DOCSLIB.ORG

University-Wide Research, Scholarship, and Creative Activity

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
University-Wide Research, Scholarship, and Creative Activity California State University Stanislaus Research Compendium 2008‐2009 California State University, Stanislaus University‐wide Research, Scholarship, and Creative Activity June, 1 2008 ‐ May 31, 2009 Activity No. ACTIVITY COA CBA COE CHHS CHSS CNS LIBR Totals 1 Books and Monographs 2 0 2 1 5 0 0 10 2 Book Chapters 0 4 8 5 15 5 0 37 3 Published Articles in Professional Journals 0 26 12 11 34 16 1 100 4 Published Case Studies w/Teaching Notes 0 0 0 0 0 0 0 0 5 Editorship 0 1 3 1 7 2 0 14 6 Editorial and Review Board Memberships 0 6 5 2 23 0 0 36 7 Grants 5 0 8 7 51 86 1 158 8 Published Computer Software 0 0 0 0 0 1 0 1 9 Published Curriculum Materials 0 0 0 0 4 0 0 4 10 Published Reviews of Books & Software 0 1 0 0 13 1 7 22 11 Conference Presentations 5 41 45 16 101 40 0 248 12 Conference Participation 6 12 10 3 35 12 2 80 13 Conference Proceedings 0 13 12 2 3 3 0 33 14 K‐12 School‐based Activities 18 0 21 1 10 22 0 72 15 Exhibits and Performances 119 1 0 1 13 9 0 143 16 Consultant 4 0 2 2 12 10 0 30 17 Reviewer 1 14 5 10 20 21 0 71 18 Educational media production 0 2 0 0 1 0 0 3 19 Non‐Refereed Publications 8 0 3 0 12 11 0 34 20 Literature Citations 0 54 1 15 5 71 1 147 21 Program and Curricular Dev. and Asses. 6 1 4 4 24 2 0 41 22 Published Maps 0 0 0 0 0 0 0 0 23 Published Abstract and Encycl. Articles 0 0 0 0 11 0 0 11 24 Other 26 9 18 5 63 15 1 138 25 Recognitions and Awards: University 1 4 0 1 11 3 0 20 Civic or Service Organization 5 0 0 4 1 1 0 11 Disciplinary 1 0 0 0 1 2 0 4 Scholarly Prizes and Honors 0 5 0 1 3 0 0 9 26 Directed students in research 17 1 11 14 27 9 0 78 27 Supervised students as research assistants 5 1 5 10 7 22 0 50 28 Student Masterʹs Theses/Projects 2 1 58 63 7 1 132 29 CSU Student Research Competition 0 0 2 5 11 8 26 College Totals 231 197 235 184 530 373 13 1763 Faculty Response Percent 71% 63% 43% 34% 67% 42% 44% California State University, Stanislaus Faculty Research, Scholarship, and Creative Activity Summary Report June 1, 2008 ‐ May 31, 2009 College Arts Number of Faculty 24 Number of Faculty Responses 17 (71 percent) 1. Books and Monographs ‐ 2 2. Book Chapters ‐ 0 3. Published Articles in Professional Journals (refereed or non‐refereed) ‐ 0 4. Published Case Studies with Teaching Notes ‐ 0 5. Editorship (regular or guest) ‐ 0 6. Editorial and Review Board Memberships ‐ 0 7. Grants (applied for/funded; university, local, state, federal, private, or corporate) ‐ 5 8. Published Computer Software ‐ 0 9. Published Curriculum Materials ‐ 0 10. Published Reviews of Books and Software ‐ 0 11. Conference Presentations (paper, research, or workshop) ‐ 5 12. Conference Participation (discussant, chair, or moderator) ‐ 6 13. Conference Proceedings ‐ 0 14. K‐12 School‐based Activities (workshops, presentations, or consultant) ‐ 18 15. Exhibits and Performances ‐ 119 16. Consultant (to businesses, agencies, or other external groups) ‐ 4 17. Reviewer (conference papers, journal articles, books, or software) ‐ 1 18. Educational Media Production ‐ 0 19. Non‐Refereed Publications (newspaper or magazine articles) ‐ 8 20. Literature Citations (your work in the work of others) ‐ 0 21. Program and Curricular Development and Assessment ‐ 6 22. Published Maps ‐ 0 23. Published Abstracts