scholarly journals A more probable explanation for a continuum flash towards a redshift ≈ 11 galaxy

2021 ◽  
Author(s):  
Charles Louis Steinhardt ◽  
Michael I. Andersen ◽  
Gabriel B. Brammer ◽  
Lise Christensen ◽  
Johan P. U. Fynbo ◽  
...  
Keyword(s):  
1989 ◽  
Vol 54 (1) ◽  
pp. 53-63 ◽  
Author(s):  
Roland Meier ◽  
Harald Frank ◽  
Reinhard Kirmse ◽  
Reiner Salzer ◽  
Joachim Stach ◽  
...  

The voltammetric behaviour of amavadine (AV) was found to be considerably different from that of the complexes of VO2+ with methyliminodiacetic acid (MIDA) and iminodiacetic acid (IDA). To get an insight in the rather complicated reduction mechanism of the latter complexes the reductions of V(III) (MIDA) and V(III) (IDA) have been studied for comparison. The species V(III) (MIDA)2 and V(III) (IDA)2 are reduced to the appropriate V(II) complexes in a chemically reversible process. VO(MIDA)2 and VO(IDA)2 are reduced to the same complexes via an ECE mechanism. The investigation of the electroreduction of AV shows that this process is not reversible in the chemical sense. As a probable explanation, the conclusion was drawn that AV and the usual V(IV)O-iminocarboxylato complexes differ in their structures.


The fact that a substance through which Röntgen rays from a focus tube are passing becomes itself a source of secondary Röntgen rays has long- been known. The most probable explanation was given by Prof. Sir J. J. Thomson. If a Röntgen pulse is due to the acceleration of a charged electron, then if the electrons in the atom are free to move under the action of the electromagnetic forces in the wave front of the primary Röntgen pulse, their motion will be accelerated during the passage of the latter through the atom, and they will themselves become sources of secondary Röntgen radiation. Considering only a single electron, the intensity of the secondary radiation at any angle α with the direction of motion will be proportional to sin 2 α . If the primary beam is unpolarised, the motion of the electron may have any direction in the plane at right angles to the primary beam. The intensity of the scattered radiation in the direction θ with the primary beam is thus the mean of all the values of sin 2 α for that direction. It can easily be shown that this is proportional to 1 + cos 2 θ . If I' θ is the intensity of the scattered radiation in the direction θ , we thus have I' θ = I' π /2 (1 + cos 2 θ ).


Paleobiology ◽  
1994 ◽  
Vol 20 (3) ◽  
pp. 362-367 ◽  
Author(s):  
William I. Ausich ◽  
David L. Meyer

Potential hybrid fossil crinoids, Eretmocrinus magnificus x Eretmocrinus praegravis, are identified from the Lower Mississippian Fort Payne Formation of south-central Kentucky. These are the first fossil hybrid crinoids identified, and one of very few examples of hybrids recognized in the fossil record. Eretmocrinus magnificus x E. praegravis specimens have shapes and calyx plate sculpturing that are morphologically intermediate between well-defined, distinct parent species. Suspected hybrids occur at localities where parent species co-occur and where the parent species are the most abundant; the hybrids occur at what may have been the distributional margins of the parent species; and the mixture of characters on suspected hybrids seems to be morphogenetically partitioned. Parent species are derived from separate lineages within Eretmocrinus, and hybridization is the most probable explanation for these morphologically intermediate specimens. This example highlights the need to consider hybridization as a potential interpretation of intermediate morphologies among fossils and raises questions concerning the impact of hybridization for our interpretation of the fossil record and the role of hybridization in the evolutionary process.


