bluuebunny/crossref_metadata_2025 huggingface dataset:
Effectiveness of Competition to Limit Rail Rate Increases Under Deregulation: The Case of Wheat Exports from the Southern Plains
Authors: Fuller Stephen , Shanmugham C. V.
Published: July 2016

Much of the early 1860s discontent with railroads was centered in agricultural regions, particularly the new regions of the West, where monopolistic price discrimination was most easily practiced by railroads. Because of unavailable or inaccessible forms of competing transportation and numerous small shippers, railroads were able to exploit their monopolistic position (Meyer et al.). Agrarian political action in the 1860s resulted in unsuccessful regulatory efforts by states, but laid the base for the cornerstone of federal transportation regulation, the Act to Regulate Commerce, which was passed in 1887. The Act requires that all rates be “just and reasonable” and provides that “every unjust and unreasonable charge” is unlawful.
Adaptive Planning Under Price Uncertainty in Pork Production
Authors: Plain Ronald L. , Williams Joseph E.
Published: July 2016

Market hog prices historically have shown great variation and have often followed a cyclical pattern. Franzmann (1979) finds evidence of a four-year and a twenty-eight-year cycle in hog prices. Price cycles imply the possibility of forecasting long-range prices. In turn, forecasting suggests the opportunity to vary the production or marketing process in order to maximize profits.
A Tobit Model of the Demand for Farmland
Authors: Ziemer Rod F. , White Fred C.
Published: July 2016

The market for farmland has often been a subject of interest to agricultural economists, as evidenced by numerous studies that have investigated factors determining rural land values (Aines; Reynolds and Timmons; Ruttan; Sco-field). Despite the wealth of literature concerned with land values, little is known about who owns and exercises entrepreneurial control over land resources in the U.S. Consequently, there is a lack of understanding concerning the decision to purchase farmland. Lewis has suggested that better understanding of landowner investment decisions is important in determining and implementing effective land-use policy. Also, Wunderlich has noted the importance of understanding land ownership with regard to land-use decisions. Long et al. (p. 44) have suggested that “if policies are to be designed to influence private landowners’ decisions, then it seems imperative that the factors affecting landowners’ decisions and the decision process be better understood.”
A Method For Estimating the Value of Water Among Sectors of A Regional Economy
Authors: Henry Mark S. , Bowen Ernie
Published: July 2016

Recent trends in the southeastern states toward increased use of irrigation in agriculture may be attributed to risk aversion management by farmers in response to recent drought periods. Despite ample annual average rainfall in the Southeast during the growing season, the vicissitudes of rainfall patterns provide sufficient reason to consider irrigation for field crops as well as for vegetables and fruit (Ganguly). Increased use of irrigation additionally results in new demands for water in rural areas.

It is also well documented that nonmetropolitan areas are experiencing substantial rates of positive net immigration (Wardell and Gilchrist). In the Southeast, there is a trend for new manufacturing plants to locate in rural areas where wages, taxes, and union activity are at low levels. As growth occurs in these nonmetropolitan regions, industrial, residential, and commercial activities require additional supplies of water.
Research and Extension Issues in Production Economics
Authors: Lacewell Ronald D. , McGrann James M.
Published: July 2016

The role of the economist in agriculture has increased in significance in the 1970s and 80s. A review of the recent history of agriculture begins with the period of stability and relative certainty of agricultural input and product prices in the 1950s. But by the 1970s, the economic impacts of the oil crisis, inflation, and orientation to free market prices of agricultural products necessitated a transition in the role and importance of the agricultural economist. Economists became vital to farmers who had to make economic decisions on appropriate cropping patterns, when and how to market products, and how to invest wisely.
Economic Homogeneity of Grade Classifications Under the New and Old Feeder Cattle Grading Systems
Authors: Trapp James N.
Published: July 2016

In 1979, the USDA implemented a new feeder cattle grading system that is distinctly different from the old, both in concept and terminology. Under the old grading system, the traditional grade categories of Prime, Choice, Good, and so on were used. Animals were graded according to their ability to satisfy a number of qualitative characteristics. The new system is based upon a dual criterion of framesize and muscling. Cattle are graded as either having large, medium, or small framesizes and No. 1, No. 2, or No. 3 muscling (thickness).

Casual observation of the two grading systems indicates that cattle graded as Choice under the old system will in most cases be classified as Medium Frame, No. 1 Muscled cattle under the new system. Likewise, cattle previously graded as Good will in most cases likely be graded as Medium Frame, No. 2 Muscled animals.
Some Fallacies in Agricultural Economics: A Macroeconomic Interpretation
Authors: Belongia Mike , Fisher Douglas
Published: July 2016

