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The Wyley History of the Geologists' Association in the 50 Years 1958
THE WYLEY HISTORY OF THE GEOLOGISTS’ ASSOCIATION 1958–2008 Leake, Bishop & Howarth ASSOCIATION THE GEOLOGISTS’ OF HISTORY WYLEY THE The Wyley History of the Geologists’ Association in the 50 years 1958–2008 by Bernard Elgey Leake, Arthur Clive Bishop ISBN 978-0900717-71-0 and Richard John Howarth 9 780900 717710 GAHistory_cover_A5red.indd 1 19/08/2013 16:12 The Geologists’ Association, founded in 1858, exists to foster the progress and Bernard Elgey Leake was Professor of Geology (now Emeritus) in the diffusion of the science of Geology. It holds lecture meetings in London and, via University of Glasgow and Honorary Keeper of the Geological Collections in the Local Groups, throughout England and Wales. It conducts field meetings and Hunterian Museum (1974–97) and is now an Honorary Research Fellow in the School publishes Proceedings, the GA Magazine, Field Guides and Circulars regularly. For of Earth and Ocean Sciences in Cardiff University. He joined the GA in 1970, was further information apply to: Treasurer from 1997–2009 and is now an Honorary Life Member. He was the last The Executive Secretary, sole editor of the Journal of the Geological Society (1972–4); Treasurer (1981–5; Geologists’ Association, 1989–1996) and President (1986–8) of the Geological Society and President of the Burlington House, Mineralogical Society (1998–2000). He is a petrologist, geochemist, mineralogist, Piccadilly, a life-long mapper of the geology of Connemara, Ireland and a Fellow of the London W1J 0DU Royal Society of Edinburgh. He has held research Fellowships in the Universities of phone: 020 74349298 Liverpool (1955–7), Western Australia (1985) and Canterbury, NZ (1999) and a e-mail: [email protected] lectureship and Readership at the University of Bristol (1957–74). -
FALL 2017 President’S Reflections
PriscumPriscum NEWSLETTER OF THE VOLUME 24, ISSUE 1 President’s Reflections Paleobiology, the finances of both journals appear secure for INSIDE THIS ISSUE: the foreseeable future, and with a much-improved online presence for both journals. To be sure, more work lies ahead, Report on Student but we are collaborating with Cambridge to expand our au- 3 Diversity and Inclusion thor and reader bases, and, more generally, to monitor the ever-evolving publishing landscape. Our partnership with The Dry Dredgers of 10 Cambridge is providing additional enhancements for our Cincinnati, Ohio members, including the digitization of the Society’s entire archive of special publications; as of this writing, all of the PS Embraces the 13 Hydrologic Cycle Society’s short course volumes are now available through the member’s portal, and all remaining Society publications will be made available soon. We are also exploring an exciting PS Events at 2017 GSA 14 new outlet through Cambridge for all future Special Publica- By Arnie Miller (University of tions. Stay tuned! Book Reviews 15 Cincinnati), President In my first year as President, the Society has continued to These are challenging times for move forward on multiple fronts, as we actively explore and Books Available for 28 scientists and for the profes- pursue new means to carry out our core missions of enhanc- Review Announcement sional societies that represent ing and broadening the reach of our science and of our Socie- them. In the national political ty, and providing expanded developmental opportunities for arena, scientific findings, policies, and funding streams that all of our members. -
Trace Fossils from the Baltoscandian Erratic Boulders in Sw Poland
Annales Societatis Geologorum Poloniae (2017), vol. 87: 229–257 doi: https://doi.org/10.14241/asgp.2017.014 TRACE FOSSILS FROM THE BALTOSCANDIAN ERRATIC BOULDERS IN SW POLAND Alina CHRZĄSTEK & Kamil PLUTA Institute of Geological Sciences, Wrocław University; Maksa Borna 9, 50-204 Wrocław, Poland e-mails: [email protected], [email protected] Chrząstek, A. & Pluta, K, 2017. Trace fossils from the Baltoscandian erratic boulders in SW Poland. Annales Societatis Geologorum Poloniae, 87: 229–257. Abstract: Many well preserved trace fossils were found in erratic boulders and the fossils preserved in them, occurring in the Pleistocene glacial deposits of the Fore-Sudetic Block (Mokrzeszów Quarry, Świebodzice outcrop). They include burrows (Arachnostega gastrochaenae, Balanoglossites isp., ?Balanoglossites isp., ?Chondrites isp., Diplocraterion isp., Phycodes isp., Planolites isp., ?Rosselia isp., Skolithos linearis, Thalassinoides isp., root traces) and borings ?Gastrochaenolites isp., Maeandropolydora isp., Oichnus