and Encyclopedia Articles (refereed or non‐refereed) ‐ 0 24. Other (please specify) – Online article accepted for publication ‐ 26 25. Recognitions and Awards: University ‐ 1 Disciplinary ‐ 1 Civic or Service Organization ‐ 5 Scholarly Prizes and Honors ‐ 0 26. Directed students in their research culminating into either a publication, presentation, or both ‐ 17 27. Supervised students as research assistants in your research, scholarship, or creative activity ‐ 5 28. Student Master’s Theses / Projects ‐ 2 29. CSU Student Research Competition (Campus and State‐wide) ‐ 0 California State University, Stanislaus Faculty Research, Scholarship, and Creative Activity Detailed Report June 1, 2008 ‐ May 31, 2009 College Arts Number of Faculty 24 Number of Faculty Responses 17 (71 percent) 1. Books and Monographs ‐ 2 Nevala, Andrew. Music. Latin Jazz Techniques for the Music Educator. Boulder: University 1. of Colorado, 2009. Nevala, Andrew. Music. The Influence of Jazz and Impressionistic Ideals Found in the Music 2. of Claude Debussy, Darius Mihaud, Maurice Ravel, Bix Beiderbecke, Art Tatum and Bill Evans. Boulder: University of Colorado, 2009. 2. Book Chapters ‐ 0 3. Published Articles in Professional Journals (refereed or non‐refereed) ‐ 0 4. Published Case Studies with Teaching Notes ‐ 0 5. Editorship (regular or guest) ‐ 0 6. Editorial and Review Board Memberships ‐ 0 7. Grants (applied for/funded; university, local, state, federal, private, or corporate) ‐ 5 Davies, Daniel. Music. Research Grant. “Arts Grant,” funded by Turlock Target Store 1. (corporate). DeCocker, Dean. Art. RSCA Grant. “Exhibition Funding,” funded by CSU Stanislaus 2. (university). Gomula, Jessica. Art. Research Grant. “Building Imagination,” funded by Creative 3. Work Fund (private). Olivant, David. Art. RSCA Grant. “Studio Equipment,” funded by CSU Stanislaus 4. (university). Thomas, Stephen. Music. Faculty Development Center Mini‐grant. “Grant to Attend 5. the Golandsky Institute Berkeley Seminar on the Taubman Approach to Piano Playing,” funded by CSU Stanislaus (university). 8. Published Computer Software ‐ 0 9. Published Curriculum Materials ‐ 0 10. Published Reviews of Books and Software ‐ 0 11. Conference Presentations (paper, research, or workshop) ‐ 5 Kavasch, Deborah. Music. “Meet the Composer.” Workshop at John Donald Robb 1. Symposium, Albuquerque, NM, March/April 2009. Mayer, John. Theatre. “Chicago Style Improvisation.” Workshop at Kennedy Center 2. American College Theatre Festival, Fullerton, CA, February 2009. Nevala, Andrew. Music. “Nocturne”and “Serpentina.” Workshop at 2008 Society of 3. Composers, Inc. Region VIII Conference, Turlock, CA, November 2008. Weddle, John. Music. “Performance Techniques for Players and Conductors.” 4. Workshop at California Music Educators Conference, Sacramento, CA, March 2009. Weddle, John. Music. “Quality Music Without Excessive Technical Demands.” 5. Workshop at College Band Director’s National Association Conference, Reno, NV, March 2009. 12. Conference Participation (discussant, chair, or moderator) ‐ 6 Gomula, Jessica. Art. Discussant. Summit on Digital Democracy in Exhibit Design, Tech 1. Museum of Innovation, San Jose, CA, June 2008. Kavasch, Deborah. Music. Chair. 