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SI Appendix for Hopkins, Melanie J, and Smith, Andrew B
Hopkins and Smith, SI Appendix SI Appendix for Hopkins, Melanie J, and Smith, Andrew B. Dynamic evolutionary change in post-Paleozoic echinoids and the importance of scale when interpreting changes in rates of evolution. Corrections to character matrix Before running any analyses, we corrected a few errors in the published character matrix of Kroh and Smith (1). Specifically, we removed the three duplicate records of Oligopygus, Haimea, and Conoclypus, and removed characters C51 and C59, which had been excluded from the phylogenetic analysis but mistakenly remain in the matrix that was published in Appendix 2 of (1). We also excluded Anisocidaris, Paurocidaris, Pseudocidaris, Glyphopneustes, Enichaster, and Tiarechinus from the character matrix because these taxa were excluded from the strict consensus tree (1). This left 164 taxa and 303 characters for calculations of rates of evolution and for the principal coordinates analysis. Other tree scaling methods The most basic method for scaling a tree using first appearances of taxa is to make each internal node the age of its oldest descendent ("stand") (2), but this often results in many zero-length branches which are both theoretically questionable and in some cases methodologically problematic (3). Several methods exist for modifying zero-length branches. In the case of the results shown in Figure 1, we assigned a positive length to each zero-length branch by having it share time equally with a preceding, non-zero-length branch (“equal”) (4). However, we compared the results from this method of scaling to several other methods. First, we compared this with rates estimated from trees scaled such that zero-length branches share time proportionally to the amount of character change along the branches (“prop”) (5), a variation which gave almost identical results as the method used for the “equal” method (Fig. -
Abernathy, Adams, Addison, Alewine, Allen, Allred
BUSCAPRONTA www.buscapronta.com ARQUIVO 14 DE PESQUISAS GENEALÓGICAS 168 PÁGINAS – MÉDIA DE 54.100 SOBRENOMES/OCORRÊNCIA Para pesquisar, utilize a ferramenta EDITAR/LOCALIZAR do WORD. A cada vez que você clicar ENTER e aparecer o sobrenome pesquisado GRIFADO (FUNDO PRETO) corresponderá um endereço Internet correspondente que foi pesquisado por nossa equipe. Ao solicitar seus endereços de acesso Internet, informe o SOBRENOME PESQUISADO, o número do ARQUIVO BUSCAPRONTA DIV ou BUSCAPRONTA GEN correspondente e o número de vezes em que encontrou o SOBRENOME PESQUISADO. Número eventualmente existente à direita do sobrenome (e na mesma linha) indica número de pessoas com aquele sobrenome cujas informações genealógicas são apresentadas. O valor de cada endereço Internet solicitado está em nosso site www.buscapronta.com . Para dados especificamente de registros gerais pesquise nos arquivos BUSCAPRONTA DIV. ATENÇÃO: Quando pesquisar em nossos arquivos, ao digitar o sobrenome procurado, faça- o, sempre que julgar necessário, COM E SEM os acentos agudo, grave, circunflexo, crase, til e trema. Sobrenomes com (ç) cedilha, digite também somente com (c) ou com dois esses (ss). Sobrenomes com dois esses (ss), digite com somente um esse (s) e com (ç). (ZZ) digite, também (Z) e vice-versa. (LL) digite, também (L) e vice-versa. Van Wolfgang – pesquise Wolfgang (faça o mesmo com outros complementos: Van der, De la etc) Sobrenomes compostos ( Mendes Caldeira) pesquise separadamente: MENDES e depois CALDEIRA. Tendo dificuldade com caracter Ø HAMMERSHØY – pesquise HAMMERSH HØJBJERG – pesquise JBJERG BUSCAPRONTA não reproduz dados genealógicos das pessoas, sendo necessário acessar os documentos Internet correspondentes para obter tais dados e informações. DESEJAMOS PLENO SUCESSO EM SUA PESQUISA. -
FEBRUARY 5Th, 1875
