Note on the Flora of the Highest “Coal Measures” of Warwickshire

1935 ◽  
Vol 72 (12) ◽  
pp. 555-557 ◽  
Author(s):  
Emily Dix

Recently the author has been investigating the sequence of floras and faunas in the Warwickshire Coalfield. In the course of this work particular attention has been given to the flora of the barren Upper Coal Measures, which, according to Eastwood (1923, p. 42), includes the Keele Series and at least 1,700 feet of the Corley or Enville Series. Vernon, on the other hand, placed the latter in the Permian (1912, pp. 590, 603), and he noted that the Corley Series rests unconformably on the underlying Upper Carboniferous strata. Shotton, however, stated (1929, p. 169) that in this area he could see “no evidence for any Permian System (in the sense of System being separated from the Carboniferous by an unreprented time-interval)”.

1929 ◽  
Vol 66 (4) ◽  
pp. 164-177 ◽  
Author(s):  
D. G. Evans ◽  
R. O. Jones

The precise age of the Millstone Grit of South Wales has been in doubt for some years. Although it has been shown to be of Upper Carboniferous age, it has been uncertain whether the whole of the earliest part of the Upper Carboniferous is represented by deposits in southern Britain. Some part of the Millstone Grit of Pembrokeshire has been regarded, on the basis of its flora, as of Middle Coal Measure or Yorkian age (Goode, 1913, p. 272). Similar conclusions have been reached by Dr. R. Crookall concerning part of the Millstone Grit of Somerset (1925, p. 403). As yet, the flora characteristic of the Lanarkian of northern Britain has not been proved to be present in South Wales and elsewhere in south Britain. On the other hand, it has been argued that the absence of a Lanarkian flora does not necessarily imply an important break in the sequence, since recent work on the lamellibranch fauna of various British coalfields points to the conclusion that the lowest part of the Lower Coal Series of South Wales is of approximately the same age as the Lower Coal Measures of northern England (Davies and Trueman, 1927, p. 253).


1913 ◽  
Vol 10 (1) ◽  
pp. 3-7 ◽  
Author(s):  
T. G. Halle

Stems of Ecquisetites columnaris (Brong.) have long been known to occur in a vertical position in the sandstones of the Inferior Oolite on the Yorkshire coast. This mode of occurrence has commonly been held as proving that the stems are preserved in the position in which they once grew, having been buried in situ beneath the layers of sand that accumulated on the spot. On the other hand, it has been argued that the upright position need not be primary; it might be as readily explained if the stems are regarded as drifted and secondarily deposited on the spots where they are now found. It is well known and has been pointed out, particularly in the discussions of the upright stems in the Coal-measures, that a drifting tree often has a tendency to sink in a vertical position, the root-end being heavier because of adhering mineral matter or from some other reason. Phillips describes, in his Geology of the Yorkshire Coast, a locality at High Whitby where upright stems of Equisetites columnaris occur in the sandstone. He continues: “They … are broken off or imperfect above, and seldom reach to the upper surface of the bed; they are also broken off below, but commonly pass to the lower surface; and some of the lower joints nearest the roots are found in the subjacent bed of shale.”


2012 ◽  
Vol 19 (1-2) ◽  
Author(s):  
Zbyněk Šimůnek ◽  
Helena Gilíková ◽  
Kristýna Hrdličková

During the geological mapping in the Boskovice Basin, two new palaeobotanical localities in Veverské Knínice and a locality in Veverská Bítýška have been found. The most abundant flora comes from the Veverské Knínice localities. Conifers dominate in the floral assemblage. Pteridosperms are also relatively common, whereas ferns and sphenopsids are rare. These localities are assignable to the Padochov Formation, Říčany Horizon of the Permian (Rotliegend, Asselian) age. The subsequent Veverská Bítýška Formation belongs still to the Asselian. This formation contains Chudčice Horizon that yields very poor conifer flora at the Veverská Bítýška locality. Permian system is a period of progressing aridity in Moravia. Only fossiliferous horizons represent spans with higher humidity that enabled plants to live. However, the climate was not so humid, but it was rather seasonal, because pure hygrophyte plants lack in the assemblage, on the other hand, “xerophyte” plants, like conifers, dominate here.


