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Cambrian Phytoplankton of the Brunovistulicum – Taxonomy and Biostratigraphy
MONIKA JACHOWICZ-ZDANOWSKA Cambrian phytoplankton of the Brunovistulicum – taxonomy and biostratigraphy Polish Geological Institute Special Papers,28 WARSZAWA 2013 CONTENTS Introduction...........................................................6 Geological setting and lithostratigraphy.............................................8 Summary of Cambrian chronostratigraphy and acritarch biostratigraphy ...........................13 Review of previous palynological studies ...........................................17 Applied techniques and material studied............................................18 Biostratigraphy ........................................................23 BAMA I – Pulvinosphaeridium antiquum–Pseudotasmanites Assemblage Zone ....................25 BAMA II – Asteridium tornatum–Comasphaeridium velvetum Assemblage Zone ...................27 BAMA III – Ichnosphaera flexuosa–Comasphaeridium molliculum Assemblage Zone – Acme Zone .........30 BAMA IV – Skiagia–Eklundia campanula Assemblage Zone ..............................39 BAMA V – Skiagia–Eklundia varia Assemblage Zone .................................39 BAMA VI – Volkovia dentifera–Liepaina plana Assemblage Zone (Moczyd³owska, 1991) ..............40 BAMA VII – Ammonidium bellulum–Ammonidium notatum Assemblage Zone ....................40 BAMA VIII – Turrisphaeridium semireticulatum Assemblage Zone – Acme Zone...................41 BAMA IX – Adara alea–Multiplicisphaeridium llynense Assemblage Zone – Acme Zone...............42 Regional significance of the biostratigraphic -
£2.00 North West Mountain Rescue Team Intruder Alarms Portable Appliance Testing Approved Contractor Fixed Wire Testing
north west mountain rescue team ANNUAL REPORT 2013 REPORT ANNUAL Minimum Donation nwmrt £2.00 north west mountain rescue team Intruder Alarms Portable Appliance Testing Approved Contractor Fixed Wire Testing AA Electrical Services Domestic, Industrial & Agricultural Installation and Maintenance Phone: 028 2175 9797 Mobile: 07736127027 26b Carncoagh Road, Rathkenny, Ballymena, Co Antrim BT43 7LW 10% discount on presentation of this advert The three Tavnaghoney Cottages are situated in beautiful Glenaan in the Tavnaghoney heart of the Antrim Glens, with easy access to the Moyle Way, Antrim Hills Cottages & Causeway walking trails. Each cottage offers 4-star accommodation, sleeping seven people. Downstairs is a through lounge with open plan kitchen / dining, a double room (en-suite), a twin room and family bathroom. Upstairs has a triple room with en-suite. All cottages are wheelchair accessible. www.tavnaghoney.com 2 experience the magic of geological time travel www.marblearchcavesgeopark.com Telephone: +44 (0) 28 6634 8855 4 Contents 6-7 Foreword Acknowledgements by Davy Campbell, Team Leader Executive Editor 8-9 nwmrt - Who we are Graeme Stanbridge by Joe Dowdall, Operations Officer Editorial Team Louis Edmondson 10-11 Callout log - Mountain, Cave, Cliff and Sea Cliff Rescue Michael McConville Incidents 2013 Catherine Scott Catherine Tilbury 12-13 Community events Proof Reading Lowland Incidents Gillian Crawford 14-15 Search and Rescue Teams - Where we fit in Design Rachel Beckley 16-17 Operations - Five Days in March Photography by Graeme Stanbridge, Chairperson Paul McNicholl Anthony Murray Trevor Quinn 18-19 Snowbound by Archie Ralston President Rotary Club Carluke 20 Slemish Challenge 21 Belfast Hills Walk 23 Animal Rescue 25 Mountain Safety nwmrt would like to thank all our 28 Contact Details supporters, funders and sponsors, especially Sports Council NI 5 6 Foreword by Davy Campbell, Team Leader he north west mountain rescue team was established in Derry City in 1980 to provide a volunteer search and rescue Tservice for the north west of Northern Ireland. -
APRIL 2020 I Was Hungry and You Gave Me Something to Eat Matthew 25:35
