reviewedLicense: CC BYGFZ German Research Centre for GeosciencesArticle . 2023License: CC BYData sources: GFZ German Research Centre for GeosciencesGhent University Academic BibliographyArticle . 2023Data sources: Ghent University Academic BibliographyCopenhagen University Research Information SystemArticle . 2023Data sources: Copenhagen University Research Information SystemBern Open Repository and Information System (BORIS)Article . 2023 . Peer-reviewedData sources: Bern Open Repository and Information System (BORIS)Flore (Florence Research Repository)Article . 2023Data sources: Flore (Florence Research Repository)Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.inrae.fr/hal-04288936/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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description Publicationkeyboard_double_arrow_right Article 2024 ItalyPublisher:Elsevier BV Arienti, G; Bistacchi, A; Caumon, G; Dal Piaz, G; Monopoli, B; Bertolo, D;International audience; Leveraging a high resolution geological and structural dataset acquired over decades of fieldwork, we build the 3D structural model of a portion of the highly deformed core of the Alpine orogen, in the Northern Aosta Valley. The model represents tectonic contacts separating the tectono-metamorphic units outcropping along the section between Mont Blanc and Monte Rosa, and it covers an area of ca. 1500 km2. The input source data include original 1:10,000 geological surveys synthetised in a 1:75,000 tectonic map, and a dense database of structural stations. After a first orientation statistics study of the structural field database, our workflow develops through structural interpretation in vertical cross-sections that allow including in the modelling process structural drivers such as crosscutting relationships, interference patterns, kinematic constraints and fold morphology from detailed field studies. Three-dimensional interpolation on a tetrahedral mesh using the implicit Discrete Smooth Interpolator method follows, using also foliation and fold axes data as interpolation constraints. After describing the workflow and the model, we discuss the difficulties of modelling in polydeformed metamorphic complexes. In particular, we address the issue of modelling shear zones, refolded, isoclinal and/or recumbent folds and dense networks of faults, that characterise the geology of the Northern Aosta Valley.
Journal of Structura... arrow_drop_down Journal of Structural Geology; BOA - Bicocca Open ArchiveArticle . 2024 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la CommunicationArticle . 2024Full-Text: https://hal.science/hal-04388453/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Journal of Structura... arrow_drop_down Journal of Structural Geology; BOA - Bicocca Open ArchiveArticle . 2024 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la CommunicationArticle . 2024Full-Text: https://hal.science/hal-04388453/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2024Publisher:Geological Society of London Dominique Cluzel; Alessandra Montanini; Arianna Secchiari; Elisa Ferrari; Matt Heizler; Fred Jourdan; Sebastien Meffre; Renjie Zhou; Christian Teyssier;The New Caledonia Ophiolite is cross-cut by coarse- to medium-grained pyroxenite and hornblende gabbro/diorite dykes intruded between 55.5 and 50 Ma (U–Pb zircon and 40 Ar/ 39 Ar hornblende), whereas the finer grained dolerites of tholeiitic affinity are younger (50–47 Ma). The production of hornblende gabbros/diorites was modelled by moderate degrees (20–40%) of partial melting of the high-temperature amphibolites of the metamorphic sole. The end-member compositions (hornblendites and anorthosites) resulted from solid-state phase segregation of crystal mushes within tectonically active magmatic conduits. Cascade reactions of the slab melts with mantle wedge peridotites successively formed clinoenstatite-bearing boninite magmas, which fed gabbronorite cumulate lenses at the mantle–crust transition; in turn, the clinoenstatite-bearing boninite melts reacted with peridotites to form websterites. The youngest magmas (of tholeiitic affinity) appeared c. 6 Myr after the inception of subduction when the cooler subducting slab plunged more steeply. Incipient slab retreat allowed corner flow, triggering low-pressure hydrous melting of the uplifted asthenosphere. The early stages of forearc magmatism were closely associated with transcurrent shear zones, which recorded oblique subduction inception. The early Eocene tectonic and magmatic features of the New Caledonia Ophiolite provide evidence for a north- or NE-dipping hot (forced) subduction zone in the SW Pacific, notably distinct from the slightly younger west-dipping Izu-Bonin–Marianna cold (spontaneous) subduction system. Supplementary material: Field pictures, additional diagrams, GPS location of dated samples, whole-rock geochemical and isotope data, Ar/Ar data, U–Pb zircon data, and distribution coefficients ( K d ) of trace elements used for modelling are available at https://doi.org/10.6084/m9.figshare.c.6949265 Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists
