webdoc.sub.gwdg.dewebdoc.sub.gwdg.de/.../2005/reitner/1991-rudisten.pdf · [First evidence of a rudist (Durania mortoni (MANTELL 1833)) from the Mid-Cretaceous of Helgoland] Abs tra
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GWDGwebdoc.sub.gwdg.de/pub/geo/geobiologie/2005/... · The calicles initially parallel to the substrate surface, and then curve up- wards, perpendicular to lt. This is presumably
MICROBIALITE FORMATION IN SEAWATER OF INCREASED …webdoc.sub.gwdg.de/.../2005/reitner/2003-satonda.pdf · 2004-04-08 · 106 G. ARP ET AL. FIG. 1.—A) Location of the Satonda island,
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AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS · In the central region of the corallum the calicles are contiguous, the walls being frequently in contact with each other; near the margin
webdoc.sub.gwdg.dewebdoc.sub.gwdg.de/.../reitner/1996-hydrochemistry.pdf · Research Topic: Microbialites and hydrochemistry Abstract The Satonda crater lake is up to now the only
![webdoc.sub.gwdg.dewebdoc.sub.gwdg.de/.../2005/reitner/1991-rudisten.pdf · [First evidence of a rudist (Durania mortoni (MANTELL 1833)) from the Mid-Cretaceous of Helgoland] Abs tra](https://static.documents.pub/doc/80x56/5b9d7b7509d3f275078c735c/-first-evidence-of-a-rudist-durania-mortoni-mantell-1833-from-the-mid-cretaceous.jpg)
