Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Mathia Sabino"'
Autor:
Vitale, Giulia, Massimiliano, Vardé, Federico, Giglio, Giansiracusa, Sara, Stefano, Miserocchi, Mathia, Sabino, Rosso, Beatrice, Ingegorg, Hallanger, Corami, Fabiana
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3655::38acd562104eb19407445241ef62a0c8
https://hdl.handle.net/10278/5029480
https://hdl.handle.net/10278/5029480
Autor:
Mathia Sabino
Geological setting, methodology, and lipid abundance, carbon stable isotopes, and sources (Tables S1–S4; Figures S1–S3).
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::269c6b3a099cdc041ec5d764776ae772
https://doi.org/10.1130/geol.s.15832095
https://doi.org/10.1130/geol.s.15832095
Autor:
Mathia Sabino, Luca Pellegrino, Jörn Peckmann, Bernhard Schnetger, Hans J. Brumsack, Marcello Natalicchio, Daniel Birgel, Giorgio Carnevale, Francesco Dela Pierre, Francesca Lozar, Rocco Gennari, Susanne Gier
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 518:45-61
In marginal Mediterranean sub-basins, the early phase of the Messinian salinity crisis (MSC) is recorded by cyclic successions of gypsum and shales, which in deeper parts of the sub-basins make lateral transition into organic-rich shales, marls, and
In the late Miocene, the Mediterranean Basin became a restricted basin because of its progressive tectonic isolation from the Global Ocean. The almost complete halt of the Atlantic-Mediterranean water exchange about 6 Ma ago triggered the deposition
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c77136c5515050e29c0b9412fac4ec9
https://doi.org/10.5194/egusphere-egu21-1475
https://doi.org/10.5194/egusphere-egu21-1475
Since the discovery of the late Miocene (Messinian) Mediterranean Salt Giant more than 50 years ago, the environmental conditions that caused its formation have been debated. Such reconstruction suffers from the absence of modern analogues, the lack
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a5b59f2784b772e9f6cd2fa706275ea
https://doi.org/10.5194/egusphere-egu2020-3852
https://doi.org/10.5194/egusphere-egu2020-3852
Autor:
Susanne Gier, Francesco Dela Pierre, Jörn Peckmann, Mathia Sabino, Marcello Natalicchio, Daniel Birgel
During Messinian time, the Mediterranean underwent hydrological modifications culminating 5.97 Ma ago with the Messinian salinity crisis (MSC). Evaporite deposition and alleged annihilation of most marine eukaryotes were taken as evidence of the esta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::47693e5ed92efb5ddaec1aa0d3063853
http://hdl.handle.net/2318/1755258
http://hdl.handle.net/2318/1755258
Autor:
Bernhard Schnetger, Francesco Dela Pierre, Jörn Peckmann, David Bortels, Enno Schefuß, Mathia Sabino, Marcello Natalicchio, Daniel Birgel
The youngest and one of the largest saline deposits of Earth history formed in the Mediterranean during the Messinian salinity crisis (MSC; 5.97–5.33 Ma, Late Miocene), when global climate was experiencing a trend of cooling and aridification. Howe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::caad6a8983dca5c749d19123c1168744
http://hdl.handle.net/2318/1741342
http://hdl.handle.net/2318/1741342