isp., Osprioneides kamp- to, ?Palaeosabella isp., Talpina isp., Teredolites isp., Trypanites weisei, Trypanites isp., ?Trypanites isp., and an unidentified polychaete boring in corals. The boulders, Cambrian to Neogene (Miocene) in age, mainly came from Scandinavia and the Baltic region. The majority of the trace fossils come from the Ordovician Orthoceratite Limestone, which is exposed mainly in southern and central Sweden, western Russia and Estonia, and also in Norway (Oslo Region). The most interesting discovery in these deposits is the occurrence of Arachnostega gastrochaenae in the Ordovician trilobites (?Megistaspis sp. and Asaphus sp.), cephalopods and hyolithids. This is the first report ofArachnostega on a trilobite (?Megistaspis) from Sweden. So far, this ichnotaxon was described on trilobites from Baltoscandia only from the St. -
The Birds (Aves) of Oromia, Ethiopia – an Annotated Checklist
European Journal of Taxonomy 306: 1–69 ISSN 2118-9773 https://doi.org/10.5852/ejt.2017.306 www.europeanjournaloftaxonomy.eu 2017 · Gedeon K. et al. This work is licensed under a Creative Commons Attribution 3.0 License. Monograph urn:lsid:zoobank.org:pub:A32EAE51-9051-458A-81DD-8EA921901CDC The birds (Aves) of Oromia, Ethiopia – an annotated checklist Kai GEDEON 1,*, Chemere ZEWDIE 2 & Till TÖPFER 3 1 Saxon Ornithologists’ Society, P.O. Box 1129, 09331 Hohenstein-Ernstthal, Germany. 2 Oromia Forest and Wildlife Enterprise, P.O. Box 1075, Debre Zeit, Ethiopia. 3 Zoological Research Museum Alexander Koenig, Centre for Taxonomy and Evolutionary Research, Adenauerallee 160, 53113 Bonn, Germany. * Corresponding author: [email protected] 2 Email: [email protected] 3 Email: [email protected] 1 urn:lsid:zoobank.org:author:F46B3F50-41E2-4629-9951-778F69A5BBA2 2 urn:lsid:zoobank.org:author:F59FEDB3-627A-4D52-A6CB-4F26846C0FC5 3 urn:lsid:zoobank.org:author:A87BE9B4-8FC6-4E11-8DB4-BDBB3CFBBEAA Abstract. Oromia is the largest National Regional State of Ethiopia. Here we present the first comprehensive checklist of its birds. A total of 804 bird species has been recorded, 601 of them confirmed (443) or assumed (158) to be breeding birds. At least 561 are all-year residents (and 31 more potentially so), at least 73 are Afrotropical migrants and visitors (and 44 more potentially so), and 184 are Palaearctic migrants and visitors (and eight more potentially so). Three species are endemic to Oromia, 18 to Ethiopia and 43 to the Horn of Africa. 170 Oromia bird species are biome restricted: 57 to the Afrotropical Highlands biome, 95 to the Somali-Masai biome, and 18 to the Sudan-Guinea Savanna biome. -
In Retrospect: Leibniz's Protogaea
NATURE|Vol 455|4 September 2008 OPINION In Retrospect: Leibniz’s Protogaea The first English translation of Gottfried Leibniz’s earth science treatise records the difficulties of understanding our planet before geologists appreciated deep time, Richard Fortey discovers. Protogaea When considering the origin of minerals, by Gottfreid Wilhelm Leibniz Leibniz has an intuitive sense that a kind Translated by Claudine Cohen and of natural cookery is involved: “One is thus Andre Wakefield inclined to suspect that nature, using volca- University of Chicago Press: 2008. noes as furnaces and mountains as alembics, 204 pp. $55. has accomplished in her mighty works what we play at with our little examples [in labo- It is something of a game among historians ratories].” That the furnaces of the ‘chymist’ to try and detect the earliest hints of a major might simulate Earth’s processes is a hope scientific breakthrough in a little-known work that still drives research into petrology and discovered through recondite scholarship. geochemistry today. Charles Darwin’s supposed debt to his grandfa- Why then did Leibniz’s shrewd obser- ther Erasmus is an example, or maybe geologist vations fail to move geology significantly Charles Lyell’s insufficient acknowledgement towards becoming a mature science? For all its of the early geological work of Nicolaus Steno. insights, Protogaea does not seem to a modern When the savant in question is Gottfried Wil- geologist like the natural ancestor of Lyell’s helm Leibniz (1646–1716) — the man who Principles of Geology. The missing ingredient developed calculus independently of Isaac is an awareness of geological time. -
Newsletter for Members of the Palaeontological Associationr Number 37 1998
