VI.—New Devonian Fossils from Cornwall

1912 ◽  
Vol 9 (2) ◽  
pp. 82-84
Author(s):  
Ivor Thomas
Keyword(s):  
Geological Survey ◽  
Short Time

A Short time ago a Devonian fossil of considerable interest was found in the grits of the Ladock neighbourhood. It had been found by a workman in a road-heap on the Grampound Road and was placed for preservation in the Truro Museum. A cast was kindly made by Mr. C. Davies Sherborn and presented to the Museum of Practical Geology [22466]. This fossil was named Orthis sp., and is referred to as such in the Memoir of the Geological Survey on the geology of the country near Newquay (p. 35).

scholarly journals IV.—On the Discovery of a Skeleton of the Hippopotamus in Post-pliocene Drift near Motcomb, Dorset

1869 ◽  
Vol 6 (59) ◽  
pp. 206-208
Author(s):  
T. Thompson
Keyword(s):  
Thin Section ◽  
Geological Survey ◽  
Green Sand ◽  
Weak State ◽  
Small Section ◽  
Short Time ◽  
Bison Priscus ◽  
Horn Core ◽  
Leg Bones

The existence of Post-pliocene deposits in this neighbourhood has until lately been quite unknown, nothing of the kind having been detected either by the Geological Survey or subsequent observers. However, in tlie winter of 1866, a small section was exposed in a brick-field situated on a low rising-ground at the first milestone out of Shaftesbtiry towards Gillingham, and known as Hawkers' Hill. The clay here dug for brickmaking is Kimmeridge, presenting fossilized bones of the Pliosaurus and Icthyosaurus, and very friable remains of an Ammonite, etc. The attention of the writer was first attracted to the Drift on observing, above part of the Kimmeridge clay, a thin section of soil of an ochreous tint due to oxide of iron, and somewhat resembling the loose stratum of chert and sand which caps the neighbouring Green-sand rock. He learnt on inquiring of the labourers that they had recently found some large bones in this deposit, but thinking them of no use they had wheeled them off with the rubbish, in which they then lay, efiectually re-buried. Much interested at this announcement, he induced the men again to remove the rubbish, and found that the bones were some vertebræ of a large mammalian animal, together with fragments of the ribs and leg-bones. They were, of course, not at all fossilized, and their original weak state had been sadly aggravated by a second burial and disinterment. Nothing more was turned out that winter, and it was not until the end of 1867, that digging was resumed. Further portions of the same skeleton were now found, including another instalment of vertebræ, and portions of the skull and jaws. With the latter were several teeth in a suffciently entire state to show that the creature weis undoubtedly a Hippopotamus; numerous fragments of the tusks affording further proof of this. The writer now frequently visited and watched “the diggings,” and after a short time two horn-cores, considerable portions of the skull, and some fragments of the leg-bones of Bison priscus of unusual size came to light. The more perfect horn-core is 18 inches long and 14: inches in diameter at the base.

scholarly journals Finlay Lorimer Kitchin, 1870-1934

1934 ◽  
Vol 1 (3) ◽  
pp. 349-352
Keyword(s):  
Natural History ◽  
British Museum ◽  
Geological Survey ◽  
Specialized Training ◽  
University Of Munich ◽  
The University ◽  
Short Time

Finlay Lorimer Kitchin, the son of William Henry Kitchin, was born at Whitehaven on December 13, 1870. He was educated at St. Bees School and at St. John’s College, Cambridge, where he spent four years (1890-1894), the last year being devoted entirely to the study of Geology and Palaeontology. Soon after leaving Cambridge he proceeded to the University of Munich, where he commenced research in palaeontology under the direction of Zittel, and graduated Ph.D. summa cum laude in 1897. In after years Kitchin valued equally the broad outlook which he gained in Cambridge and the more specialized training which he received in Munich. After working for a short time unofficially in the British Museum (Natural History) he was appointed Assistant Palaeontologist to the Geological Survey in 1898, and in 1905 he succeeded the late E. T. Newton as Palaeontologist—a post previously held by Edward Forbes, T. H. Huxley, J. W. Salter, and R. Etheridge.