2008 Society of Composers, Inc. Region VIII 2. Conference, Turlock, CA, October/November 2008. Mayer, John. Theatre. Moderator. Kennedy Center American College Theatre Festival, 3. Fullerton, CA, February 2009. Mayer, John. Theatre. Moderator. Faculty Athletic Representative Association, San 5. Diego, CA, November 2008. Mayer, John. Theatre. Moderator. Division II Faculty Athletic Representative Fellows 4. Conference, Indianapolis, IN, October 2008. 6. Wiggett, Joseph. Music. Discussant. Vocal Pedagogy Seminar, Reno, NV, March 2009. 13. Conference Proceedings ‐ 0 14. K‐12 School‐based Activities (workshops, presentations, or consultant) ‐ 18 Davies, Daniel. Music. Consultant. California Music Educators Association Solo and 1. Ensemble Festival. CSU Stanislaus. Turlock, CA, March 2009. Davies, Daniel. Music. Workshop. Cello Workshop for Visalia‐area String Teachers. 2. Visalia, CA, February 2009. Davies, Daniel. Music. Workshop. Cello Master Class. College of the Sequoias. Visalia, 3. CA, February 2009. Davies, Daniel. Music. Workshop. Cello Section Coaching. Modesto Youth Symphony 4. Orchestra. Turlock, CA, November 2008. Davies, Daniel. Music. Workshop. String Coaching. Turlock High School. Turlock, CA, 5. September 2008. Davies, Daniel. Music. Consultant. Summer Music at Stanislaus. CSU Stanislaus. 6. Turlock, CA, June 2008. Nevala, Andrew. Music. Workshop/Presenter. Stanislaus Youth Jazz Orchestra. CSU 7. Stanislaus. Turlock, CA, October 2008‐May 2009. Nevala, Andrew. Music. Judge/Reviewer. 12th Annual Sylvia M. Ghiglieri Piano 8. Competition. CSU Stanislaus. Turlock, CA, May 2009. Nevala, Andrew. Music. Workshop/Judge/Reviewer. California Music Educators 9. Association Jazz Festival. California Music Educators Association. Hanford, CA, March 2009. Nevala, Andrew. Music. Workshop/Presenter/Consultant/Judge/Reviewer. CSU 10. Stanislaus Jazz Festival. CSU Stanislaus. Turlock, CA, February 2009. Nevala, Andrew. Music. Workshop/Consultant. Davis High School Jazz Ensemble. 11. Davis High School. Modesto, CA, January 2009. Nevala, Andrew. Music. Workshop/Judge/Reviewer. Inter‐American Piano Festival. 12. CSU Stanislaus. Turlock, CA, January 2009. Nevala, Andrew. Music. Workshop/Judge/Reviewer. Folsom High School Jazz Festival. 13. Folsom High School. Folsom, CA, January 2009. Nevala, Andrew. Music. Workshop/Presenter/Consultant. Lodi High School Jazz 14. Ensemble. Lodi High School. Lodi, CA, December 2008. Nevala, Andrew. Music. Workshop/Judge/Reviewer. CSU Sacramento Jazz Festival. 15. CSU Sacramento. Sacramento, CA, December 2008. Nevala, Andrew. Music. Workshop/Judge/Reviewer. Delta College Jazz Festival. Delta 16. College. Stockton, CA, December 2008. Nevala, Andrew. Music. Workshop/Consultant. Pitman High School Jazz Ensemble. 17. Pitman High School. Turlock, CA, October 2008. O’Donnell, Jerome. Theatre. Workshop/Presenter. YES Company. Modesto, CA, 2008‐ 18. 09. 15. Exhibits and Performances ‐ 119 Broadwater, Eric. Theatre. Exhibit. Child’s Play Scene Design. CSU Stanislaus, Turlock, 1. CA, March 2009. Broadwater, Eric. Theatre. Exhibit. A Christmas Carol Scene Design. CSU Stanislaus, 2. Turlock, CA, December 2008. Broadwater, Eric. Theatre. Exhibit. Crimes of the Heat Scene Design. CSU Stanislaus, 3. Turlock, CA, September 2009. Davies, Daniel. Music. Performance. Ode to Joy. Modesto Symphony Orchestra, 4. Modesto, CA, May 2009. Davies, Daniel. Music. Performance. In the Shadows. Modesto Symphony Orchestra, 5. Modesto, CA, April 2009. Davies, Daniel. Music. Performance. Solo Recital. CSU Stanislaus, Turlock, CA, April 6. 2009. Davies, Daniel. Music. Performance. Casey at the Bat.
