Larger foraminifera as a substratum for encrusting bryozoans (Late Oligocene, Tethyan Seaway, Iran)-Reference-Cited by-同舟云学术

Larger foraminifera as a substratum for encrusting bryozoans (Late Oligocene, Tethyan Seaway, Iran)

Published:2008-11-27 Issue:2 Volume:55 Page:227-241
ISSN:0172-9179
Container-title:Facies
language:en
Short-container-title:Facies

Author:

Berning B.,Reuter M.,Piller W. E.,Harzhauser M.,Kroh A.

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Stratigraphy,Geology

Link

http://link.springer.com/content/pdf/10.1007/s10347-008-0169-x.pdf

Reference62 articles.

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3. Beavington-Penney SJ, Racey A (2004) Ecology of extant nummulitids and other larger benthic foraminifera: applications in palaeoenvironmental analysis. Earth Sci Rev 67:219–265. doi: 10.1016/j.earscirev.2004.02.005

4. Beavington-Penney SJ, Wright VP, Racey A (2005) Sediment production and dispersal on foraminifera-dominated early Tertiary ramps: the Eocene El Garia Formation, Tunisia. Sedimentology 52:527–569. doi: 10.1111/j.1365-3091.2005.00709.x

5. Berning B (2006) The cheilostome bryozoan fauna from the late Miocene of Niebla (Guadalquivir Basin, SW Spain): environmental and biogeographic implications. Mitt Geol-Paläontol Inst Univ Hamburg 90:7–156

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