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The First International Conodont SymposiumJuly 12 - 30, 2006 |
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No formal technical sessions are scheduled for Wednesday, July 19. Instead a day-long field-excursion and a visit to the collections of the NHM have been arranged. It may also be possible to provide bench space and microscopes for informal specimen based discussion, should there be demand for this (contact the organisers - ICOS2006@leicester.ac.uk). Short Field Excursion: Lower Carboniferous, North Staffordshire. Leaders: Patrick Cossey (University of Staffordshire) and Mark Purnell. This trip will visit two or three localities which expose Lower Carboniferous sections on the margins of the beautiful Peak District National Park. Localities to be visited will include Brown End Quarry, of early Visean age, and Cauldon Railway Cutting, of Serpukhovian age. Both localities yield some rich conodont faunas; the Cauldon fauna (which also includes abundant micro-remains of other vertebrates) was reported in Higgins (1975, Conodont zonation of the Late Visean-early Westphalian strata of the south and central Pennines of northern England. Bull. Geol. Surv. of Great Britain, 53, 1-90). There may also be opportunities to visit nearby Dovedale and the fantastic Yew Tee Inn. Day trip to the Natural History Museum, London. Leader: Giles Miller. Visit one of the world's best known museums; an opportunity to go behind the scenes and examine conodont collections, including material deposited by Hinde, Higgins and large collections donated by Austin. For more information go to: http://www.nhm.ac.uk/research-curation/projects/conodonts/. Provisional itinerary Workshop 1 Conodont Bodies and Skeletons An opportunity to examine and discuss specimens preserving conodont soft tissues and articulated skeletons, including much of the best material from around the world. Excursion 1: The Carboniferous of Ireland July 12 - 16 (pre-meeting) This field trip will focus on Mississippian (Carboniferous) rocks of the Dublin Basin and Hook Head, County Wexford. The Dublin Basin provides sections (mainly coastal) of the late Tournaisian (in a shelf/ramp setting) and all of the Visean (in both basinal and shelf settings). The basin/shelf margin is preserved and the sedimentology of both shelf and basinal carbonates (and less abundant siliciclastics) is exciting. Conodonts occur at many horizons together with foraminiferans and macrofossils. Current research activity includes identification of the Tournaisian/Visean boundary in both shelf and basinal settings. Hook Head provides a spectacular section from early Tournaisian redbeds and shallow marine carbonates and siliciclastics through progressively deeper water limestones and shales (youngest part of the Polygnathus communis carina Zone in the highest preserved beds). Conodonts from Hook Head were described by Johnston and Higgins (1981; Conodont faunas from the Lower Carboniferous rocks at Hook Head, County Wexford, Journal of Earth Sciences of the Royal Dublin Society, 4, 83-96). Outline Itinerary Accommodation Hostels: Barnacles Temple Bar Hostel, 19 Temple Lane+353 1 6716277 www.barnacles.ie Hotels: Harcourt Hotel, Harcourt Street +353 1 4783677www.harcourthotel.ie Holiday Inn, Pearse Street +353 1 6700366 www.holidayinndublin.ie Trinity Capital Hotel, Pearse Street +353 1 6481100 www.trinitycapitalhotel.com Trinity Lodge, 12 Sth. Frederick Street +353 1 6170900 www.trinitylodge.com Stauntons on the Green, St Stephens Green +353 1 4782300 www.stauntonsonthegreen.ie Jurys Inn Christchurch, Christchurch +353 1 6070000 www.jurysdoyle.com TCD Student rooms
Trinity College student rooms, may be on or off campus Excursion 2: Iapetus - from coast to coast July 22 - 27 The trip will commence by looking at the Ordovician-Silurian succession in the Lake District, including an examination of the Ashgill in its type area. We will then cross the Scotland-England border, marking the leap from Avalonian to Laurentian crust, with the next stops at deep water Ordovician localities in the Southern Uplands, where current controversies over the tectonic interpretation of the Southern Uplands and Midland Valley terranes will be discussed. Crossing the Midland Valley of Scotland, the Neoproterozoic Dalradian Supergroup will be traversed from the Highland Boundary Fault, where obducted Ordovician ocean floor and islands with shallow water Laurentian conodont faunas can be seen at Dounans, north to the Great Glen fault and Loch Ness. We will then continue northward across the Moine thrust belt, where Neoproterozoic metasediments are thrust over the Laurentian foreland, to end the trip on the shoreline of Laurentia at the classic Cambro-Ordovician sections in Durness. In addition to providing the opportunity to sample conodont localities described by Higgins, Bergström, Ethington, Lindström, Armstrong and Orchard, the trip will also consider the history of geological exploration in this region, together with current interpretations and controversies regarding the margins of Iapetus, its constituent terranes and the final closure of the ocean in the Silurian. The trip will traverse some of the most scenic parts of northern England and Scotland, and the majority of localities will be close to the road. Numbers will be limited to 25-30 participants and accommodation will be in a mixture of hotels and guest houses. Outline itinerary |
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