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We demonstrate that momentum-dependent nuclear interactions (MDI) have a large effect on the dynamics and on the observables of high-energy heavy-ion collisions: A soft potential with MDI suppresses pion and kaon yields much more strongly than a local hard potential and results in transverse momenta intermediate between soft and hard local potentials. The collective-flow angles and the deuteron-to-proton ratios are rather insensitive to the MDI. Only simultaneous measurements of these observables can give clues on the nuclear equation of state at densities of interest for supernova collapse and neutron-star stability.
The present article is a crosslinguistic discussion of the distinction between a word class of nouns and a word class of verbs in the UNI TYP framework of the dimension of PARTICIPATION (for a first overall sketch of PARTICIPATION see Seiler 1984). According to this framework the noun/verb-distinction (henceforth N/V-D) must be regarded as a gradable, continuous phenomenon ranging from the stage of a clear-cut distinction with no overlap to almost a non-distinction. Although there is no question that most, if not all, languages do differentiate between nouns and verbs, it is also quite apparent that the languages do so to a different degree and by different means, and that it only makes sense to use the terms "noun" and "verb" in different languages when one actually has a common functional denominator in mind (see below). After a general introduction to the notion of a noun/verb-continuum (chapter 1) the reader will be presented with a survey of languages as diverse as German. English, Russian, Hebrew, Turkish, Salish. and Tongan (see chapter 2) in support of the continuum hypothesis. In chapter 3 the facts are coordinated in an overall pattern of regularities underlying the Increase or decrease of categorical restrictions between the respective word classes. Also, chapter 3 raises the issue to what degree a N/V-D can be considered a matter of certain lexemes or a matter of the morphosyntactic environment of certain lexical units. Lastly, we shall seek for an answer to the question why it is not a necessary requirement for languages to draw a sharp distinction between a word class of nouns and a word class of verbs.
Multivariate statistical procedures are used to distinguish species in the reef-coral genus Stephanocoenia through a continuous Neogene sequence (five-million year time interval) in the Cibao Valley of the northern Dominican Republic. This genus is the only member of the family Astrocoeniidae that occurs in the sequence. The material consists of 56 colonies (17 of which are measured) from 24 localities in four river sections, the most important being Rio Gurabo and Rio Cana. Ten characters are measured on each of 10 corallites per colony. The data are analyzed using cluster and canonical discriminant analysis to group colonies into clusters representing species. Identical measurements on modem colonies collected near Discovery Bay, Jamaica are included for comparison. Two fossil species are defined in the analysis, one of which is new (Stephanocoenia duncani, n. sp.). Both species are significantly distinct from the single modem species (S. intersepla) that is the sole living representative of the genus. Study of collections from other reef localities shows that both fossil species occur only during Neogene time and only at a limited number of localities. Patterns within each species are traced up a composite stratigraphic section using nonparametric statistical analyses. One of the two fossil species (S. spongiformis) is found to remain stable through time, whereas the other (S. duncam) changes its morphology in a direction approaching the cluster for the modem species. Further study of patterns of variation within the one modern and two fossil clusters shows that intraspecific variation is unusually complicated in this genus. The clusters overlap, and colonies within each cluster differ widely. Variation between populations within the modem species occurs in the same characters as those which distinguish the modem species from the fossil species converging with it (S. duncam). However, these two species form a morphologic continuum that cannot be explained by environment alone. Therefore, they may represent two gradually intergrading chronospecies within one lineage. Of the two fossil species of Stephanocoenia defined, one species (s. spongiformis) exhibits an evolutionary pattem similar to that observed in the family Poritidae. In this pattern, species were found to have short durations and stable morphologies and to have become extinct during the mid- to late Pliocene through early Pleistocene mass extinction. In contrast, the second species of Slephanocaenia (S. duncam) may have evolved over a long time period, possibly forming chronospecies that survived the mass extinction. Unlike genera in the Poritidae, however, no radiation of taxa occurred in the genus after the extinction event. Since no consistent relationship has been discovered between morphology and environment in these corals with the data at hand, their paleoecologic value can only be determined after data on more taxa are collected, and their associations with other corals are studied. This study represents part of a multidisciplinary project on the stratigraphy and paleontology of the northern Dominican Republic, coordinated by P. Jung and J. B. Saunders of the Naturhistorisches Museum Basel, Switzerland.
The 20 species of Neogene Scleractinia in the suborders Caryophylliina and Dendrophylliina known from the Dominican Republic are revised and illustrated. This research was based on 1590 specimens obtained primarily from the collections of the Naturhistorisches Museum, Basel, Switzerland; National Museum of Natural History, Smithsonian Institution, Washington, DC, U.S.A.; and Tulane University, New Orleans, LA, U.S.A. Eight new records are reported for the Neogene of the Dominican Republic, including four new species: Antillocyathus alatus, Trochocyathus chevalieri, T. duncani, and Paracyathus sinuosus. Special attention is given to the genus Asterosmilia, since half (five) of the known species in this genus occur in the Dominican Republic. Most species described herein are assumed to constitute a deep-water fauna by analogy to depth ranges of the same or similar species known from the Recent. Certain localities and parts of formations are inferred to represent deep-water (> 200 m) facies. These inferences may aid in the paleoecological interpretation of other fossils collected from these areas.
The final states of central Ca + Ca and Nb + Nb collisions at 400 and 1050 MeV/nucleon and at 400 and 650 MeV/nucleon, respectively, are studied with two independently developed statistical models, namely the classical microcanonical model and the quantum-statistical grand canonical model. It is shown that these models are in agreement with each other for these systems. Furthermore, it is demonstrated that there is essentially a one-to-one relationship between the observed relative abundances of the light fragments p, d, t, 3He, and α and the entropy per nucleon, for breakup temperatures greater than 30 MeV. Entropy values of 3.5–4 are deduced from high-multiplicity selected fragment yield data.
We present a mechanism for the separation of strangeness from antistrangeness in the deconfinement transition. For a net strangeness of zero in the total system, the population of s quarks is greatly enriched in the quark-gluon plasma, while the s¯ quarks drift into the hadronic phase. This separation could result in ‘‘strangelet’’ formation, i.e., metastable blobs of strange-quark matter, which could serve as a unique signature for quark-gluon plasma formation in heavy-ion collisions. PACS: 25.70.Np, 12.38.Mh
The recent attempts to extract the temperature in the late stage of medium energy (20–60 MeV/nucleon) heavy ion collisions from the yields of γ- and particle-instable fragments are discussed. The quantum statistical model is employed to demonstrate that feeding from instable states distorts the yields used for the temperature determination severely. Some particle instable fragments are only moderately affected by feeding. These selected species can still be useful for determining the temperature. The breakup temperatures of the fragment conglomerate extracted with this method are T≃4–8 MeV, much smaller than the corresponding slope factors, which indicate T∼15 MeV.