The relevance of macroeconomic theory to the analysis of economic behavior in the agricultural sector is a recurring theme in applied research in this area. On the one hand, it is possible to find the view that the agricultural sector should be treated in isolation as an independent market or set of markets not subject to the influences of changes in monetary and fiscal policy or (other) changes in aggregate demand and supply. On the other hand, it is also possible to find literal acceptance of the usefulness of macroeconomics—perhaps in the form of a particular version of the theory—with the controversial part surfacing in the particular view of macroeconomics and how it bears on (and is influenced by) agricultural markets. The fact that this dichotomy exists is highlighted by the contrasting views expressed recently by Breimyer (1981) and Tweeten. At the same time that Breimyer advocated that “macro-economics should be struck from the lexicon,” Tweeten chose to devote his AAEA Presidential address to a discussion of the implications of current developments in macroeconomic theory and policy for the agricultural sector; his particular emphasis is on the important role of “supply-side” macroeconomics.
Effects of the Food Stamp Program on Food Consumption in the Southern United States
Authors: Chavas Jean-Paul , Yeung M. L.
Published: July 2016

The Food Stamp Program (FSP) began in 1939 on a limited basis. In 1961, President Kennedy created an experimental Food Stamp Program that became nationwide after enactment of the Food Stamp Act of 1964. The two main purposes of the FSP are to improve the nutritional status of low income families and to support farm income by increasing food demand. The cost of the FSP rose from $1.8 billion in 1972, to $6.9 billion in 1979. This dramatic increase has motivated a considerable research effort to evaluate the program. This research can be classified into three broad categories (that are not necessarily mutually exclusive).
Nutrition and the Economics of Swine Management
Authors: Boland Michael A. , Foster Kenneth A. , Preckel Paul V.
Published: July 2016

Current methods of formulating animal rations lead to excess nutrient excretion which can potentially lead to excess manure nutrients and an increase in economic costs. These methods do not recognize the impact of diminishing returns. The objective is to simultaneously optimize feed ration composition and replacement. The results, when compared against results from a survey of feed companies, indicate that using a profit maximization rather than live weight growth maximization criterion targets nutrients to an animal's actual needs and, hence, fewer nutrients are excreted and higher returns for producers are obtained.
Trilobite vision: a comparison of schizochroal and holochroal eyes with the compound eyes of modern arthropods
Authors: Fordyce David , Cronin Thomas W.
Published: July 2016

The compound eyes of trilobites provide the best examples of fossilized sensory organs for which the function in life can be worked out today because the optical array of their corneal lenses preserves the geometry with which the eye originally sampled the visual world. An analysis of trilobite vision is strengthened by the use of new mathematical approaches to compound eye design. In particular, the product of the facet diameter (D) and the interommatidial angle (Δϕ) gives the value of the eye parameter, DΔϕ, which is a reliable indicator of the photic conditions in which the eye was used. In modern arthropods, DΔϕ values range from 0.3 for animals active in bright sunlight to 20 or more for nocturnal or deep-sea animals. Two major types of compound eyes existed in trilobites: schizochroal and holochroal. In our previous work with schizochroal eyes in the phacopids Phacops rana crassituberculata and Phacops rana milleri, we found that eye parameter values ranged from 10 to >150. These values of the eye parameter are much greater than in any living arthropod, implying that modern compound eye theory does not apply to schizochroal eyes. We suggested that each ommatidium of the schizochroal eye served as a miniature lens eye. If so, phacopid vision must have been unique, with multiply overlapping visual fields. In the new work of this paper, we examined holochroal compound eyes in Asaphus cornutus, Isotelus gigas, and Homotelus sp. Holochroal eyes contain far more ommatidia than do schizochroal types, reducing both facet diameter (D) and interommatidial angle (Δϕ). Thus, DΔϕ values in these species fall into the same range as in modern nocturnal compound eyes. This implies that function of the holochroal eye was similar to that of modern arthropods, and that they were used in moderate to dim intensities of light.
Comparative physiology of suspension-feeding in living brachiopods and bivalves: evolutionary implications
Authors: Rhodes Melissa Clark , Thompson R. J.
Published: July 2016

This paper presents scaling equations relating suspension-feeding rates to body size for articulate brachiopods and bivalve molluscs, two classes which represent a significant component of the fossil record of marine benthic communities. Clearance (feeding) rates of five species of living articulate brachiopods and three species of epifaunal suspension-feeding bivalve molluscs collected from mid-latitude fjords of Newfoundland and New Zealand were measured in similar experimental conditions. In comparisons within and between the two classes, we found that both plectolophous and spirolophous brachiopods had significantly lower feeding rates than mytilids, which are filibranchs, but that a sympatric primitive eulamellibranch veneroid bivalve had rates comparable to the brachiopods. Articulate brachiopods do not appear to feed effectively at the high algal concentrations which bivalves can exploit. The data on comparative suspension-feeding rates support the hypothesis that past changes in diversity and distribution of bivalves and brachiopods may be related to an overall increase in energy flux and escalation of metabolic rates during the Phanerozoic.
A faster-paced world?: contrasts in biovolume and life-process rates in cyclostome (Class Stenolaemata) and cheilostome (Class Gymnolaemata) bryozoans
Authors: McKinney Frank K.
Published: July 2016

