Body shape and mode of swimming were major factors that affected the swimming capabilities of Mesozoic marine reptiles. By estimating the total drag and the amount of energy available through metabolism, the maximum sustained swimming speed was calculated for 115 marine reptile specimens. Calculated sustained swimming speeds range from 1.8 to 2.7 m/sec, but are probably too high by as much as a factor of two. Mesozoic marine reptiles were probably much slower than modern toothed whales. The diversification of fast, agile teleost fish in the Cretaceous may have therefore contributed to the decline of the marine reptiles.

Long-bodied reptiles appear to have had slower sustained swimming speeds than deep-bodied forms of the same length. For a given length, ichthyosaurs were probably faster sustained swimmers than plesiosaurs, and plesiosaurs were probably faster sustained swimmers than crocodiles and mosasaurs. This suggests that the long-bodied forms probably used an ambush technique to capture prey, to maximize the range of possible prey and to minimize competition with the faster pursuit predators.

Modern ruminant species have traditionally been placed in three broad dietary categories (browsers, grazers and intermediates) based on their observed feeding habits. Shape analysis of premaxillary outlines of 31 species of ruminants shows that their premaxillae differ according to their dietary category. Browsers have pointed premaxillae and grazers square ones. Intermediate feeders have intermediate outlines.

The Miocene giraffid Samotherium boissieri has always been viewed as a specialized browser similar to the modern okapi, Okapia johnstoni. However, the premaxillary shape of S. boissieri falls very close to the mean of the grazers and is most similar to that of the African buffalo (Syncerus caffer), a committed grazer.

Quantitative analyses of the microscopic wear patterns on the molars reveal significant differences between three modern species from the three dietary groups. S. boissieri has more microscopic scratches on its teeth than either the modern giraffe Giraffa camelopardalis (a browser) or Grant's gazelle Gazella granti (an intermediate feeder). In this respect, it is indistinguishable from the wildebeest Connochaetes taurinus which is a committed grazer.

Both of these analyses suggest that this extinct giraffid was a grazer, although we cannot rule out the possibility that it was an intermediate feeder. It was definitely not a specialized browser as are both living members of the Giraffidae.

George Gaylord Simpson was one of the first paleontologists to apply survivorship analysis to the study of fossil taxa. His finding that the survivorship curve for extant bivalve genera plotted above that for extinct genera led him to conclude that bivalve genera are drawn from at least two distinct distributions of longevities, and formed the fundamental basis for his influential concepts of horotelic and bradytelic evolutionary rates. Survivorship curves presented in this paper show the same pattern of disjunct survivorship in genera from the Treatise on Invertebrate Paleontology and in families from Sepkoski's compendium.

Some of the observed differences between survivorship curves are artificial, occurring because long-lived genera and families are more likely to survive to the Recent than short-lived genera and families. The living fauna thus contains a disproportionate number of long-lived genera and families, and the survivorship curve for the living fauna is expected to lie above that for the extinct fauna for this reason alone—even if all longevities are drawn from the same distribution. Recognition of this bias led Raup (1975) to question the significance of the survivorship patterns presented by Van Valen (1973), and Stanley's (1984) acceptance of Raup's argument led him to dismiss the survivorship pattern discovered by Simpson. But statistical analysis using bootstrapping shows that this bias accounts for only a small proportion of the difference between survivorship curves. Other biases considered, such as “pull of the Recent,” “asymmetrical range truncation,” and erroneous concatenation of stratigraphic ranges, do not account for the pattern either. Although still other biases, as yet unknown, cannot definitively be ruled out, it appears that the longevities of extinct and living bivalve taxa are meaningfully different, and that the fundamental causes are biological.

Seven taxa of raptorial birds were experimentally fed a controlled sample of 50 house mice (Mus musculus). Bones recovered from the pellets were examined for interspecies variability in preservation to assess the potential contribution of specific raptors to patterning in fossil assemblages. Quantitative analyses demonstrate that patterns in bone fragmentation may assist in the identification of particular raptor species as depositional agents in small mammal assemblages.

The ability of paleobiologists to draw paleoecological inferences based on spatial faunal variability within a single stratigraphic interval depends ultimately on the spatial resolving power of the fossil record. This paper evaluates the potential spatial resolution of fossil assemblages by examining modern skeletal remains of molluscs on a benthic transect, along which there is a marked decrease in seagrass cover, in Smuggler's Cove, St. Croix, U.S. Virgin Islands. The sampling transect began in a Thalassia-covered area approximately three meters deep, extended into slightly deeper water with lighter seagrass cover, and ended on an open, bioturbated sandy tract at a depth of nearly six meters.

Two-way cluster analysis and polar ordination of 37 samples of molluscan remains, taken at 10-meter intervals along the 360-meter transect, reveal patterns of variation that are shown by correlation analyses and consideration of the autecologies of individual species to be related to measured changes in vegetation. There is a transition from dominance primarily by epifaunal gastropods living on seagrass blades to dominance by infaunal, burrowing bivalves as grass cover becomes lighter. Some non-systematic variability exists in faunal distributional patterns within areas where the environment does not vary systematically, but this does not mask the regular faunal transitions related to environmental changes. Correspondence between the dead and live faunas is difficult to ascertain because of the scarcity of live fauna in collected samples.

