Paleoceanography and climate of the Badenian (Middle Miocene, 16.4–13.0 Ma) in the Central Paratethys based on foraminifera and stable isotope (δ18O and δ13C) evidence-Reference-Cited by-同舟云学术

Paleoceanography and climate of the Badenian (Middle Miocene, 16.4–13.0 Ma) in the Central Paratethys based on foraminifera and stable isotope (δ18O and δ13C) evidence

Published:2005-10-05 Issue:1 Volume:95 Page:119-142
ISSN:1437-3254
Container-title:International Journal of Earth Sciences
language:en
Short-container-title:Int J Earth Sci (Geol Rundsch)

Author:

Báldi Katalin

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s00531-005-0019-9.pdf

Reference92 articles.

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3. Báldi T (1986) Mid-tertiary stratigraphy and paleogeographic evolution of Hungary. Akadémiai Kiadó Budapest, pp 1–201

4. Báldi K (1997) Assumed circulation pattern of the Central Paratethys through Badenian (Middle Miocene) times: quantitative paleoeceological analysis of foraminifera from borehole Tengelic-2 (SW Hungary). Acta Geol Hung 40(1):57–71

5. Báldi K (1999) Taxonomic notes on benthic foraminifera from SW-Hungary Middle Miocene (Badenian) Paratethys. Acta Geol Hung 42(2):193–236

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