APRIL 2020 I was hungry and you gave me something to eat Matthew 25:35 Barnabas stands alongside our Christian brothers and sisters around the world where they suffer discrimination and persecution. By providing aid through our Christian partners on the ground, we are able to maintain our overheads at less than 12% of our income. Please help us to help those who desperately need relief from their suffering. Barnabas Fund Donate online at: is a company Office 113, Russell Business Centre, registered in England 40-42 Lisburn Road, Belfast BT9 6AA www.barnabasaid.org/herald Number 04029536. Registered Charity [email protected] call: 07875 539003 Number 1092935 CONTENTS | APRIL 2020 FEATURES 12 Shaping young leaders The PCI Intern Scheme 16 Clubbing together A story from Bray Presbyterian 18 He is risen An Easter reflection 20 A steep learning curve A story from PCI’s Leaders in Training scheme 22 A shocking home truth New resource on tackling homelessness 34 Strengthening your pastoral core Advice for elders on Bible use 36 Equipping young people as everyday disciples A shocking home truth p22 Prioritising discipleship for young people 38 A San Francisco story Interview with a Presbyterian minister in California 40 Debating the persecution of Christians Report on House of Commons discussion REGULARS A San Francisco story p38 Debating the persecution of Christians p40 4 Letters 6 General news CONTRIBUTORS 8 In this month… Suzanne Hamilton is Tom Finnegan is the Senior Communications Training Development 9 My story Assistant for the Herald. Officer for PCI. In this role 11 Talking points She attends Ballyholme Tom develops and delivers Presbyterian in Bangor, training and resources for 14 Life lessons is married to Steven and congregational life and 15 Andrew Conway mum to twin boys. -
Palaeogene Marine Stratigraphy in China
LETHAIA REVIEW Palaeogene marine stratigraphy in China XIAOQIAO WAN, TIAN JIANG, YIYI ZHANG, DANGPENG XI AND GUOBIAO LI Wan, X., Jiang, T., Zhang, Y., Xi, D. & Li G. 2014: Palaeogene marine stratigraphy in China. Lethaia, Vol. 47, pp. 297–308. Palaeogene deposits are widespread in China and are potential sequences for locating stage boundaries. Most strata are non-marine origin, but marine sediments are well exposed in Tibet, the Tarim Basin of Xinjiang, and the continental margin of East China Sea. Among them, the Tibetan Tethys can be recognized as a dominant marine area, including the Indian-margin strata of the northern Tethys Himalaya and Asian- margin strata of the Gangdese forearc basin. Continuous sequences are preserved in the Gamba–Tingri Basin of the north margin of the Indian Plate, where the Palaeogene sequence is divided into the Jidula, Zongpu, Zhepure and Zongpubei formations. Here, the marine sequence ranges from Danian to middle Priabonian (66–35 ma), and the stage boundaries are identified mostly by larger foraminiferal assemblages. The Paleocene/Eocene boundary is found between the Zongpu and Zhepure forma- tions. The uppermost marine beds are from the top of the Zongpubei Formation (~35 ma), marking the end of Indian and Asian collision. In addition, the marine beds crop out along both sides of the Yarlong Zangbo Suture, where they show a deeper marine facies, yielding rich radiolarian fossils of Paleocene and Eocene. The Tarim Basin of Xinjiang is another important area of marine deposition. Here, marine Palae- ogene strata are well exposed in the Southwest Tarim Depression and Kuqa Depres- sion. -
The Carboniferous Bowland Shale Gas Study: Geology and Resource Estimation
THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION The Carboniferous Bowland Shale gas study: geology and resource estimation i © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Disclaimer This report is for information only. It does not constitute legal, technical or professional advice. The Department of Energy and Climate Change does not accept any liability for any direct, indirect or consequential loss or damage of any nature, however caused, which may be sustained as a result of reliance upon the information contained in this report. All material is copyright. It may be produced in whole or in part subject to the inclusion of an acknowledgement of the source, but should not be included in any commercial usage or sale. Reproduction for purposes other than those indicated above requires the written permission of the Department of Energy and Climate Change. Suggested citation: Andrews, I.J. 2013. The Carboniferous Bowland Shale gas study: geology and resource estimation. British Geological Survey for Department of Energy and Climate Change, London, UK. Requests and enquiries should be addressed to: Toni Harvey Senior Geoscientist - UK Onshore Email: [email protected] ii © DECC 2013 THE CARBONIFEROUS BOWLAND SHALE GAS STUDY: GEOLOGY AND RESOURCE ESTIMATION Foreword This report has been produced under contract by the British Geological Survey (BGS). It is based on a recent analysis, together with published data and interpretations. Additional information is available at the Department of Energy and Climate Change (DECC) website. https://www.gov.uk/oil-and-gas-onshore-exploration-and-production. This includes licensing regulations, maps, monthly production figures, basic well data and where to view and purchase data. -
