Alcide D'orbigny, His Life and His Work
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Attempt on Magnification of the Mechanism of Enzyme Catalyzed Reaction Through Bio-Geometric Model for the Five Points Circle In
International Journal of Emerging Scientific Research 1 (2020) 1 – 19 International Journal of Emerging Scientific Research (IJESR) Journal homepage: www.sciengtexopen.org/index.php/ijesr Attempt on Magnification of the Mechanism of Enzyme Catalyzed Reaction through Bio-geometric Model for the Five Points Circle in the Triangular Form of Lineweaver-Burk Plot a, b, c, d Vitthalrao Bhimasha Khyade , Avram Hershko a Sericulture Unit, Malegaon Sheti Farm, Agricultural Development Trust Baramati, Shardanagar, Maharashtra, India b Department of Zoology, Shardabai Pawar Mahila Mahavidyalaya, Shardanagar Tal. Baramati Dist. Pune – 413115, India c Dr. APIS, Shrikrupa Residence, Teachers Society, Malegaon Colony (Baramati) Dist. Pune – 413115, India d Unit of Biochemistry, The B. Rappaport Faculty of Medicine, and the Rappaport Institute for Research in the Medical Sciences, Technion-Israel Institute of Technology, Haifa 31096, Israel Authors’ Contributions This work was carried out in collaboration between all authors. V. B. Khyade carried out the research work, supervised by A. Hershko. Both authors (V. B. Khyade and A. Hershko) performed statistical analysis. Revision of the manuscript as well as corrections were made and approved by both authors. ARTICLE INFO ABSTRACT Article history: The bio-geometrical model is dealing with correlation between the “five events for Received 26 August 2020 enzyme catalyzed reaction” and “triple point event serving groups on the circle” in Received in revised form 23 September 2020 triangle obtained for the graphical presentation of the double reciprocal for magnification of the mechanism of enzyme catalyzed reaction. This model is based on Accepted 22 October 2020 the nine point circle in triangle of the double reciprocal plot. -
From the Gulf of Alaska and Southeastern Alaska
Recent Foraminifera From the Gulf of Alaska And Southeastern Alaska By RUTH TODD and DORIS LOW CONTRIBUTIONS TO PALEONTOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 573-A A study resulting from a search for evidence that Pamplona Searidge is the foundered remnant of the 18th century "Pamplona Rock" UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 55 cents (paper cover) CONTENTS Page A18 18 2 1 21 2 1 2 5 26 3 0 31 3 3 34 3 5 35 36 38 38 38 39 39 39 4 0 4 3 ILLUSTRATIONS [Plates 1-5 follow index] PLATE 1. Recent arenaceous Foraminifera from Alaska. 2. Recent arenaceous and porcellaneous Foraminifera from Alaska. 3. Recent Lagenidae, Polymorphinidae, and Buliminidae from Alaska. 4. Recent Buliminidae, Elphidiidae, Discorbidae, and Rotaliidae from Alaska. 5. Recent miscellaneous benthonic and planktonic Foraminifera from Alaska. FIGURE1. Map of Gldf of Alaska and southeastern Alaska showing locution of dredged samples- _._ _ _ A3 TABLES Page TABLE1. List of stations and locality data for Foraminifera samples- _ _._ _ _ _ . A2 2. Distribution and abundance of Iiecent Foraminifera off Alaska. _._ _. - _ _ 4 CONTRIBUTIONS TO PALEONTOLOGY RECENT FORAMINIFERA FROM THE GULF OF ALASKA AND SOUTHEASTERN ALASKA By RUTHTODD and DORISLOW ABSTRACT / In each of these places numerous species were found in common Pamplona Searidge is a northeast-trending submarine ridge, with the present assemblages. -
Emplacement of the Jurassic Mirdita Ophiolites (Southern Albania): Evidence from Associated Clastic and Carbonate Sediments
Int J Earth Sci (Geol Rundsch) (2012) 101:1535–1558 DOI 10.1007/s00531-010-0603-5 ORIGINAL PAPER Emplacement of the Jurassic Mirdita ophiolites (southern Albania): evidence from associated clastic and carbonate sediments Alastair H. F. Robertson • Corina Ionescu • Volker Hoeck • Friedrich Koller • Kujtim Onuzi • Ioan I. Bucur • Dashamir Ghega Received: 9 March 2010 / Accepted: 15 September 2010 / Published online: 11 November 2010 Ó Springer-Verlag 2010 Abstract Sedimentology can shed light on the emplace- bearing pelagic carbonates of latest (?) Jurassic-Berrasian ment of oceanic lithosphere (i.e. ophiolites) onto continental age. Similar calpionellid limestones elsewhere (N Albania; crust and post-emplacement settings. An example chosen N Greece) post-date the regional ophiolite emplacement. At here is the well-exposed Jurassic Mirdita ophiolite in one locality in S Albania (Voskopoja), calpionellid lime- southern Albania. Successions studied in five different stones are gradationally underlain by thick ophiolite-derived ophiolitic massifs (Voskopoja, Luniku, Shpati, Rehove and breccias (containing both ultramafic and mafic clasts) that Morava) document variable depositional processes and were derived by mass wasting of subaqueous fault scarps palaeoenvironments in the light of evidence from compara- during or soon after the latest stages of ophiolite emplace- ble settings elsewhere (e.g. N Albania; N Greece). Ophiolitic ment. An intercalation of serpentinite-rich debris flows at extrusive rocks (pillow basalts and lava breccias) locally this locality is indicative of mobilisation of hydrated oceanic retain an intact cover of oceanic radiolarian chert (in the ultramafic rocks. Some of the ophiolite-derived conglom- Shpati massif). Elsewhere, ophiolite-derived clastics typi- erates (e.g. -