1951 ◽  
Vol 3 (1) ◽  
pp. 36-42 ◽  
Author(s):  
Valerie Dees ◽  
G. C. Grindley

Re-examination of the data discussed in previous papers of this series shows a greater tendency toward “overshooting” when the time interval between trials, in some of the experiments, is short than when it is longer. The subject tends to make a bigger movement or exert more pressure with short intervals. This seems to be true with or without visual knowledge of results. On the other hand, with the experiments in which the task was to press a key for a given short interval, the effect was not conclusively shown. A hypothesis is put forward to explain these results in terms of proprioceptive adaptation.


2017 ◽  
Vol 5 (3) ◽  
pp. 272
Author(s):  
Jordi Morell Rovira

The article explores the relationship of the person with the hole through both literal and metaphorical situations. On the one hand, it points up the body in seclusion and suspended in a time interval, as in the case of the accident at the mine in San José (Chile) or works by artists like J. Wall, G. Schneider or R. Ondák. In this way, opposed feelings evoke the experiences of waiting and/or punishment, which are explanatory of a confined body or a hole. Literature, cinema and art deal with these events from multiple aspects, which become existential allegories about the individual. On the other hand, the act of digging gains prominence as a symbol of work, but also of the absurd. Recalling the ambivalence that may suggest a person making a hole, this article carries out a drift through works by artists of different generations and contexts, such as C. Burden, M. Heizer, F. Miralles, Geliti, S. Sierra, F. Alÿs, M. Salum, X. Ristol or N. Güell. A series of clearly performative or conceptual works, where the act of digging, drilling, burying or unburying become common practices that show the diversity of meanings and intentions.


Author(s):  
Konrad A. Szychowski ◽  
Bartosz Skóra ◽  
Anna Kryshchyshyn-Dylevych ◽  
Danylo Kaminskyy ◽  
Kamila Rybczyńska-Tkaczyk ◽  
...  

Abstract4-Thiazolidinones and related derivatives are regarded as privileged structures in medicinal chemistry and a source of new drug-like compounds. To date it is known that thiazolidinones are able to induce CYP1A1 activity in 3T3-L1 cells. Therefore, to extend the knowledge of the mechanism of thiazolidinones in the cell, four chemically synthesized heterocycles were tested on 3T3-L1 cells. The 3T3-L1 cells were exposed to Les-2194, Les-3640, Les-5935, and Les-6166. Our study showed that 1 μM βNF, Les-2194, and Les-6166 decreased the expression of Ahr mRNA. In turn, βNF, Les-2194, and Les-3640 increased the Cyp1a1 mRNA expression at the same time interval. On the other hand, Les-5935 was found to decrease the Cyp1a1 mRNA expression. Interestingly, the expression of Cyp1a2 mRNA was activated only by βNF and Les-2194. The expression of Cyp1b1 mRNA in the 3T3 cell line increased after the βNF and Les-2194 treatment but declined after the exposure to Les-5935 and Les-6166. Moreover, the Les-2194 and Les-5935 compounds were shown to increase the activity of EROD, MROD, and PROD. Les-3640 increased the activity of EROD and decreased the activity of PROD. In turn, the treatment with Les-6166 resulted in an increase in the activity of EROD and a decrease in the activity of MROD and PROD in the 3T3-L1 cells.


1872 ◽  
Vol 162 ◽  
pp. 283-318 ◽  

In the last memoir which I laid before the Royal Society I described a number of forms of Lepidodendroid plants from the Coal-measures, without making any material attempt to ascertain the relationship which they bore to each other. I now propose to carry the subject somewhat further, and to show that some of these apparently varied forms of Lycopodiaceæ merely represent identical or closely allied plants in different stages of their growth. The discovery of some remarkable beds in Burntisland, by George Grieve, Esq., and his persistent kindness in supplying me abundantly with the raw material upon which I could work, have enabled me to do this in a manner, at least, satisfactory to myself. Upon the geology of these remarkable beds I will not now enter, beyond saying that they appear to have been patches of peat belonging to the lower Burdiehouse series, which are now imbedded in masses of volcanic amygdaloid. The stratum, where unaltered by contact with the lava, is little more than a mass of vegetable fragments, the minute structure of most of which is exquisitely preserved. The more perfect remains that are capable of being identified belong to but few types. The most abundant of these are the young twigs of a Lepidodendron , portions of the stem of a Diploxylon , stems of a remarkable Lycopodiaceous plant belonging to my new genus Dictyoxylon (but which, for reasons to be stated in a future memoir, I propose to unite with Corda’s genus Heterangium , under the name of H. Grievii ), and fragments of Stigmaria-ficoides . Along with these occur, but more rarely, several other curious Lycopodiaceous and Fern stems, and those of an articulated plant, which I believe to be an Asterophyllites ; also some true Lepidostrobous fruits and myriads of caudate macrospores belonging to the Lepidostrobi . The first point to be noted is that all the Lepidodendroid branches are young twigs. No one example of a large stem has been found presenting exactly the same structure as these small branches, which, as already stated, are so abundant. On the other hand, all the Diploxylons are large branches or matured stems. These facts at once suggested the inquiry whether the two plants referred to might not be complementary to each other. A careful and very extended study of a large number of specimens has convinced me that such is the case. I have made more than a hundred sections of the two forms, and the result has been a remarkably clear testimony that the Lepidodendra are the twigs and young branches of the Diploxylon -stems. I am also led to the conclusion that the Lepidostrbi , with their peculiar macrospores and microspores, belong to the same plant. I will examine each of these forms in detail.