Load more

Recommended publications
  • New Theropod, Thyreophoran, and Small Sauropod Tracks from the Middle Jurassic Bagå Formation, Bornholm, Denmark
    New theropod, thyreophoran, and small sauropod tracks from the Middle Jurassic Bagå Formation, Bornholm, Denmark JESPER MILÀN Milàn, J. 2011. New theropod, thyreophoran, and small sauropod tracks from the Middle Jurassic Bagå Formation, Bornholm, Denmark © 2011 by Bulletin of the Geological Society of Denmark, Vol. 59, pp. 51–59. ISSN 0011–6297. (www.2dgf.dk/publikationer/bulletin) https://doi.org/10.37570/bgsd-2011-59-06 Three new dinosaur tracks are described from the Middle Jurassic Bagå Formation of Bornholm, Denmark. The tracks are all preserved as natural casts on the underside of fluvial sandstone blocks originating from the old Hasle Klinkefabrik’s clay pit, now called Pyritsøen. The new tracks are from a medium-sized theropod, a thyreophoran, and a small sauropod. Together with a thyreophoran track and large sauropod tracks described in 2005, the Middle Jurassic dinosaur fauna of Bornholm now comprises theropods, two sizes of sauropods and at least one type of thyreophoran dinosaur. This is important additional data for the very scarce Middle Jurassic dinosaurian skeletal record of Europe. Received 22 November 2010 Accepted in revised form Key words: Dinosaur fauna, trace fossils, Middle Jurassic, theropod, thyreophoran, sauropod. 21 September 2011 Published online Jesper Milàn [[email protected]], GeomuseumFaxe, Østsjællands Museum, Østervej 2, DK-4640 Faxe, 30 September 2011 Denmark. Also Department of Geography and Geology, University of Copenhagen, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark. Remains of Mesozoic terrestrial vertebrates are scarce Dinosaur remains are more commonly encountered in Denmark and have so far only been found in the in the southern part of Sweden, where numerous di- few Mesozoic outcrops along the west and southwest nosaur tracks and trackways of theropod dinosaurs, a coast of the Baltic island of Bornholm (Fig.
    [Show full text]
  • Tennant Et Al AAM.Pdf
    Zoological Journal of the Linnean Society Evolutionary relations hips and systematics of Atoposauridae (Crocodylomorpha: Neosuchia): implications for the rise of Eusuchia Journal:For Zoological Review Journal of the Linnean Only Society Manuscript ID ZOJ-08-2015-2274.R1 Manuscript Type: Original Article Bayesian, Crocodiles, Crocodyliformes < Taxa, Implied Weighting, Laurasia Keywords: < Palaeontology, Mesozoic < Palaeontology, phylogeny < Phylogenetics Note: The following files were submitted by the author for peer review, but cannot be converted to PDF. You must view these files (e.g. movies) online. S1 Atoposaurid character matrix.nex Page 1 of 167 Zoological Journal of the Linnean Society 1 2 3 1 Abstract 4 5 2 Atoposaurids are a group of small-bodied, extinct crocodyliforms, regarded as an important 6 3 component of Jurassic and Cretaceous Laurasian semi-aquatic ecosystems. Despite the group being 7 8 4 known for over 150 years, the taxonomic composition of Atoposauridae and its position within 9 5 Crocodyliformes are unresolved. Uncertainty revolves around their placement within Neosuchia, in 10 11 6 which they have been found to occupy a range of positions from the most basal neosuchian clade to 12 13 7 more crownward eusuchians. This problem stems from a lack of adequate taxonomic treatment of 14 8 specimens assigned to Atoposauridae, and key taxa such as Theriosuchus have become taxonomic 15 16 9 ‘waste baskets’. Here, we incorporate all putative atoposaurid species into a new phylogenetic data 17 10 matrix comprising 24 taxa scored for 329 characters. Many of our characters are heavily revised or 18 For Review Only 19 11 novel to this study, and several ingroup taxa have never previously been included in a phylogenetic 20 21 12 analysis.
    [Show full text]
  • Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal)
    Alexandre Renaud Daniel Guillaume Licenciatura em Biologia celular Mestrado em Sistemática, Evolução, e Paleobiodiversidade Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal) Dissertação para obtenção do Grau de Mestre em Paleontologia Orientador: Miguel Moreno-Azanza, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Co-orientador: Octávio Mateus, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Júri: Presidente: Prof. Doutor Paulo Alexandre Rodrigues Roque Legoinha (FCT-UNL) Arguente: Doutor Hughes-Alexandres Blain (IPHES) Vogal: Doutor Miguel Moreno-Azanza (FCT-UNL) Júri: Dezembro 2018 MICROVERTEBRATES OF THE LOURINHÃ FORMATION (LATE JURASSIC, PORTUGAL) © Alexandre Renaud Daniel Guillaume, FCT/UNL e UNL A Faculdade de Ciências e Tecnologia e a Universidade Nova de Lisboa tem o direito, perpétuo e sem limites geográficos, de arquivar e publicar esta dissertação através de exemplares impressos reproduzidos em papel ou de forma digital, ou por qualquer outro meio conhecido ou que venha a ser inventado, e de a divulgar através de repositórios científicos e de admitir a sua cópia e distribuição com objetivos educacionais ou de investigação, não comerciais, desde que seja dado crédito ao autor e editor. ACKNOWLEDGMENTS First of all, I would like to dedicate this thesis to my late grandfather “Papi Joël”, who wanted to tie me to a tree when I first start my journey to paleontology six years ago, in Paris. And yet, he never failed to support me at any cost, even if he did not always understand what I was doing and why I was doing it. He is always in my mind. Merci papi ! This master thesis has been one-year long project during which one there were highs and lows.
