In the geologic timescale, the Ludfordian is the age of the Ludlow epoch of the Silurian period of the Paleozoic era of the Phanerozoic eon that occurred between 425.6 ± 0.9Ma and 423. ± 2.3 Ma (million years ago). The Ludfordian age succeeds the Gorstian age and precedes the Pridoli epoch. It is named for the town of Ludford in Shropshire, England.

Epochs in the Silurian
Epochs of the Silurian Period.
Axis scale: millions of years ago.

The Lau event is a rapid pulse of cooling during the Ludfordian, about 420 million years ago; it is identified by a pulse of extinctions and oceanic changes. It is one of the series of fast sea-level and excursions in oxygen isotope ratios that signal fast switches between warm and cold climate states, characteristic of the Silurian climatic instability. The Lau Event occurred during an extended period of elevated seawater saturation state, explained by reservoirs of the planet's fresh water being locked up in massive polar ice caps. The sudden reappearance in normally saline marine environments of stromatolites and a mass occurrence of oncoids during the event suggested that minor extinction events like the Lau Event also resulted in periods of reduced grazing pressures on surviving "disaster biota", which can be compared to the aftermath of the more catastrophic end-Ordovician and end-Permian mass extinctions.[3]



Arthropods of the Ludfordian
Taxa Presence Location Description Images
Trimpley, Worcestershire, UK


Plants of the Ludfordian
Taxa Presence Location Description Images
Cornwallis Island, Northern Canada[4]
Cornwallis Island, Northern Canada[4]


  1. Jeppsson, L.; Calner, M. (2007). "The Silurian Mulde Event and a scenario for secundo—secundo events". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 93 (02): 135–154. doi:10.1017/S0263593300000377.
  2. Munnecke, A.; Samtleben, C.; Bickert, T. (2003). "The Ireviken Event in the lower Silurian of Gotland, Sweden-relation to similar Palaeozoic and Proterozoic events". Palaeogeography, Palaeoclimatology, Palaeoecology. 195 (1): 99–124. doi:10.1016/S0031-0182(03)00304-3.
  3. M. Calner, "A Late Silurian extinction event and anachronistic period" Geology 33, pp. 305–308; Geology On-line Forum: response to a reply.
  4. Steven T. LoDuca, Michael J. Melchin & Heroen Verbruggen (2011). "Complex noncalcified macroalgae from the Silurian of Cornwallis Island, Arctic Canada" (PDF). Journal of Paleontology. 85 (1): 111–121. doi:10.1666/10-025.1. Archived from the original (PDF proofs) on 2011-07-22.

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.