HEADLINE NEWS • 6/23/09 • PAGE 2 of 8
EADLINE H Battle for Ky NEWS Slots For information about TDN, See page 2 call 732-747-8060. www.thoroughbreddailynews.com TUESDAY, JUNE 23, 2009 RACHEL WORKS HALF FOR MOTHER GOOSE GOLDEN IN THE DAPHNIS Stonestreet Stables and Harold McCormick=s Rachel Golden Century (El Prado {Ire}) made the most of soft Alexandra (Medaglia d=Oro) worked a half in :49 4/5 at early fractions and proved best late to hold off Allybar Churchill Downs yesterday in advance of Saturday=s GI (Ire) (King=s Best) by a length in yesterday=s G3 Prix Mother Goose Daphnis at Longchamp. AHe is a nice horse and won S. at Belmont well,@ said winning jockey Maxime Guyon. AI don=t Park. The filly know what [trainer, Andre] Mr. Fabre is going to do ships to New with him, but he won=t stay much further than that.@ York this Golden Century followed a debut win over this trip at morning. Un- Fontainebleau Apr. 10 with a third when upped to a der exercise mile and a half in a conditions event at Saint-Cloud rider Dominic May 1. Back to a mile at this track last time May 30, Terry, Rachel the homebred returned to winning ways and extended was caught his sequence under an enterprising ride. Allowed to through frac- saunter along behind reluctant rivals shortly after the tions of :13, start, the bay ran freely until settled into his soft lead, :25 and and after kicking at the top of the stretch, was mainly hand ridden to comfortably beat the Wertheimer=s Reed Palmer photo :37.40; she galloped out homebred Allybar. -
Recent and Quaternary Foraminifera Collected Around New Caledonia
Plates 6/1 & 6/2 Recent and Quaternary foraminifera collected around New Caledonia Jean-Pierre DEBENAY 1 & Guy CABIOCH 2 1 UPRES EA, Universite d'Angers, 2 Bd Lavoisiere, 49045, Angers cedex, France 2 Institut de Recherche pour Developpement, UR 055, Paliotropique, Centre IRD, BPA5, 98848 Noumea cedex, Nouvelle-Caledonie [email protected] Abstract The compilation of the works carried out on Recent and Quaternary foraminifera collected in the waters surrounding New Caledonia allowed us to identify 574 species. These species are listed according to the classification of Loeblish & Tappan (1988), updated for the Recent species by Debenay et al. (1996). Their affinity with microfaunas from other regions is briefly discussed. Resume La compilation des travaux sur les foramini:feres actuels et quaternaires recoltes dans les eaux entourant la Nouvelle-Caledonie nous a permis de repertorier 574 especes. Ces especes sont presen tees selon la classification de Loeblish & Tappan (1988), mise ajour pour les especes actuelles par Debenay et al. (1996). Leur affinite avec les microfaunes d'autres regions est discutee brievement. Introduction The first study about foraminifera from the southwestern Pacific near New Caledonia was carried out by Brady (1884) during the voyage of H.M.S. Challenger (1873-1876), updated by Barker (1960), The nearest station was station 177, near Vanuatu (16°45'S-168°5'E). However, studies concerning directly New Caledonia began much later, with partial and local inventories in coastal samples (Gambini,1958, 1959; Renaud-Debyser, 1965; Toulouse, 1965, 1966). Samples of recent and fossil sediments collected during the Singer-Polignac mission (1960-1965) were further used for several studies of foraminiferal assemblages (Coudray & Margerel, 1974; Coudray, 1976; Margerel, 1981). -
Middlesex University Research Repository
Middlesex University Research Repository An open access repository of Middlesex University research http://eprints.mdx.ac.uk Delve, Janet (1999) The development of the mathematical department of the Educational Times from 1847 to 1862. PhD thesis, Middlesex University. Available from Middlesex University’s Research Repository at http://eprints.mdx.ac.uk/7993/ Copyright: Middlesex University Research Repository makes the University’s research available electronically. Copyright and moral rights to this thesis/research project are retained by the author and/or other copyright owners. The work is supplied on the understanding that any use for commercial gain is strictly forbidden. A copy may be downloaded for personal, non- commercial, research or study without prior permission and without charge. Any