PAL A EONTOLOGY E W S L E T T E NThe Newsletter for members of the Palaeontological AssociationR Number 37 1998 http://www.nhm.ac.uk/paleonet/PalAss/PalAss.html Newsletter copy Information, whether copy as such or Newsletter messages, review material, news, emergencies and advertising suggestions, can be sent in writing to Dr Sue Rigby, Dept of Geology and Geophysics, Grant Institute, West Mains Road, Edinburgh EH9 3JW; fax 0131 668 3184; email [email protected]. It would be 1 helpful if longer items of copy could be sent on a 3 /2" disk with text in Microsoft Word, WordPerfect or ASCII format. Disks clearly marked with the owner's name and address will be returned as soon as possible. The Newsletter is produced by Meg Stroud, and printed by Edinburgh University Printing Services. Deadline for copy for Issue No. 38 is 22nd May 1998. Palaeontological Association on the Internet The Palaeontological Association has its own pages on the World Wide Web, including information about the Association, and copies of the Newsletter. Site-keeper Mark Purnell can be reached by email at [email protected]. The locator is: http://www.nhm.ac.uk/paleonet/PalAss/PalAss.html Advertising in the Newsletter Advertising space in the Newsletter will be made available at the rates given below to any organisation or individual provided the content is appropriate to the aims of the Palaeontological Association. Association Members receive a 30% discount on the rates listed. All copy will be subjected to editorial control. Although every effort will be made to ensure the bona fide nature of advertisements in the Newsletter, the Palaeontological Association cannot accept any responsibility for their content. -
The Mesozoic Corals. Bibliography 1758-1993
June, 1, 2017 The Mesozoic Corals. Bibliography 1758-1993. Supplement 22 ( -2016) Compiled by Hannes Löser1 Summary This supplement to the bibliography (published in the Coral Research Bulletin 1, 1994) contains 18 additional references to literary material on the taxonomy, palaeoecology and palaeogeography of Mesozoic corals (Triassic - Cretaceous; Scleractinia, Octocorallia). The bibliography is available in the form of a data bank with a menu-driven search program for Windows-compatible computers. Updates are available through the Internet (www.cp-v.de). Key words: Scleractinia, Octocorallia, corals, bibliography, Triassic, Jurassic, Cretaceous, data bank Résumé Le supplément à la bibliographie (publiée dans Coral Research Bulletin 1, 1994) contient 18 autres références au sujet de la taxinomie, paléoécologie et paléogéographie des coraux mesozoïques (Trias - Crétacé; Scleractinia, Octocorallia). Par le service de mise à jour (www.cp-v.de), la bibliographie peut être livrée sur la base des données avec un programme de recherche contrôlée par menu avec un ordinateur Windows-compatible. Mots-clés: Scleractinia, Octocorallia, coraux, bibliographie, Trias, Jurassique, Crétacé, base des données Zusammenfassung Die Ergänzung zur Bibliographie (erschienen im Coral Research Bulletin 1, 1994) enthält 18 weitere Literaturzitate zur Taxonomie und Systematik, Paläoökologie und Paläogeographie der mesozoischen Korallen (Trias-Kreide; Scleractinia, Octocorallia). Die Daten sind als Datenbank zusammen mit einem menügeführten Rechercheprogramm für Windows-kompatible Computer im Rahmen eines Ände- rungsdienstes im Internet (www.cp-v.de) verfügbar. Schlüsselworte: Scleractinia, Octocorallia, Korallen, Bibliographie, Trias, Jura, Kreide, Datenbank 1 Estación Regional del Noroeste, Instituto de Geología, Universidad Nacional Autónoma de México, Hermosillo, Sonora, México; [email protected] © CPESS VERLAG 2017 • http://www.cp-v.de/crb • [email protected] 3 extremely rare. -
Late Jurassic Reef Bioerosion – the Dawning of a New Era
Late Jurassic reef bioerosion – the dawning of a new era MARKUS BERTLING Bertling, M.: Late Jurassic reef bioerosion - the dawning of a new era. Bulletin of the Geological Society of Denmark, Vol. 45, pp. 173–176. Copenhagen 1999– 01–30. Coral reefs of the Late Jurassic (Oxfordian) in northern Germany and France have a style of bioerosion that is closer to that of Late Triassic reefs than of modern ones. Boring sponges played minor roles here but gradually became more important in more southerly regions during the Tithonian. This is likely to be linked to a falling sea-level whose increased nutrient input triggered microbial growth in shallow water. With sponges feeding on microbes, the Late Jurassic was the time of a change to modern borer associations in reefs. Key words: Bioerosion, reefs, Jurassic, nutrients, sponges. M. Bertling [[email protected]], Geologisch-Paläontologisches Museum, Pferdegasse 3, D - 48143 Münster, Germany. 