I.—The Ancient Life-History of the Earth. A Comprehensive Outline of the Principles and Leading Facts of Palæontological Science. By H. Alleyne Nicholson, M.D., D.Sc., M.A., etc., Professor of Nat. Hist. in the University of St. Andrews. 8vo., pp. xvi. and 407, and 276 woodcuts. (Edinburgh and London, W. Blackwood and Son.)

1877 ◽  
Vol 4 (5) ◽  
pp. 222-225
1887 ◽  
Vol 42 (251-257) ◽  
pp. 308-310

Dr. Alleyne Nicholson, a palæontologist of no small repute, refers to this subject in his work on the ‘ Ancient Life History of the Earth,’ p. 34. He considers that the silica which has surrounded and infiltrated the fossils which flint contains, must have been deposited “from sea-water in a gelatinous condition, and subsequently have hardened.” Also that “the formation of flint may therefore be regarded as due to the separation of silica from sea-water, and its deposition round some organic body in a state of chemical change or decay.”


Parasitology ◽  
1963 ◽  
Vol 53 (1-2) ◽  
pp. 201-215 ◽  
Author(s):  
Gwendolen Rees

1. A plerocercoid of ‘Acanthotaenia’ has been found in large numbers in ‘cysts’ in the pancreas of Rana occipitalis (Günther) in Ghana.2. ‘Cysts’ containing plerocercoids were fed to Varanus niloticus (L.). Adults of Proteocephalus niloticus (Beddard) were recovered from the intestine 3 weeks later.3. It is suggested that the life cycle involves three hosts, the first being a copepod.4. The morphology of the larva and adult is described.I wish to express my sincere gratitude to the authorities of the University of Ghana for inviting me to spend some time in the Zoology Department there. I am most grateful, also, to Professor R. D. Purchon for his kindly interest and for the facilities which he placed at my disposal. It is a pleasure to thank Dr J. D. Thomas and the technical staff for their assistance in the collection of material.


2020 ◽  
Vol 69 ◽  
pp. 109-131
Author(s):  
R. W. Ogden

Peter Chadwick studied mathematics as an undergraduate at the University of Manchester, graduating with first-class honours in 1952, from where he moved to Cambridge and completed a PhD on the thermal history of the Earth in the Department of Geodesy and Geophysics under the supervision of Dr Robert Stoneley. His research then developed to focus primarily on the propagation of waves, and he made a major contribution to the mathematical theory of elastic wave propagation and became a world-leading authority in this area. He also made fundamental advances in the modelling of the thermo-elastic properties of rubberlike materials. At the University of East Anglia, where he was a professor for 26 years, he was the driving force behind the development of a research group in theoretical mechanics in the School of Mathematics and Physics, leading by example and supporting and encouraging fellow faculty members, especially the younger staff, academic visitors and students. He gave considerable service to the University of East Anglia in a number of capacities, including a period as Dean of the School, and to the scientific community, through substantial journal editorial activities and as a member of several national and international committees.


PEDIATRICS ◽  
1964 ◽  
Vol 33 (5) ◽  
pp. 805-805
Author(s):  
CLEMENT A. SMITH

For the pediatrician curious enough to pursue the life history of his patient into its prenatal phase or the obstetrician interested in more than one of his two patients, this small book will be of great usefulness. Of the twenty-one chapters, twelve are by Australian or New Zealand workers, the Editor, a Professor of Obstetrics and Gynaecology at the University of New South Wales, among them. The international flavor is augmented by Swedish, German, and Scottish contributors.