1885 ◽  
Vol 2 (4) ◽  
pp. 145-148
Author(s):  
J. Starkie Gardner

In the latest number of the Quarterly Journal of the Geological Society there is a description by Mr. D. Pigeon, F.G.S., of recent discoveries in the submerged Forest of Torbay. The paper is highly interesting, and records many facts, valuable alike to the geologist and archæologist. But the inferences he draws from them in opposition to Mr. Pengelly, though not altogether unchallenged in the discussion of his paper, were not contradicted as emphatically as they might have been. As I take interest in, and have observed signs of upheaval and depression along our coast-line, and believe that scarcely any part of the coast is at rest, I beg leave to protest against this latest of several attempts to show, that remains of forests, now beneath the sea-level, originally grew at the levels they now occupy. We know that it is possible that forests might grow at a lower level than the sea until a protecting dam gave way and they became overwhelmed; but I would ask whether there is any example of such growing anywhere round the coasts of Great Britain to-day, and whether there is anything to lead to the belief that there were, at the epochs of these submerged forests, any physical conditions that rendered it more probable that forests might have grown below high-water mark along the coasts, then than now. To admit that there were, would admit a change of some kind, presumably of level, which is what I maintain. My own idea is that the physiography, of the south coast at least, is entirely opposed to the growth of forests behind dykes below the sea-level, and that the only probable explanation of their present position is a subsidence of the area on which they grew. This seems so self-evident that I should hardly have thought any other view could have been supported. The conclusion I take most particular exception to is this: “That a coast which has remained stationary for the last 2000 years should have made such active use of the preceding twelve or twenty centuries for the purposes of oscillation, is rather hard of belief.” In the first place there is no sort of evidence that the coast was stationary for 2000 years, and in the second, were it so, it would not present any reason to my mind why evidence of the occurrence of oscillations in the 2000 years preceding should be rejected.


2006 ◽  
Vol 453 (3) ◽  
pp. L35-L37 ◽  
Author(s):  
E. A. Dorfi ◽  
A. Gautschy ◽  
H. Saio

2011 ◽  
Vol 16 (1) ◽  
pp. 137-159
Author(s):  
Ülar Ploom

The aim of the present article is to study some aspects of subversive rhetoric in the poetry of Juhan Viiding (1948–1995), one of Estonia’s most admired and cherished poets and actors whose “Complete Poetry” (edited by Hasso Krull) includes texts written between 1968 and 1994, published either in collections (until 1978, under the pseudonym of Jüri Üdi, which translates as George Marrow in English) or separately in newspapers and magazines. It is important to mention that Juhan Viiding often read and sang his texts (accompanied on the piano by Tõnis Rätsep, a friend and colleague from the Estonian Drama Theatre), quite a few of which are recorded on cassette and CD. Üdi/Viiding was and continues to be widely read, quoted, imitated and discussed by his Estonian readers, fellow poets, intellectuals and critics. However, despite the fact that Viiding’s poetry has been translated into sixteen languages, according to Aare Pilv’s “Juhan Viidingu ja Jüri Üdi bibliograafia” (Pilv 2010: 170–175), Viiding has not achieved the sort of fame abroad which he enjoys in Estonia. Indeed, the volume of articles and essays written in Estonian on Viiding’s poetry is not equalled by writing in other languages. Reviews written in English and Russian are mostly by Estonian critics or Russian critics from Estonia (ib. 196–208). Of course, poetry in general does not submit easily to being translated, but in Üdi/Viiding’s case we are dealing with a kind of poetic which makes the process even more complicated, perhaps also partly unachievable. This seems to be the most probable explanation for the asymmetry of Üdi/Viiding’s poetic reputation. So, apart from the peculiar charm of his poetry, with its highly intricate poly-semantic spectrum which calls out for discussion of the organising principles of his texts, I am writing this article in the hope that more foreign critics will take an interest in this exceptional poet and more poets who write in other languages will rise to the challenge of translating his texts or providing their own original pieces of creative writing in Üdi/Viiding’s wake.


1982 ◽  
Vol 14 (1) ◽  
pp. 1-6 ◽  
Author(s):  
J. Richard Udry ◽  
Fred R. Deven ◽  
Samuel J. Coleman

SummaryParallel analyses of recent data from the United States, Thailand, Belgium, and Japan all confirm the finding that female age and not male age is the more important contributor to the decline in frequency of marital intercourse during the childbearing ages. The most probable explanation is the decline in female (but not male) androgen levels during the age span examined.


1983 ◽  
Vol 72 ◽  
pp. 207-210
Author(s):  
V. Piirola ◽  
O. Vilhu ◽  
I. Tuominen

ABSTRACTCircular polarimetry in the red and simultaneous photometric observations in the UBVRI bands during the period June 1-3, 1981, are discussed. The peak value of negative circular polarization PV ~ -15 % is stronger than observed in 1976-79. Variations in the shape of the polarization and light curves occur from night to night. The positive crossover and reversal of the sign of the circular polarization are only marginal. A probable explanation of the short term variations seems to be the changing shape and position of the accretion columns with respect to the magnetic axis


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