Black Sea desiccation during the Messinian Salinity Crisis: Fact or fiction?-Reference-Cited by-同舟云学术

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Black Sea desiccation during the Messinian Salinity Crisis: Fact or fiction?

Published:2014-07 Issue:7 Volume:42 Page:563-566
ISSN:1943-2682
Container-title:Geology
language:en
Short-container-title:

Author:

Grothe Arjen,Sangiorgi Francesca,Mulders Yannick R.,Vasiliev Iuliana,Reichart Gert-Jan,Brinkhuis Henk,Stoica Marius,Krijgsman Wout

Publisher

Geological Society of America

Subject

Geology

Link

http://pubs.geoscienceworld.org/geology/article-pdf/42/7/563/3544723/563.pdf

Reference26 articles.

1. Modelling depositional shifts between sedimentary basins: Sediment pathways in Paratethys basins during the Messinian Salinity Crisis;Bartol;Tectonophysics,2012

2. The Northern Apennines palynological record as a contribute for the reconstruction of the Messinian palaeoenvironments;Bertini;Sedimentary Geology,2006

3. Late Eocene–Quaternary dinoflagellate cysts from ODP Site 1168, off western Tasmania;Brinkhuis,2003

4. Refinements of calcareous nannofossil biostratigraphy at the Miocene/Pliocene boundary in the Mediterranean region;Di Stefano;Geobios,2010

5. Quaternary mass wasting on the western Black Sea margin, offshore of Amasra;Dondurur;Global and Planetary Change,2013

Cited by 42 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Neogene Regional Scale of the Eastern Paratethys, Stratigraphy and Paleontological Basis;Paleontological Journal;2022-12

2. Mediterranean–Black Sea gateway exchange: scientific drilling workshop on the BlackGate project;Scientific Drilling;2022-10-28

3. A review of the Odontura (Orthoptera, Phaneropterinae) from Italy, Malta, Algeria and Tunisia;Zootaxa;2022-07-26

4. The geochemical riddle of “low-salinity gypsum” deposits;Geochimica et Cosmochimica Acta;2022-06

5. Freshening of the Mediterranean Salt Giant: controversies and certainties around the terminal (Upper Gypsum and Lago-Mare) phases of the Messinian Salinity Crisis;Earth-Science Reviews;2021-05

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