Author(s):  
Igor Dobeš ◽  
Jan Kuchtík

The aim of our study was to evaluate the effects of chosen factors (crossbreds, sex, litter size, age of ewes and interaction between sex and litter size) on the growth of lambs crossbreds of the breeds Charollais (Ch), Suffolk (Sf) and Improved Valachian (IV). The evaluation was performed in the year 2004 on the farm Růžďka and involved altogether 96 lambs. The growth ability was evaluated at the following crossbreds: Ch x Sf (n = 28), (Ch x Sf) x Sf (n = 28), IV x Sf (n = 21) and (IV x Sf) x Sf (n = 19). All lambs under study were born indoor in January. Lambs were kept indoor till the end of the evaluation. From the evaluation of effects of crossbreds, sex and age of ewes on the live body weights and daily gains of lambs above all result that these factors showed a significant effect only on the live body weight at birth. On the other hand, the factors of litter size and interaction between sex and litter size showed a highly significant (P < 0.01) effect on the live body weights of lambs at birth, at 70 and at 100 days of age as well as on their daily gains within the intervals from birth to 70 and 100 days of age. It can be concluded that the daily gains were highly uniform but relatively low in all crossbreds under the study within the time interval from birth to the age of 100 days, while the non-significantly highest daily gain was recorded in the crossbreds of IV x Sf (211 g). On the other hand the lowest ones were observed in the crossbreds of CH x Sf and (IV x Sf) x Sf (199 g).


2021 ◽  
Vol 2081 (1) ◽  
pp. 012029
Author(s):  
A V Shepelin ◽  
A M Rostom ◽  
V A Tomilin ◽  
L V Il’ichov

Abstract We propose a new model, entitled S-CTC, for description of quantum systems in the presence of CTC – closed time-like curves. The model is based on the viewpoint on any quantum state as an observer’s state of knowledge of the system preparation procedure. We compare and contrast our S-CTC model with D-CTC and P-CTC models and show that S-CTC shares special quantum features with both D-CTC and P-CTC. As far as the interaction of the quantum system with itself coming from the future concerns, S-CTC is formally equivalent to P-CTC. On the other hand, when calculating outcome probabilities for a measurement within the time interval between the entrance and exit of CTC, S-CTC becomes equivalent to D-CTC. Both these models require the concept of alternative realities (worlds) where different measurement outcomes are recorded and alternative connections of these realities by CTC.


1988 ◽  
Vol 27 (04) ◽  
pp. 147-150
Author(s):  
B. Palagi ◽  
F. Villa ◽  
P. Verga ◽  
Angela Broggi ◽  
F. Guzzini ◽  
...  

Impulse synthesis is a technique which relies upon the logic of continuous infusion but extracts the clearance value from single-injection data by shifting and adding them until an asymptotic value is attained. This study has been aimed at validating and optimizing clinically the measurement of glomerular filtration rate by impulse synthesis. A single intravenous injection of 51Cr-EDTA has been made in 32 patients and plasma activity monitored over the next 6 h. Glomerular filtration rate computed by a single-exponential fit method (GFR- SEF) has been shown to be significantly (p <0.001) overestimated when compared with the glomerular filtration rate obtained by the impulse synthesis technique (GFR-IS) in spite of an excellent (r = 0.989) linear correlation between the two sets of data. On the other hand, the comparison between GFR-IS and 24-h creatinine clearance has not shown any significant difference. Moreover, we have found that in patients with severe renal failure GFR-IS is overestimated when the sampling time span is shortened to 3 h. On the other hand, GFR-IS is slightly underestimated in patients with severe renal failure when the convolution time interval is increased over a few minutes.


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