Author(s):  
John J. W. Rogers ◽  
M. Santosh

Alfred Wegener never set out to be a geologist. With an education in meteorology and astronomy, his career seemed clear when he was appointed Lecturer in those subjects at the University of Marburg, Germany. It wasn’t until 1912, when Wegener was 32, that he published a paper titled “Die Entstehung der Kontinente” (The origin of the continents) in a recently founded journal called Geologische Rundschau. This meteorologist had just fired the opening shot in a revolution that would change the way that geologists thought about the earth. In a series of publications and talks both before and after World War I, Wegener pressed the idea that continents moved around the earth independently of each other and that the present continents resulted from the splitting of a large landmass (we now call it a “supercontinent”) that previously contained all of the world’s continents. After splitting, they moved to their current positions, closing oceans in front of them and opening new oceans behind them. Wegener and his supporters referred to this process as “continental drift.” The proposal that continents moved around the earth led to a series of investigations and ideas that occupied much of the 20th century. They are now grouped as a set of concepts known as “plate tectonics.” We begin this chapter with an investigation of the history of this development, starting with ideas that preceded Wegener’s proposal. This is followed by a section that describes the reactions of different geologists to the idea of continental drift, including some comments that demonstrate the rancorous nature of the debate. The next section discusses developments between Wegener’s proposal and 1960, when Harry Hess suggested that the history of modern ocean basins is consistent with the concept of drifting continents. We finish the chapter with a brief description of seafloor spreading and leave a survey of plate tectonics to chapter 2. Although Wegener is credited with first proposing continental drift, some tenuous suggestions had already been made. We summarize some of this early history from LeGrand (1988).


1877 ◽  
Vol 4 (11) ◽  
pp. 481-496
Author(s):  
Searles V. Wood

From no part of the world have we of late years derived more additions to the Geological Record than from North America. Besides important additions to the earliest pages of that record, the rich collections made by the United States Surveyors, both of fauna and flora, from the Cretaceous, Eocene, and Miocene deposits, have thrown much light upon the life history of the Earth; and it is even contended that they have bridged over the interval which, notwithstanding the Maestricht beds, the Pisolitic, and the Faxoe Limestones, still remains sharply marked between the Cretaceous and Tertiary formations of Europe so far as they have yet been examined.


2013 ◽  
Vol 16 ◽  
pp. 63-72 ◽  
Author(s):  
G. S. Soreghan ◽  
A. S. Cohen

Abstract. A US National Science Foundation-funded workshop occurred 17–19 May 2013 at the University of Oklahoma to stimulate research using continental scientific drilling to explore earth's sedimentary, paleobiological and biogeochemical record. Participants submitted 3-page "pre-proposals" to highlight projects that envisioned using drill-core studies to address scientific issues in paleobiology, paleoclimatology, stratigraphy and biogeochemistry, and to identify locations where key questions can best be addressed. The workshop was also intended to encourage US scientists to take advantage of the exceptional capacity of unweathered, continuous core records to answer important questions in the history of earth's sedimentary, biogeochemical and paleobiologic systems. Introductory talks on drilling and coring methods, plus best practices in core handling and curation, opened the workshop to enable all to understand the opportunities and challenges presented by scientific drilling. Participants worked in thematic breakout sessions to consider questions to be addressed using drill cores related to glacial–interglacial and icehouse–greenhouse transitions, records of evolutionary events and extinctions, records of major biogeochemical events in the oceans, reorganization of earth's atmosphere, Lagerstätte and exceptional fossil biota, records of vegetation–landscape change, and special sampling requirements, contamination, and coring tool concerns for paleobiology, geochemistry, geochronology, and stratigraphy–sedimentology studies. Closing discussions at the workshop focused on the role drilling can play in studying overarching science questions about the evolution of the earth system. The key theme, holding the most impact in terms of societal relevance, is understanding how climate transitions have driven biotic change, and the role of pristine, stratigraphically continuous cores in advancing our understanding of this linkage. Scientific drilling, and particularly drilling applied to continental targets, provides unique opportunities to obtain continuous and unaltered material for increasingly sophisticated analyses, tapping the entire geologic record (extending through the Archean), and probing the full dynamic range of climate change and its impact on biotic history.


1902 ◽  
Vol 34 (8) ◽  
pp. 214-216
Author(s):  
Richard. F. Pearsall

Full-grown larvæ were taken on wild cherry (Prunus) in the latter part of September, 1901. Placed in a box over earth, they fed but a day or two, truned a deep green, and entering the earth two to three inches, formed rounded cells, in which they remained as larvæ all winter, transforming to pupæ just before emergence. They are gregarious, remaining in their web, filled with its mass of exuvia, untill full-grown, when, as their growth is completed, individually they drop from it and enter the ground. One which was kept under observation formed a pupa on April 28th, and emerged eight days thereafter. The pupal skin is very thin, showing distictly the parts of the enclosed imago. This brood commenced emerging April 25th, and a few individuals are still coming out, May 31st. In the eariler days the males predominated, later the females, Altogether, 134 males and 123 females have appeared. Copulation took place at once, the pair remaining in coitu from three to five hours.