    [Show full text]
  • Weathering Profiles and Clay Mineralogical Developments, Bornholm, Denmark
    Weathering profiles and clay mineralogical developments, Bornholm, Denmark Pingchuan Tan1, 2, Nikolas Oberhardt1, Henning Dypvik1,2, Lars Riber1, Ray E. Ferrell Jr3. 1 Department of Geoscience, University of Oslo, P.O.BOX 1047, Blindern, NO-0316 Oslo, Norway 2 Centre for Earth Evolution and Dynamics, University of Oslo, P.O.BOX 1028, Blindern, NO-0315 Oslo, Norway 3 Department of Geology & Geophysics, Louisiana State University, Baton Rouge, LA, 70803, USA Corresponding author – Pingchuan Tan: [email protected] ABSTRACT Saprock-saprolite associations were studied by field and laboratory methods (optical microscopy, X-ray powder diffraction, scanning electron microscopy, electron microprobe) in order to describe regolith development in the crystalline rocks of the Nygård kaolin pit (Bornholm, Denmark). The clay sequences and stages of porosity development are similar to those observed for reservoir rocks from the Utsira High (Riber, L., Dypvik, H., Sørlie, R. and Ferrell, R. (2016) Clay minerals in deeply buried paleoregolith profiles, Norwegian North Sea. Clays and Clay Minerals, in press). The weathering of the parent granite began before the end of the Mesozoic. Two stages of syn- /pre-burial alteration, followed by diagenesis during burial, and then post-uplift weathering have been recognized. In stage Ι, plagioclase and some biotite (biotite-vermiculite-kaolinite) reacted to form elongate booklets of highly-ordered kaolinite or smaller, blocky pseudohexagonal crystals. Stage II represented more extreme weathering developed along local fracture systems. The higher potential for fluid flow in the fractures caused highly-ordered kaolinite to alter to halloysitic, poorly- ordered kaolinite. Plagioclase, biotite, and K-feldspar continued to interact with formation water and formed additional quantities of secondary clay minerals.
    [Show full text]
  • Small Ornithopod Dinosaur Tracks And
    LJMU Research Online Milàn, J, Falkingham, PL and Mueller-Töwe, IJ Small ornithopod dinosaur tracks and crocodilian remains from the Middle Jurassic Bagå Formation, Bornholm, Denmark: Important additions to the rare Middle Jurassic vertebrate faunas of Northern Europe http://researchonline.ljmu.ac.uk/id/eprint/14014/ Article Citation (please note it is advisable to refer to the publisher’s version if you intend to cite from this work) Milàn, J, Falkingham, PL and Mueller-Töwe, IJ (2020) Small ornithopod dinosaur tracks and crocodilian remains from the Middle Jurassic Bagå Formation, Bornholm, Denmark: Important additions to the rare Middle Jurassic vertebrate faunas of Northern Europe. Bulletin of the Geological LJMU has developed LJMU Research Online for users to access the research output of the University more effectively. Copyright © and Moral Rights for the papers on this site are retained by the individual authors and/or other copyright owners. Users may download and/or print one copy of any article(s) in LJMU Research Online to facilitate their private study or for non-commercial research. You may not engage in further distribution of the material or use it for any profit-making activities or any commercial gain. The version presented here may differ from the published version or from the version of the record. Please see the repository URL above for details on accessing the published version and note that access may require a subscription. For more information please contact [email protected] http://researchonline.ljmu.ac.uk/ BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK · VOL. 68 · 2020 Small ornithopod dinosaur tracks and crocodilian remains from the Middle Jurassic Bagå Formation, Bornholm, Denmark: Important additions to the rare Middle Jurassic vertebrate faunas of Northern Europe JESPER MILÀN, PETER L.