Zooids of cheilostome bryozoans are on average substantially more robust than are zooids of cyclostome bryozoans. The differences include greater number, length, and cross-sectional area of tentacles, plus a more extensively developed funiculus. Median values for mouth size and cilia-generated feeding current velocity are greater for cheilostomes than for cyclostomes so that cheilostomes have the potential for greater intake of nutrient energy per unit time, which may explain their apparently higher growth rates. For unit area of substrate occupied, the Cheilostomata (Class Gymnolaemata; members of the post-Paleozoic fauna) contain greater biomass and apparently generate greater energy flow than do the Cyclostomata, which are the only extant order of the Class Stenolaemata (characteristic of the Paleozoic fauna).
Models for fossil concentrations: paleobiologic implications
Authors: Kidwell Susan M.
Published: July 2016

Four basic types of skeletal concentrations are modeled in terms of changes in sedimentation rate alone. The model categorizes fossil concentrations on the relatively objective basis of their bed contacts, and uses this criterion to infer directional shifts in net sedimentation. This radical simplification of accumulation histories, in which hardpart input is held constant, yields a surprisingly powerful model capable of predicting a broad spectrum of taphonomic and paleobiologic phenomena.Type Iconcentrations grade from less fossiliferous sediments and terminate in omission surfaces; if hardpart supply is held constant, they record a slowdown from positive to zero net sedimentation.Type IIconcentrations are the same as Type I but terminate in erosion surfaces (slowdown to negative net sedimentation), andType IIIandIVconcentrations are characterized by basal erosion or omission surfaces, respectively, grade upward into less fossiliferous sediments, and record increases in net sedimentation from negative or zero rates to positive rates. According to the model, samples collected from successive horizons within any of these shell beds will differ in the degree and type of post-mortem bias owing to differing histories of hardpart exposure at the depositional interface. Moreover, because rates of sediment accumulation govern the abundance of hardparts at the depositional interface and thus many of the physical characteristics of the benthic habitat, the dynamics of fossil accumulation have direct consequences for the structure of benthic communities (taphonomic feedback) and for ecologically controlled species morphometry.

The model is highly robust to fluctuations in hardpart input, as judged by its ability to correctly infer modes of formation of concentrations in synthetic stratigraphic sections. In addition, field examples of Type I–IV concentrations show independent evidence of formation during intervals of reduced net sedimentation, and many exhibit trends in taphonomic and paleobiologic features expected from the postulated changes in net sedimentation. The model thus provides a testable working hypothesis for the accumulation of fossil material in a wide range of environments, and should be applicable to concentrations of any taxonomic composition, state of preservation, or geologic age. The power and robustness of this heuristic model in fact argue that fossil-rich and fossil-poor strata provide fundamentally different records of past conditions, and that sedimentation rather than hardpart input is the primary control on the nature of the fossil record.
Burrowing sculptures and life habits in Paleozoic lingulacean brachiopods
Authors: Savazzi Enrico
Published: July 2016

A range of specialized burrowing sculptures evolved convergently in at least one lingulid and in several obolid and lingulasmatid genera. The sculptures inLingula punctata(Ordovician) indicate a burrowing process with the pedicle trailing behind the shell, similar to that of Recent Lingulidae. In the Obolidae and Lingulasmatidae, the orientation of the sculptures indicates a burrowing process with the pedicle oriented downward in the sediment. A burrowing mechanism in which the valves alternated in functioning as anchors, without active participation of the pedicle, is proposed for these forms. Infaunal life habits for several obolid genera are further indicated by the shell morphology and by the distribution of repaired shell damage.

The burrowing Obolidae are likely to have been adapted to relatively high-energy environments, which required frequent reburrowing in addition to escape (upward) burrowing. The increase in bioturbation in these environments in the Middle Paleozoic may have contributed to their extinction. The Lingulidae, instead, being mostly adapted to extreme environmental conditions, could survive in marginal niches which were not intensively exploited by actively burrowing organisms.
Calculation and simulation of ammonoid hydrostatics
Authors: Saunders W. Bruce , Shapiro Earl A.
Published: July 2016

The buoyancy, stability, and orientation of a shelled cephalopod in water are the predictable products of shell geometry, body chamber length, and such physical parameters as shell, tissue, and water densities. Given such physical characteristics as shell geometry, shell, tissue, and water densities, and shell thickness, the hydrostatic characteristics of planispiral shelled cephalopods, including orientation, centers of mass and buoyancy, stability, and neutrally buoyant body chamber length, can be calculated and simulated using microcomputer-based techniques. Individual variables such as geometry, body chamber length, and shell thickness are linked in a calculable manner to orientation, neutral buoyancy, and stability. Living Nautilus provides a means of testing the model and for making hydrostatic comparisons between ammonoids and nautiloids. The close agreement between calculated versus observed body chamber lengths in five species of Mississippian ammonoids shows that neutral buoyancy, and (with one exception) Nautilus-like orientations, were at least feasible for these species.
Fossil horses from “Eohippus” (Hyracotherium) to Equus: scaling, Cope's Law, and the evolution of body size
Authors: MacFadden Bruce J.
Published: July 2016

