Abstract
The environment of deposition of the plant-bearing horizons of the Devonian-Carboniferous Kiltorcan Formation in Co. Kilkenny is poorly known. Previous studies suggested a possible lacustrine palaeoenvironment with plant material being swept in and fluvial conditions. Reinvestigation of the plant-rich localities on Kiltorcan Hill using both sedimentological facies and palynofacies suggests that there were high-sinuosity streams carrying fine-grained sediments with the plant fossils preserved on point bars, and marginal back-swamp conditions with plant material deposited close to the growth site.
| Original language | English |
|---|---|
| Pages (from-to) | 333-341 |
| Number of pages | 9 |
| Journal | Geological Society Special Publication |
| Volume | 180 |
| DOIs | |
| Publication status | Published - 2000 |
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