John Smith Flett, 1869-1947

1948 ◽  
Vol 5 (16) ◽  
pp. 688-696
Keyword(s):  
Medical Practice ◽  
Natural Science ◽  
Academic Career ◽  
Transitional Period ◽  
Geological Survey ◽  
Small Island ◽  
Geological Museum ◽  
University Of Edinburgh ◽  
The University ◽  
Short Time

John Smith Flett, who died on 26 January 1947, at the age of seventy-seven, has left an abiding mark on British geology, both as a scientific investigator and as an official administrator. His scientific contributions dealt mainly with petrography and many of them were necessarily of a routine and official character. His greatest services to his science were undoubtedly those given during his fifteen years as Director of His Majesty’s Geological Survey. In the unsettled and transitional period between the wars, it was indeed fortunate for the Survey and for geology that a man of Flett’s stamp—in intellect keen and acute, in character resolute and virile—should be at the helm. Under his guidance there arose the magnificent Geological Museum at South Kensington —a monument to a vision persistently followed. When we contemplate the outstanding part that the geologists of this small island have played in the foundation and evolution of their science, we must rejoice that at last an exhibition worthy of that record can be made. Flett was born in Kirkwall, Orkney, and received his early education at the Burgh School of that town. He passed to George Watson’s College, Edinburgh, and thence to the University of Edinburgh, where he graduated M.A., B.Sc. (with honours in Natural Science), in 1892 and M.B., C.M., in 1894. During his academic career he gained an extraordinary variety of prizes, medals and scholarships. This was no ephemeral brilliance or inclination, and he maintained an interest in subjects outside his professional orbit all his life; he was especially attracted to literature of a somewhat caustic or satiric cast. After graduation, Flett was for a short time in medical practice but, in 1895, he forsook that career and turned himself for good to geology.

Notes on the Archaeology of the Utukok River, Northwestern Alaska

1948 ◽  
Vol 14 (1) ◽  
pp. 62-65 ◽  
Author(s):  
Raymond M. Thompson
Keyword(s):  
United States ◽  
Arctic Ocean ◽  
Geological Survey ◽  
The Arctic ◽  
Archaeological Sites ◽  
United States Geological Survey ◽  
The Arctic Ocean ◽  
Important Exception ◽  
Short Time ◽  
Working Out

Early in May 1947, a United States Geological Survey field party of five was flown by ski plane to the headwaters of the Utukok River in northwestern Alaska, about 200 miles southwest of Barrow. Three 18–foot canvas boats of a special folding design were taken in along with enough equipment for four months. Food caches had been flown in to six localities on the 200–mile–long river a short time before the group landed. When the “break–up” came late in May the party started down the river working out the geology of the area from a series of 18 camps which were established before reaching the Arctic Ocean in August.During the season 17 archaeological sites were discovered. It is believed that most of these sites are of Eskimo origin and are probably fairly recent. However, an important exception is a well–made Folsom point, announcement of which has been made.

What the replication reformation wrought

2018 ◽  
Vol 41 ◽  
Author(s):  
Barbara A. Spellman ◽  
Daniel Kahneman
Keyword(s):  
Reform Movement ◽  
Short Time

AbstractReplication failures were among the triggers of a reform movement which, in a very short time, has been enormously useful in raising standards and improving methods. As a result, the massive multilab multi-experiment replication projects have served their purpose and will die out. We describe other types of replications – both friendly and adversarial – that should continue to be beneficial.

Periodic Variations in the Coronal Green Line Intensity and their Connection with the White-light Coronal Structures

2000 ◽  
Vol 179 ◽  
pp. 197-200
Author(s):  
Milan Minarovjech ◽  
Milan Rybanský ◽  
Vojtech Rušin
Keyword(s):  
Time Resolution ◽  
White Light ◽  
Short Time Scale ◽  
High Time Resolution ◽  
Green Line ◽  
Periodic Intensity ◽  
Coronal Green Line ◽  
Significant Intensity ◽  
Short Time ◽  
Coronal Structures

AbstractWe present an analysis of short time-scale intensity variations in the coronal green line as obtained with high time resolution observations. The observed data can be divided into two groups. The first one shows periodic intensity variations with a period of 5 min. the second one does not show any significant intensity variations. We studied the relation between regions of coronal intensity oscillations and the shape of white-light coronal structures. We found that the coronal green-line oscillations occur mainly in regions where open white-light coronal structures are located.

Destruction of Actin Filaments by Osmium Tetroxide

1977 ◽  
Vol 35 ◽  
pp. 466-467
Author(s):  
P. Maupin-Szamier ◽  
T. D. Pollard
Keyword(s):  
Actin Filaments ◽  
Time Course ◽  
Osmium Tetroxide ◽  
Rabbit Muscle ◽  
Muscle Actin ◽  
Sodium Phosphate Buffer ◽  
Transmission Electron ◽  
The Difference ◽  
Rates Of Decay ◽  
Short Time

We have studied the destruction of rabbit muscle actin filaments by osmium tetroxide (OSO4) to develop methods which will preserve the structure of actin filaments during preparation for transmission electron microscopy.Negatively stained F-actin, which appears as smooth, gently curved filaments in control samples (Fig. 1a), acquire an angular, distorted profile and break into progressively shorter pieces after exposure to OSO4 (Fig. 1b,c). We followed the time course of the reaction with viscometry since it is a simple, quantitative method to assess filament integrity. The difference in rates of decay in viscosity of polymerized actin solutions after the addition of four concentrations of OSO4 is illustrated in Fig. 2. Viscometry indicated that the rate of actin filament destruction is also dependent upon temperature, buffer type, buffer concentration, and pH, and requires the continued presence of OSO4. The conditions most favorable to filament preservation are fixation in a low concentration of OSO4 for a short time at 0°C in 100mM sodium phosphate buffer, pH 6.0.