figshare arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2024add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert figshare arrow_drop_down Mémoires en Sciences de l'Information et de la CommunicationArticle . 2024add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Preprint , Other literature type 2023 FrancePublisher:American Physical Society (APS) Funded by:SNSF | Experimental Particle and..., ANR | SUNCORE, NSERC +6 projectsSNSF| Experimental Particle and Astroparticle Physics Beyond The Standard Model ,ANR| SUNCORE ,NSERC ,EC| INPhINIT ,EC| SK2HK ,SNSF| Towards neutrino CP violation: Strengthening the Japanese neutrino program T2K and Hyper-Kamiokande ,EC| JENNIFER2 ,EC| FELLINI ,SNSF| TOWARDS THE IMPROVEMENT OF NEUTRINO OSCILLATION MEASUREMENTS: T2K AND THE JAPANESE PROGRAMK. Abe; N. Akhlaq; R. Akutsu; H. Alarakia-Charles; A. Ali; Y. I. Alj Hakim; S. Alonso Monsalve; C. Alt; C. Andreopoulos; M. Antonova; S. Aoki; T. Arihara; Y. Asada; Y. Ashida; E. T. Atkin; M. Barbi; G. J. Barker; G. Barr; D. Barrow; M. Batkiewicz-Kwasniak; F. Bench; V. Berardi; L. Berns; S. Bhadra; A. Blanchet; A. Blondel; S. Bolognesi; T. Bonus; S. Bordoni; S. B. Boyd; A. Bravar; C. Bronner; S. Bron; A. Bubak; M. Buizza Avanzini; J. A. Caballero; N. F. Calabria; S. Cao; D. Carabadjac; A. J. Carter; S. L. Cartwright; M. P. Casado; M. G. Catanesi; A. Cervera; J. Chakrani; D. Cherdack; P. S. Chong; G. Christodoulou; A. Chvirova; M. Cicerchia; J. Coleman; G. Collazuol; L. Cook; A. Cudd; C. Dalmazzone; T. Daret; P. Dasgupta; Yu. I. Davydov; A. De Roeck; G. De Rosa; T. Dealtry; C. C. Delogu; C. Densham; A. Dergacheva; F. Di Lodovico; S. Dolan; D. Douqa; T. A. Doyle; O. Drapier; J. Dumarchez; P. Dunne; K. Dygnarowicz; A. Eguchi; S. Emery-Schrenk; G. Erofeev; A. Ershova; G. Eurin; D. Fedorova; S. Fedotov; M. Feltre; A. J. Finch; G. A. Fiorentini Aguirre; G. Fiorillo; M. D. Fitton; J. M. Franco Patiño; M. Friend; Y. Fujii; Y. Fukuda; Y. Furui; K. Fusshoeller; L. Giannessi; C. Giganti; V. Glagolev; M. Gonin; J. González Rosa; E. A. G. Goodman; A. Gorin; M. Grassi; M. Guigue; D. R. Hadley; J. T. Haigh; P. Hamacher-Baumann; D. A. Harris; M. Hartz; T. Hasegawa; S. Hassani; N. C. Hastings; Y. Hayato; D. Henaff; A. Hiramoto; M. Hogan; J. Holeczek; A. Holin; T. Holvey; N. T. Hong Van; T. Honjo; F. Iacob; A. K. Ichikawa; M. Ikeda; T. Ishida; M. Ishitsuka; H. T. Israel; A. Izmaylov; N. Izumi; M. Jakkapu; B. Jamieson; S. J. Jenkins; C. Jesús-Valls; J. J. Jiang; J. Y. Ji; P. Jonsson; S. Joshi; C. K. Jung; P. B. Jurj; M. Kabirnezhad; A. C. Kaboth; T. Kajita; H. Kakuno; J. Kameda; S. P. Kasetti; Y. Kataoka; T. Katori; M. Kawaue; E. Kearns; M. Khabibullin; A. Khotjantsev; T. Kikawa; S. King; V. Kiseeva; J. Kisiel; T. Kobata; H. Kobayashi; T. Kobayashi; L. Koch; S. Kodama; A. Konaka; L. L. Kormos; Y. Koshio; A. Kostin; T. Koto; K. Kowalik; Y. Kudenko; Y. Kudo; S. Kuribayashi; R. Kurjata; T. Kutter; M. Kuze; M. La Commara; L. Labarga; K. Lachner; J. Lagoda; S. M. Lakshmi; M. Lamers James; M. Lamoureux; A. Langella; J.-F. Laporte; D. Last; N. Latham; M. Laveder; L. Lavitola; M. Lawe; Y. Lee; C. Lin; S.-K. Lin; R. P. Litchfield; S. L. Liu; W. Li; A. Longhin; K. R. Long; A. Lopez Moreno; L. Ludovici; X. Lu; T. Lux; L. N. Machado; L. Magaletti; K. Mahn; M. Malek; M. Mandal; S. Manly; A. D. Marino;This paper reports the first measurement of muon neutrino charged-current interactions without pions in the final state using multiple detectors with correlated energy spectra at T2K. The data was collected on hydrocarbon targets using the off-axis T2K near detector (ND280) and the on-axis T2K near detector (INGRID) with neutrino energy spectra peaked at 0.6 GeV and 1.1 GeV respectively. The correlated neutrino flux presents an opportunity to reduce the impact of the flux uncertainty and to study the energy dependence of neutrino interactions. The extracted double-differential cross sections are compared to several Monte Carlo neutrino-nucleus interaction event generators showing the agreement between both detectors individually and with the correlated result. Updated discussion in Sec. V-A; Updated author list
https://doi.org/10.1... arrow_drop_down https://doi.org/10.1103/physre...Article . 2023 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . Preprint . 2023add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert https://doi.org/10.1... arrow_drop_down https://doi.org/10.1103/physre...Article . 2023 . Peer-reviewedLicense: CC BYData sources: CrossrefMémoires en Sciences de l'Information et de la Communication; HAL-CEAArticle . Preprint . 2023add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 France, ItalyPublisher:Springer Science and Business Media LLC Mike Burton; Alessandro Aiuppa; Patrick Allard; María Asensio-Ramos; Ana Pardo Cofrades; Alessandro La Spina; Emma J. Nicholson; Vittorio Zanon; José Barrancos; Marcello Bitetto; Margaret Hartley; Jorge E. Romero; Emma Waters; Alex Stewart; Pedro A. Hernández; João Pedro Lages; Eleazar Padrón; Kieran Wood; Benjamin Esse; Catherine Hayer; Klaudia Cyrzan; Estelle F. Rose-Koga; Federica Schiavi; Luca D’Auria; Nemesio M. Pérez;handle: 10447/621695
AbstractAlkaline mafic magmas forming intra-plate oceanic islands are believed to be strongly enriched in CO2 due to low-degree partial melting of enriched mantle sources. However, until now, such CO2 enhancement has not been verified by measuring CO2 degassing during a subaerial eruption. Here, we provide evidence of highly CO2-rich gas emissions during the 86-day 2021 Tajogaite eruption of Cumbre Vieja volcano on La Palma Island, in the Canary archipelago. Our results reveal sustained high plume CO2/SO2 ratios, which, when combined with SO2 fluxes, melt inclusion volatile contents and magma production rates at explosive and effusive vents, imply a magmatic CO2 content of 4.5 ± 1.5 wt%. The amount of CO2 released during the 2021 eruptive activity was 28 ± 14 Mt CO2. Extrapolating to the volume of alkaline mafic magmas forming La Palma alone (estimated as 4000 km3 erupted over 11 Ma), we infer a maximum CO2 emission into the ocean and atmosphere of 1016 moles of CO2, equivalent to 20% of the eruptive CO2 emissions from a large igneous province eruption, suggesting that the formation of the Canary volcanic archipelago produced a CO2 emission of similar magnitude as a large igneous province.
