Last update: Feb 16th, 2016

Dr. Benjamin Sames

Benjamin Sames

 

Dipl.-Geol., Dr. rer. nat.

 

Micropalaeontology

Stratigraphy

Geology

 

 

Project Leader LCCNS (FWF)

Secretary IGCP 609

Associate-Editor AJES

University of Vienna

 

Department for Geodynamics and Sedimentology

Geozentrum, Althanstrasse 14

1090 Vienna

AUSTRIA

 

UZA II, Room 2A 276

Phone:  +43 (0) 1 4277 - 53479

E-Mail: benjamin.sames(at)univie.ac.at

Department Website: http://geologie.univie.ac.at/

This site: http://homepage.univie.ac.at/benjamin.sames/

Further Affiliations

 

§ Visiting Staff

Universität Wien, Institut für Paläontologie

Geozentrum, Althanstrasse 14

1090 Wien, AUSTRIA

http://www.univie.ac.at/Palaeontologie/INDEX1_EN.html

 

§ Affiliated Research Associate (Vert. Pal.)

Sam Noble Oklahoma Museum of Natural History (SNOMNH)

2401 Chautauqua Ave.

Norman, OK 73072-7029, USA

http://www.snomnh.ou.edu/collections-research/vertpaleo.htm

 

§ Stratigraphic Consultant

Petrobras (Petróleo Brasileiro S.A.)

http://www.petrobras.com/en/home.htm

News

Sames, B. et al., 2016. Review: Short-term sea-level changes in a greenhouse world — A view from the Cretaceous. Palaeogeography, Palaeoclimatology, Palaeoecology, 441 (3), 393–411. http://dx.doi.org/10.1016/j.palaeo.2015.10.045

Research Summary

My research focuses on micropalaeontology of late Mesozoic (Late Jurassic - Early Cretaceous) non-marine deposits. Central aspects of my research are the taxonomy, phylogeny, palaeobiology and biostratigraphical application of ostracods (microcrustaceans of around 1mm size with a calcified bivalved shell, the carapace), that today inhabit virtually all aquatic environments, both marine and non-marine). Ostracods' small size, morphological variability, ecology, fossilization potential and long geological history render them excellent candidates for a wide array of applications. In non-marine deposits, ostracods are among the most common fossils, at least since the Middle-Late Jurassic, and consequently one of the most useful groups.