    [Show full text]
  • Dinosaur Tracks in Lower Jurassic Coastal Plain Sediments (Sose Bugt Member, Rønne Formation) on Bornholm, Denmark
    Dinosaur tracks in Lower Jurassic coastal plain sediments (Sose Bugt Member, Rønne Formation) on Bornholm, Denmark LARS B. CLEMMENSEN, JESPER MILAN, GUNVER K. PEDERSEN, ANNE B. JOHANNESEN AND CONNIE LARSEN Clemmensen, L.B., Milan, J., Pedersen, G.K., Johannesen, A.B. & Larsen, C. 2014: Dinosaur tracks in Lower Jurassic coastal plain sediments (Sose Bugt Member, Rønne Formation) on Bornholm, Denmark. Lethaia,Vol. 47, pp. 485–493. Fluvial palaeochannels of coastal plain sediments of the Lower Jurassic Sose Bugt Member of the Rønne Formation exposed in the coastal cliffs at Sose Bugt, Bornholm, contain abundant dinosaur or other large vertebrate tracks in the form of deformation structures exposed in vertical section. The tracks are represented by steep-walled, flat- to-concave-bottomed depressions, with a raised ridge at each side. The tracks are filled with laminated sediments, draping the contours of the bottom of the depression. Un- derprints, stacked concave deformations beneath the prints, are present beneath each track. Contemporary Upper Triassic – Lower Jurassic strata from southern Sweden and Poland contain a diverse track fauna, supporting our interpretation. This is the earliest evidence of dinosaur activity in Denmark. □ Bornholm, coastal plain, dinosaur tracks, lake sediments, Lower Jurassic. Lars B. Clemmensen [[email protected]], Jesper Milan [[email protected]], Anne B. Joh- annesen [[email protected]], and Connie Larsen [[email protected]], Depart- ment for Geosciences and Natural Resource Managements, University of Copenhagen, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark; Jesper Milan [[email protected]], Geomuseum Faxe/Østsjællands Museum, Østervej 2, DK-4640 Faxe, Denmark; Gunver K. Pedersen [[email protected]], GEUS Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark; manuscript received on 12/04/2013; manuscript accepted on 04/12/2013.
    [Show full text]
  • An Introduction to the Mesozoic Biotas of Scandinavia and Its Arctic Territories
    Downloaded from http://sp.lyellcollection.org/ at Uppsala Universitetsbibliotek on August 1, 2016 An introduction to the Mesozoic biotas of Scandinavia and its Arctic territories BENJAMIN P. KEAR1*, JOHAN LINDGREN2, JØRN H. HURUM3,4, JESPER MILA` N5,6 & VIVI VAJDA2,7 1Museum of Evolution, Uppsala University, Norbyva¨gen 16, 752 36 Uppsala, Sweden 2Department of Geology, Lund University, So¨lvegatan 12, 223 62 Lund, Sweden 3Natural History Museum, University of Oslo, Postboks 1172, Blindern, 0318 Oslo, Norway 4The University Centre in Svalbard, UNIS, Postboks 156, 9171 Longyearbyen, Norway 5Geomuseum Faxe/Østsjællands Museum, Østervej 2, DK-3640 Faxe, Denmark 6Natural History Museum of Denmark, Øster Voldgade 5-7, DK-1350 Copenhagen K, Denmark 7Department of Palaeobiology, Swedish Museum of Natural History, Postboks 50007, SE-104 05 Stockholm, Sweden *Corresponding author (e-mail: [email protected]) Abstract: The Mesozoic biotas of Scandinavia have been studied for nearly two centuries. How- ever, the last 15 years have witnessed an explosive advance in research, most notably on the richly fossiliferous Triassic (Olenekian–Carnian) and Jurassic (Tithonian) Lagersta¨tten of the Norwe- gian Arctic Svalbard archipelago, Late Cretaceous (Campanian) Kristianstad Basin and Vomb Trough of Ska˚ne in southern Sweden, and the UNESCO heritage site at Stevns Klint in Denmark – the latter constituting one of the most complete Cretaceous–Palaeogene (Maastrichtian–Danian) boundary sections known globally. Other internationally significant deposits include earliest (Induan) and latest Triassic (Norian–Rhaetian) strata from the Danish autonomous territory of Greenland, and the Early Jurassic (Sinemurian–Pliensbachian) to Early Cretaceous (Berriasian) rocks of southern Sweden and the Danish Baltic island of Bornholm, respectively.