Communications Earth... arrow_drop_down Communications Earth & Environment; Archivio istituzionale della ricerca - Università di PalermoArticle . 2023 . Peer-reviewedLicense: CC BYHAL Clermont Université; Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert Communications Earth... arrow_drop_down Communications Earth & Environment; Archivio istituzionale della ricerca - Università di PalermoArticle . 2023 . Peer-reviewedLicense: CC BYHAL Clermont Université; Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 Spain, Italy, GermanyPublisher:American Meteorological Society Funded by:EC | A-LIFE, EC | EUNADICS-AV, EC | FRAGMENT +1 projectsEC| A-LIFE ,EC| EUNADICS-AV ,EC| FRAGMENT ,EC| ACTRIS IMPMona, Licia; Amiridis, Vassilis; Cuevas, Emilio; Gkikas, Antonis; Trippetta, Serena; Vandenbussche, Sophie; Benedetti, Angela; Dagsson-Waldhauserova, Pavla; Formenti, Paola; Haefele, Alexander; Kazadzis, Stelios; Knippertz, Peter; Laurent, Benoit; Madonna, Fabio; Nickovic, S.; Papagiannopoulos, Nikolaos; Pappalardo, Gelsomina; Perez Garcia-Pando, Carlos; Popp, Thomas; Rodriguez, Sergio; Sealy, Andrea; Sugimoto, Nobuo; Terradellas, Enric; Vukovic Vimic, Ana; Weinzierl, Bernadett; Basart, Sara;handle: 10261/339009 , 20.500.11765/15177 , 2117/393050
Authors acknowledge dr Sangboom Ryoo of Korean Meteorological Administration in Seoul for his help and support.The research leading to these results has received funding from the COST ActionCA16202, supported by COST Association (European Cooperation in Science and Technology), from DustClim Project as part of ERA4CS, an ERA-NET initiated by JPI Climate, and funded by FORMAS (SE), DLR (DE), BMWFW (AT), IFD (DK), MINECO (ES), ANR (FR) with co-funding by the European Union (Grant 690462) and by the European Union’s Horizon 2020 research program for societal challenges – smart, green and integrated transport under grant agreement no.723986 (project EUNADICS-AV – European Natural Disaster Coordination and Information System for Aviation). L. Mona acknowledges the ACTRIS-IMP (Implementation project), funded by the European Union’s Horizon 2020 research and innovation programme (Grant no 871115) and the contribution of the ACTRIS-ITALIA JRU (CNR prot. n. 0067310/2017). S. Basart acknowledges CAMS-84 and CAMS2-82 (part of the Copernicus Atmospheric Monitoring Services, CAMS) and the Spanish Jose Castillejo mobility programme (CAS18/0033). V. Amiridis acknowledges support from the European Research Council (grant no. 725698, D-TECT). A. Gkikas acknowledges support by the Hellenic Foundation for Research and Innovation (H.F.R.I.) under the “2nd Call for H.F.R.I. Research Projects to support Post-Doctoral Researchers” (project acronym: ATLANTAS, project number: 544). S. Kazadzis acknowledges the ACTRIS-CH (Aerosol, Clouds and Trace Gases Research Infrastructure–- Swiss contribution) funded by the State Secretariat for Education, Research, and Innovation, Switzerland. Work of P. Dagsson-Waldhauserova was partly funded by the Czech Science Foundation (HLD-CHANGE project, no. 20-06168Y). C. Pérez García-Pando acknowledges the long-term support from the AXA Research Fund, as well as the support received through the Ramón y Cajal programme (grant RYC-2015-18690) of the Spanish Ministry of Economy and Competitiveness, and the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (grant agreement No. 773051).B. Weinzierl acknowledges funding under the European Union’s Horizon 2020 research and innovation programme (grant agreement No. 640458, A‐LIFE). Mineral dust produced by wind erosion of arid and semi-arid surfaces is a major component of atmospheric aerosol that affects climate, weather, ecosystems, and socio-economic sectors such as human health, transportation, solar energy, and air quality. Understanding these effects and ultimately improving the resilience of affected countries requires a reliable, dense, and diverse set of dust observations, fundamental for the development and the provision of skillful dust forecasts tailored products. The last decade has seen a notable improvement of dust observational capabilities in terms of considered parameters, geographical coverage, and delivery times, as well as of tailored products of interest to both the scientific community and the various end-users. Given this progress, here we review the current state of observational capabilities including in-situ, ground-based and