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| Content Provider | Springer Nature Link |
|---|---|
| Author | Mamet, Bernard Préat, Alain Ridder, Chantal |
| Copyright Year | 1997 |
| Abstract | The deep-red lenses of the Pragian Slivenec Limestone have been extensively quarried for ornamental purposes since the XIIth century. Petrographic microscope observations indicate that the hematite stainings of the limestone follow ten different patterns. They range from massive non-directional filling of cavities to mineralized films and microstromatolites. Numerous ironrich endolithes are observed. Some could be derived from bacterial or lichen perforations and some related to ferric bacteria. Infiltration along welded calcite crystals, regular mineralized films and microstromatolites suggest a ferric bacterial origin for the pigment. This is confirmed by scanning microscope examinations of polished sections, that show hematite concentrations along micrometric filamentous sheaths. |
| Starting Page | 173 |
| Ending Page | 187 |
| Page Count | 15 |
| File Format | |
| ISSN | 01729179 |
| Journal | Facies |
| Volume Number | 36 |
| Issue Number | 1 |
| e-ISSN | 16124820 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 1997-01-01 |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Geobiochemistry Red Pigment Iron-Oxidizing Bacteria Endolithic Perforations Barrandian Basin (Czech Republic) Lower Devonian (Pragian) Biogeosciences Geochemistry Paleontology Sedimentology Ecology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geology Stratigraphy Paleontology |
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