use of the thesis/research project for private study or research must be properly acknowledged with reference to the work’s full bibliographic details. This thesis/research project may not be reproduced in any format or medium, or extensive quotations taken from it, or its content changed in any way, without first obtaining permission in writing from the copyright holder(s). If you believe that any material held in the repository infringes copyright law, please contact the Repository Team at Middlesex University via the following email address: [email protected] The item will be removed from the repository while any claim is being investigated. MX 7226926 X Contents ABSTRACT Mathematics held an important place in the first twelve of years of the Educational Times (1847-1923), and in November 1848 a department of mathematical questions and solutions was launched. In 1864 this department was reprinted in a daughter journal: Mathematical Questions with Their solutions from The Educational Times (MQ). -
Recent Foraminifera of the Marshall Islands
Recent Foraminifera of the Marshall Islands Bikini and Nearby Atolls, Part 2, Oceanography (Biologic) GEOLOGICAL SURVEY PROFESSIONAL PAPER 260-H ERRATA SLIP FOR PROFESSIONAL PAPER 260-H In the distribution tables (1-5) italic numbers indicate abundance of the species in percentages of the Foraminifera present in the sample. Arabic numbers indicate actual count of specimens. Recent Foraminifera of the Marshall Islands By JOSEPH A. CUSHMAN, RUTH TODD, and RITA J. POST Bikini and Nearby Atolls, Part 2, Oceanography (Biologic) GEOLOGICAL SURVEY PROFESSIONAL PAPER 260-H UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.75 (paper cover) CONTENTS Page Page ______.____-_-__-____-___-.-..______.____ 319 Systematic descriptions—Continued Introduction- ______---_-____--__-__-_-____-____--__ 319 Trochamminidae. _______________________________ 342 General features_____----------_--_-_-__-________^__ 319 Lagenidae _____________________________________ 342 Fauna of reef flats.__.--________-_-___._________ 319 Polymorphinidae_ ________-_-_-_----_--_-_-_-_-_ 344 Fauna of lagoons_______________________________ 320 Nonionidae_ __-__________________---_-----_---_ 345 Fauna of outer slopes. __.-_.____-_-_. ___________ 321 Camerinidae ___________________________________ 346 Fauna of deep water. ___________________________ 321 Peneroplidae___________________________________ 348 Sylvania Guyot core.______________^___-____ 322 Alveolinellidae________________________________ 348 Species restricted to guyot-__.___-_-.-_______ 322 Heterohelicidae- ________________________________ 349 Nondiagnostic species._________----_-__^________ 323 Buliminidae_- _ _________-_______-_-__--_--___--_ 349 Notes on distribution by families. -
Ernest Guiraud: a Biography and Catalogue of Works
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1990 Ernest Guiraud: A Biography and Catalogue of Works. Daniel O. Weilbaecher Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Weilbaecher, Daniel O., "Ernest Guiraud: A Biography and Catalogue of Works." (1990). LSU Historical Dissertations and Theses. 4959. https://digitalcommons.lsu.edu/gradschool_disstheses/4959 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS The most advanced technology has been used to photograph and reproduce this manuscript from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. -
Vicksburg (Oligocene) Smaller Foraminifera from Mississippi
Vicksburg (Oligocene) Smaller Foraminifera From Mississippi GEOLOGICAL SURVEY PROFESSIONAL PAPER 241 Vicksburg (Oligocene) Smaller Foraminifera From Mississippi By RUTH TODD GEOLOGICAL SURVEY PROFESSIONAL PAPER 241 Descriptions and illustrations of smaller Foraminifera from jive measured sections in western Mississippi UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1952 UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. Contents Page Abstract _________________ 1 Systematic descriptions— Continued Introduction ______________ 1 Family Heterohelicidae- _______ 24 Stratigraphic sections _ _____ 2 Family Buliminidae.-__________ 25 Systematic descriptions_ 4 Family Rotaliidae-___________ 34 Family Textulariidae___ 4 Family Amphisteginidae------- 42 Family Verneuilinidae__ 5 Family Cassidulinidae- _ __--___. 42 Family Valyulinidae _ _ 6 Family Chilostomellidae-______ 43 Family Miliolidae. ____ 6 Family Globigerinidae--------- 43 Family Ophthalmidiidae 10 Family Anomalinidae_________ 44 Family Lagenidae____ 10 Family Planorbulinidae__ 46 Family Polymorphinidae 16 Bibliography __ ___________________ 47 Family Nonionidae. ____________________________ 21 Index.___________--_------_-____ 49 Illustrations Plate 1. Textulariidae, Verneuilinidae, Valvulinidae, Miliolidae, Ophthalmidiidae__--_----------_----_-------_ 2. Lagenidae______--____________________-_______________________________-___-------_-------_-- -