The evolution of body size in fossil horses is frequently depicted as a gradual, progressive trend toward increased body size (Cope's Law). Body size (actually body mass) was estimated for 40 species of fossil horses using dental and skeletal characters and regression equations derived from the same characters in extant species of Equus with known body mass. After body sizes were estimated, rates of morphological evolution, in darwins (d), were calculated between known ancestral and descendant fossil horse species. For the first half of horse evolution (from ca. 57 to 25 ma) body mass remained relatively static between about 25 and 50 kg with very slow evolutionary rates of 0.003–0.04 d. During the early–middle Miocene (from ca. 25 to 10 ma) there was a major diversification of body mass to about 75–400 kg and consistently higher evolutionary rates between 0.04 and 0.24 d. Since the late Miocene, body mass has generally increased with a maximum seen (in natural populations) in Equus scotti (ca. 500 kg) during the middle Pleistocene. Therefore, for horses, the traditional interpretation of gradual increase in body size through time is oversimplified because: (1) although the exception to the rule, 5 of 24 species lineages studied are characterized by dwarfism; and (2) the general trend seems to have been a long period (32 ma) of relative stasis followed by 25 ma of diversification and progressive (although not necessarily gradual) change in body size.
The origin and early diversification of birds
Authors: Cracraft Joel
Published: July 2016

Numerical cladistic analysis of 73 cranial and postcranial characters has resulted in a highly corroborated hypothesis describing the phylogenetic pattern of early avian evolution. Using “non-avian theropod” dinosaurs as a comparative outgroup and root for the tree, the analysis confirmedArchaeopteryxto be the sister-group of all remaining avian taxa, or Ornithurae. This latter taxon is subdivided into two lineages, the Hesperornithiformes and the Carinatae. The carinates, in turn, were also resolved into two sister-groups, the Ichthyornithiformes and the modern birds, or Neornithes. This paper provides morphological data corroborating the divergence of the two basal clades of the Neornithes: the Palaeognathae (tinamous and ratites) and Neognathae (all other modern birds). The phylogenetic relationships of four important Cretaceous taxa were also investigated, but these fossil taxa were too fragmentary to determine their phylogenetic position unambiguously.AlexornisandAmbiortusare both carinates, but their relationships cannot be resolved in greater detail. The relationships of the Enantiornithes may lie within the Carinatae or these two taxa may be sister-groups.Gobipteryxis a neornithine and possibly the sister-group of the Palaeognathae.

This analysis indicates that major patterns of morphological change took place at the time of origin of the ancestors of the Ornithurae and the Carinatae. Ornithurine innovations included major changes throughout the skeleton, whereas those of the carinates, while substantial, were primarily restricted to the pectoral girdle and forelimb. The phylogenetic results, in conjunction with the known ages of fossil taxa, indicate that the early lineages of birds very likely arose in the Jurassic. The early cladistic events within the neornithine lineage are also more ancient than generally recognized, and may well extend back to the early Cretaceous.
Phanerozoic development of tiering in soft substrata suspension-feeding communities
Authors: Bottjer David J. , Ausich William I.
Published: July 2016

Tiering is the vertical distribution of organisms within the benthic boundary layer. Primary tierers are suspension-feeding organisms with a body or burrow that intersects the seafloor. Secondary tierers are suspension-feeders that maintain positions above or below the sediment-water interface as either epizoans on primary tierers and plants or by living in the burrows of primary tierers. Different primary tierers from soft substrata, nonreef, shallow subtidal shelf and epicontinental sea settings have had different tiering histories, resulting largely from contrasting constructional and phylogenetic constraints. Primary colonial tierers generally occupied lower epifaunal tiers during the Paleozoic and Mesozoic, but since the Cretaceous they have been dominant in the highest tier (+ 20 to +50 cm). Primary echinoderm tierers have been almost exclusively epifaunal, and from the Paleozoic through the Jurassic they were present throughout the epifaunal tiered structure. Although primary bivalve tierers have been both epifaunal and infaunal, they have occupied only lower epifaunal tiers, whereas they have adapted to all levels of the infaunal tiering structure, particularly from the late Paleozoic through the Recent. Brachiopods have lived primarily in tiers directly above or below the water-sediment interface and have not contributed significantly to tiering complexity.

Of the numerous physical and biotic processes and constraints that affect shallow marine benthos, a few have contributed more significantly to changes in tiering patterns. Trends for increasing body size could have accounted for most of the development of tiering complexity up to +50 cm and down to –12 cm. Development of tiering above +50 cm could have been due to processes which would have yielded greater feeding capability, such as competitive interactions for a place from which to feed or adaptations to velocity gradients in the hydrodynamic boundary layer. The most significant process for development of infauanl tiering below –12 cm appears to have been as an adaptive response for predator avoidance.

