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What kind of calcite? Disclosing the origin of sparry calcite temper in ancient ceramics

Autor: Maritan L.[1], Ganzarolli G.[2, Antonelli F.[4], Rigo M.[1, 2, 3, 4, Kapatza A.[6], Bajnok K.[7], Coletti C.[1], Mazzoli C.[1], Lazzarini L.[4], Vedovetto P.[3], Chavarría Arnau A.[3]

Publikováno v: Journal of Archaeological Science
Journal of Archaeological Science, 2021, 129, pp.105358. ⟨10.1016/j.jas.2021.105358⟩
Journal of Archaeological Science, Elsevier, 2021, 129, pp.105358. ⟨10.1016/j.jas.2021.105358⟩
Journal of archaeological science 129 (2021): 1–13. doi:10.1016/j.jas.2021.105358
info:cnr-pdr/source/autori:Maritan L.[1], Ganzarolli G.[2,3], Antonelli F.[4], Rigo M.[1,2,3,4,5], Kapatza A.[6], Bajnok K.[7], Coletti C.[1], Mazzoli C.[1], Lazzarini L.[4], Vedovetto P.[3], Chavarría Arnau A.[3]/titolo:What kind of calcite? Disclosing the origin of sparry calcite temper in ancient ceramics/doi:10.1016%2Fj.jas.2021.105358/rivista:Journal of archaeological science/anno:2021/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:129

The addition of temper in the pottery manufacturing process is attested since Prehistoric Times and is still a production choice adopted in the ceramic industry. When the temper is composed of minerals and rocks which outcrop in regions distant from

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::29902a3c3dcc8f8612043333cc9f1c01
https://hal.science/hal-03601284

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Sedimentary record of Upper Triassic impact in the Lagonegro Basin, southern Italy: Insights from highly siderophile elements and Re-Os isotope stratigraphy across the Norian/Rhaetian boundary

Autor: Sato H.[1], Ishikawa A.[2, Onoue T.[4], Tomimatsu Y.[4], Rigo M.[1

Publikováno v: Chemical geology 586 (2021): 1–20. doi:10.1016/j.chemgeo.2021.120506
info:cnr-pdr/source/autori:Sato H.[1], Ishikawa A.[2,3], Onoue T.[4], Tomimatsu Y.[4], Rigo M.[1,5]/titolo:Sedimentary record of Upper Triassic impact in the Lagonegro Basin, southern Italy: Insights from highly siderophile elements and Re-Os isotope stratigraphy across the Norian%2FRhaetian boundary/doi:10.1016%2Fj.chemgeo.2021.120506/rivista:Chemical geology/anno:2021/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:586

The Norian and Rhaetian transition (Late Triassic) is characterized by a faunal turnover in major pelagic groups, such as radiolarians, conodonts, and ammonoids. Although catastrophic events such as emplacements of large igneous provinces and/or extr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fbcba7acea68232abc83bda3a764bba7

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LANDSLIDES OF THE WESTERN DOLOMITES: CASE STUDIES FROM THE ADIGE AND SARCA VALLEYS(NE ITALY)

Autor: Martin S.[1], Ivy-Ochs S.[2, Viganò A.[4], Campedel P.[4], Rigo M.[1, Vockenhuber C.[3], Gabrieli F.[6], Mair V.[7], Rossato S.[5]

Publikováno v: Alpine and Mediterranean Quaternary
33 (2020): 191–207. doi:10.26382/AMQ.2020.15
info:cnr-pdr/source/autori:Martin S.[1], Ivy-Ochs S.[2,3], Viganò A.[4], Campedel P.[4], Rigo M.[1,5], Vockenhuber C.[3], Gabrieli F.[6], Mair V.[7], Rossato S.[5]/titolo:LANDSLIDES OF THE WESTERN DOLOMITES: CASE STUDIES FROM THE ADIGE AND SARCA VALLEYS(NE ITALY)./doi:10.26382%2FAMQ.2020.15/rivista:Alpine and Mediterranean Quaternary (Print)/anno:2020/pagina_da:191/pagina_a:207/intervallo_pagine:191–207/volume:33

The Lavini di Marco, Marocche di Dro and Molveno rock avalanches in Trentino, and the Termeno landslide in South Tyrol are here presented as case studies for the western Dolomites(Adige and Sarca Valleys, NE Italy). Their structural predisposition, r

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::65f2494981af1037965f1d218752043e

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Integrated conodont and radiolarian biostratigraphy of the upper Norian in Baoshan Block, Southwestern China

Autor: Du Y.[1, Bertinelli A.[3], Jin X.[2, Shi Z.[2], Karadi V.[5], Yin H.[2], Han L.[2], Wu Q.[2], Rigo M.[1

Publikováno v: Lethaia (Oslo, Trykt utg.) 53 (2020): 533–545. doi:10.1111/let.12374
info:cnr-pdr/source/autori:Du Y.[1,2], Bertinelli A.[3], Jin X.[2,4], Shi Z.[2], Karadi V.[5], Yin H.[2], Han L.[2], Wu Q.[2], Rigo M.[1,6]/titolo:Integrated conodont and radiolarian biostratigraphy of the upper Norian in Baoshan Block, Southwestern China/doi:10.1111%2Flet.12374/rivista:Lethaia (Oslo, Trykt utg.)/anno:2020/pagina_da:533/pagina_a:545/intervallo_pagine:533–545/volume:53