Doi:10.32703/2415-7422-2020-10-1(16)-62-71
http://www.hst-journal.com Історія науки і техніки 2020, том 10, вип. 1(16) History of science and technology, 2020, vol. 10, issue 1(16) DOI:10.32703/2415-7422-2020-10-1(16)-62-71 UDC 94(477):929 Лігін (Lihin) Oliinyk Olha Independent researcher, Ukraine e-mail: [email protected] https://orcid.org/0000-0002-1398-6679 The role of V. Lihin's scientific publications in international journals Abstract. In the 21st century, we live in the stage of human history when any information is as accessible as possible. The modern scientific world is based on an extensive network of journals. Thanks to them, we have the opportunity to get acquainted with the latest research results. In the 21st century, every reputable journal also has an online version, which makes the dissemination of scientific information almost instantaneous. We are so accustomed to the conveniences of the information age that it is difficult for us to imagine the difficulties that scientists faced a little over 150 years ago. In the second half of the nineteenth century, almost most of the sciences known to mankind were formed. The genesis of science launched the process of forming branch scientific communities and demanded stable ways of communication for productive and effective development of the branch. Scientific journals have become an ideal means of disseminating information, and a scientific article has been transformed from an ordinary letter into a modern form and has taken on an ideal form. Given all the above, it is important to consider the experience of V. Lihin in publishing articles in scientific journals abroad. -
On Leonardo Da Vinci's Proof of the Theorem of Pythagoras
LEONARDO DA VINCI'S PROOF OF THE THEOREM OF PYTHAGORAS FRANZ LEMMERMEYER While collecting various proofs of the Pythagorean Theorem for presenting them in my class (see [12]) I discovered a beautiful proof credited to Leonardo da Vinci. It is based on the diagram on the right, and I leave the pleasure of reconstructing the simple proof from this diagram to the reader (see, however, the proof given at the end of this article). Since I had decided to give correct references to as many results as possible (if only to set an example) I started looking at the many presen- tations of da Vinci's proofs on the internet for finding out where da Vinci had published his proof. It turned out that although this was a very well known proof, none of the many sources was able to point me to a book with a sound reference let alone to one of da Vinci's original publications. For this reason I gave up and simple remarked As a rule, one has to be very careful in such situations, meaning that claims that cannot be verified often turn out to be wrong. A simple search (with the keywords \da Vinci" and Pythagoras or Pitagoras) will reveal dozens of books that credit the proof above to da Vinci, including Maor's book [14] or the otherwise very accurate and highly readable book [17] by Ostermann & Wanner, where the proof is credited to da Vinci in Exercise 21 on p. 26. arXiv:1311.0816v2 [math.HO] 15 Jan 2014 Tracking down References. -
Redalyc.Microfossils, Paleoenvironments And
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Filkorn, Harry F.; Scott, Robert W. Microfossils, paleoenvironments and biostratigraphy of the Mal Paso Formation (Cretaceous, upper Albian), State of Guerrero, Mexico Revista Mexicana de Ciencias Geológicas, vol. 28, núm. 1, 2011, pp. 175-191 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57220090013 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de CienciasMicrofossils, Geológicas, paleoenvironments v. 28, núm. 1, 2011, and p. biostratigraphy 175-191 of the Mal Paso Formation 175 Microfossils, paleoenvironments and biostratigraphy of the Mal Paso Formation (Cretaceous, upper Albian), State of Guerrero, Mexico Harry F. Filkorn1,* and Robert W. Scott2 1 Physics and Planetary Sciences Department, Los Angeles Pierce College, 6201 Winnetka Avenue, Woodland Hills, California 91371 USA. 2 Precision Stratigraphy Associates and University of Tulsa, 149 West Ridge Road, Cleveland, Oklahoma 74020, USA. * fi[email protected] ABSTRACT Microfossils from an outcrop of the coral reef and rudist-bearing calcareous upper member of the Mal Paso Formation just north of Chumbítaro, State of Michoacán, Mexico, indicate a deepening trend and transition from nearshore through outer shelf depositional environments upward through the sampled stratigraphic interval. The microbiota is mostly composed of species of calcareous algae and foraminifera. The identified calcareous algae are: Pseudolithothamnium album Pfender, 1936; Cayeuxia kurdistanensis Elliott, 1957; Acicularia americana Konishi and Epis, 1962; and Dissocladella sp.