Unlike infaunal tiering, which never declined after it developed, epifaunal tiering has undergone a general reduction twice. Reduction in epifaunal tiering at the end of the Paleozoic appears to have been the result of the mass extinction at this time, whereas long-term biotic processes seem to have been more important for the tiering decline at the end of the Mesozoic. Tiering structure through the Phanerozoic was thus produced through interactions of a number of physical and biotic factors, tempered by constructional and phylogenetic constraints of each primary tierer group.
A thermal model of the sailback pelycosaur
Authors: Haack Steven C.
Published: July 2016

Standard techniques of energy exchange analysis are applied to modelling the thermal regimes of several species of sailback pelycosaurs. Of particular interest is the role played by the sail in thermoregulation. Although the sail did increase the rate at which the model could warm up in the morning, its effectiveness fell short of previous estimates. The sail increased the daytime internal temperature by typically 3°C to 6°C. The more massive subjects had the highest temperature increases owing partly to their higher thermal inertia and partly to their disproportionately large sails. The sail had no impact upon the nocturnal minimums in temperature.

Overheating does not appear to have been a significant problem in the Permian environment, particularly in view of the high thermal inertia of the subjects modeled. When overheating occurred, the sail was of limited value for dumping excess heat.
Growth and function of Stegosaurus plates: evidence from bone histology
Authors: de Buffrénil V. , Farlow J. O. , de Ricqlès A.
Published: July 2016

Histological examination of Stegosaurus dorsal bony plates shows a thin wall of incompletely remodeled bone surrounding a large cancellous region containing some large “pipes” delineated by thin bony walls. Growth proceeded mainly from the basal region of the plates. Histological observations provide a test against which several functional interpretations of the plates are checked. While some interpretations (e.g., plates as armor) are clearly falsified, others (linked to thermoregulatory functions) seem to be more robust, although by no means can they be viewed as clearly vindicated on the basis of the evidence presently available.
Skeletal modifications related to food capture and feeding behavior of the basketstar Astrophyton
Authors: Macurda Donald B.
Published: July 2016

The modern gorgonocephalid ophiuroid Astrophyton, a basketstar, has feeding habits which may be analogous to those of some Paleozoic crinoids that lack pinnulate arms (Meyer and Lane 1975). Field study has demonstrated the very quick response of Astrophyton when plankton impinge upon its arms. Study of the skeletal microstructure by scanning electron microscopy has shown that the quick response is facilitated by the development of relatively large ventral muscle fossae and articular surfaces whose shape follows a catenary curve. Prey are impaled by spines which articulate with the ventral surface of vertebral ossicles. Stereomic microstructure of vertebral ossicles is galleried where ligaments are present and labyrinthic where muscular tissue is present. The same microstructures are found in muscular articulations of modern crinoids. Future work on the arm structure of Paleozoic taxocrinids and cyathocrinids may demonstrate structural analogies and suggest similarities in food capture between such crinoids and modern baskets tars.
Equations of motion for post-mortem sinking of cephalopod shells and the sinking of Nautilus
Authors: Weaver J. Scott , Chamberlain John A.
Published: July 2016

Consideration of the physics of sinking of hollow, rigid bodies leads to equations of motion for sinking cephalopod shells. We have derived equations of motion for three post-mortem sinking situations: sinking with a fixed amount of water in the phragmocone; rapid phragmocone filling (no siphuncular tube); and slow phragmocone filling (siphuncular tube intact). In all three cases sinking speed can be closely approximated by the terminal velocity calculated from the total weight, buoyancy, and drag parameters of the shell.

Experiments on modern Nautilus shells yield sinking velocities in agreement with calculated values. The experiments also show that orientation of a sinking Nautilus shell varies as the phragmocone fills with water. With small negative buoyancy the shell sinks with its plane of symmetry upright, but as it fills, it begins to rock from side to side and leans over and sinks with its plane of symmetry horizontal when the camerae are about 55% full.

The maximum sinking speed of upright adult Nautilus shells is approximately 30 cm/sec, which appears to be too small for embedding in the bottom upon impact. The maximum depth to which Nautilus sinks in the upright position ranges from about 7 m for rapidly filling shells to as much as 600 m for slowly filling shells. In the latter case, the shell will continue to fill after coming to rest on the bottom, and the stability of the vertical orientation will be removed within 1 or 2 days. Thus, primary vertical preservation of cephalopod shells indicates water depths less than about 10 m.
Convergent evolution of desert rodents: multivariate analysis and zoogeographic implications
Authors: Mares Michael A.
Published: July 2016

