Ediacaran–Cambrian of Avalonian Eastern Newfoundland
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Geochemistry This
TORONTOTORONTO Vol. 8, No. 4 April 1998 Call for Papers GSA TODAY — page C1 A Publication of the Geological Society of America Electronic Abstracts Submission — page C3 Antarctic Neogene Landscapes—In the 1998 Registration Refrigerator or in the Deep Freeze? Annual Issue Meeting — June GSA Today Introduction The present Molly F. Miller, Department of Geology, Box 117-B, Vanderbilt Antarctic landscape undergoes very University, Nashville, TN 37235, [email protected] slow environmental change because it is almost entirely covered by a thick, slow-moving ice sheet and thus effectively locked in a Mark C. G. Mabin, Department of Tropical Environmental Studies deep freeze. The ice sheet–landscape system is essentially stable, and Geography, James Cook University, Townsville, Queensland 4811, Australia, [email protected] Antarctic—Introduction continued on p. 2 Atmospheric Transport of Diatoms in the Antarctic Sirius Group: Pliocene Deep Freeze Arjen P. Stroeven, Department of Quaternary Research, Stockholm University, S-106 91 Stockholm, Sweden Lloyd H. Burckle, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964 Johan Kleman, Department of Physical Geography, Stockholm University, S-106, 91 Stockholm, Sweden Michael L. Prentice, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH 03824 INTRODUCTION How did young diatoms (including some with ranges from the Pliocene to the Pleistocene) get into the Sirius Group on the slopes of the Transantarctic Mountains? Dynamicists argue for emplacement by a wet-based ice sheet that advanced across East Antarctica and the Transantarctic Mountains after flooding of interior basins by relatively warm marine waters [2 to 5 °C according to Webb and Harwood (1991)]. -
New Zealand's Genetic Diversity
1.13 NEW ZEALAND’S GENETIC DIVERSITY NEW ZEALAND’S GENETIC DIVERSITY Dennis P. Gordon National Institute of Water and Atmospheric Research, Private Bag 14901, Kilbirnie, Wellington 6022, New Zealand ABSTRACT: The known genetic diversity represented by the New Zealand biota is reviewed and summarised, largely based on a recently published New Zealand inventory of biodiversity. All kingdoms and eukaryote phyla are covered, updated to refl ect the latest phylogenetic view of Eukaryota. The total known biota comprises a nominal 57 406 species (c. 48 640 described). Subtraction of the 4889 naturalised-alien species gives a biota of 52 517 native species. A minimum (the status of a number of the unnamed species is uncertain) of 27 380 (52%) of these species are endemic (cf. 26% for Fungi, 38% for all marine species, 46% for marine Animalia, 68% for all Animalia, 78% for vascular plants and 91% for terrestrial Animalia). In passing, examples are given both of the roles of the major taxa in providing ecosystem services and of the use of genetic resources in the New Zealand economy. Key words: Animalia, Chromista, freshwater, Fungi, genetic diversity, marine, New Zealand, Prokaryota, Protozoa, terrestrial. INTRODUCTION Article 10b of the CBD calls for signatories to ‘Adopt The original brief for this chapter was to review New Zealand’s measures relating to the use of biological resources [i.e. genetic genetic resources. The OECD defi nition of genetic resources resources] to avoid or minimize adverse impacts on biological is ‘genetic material of plants, animals or micro-organisms of diversity [e.g. genetic diversity]’ (my parentheses). -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Avian Mortality at Man-Made Structures, an Annotated Bibliography
Biological Services Program FWSIOBS-78/58 July 1978 Avian Mortality at -Man-made Structures: . An Annotated Bibliography I '8/58 1nd Wildlife Service U.S. Department of the Interior !Xl&!ru~& c ~00&~©@ Susitna Joint Venture Document Number ~~OL{ · Please Return To DOGUMENT CONTROL ·).' f. t ~ -~ I I ~ .. - ; ... .. J . ~ -. ~ L;.;.,, .. ;L~i~.':-~~- ··-·~. .-.;:··-. -~ .... _-,.- ...... -. ..;.~;. •.:. < • The Biological Services Program was .established·within:the·U.S.' -Fish ·and Wildlife Seryke, to supply·scientific inforrnat·i'bn and·'meth-· odologies on key"'environmental issues which impact fish ahd w·ildlife resources and their supporting ecosystems. The mission of the Program is as follows: 1. To strengthen the Fish and Wildli.fe Service in its role as a primary sours;e .of information on national fish and wildlife resoilr<;'es;; ·'parj;.icuJ ar-ly in respect to environmenta 1 impact assessment. ' . ·- 2. To gather, analyze, and present information that \'Jill aid decision makers in the identification and resolution of problems associated with major land and water use changes. 3. To provide better ecological information and evaluation for Department of the Interior development programs, such as those relating to energy development. Information developed by the Biological Services Program is in tended for use in the planning and decision making process to prevent or minimize the impact of development on fish and wildlife. Biological Services research activities and technical assistance services are based on an analysis of the issues, the decision makers involved and their information needs, and an evaluation of the state of the art to identify information gaps and determine priorities. This is a strategy to assure that the products produced and disseminated will be timely and useful. -