Two significant stratigraphical microfossils, conodonts and radiolarians, are usually used for the Upper Triassic chronostratigraphy. The Baoshan Block was located in eastern Tethys during the Late Triassic where the biostratigraphical data of Upper

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0aac0a9ce2a9e15700ee613a9fe2c372
http://hdl.handle.net/11577/3338909

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Learning from the past to face the future: landslides in the Riave Valley (Eastern Alps, Italy)

Autor: Rossato S.[1], Ghirotti M.[2], Gabrieli F.[3], Livio F.[4], Bovo F.[3], Brezzi L.[3], Campedel P.[5], Cola S.[3], Ivy-Ochs S.[7], Martin S.[6], Mozzi P.[6], Pasuto A.[8], Rigo M.[1, Simonini P.[3], Surian N.[6], Viganò A.[5], Vockenhuber C.[7], Wolter A.[9]

Publikováno v: Alpine and Mediterranean Quaternary 33 (2020): 209–228. doi:10.26382/AMQ.2020.14
info:cnr-pdr/source/autori:Rossato S.[1], Ghirotti M.[2], Gabrieli F.[3], Livio F.[4], Bovo F.[3], Brezzi L.[3], Campedel P.[5], Cola S.[3], Ivy-Ochs S.[7], Martin S.[6], Mozzi P.[6], Pasuto A.[8], Rigo M.[1,6], Simonini P.[3], Surian N.[6], Viganò A.[5], Vockenhuber C.[7], Wolter A.[9]/titolo:Learning from the past to face the future: landslides in the Riave Valley (Eastern Alps, Italy)./doi:10.26382%2FAMQ.2020.14/rivista:Alpine and Mediterranean Quaternary/anno:2020/pagina_da:209/pagina_a:228/intervallo_pagine:209–228/volume:33

Landslides are a critical process in landscape evolution and may pose a serious threat to people and infrastructure. In the last decades, a growing interest in such phenomena has developed in the Alps, where narrow valleys are increasingly inhabited,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::bf54559cfa1c4c2cf11c0cc38b597f71
https://publications.cnr.it/doc/443037

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The asynchronous disappearance of conodonts: New constraints from Triassic-Jurassic boundary sections in the Tethys and Panthalassa

Autor: Du Y.[1], Chiari M.[2], Karádi V.[3], Nicora A.[4], Onoue T.[5], Pálfy J.[6, 7, Roghi G.[9], Tomimatsu Y.[10], Rigo M.[1

Publikováno v: Earth-science reviews 203 (2020): 1–18. doi:10.1016/j.earscirev.2020.103176
info:cnr-pdr/source/autori:Du Y.[1], Chiari M.[2], Karádi V.[3], Nicora A.[4], Onoue T.[5], Pálfy J.[6,7,8], Roghi G.[9], Tomimatsu Y.[10], Rigo M.[1,9]/titolo:The asynchronous disappearance of conodonts: New constraints from Triassic-Jurassic boundary sections in the Tethys and Panthalassa/doi:10.1016%2Fj.earscirev.2020.103176/rivista:Earth-science reviews/anno:2020/pagina_da:1/pagina_a:18/intervallo_pagine:1–18/volume:203

The End-Triassic Extinction event (ETE) has been recognized in numerous sections worldwide and it is usually marked by three negative carbon isotope excursions (NCIEs), named “precursor” (P-NCIE), “initial” (I-NCIE) and “main” (M-NCIE) ne

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c12901a70bddec6a1de932ae6a59c35f
https://doi.org/10.1016/j.earscirev.2020.103176

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A new Rhaetian ?13Corg record: Carbon cycle disturbances, volcanism, End-Triassic mass Extinction (ETE)

Autor: Zaffani M.[1], Jadoul F.[2], Rigo M.[1

Publikováno v: Earth-science reviews 178 (2018): 91–104.
info:cnr-pdr/source/autori:Zaffani M.[1], Jadoul F.[2], Rigo M.[1,3]/titolo:A new Rhaetian ?13Corg record: Carbon cycle disturbances, volcanism, End-Triassic mass Extinction (ETE)/doi:/rivista:Earth-science reviews/anno:2018/pagina_da:91/pagina_a:104/intervallo_pagine:91–104/volume:178

The links between large-scale volcanism, carbon cycle perturbations and the biotic crises at the End-Triassic Extinction event (ETE) are not well understood. The ETE seems to be marked by three carbon isotope excursions (CIEs) likely triggered by dif

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::4bef66408de491bb25748bfcd927434c
http://www.cnr.it/prodotto/i/386519

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New stratigraphic, paleontologic and geochemical data around the Triassic-Jurassic boundary at Portovenere (Northern Apennines, Italy)

Autor: Rigo M.[1, McRoberts C.[3], Ciarapica G.[4], Giordano N.[4], Bachan A.[5]

Publikováno v: Bulletin-New Mexico Museum of Natural History and Science 61 (2013): 489–499.
info:cnr-pdr/source/autori:Rigo M.[1,2], McRoberts C.[3], Ciarapica G.[4], Giordano N.[4], Bachan A.[5]/titolo:New stratigraphic, paleontologic and geochemical data around the Triassic-Jurassic boundary at Portovenere (Northern Apennines, Italy)./doi:/rivista:Bulletin-New Mexico Museum of Natural History and Science/anno:2013/pagina_da:489/pagina_a:499/intervallo_pagine:489–499/volume:61

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::a9e84f6120a8907930d7045467d22035
https://publications.cnr.it/doc/286626

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