206 ANNUAL GENERAL MEETING. FEBRUARY 5th, 1875. ROBERT ETHERIDGE, Esq., F.R.S., F.G.S., &c., Vice-President, in the Chair. The following Report was read by the Honorary Secretary :- REPORT OF THE GENERAL COMMITTEE FOR 1874. The General Committee have much pleasure in congratulating the Association upon the results of the past year. A considerable number of new Members have been added to the list, and several of these are already well known throughout the country, by their study and practice of Geological Science. There have been a few losses by death, and, if the number of those who have retired is somewhat more numerous than has been the case of later years, they consisted, with few exceptions, of Members whose interest in the proceedings of the Association was never very ardent. Members elected during 1874 49 Withdrawals 14, Deaths 4 . 18 Increase 31 The Census of the Association on the 1st January, 1875, gave the following results :- Honorary Members 12 Life Members. 42 Old Country Members 28 Other Members 257 339 The lamented death of Professor Phillips, reduces the number of Honorary Members to 12. A short notice of the sad occurrence, which deprived the Association of one amongst the most eminent 206 ANNUAL GENERAL MEETING. of its body, will be found in the forthcoming number of Vol. iv. of the" Proceedings." The financial position of the Association is very satisfactory, and the large number of Members now contributing has yielded a sum which amply provides for an increased expenditure, the benefits of which are shared by all. -
James Hutton's Reputation Among Geologists in the Late Eighteenth and Nineteenth Centuries
The Geological Society of America Memoir 216 Revising the Revisions: James Hutton’s Reputation among Geologists in the Late Eighteenth and Nineteenth Centuries A. M. Celâl Şengör* İTÜ Avrasya Yerbilimleri Enstitüsü ve Maden Fakültesi, Jeoloji Bölümü, Ayazağa 34469 İstanbul, Turkey ABSTRACT A recent fad in the historiography of geology is to consider the Scottish polymath James Hutton’s Theory of the Earth the last of the “theories of the earth” genre of publications that had begun developing in the seventeenth century and to regard it as something behind the times already in the late eighteenth century and which was subsequently remembered only because some later geologists, particularly Hutton’s countryman Sir Archibald Geikie, found it convenient to represent it as a precursor of the prevailing opinions of the day. By contrast, the available documentation, pub- lished and unpublished, shows that Hutton’s theory was considered as something completely new by his contemporaries, very different from anything that preceded it, whether they agreed with him or not, and that it was widely discussed both in his own country and abroad—from St. Petersburg through Europe to New York. By the end of the third decade in the nineteenth century, many very respectable geologists began seeing in him “the father of modern geology” even before Sir Archibald was born (in 1835). Before long, even popular books on geology and general encyclopedias began spreading the same conviction. A review of the geological literature of the late eighteenth and the nineteenth centuries shows that Hutton was not only remembered, but his ideas were in fact considered part of the current science and discussed accord- ingly. -
Reports and Proceedings
318 Reports and Proceedings. the Range having been laid down unconformably on the denuded surface of the Lower Old Red and Upper Silurian rocks: also that oscillations of level took place during the Permian and Triassic periods, as shown by the unconformities between the several members of these groups ; and that the last great catastrophe, which brought down the Trias on the Eastern side of the Range, was posterior in date to the Lias. KBPOBTS -AJXTID PROCEEDINGS. GEOLOGICAL SOCIETY OF LONDON.—June 7, 1865 ; W. J. Hamil- ton, Esq., President, in the chair. The following communications were read:— 1. ' Note on Ovibos moschatus, Blainville.' By M. E. Lartet, For. Mem.G.S. Translated by the late H.Christy, Esq., F.R.S., F.G.S.— A hoof-phalange found by Mr. Christy and the author in the Gorge d'Enfer was stated to be identical in form and dimensions with the corresponding bone of the existing Ovibos moschatus, to which species M. Lartet therefore referred it. With it were found remains of Ursus speleeus, Felis spelaa, Wolf, Reindeer, and Aurochs, as well as worked flints differing from those found in any other of the Dor- dogne caves. The author remarked that the Gorge d'Enfer is the most southern locality at which remains of Ovibos moschatus have yet been found, and is 15° south of its most southern limit at the present day; but the Reindeer has been found by Mr. Christy and himself farther south still—on the northern slope of the Pyrenees. 2. ' On somjB Additional Fossils from the Lingula-flags.' By J. -