Lessons from the Fossil Record: the Ediacaran Radiation, the Cambrian Radiation, and the End-Permian Mass Extinction
OUP CORRECTED PROOF – FINAL, 06/21/12, SPi CHAPTER 5 Lessons from the fossil record: the Ediacaran radiation, the Cambrian radiation, and the end-Permian mass extinction S tephen Q . D ornbos, M atthew E . C lapham, M argaret L . F raiser, and M arc L afl amme 5.1 Introduction and altering substrate consistency ( Thayer 1979 ; Seilacher and Pfl üger 1994 ). In addition, burrowing Ecologists studying modern communities and eco- organisms play a crucial role in modifying decom- systems are well aware of the relationship between position and enhancing nutrient cycling ( Solan et al. biodiversity and aspects of ecosystem functioning 2008 ). such as productivity (e.g. Tilman 1982 ; Rosenzweig Increased species richness often enhances ecosys- and Abramsky 1993 ; Mittelbach et al. 2001 ; Chase tem functioning, but a simple increase in diversity and Leibold 2002 ; Worm et al. 2002 ), but the pre- may not be the actual underlying driving mecha- dominant directionality of that relationship, nism; instead an increase in functional diversity, the whether biodiversity is a consequence of productiv- number of ecological roles present in a community, ity or vice versa, is a matter of debate ( Aarssen 1997 ; may be the proximal cause of enhanced functioning Tilman et al. 1997 ; Worm and Duffy 2003 ; van ( Tilman et al. 1997 ; Naeem 2002 ; Petchey and Gaston, Ruijven and Berendse 2005 ). Increased species rich- 2002 ). The relationship between species richness ness could result in increased productivity through (diversity) and functional diversity has important 1) interspecies facilitation and complementary implications for ecosystem functioning during resource use, 2) sampling effects such as a greater times of diversity loss, such as mass extinctions, chance of including a highly productive species in a because species with overlapping ecological roles diverse assemblage, or 3) a combination of biologi- can provide functional redundancy to maintain cal and stochastic factors ( Tilman et al. -
Geology of the Connaigre Peninsula and Adjacent
10′ 55° 00′ LEGEND 32 MIDDLE PALEOZOIC LATE NEOPROTEROZOIC 42 42 DEVONIAN LONG HARBOUR GROUP (Units 16 to 24) 86 Mo BELLEORAM GRANITE Rencontre Formation (Units 19 to 24) 47° 50′ 32 47 Grey to pink, medium- and fine-grained equigranular granite containing many small, dark-grey and green (Units 19 and 20 occur only in the northern Fortune Bay 47a to black inclusions; 47a red felsite and fine-grained area; Unit 22 occurs only on Brunette Island) 47b granite, developed locally at pluton’s margin; 47b Red micaceous siltstone and interbedded, buff-weath- 10 pink-to brown quartz-feldspar porphyry (Red Head 24 31 Porphyry) ering, quartzitic arkose and pebble conglomerate 20′ Pink, buff-weathering, medium- to coarse-grained, Be88 OLD WOMAN STOCK 23 cross-bedded, quartzitic arkose and granule to pebble Pink, medium- and coarse-grained, porphyritic biotite 42 46 23a conglomerate; locally contains red siltstone; 23a red 32 granite; minor aplite 31 23b pebble conglomerate; 23b quartzitic arkose as in 23, MAP 98-02 GREAT BAY DE L’EAU FORMATION (Units 44 and 45) containing minor amounts of red siltstone 37 9 83 Pyr 45 Grey mafic sills and flows 22 Red and grey, thin-bedded siltstone, and fine-grained 37 GEOLOGY OF THE CONNAIGRE PENINSULA 19b sandstone and interbedded buff, coarse-grained, cross 10 25 19b Pyr 81 Red, purple and buff, pebble to boulder conglomerate; bedded quartzitic arkose; minor bright-red shale and 32 25 42 44 W,Sn 91 minor green conglomerate and red and blackshale; green-grey and black-grey and black siltstone AND ADJACENT AREAS, -
Durham Research Online