    [Show full text]
  • Geological Survey of Denmark and Greenland Bulletin 1, 145-216
    DENMARK, SOUTHERN SWEDEN AND THE NETHERLANDS Previous page: Jurassic sediments exposed in a clay-pit at Bagå on Bornholm, Denmark – see Michelsen et al. (2003, this volume). Photo: Peter K. Warna-Moors. Jurassic lithostratigraphy and stratigraphic development onshore and offshore Denmark Olaf Michelsen, Lars H. Nielsen, Peter N. Johannessen, Jan Andsbjerg and Finn Surlyk A complete updated and revised lithostratigraphic scheme for the Jurassic succession of the onshore and offshore Danish areas is presented together with an overview of the geological evo- lution. The lithostratigraphies of Bornholm, the Danish Basin and the Danish Central Graben are described in ascending order, and a number of new units are defined. On Bornholm, the Lower–Middle Jurassic coal-bearing clays and sands that overlie the Lower Pliensbachian Hasle Formation are referred to the new Sorthat Formation (Lower Jurassic) and the revised Bagå Formation (Middle Jurassic). In the southern Danish Central Graben, the Middle Jurassic succession formerly referred to the Lower Graben Sand Formation is now included in the revised Bryne Formation. The Lulu Formation is erected to include the uppermost part of the Middle Jurassic succession, previously referred to the Bryne Formation in the northern Danish Central Graben. The Upper Jurassic Heno Formation is subdivided into two new members, the Gert Member (lower) and the Ravn Member (upper). The organic-rich part of the upper Farsund Formation, the for- mer informal ‘hot unit’, is established formally as the Bo Member. Dominantly shallow marine and paralic deposition in the Late Triassic was succeeded by wide- spread deposition of offshore marine clays in the Early Jurassic.
    [Show full text]
  • Vertebrate Coprolites
    Bulletin 57 New Mexico Museum of Natural History & Science A Division of the DEPARTMENT OF CULTURAL AFFAIRS Vertebrate Coprolites edited by Adrian P. Hunt, Jesper Milàn, Spencer G. Lucas and Justin A. Spielmann Albuquerque, 2012 Hunt et al., eds., 2012, Vertebrate Coprolites. New Mexico Museum of Natural History and Science, Bulletin 57. 235 COPROLITES WITH PREY REMAINS AND TRACES FROM COPROPHAGOUS ORGANISMS FROM THE LOWER CRETACEOUS (LATE BERRIASIAN) JYDEGAARD FORMATION OF BORNHOLM, DENMARK JESPER MILÀN1,2, BO W. RASMUSSEN1,2 AND NIELS BONDE2 1 GeomuseumFaxe, Østsjællands Museum, Østervej 2, DK-4640 Faxe, Denmark, e-mail: [email protected]; 2 Department of Geography and Geology, University of Copenhagen, Østervoldgade 10, DK-1350 Copenhagen K, Denmark Abstract—Two fragmentary coprolites from the Lower Cretaceous Jydegaard Formation of Bornholm, Denmark, represent the first record of coprolites from continental Mesozoic deposits in Denmark. Both specimens contain fish scale bone fragments of unknown affinity. Based on morphology, inclusions and the potential producers found in the Jydegaard Formation, we suggest they were made by either a turtle or a theropod with a piscivorous diet. One specimen shows pits and grooves in the surface, as well as two deep cylindrical burrows, made by copropha- gous organisms. INTRODUCTION excavations in the sand pit during the last few years. One specimen is on display (unnumbered item) in the at-the-experience-center NaturBornholm Deposits with Mesozoic continental vertebrates are rare in Den- at Åkirkeby, Bornholm, and the other specimen is part of the collection mark, and are only found in a few restricted outcrops on the Baltic Island of the Natural History Museum of Denmark (MGUH 29809).
    [Show full text]
  • Bulletin of the Geological Society of Denmark, Vol
    Structural analysis of superposed fault systems of the Bornholm horst block, Tornquist Zone, Denmark OLE GRAVERSEN Graversen, O. 2009–11–15. Structural analysis of superposed fault systems of the Bornholm horst block, Tornquist Zone, Denmark © 2009 by Bulletin of the Geological Society of Denmark, Vol. 57, pp. 25–49. ISSN 0011–6297. (www.2dgf.dk/publikationer/bulletin) https://doi.org/10.37570/bgsd-2009-57-02 The Bornholm horst block is composed of Precambrian crystalline basement overlain by Palaeozoic and Mesozoic cover rocks. The cover intervals are separated by an angular unconformity and a hiatus spanning the Devonian through Middle Triassic interval. Late Palaeozoic faulting of the Early Pal-aeozoic Baltica platform is correlated with early-middle Carboniferous deformation in the Variscan foreland and with faulting associated with dolerite dyke injection in Skåne in the Late Carboniferous – Early Permian. The Palaeozoic fault systems are striking NW-SE and WNW-ESE and the platform series are dipping towards the SE and ESE respectively. The Mesozoic faulting was associated with the development of a horst-graben framework in the Bornholm-Skåne segment of the Sorgenfrei-Tornquist Zone. Mesozoic fault subsidence started in the Rønne Graben in the Triassic. In the Jurassic the Arnager-Sose block became active, cut off from the Bornholm block; in addition the Læså Graben (new) and the Øle Å fault block complex (new) were cut into the central Bornholm block from the south. In the Late Cretaceous the central Bornholm block was perforated by isolated fault blocks, i.e. the Nyker block, the Bøsthøj block and the Lobbæk block (new) along with subsidence of the Holsterhus block and renewed subsidence of the Arnager-Sose block.