Ecological investigations were conducted on rodent faunas in the Sonoran Desert of the southwestern United States and the Monte Desert of northwestern Argentina. Both study areas are physiognomically quite similar and the rodents are only distantly related. Such conditions are ideal for an assessment of possible evolutionary convergence. Multivariate analyses of morphoecological characters support the subjective interpretation that ecological equivalents between the deserts differ in their degree of similarity. The data indicate that the Monte rodent fauna is composed of two distinct groups: a) the caviomorph rodents, which are highly desert adapted; and b) the murids, which range widely beyond the desert's boundaries and are probably not as highly desert adapted, as a group, as are the caviomorphs. When the Monte and Sonoran faunas are compared with a North American coniferous forest rodent fauna, data show that both desert groups have converged toward one another. The different degrees of desert adaptation and different distributional patterns indicate that the Monte Desert was colonized in two different periods (one in the early Tertiary and one in the late Pliocene or early Pleistocene) and can be interpreted as supporting theories regarding South America's colonization by mammals which were first proposed by Simpson (1951).
Macroevolution: the fifth dimension?
Authors: Schopf Thomas J. M.
Published: July 2016

The Field Museum of Natural History, Chicago, held a conference on Macroevolution, October 16–18; it was organized by J. Cracraft, J. Levinton, N. Eldredge and D. M. Raup. The nature of the meeting called to mind the 1946 Princeton conference on Genetics, Paleontology and Evolution (which resulted in the book of the same name1), and indeed 3 members of that conference spoke again, 34 years later, in 1980—Sewall Wright, G. Ledyard Stebbins, and Bobb Schaeffer. However, no book is planned this time.
Determinants of diversity in higher taxonomic categories
Authors: Valentine James W.
Published: July 2016

It is often assumed that, if a few species are introduced into a relatively empty environment, the subsequent diversification will take the form of a logistic growth curve, rising to an equilibrium level of species richness. The diversifications of taxa in higher categories commonly resemble logistic curves, although there are no well-defined theoretical bases for such a resemblance.

A model of diversification of taxa in higher categories is based on the notion that many taxa originate rapidly. Relatively small changes leading to new species occur at a high frequency, while larger changes leading to progressively higher taxa occur with progressive rarity. During diversification in an empty environment, few large changes will occur before the environment is filled. The rate of filling, relative to the rate of production of higher taxa, determines the richness of taxa in higher categories and gives the diversification curves a logistic appearance although the maximum level achieved is not an equilibrium. Subsequently, opportunities for diversification will generally lead only to the appearance of taxa in progressively lower categories.
Paleobotany: Perspectives in 1980
Authors: Knoll Andrew H. , Rothwell Gar W.
Published: July 2016

In the past twenty years, both knowledge of fossil plants and ways of looking at the paleobotanical record have expanded significantly. Studies of Precambrian microfossils have provided insight on early photoautotrophs, while fundamental changes in perceptions of Silurian and Devonian plant remains have clarified our understanding of the colonization of land, as well as the subsequent evolution of complex stems, leaves, and the seed habit. A recurring question concerns the phylogenetic relationships of gymnosperms: is the gymnospermy found in various living and extinct taxa the result of evolutionary convergence or of common descent? Rapidly accumulating data on the reproductive and developmental biology of Paleozoic seed ferns is reopening debate on this issue. The mystery of angiosperm origins remains “abominable”, but the past two decades of research have seen convincing documentation of the initial radiation and rise to taxonomic and ecological dominance of the flowering plants.

While phylogenetic and systematic botany remain at the core of paleobotanical research, increased attention is being devoted to studies of ontogeny and reproductive biology, paleoecology, taphonomy, paleophytochemistry, paleoclimatology, and paleobiogeography. Studies of evolutionary rates and diversity are in their infancy, but initial results permit an optimistic appraisal of the contributions that paleobotanists can make to evolutionary paleontology.
A factor analytic description of the Phanerozoic marine fossil record
Authors: Sepkoski J. John
Published: July 2016

Data on numbers of marine families within 91 metazoan classes known from the Phanerozoic fossil record are analyzed. The distribution of the 2800 fossil families among the classes is very uneven, with most belonging to a small minority of classes. Similarly, the stratigraphic distribution of the classes is very uneven, with most first appearing early in the Paleozoic and with many of the smaller classes becoming extinct before the end of that era. However, despite this unevenness, a Q-mode factor analysis indicates that the structure of these data is rather simple. Only three factors are needed to account for more than 90% of the data. These factors are interpreted as reflecting the three great “evolutionary faunas” of the Phanerozoic marine record: a trilobite-dominated Cambrian fauna, a brachiopod-dominated later Paleozoic fauna, and a mollusc-dominated Mesozoic-Cenozoic, or “modern,” fauna. Lesser factors relate to slow taxonomic turnover within the major faunas through time and to unique aspects of particular taxa and times.