Durham Research Online Deposited in DRO: 23 May 2017 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Betts, Marissa J. and Paterson, John R. and Jago, James B. and Jacquet, Sarah M. and Skovsted, Christian B. and Topper, Timothy P. and Brock, Glenn A. (2017) 'Global correlation of the early Cambrian of South Australia : shelly fauna of the Dailyatia odyssei Zone.', Gondwana research., 46 . pp. 240-279. Further information on publisher's website: https://doi.org/10.1016/j.gr.2017.02.007 Publisher's copyright statement: c 2017 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Accepted Manuscript Global correlation of the early Cambrian of South Australia: Shelly fauna of the Dailyatia odyssei Zone Marissa J. -
Proposed Global Standard Stratotype-Section And
PROPOSED GLOBAL STANDARD STRATOTYPE-SECTION AND POINT FOR THE DRUMIAN STAGE (CAMBRIAN) Prepared for the International Subcommission on Cambrian Stratigraphy by: Loren E. Babcock School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] Richard A. Robison Department of Geology, University of Kansas Lawrence, KS 66045, USA [email protected] Margaret N. Rees Department of Geoscience University of Nevada, Las Vegas Las Vegas, NV 89145, USA [email protected] Peng Shanchi Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences 39 East Beijing Road, Nanjing 210008, China [email protected] Matthew R. Saltzman School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] 31 July 2006 CONTENTS Introduction …………………………………………………………………………. 2 Proposal: Stratotype Ridge, Drum Mountains (Millard County, Utah, USA) as the GSSP for the base of the Drumian Stage ……………………………………………………. 3 1. Stratigraphic rank of the boundary …………………..…………………………… 3 2. Proposed GSSP – geography and physical geology ……………………………… 3 2.1. Geographic location …………………………………………………...….. 3 2.2. Geological location ………………..……………………...…………...….. 4 2.3. Location of level and specific point ……………………..……………...… 4 2.4. Stratigraphic completeness ………………...……………………………… 5 2.5. Thickness and stratigraphic extent …………………...……………...……. 5 2.6. Provisions for conservation, protection, and accessibility ……………..…. 5 3. Motivation for selection of the boundary level and of the potential stratotype section ………………………………………………………………………………. 6 3.1. Principal correlation event (marker) at GSSP level ………...…………..… 6 3.2. Potential stratotype section …………………………………………....….. 7 3.3. Demonstration of regional and global correlation ………………………... 8 3.3.1. Agnostoid trilobite biostratigraphy ………………………………… 9 3.3.2. Polymerid trilobite biostratigraphy …………....…………….……. -
Rare Birds of Vancouver Island: May 1, 2018: 3Rd Edition Compiled by Rick Toochin, Paul Levesque, Jamie Fenneman, and Don Cecile
Rare Birds of Vancouver Island: rd May 1, 2018: 3 Edition Compiled by Rick Toochin, Paul Levesque, Jamie Fenneman, and Don Cecile. Comments? Contact E-Fauna BC Area Covered This is a list of all known, published and unpublished records of casual and accidental species that have been reported on and around Vancouver Island. This list of records covers all of the land mass of Vancouver Island from Cape Scott at the northern most point of Vancouver Island to East Sooke Park which is the southern most point of land on Vancouver Island. The rare bird records found within this document also cover the waters that surround all of Vancouver Island. On the west coast this extends out to the 200 mile limit of what is considered Canadian waters. On the northern part of Vancouver Island this extends up into Queen Charlotte Sound down the Johnstone Strait to the middle of the Strait of Georgia south to the International Boundary and west through the Juan de Fuca Strait following the International Boundary back out to the 200 mile edge. The islands included on this list area includes Triangle Island and the Scott Islands at the northwest tip of the island. The list also includes the islands off the northeast coast of Vancouver Island such as Hope Island, Nigei Island, Hurst Island south to Malcolm Island and Hanson Island. Then the boundary travels south through Johnstone Strait including Sonora Island, Stuart Island, Quadra Island, Maurelle Island, Reed Island, Cortes Island, Martina Island, Hernando Island, Savary Island, Mitlenach Island, Harwood Island, Texada Island and Lasquetti Islands in the northern Strait of Georgia. -
Abstract Volume
https://doi.org/10.3301/ABSGI.2019.04 Milano, 2-5 July 2019 ABSTRACT BOOK a cura della Società Geologica Italiana 3rd International Congress on Stratigraphy GENERAL CHAIRS Marco Balini, Università di Milano, Italy Elisabetta Erba, Università di Milano, Italy - past President Società Geologica Italiana 2015-2017 SCIENTIFIC COMMITTEE Adele Bertini, Peter Brack, William Cavazza, Mauro Coltorti, Piero Di Stefano, Annalisa Ferretti, Stanley C. Finney, Fabio Florindo, Fabrizio Galluzzo, Piero Gianolla, David A.T. Harper, Martin J. Head, Thijs van Kolfschoten, Maria Marino, Simonetta Monechi, Giovanni Monegato, Maria Rose Petrizzo, Claudia Principe, Isabella Raffi, Lorenzo Rook ORGANIZING COMMITTEE The Organizing Committee is composed by members of the Department of