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Summary
| Description |
English: Cropped from File:Kowala Quarry Poland.png to show the Hangenberg succession in a closer view. Fig. 2: d field images (photo B.A. Matyja) of the complete pelagic DCB succession (north-eastern level of the Kowala Quarry; compare Fig. 2b); lithological units after Malec (1995, 2014): A—nodular cephalopod limestone, B—shale (including the Hangenberg Black Shale horizon in the lower part of the unit), C—marly limestone, D—marl with nodular limestone intercalations; abbreviations: KBS—Kowala Black Shale, HBS—Hangenberg Black Shale |
| Date | |
| Source | The Devonian/Carboniferous boundary interval in Poland: multidisciplinary studies in pelagic (Holy Cross Mountains and Sudetes) and ramp (Western Pomerania) successions. Palaeobio Palaeoenv 101, 421–472 (2021). https://doi.org/10.1007/s12549-020-00442-3 |
| Author | Matyja, H., Woroncowa-Marcinowska, T., Filipiak, P. et al. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 04:06, 13 August 2022 | | 2,055 × 800 (546 KB) | NGPezz | Uploaded a work by Matyja, H., Woroncowa-Marcinowska, T., Filipiak, P. et al. from The Devonian/Carboniferous boundary interval in Poland: multidisciplinary studies in pelagic (Holy Cross Mountains and Sudetes) and ramp (Western Pomerania) successions. Palaeobio Palaeoenv 101, 421–472 (2021). https://doi.org/10.1007/s12549-020-00442-3 with UploadWizard |
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