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Applying Strauss and Sadler (1989) and Marshall (1994) type confidence intervals to core, or other "discretely" collected stratigraphic data. In my 1994 paper (following Springer and Lilje, 1988) I state that confidence intervals can be safely applied in any situation (including core data) where the mean gap size and standard deviation in gap size are essentially equal. Obviously if a section were sampled every 20 cm, and if a taxon were found in every sample, the standard deviation in the gap size would be zero, and the Strauss and Sadler and/or Marshall (1994) approach should not be applied. This test is crude, but it will at least give you an idea of where you stand. There is a simpler rule of thumb for when to apply these confidence intervals: let us suppose you have sampled your stratigraphic range at some regular interval. The question you have to ask yourself is: if you were to re-sample at a smaller interval (say, at half the original interval) would the number of fossil horizons recorded go up appreciably. If the answer is NO, then go ahead and apply the Strauss and Sadler or Marshall confidence intervals. If the answer is YES, then you should NOT apply the confidence intervals, or if you do, you should recognize that they will be much too big (which may be fine if you have set up you null hypothesis in such a way that you do not increase the chance of rejecting it if the confidence intervals are too big). Norm may be quite right that many stratigraphic ranges based on core data may meet this test. Note though, that for a taxon with a "gappy" record, if the number of fossil horizons goes up with a finer sampling interval, then the confidence intervals should not be applied, despite the fact that the range is "gappy". You should not use as you rule-of-thumb that any range with gaps in it is analyzable with the Strauss and Sadler or Marshall approaches (Caveat: it may be that you can, but this must be demonstrated - I am currently working a method that does this). With regards the difficulties in converting rock thicknesses to time, this is an important problem. However, the Marshall (1994) approach does NOT make the assumption that sedimentation rates are constant or uniform (unlike Strauss and Sadler), as long as one is willing to have one's confidence intervals expressed in terms of rock thickness and not time (which is better than nothing, but not ideal ...). BUT the Marshall approach (along with Strauss and Sadler) does make the assumption that there is no secular trend in sedimentation rate etc. on the scale length of the entire observed stratigraphic range. Charles Marshall Earth and Space Sciences UCLA
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