Ichnology of an Upper Carboniferous fluvio-estuarine paleovalley: The Tonganoxie Sandstone, Buildex Quarry, Eastern Kansas, USA

1998 ◽  
Vol 72 (1) ◽  
pp. 152-180 ◽  
Author(s):  
Luis A. Buatois ◽  
M. Gabriela Mangano ◽  
Christopher G. Maples ◽  
William P. Lanier
Keyword(s):  
Tidal Flats ◽  
Tidal Currents ◽  
Type B ◽  
Upper Carboniferous ◽  
Irregular Networks ◽  
Freshwater Biota ◽  
Taphonomic Analysis ◽  
Proximal Zone

Tidal rhythmites of the Tonganoxie Sandstone Member (Stranger Formation, Douglas Group) at Buildex Quarry, eastern Kansas, contain a relatively diverse ichnofauna. The assemblage includes arthropod locomotion (Dendroidichnites irregulare, Diplichnites gouldi types A and B, Diplopodichnus biformis, Kouphichnium isp., Mirandaichnium famatinense, and Stiaria intermedia), resting (Tonganoxichnus buildexensis) and feeding traces (Stiallia pilosa, Tonganoxichnus ottawensis); grazing traces (Gordia indianaensis, Helminthoidichnites tenuis, Helminthopsis hieroglyphica); feeding structures (Circulichnis montanus, Treptichnus bifurcus, Treptichnus pollardi, irregular networks), fish traces (Undichna britannica, Undichna simplicitas), tetrapod trackways, and root traces. The taxonomy of some of these ichnotaxa is briefly reviewed and emended diagnoses for Gordia indianaensis and Helminthoidichnites tenuis are proposed. Additionally, the combined name Dendroidichnites irregulare is proposed for nested chevron trackways. Traces previously regarded as produced by isopods are reinterpreted as myriapod trackways (D. gouldi type B). Trackways formerly interpreted as limulid crawling and swimming traces are assigned herein to Kouphichnium isp and Dendroidichnites irregulare, respectively.Taphonomic analysis suggests that most grazing and feeding traces were formed before the arthropod trackways and resting traces. Grazing/feeding traces were formed in a soft, probably submerged substrate. Conversely, the majority of trackways and resting traces probably were produced subaerially in a firmer, dewatered and desiccated sediment.The Buildex Quarry ichnofauna records the activity of a terrestrial and freshwater biota. The presence of this assemblage in tidal rhythmites is consistent with deposition on tidal flats in the most proximal zone of the inner estuary, between the maximum landward limit of tidal currents and the salinity limit further towards the sea.

scholarly journals Investigating Permeability of Coal Samples of Various Porosities under Stress Conditions

Energies ◽  
2019 ◽  
Vol 12 (4) ◽  
pp. 762 ◽  
Author(s):  
Mateusz Kudasik
Keyword(s):  
Mechanical Stress ◽  
Permeability Coefficient ◽  
Stress Conditions ◽  
Low Permeability ◽  
Type B ◽  
Upper Carboniferous ◽  
Coal Permeability ◽  
Slippage Effect ◽  
Stress Result ◽  
Change Of Porosity

Among the numerous factors that have an impact on coal permeability, coal porosity is one of the main parameters. A change in the mechanical stress applied to coal results in a change of porosity. The main objective of the conducted research was to answer the following question: is a decline in coal permeability a direct effect of a decrease in coal porosity, and does mechanical stress result solely in a porosity change? A study of coal porosity under mechanical stress conditions was conducted using a uniquely constructed measurement stand. The coal samples used were briquettes prepared from a granular coal material (middle-rank coal of type B—meta bituminous, upper carboniferous formation) from the “Zofiówka” coal mine, in Poland. In order to describe coal permeability, the Klinkenberg equation was used, as it takes into consideration the slippage effect, typical of porous media characterized by low permeability. On the basis of the obtained results, it was established that the values of the Klinkenberg permeability coefficient decrease as the mechanical stress and the corresponding reduction in porosity become greater. As the briquette porosity increased, the Klinkenberg slippage effect: (i) disappeared in the case of nitrogen, (ii) and was minor for methane. The briquettes used were characterized by various porosities and showed that mechanical stress results mainly in a change in coal porosity, which, in turn, reduces coal permeability.