1 September 1998. The bioerosion of modern reefs is characterised by vironment has been documented before (Bertling the prevalent action of grazing sea urchins and fishes; 1993; Bertling & Insalaco 1998). The study sites (Fig. clionid sponges generally are the most important 1) are similar in depth (0–20 m) as well as climatic, macroborers, with lithophagine bivalves and micro- nutrient and salinity conditions but represent various polychaetes being locally abundant (e.g. Hutchings environments regarding water energy and sedimenta- 1986). Neither Lithophaginae nor sponges of the fam- tion (including turbidity): a high-energy coral-micro- ily Clionidae (or related forms) have been reported bial reef (Novion-Porcien NP), an occurrence within from reefs older than Late Triassic age (own observa- permanently turbulent water with slight intermittent tions); and grazing reef fish families only originated (storm) sedimentation (Luchsholklippe LU), a deep- in the Eocene (Bellwood 1996). -
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. -
Paleoecology ...Of ... Reefs from the Late Jurassic
Project: Le “Vergleichende Palokologie und Faziesentwicklung oberjurassischer Riffstrukturen des westlichen Tethys-Nordrandes * und des Lusitanischen Beckens (Zentraiportugal)/E, Project Leader: R. Leinfelder (Stuttgart) . Paleoecology, Growth Parameters and Dynamics of Coral, Sponge and Microbolite Reefs from the Late Jurassic Reinhold R. Werner, Martin Nose, Dieter U. Schmid, Laternser, Martin Takacs & Dorothea Area of Study: Portugal, Spain, Southern Germany, France, Poland Environment: Shallow to deep carbonate platforms Stratigraphy: Late Jurassic Organisms: Corals, siliceous sponges, microbes, microen- crusters Depositional Setting: Brackish-lagoonal to deep ramp set- tings Constructive Processes: Frame-building, baffling and binding (depending on reef type and type of reef- building organisms) Destructive Processes: Borings by bivalves and sponges; wave action Preservation: Mostly well preserved Research Topic: Comparative facies analysis and paleo- ecology of Upper Jurassic reefs, reef organisms and communities Spongiolitic facies Fig. I: Distribution of Upper Jurassic reefs studied in detail. Abstract framework and pronounced relief whenever microbolite crusts provided stabilization. Reefs in steepened slope set- Reefs from the Late Jurassic comprise various types of tings are generally rich in microbolites because of bypass coral reefs, siliceous sponge reefs and microbolite reefs. possibilities for allochthonous sediment. Reef rimmed shal- Upper Jurassic corals had a higher ratio of heterotrophic low-water platforms did occur but only developed on pre- versus autotrophic energy uptake than modern ones, which existing uplifts. Upper Jurassic sponge-microbolite mud explains their frequent occurrence in terrigenous settings. mounds grew in subhorizontal mid to outer ramp settings Coral communities changed along a bathymetric gradient and reflect a delicate equilibrium of massive and peloidal but sedimentation exerted a stronger control on diversities microbolite precipitation and accumulation of allochthonous than bathymetry. -
BIASES in INTERPRETATION of the FOSSIL RECORD of CONODONTS by MARK A
[Special Papers in Palaeontology, 73, 2005, pp. 7–25] BETWEEN DEATH AND DATA: BIASES IN INTERPRETATION OF THE FOSSIL RECORD OF CONODONTS by MARK A. PURNELL* and PHILIP C. J. DONOGHUE *Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK; e-mail: [email protected] Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK; e-mail: [email protected] Abstract: The fossil record of conodonts may be among and standing generic diversity. Analysis of epoch ⁄ stage-level the best of any group of organisms, but it is biased nonethe- data for the Ordovician–Devonian interval suggests that less. Pre- and syndepositional biases, including predation there is generally no correspondence between research effort and scavenging of carcasses, current activity, reworking and and generic diversity, and more research is required to bioturbation, cause loss, redistribution and breakage of ele- determine whether this indicates that sampling of the cono- ments. These biases may be exacerbated by the way in which dont record has reached a level of maturity where few genera rocks are collected and treated in the laboratory to extract remain to be discovered. One area of long-standing interest elements. As is the case for all fossils, intervals for which in potential biases and the conodont record concerns the there is no rock record cause inevitable gaps in the strati- pattern of recovery of different components of the skeleton graphic distribution of conodonts, and unpreserved environ- through time. We have found no evidence that the increas- ments lead to further impoverishment of the recorded ing abundance of P elements relative to S and M elements spatial and temporal distributions of taxa.