Echinoid Burrow Bichordites Monastiriensis from the Oligocene of NE Italy
Echinoid burrow Bichordites monastiriensis from the Oligocene of NE Italy MASSIMO BERNARDI, SERGIO BOSCHELE, PAOLO FERRETTI, and MARCO AVANZINI Bernardi, M., Boschele, S., Ferretti, P., and Avanzini, M. 2010. Echinoid burrow Bichordites monastiriensis from the Oligocene of NE Italy. Acta Palaeontologica Polonica 55 (3): 479–486. Several specimens of trace fossil Bichordites monastiriensis were discovered in two shallow water Oligocene sandstone beds from Valsugana (Trentino, NE Italy) representing the oldest documented occurrence for this ichnospecies. They are grazing−crawling (pascichnion−repichnion) structures and are occasionally associated with enlarged structures that can be interpreted as resting traces (cubichnia) and assigned to the ichnogenus Cardioichnus. The resulting Bichordites–Cardio− ichnus compound trace fossil is here described for the first time. In the basal part of some specimens, skeletal remains of Eupatagus ornatus were found in life position. This founding enables to widen the spectrum of known Bichordites trace− makers. Exceptional conditions of preservation of one specimen extending in two beds recording different environmental conditions gave an opportunity to document the effects of various taphonomical histories on the preservation of this traces. Key words: Trace fossils, Bichordites, echinoid burrows, Upogebia, foredeep, Oligocene, Italy. Massimo Bernardi [[email protected]], Paolo Ferretti [[email protected]], and Marco Avanzini [avanzini @mtsn.tn.it], Museo Tridentino di Scienze Naturali, Via -
Adec Preview Generated PDF File
Records of the Western Australian Museum 21: 157-165 (2002). The asterostomatid echinoid Antillaster from the Paradash Group (Middle Eocene) of the Nakhichevan Region of Azerbaijan Kenneth J. McNamaral and Oktay H. Melikov2 I Department of Earth and Planetary Sciences, Western Australian Museum, Francis Street, Perth, Western Australia 6000, Australia 2 Azerbaijan State Oil Academy, 370102 Azadlik pr. 20, Baku, Azerbaijan Abstract - The asterostomatid echinoid Antillaster has previously been recorded only from the Caribbean region and northeastern South America. Here we report the first occurrence of this genus from outside the Americas, in the Lesser Caucasus, where it has been found in Middle Eocene sediments of the Paradash Group in the Nakhichevan region of Azerbaijan. The material is described as Antillaster bagmanovi sp. novo It is the earliest known occurrence of the genus. Its presence in the Paratethys, in a region far removed from previous known occurrences, has significant palaeobiogeographic implications. Its disappearance from the Lesser Caucasus, but persistence in the Caribbean, may be linked to the contraction of the Tethys during the Cenozoic. INTRODUCTION from Eocene to Miocene sediments in Venezuela, Eocene sediments in the Nakhichevan region of Cuba, Jamaica, Bonaire, Antigua, Puerto Rico and Azerbaijan have long attracted the attention of Mexico (ICier 1984). Here we report the first record many investigators, due to their good exposure and of this genus from outside the Caribbean region, in extensive foraminiferal and molluscan fauna. The Middle Eocene sediments of the Lesser Caucasus dating of the predominantly clay-sand facies as region in Azerbaijan. This provides the earliest being Eocene is based on this rich foraminiferal and record of asterostomatid echinoids in the Paratethys molluscan fauna (Azizbekov 1961; Bagmanov 1966, region. -
The Geology of the District Around St. David's, Pembrokeshire