Assessing the Chronostratigraphic Fidelity of Sedimentary Geological Outcrops in the Pliocene–Pleistocene Red Crag Formation, Eastern England
Downloaded from http://jgs.lyellcollection.org/ by guest on September 25, 2021 Research article Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2019-056 Where does the time go? Assessing the chronostratigraphic fidelity of sedimentary geological outcrops in the Pliocene–Pleistocene Red Crag Formation, eastern England Neil S. Davies1*, Anthony P. Shillito1 & William J. McMahon2 1 Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK 2 Faculty of Geosciences, Utrecht University, Princetonlaan 8a, Utrecht 3584 CB, Netherlands NSD, 0000-0002-0910-8283; APS, 0000-0002-4588-1804 * Correspondence: [email protected] Abstract: It is widely understood that Earth’s stratigraphic record is an incomplete record of time, but the implications that this has for interpreting sedimentary outcrop have received little attention. Here we consider how time is preserved at outcrop using the Neogene–Quaternary Red Crag Formation, England. The Red Crag Formation hosts sedimentological and ichnological proxies that can be used to assess the time taken to accumulate outcrop expressions of strata, as ancient depositional environments fluctuated between states of deposition, erosion and stasis. We use these to estimate how much time is preserved at outcrop scale and find that every outcrop provides only a vanishingly small window onto unanchored weeks to months within the 600–800 kyr of ‘Crag-time’. Much of the apparently missing time may be accounted for by the parts of the formation at subcrop, rather than outcrop: stratigraphic time has not been lost, but is hidden. The time-completeness of the Red Crag Formation at outcrop appears analogous to that recorded in much older rock units, implying that direct comparison between strata of all ages is valid and that perceived stratigraphic incompleteness is an inconsequential barrier to viewing the outcrop sedimentary-stratigraphic record as a truthful chronicle of Earth history. -
Late Paleozoic Sea Levels and Depositional Sequences Charles A
Western Washington University Western CEDAR Geology Faculty Publications Geology 1987 Late Paleozoic Sea Levels and Depositional Sequences Charles A. Ross Western Washington University, [email protected] June R. P. Ross Western Washington University Follow this and additional works at: https://cedar.wwu.edu/geology_facpubs Part of the Geology Commons, and the Paleontology Commons Recommended Citation Ross, Charles A. and Ross, June R. P., "Late Paleozoic Sea Levels and Depositional Sequences" (1987). Geology Faculty Publications. 61. https://cedar.wwu.edu/geology_facpubs/61 This Article is brought to you for free and open access by the Geology at Western CEDAR. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. Cushman Foundation for Foraminiferal Research, Special Publication 24, 1987. LATE PALEOZOIC SEA LEVELS AND DEPOSITIONAL SEQUENCES CHARLES A. ROSSI AND JUNE R. P. ROSS2 1 Chevron U.S.A., Inc.,P. O. BOX 1635, Houston, TX 77251 2 Department of Biology, Western Washington University, Bellingham, WA 98225 ABSTRACT studies on these changes in sea level and their paleogeographic distribution (Ross, 1979; Ross Cyclic sea level charts for the Lower and Ross, 1979, 1981a, 1981b, 1985a, 1985b) are Carboniferous (Mississippian), Middle and Upper elaborated on in this paper with charts in a Carboniferous (Pennsylvanian), and Permian show similar format to that used for Mesozoic and considerable variability in the duration and Cenozoic sea-level cyclic fluctuations by Haq, magnitude of third-order depositional sequences, Hardenbol, and Vail (1987 and this volume). and also in the position of general sea level as represented by second-order sea level. -
46.2 Comparison Between Formations Drilled
