File:ChondritesMiddleSilurian.jpg
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Summary
| Description |
English: Chondrites Middle Silurian Co.Kerry Chondrites are small branching burrows of the same diameter, which superficially resemble the roots of a plant. The most likely candidate for having constructed these burrows is a nematode (roundworm). Chondrites are found in marine sediments from the Cambrian period of the Paleozoic onwards. They are especially common in sediments which were deposited in reduced-oxygen environments. |
| Date | |
| Source | Own work |
| Author | Notafly |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 03:58, 15 April 2013 | | 2,250 × 1,756 (1.07 MB) | The Cosmonaut | white background |
| 15:34, 28 October 2011 |  | 3,072 × 2,304 (2.67 MB) | Notafly |
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