The results suggest that spatial faunal transitions in fossil remains at even the fine scale evaluated in this study are potentially preservable in the fossil record.

Application of computed tomography to the most recently recognized specimen of Archaeopteryx demonstrates the potential of this technique for paleontological issues. Contrary to earlier interpretations of these specimens, the results of computed tomography appear to show the presence of an avian-like doubled-headed quadrate bone in this earliest true bird.

The logistic model provides a useful geometric description of coiling for larger Foraminifera. This model represents a spiral in polar coordinates by means of a logistic equation. The model describes the spires of the genera Alveolina, Nummulites, and Assilina very well. The logistic model is a consequence of allometric growth in these genera. The spires of Nummulites do not fit the logarithmic spiral model well, because the model does not accommodate ontogenetic change of form. Computer simulations using the logistic model also show the very different morphologies of the genus Alveolina. The model allows study of geometrical constraints on test form and of pathways followed by the evolution of the genus (or genera). The logistic model describes ontogenetic change in the organism's functional requirements. The main physiological requirements are nourishment, general exchanges of matter and energy with the environment, and light for the photosynthetic symbionts that live in the cytoplasm of these larger Foraminifera. All these functions require suitable area/volume ratios, that mandate changes of form during growth. The possible biological meaning of the parameters of the model is explored. The use of the more meaningful parameters is proposed in statistical multivariate studies.

Megafossil remains of conifers allied to taxa of the high montane fir-spruce-hemlock-white pine zone often occur in relatively lowland Tertiary floras together with taxa typical of the mixed-conifer and broadleaved sclerophyll forest zones. Even though these forests are now separated in elevation by fully 1,000 m and in distance by 10–20 km or more, it has been generally accepted that the structures of the high montane conifers were transported to the basins of deposition from distant, high mountains. Several lines of evidence show that montane conifers were regular members of both mixed-conifer and montane conifer forests. They were restricted to higher elevations in the late Neogene–Quaternary; as summers became drier and hotter, the germinating seedlings failed to become established in the mixed-conifer forest zone. They were further isolated from the broadleaved sclerophyll zone, which was confined to lower levels as winters became colder and snow more frequent.

Recovery of trilobite faunas following a mass extinction during the Upper Cambrian Sunwaptan Stage (equal to the “Ptychaspid Biomere”) involved increases in both within-habitat (alpha) diversity and in levels of biofacies differentiation. This pattern parallels, at a lower hierarchical level, the global increase in Phanerozoic marine invertebrate species richness (Sepkoski et al. 1981), which was influenced by changes in provinciality and in alpha diversity. Diversification slowed markedly in subtidal shelf carbonate habitats in the upper half of the stage, but continued in carbonate shelf margin environments, possibly due to higher rates of immigration from off-shelf sites. Trilobite clades appearing early in the stage have low centers of gravity, reflecting high immigration rates during and shortly after an interval of mass extinction. Expansion of shallow-water carbonate deposition in the upper half of the stage was accompanied by the spread of carbonate bank biofacies. Families occurring in these biofacies gradually increased in species richness and tended to have high centers of gravity.

Plesiadapiforms were among the most diverse and abundant of North American mammalian groups during the Paleocene epoch. Their decline and extinction has been attributed to a variety of causes, including competitive exclusion by rodents and/or by primates of modern aspect (euprimates), and the effects of late Paleocene–early Eocene climatic warming. However, analyses of generic and species richness and relative abundance patterns indicate that the decline of plesiadapiforms was more complex than usually supposed. The two major superfamilies, Plesiadapoidea and Microsyopoidea, exhibited very different patterns of decline. Microsyopoids and paromomyid plesiadapoids do not exhibit a pronounced decline in taxonomic richness and relative abundance during the Early Tertiary. Non-paromomyid plesiadapoids do decline markedly, but, when their taxonomic richness and relative abundance patterns are compared with those of potentially competing taxa (rodents and euprimates) only non-paromomyid plesiadapoids and rodents show the inverse relationship consistent with taxonomic displacement. Euprimates appear in North America after non-paromomyid plesiadapoids were virtually extinct. Analyses of body size, diet, diel activity patterns, and locomotion support the hypothesis that rodents and non-paromomyid plesiadapoids may have competed for the same resources; their paleobiogeographic histories also are consistent with the competition argument.

Currently available paleoclimatological data for the Early Tertiary largely pertain to global temperature trends and are not detailed enough to demonstrate unequivocally whether the decline of non-paromomyid plesiadapoids coincided with climatic change. A more complete record of paleoclimatic indicators, especially from the Western Interior of North America, is needed to test the climate hypothesis adequately. The several independent lines of evidence considered here and elsewhere in reference to other mammalian taxa strongly support the hypothesis that competition with rodents was an important factor in a major restructuring of Early Tertiary mammalian communities in North America.