satellite remote sensing observations, in Northern Africa, the Middle East and Europe for the provision of dust information considering the needs of various users. We also critically discuss observational gaps and related unresolved questions while providing suggestions for overcoming the current limitations. Our review aims to be a milestone for discussing dust observational gaps at a global level to address the needs of users, from research communities to nonscientific stakeholders "Article signat per 26 autors/es: Lucia Mona, Vassilis Amiridis, Emilio Cuevas, Antonis Gkikas, Serena Trippetta, Sophie Vandenbussche, Angela Benedetti, Pavla Dagsson-Waldhauserova, Paola Formenti, Alexander Haefele, Stelios Kazadzis, Peter Knippertz, Benoit Laurent, Fabio Madonna, Slobodan Nickovic, Nikolaos Papagiannopoulos, Gelsomina Pappalardo, Carlos Pérez García-Pando, Thomas Popp, Sergio Rodríguez, Andrea Sealy, Nobuo Sugimoto, Enric Terradellas, Ana Vukovic Vimic, Bernadette Weinzierl, and Sara Basart " Peer Reviewed
CNR ExploRA arrow_drop_down Bulletin of the American Meteorological Society; UPCommons. Portal del coneixement obert de la UPC; DLR publication serverOther literature type . Article . 2023 . Peer-reviewedUPCommons. Portal del coneixement obert de la UPCArticle . 2023Data sources: UPCommons. Portal del coneixement obert de la UPCRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2023 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!visibility 140visibility views 140 download downloads 146 Powered bymore_vert CNR ExploRA arrow_drop_down Bulletin of the American Meteorological Society; UPCommons. Portal del coneixement obert de la UPC; DLR publication serverOther literature type . Article . 2023 . Peer-reviewedUPCommons. Portal del coneixement obert de la UPCArticle . 2023Data sources: UPCommons. Portal del coneixement obert de la UPCRecolector de Ciencia Abierta, RECOLECTA; DIGITAL.CSICArticle . 2023 . Peer-reviewedadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Preprint 2023 Germany, France, Spain, Italy, FrancePublisher:Springer Science and Business Media LLC Abe, S.; Adams, J.; Allard, D.; Alldredge, P.; Anchordoqui, L.; Anzalone, A.; Arnone, E.; Baret, B.; Barghini, D.; Battisti, M.; Bayer, J.; Bellotti, R.; Belov, A.; Bertaina, M.; Bertone, P.; Bianciotto, M.; Biermann, P.; Bisconti, F.; Blaksley, C.; Blin-Bondil, S.; Bobik, P.; Bolmgren, K.; Briz, S.; Burton, J.; Cafagna, F.; Cambié, G.; Campana, D.; Capel, F.; Caruso, R.; Casolino, M.; Cassardo, C.; Castellina, A.; Černý, K.; Christl, M.; Colalillo, R.; Conti, L.; Cotto, G.; Crawford, H.; Cremonini, R.; Creusot, A.; Cummings, A.; Castro Gónzalez, A.; Taille, C.; Peral, L.; Diesing, R.; Dinaucourt, P.; Nola, A.; Ebersoldt, A.; Ebisuzaki, T.; Eser, J.; Fenu, F.; Ferrarese, S.; Filippatos, G.; Finch, W.; Flaminio, F.; Fornaro, C.; Fuehne, D.; Fuglesang, C.; Fukushima, M.; Gardiol, D.; Garipov, G.; Golzio, A.; Gorodetzky, P.; Guarino, F.; Guépin, C.; Guzmán, A.; Haungs, A.; Heibges, T.; Hernández-Carretero, J.; Isgrò, F.; Judd, E.; Kajino, F.; Kaneko, I.; Kawasaki, Y.; Kleifges, M.; Klimov, P.; Kreykenbohm, I.; Krizmanic, J.; Kungel, V.; Kuznetsov, E.; López Martínez, F.; Mackovjak, S.; Mandát, D.; Manfrin, M.; Marcelli, A.; Marcelli, L.; Marszał, W.; Matthews, J.; Menshikov, A.; Mernik, T.; Mese, M.; Meyer, S.; Mimouni, J.; Miyamoto, H.; Mizumoto, Y.; Monaco, A.; Morales de los Ríos, J.A; Nagataki, S.; Nachtman, J.; Naumov, D.; Neronov, A.; Nonaka, T.; Ogawa, T.; Ogio, S.; Ohmori, H.; Olinto, A.; Onel, Y.; Osteria, G.; Pagliaro, A.; Panico, B.; Parizot, E.; Park, I.; Pastircak, B.; Paul, T.; Pech, M.; Perfetto, F.; Picozza, P.; Piotrowski, L.; Plebaniak, Z.; Posligua, J.; Prevete, R.; Prévôt, G.; Prieto, H.; Przybylak, M.; Putis, M.; Reali, E.; Reardon, P.; Reno, M.; Ricci, M.; Rodríguez Frías, M.; Romoli, G.; Sáez Cano, G.; Sagawa, H.; Sakaki, N.; Santangelo, A.; Saprykin, O.; Sarazin, F.; Sato, M.; Schieler, H.; Schovánek, P.; Scotti, V.; Selmane, S.; Sharakin, S.; Shinozaki, K.; Soriano, J.; Szabelski, J.; Tajima, N.; Tajima, T.; Takahashi, Y.; Takeda, M.; Takizawa, Y.; Tenzer, C.; Thomas, S.; Tkachev, L.; Tomida, T.; Toscano, S.; Traïche, M.; Trofimov, D.; Tsuno, K.; Vallania, P.; Valore, L.; Venters, T.; Vigorito, C.; Ballmoos, P.; Vrabel, M.; Wada, S.; Watts, J.; Weindl, A.; Wiencke, L.; Wilms, J.; Winn, D.; Wistrand, H.; Yashin, I.; Young, R.; Zotov, M.;JEM-EUSO