Allostratigraphic and Sedimentologic Applications of Trace Fossils to the Study of Incised Estuarine Valleys

1998 ◽  
pp. 1-27
Author(s):  
Luis A. Buatois ◽  
Gabriela Mangano ◽  
Christopher G. Maples ◽  
William P. Lanier
Keyword(s):  
Sea Level ◽  
Late Carboniferous ◽  
Late Paleozoic ◽  
Incised Valley ◽  
Plant Remains ◽  
Freshwater Biota ◽  
System Tracts ◽  
Proximal Zone ◽  
The U.S ◽  
Glossifungites Ichnofacies

The Tonganoxie Sandstone Member (Stranger Formation) records part of the infill of an estuarine valley system that was incised during a late Missourian (Late Carboniferous) drop in sea level and subsequently infilled during a transgressive episode later in the Virgilian (Late Carboniferous). At Buildex Quarry, in an eastern valley-margin position, this unit is represented by planar-bedded-and-laminated siltstone beds (tidal rhythmites) overlying a coplanar surface of lowstand erosion and subsequent transgression. These tidal rhythmites contain a relatively diverse ichnofauna dominated by arthropod trackways, surface grazing trails, fish traces, and tetrapod tracks, including the ichnogenera Circulichnis Vyalov, Dendroidichnites Demathieu, Gand, and Toutin-Morin, Diplichnites Dawson, Diplopodichnus Brady, Gordia Emmons, Helminthoidichnites Fitch, Helminthopsis Heer, Kouphichnium Nopcsa, Mirandaichnium Aceñolaza, Stiaria Smith, Stiallia Smith, Tonganoxichnus Mángano, Buatois, Maples, and Lanier, Treptichnus Miller, and Undichna Anderson. The Buildex ichnofauna represents a mixture of the nonmarine Scoyenia and Mermia ichnofacies and records the activity of a terrestrial and freshwater biota. Ichnologic evidence, coupled with sedimentologic data, suggests that the Buildex succession was deposited on tidal flats in the most proximal zone of the inner estuary, between the landward limit of tidal currents and the salinity limit further towards the sea. This type of trace-fossil assemblage seems to characterize the lower part of transgressive system tracts, immediately overlying the coplanar surface during the late Paleozoic. As transgression proceeded, tide-influenced freshwater facies tended to be replaced by retrogradational brackish-water parasequences, and the mixed Scoyenia and Mermia ichnofacies was replaced by a Skolithos-impoverished Cruziana ichnofacies. The coplanar surface (flooding surface and sequence boundary) that marks the base of the Tonganoxie sequence at Buildex lacks the substrate-controlled, marine Glossifungites ichnofacies. The coals and paleosols with upright plant remains that typify the coplanar surface at Buildex represent erosional truncation and subsequent omission close to the interfluves and may be regarded as the landward equivalent of the Glossifungites ichnofacies. Buildex-type ichnofaunas probably are widespread in Pennsylvanian tidal rhythmites of the U.S. Midcontinent and may be used to identify freshwater inner estuarine facies, to delineate fluvio-estuarine transitions in incised valley systems, and to refine models based exclusively on lithofacies evidence.

Polished and Striated Mud Surfaces in the St. Lawrence Tidal Flats, Quebec

1974 ◽  
Vol 11 (6) ◽  
pp. 860-866 ◽  
Author(s):  
Jean-Claude Dionne
Keyword(s):  
Shallow Water ◽  
Sedimentary Rocks ◽  
Tidal Flats ◽  
Tidal Currents ◽  
Cold Environment ◽  
Current Direction ◽  
Lawrence Estuary ◽  
St Lawrence Estuary

Drift ice polishes and striates the surface of mud tidal flats along the St. Lawrence Estuary. Drag marks are due to tidal currents dragging ice cakes on the bottom. Striated and polished mud surfaces can be fossilized and preserved. If found in consolidated sedimentary rocks, they would be indicators of: the top of a bed, current direction, shallow water, and a cold environment.

