Publication: Tying the C-isotope excursions of the Neoproterozoic successions of Tandilia System: Phantom glaciations?
dc.contributor | Lizzoli, Sabrina | |
dc.contributor | Isla, Manuel Fermín | |
dc.contributor | López, Manuel | |
dc.contributor | Moyano Paz, Damián | |
dc.contributor | Raigemborn, María Sol | |
dc.creator | Gómez Peral, Lucia | |
dc.creator | Arrouy, Maria Julia | |
dc.creator | Penzo, Victoria | |
dc.creator | Ferreyra, Camila | |
dc.creator | Poire, Daniel Gustavo | |
dc.creator | Sial, Alcides N. | |
dc.date.issued | 2023 | |
dc.description.abstract | The Neoproterozoic era (1000–539 Ma) encompasses drastic global changes, including extreme climatic events and transformative evolutionary transitions. Snowball Earth hypothesis (cf. Snowball vs Slushball Earth hypotheses) suggests that during Cryogenian the Earth was “completely” ice-covered Sturtian (~720-710 Ma) and Marinoan (635 Ma) events. In Ediacaran times, Gaskiers (582 Ma) followed by Shuram (~570 Ma) events were related to δ13C excursions recorded globally and commonly associated with prominent sedimentological, geobiological and geochemical changes. | |
dc.identifier | Tying the C-isotope excursions of the Neoproterozoic successions of Tandilia System: Phantom glaciations?; XVIII Reunión Argentina de Sedimentología; IX Congreso Latinoamericano de Sedimentología; La Plata; Argentina; 2023; 157-157 | |
dc.identifier | 978-631-90299-0-1 | |
dc.identifier | http://hdl.handle.net/11336/228478 | |
dc.identifier | CONICET Digital | |
dc.identifier | CONICET | |
dc.identifier.uri | https://naturalis.fcnym.unlp.edu.ar/handle/628872547/57030 | |
dc.language | eng | |
dc.publisher | Asociación Argentina de Sedimentología | |
dc.relation | info:eu-repo/semantics/altIdentifier/url/https://www.ras2023laplata.com/_files/ugd/0306a6_082d4a01e5e04c90864152b3296837f4.pdf | |
dc.source | Actas XVIII Reunión Argentina de Sedimentología; IX Congreso Latinoamericano de Sedimentología | |
dc.subject | Río de La Palta Craton | |
dc.subject | Phamton glaciations | |
dc.subject | Neoproterozoic | |
dc.title | Tying the C-isotope excursions of the Neoproterozoic successions of Tandilia System: Phantom glaciations? | |
dc.type | info:eu-repo/semantics/publishedVersion | |
dc.type | info:eu-repo/semantics/conferenceObject | |
dc.type | info:ar-repo/semantics/documento de conferencia | |
dspace.entity.type | Publication |