Each of the three major faunas seems to have its own characteristic diversity so that its expansion or contraction appears as being intimately associated with a particular phase in the history of total marine diversity. The Cambrian fauna expands rapidly during the Early Cambrian radiations and maintains dominance during the Middle to Late Cambrian “equilibrium.” The Paleozoic fauna then ascends to dominance during the Ordovician radiations, which increase diversity dramatically; this new fauna then maintains dominance throughout the long interval of apparent equilibrium that lasts until the end of the Paleozoic Era. The modern fauna, which slowly increases in importance during the Paleozoic Era, quickly rises to dominance with the Late Permian extinctions and maintains that status during the general rise in diversity to the apparent maximum in the Neogene. The increase in diversity associated with the expansion of each new fauna appears to coincide with an approximately exponential decline of the previously dominant fauna, suggesting possible displacement of each evolutionary fauna by its successor.
Arguments for a glossopterid ancestry of angiosperms
Authors: Retallack Greg , Dilcher David L.
Published: July 2016

Almost every living and fossil group of gymnosperms has been proposed as a possible ancestor of angiosperms. A common problem with many of these proposals is their reliance on hypothetical intermediate forms. Another common problem is finding correctly-oriented organs homologous to all the important reproductive structures of angiosperms.

These problems are least troublesome for a glossopterid origin of angiosperms. Recently discovered ovule-bearing organs of these plants may represent evolutionary intermediates, or analogous plants, between glossopterids and angiosperms. According to recent reinterpretations of glossopterid ovule-bearing organs, they have structures in an orientation which may be homologous with both the outer ovular integument and the carpel of angiosperms. Considering the reproductive and vegetative features of glossopterids, the hypothesis that they may be part of a stock ancestral to angiosperms should be seriously considered.
Brachiopods and pedicles
Authors: Richardson J. R.
Published: July 2016

The pedicle differentiates brachiopods from all other phyla. With its associated musculature, it is more variable than any other brachiopod system at or above the generic level and is considered to contribute to the versatility of behavior possessed by some species. Differences in pedicle type are reflected clearly in the beak.
Shell sculpture as a defensive adaptation in ammonoids
Authors: Ward Peter
Published: July 2016

Quantification of Paleozoic, Triassic, Jurassic, and Cretaceous ammonoid shell ornamentation shows that commonality and roughness of ornamentation increased throughout the geologic range of the ammonoids. The two major hypotheses concerning the function of ammonoid shell ornamentation are that 1) ornament served a protective (defensive) function against shell breakage by predators, and 2) it increased hydrodynamic efficiency of the shell during swimming. The heavily ribbed and spined ammonoid shells of the late Mesozoic have ornamentation too coarse to have served any hydrodynamic purpose. The increasing proportion of such shells during the Jurassic and Cretaceous may have been in response to increased numbers of late Mesozoic shell crushing predators and “better armed” ammonoid prey. This trend parallels adaptive trends of other invertebrate groups during the “Mesozoic marine revolution” as defined by Vermeij (1977).
But Not Wright Enough: Reply to Orzack
Authors: Gould Stephen Jay
Published: July 2016

As The Blob, of Steve McQueen's greatest triumph, so amply demonstrated, the more you encompass the more formless you become. Orzack accuses me of construing the modern synthesis too narrowly in describing a version championed only by Mayr and Fisher—a pair of unlikely bedfellows, I would have thought. Yet his version is so broad that he wins his own argument by internal definition, thus rendering it meaningless. As “the basis of the modern synthesis,” Orzack cites “the great evolutionary idea” — “all evolution can be explained in principle by an examination of the properties of individuals and of populations.” But what else is there, except perhaps Schindewolf's supernovae and Teilhard's ever-watchful Jesus, drawing organic activity towards Omega. If the synthesis only excludes some fringing finalists and unrepentant Lamarckians, then we are all inevitably in it, and we might as well recast the term as a synonym for evolution itself.
Crocodilian scatology, microvertebrate concentrations, and enamel-less teeth
Authors: Fisher Daniel C.
Published: July 2016

It has been suggested that certain fossil assemblages consisting of disarticulated and broken remains of small to medium-sized vertebrates (“microvertebrate concentrations”) may be accumulations of incompletely digested material defecated by crocodilians. Experiments on crocodilian digestion show, however, that these reptiles demineralize calcified tissues, frequently leaving intact organic matrices of dentine, cementum, and bones in their feces. Such matrices, even if preserved as fossils, would not resemble most specimens in microvertebrate concentrations. Therefore, crocodilian digestion does not appear to have been an important factor in the formation of these fossil assemblages. Teeth similar to those defecated by crocodilians nevertheless do occur in the fossil record. Such teeth, lacking enamel but often complete in other respects, are interpreted here as having been digested by crocodilians, defecated as demineralized organic matrices, and subsequently remineralized. Enamel, with its extremely low organic content, does not yield a demineralized matrix susceptible to remineralization. A number of recently recognized occurrences of enamel-less teeth attest to the significance of crocodilian digestion as a factor in the taphonomic history of many Mesozoic and Cenozoic fossil vertebrate assemblages.
Kosmoceras: Evolutionary Jumps and Sedimentary Breaks
Authors: Raup David M. , Crick Rex E.
Published: July 2016