is an international program for the development of space-based Ultra-High Energy Cosmic Ray observatories. The program consists of a series of missions which are either under development or in the data analysis phase. All instruments are based on a wide-field-of-view telescope, which operates in the near-UV range, designed to detect the fluorescence light emitted by extensive air showers in the atmosphere. We describe the simulation software ESAF in the framework of the JEM-EUSO program and explain the physical assumptions used. We present here the implementation of the JEM-EUSO, POEMMA, K-EUSO, TUS, Mini-EUSO, EUSO-SPB1 and EUSO-TA configurations in ESAF. For the first time ESAF simulation outputs are compared with experimental data. Comunidad de Madrid
Archivio Istituziona... arrow_drop_down Archivio Istituzionale (AperTO); European Physical Journal C: Particles and Fields; Biblioteca Digital de la Universidad de AlcaláOther literature type . Article . 2023 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.science/hal-04288595/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen gold 3 citations 3 popularity Average influence Average impulse Average Powered by BIP!more_vert Archivio Istituziona... arrow_drop_down Archivio Istituzionale (AperTO); European Physical Journal C: Particles and Fields; Biblioteca Digital de la Universidad de AlcaláOther literature type . Article . 2023 . Peer-reviewedLicense: CC BY NC NDMémoires en Sciences de l'Information et de la Communication; HAL-CEA; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.science/hal-04288595/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 France, Belgium, Italy, Spain, Sweden, United Kingdom, Sweden, PolandPublisher:Elsevier BV Funded by:EC | ALECEC| ALECTianyu Zhao; Iana Markevych; Elaine Fuertes; Kees de Hoogh; Simone Accordini; Anne Boudier; Lidia Casas; Bertil Forsberg; Judith Garcia Aymerich; Marco Gnesi; Mathias Holm; Christer Janson; Deborah Jarvis; Ane Johannessen; Rudolf A. Jörres; Stefan Karrasch; Benedicte Leynaert; José Antonio Maldonado Perez; Andrei Malinovschi; Jesús Martínez-Moratalla; Lars Modig; Dennis Nowak; James Potts; Nicole Probst-Hensch; José Luis Sánchez-Ramos; Valerie Siroux; Isabel Urrutia Landa; Danielle Vienneau; Simona Villani; Bénédicte Jacquemin; Joachim Heinrich;Background: While the adverse effects of short-term ambient ozone exposure on lung function are well-documented, the impact of long-term exposure remains poorly understood, especially in adults. Methods: We aimed to investigate the association between long-term ozone exposure and lung function decline. The 3014 participants were drawn from 17 centers across eight countries, all of which were from the European Community Respiratory Health Survey (ECRHS). Spirometry was conducted to measure pre-bronchodilation forced expiratory volume in 1 s (FEV1) and forced vital capacity (FVC) at approximately 35, 44, and 55 years of age. We assigned annual mean values of daily maximum running 8-h average ozone concentrations to individual residential addresses. Adjustments were made for PM2.5, NO2, and greenness. To capture the ozone-related change in spirometric parameters, our linear mixed effects regression models included an interaction term between long-term ozone exposure and age. Findings: Mean ambient ozone concentrations were approximately 65 μg/m³. A one interquartile range increase of 7 μg/m³ in ozone was associated with a faster decline in FEV1 of -2.08 mL/year (95% confidence interval: -2.79, -1.36) and in FVC of -2.86 mL/year (-3.73, -1.99) mL/year over the study period. Associations were robust after adjusting for PM2.5, NO2, and greenness. The associations were more pronounced in residents of northern Europe and individuals who were older at baseline. No consistent associations were detected with the FEV1/FVC ratio. Interpretation: Long-term exposure to elevated ambient ozone concentrations was associated with a faster decline of spirometric lung function among middle-aged European adults over a 20-year period. Funding: German Research Foundation. The present analyses are part of the Ageing Lungs in European Cohorts (ALEC) Study (www.alecstudy.org), which has also received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 633212. The local investigators and funding agencies for the European Community Respiratory Health are reported in the Supplementary Material.
