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1
Content available Kraina mięsa
100%
EN
Originally published by Granta in 1995, the essay  "Meat Country" by John Maxwell Coetzee is a starting point to think about human-animal relations in the context of food culture. Written by Coeztee during his stay in Austin, Texas, the essay explores American obsession with meat and the likelihood of vegetarianism to become a universal diet.
PL
Artykuł "Kraina Mięsa" jest pierwszym polskim tłumaczeniem eseju Johna Maxwella Coetzee'go "Meat Country" opublikowanego w 1995 roku przez czasopisma Granta.  
PL
Artykuł skupia się przede wszystkim na instytucji parafii i rodziny w odniesieniu do dziedzictwa kulturowego polskich Teksańczyków drugiej fali trwającej od 1867 r. Sięgając do początków polskiego wychodźtwa do Stanów Zjednoczonych, które wiązało się z założeniem osady Panna Maria w Teksasie przez emigrantów ze Śląska Opolskiego, artykuł przedstawia drugą falę emigracji głównie z Galicji i Wielkopolski. Analiza oparta została na materiałach archiwalnych Polskiego Towarzystwo Genealogicznego w Teksasie (Polish Genealogical Society of Texas – PGST), które to wydawało periodyki od 1984 do 2021 r. Materiał badawczy zebrano z 124 woluminów PGST (4358 stron). Dowiedziono w artykule, że zarówno parafia, jak też rodzina były podstawowym jednostkami w życiu polskich emigrantów, wokół których toczyło się życie codziennie, rodzinne, społeczne i religijne.
EN
The article focuses primarily on the institutions of the parish and family in relation to the cultural heritage of Polish Texans of the second wave since 1867. Reaching back to the beginnings of Polish emigration to the United States, which is associated with the settlement of Panna Maria in Texas by emigrants from Opole Silesia, the article presents the second wave of emigration from Galicia and Greater Poland. The analysis was based on the archival materials of the Polish Genealogical Society of Texas (PGST), which cover the periods from 1984 to 2021. The research material was collected from 124 PGST volumes (4,358 pages). The document proves that both the parish and the family were the basic units in the lives of Polish emigrants, around whom everyday family, social and religious life revolved.
EN
An unusual 6–8 cm layer of prismatic cartilage and matrix containing some 8,800 teeth, coprolites, incomplete occipital spines, and denticles of Orthacanthus platypternus (Cope, 1883) occurs in the lower Permian (Artinskian) Craddock Bonebed in Texas, USA. It is the only species of shark present in the Clear Fork Group except for three worn Xenacanthus Beyrich, 1848 occipital spine fragments and two teeth of ?Lissodus (Polyacrodus) zideki (Johnson, 1981) (Hybodontoidei), both being the first occurrences in this unit. Analysis of measurements of teeth with complete bases randomly selected from 3,050 initially available teeth failed to reveal the presence of sexual dimorphism or the discrete presence of juveniles as expected, based on an independent study which identified the presence of Orthacanthus juvenile occipital spines. A few highly symmetrical small teeth are present, which had not been previously observed in the Texas lower Permian. They may be symphyseals and restricted only to juveniles. Other unusual teeth include germinal teeth and deformed teeth, both of which occur in the Clear Fork and underlying Wichita groups. One tooth displays an apparent example of the equivalent of an “enamel pearl” on one of its cusps. The most unusual teeth are those that appear to have undergone various stages of resorption. Only the lingual margin of the base is affected in which the apical button is resorbed to varying degrees until only the labial margin with the basal tubercle and the three cusps are all that remain. If the teeth were undergoing resorption, then the perplexing problem is why the apical button is resorbed and not the superjacent basal tubercle. Other vertebrate remains include palaeoniscoid scales and teeth and unidentified tetrapod bone fragments, jaw fragments, and teeth. Rare fragments of bones (scales?) bear a “comb edge” which have not been previously observed in the Texas lower Permian.
EN
The WalMart section on Ten Mile Creek, Lancaster, Dallas County, Texas, exposes a 23 metre section of Austin Chalk that can be integrated into a more than 60 m composite sequence for the Dallas area on the basis of bed-by-bed correlation. The section was proposed as a possible candidat e Global Boundary Stratotype at the 1995 Brussels meeting on Cretaceous Stage boundaries, with the first occurrence of the inoceramid bivalve Cladoceramus undulatoplicatus (ROEMER, 1852) as the potential boundary marker. An integrated study of the inoceramid bivalves, ammonites, planktonic foraminifera, and calcareous nannofossils places the first occurrence of Cl. undulatoplicatus in a matrix of ten ancillary biostratigraphic markers. The candidate Global boundary Stratotype Section and Point (GSSP) is located within a composite stable carbon isotope curve for the Austin Chalk as a whole. This shows it to lie 3.5 m below the Michel Dean stable carbon isotope event, originally recognised in the English Chalk. The first occurrence of Cl. undulatoplicatus lies in the same position in relation to stable carbon isotope events in both Texas and England that can in principle be recognised globally in marine sediments. The WalMart section satisfies many of the criteria required of a GSSP for the base of the Santonian Stage, although ownership and access require clarification.
11
Content available remote Ctenacanthiform Cladodont Teeth from the Lower PermianWichita Group, Texas, U.S.A.
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EN
Isolated teeth of Glikmanius occidentalis occur in ten vertebrate faunas in the Waggoner Ranch Formation and in one fauna in the underlying Petrolia Formation. They range in size (anteromedial-posterolateral base length) from 1.28 mm to 10.15 mm (n = 12). In addition to the typical teeth, one with an asymmetrical base and one possible posterior tooth (both G. ?occidentalis), and a questionable symphyseal tooth (Glikmanius?), occur in the collection.
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