Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Cunarro Otero, Daniel"'
Autor:
Micallef, Aaron, Camerlenghi, Angelo, García-Castellanos, Daniel, Cunarro Otero, Daniel, Gutscher, Marc-André, Barreca, G., Spatola, Daniele, Facchin, Lorenzo, Geletti, Riccardo, Krastel, Sebastian, Gross, Felix, Urlaub, M.
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
The Messinian salinity crisis (MSC) was an outstanding palaeo-oceanographic event that affected the Mediterranean region from 5.97 to 5.33 Ma. This event resulted in the deposition of kilometre-thick sequences of salt and is widely associated with th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::602a0f08f11722fa90412bb163d3b43c
http://hdl.handle.net/10261/186848
http://hdl.handle.net/10261/186848
Autor:
Riccardo Geletti, Aaron Micallef, Daniele Spatola, Daniel García-Castellanos, Daniel Cunarro Otero, Felix Gross, Angelo Camerlenghi, Sebastian Krastel, Giovanni Barreca, Morelia Urlaub, Marc-André Gutscher, Lorenzo Facchin
Publikováno v:
Scientific Reports
Scientific Reports, Vol 8, Iss 1, Pp 1-8 (2018)
Scientific Reports, Nature Publishing Group, 2018, 8 (1), ⟨10.1038/s41598-018-19446-3⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Scientific Reports, 8 (1078).
Scientific Reports (2045-2322) (Nature Publishing Group), 2018-01, Vol. 8, N. 1078, P. 8p.
Scientific Reports, Vol 8, Iss 1, Pp 1-8 (2018)
Scientific Reports, Nature Publishing Group, 2018, 8 (1), ⟨10.1038/s41598-018-19446-3⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Scientific Reports, 8 (1078).
Scientific Reports (2045-2322) (Nature Publishing Group), 2018-01, Vol. 8, N. 1078, P. 8p.
A. Micallef et. al.
The Messinian salinity crisis (MSC)-the most abrupt, global-scale environmental change since the end of the Cretaceous-is widely associated with partial desiccation of the Mediterranean Sea. A major open question is the way n
The Messinian salinity crisis (MSC)-the most abrupt, global-scale environmental change since the end of the Cretaceous-is widely associated with partial desiccation of the Mediterranean Sea. A major open question is the way n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dfdc400a890e10f5b17910b1fa17df77
http://hdl.handle.net/11573/1645512
http://hdl.handle.net/11573/1645512
Autor:
Micallef A; Marine Geology & Seafloor Surveying, Department of Geosciences, University of Malta, Msida, Malta. aaron.micallef@um.edu.mt., Camerlenghi A; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Trieste, Italy., Garcia-Castellanos D; Instituto de Ciencias de la Tierra Jaume Almera, CSIC, Barcelona, Spain., Cunarro Otero D; Marine Geology & Seafloor Surveying, Department of Geosciences, University of Malta, Msida, Malta., Gutscher MA; Laboratoire Géosciences Océan, University of Brest/CNRS, IUEM, Pl. N. Copernic, Plouzané, 29280, France., Barreca G; Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Università di Catania, Catania, Italy., Spatola D; Marine Geology & Seafloor Surveying, Department of Geosciences, University of Malta, Msida, Malta., Facchin L; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Trieste, Italy., Geletti R; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Trieste, Italy., Krastel S; Christian-Albrechts-Universität zu Kiel, Institut für Geowissenschaften, Kiel, Germany., Gross F; Christian-Albrechts-Universität zu Kiel, Institut für Geowissenschaften, Kiel, Germany., Urlaub M; GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany.
Publikováno v:
Scientific reports [Sci Rep] 2018 Jan 18; Vol. 8 (1), pp. 1078. Date of Electronic Publication: 2018 Jan 18.