IRIS - Università de... arrow_drop_down IRIS - Università degli Studi di Verona; The Lancet Regional Health. EuropeArticle . 2023 . Peer-reviewedLicense: CC BYIRIS - Università degli Studi di VeronaArticle . 2023Data sources: IRIS - Università degli Studi di VeronaSpiral - Imperial College Digital RepositoryArticle . 2023License: CC BYData sources: Spiral - Imperial College Digital RepositoryThe Lancet Regional Health. EuropeArticle . 2023Data sources: Institutional Repository Universiteit Antwerpenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess Routesgold 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert IRIS - Università de... arrow_drop_down IRIS - Università degli Studi di Verona; The Lancet Regional Health. EuropeArticle . 2023 . Peer-reviewedLicense: CC BYIRIS - Università degli Studi di VeronaArticle . 2023Data sources: IRIS - Università degli Studi di VeronaSpiral - Imperial College Digital RepositoryArticle . 2023License: CC BYData sources: Spiral - Imperial College Digital RepositoryThe Lancet Regional Health. EuropeArticle . 2023Data sources: Institutional Repository Universiteit Antwerpenadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023 ItalyPublisher:Elsevier BV Negrel P.; Ladenberger A.; Reimann C.; Demetriades A.; Birke M.; Sadeghi M.; Albanese S.; Andersson M.; Baritz R.; Batista M. J.; Bel-lan A.; Cicchella D.; De Vivo B.; De Vos W.; Dinelli E.; Duris M.; Dusza-Dobek A.; Eklund M.; Ernstsen V.; Filzmoser P.; Flem B.; Flight D. M. A.; Forrester S.; Fuchs M.; Fugedi U.; Gilucis A.; Gosar M.; Gregorauskiene V.; De Groot W.; Gulan A.; Halamic J.; Haslinger E.; Hayoz P.; Hoffmann R.; Hoogewerff J.; Hrvatovic H.; Husnjak S.; Janik L.; Jordan G.; Kaminari M.; Kirby J.; Kivisilla J.; Klos V.; Krone F.; Kwecko P.; Kuti L.; Lima A.; Locutura J.; Lucivjansky D. P.; Mann A.; Mackovych D.; Matschullat J.; McLaughlin M.; Malyuk B. I.; Maquil R.; Meuli R. G.; Mol G.; O'Connor P.; Oorts R. K.; Ottesen R. T.; Pasieczna A.; Petersell W.; Pfleiderer S.; Ponavic M.; Pramuka S.; Prazeres C.; Rauch U.; Radusinovic S.; Salpeteur I.; Scanlon R.; Schedl A.; Scheib A. J.; Schoeters I.; Sefcik P.; Sellersjo E.; Skopljak F.; Slaninka I.; Sorsa A.; Srvkota R.; Stafilov T.; Tarvainen T.; Trendavilov V.; Valera P.; Verougstraete V.; Vidojevic D.; Zissimos A.; Zomeni Z.;The chemical composition of soil represents to a large extent the primary mineralogy and geochemistry of the source bedrock, the effects of pre- and post-depositional weathering and element mobility, either by leaching or mineral sorting with the addition of secondary products such as clays. Agricultural soil in Europe (0–20 cm, 33 countries, 5.6 million km2) was sampled during the continental-scale soil mapping project (GEochemical Mapping of Agricultural and grazing land Soil - GEMAS). Total element concentrations were determined by wavelength dispersive X-ray fluorescence spectrometry. Bulk content of major elements (SiO2, TiO2, Al2O3, Fe2O3, MgO, CaO, Na2O, K2O, P2O5) in soil has been used to calculate weathering indices such as chemical index of alteration (CIA), reductive and oxidative mafic indices of alteration (MIA), the change in mass balance (τ calculation relative to immobile Nb) for soil derived from silicate bedrocks (granite, gneiss and schist) at the European continental-scale, which are useful tools for evaluating chemical weathering trends.The greatest variation of CIA values is exhibited by soil derived from granite, followed by soil derived from schist. The CIA results show clearly that Ca and Na are removed from agricultural soil (0–20 cm) during soil development. Geographical distribution of weathering indices shows that weak chemical weathering of agricultural soil samples, sourced from gneissic and granitic bedrock, occurs in the Fennoscandian Shield; intermediate chemical weathering in granite, schist and gneiss occurring in the Iberian Peninsula and France, and intense chemical weathering in schist sourced agricultural soil occurring in areas with intense rainfall and moderate temperature (Wales, England, Ireland and western Iberia). In addition, values of CIA and MIA, higher than those for standard rock compositions, suggest more active enrichment/depletion processes during soil formation and subsequent soil weathering/maturation.The range of the elemental mass transfer coefficient τ is wide for agricultural soil derived from gneiss and granite, and narrow for agricultural soil sourced from schist parent rocks. The weathering behaviour of chemical elements, assessed by using the τ mass transport model, suggests an order of susceptibility of K ≈ Na > Al > Fe > Ca > Mg > Ti.Weathering indices and gain-loss mass transfer coefficients, tested on agricultural soil samples, provide an insight to the weathering processes affecting the silicate parent rocks and their impact on soil development at the European scale. This can have further implications for evaluation of soil nutritional conditions and mitigating of soil erosion and deprivation.
Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Alma Mater Studiorum Università di Bologna; Chemical GeologyArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Alma Mater Studiorum Università di Bologna; Chemical GeologyArticle . 2023 . Peer-reviewedLicense: Elsevier TDMadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article 2023Publisher:Wiley Francesca Meneghini; Maria Di Rosa; Michele Marroni; Hugues Raimbourg; Luca Pandolfi;doi: 10.1111/ter.12694
AbstractThe Internal Ligurian units (Northern Apennine) represent deformed and metamorphosed fragments of the oceanic lithosphere of the Ligure–Piemontese oceanic basin. Different tectonic models have been proposed for the geodynamic setting in which the deformation and metamorphism have been acquired. However, the lack of updated, clear, thermo‐barometric data has made it hard to unambiguously discriminate between these different proposed models. In this article, we provide evidence for the deformation of the Palombini Shale, i.e., pelagic deposits belonging to the Internal Ligurian units, under P and T peak conditions of 230–300°C. and 0.6–0.9 GPa, respectively. These data indicate that the Internal Ligurian units were affected by a blueschist facies metamorphism achieved during the underplating within the accretionary wedge developed during the Late Cretaceous—Early Tertiary Alpine subduction. These data support the hypothesis of a unique, pre‐Oligocene orogenic system for the Alpine belt and the westernmost sector of the Northern Apennines belt.
