Zobrazeno 1 - 10
of 47
pro vyhledávání: '"Iuliana Vasiliev"'
Autor:
Clemens Schmitt, Iuliana Vasiliev, Niels Meijer, Julia Brugger, Stefanie Kaboth-Bahr, André Bahr, Andreas Mulch
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-9 (2024)
Abstract Eocene hyperthermal events reflect profound perturbations of the global carbon cycle. Most of our knowledge about their onset, timing, and rates originates from marine records. Hence, the pacing and magnitude of hyperthermal continental warm
Externí odkaz:
https://doaj.org/article/d9a31bf18d7e4be19be73b625405a04a
Autor:
Evangelia Besiou, George Kontakiotis, Iuliana Vasiliev, Pierre Moissette, Jean-Jacques Cornée, Assimina Antonarakou
Publikováno v:
Journal of Marine Science and Engineering, Vol 11, Iss 6, p 1228 (2023)
The Tortonian–Messinian transition is associated with important climatic and oceanographic changes in the Mediterranean Basin, which have shaped both the biotic and abiotic nature of this setting. The morphological variability of the planktonic for
Externí odkaz:
https://doaj.org/article/c48e0970753f4cee96d736aa4d1726ef
Autor:
Dan Valentin Palcu, Irina Stanislavovna Patina, Ionuț Șandric, Sergei Lazarev, Iuliana Vasiliev, Marius Stoica, Wout Krijgsman
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-12 (2021)
Abstract The largest megalake in the geological record formed in Eurasia during the late Miocene, when the epicontinental Paratethys Sea became tectonically-trapped and disconnected from the global ocean. The megalake was characterized by several epi
Externí odkaz:
https://doaj.org/article/f0c32ac49098446fbad763a2cd2bce9c
Autor:
Iuliana Vasiliev, Marius Stoica, Arjen Grothe, Sergei Lazarev, Dan Valentin Palcu, Christiaan vanBaak, Arjan DeLeeuw, Francesca Sangiorgi, Gert‐Jan Reichart, Gareth R. Davies, Wout Krijgsman
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 7, Pp n/a-n/a (2021)
Abstract The Dacian Basin was uniquely situated to record late Miocene hydrological changes that influenced depositional environments and faunal dispersal patterns in Central Eurasia's mega‐lake Paratethys. Differences between the high strontium is
Externí odkaz:
https://doaj.org/article/21b10d39ca2e4f26b18b2baeb50437ee
Publikováno v:
Geologia Croatica, Vol 60, Iss 2, Pp 151-163 (2008)
The Sarmatian/Pannonian boundary in the Central Paratethys basin is marked by a major regressive event, which isolated the basin from the open sea and resulted in a palaeoenvironmental change from restricted marine to brackish water ecosystems. The e
Externí odkaz:
https://doaj.org/article/bf9eeac29df54f4e9173ff536f9bf3f9
Autor:
Antonarakou, Evangelia Besiou, George Kontakiotis, Iuliana Vasiliev, Pierre Moissette, Jean-Jacques Cornée, Assimina
Publikováno v:
Journal of Marine Science and Engineering; Volume 11; Issue 6; Pages: 1228
The Tortonian–Messinian transition is associated with important climatic and oceanographic changes in the Mediterranean Basin, which have shaped both the biotic and abiotic nature of this setting. The morphological variability of the planktonic for
Autor:
Konstantina Agiadi, Iuliana Vasiliev, Geanina Butiseaca, George Kontakiotis, Danae Thivaiou, Evangelia Besiou, Stergios Zarkogiannis, Efterpi Koskeridou, Assimina Antonarakou, Andreas Mulch
The restriction of the Mediterranean–Atlantic marine connection over the Messinian stage, which led to a salinity crisis and the deposition of the youngest salt giant on Earth, impacted the composition and structure of marine biota in unprecedented
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9110f3bbcd59fd4ea70feec3bc04553f
https://doi.org/10.5194/egusphere-egu23-1186
https://doi.org/10.5194/egusphere-egu23-1186
In the Mediterranean region, the end of the Miocene is marked by the Messinian Salinity Crisis (MSC; 5.97 - 5.33 Ma), a peculiar event that governed environmental modifications in the region, causing the deposition of large thicknesses of evaporitic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d745b16e536b664c6e7bd201afb5de26
https://doi.org/10.5194/egusphere-egu23-9065
https://doi.org/10.5194/egusphere-egu23-9065
Between 5.97-5.33 Ma, kilometre-thick evaporite units were deposited in the Mediterranean Basin during the so-called Messinian Salinity Crisis (MSC). The MSC was marked by a strongly negative hydrological budget, with a net evaporative loss of water
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e5616a4fe360af65e99a60f3f809626
https://doi.org/10.5194/egusphere-egu23-13297
https://doi.org/10.5194/egusphere-egu23-13297
Autor:
Anton Matoshko, Arjan de Leeuw, Marius Stoica, Oleg Mandic, Iuliana Vasiliev, Alina Floroiu, Wout Krijgsman
Publikováno v:
Geobios.
Well-documented, high-resolution sedimentary sections are critical to our understanding of the often eventful evolution of semi-isolated basins that form during the final stages of continent–continent convergence, as exemplified by the Mediterranea