Brinkmann (1929) argued that phyletic evolution in the Jurassic ammonite Kosmoceras is sufficiently linear that the amount of time missing at diastems can be estimated by the magnitude of morphologic jumps at those horizons. Brinkmann's unpublished raw data have been re-analyzed in order to evaluate the association between evolutionary jumps and physical breaks. All horizons in Brinkmann's 1400 centimeter stratigraphic section have been tested for morphological jumps. Up to 40 statistically significant morphological jumps exist in the section, the actual number depending on the sample interval used. A few of these correspond to the jumps found by Brinkmann and a few coincide with diastems. However, the correspondence between morphological jumps and physical breaks is not as consistent as was thought by Brinkmann. Furthermore, it is argued that the association between physical and biological discontinuities is not dependent on linear evolution but rather is the expected condition wherever phyletic evolution occurs. Due to the irregularity and unpredictability of evolutionary change in Kosmoceras, morphologic jumps cannot be used to assess the amount of time missing at diastems.
Heterochrony and Phylogenetic Trends
Authors: McNamara Kenneth J.
Published: July 2016

A model is proposed, based on examples that have been interpreted as phylogenetic trends, to explain how directional morphological evolution at the species level can arise by heterochrony. The examples illustrated are of Tertiary to Recent rhynchonellide brachiopods, Cambrian olenellid trilobites, living spatangoid echinoids, Tertiary to Recent schizasterid echinoids, Cenomanian ammonites and Silurian monograptids. Morphological discontinuities between species along morphological gradients (which can be recognised both spatially and/or temporally), and temporal morphological stasis within species, are both consistent with the punctuated equilibria model of macroevolution. It is argued that morphological discontinuities have arisen by selection of morphological novelties produced by heterochronic processes. These novelties are preadaptations which allow ecological and, consequently, genetic isolation from ancestral species. Establishment of a heterochronic morphological gradient is only possible given a suitable environmental gradient. The terms “paedomorphocline” and “peramorphocline” are proposed for these heterochronic morphological gradients. Paedomorphoclines and peramorphoclines each comprise a number of species occupying a series of adaptive peaks, which have evolved sequentially through time by selection along an environmental gradient.
Paleoanthropology: Pliocene and Pleistocene human evolution
Authors: Delson Eric
Published: July 2016

Modern paleoanthropology is broadly interdisciplinary, integrating the results of studies in hominid (or more generally primate) paleontology, morphology and systematics with archeology, stratigraphy, chronometry, general paleontology, taphonomy and ecology, among other fields. (I here employ the term “hominid” to include all advanced hominoids of Miocene to Pleistocene age, following Delson and Andrews, 1975; similarly “hominine” (or “human”) refers to members of the subfamily Homininae of this usage, especiallyAustralopithecusandHomo.Many other authors restrict hominine/human toHomoalone, employing hominid where I use hominine.) This integrative approach has been both spectacular and successful in eastern Africa (see Laporte 1980), due to the influence of F. C. Howell, the Leakeys and their colleagues, but it has also been responsible for recent advances in other temporal and spatial intervals in human evolution. In this review, I will concentrate on the morpho-evolutionary aspects of recent paleoanthropological studies, indicating major sources and new developments. Most fossils not otherwise referenced are discussed, albeit often with a different interpretation, in Wolpoff's (1980a) text.
A test of macroevolutionary problems with neontological data
Authors: Lemen Cliff A. , Freeman Patricia W.
Published: July 2016

Ricklefs (1980) suggested the use of neontological data to distinguish between puncuated equilibrium and gradualism as modes of evolution. This paper investigates his model and finds it contains oversimplifications that make any test difficult. We modify his model slightly and use it as a limited test of punctuated equilibrium by large morphological shifts at speciation. This test is applied to a data set of 110 species from two families of bats, the Emballonuridae and the Molossidae. We find no evidence of consistently large morphological shifts at the formation of subspecies, species or genera.
Crinoid arms and banana plantations: an economic harvesting analogy
Authors: Cowen Richard
Published: July 2016

The pattern of arm branching and arm morphology in the camerate crinoid family Melocrinitidae became more complex during an evolutionary sequence which extended from Late Ordovician to Late Devonian. The fully evolved melocrinitid arm pattern bears an amazing resemblance to the theoretically ideal lay-out for harvesting roads on a banana plantation. This may not be coincidental since the problems faced by a banana plantation manager are much the same as those of a crinoid: the harvesting of an evenly distributed micro-particulate resource from an area and its delivery to a central point for processing. The analogy suggests a detailed explanation of the melocrinitid morphology and evolution. It also raises the question: why did the pattern not become dominant among crinoids if it was so efficient? It may have been unlikely to evolve; it may reflect an unusual food supply. I prefer an explanation in which the plantation pattern demands a rigidity of the crinoid crown which is characteristic of camerates but is uncommon among other crinoids: the latter have adopted a strategy of feeding which emphasizes flexibility in anatomy and behavior. The banana plantation pattern is equally rare among other organisms. Thus an “ideal” may not be common in a group of organisms for cost-benefit reasons. This does not mean that the adaptationist's approach is improper, or that random, historical, or constructional constraints routinely overwhelm adaptation. Rather, it means that cost-benefit analysis should take a larger part in functional studies, as it does in natural selection, and that theoretical ideals should be viewed with caution.