Le Pichon, X., Pautot, G., Auzende, J. M, and Olivet, J. L., Ryan, W. F. B., Hsü, K. J., et al., 1973. Initial Reports of the 1971. La Méditerranée occidentale depuis 1'Oligocène. Deep Sea Drilling Project, Volume 13: Washington (U. S. Schema d'evolution: Earth Planet. Sci. Lett., v. 13, p. 145- Government Printing Office). 152. Stoeckinger, W. T., 1976. Valencia Gulf. Offer Deadline Mauffret, A., 1976. Etude géodyamique de la marge des iles nears: Oil Gas J., March, p. 197-204; April, p. 181-183. Baléares. 46.2. COMPARISON BETWEEN FORMATIONS DRILLED AT DSDP SITE 372 IN THE WESTERN MEDITERRANEAN AND EXPOSED SERIES OF LAND G. Bizon and J. J. Bizon, Bureau d'Etudes Industrielles et Cooperation de 1'Institute Français du Pétrole, 92500 Rueil Malmaison, France and B. Biju-Duval, Institut Français du Pétrole, 92500 Rueill-Malmaison ABSTRACT Formations penetrated at Site 372 are compared with series cropping out on land in the Balearic Islands, Southern Spain, and Sardinia. The comparison is extended to wells drilled in the Gulf of Lion. The margin at Menorca and the North Balearic Provencal Basin appear to be at least of Burdigalian age. The entire Miocene is undisturbed at Site 372 in contrast to Mallorca and continental Spain where important tectonic events occurred during middle and upper Miocene. INTRODUCTION By comparing these rocks with those of Mallorca, Bourrouilh considered the age of tectonism to be Because DSDP Site 372 is located only 40 km from middle Miocene. This conclusion is questionable con- the Balearic Islands, it is logical to compare the series sidering that at Site 372 the entire Miocene is undis- penetrated at the site with land equivalents, particu- turbed. -
Climatic Shifts Drove Major Contractions in Avian Latitudinal Distributions Throughout the Cenozoic
Climatic shifts drove major contractions in avian latitudinal distributions throughout the Cenozoic Erin E. Saupea,1,2, Alexander Farnsworthb, Daniel J. Luntb, Navjit Sagooc, Karen V. Phamd, and Daniel J. Fielde,1,2 aDepartment of Earth Sciences, University of Oxford, OX1 3AN Oxford, United Kingdom; bSchool of Geographical Sciences, University of Bristol, Clifton, BS8 1SS Bristol, United Kingdom; cDepartment of Meteorology, Stockholm University, 106 91 Stockholm, Sweden; dDivision of Geological and Planetary Sciences, Caltech, Pasadena, CA 91125; and eDepartment of Earth Sciences, University of Cambridge, CB2 3EQ Cambridge, United Kingdom Edited by Nils Chr. Stenseth, University of Oslo, Oslo, Norway, and approved May 7, 2019 (received for review March 8, 2019) Many higher level avian clades are restricted to Earth’s lower lati- order avian historical biogeography invariably recover strong evi- tudes, leading to historical biogeographic reconstructions favoring a dence for an origin of most modern diversity on southern land- Gondwanan origin of crown birds and numerous deep subclades. masses (2, 6, 11). However, several such “tropical-restricted” clades (TRCs) are repre- The crown bird fossil record has unique potential to reveal sented by stem-lineage fossils well outside the ranges of their clos- where different groups of birds were formerly distributed in deep est living relatives, often on northern continents. To assess the time. Fossil evidence, for example, has long indicated that total- drivers of these geographic disjunctions, we combined ecological group representatives of clades restricted to relatively narrow niche modeling, paleoclimate models, and the early Cenozoic fossil geographic regions today were formerly found in different parts of record to examine the influence of climatic change on avian geo- – graphic distributions over the last ∼56 million years. -
Paleontology, Stratigraphy, Paleoenvironment and Paleogeography of the Seventy Tethyan Maastrichtian-Paleogene Foraminiferal Species of Anan, a Review
Journal of Microbiology & Experimentation Review Article Open Access Paleontology, stratigraphy, paleoenvironment and paleogeography of the seventy Tethyan Maastrichtian-Paleogene foraminiferal species of Anan, a review Abstract Volume 9 Issue 3 - 2021 During the last four decades ago, seventy foraminiferal species have been erected by Haidar Salim Anan the present author, which start at 1984 by one recent agglutinated foraminiferal species Emirates Professor of Stratigraphy and Micropaleontology, Al Clavulina pseudoparisensis from Qusseir-Marsa Alam stretch, Red Sea coast of Egypt. Azhar University-Gaza, Palestine After that year tell now, one planktic foraminiferal species Plummerita haggagae was erected from Egypt (Misr), two new benthic foraminiferal