2019 ◽  
Vol 10 (1) ◽  
Author(s):  
Aji Wicaksosno

Abstract - This study aimed to examine the interest of tourists at the HM General Memorial Museum. Suharto in Bantul Regency. This study employed descriptive qualitativemethodand the data were collected through interview, observation, literature studies, and documentation. Interview wascarried outwith managers and visitors (public peopleand students). The data analyzed using Miles Hubberman's qualitative descriptive analysis coveringdata reduction, data presentation, and drawing conclusion . The results showed that the interest of tourists at the HM General Memorial Museum Soeharto was quite high. In addition to that,the interest of the vast majority ofthe students who visited the HM General Memorial Museum. Soeharto was to conduct a study tour and find out the life history of the Great General HM. Suharto, while the personal interest of the university studentswas to find out information about the life history of the Great General HM. Suharto and gather with fellow students to just discuss and enjoy wifi facilities. The interest of the public peoplewasto reminisceaboutthe late Great General HM. Suharto. Visitors werealso interested coming to the HM General Memorial Museum. Suharto for recreation and gathering with friends and family.Moreover, they enjoyed adequate facilities available, of museum’s collections which were diverse and packaged in a modern way, as well as the historical elements related to Soeharto's life that invited visitors to be curious while providing education for visitors. Visitors also showed social interest when they visited to the HM General Memorial Museum. Soeharto either gathering with family and friends or participating in various community activities such as commemorating national holidays and participating in competitions, gymnastics and others. Keywords: Soeharto museum, tourism, tourist interest Abstract - Penelitian ini bertujuan untuk mengkaji minat wisatawan di Museum Memorial Jenderal Besar HM. Soeharto di Kabupaten Bantul. Metode dalam penelitian ini yaitu deskriptif kualitatif dengan pengumpulan data melalui wawancara, observasi, studi pustaka, dan dokumentasi. Wawancara dilakukan kepada pengelola dan pengunjung (umum, pelajar, dan mahasiswa). Analisis data menggunakan analisis deskriptif kualitatif Miles Hubberman yaitu reduksi data, penyajian data, dan penarikan kesimpulan. Hasil penelitian menunjukkan bahwa minat wisatawan di Museum Memorial Jenderal Besar HM. Soeharto cukup tinggi, Minat pribadi pelajar yang mengunjungi Museum Memorial Jenderal Besar HM. Soeharto umumnya adalah untuk melakukan study tour serta mengetahui sejarah kehidupan Jenderal Besar HM. Soeharto, sedangkan minat pribadi mahasiswa adalah untuk mengetahui informasi tentang sejarah kehidupan Jenderal Besar HM. Soeharto serta berkumpul dengan rekan-rekan sesama mahasiswa untuk berdiskusi maupun menikmati fasilitas wifi. Minat pribadi masyarakat umum adalah bernostalgia dengan mendiang Jenderal Besar HM. Soeharto. Pengunjung juga berminat datang ke Museum Memorial Jenderal Besar HM. Soeharto untuk berekreasi dan berkumpul bersama teman dan keluarga sambil memanfaatkan beragam fasilitas yang cukup memadai. Adanya koleksi museum yang beragam dan dikemas secara modern, serta adanya unsur historis terkait kehidupan Jenderal Besar HM. Soeharto yang mengundang rasa penasaran pengunjung sekaligus memberikan edukasi bagi pengunjung. Pengunjung juga menunjukkan minat sosial ketika datang ke Museum Memorial Jenderal Besar HM. Soeharto baik sekedar berkumpul dengan keluarga dan teman maupun mengikuti berbagai kegiatan komunitas seperti memperingati hari besar nasional maupun mengikuti kegiatan lomba, senam dan lain-lain. Kata kunci: museum soeharto, pariwisata, minat wisatawan


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