Cohort analysis provides an effective method of analysing taxonomic survivorship in the fossil record where large data sets are available. An analysis of the stratigraphic ranges of about 8,500 fossil genera and subgenera shows that survivorship patterns are substantially the same throughout the Phanerozoic. These patterns are used to calculate an average value for mean species duration among fossil invertebrates (11.1 Myr.). Also, the extra extinctions near the Permo-Triassic boundary are shown to be equivalent to about 85 Myr of normal, background extinction.

Both intensive analysis of Gryphaea and an extensive survey of Jurassic bivalves in Europe supports the punctuated equilibria model of speciation, with the exception of phyletic size increase, which appears within the limits of the data to be gradualistic and affects at least a significant minority of species. The size increase takes place both within species and between successive species in a lineage. In Liassic Gryphaea, a combination of allometry in the ontogenetic development of the ancestral species and paedomorphosis led also to changes of shape up the sequence. The production of evolutionary trends by species selection is not supported.

The favoured interpretation of phyletic size increase is a gradual delay in maturation time consequent upon a change in the organisms' adaptive strategy from the r-selected to the K-selected mode and is backed up by evidence on changing population numbers and distribution. An extinction/speciation model is proposed for neritic organisms based on fluctuating sea levels. Times of low sea level or regression correspond with times of high stress and hence high extinction among stenotopic organisms and increased rates of allopatric speciation, with r-selection as the dominant mode. Times of high sea level or transgression correspond with low extinction and speciation rates and increased freedom of migration. K-selection is the dominant mode and often leads to phyletic size increase provided the environment remains stable for a sufficiently long period.

Taxonomists working with late Cenozoic faunas tend to view living species as starting points for the evaluation of chronospecies (i.e., segments of evolutionary lineages subjectively designated as species) that extend backward in time from the Recent. This practice makes it possible to construct a survivorship curve for late Cenozoic chronospecies by evaluating all fossil lineages believed to have survived to the present day. A survivorship curve is produced by plotting the fraction of these lineages existing at any time that have not undergone enough phyletic evolution that their extant representatives are assigned to new species. This kind of surviviorship curve has been plotted for chronospecies of mammals using the beginning of the Würm, rather than the Recent, as an endpoint in order to avoid the effects of the Würm and post-Würm mass extinction. The survivorship curve reveals that all but a small fraction of established chronospecies have long durations relative to intervals of time during which distinctive higher taxa have arisen. Phyletic turnover of species has been remarkably slow. Most net evolutionary change must have been associated with saltational speciation. Even the large majority of genera must have arisen rapidly by one or more divergent speciation events. Estimates of rates of extinction suggest that the bottleneck effect, in which constriction of a lineage is followed by re-expansion as a distinct species, cannot be a major source of evolutionary change. These conclusions, based on the evaluation of mammalian phylogeny, seem also to apply to other taxa of animals, supporting the punctuational model of evolution. The long durations of hominid species imply that the evolution of humans, like that of other mammals, conforms to this model.

The pattern observed in nature has often served as a compelling motivation for seeking the underlying processes which are assumed to control the pattern. Spatial and temporal patterns of species diversity are the most commonly observed and described from the study of recent and paleocommunities. These patterns include those found within a local or discrete region such as succession and changes along an environmental gradient and interregional or global patterns such as latitudinal diversity gradients and comparisons of the deep-sea and the continental shelf faunas. Many hypotheses have been advanced to explain these patterns in terms of differences in the biology of species adapted to different or changing environments. However, a more simple explanation is possible: that these patterns do not result from any specific biologic processes.

We examine this possibility and show that succession can result from probabilistic immigration and local extinction of species, diversity gradients can result from probabilistic disturbance in naturally patchy environments, and that latitudinal gradients can be simply a function of the shape of the earth. As long as such diversity patterns can be explained independent of any specific biologic processes, they offer no test of the importance of these processes, either ecologically or evolutionarily.

Much new empirical evidence on the levels of Phanerozoic paleoprovinciality and of species diversity within paleocommunities now permits a reevaluation of marine diversity patterns. Data on paleoprovincial patterns are assembled from the literature and evaluated by means of a stochastic computer simulation model. The simulation is based on the statistics of modern patterns of diversity and endemism extrapolated conservatively to the paleoprovincial patterns and on estimates of species duration from the fossil record. The species diversities associated with the paleoprovincial patterns are then corrected for temporal changes in species packing in communities as determined by Bambach (1977) from studies of paleocommunities. The model thus has an empirical basis throughout. Furthermore it is free of biases that can arise due to the differential preservation of taxa in space and time.

The Paleozoic and Mesozoic were characterized by low provinciality and low average species diversity, on the order of 38,000 to 40,000 species, although there were significant fluctuations in standing diversities. In the Cenozoic, provinciality rose markedly, primarily through the appearance of latitudinal provincial chains, and average species diversity rose to about 240,000. Today it stands over 350,000; this is an order of magnitude greater than the Paleozoic average.

Size distributions, based on molar length, are presented for various groups of living and fossil primates. I examine (1) the extent to which particular taxonomic groups with distinctive morphological and behavioral attributes are characterized by distinctive size ranges or distributions and (2) the way in which size ranges and distributions are affected by the presence or absence of other primates within the same geographical area and time. Distinctive behavioral and ecological “adaptive zones” are characterized by distinctive size ranges and behavioral and morphological parallelism or convergence among living and fossil primate taxa usually results in similar size distributions.

Shotwell's method of paleoecological reconstruction attempts to define community membership of mammals represented within paleontological assemblages. Analysis of the measure of community membership upon which the method is based (relative skeletal completeness) shows this measure to be a function of sample size. A method for controlling for the effects of sample size upon measures of relative skeletal completeness is needed. A method is suggested which employs ratios of numbers of individuals to numbers of specimens, and a specific correction of Shotwell's method is proposed.

Three genera of the echinoderm class Edrioasteroidea comprise the suborder Cyathocystina; each is small, has five short straight ambulacra, few thecal plates, and commonly has a modified peripheral rim with tightly sutured or fused plates. The cyathocystids appear to have evolved by paedomorphosis; they have become sexually mature “adults” while retaining a morphology similar to juveniles of isorophid edrioasteroids. This mode of evolution may have been beneficial in colonizing shallow water, nearshore, current-swept environments.

Life-sized scale models and a flume were used to observe simulated feeding and hydrodynamics of the Paleozoic camerate crinoid, Pterotocrinus. Three orientations of the crown and filtration fan (downcurrent, upcurrent, upright) in a gentle (3.5 cm/sec) current were used. Maximum baffling of the current and eddying of water into feeding areas occurred where models were oriented like most living stalked crinoids, with a parabolic filtration fan perpendicular to the current and ambulacral side downcurrent. Facing the ambulacral side of the fan upcurrent reduced time available for entrapment of potential food particles. Calyx shape was important in modifying the nature of the filtration fan baffle. Overlapping (36%) of the pinnulate arms increased the baffling effect of the filtration fan. Conspicuous tegminal structures, the Pterotocrinus wing plates, only had a baffling effect where the fan was in an upright position or the arms were infolded between the wing plates. Species of Pterotocrinus possessing blade-like wing plates could have fed effectively in several different orientations. Evolutionary success of Pterotocrinus species with blade-like wing plates probably resulted from dual feeding and protective functions of the wing plates.