Terra Nova arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eu1 citations 1 popularity Average influence Average impulse Average Powered by BIP!more_vert Terra Nova arrow_drop_down add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.eudescription Publicationkeyboard_double_arrow_right Article , Other literature type 2023 Germany, United Kingdom, Netherlands, Italy, Denmark, Italy, Switzerland, Switzerland, Austria, Belgium, Italy, France, GermanyPublisher:Springer Science and Business Media LLC Ma, Haozhi; Crowther, Thomas W.; Crowther, Thomas W.; Mo, Lidong; Maynard, Daniel S.; Renner, Susanne S.; Van Den Hoogen, Johan; Zou, Yibiao; Liang, Jingjing; De-Miguel, Sergio; Nabuurs, Gert-Jan; Reich, Peter B.; Niinemets, Ülo; Abegg, Meinrad; Adou Yao, Yves C.; Alberti, Giorgio; Almeyda Zambrano, Angelica M.; Alvarado, Braulio Vilchez; Alvarez-Dávila, Esteban; Alvarez-Loayza, Patricia; Alves, Luciana F.; Ammer, Christian; Antón-Fernández, Clara; Araujo-Murakami, Alejandro; Arroyo, Luzmila; Avitabile, Valerio; Aymard, Gerardo A.; Baker, Timothy R.; Bałazy, Radomir; Banki, Olaf; Barroso, Jorcely G.; Bastian, Meredith L.; Bastin, Jean-Francois; Birigazzi, Luca; Birnbaum, Philippe; Bitariho, Robert; Boeckx, Pascal; Bongers, Frans; Bouriaud, Olivier; Brancalion, Pedro H. S.; Brandl, Susanne; Brearley, Francis Q.; Brienen, Roel; Broadbent, Eben N.; Bruelheide, Helge; Bussotti, Filippo; Cazzolla Gatti, Roberto; César, Ricardo G.; Cesljar, Goran; Chazdon, Robin; Chen, Han Y. H.; Chisholm, Chelsea; Cho, Hyunkook; Cienciala, Emil; Clark, Connie; Clark, David; Colletta, Gabriel D.; Coomes, David A.; Valverde, Fernando Cornejo; Corral-Rivas, José J.; Crim, Philip M.; Cumming, Jonathan R.; Dayanandan, Selvadurai; De Gasper, André L.; Decuyper, Mathieu; Derroire, Géraldine; DeVries, Ben; Djordjevic, Ilija; Dolezal, Jiri; Dourdain, Aurélie; Engone Obiang, Nestor Laurier; Enquist, Brian J.; Eyre, Teresa J.; Fandohan, Adandé Belarmain; Fayle, Tom M.; Feldpausch, Ted R.; Ferreira, Leandro V.; Finér, Leena; Fischer, Markus; Fletcher, Christine; Fridman, Jonas; Frizzera, Lorenzo; Gamarra, Javier G. P.; Gianelle, Damiano; Glick, Henry B.; Harris, David J.; Hector, Andrew; Hemp, Andreas; Hengeveld, Geerten; Hérault, Bruno; Herbohn, John L.; Herold, Martin; Hillers, Annika; Honorio Coronado, Eurídice N.; Hui, Cang; Ibanez, Thomas T.; Amaral, Iêda; Imai, Nobuo; Jagodziński, Andrzej M.; Jaroszewicz, Bogdan; Johannsen, Vivian Kvist; Joly, Carlos A.; Jucker, Tommaso; Jung, Ilbin; Karminov, Viktor; Kartawinata, Kuswata; Kearsley, Elizabeth; Kenfack, David; Kennard, Deborah K.; Kepfer-Rojas, Sebastian; Keppel, Gunnar; Khan, Mohammed Latif; Khan, Mohammed Latif; Killeen, Timothy J.; Kim, Hyun Seok; Kitayama, Kanehiro; Köhl, Michael; Korjus, Henn; Kraxner, Florian; Kucher, Dmitry; Laarmann, Diana; Lang, Mait; Lewis, Simon L.; Lu, Huicui; Lukina, Natalia V.; Maitner, Brian S.; Malhi, Yadvinder; Marcon, Eric; Marimon, Beatriz Schwantes; Marimon-Junior, Ben Hur; Marshall, Andrew R.; Martin, Emanuel H.; Meave, Jorge A.; Melo-Cruz, Omar; Mendoza, Casimiro; Merow, Cory; Monteagudo Mendoza, Abel; Moreno, Vanessa S.; Mukul, Sharif A.; Mundhenk, Philip; Nava-Miranda, María Guadalupe; Neill, David; Neldner, Victor J.; Nevenic, Radovan V.; Ngugi, Michael R.; Niklaus, Pascal A.; Oleksyn, Jacek; Ontikov, Petr; Ortiz-Malavasi, Edgar; Pan, Yude; Paquette, Alain; Parada-Gutierrez, Alexander; Parfenova, Elena I.; Park, Minjee; Parren, Marc; Parthasarathy, Narayanaswamy; Peri, Pablo L.; Pfautsch, Sebastian; Phillips, Oliver L.; Picard, Nicolas; Piedade, Maria Teresa F.; Piotto, Daniel; Pitman, Nigel C. A.; Mendoza-Polo, Irina; Poulsen, Axel D.; Poulsen, John R.; Pretzsch, Hans; Ramirez Arevalo, Freddy; Restrepo-Correa, Zorayda; Rodeghiero, Mirco; Rolim, Samir G.; Roopsind, Anand; Rovero, Francesco; Rutishauser, Ervan; Saikia, Purabi; Salas-Eljatib, Christian; Saner, Philippe; Schall, Peter; Schelhaas, Mart-Jan; Schepaschenko, Dmitry; Scherer-Lorenzen, Michael; Schmid, Bernhard; Schöngart, Jochen; Searle, Eric B.; Seben, Vladimír; Serra-Diaz, Josep M.; Sheil, Douglas; Shvidenko, Anatoly Z.; Silva-Espejo, Javier E.; Silveira, Marcos; Singh, James; Sist, Plinio; Slik, Ferry; Sonké, Bonaventure; Souza, Alexandre F.; Miścicki, Stanislaw; Stereńczak, Krzysztof J.; Svenning, Jens-Christian; Svoboda, Miroslav; Swanepoel, Ben; Tchebakova, Nadja; Ter Steege, Hans; Umunay, Peter M.; Van Der Plas, Fons; Van Do, Tran; Verbeeck, Hans; Viana, Helder; Vibrans, Alexander C.; Vieira, Simone; Westerlund, Bertil; Wiser, Susan K.; Zo-Bi, Irie C.; Zohner, Constantin M.;doi: 10.1038/s41477-023-01543-5 , 10.3929/ethz-b-000643725 , 10.5445/ir/1000163924 , 10.48350/187399
