scholarly journals Ronald George Hatton,1886-1965

1966 ◽  
Vol 12 ◽  
pp. 250-258 ◽  

Ronald George Hatton was a distinguished pomologist, an able administrator and a man who won the affection and esteem of his friends and colleagues alike. Ronald was born on 6 July 1886, in Yorkshire, a county for which he always retained a great affection. He was the youngest child of Ernest Hatton who was a barrister of the Inner Temple. Ronald’s mother was Amy Pearson, a woman of forceful character who came from a similar environment, since she was the daughter of William Pearson, also a barrister, who had taken silk. With such legal forebears on both sides of the family it would scarcely have been surprising if their son had followed the law, but perhaps this hereditary influence manifested itself, in later life, in a marked ability for administration and the handling of finance. But, though Ronald’s ancestry was mainly non-scientific, there was one very distinguished scientist on the mother’s side, namely his uncle, Professor Karl Pearson, F.R.S., the famous statistician and author of The grammar of science . The other members of the family were two sisters. The elder of these, Margerie, followed a successful career as a nurse. She became Matron of the Cottage Hospital at Lyme Regis and, later, for a period of thirteen years till the time of her death, was Matron of the hospital at Teignmouth. The younger sister, Dorothy, studied modern languages at Exeter and was indeed the first woman to receive the Batchelor of Arts Degree from the, then newly established, College of the South-West. She next turned her attention to chemistry, though at this time and subsequently, after her marriage, outdoor pursuits always claimed her great interest.

1857 ◽  
Vol 3 ◽  
pp. 294-295
Author(s):  
Robert Harkness

The author remarks that the existence of Annelida during the Palæozoic formations is manifested in two conditions. In the one, we have the shelly envelope which invests the order Tubicola, in the form of Seapolites; and in the other, the tracks of the orders Abranchia and Dorsi-branchiata are found impressed on deposits which were, at one time, in a sufficiently soft state to receive the impressions of the wanderings of these animals.Among the strata which have hitherto afforded annelid tracks, those which, in the county of Clare, represent a portion of the equivalents of the Millstone Grit, contain such tracks, in their most perfect state of preservation in great abundance; and these strata also furnish evidence concerning the circumstances which prevailed during their deposition.


Phytotaxa ◽  
2021 ◽  
Vol 522 (1) ◽  
pp. 27-37
Author(s):  
DANIEL F. BRUNTON ◽  
MICHAEL GARRETT ◽  
PAUL C. SOKOLOFF ◽  
GINTARAS KANTVILAS

Isoetes jarmaniae sp. nov. is described as a new lycophyte endemic to Tasmania, Australia, where it is confined to peat-bound karstic wetlands in several river valleys in the south-west wilderness. While seemingly morphologically closest to I. drummondii, this quillwort has features that are globally uncommon in Isoetes and unknown in other Australasian taxa. Most notable are its markedly flattened, strongly recurved leaves and disproportionately large sporangium ligules that are more suggestive of South American than Australian taxa. As well, the exceptionally thin and wide (alate) megaspore equatorial ridge is swollen at suture intersections, presenting a slightly triangular shape suggestive of the Indian taxon I. udupiensis. The microspores of I. jarmaniae exhibit exceptionally, perhaps uniquely, fine-papillate ornamentation. An original key placing I. jarmaniae in context with the other Tasmanian Isoetes species is provided. This diminutive, apparently diploid species is evidently maintaining a self-sustaining population within a regionally unique habitat and small geographic range.


1981 ◽  
Vol 101 ◽  
pp. 78-86 ◽  
Author(s):  
Harold B. Mattingly

The American excavators in the south-west area of the Forum at Corinth have revealed an intriguing architectural complex, which they have called the ‘Punic Amphora Building’. Evidently it housed a thriving import business with a speciality in fish and wine, whose trade extended in one direction to Sicily and perhaps Spain and in the other to Chalkidike and Chios. Masses of fragments of Punic and Chian amphoras were found crushed and pounded in the make-up of successive floor-levels in the courtyard, together with numerous pieces from Mende and elsewhere. Many others emerged from the single floors of most of the rooms or were discovered in the littered debris from the final phase of occupation. The life of this business house was somewhat short, but a domestic building on the same site had earlier been partly devoted to the same trade. All this activity ceased with dramatic suddenness; the emporium went out of use and in the late fifth century it was overlaid in one area by a new road. The end seems to be securely dated c. 430 B.C. by Attic black-glaze pottery in the final floor-level or in the debris covering the last floor. Professor Williams plausibly links the collapse of business with the interruption of Corinth's trade caused by the outbreak of the Peloponnesian War: one of Athens' first war measures was to blockade both the Saronic and the Corinthian Gulfs. This new material evidence for Corinthian commerce is most welcome in itself and, as I hope to show in this paper, it may help clarify other problems.


2013 ◽  
Vol 33 (2) ◽  
pp. 211-226
Author(s):  
Agni Sesaria Mochtar

Borobudur temple has been famously known as one of the Indonesian heritage masterpiece. Various aspects of it had been studied thoroughly since the beginning of 20th century A.D. Those studies tended to be monumental centric, giving less attention to the cultural context of the temple and its surroundings. Settlement in the nearby places is one of the topics which not have been studied much yet; leaving a big question about how the settlement supported continuity of many activities in the temple, or even the other way around; how the temple affected the settlement. There is only a few data about old settlement found in situ in Borobudur site, only abundance of pottery sherds. The analysis applied on to the potteries find during the 2012 excavation had given some information about the old settlement in Borobodur site. The old settlement predicted as resided in the south west area, in the back side of the monument.