121 THE GEOLOGY OF THE DISTRICT AROUND ST. DAVID'S, PEMBROKESHIRE. By J. FREDERICK N. GREEN, B.A., F.G.S. [Read March 3rd, 191f.1 Advance copies of this Paper and of the Paper on Ramsey Island were printed and issued to Members in connection with the Easter Excursion of IgII. The two Papers are now reprinted with a few additions and alterations. INTRODUCTION. ---HE Council of the Geologists' Association have done me 1 the honour of appointing me Director of an excursion to St. David's.'*' My experience of the district is not extended, and during my stay there I have devoted myself wholly to the struc• tural problems, leaving on one side the zonal paheontology and surface geology. Most of what follows must therefore be looked upon as a compilation from the papers mentioned in the Biblio• graphy (p. 136). Further, the area has been very insufficiently worked, especially in respect of its remarkable glacial geology, so that in these notes there must be many imperfections, the elimination of which may, I hope, be advanced by our excursion. The structure of this region, properly named" Dewisland," has occasioned one of the most severe disputes in the history of British geology. This controversy attained grave proportions owing to its bearing on other areas and on the generalisations drawn therefrom. I should not have ventured to assume in these notes the correctness of the interpretation given by myself in 19°8, which substantially upheld the main contentions of the late Henry Hicks, who made this corner of Wales a classical district for the study of our oldest rocks, had I not been authorised by the kindness of Mr. -
Meteorite Iron in Egyptian Artefacts
SCIENTISTu u GEO VOLUME 24 NO 3 APRIL 2014 WWW.GEOLSOC.ORG.UK/GEOSCIENTIST The Fellowship Magazine of the Geological Society of London UK / Overseas where sold to individuals: £3.95 READ GEOLSOC BLOG! [geolsoc.wordpress.com] Iron from the sky Meteorite iron in Egyptian artefacts FISH MERCHANT WOMEN GEOLOGISTS BUMS ON SEATS Sir Arthur Smith Woodward, Tales of everyday sexism If universities think fieldwork king of the NHM fishes - an Online Special sells geology, they’re mistaken GEOSCIENTIST CONTENTS 06 22 10 16 FEATURES IN THIS ISSUE... 16 King of the fishes Sir Arthur Smith Woodward should be remembered for more than being caught by the Piltdown Hoax, says Mike Smith REGULARS 05 Welcome Ted Nield has a feeling that some eternal verities have become - unsellable 06 Society news What your Society is doing at home and abroad, in London and the regions 09 Soapbox Jonathan Paul says universities need to beef up their industrial links to attract students ON THE COVER: 21 Letters Geoscientist’s Editor in Chief sets the record straight 10 Iron from the sky 22 Books and arts Four new books reviewed by Catherine Meteoritics and Egyptology, two very different Kenny, Mark Griffin, John Milsom and Jason Harvey disciplines, recently collided in the laboratory, 25 People Geoscientists in the news and on the move write Diane Johnson and Joyce Tyldesley 26 Obituary Duncan George Murchison 1928-2013 27 Calendar Society activities this month ONLINE SPECIALS Tales of a woman geologist Susan Treagus recalls her experiences in the male-dominated groves of -
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THE GEOLOGICAL CURATOR VOLUME 7, NO. 9 CONTENTS THE CHARLES W. PEACH (1800-1886) COLLECTION OF CORNISH FOSSILS by P.R. Crowther.....................................................................................................................................................323 A LARGE SCALE ‘MICROCLIMATE’ ENCLOSURE FOR PYRITIC SPECIMENS by A.M. Doyle........................................................................................................................................................329 A NEW TOOL FOR FOSSIL PREPARATION by P.A. Selden........................................................................................................................................................337 OBITUARY: RICHARD MICHAEL CARDWELL EAGAR 1919-2003 by J.R. Nudds........................................................................................................................................................341 BOOK REVIEWS.......................................................................................................................................................336 GEOLOGICAL CURATORS’ GROUP - 28TH ANNUAL GENERAL MEETING.................................................343 PRESENTATION OF THE A.G. BRIGHTON MEDAL TO H. PHILIP POWELL - CITATION...........................349 GEOLOGICAL CURATORS’ GROUP - April 2003 -321- -322- THE CHARLES W. PEACH (1800-1886) COLLECTION OF CORNISH FOSSILS by Peter R. Crowther Crowther, P.R. 2003. The Charles W. Peach (1800-1886) Collection of Cornish fossils. The Geological Curator 7(9): -