pmid: 37872262
pmc: PMC10654052
Understanding what controls global leaf type variation in trees is crucial for comprehending their role in terrestrial ecosystems, including carbon, water and nutrient dynamics. Yet our understanding of the factors influencing forest leaf types remains incomplete, leaving us uncertain about the global proportions of needle-leaved, broadleaved, evergreen and deciduous trees. To address these gaps, we conducted a global, ground-sourced assessment of forest leaf-type variation by integrating forest inventory data with comprehensive leaf form (broadleaf vs needle-leaf) and habit (evergreen vs deciduous) records. We found that global variation in leaf habit is primarily driven by isothermality and soil characteristics, while leaf form is predominantly driven by temperature. Given these relationships, we estimate that 38% of global tree individuals are needle-leaved evergreen, 29% are broadleaved evergreen, 27% are broadleaved deciduous and 5% are needle-leaved deciduous. The aboveground biomass distribution among these tree types is approximately 21% (126.4 Gt), 54% (335.7 Gt), 22% (136.2 Gt) and 3% (18.7 Gt), respectively. We further project that, depending on future emissions pathways, 17–34% of forested areas will experience climate conditions by the end of the century that currently support a different forest type, highlighting the intensification of climatic stress on existing forests. By quantifying the distribution of tree leaf types and their corresponding biomass, and identifying regions where climate change will exert greatest pressure on current leaf types, our results can help improve predictions of future terrestrial ecosystem functioning and carbon cycling. Nature Plants, 9 (11) ISSN:2055-026X ISSN:2055-0278
Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Fondazione Edmund MachArticle . 9999 . 2023Nature Plants; PURE Aarhus University; IRIS - Institutional Research Information System of the University of TrentoArticle . 2023 . Peer-reviewedLicense: CC BYGFZ German Research Centre for GeosciencesArticle . 2023License: CC BYData sources: GFZ German Research Centre for GeosciencesGhent University Academic BibliographyArticle . 2023Data sources: Ghent University Academic BibliographyCopenhagen University Research Information SystemArticle . 2023Data sources: Copenhagen University Research Information SystemBern Open Repository and Information System (BORIS)Article . 2023 . Peer-reviewedData sources: Bern Open Repository and Information System (BORIS)Flore (Florence Research Repository)Article . 2023Data sources: Flore (Florence Research Repository)Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.inrae.fr/hal-04288936/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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For further information contact us at helpdesk@openaire.euAccess RoutesGreen hybrid 0 citations 0 popularity Average influence Average impulse Average Powered by BIP!more_vert Archivio istituziona... arrow_drop_down Archivio istituzionale della ricerca - Fondazione Edmund MachArticle . 9999 . 2023Nature Plants; PURE Aarhus University; IRIS - Institutional Research Information System of the University of TrentoArticle . 2023 . Peer-reviewedLicense: CC BYGFZ German Research Centre for GeosciencesArticle . 2023License: CC BYData sources: GFZ German Research Centre for GeosciencesGhent University Academic BibliographyArticle . 2023Data sources: Ghent University Academic BibliographyCopenhagen University Research Information SystemArticle . 2023Data sources: Copenhagen University Research Information SystemBern Open Repository and Information System (BORIS)Article . 2023 . Peer-reviewedData sources: Bern Open Repository and Information System (BORIS)Flore (Florence Research Repository)Article . 2023Data sources: Flore (Florence Research Repository)Mémoires en Sciences de l'Information et de la Communication; HAL-IRDArticle . 2023License: CC BYFull-Text: https://hal.inrae.fr/hal-04288936/documentadd ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
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