1971 ◽  
Vol 11 (2) ◽  
pp. 87-116 ◽  
Author(s):  
Christopher Clay

The Lords Petre were always one of the most prominent of English Catholic families, and they were also one of the richest. Their landed estates had been built up in the middle of the sixteenth century by Sir William Petre, Secretary of State to three Tudor sovereigns. Sir William's son, John, was created a Baron in 1611, but in the early 17th century the family properties ceased to grow in size, partly because Catholicism excluded them from the profits of office, and partly because provision for younger sons offset such new acquisitions as were made. But even so the estates inherited by the third Lord Petre in 1637 were large enough to place him clearly in the ranks of the great landed magnates. In Essex he had a well-consolidated belt of land lying to the west and south-west of Chelmsford, and centred on the two family residences of Ingatestone Hall and Thorndon Hall. Altogether in Essex Petre had about 11,000 acres of freehold land and the lordship of seventeen manors, and these produced some £5,500 per annum or considerably more than half his total income from land. In addition he had a large estate on the opposite side of the country, in Devon. This lay in two distinct areas, one centred on Axminster and extending down the Axe valley and its tributaries, and the other in the southerly projection of the county on the southern edge of Dartmoor, where the principal possession was the vast moorland manor of South Brent. Besides the main estates in Essex and Devon, there were some isolated properties: the manor of Osmington down on the Dorset coast; Toddenham and Sutton in Gloucestershire; Kennett and Kentford on the Cambridgeshire-Suffolk border.


1989 ◽  
Vol 84 ◽  
pp. 177-185
Author(s):  
R.W.V. Catling ◽  
R.E. Jones

Two vases, a cup and an oinochoe, from Arkesine in south-west Amorgos are published for the first time. It is argued that both are probably Middle Protogeometric, one an import from Euboia, the other from the south-east Aegean; chemical analysis supports both attributions. Their implications for the early history of Amorgos are discussed.


1917 ◽  
Vol 4 (4) ◽  
pp. 150-157 ◽  
Author(s):  
Arthur Holmes ◽  
H. F. Harwood

Almost due west of Mozambique Island, at a distance of about forty-two miles from the sea, the military road from Mosuril to Nampula crosses the Ampwihi River, an important tributary of the Monapo. During the dry season the stream is reduced to a string of stagnant pools, separated by long reaches of sand and gravel that here and there are interrupted by outcrops of the underlying formations. Throughout the greater part of its course the Ampwihi flows through a region in which gneisses persist with monotonous regularity, the only variation being that due to occasional intrusions of granite and of still later pegmatite dykes. At the point where the military road crosses the narrow channel a welcome diversion is introduced by the presence of a dark compact dyke about 10 feet in thickness. The dyke appears on the right-hand bank and crosses obliquely to the other side, taking a N.N.W.–S.S.E. course across the strike of the older rocks. Upstream, about seventy yards to the south-east, the Ampwihi bends to the south-west, so that it returns towards the dyke, which is again exposed across its sandy floor. The dyke was traced by Mr. E. J. Wayland in July, 1911, for a distance of altogether 200 yards, and was examined by Mr. D. Alex. Wray and later by myself during the same year. It is clearly the latest rock of the district, and is intruded along a line of fault, for in two cases pegmatite dykes seen on the eastern side are broken across and reappear on the western side with a well-marked northerly displacement.


1956 ◽  
Vol 4 (1) ◽  
pp. 13 ◽  
Author(s):  
KM Pike

The pollen grains of 300 species of 71 genera of the family Myrtaceae have been examined and their characteristic features summarized in tabular form. The investigation has been mainly concerned with those species that occur in the south-west, Pacific area, particularly Australia. For comparative purposes, the pollen morphology of a limited number of South American and two South African species has been included. The significance of pollen characters for distinguishing genera and species within the family is discussed. In some instances pollen morphology has provided additional evidence for the classification of certain species as suggested by taxonomists. A provisional key to pollen grains of the genera examined has been included.


1953 ◽  
Vol 1 (1) ◽  
pp. 1 ◽  
Author(s):  
HD Ingle ◽  
HE Dadswell

The results reported cover 12 genera of the family Apocynaceae and 12 genera of the Annonaceae. The anatomical features of these genera have been summarized for each family and the results compared with published information on the representatives of the families from other parts of the world. An artificial key has been developed for the separation of groups of genera in the Apocynaceae. This separation, however, does not conform with groupings based on botanical features. Possible affinities of this family have been discussed. In the Annonaceae separation of the genera on anatomical features has been found to be diffcult on account of the homogeneity in wood structure of the family as a whoIe.


1925 ◽  
Vol 3 (3-4) ◽  
pp. 163-166 ◽  
Author(s):  
Thomas W. M. Cameron

In 1923, the writer in studying some species of the family Trichostrongylidæ, had occasion to create a new genus Graphidioides to receive the form previously known as Graphidium affine (Megnin, 1895), Railliet and Henry, 1909. This species differs from the type species of the genus Graphidium on the following points: absence of cervical papillæ, shape of bursa and disposition of ventro-ventral rays, shape of accessory piece and spicules, shape of the ovejectors and vagina and posterior extremity of the female. In an addendum on the remaining species of Graphidium, G. rudicaudatum the following statement was made:—“Graphidium rudicaudatus R. & H., 1909, from Viscacia viscacia from Argentina resembles G. affinis very closely. It differs mainly by its smaller size, equal ovejectors, sharply pointed externo-dorsal ray and absence of an accessory piece. Its affinities to Graphidioides are so close, that the latter point requires re-investigation. The other points are only of specific value, and it is proposed to include it in this new genus. Should the absence of an accessory piece be confirmed, its position would require re-determination.”


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