Associations Between Three Irregular Urchins and Cone-And-Funnel Topography in a Tropical Soft-Bottom Community Daniel Ray Norri
Associations between three irregular urchins and cone-and-funnel topography in a tropical soft-bottom community by Daniel Ray Norris A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE IN BIOLOGY UNIVERSITY OF GUAM 5 APRIL 1994 AN ABSTRACT OF THE THESIS by Daniel Ray Norris for the Master of Science degree in Biology presented 5 April 1994. Title: Associations between three irregular urchins and cone-and-funnel topography in a tropical soft-bottom community Approved: Charles Birkeland, Chair, Thesis Committee Habitat characteristics and densities of three species of irregular urchins were measured in Apra Harbor, Guam. The densities of Maretia planulata, Metalia dicrana and Fibularia ovulum in the microhabitat defined as cone-and-funnel topography were analyzed at 10, 20 and 30 m in depth. Urchins were sampled to measure densities for each depth with respect to characteristics of the cone-and-funnel topography including: depth of anoxic layer, sediment granulometry, sediment organics and mean dis tance between sediment cones. Secondarily, growth rates for Maretia planulata were measured along a sediment gradient. Sediment organic content was also analyzed. Laboratory experiments demonstrated that growth rates for Maretia planulata were not significantly different at 10, 20 and 30 m depths, but densities for each species, organic content and cone densities were significantly different across the depth gradient. Densities of Maretia planulata and Metalia dicrana densities were more similar across depth gradients and not between microhabitats. Fibularia ovulum densities were generally grouped with respect to either the cone microhabi tat or the funnel microhabitat. Physical differences (organic content, an oxia, and sediment granulometry) and other niche partitioning may regulate densities of these macroinvertebrates along the depth gradient. -
FOR the COASTAL PLAIN of NORTH CAROLINA ~--E Roy"- Tj Y"",Cf'
STRUCTURAL AND STRATIGRAPHIC FRAMEWORK FOR THE COASTAL PLAIN OF NORTH CAROLINA ~--e roY"- tJ y"",cf' Edited By Gerald R. Baum T:~-- w. Burleigh Harris ) And !~- Victor A. Zullo ;' -j Carolina Geological Society Field Trip Guidebook And October 19-21, 1979 Atlantic Coastal Plain Geological Association Wrightsville Beach, North Carolina Cover illustration: Major structural features of the North Carolina Coastal Plain. (Figure 1 from Harris, Zullo and Baum) Layout by Anne Virant-Lazar and Ben McKenzie Copies of this guidebook can be purchased fram: Geological Survey Section Department of Natural Resources and Community Development P. O. Box 27687 Raleigh, NC 27611 Ii CAROLI NA GEOLOGI CAL SOC IETY AND ATLANTIC COASTAL PLAIN GEOLOGICAL ASSOCIATION October 19-21, 1979 STRUCTURAL AND STRATIGRAPHIC FRAMEWORK FOR THE COASTAL PLAIN OF NORTH CAROLINA Edited by Gerald R. Baum Department of Geology College of Charleston Charleston, South Carolina 29401 W. Burleigh Harris and Victor A. Zullo Department of Earth Sciences University of North Carolina, Wilmington Wilmington, North Carolina 28403 Carolina Geological Society 1979 Officers President: Arthur W. Snoke Department of Geology University of South Carolina Columbia, South Carolina Vice-President: Robert E. Lemmon Department of Geography and Earth Sciences University of North Carolina at Charlotte Charlotte, North Carolina Secretary-Treasurer: S. Duncan Heron, Jr. Department of Geology Duke University Durham, North Carolina Membership Chairman: Paul Nystrom South Carolina Geological Survey Columbia, South Carolina Atlantic Coastal Plain Geological Association 1979 Officers Secretary-Treasurer: Tom Pickett Delaware Geological Survey University of Delaware Newark, Delaware Field Trip Leaders: Gerald R. Baum Department of Geology College of Charleston Charleston, South Carolina W.