Hi Maeght,
Not according to my understanding. Can you point to any non-localised examples.
How about Joggins Fossil Cliffs?
I said "Unless it can be shown that there is evidence of long breaks in sedimentation above and below the fossils." You said,
This would only be relevant if you can show they are not localised.
Joggins Fossil Cliffs are said to date back to 300 mya, preserving a 15 million year sequence.
Take a giant lycopod that cuts through dozens of layers. Allow 50 years for these layers to accumulate around the upright trunk, to a depth of say 5 meters. Take the total depth of the deposit at Joggins to be 1000 m (given a 3 km long cliff and a 20 degree angle of inclination of the strata). We have 5 m of sediment accumulating in 50 years. If this occurs continually it will take 1000/5 x 50 = 10,000 years for all 1000 m of sediments to accumulate.
If they were forming at the rate of 5 m per 50 years but had taken 15 million years to accumulate, there would have been periods of thousands of years where no sediment was laid down. During these periods we would expect to see erosion of the layers so that the boundaries would now appear irregular. Instead the boundaries are flat, indicating that little or no erosion occurred and therefore that the entire sequence was laid down over a relatively short time span, not 15 million years.