Earth Sciences “Ardito Desio” and of the Società Geologica Italiana Lucia Angiolini, Cinzia Bottini, Bernardo Carmina, Domenico Cosentino, Fabrizio Felletti, Daniela Germani, Fabio M. Petti, Alessandro Zuccari FIELD TRIP COMMITTEE Fabrizio Berra, Mattia Marini, Maria Letizia Pampaloni, Marcello Tropeano ABSTRACT BOOK EDITORS Fabio M. Petti, Giulia Innamorati, Bernardo Carmina, Daniela Germani Papers, data, figures, maps and any other material published are covered by the copyright own by the Società Geologica Italiana. DISCLAIMER: The Società Geologica Italiana, the Editors are not responsible for the ideas, opinions, and contents of the papers published; the authors of each paper are responsible for the ideas opinions and con- tents published. La Società Geologica Italiana, i curatori scientifici non sono responsabili delle opinioni espresse e delle affermazioni pubblicate negli articoli: l’autore/i è/sono il/i solo/i responsabile/i. ST3.2 Cambrian stratigraphy, events and geochronology Conveners and Chairpersons Per Ahlberg (Lund University, Sweden) Loren E. -
The Earliest Bioturbators As Ecosystem Engineers
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 Engineering the Cambrian explosion: the earliest bioturbators as ecosystem engineers LIAM G. HERRINGSHAW1,2*, RICHARD H. T. CALLOW1,3 & DUNCAN MCILROY1 1Department of Earth Sciences, Memorial University of Newfoundland, Prince Philip Drive, St John’s, NL, A1B 3X5, Canada 2Geology, School of Environmental Sciences, University of Hull, Cottingham Road, Hull HU6 7RX, UK 3Statoil ASA, Stavanger 4035, Norway *Correspondence: [email protected] Abstract: By applying modern biological criteria to trace fossil types and assessing burrow mor- phology, complexity, depth, potential burrow function and the likelihood of bioirrigation, we assign ecosystem engineering impact (EEI) values to the key ichnotaxa in the lowermost Cambrian (Fortunian). Surface traces such as Monomorphichnus have minimal impact on sediment properties and have very low EEI values; quasi-infaunal traces of organisms that were surficial modifiers or biodiffusors, such as Planolites, have moderate EEI values; and deeper infaunal, gallery biodiffu- sive or upward-conveying/downward-conveying traces, such as Teichichnus and Gyrolithes, have the highest EEI values. The key Cambrian ichnotaxon Treptichnus pedum has a moderate to high EEI value, depending on its functional interpretation. Most of the major functional groups of mod- ern bioturbators are found to have evolved during the earliest Cambrian, including burrow types that are highly likely to have been bioirrigated. In fine-grained (or microbially bound) sedimentary environments, trace-makers of bioirrigated burrows would have had a particularly significant impact, generating advective fluid flow within the sediment for the first time, in marked contrast with the otherwise diffusive porewater systems of the Proterozoic. -
Garnish Burin – Marystown
Burin Peninsula Voluntary Clusters Project Directory of Nonprofit and Voluntary Organizations Areas including: Placentia West Fortune Bay East Grand Bank - Fortune Frenchman’s Cove - Garnish Burin – Marystown Online Version Directory of Nonprofit and Voluntary Organizations on the Burin Peninsula Community Sector Council Newfoundland and Labrador The Community Sector Council Newfoundland and Labrador (CSC) is a leader in the voluntary community sector in Canada. Its mission is to promote the integration of social and economic development, encourage citizen engagement and provide leadership in shaping public policies. Our services include conducting research to help articulate the needs of the voluntary community sector and delivery of training to strengthen organizations and build the skills of staff and volunteers. Acknowledgements Prepared with the assistance of Trina Appleby, Emelia Bartellas, Fran Locke, Jodi McCormack, Amelia White, and Louise Woodfine. Many thanks to the members of the Burin Peninsula Clusters Pilot Advisory Committee for their support: Kimberley Armstrong, Gord Brockerville, Albert Dober, Everett Farwell, Con Fitzpatrick, Mike Graham, Elroy Grandy, Charles Hollett, Ruby Hoskins, Kevin Lundrigan, Joanne Mallay-Jones, Russ Murphy, and Sharon Snook. Disclaimer The listing of a particular service or organization should not be taken to mean an endorsement of that group or its programs. Similarly, omissions and inclusions do not necessarily reflect editorial policy. Also, while many groups indicated they have no problem being included in a version of the directory, some have requested to be omitted from an online version. Copyright © 2011 Community Sector Council Newfoundland and Labrador. All rights reserved. Reproduction in whole, or in part, is forbidden without written permission.