Effect of a Complex Heat Treatment on the Structure of 300M Steel

1981 ◽  
Vol 39 ◽  
pp. 312-313
Author(s):  
R. Padmanabhan ◽  
W. E. Wood
Keyword(s):  
Heat Treatment ◽  
Metal Carbides ◽  
Austenite Grain Size ◽  
300M Steel ◽  
Heat Treated ◽  
Strain Fracture ◽  
Prior Austenite Grain Size ◽  
Short Time ◽  
Final Tempering ◽  
Similar Yield

Intermediate high temperature tempering prior to subsequent reaustenitization has been shown to double the plane strain fracture toughness as compared to conventionally heat treated UHSLA steels, at similar yield strength levels. The precipitation (during tempering) of metal carbides and their subsequent partial redissolution and refinement (during reaustenitization), in addition to the reduction in the prior austenite grain size during the cycling operation have all been suggested to contribute to the observed improvement in the mechanical properties. In this investigation, 300M steel was initially austenitized at 1143°K and then subjected to intermediate tempering at 923°K for 1 hr. before reaustenitizing at 1123°K for a short time and final tempering at 583°K. The changes in the microstructure responsible for the improvement in the properties have been studied and compared with conventionally heat treated steel. Fig. 1 shows interlath films of retained austenite produced during conventionally heat treatment.

Transmission Electron Microscopy of an Aluminum-Silver-Stainless Steel Solid State Bond

1985 ◽  
Vol 43 ◽  
pp. 172-173
Author(s):  
M. J. Carr ◽  
J. F. Shewbridge ◽  
T. O. Wilford
Keyword(s):  
Electron Microscopy ◽  
Transmission Electron Microscopy ◽  
Solid State ◽  
Specimen Preparation ◽  
Dimensional Control ◽  
Tem Analysis ◽  
Metal Parts ◽  
Dissimilar Metal ◽  
Transmission Electron ◽  
Short Time

Strong solid state bonds are routinely produced between physical vapor deposited (PVD) silver coatings deposited on sputter cleaned surfaces of two dissimilar metal parts. The low temperature (200°C) and short time (10 min) used in the bonding cycle are advantageous from the standpoint of productivity and dimensional control. These conditions unfortunately produce no microstructural changes at or near the interface that are detectable by optical, SEM, or microprobe examination. Microstructural problems arising at these interfaces could therefore easily go undetected by these techniques. TEM analysis has not been previously applied to this problem because of the difficulty in specimen preparation. The purpose of this paper is to describe our technique for preparing specimens from solid state bonds and to present our initial observations of the microstructural details of such bonds.

Electronmicroscopic localization of ribonucleic acids in ciliate Bursaria truncatella during cell division

1990 ◽  
Vol 48 (3) ◽  
pp. 132-133
Author(s):  
Vladimir Popenko ◽  
Natalya Cherny ◽  
Maria Yakovleva
Keyword(s):  
Cell Division ◽  
High Specificity ◽  
Longitudinal Axis ◽  
Gold Complexes ◽  
Somatic Nucleus ◽  
Ribonucleic Acids ◽  
Biological Meaning ◽  
Bivalent Cations ◽  
Lowicryl K4m ◽  
Short Time

Highly polyploid somatic nucleus (macronucleus) of ciliate Bursaria truncatella under goes severe changes in morphology during cell division. At first, macronucleus (Ma) condences, diminishes in size and turns perpendicular to longitudinal axis of the cell. After short time, Ma turns again, elongates and only afterwards the process of division itself occurs. The biological meaning of these phenomena is not clear.Localization of RNA in the cells was performed on sections of ciliates B. truncatella, embedded in “Lowicryl K4M” at various stages: (1) before cell division (Figs. 2,3); (11) at the stage of macronucleus condensation; (111) during elongation of Ma (Fig.4); (1111) in young cells (0-5min. after division). For cytochemical labelling we used RNaseAcolloidal gold complexes (RNase-Au), which are known to bind to RNA containing cell ularstructures with high specificity. The influence of different parameters on the reliability and reproducibility of labelling was studied. In addition to the factors, discussed elsewhere, we found that the balance of mono- and bivalent cations is of great significance.

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