Surficial Physical Sedimentary Structures of Bahia la Choya

1987 ◽  
Vol 2 ◽  
pp. 52-61
Author(s):  
Michael J. Hayes
Keyword(s):  
Tidal Flats ◽  
Tidal Currents ◽  
High Marsh ◽  
Tidal Channel ◽  
Small Current ◽  
Tool Marks ◽  
Sedimentary Structures ◽  
Current Ripples ◽  
Primary Current

I observed and measured the orientations of common physical sedimentary structures on the beach and spit, estero, tidal channel, and inner and outer tidal flats of Bahia la Choya. The spit is characterized by wind ripples and the beach typically displays swash marks. Mudcracks typify the high marsh portions of the estero while the meandering estero channel contains ripples and megaripples. The inner and outer tidal flats are dominated by small, ebb-oriented, straight-crested to undulatory current ripples. The current ripples are often superimposed on flood-oriented ridges and runnels of the outer flat. Rill marks, tool marks, and current crescents occur sporadically. Ebb-oriented megaripples, small current ripples, and primary current lineations occur in the tidal channel.Ripple crests trend from N15E - N40E on the southern tidal flats to N10W - N20W on the northern flats. The crests roughly parallel the shoreline and are normal to tidal currents.

Biological and Morphological Studies on Low-Leukemia-Strain Mice with Hodgkin's-Like Neoplasia Induced by Serial Cell-Free Transmission of Leukemic Organs of SJL/J Strain Mice

1968 ◽  
Vol 26 ◽  
pp. 210-211
Author(s):  
S. Fujinaga ◽  
K. Maruyama ◽  
C.W. Williams ◽  
K. Sekhri ◽  
L. Dmochowski
Keyword(s):  
Tissue Culture ◽  
Type A ◽  
Reticulum Cell ◽  
Type B ◽  
Viral Origin ◽  
Serial Transfer ◽  
Strain Mouse ◽  
Morphological Studies ◽  
Cell Neoplasm ◽  
Free Material

Yumoto and Dmochowski (Cancer Res.27, 2098 (1967)) reported the presence of mature and immature type C leukemia virus particles in leukemic organs and tissues such as lymph nodes, spleen, thymus, liver, and kidneys of SJL/J strain mice with Hodgki's-like disease or reticulum cell neoplasm (type B). In an attempt to ascertain the possibility that this neoplasia may be of viral origin, experiments with induction and transmission of this neoplasm were carried out using cell-free extracts of leukemic organs from an SJL/J strain mouse with spontaneous disease.It has been possible to induce the disease in low-leukemia BALB/c and C3HZB strain mice and serially transfer the neoplasia by cell-free extracts of leukemic organs of these mice. Histological examination revealed the neoplasia to be of either reticulum cell-type A or type B. Serial transfer is now in its fifth passage. In addition leukemic spleen from another SJL/J strain mouse with spontaneous reticulum cell neoplasm (type A) was set up in tissue culture and is now in its 141st serial passage in vitro. Preliminary results indicate that cell-free material of 39th tissue culture passage can reproduce neoplasia in BALB/c mice.

Cryo-electron microscopy of two-dimensional crystals of reduced type B botulinum neurotoxin

1992 ◽  
Vol 50 (1) ◽  
pp. 530-531
Author(s):  
P. F. Flicker ◽  
V.S. Kulkarni ◽  
J. P. Robinson ◽  
G. Stubbs ◽  
B. R. DasGupta
Keyword(s):  
Disulfide Bonds ◽  
Clostridium Botulinum ◽  
Structural Changes ◽  
Two Dimensional ◽  
Type B ◽  
Single Chain ◽  
Muscle Paralysis ◽  
Cryo Electron Microscopy ◽  
Disulfide Linkages ◽  
Intracellular Action

Botulinum toxin is a potent neurotoxin produced by Clostridium botulinum. The toxin inhibits release of neurotransmitter, causing muscle paralysis. There are several serotypes, A to G, all of molecular weight about 150,000. The protein exists as a single chain or or as two chains, with two disulfide linkages. In a recent investigation on intracellular action of neurotoxins it was reported that type B neurotoxin can inhibit the release of Ca++-activated [3H] norepinephrine only if the disulfide bonds are reduced. In order to investigate possible structural changes in the toxin upon reduction of the disulfide bonds, we have prepared two-dimensional crystals of reduced type B neurotoxin. These two-dimensional crystals will be compared with those of the native (unreduced) type B toxin.

Abstract #108: A Case of Type B Insulin Resistance

2004 ◽  
Vol 10 ◽  
pp. 37-38
Author(s):  
Lisa C. Moore ◽  
Archana Sadhu ◽  
Dorothy Martinez ◽  
Robin Kate Kelley
Keyword(s):  
Insulin Resistance ◽  
Type B
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