Sepkoski J J
Department of the Geophysical Sciences, University of Chicago, Illinois 60637, USA.
Acta Palaeontol Pol. 1994;38(3-4):175-98.
The question of how random, or unconstrained, paleobiologic models should be is examined with a case study: Signor's (1982, 1985) inverse calculation of levels of marine species diversity through the Phanerozoic. His calculation involved an ingenious model that estimated species numbers and species abundances in the world oceans of the past by correcting known numbers of fossil species for variations in sedimentary rocks available for sampling and in effort paleontologists might devote to sampling. The model proves robust to changes in possible shapes of species-abundance distributions, but it is sensitive to alterations in the assumption that paleontologists collect fossils at random. If it is assumed that ease of collecting varies with age of sediment (with the Cenozoic offering easy sampling) or that paleontologists tend to seek out rarer fossils, results of the inverse calculation change. In particular, the magnitude of the calculated Cenozoic diversity increase always declines from the factor of about seven as originally reported to something considerably smaller. This leaves open the problem of the magnitude of Cenozoic increase in marine species diversity, awaiting better empirical data and, perhaps, more exacting models, random or otherwise.
西尼奥尔(1982年、1985年)对显生宙期间海洋物种多样性水平的反向计算。他的计算涉及一个巧妙的模型,该模型通过校正已知化石物种数量,以考虑可用于采样的沉积岩变化以及古生物学家可能投入到采样中的工作量,从而估算过去世界海洋中的物种数量和物种丰度。该模型被证明对于物种丰度分布可能形状的变化具有稳健性,但对于古生物学家随机采集化石这一假设的改变很敏感。如果假设采集的难易程度随沉积物年龄而变化(新生代提供了容易采样的条件),或者古生物学家倾向于寻找更稀有的化石,那么反向计算的结果就会改变。特别是,计算出的新生代多样性增加幅度总是从最初报告的约7倍下降到小得多的数值。这使得新生代海洋物种多样性增加幅度的问题悬而未决,有待更好的实证数据以及或许更精确的模型(无论是否随机)来解决。