genera Leroyia (with its 3 species) Correspondence: Haidar Salim Anan, Emirates Professor of and Lenticuzonaria (2 species), and another 18 agglutinated species, 3 porcelaneous, 26 Stratigraphy and Micropaleontology, Al Azhar University-Gaza, Lagenid and 18 Rotaliid species. All these species were recorded from Maastrichtian P. O. Box 1126, Palestine, Email and/or Paleogene benthic foraminiferal species. Thirty nine species of them were erected originally from Egypt (about 58 %), 17 species from the United Arab Emirates, UAE (about Received: May 06, 2021 | Published: June 25, 2021 25 %), 8 specie from Pakistan (about 11 %), 2 species from Jordan, and 1 species from each of Tunisia, France, Spain and USA. More than one species have wide paleogeographic distribution around the Northern and Southern Tethys, i.e. Bathysiphon saidi (Egypt, UAE, Hungary), Clavulina pseudoparisensis (Egypt, Saudi Arabia, Arabian Gulf), Miliammina kenawyi, Pseudoclavulina hamdani, P. hewaidyi, Saracenaria leroyi and Hemirobulina bassiounii (Egypt, UAE), Tritaxia kaminskii (Spain, UAE), Orthokarstenia nakkadyi (Egypt, Tunisia, France, Spain), Nonionella haquei (Egypt, Pakistan). -
Appendix 3.Pdf
A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin Item Type Thesis or dissertation Authors Nicholls, Keith H. Citation Nicholls, K. (2019). A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin. (Doctoral dissertation). University of Chester, United Kingdom. Publisher University of Chester Rights Attribution-NonCommercial-NoDerivatives 4.0 International Download date 26/09/2021 02:37:15 Item License http://creativecommons.org/licenses/by-nc-nd/4.0/ Link to Item http://hdl.handle.net/10034/622234 International Chronostratigraphic Chart v2013/01 Erathem / Era System / Period Quaternary Neogene C e n o z o i c Paleogene Cretaceous M e s o z o i c Jurassic M e s o z o i c Jurassic Triassic Permian Carboniferous P a l Devonian e o z o i c P a l Devonian e o z o i c Silurian Ordovician s a n u a F y r Cambrian a n o i t u l o v E s ' i k s w o Ichnogeneric Diversity k p e 0 10 20 30 40 50 60 70 S 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 Number of Ichnogenera (Treatise Part W) Ichnogeneric Diversity 0 10 20 30 40 50 60 70 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 c i o 63 z 65 o e 67 a l 69 a 71 P 73 75 77 79 81 83 n 85 a i r 87 b 89 m 91 a 93 C Number of Ichnogenera (Treatise Part W) -
The Stratigraphic Architecture and Evolution of the Burdigalian Carbonate—Siliciclastic Sedimentary Systems of the Mut Basin, Turkey
The stratigraphic architecture and evolution of the Burdigalian carbonate—siliciclastic sedimentary systems of the Mut Basin, Turkey P. Bassanta,*, F.S.P. Van Buchema, A. Strasserb,N.Gfru¨rc aInstitut Franc¸ais du Pe´trole, Rueil-Malmaison, France bUniversity of Fribourg, Switzerland cIstanbul Technical University, Istanbul, Turkey Received 17 February 2003; received in revised form 18 November 2003; accepted 21 January 2004 Abstract This study describes the coeval development of the depositional environments in three areas across the Mut Basin (Southern Turkey) throughout the Late Burdigalian (early Miocene). Antecedent topography and rapid high-amplitude sea-level change are the main controlling factors on stratigraphic architecture and sediment type. Stratigraphic evidence is observed for two high- amplitude (100–150 m) sea-level cycles in the Late Burdigalian to Langhian. These cycles are interpreted to be eustatic in nature and driven by the long-term 400-Ka orbital eccentricity-cycle-changing ice volumes in the nascent Antarctic icecap. We propose that the Mut Basin is an exemplary case study area for guiding lithostratigraphic predictions in early Miocene shallow- marine carbonate and mixed environments elsewhere in the world. The Late Burdigalian in the Mut Basin was a time of relative tectonic quiescence, during which a complex relict basin topography was flooded by a rapid marine transgression. This area was chosen for study because it presents extraordinary large- scale 3D outcrops and a large diversity of depositional environments throughout the basin. Three study transects were constructed by combining stratal geometries and facies observations into a high-resolution sequence stratigraphic framework. 3346 m of section were logged, 400 thin sections were studied, and 145 biostratigraphic samples were analysed for nannoplankton dates (Bassant, P., 1999.