    [Show full text]
  • An Enigmatic, Diminutive Theropod Footprint in the Shallow Marine Pliensbachian Hasle Formation, Bornholm, Denmark
    An enigmatic, diminutive theropod footprint in the shallow marine Pliensbachian Hasle Formation, Bornholm, Denmark JESPER MILAN AND FINN SURLYK Milan, J. & Surlyk, F. 2015: An enigmatic, diminutive theropod footprint in the shallow marine Pliensbachian Hasle Formation, Bornholm, Denmark. Lethaia , Vol. 48, pp. 429–435. A well-preserved three-toed footprint, measuring 34 mm in length from a very small predatory dinosaur with an estimated hip height of 153 mm and a total body length around 50 cm including tail, is reported from the type section of the marine Lower Jurassic (Pliensbachian), Hasle Formation on the Danish island of Bornholm in the Baltic Sea. The morphology of the footprint is similar to the ichnogenus Stenonyx Lull 1904 from the contemporaneous Pliensbachian Szydlowek site in Poland. Apart from the Polish material, footprints from diminutive dinosaurs are rare and reported from few other localities around the world. The occurrence of a diminutive dinosaur foot- print in a shallow marine sandstone is enigmatic. The well-defined morphology of the footprint, together with the very small size of the trackmaker, excludes the possibility that the track was emplaced by a swimming or wading animal. At the type locality where the footprint was found the formation consists of ferruginous coarse siltstone and very fine-grained sandstone, showing hummocky and swaley cross-stratification and rare large-scale trough cross-bedding and planar lamination. Deposition took place mainly in the upper shoreface in a storm-dominated environment 1 km west of the NÀS-oriented faulted coastline. The formation becomes thinner and finer grained with heterolithic intercalations towards the south, indicating coast-parallel transport in this direction.
    [Show full text]
  • Geology of Bornholm
    INTERNATIONAL GEOLOGlAL CONGRESS XXI SESSION NORDEN 1960 GEOLOGY OF BORNHOLM GUIDE TO EX CURSIONS NOS A 40 AN D C 45 BY HELGE GRY Editor of Danish guide-books : TH EODOR SORGENFREJ COPENHAGEN 1960 CONTENTS Page Outline of the geology of Bornholm . 3 Bibliography. 7 Field Guide . Il Key map: see back side of cover. Map of Bornholm: see folder. Exeursion no. A 45: Aug. 7th-11th 1960. C 40: Aug. 25th-29th 1960. Leader: Statsgeolog, dr. phil. HELGE GRY Danmarks Geologiske Undersøgelse Charlottenlund. -------�--- 1 l BORNHOLM BOUGUER ANOMALlES go-]j'o Equidistance: 2mgals l' •M•ouurlng point l ������-+--------------+,0���-�-�· ='="-"�·'-'�'-''�:���'-'_' -'�:��="�.-. � 6 _____ _ Mttu �1 $5°1 ' 1 6 l l r� �· . - ---------1--- _j� Fig. l. Outline of the Geology of Bornholm The island of Bornholm (58 7 km2) is one of the horsts of the Fenno-scandian border zone, i. e. the faulted zone between the Fennoscandian shield and the Danish - Polish sedimentary basin. The shape of the island is to a certain degree determined by the directions of the important faults of the area viz. faults trending WNW, N, NNE and NNW. Two faults are especially important, the one running along the west coast and the other running along the western part of the southwestern coast. These two faults are border faults of the horst proper. The dispiacement of the western fault 3 is, according to gravity measurements, abt. 1500 m (5000 ft), and the dispiacement of the southwestern fault is also considerable compared with the rest of the faults of the island. West and south of the two faults Triassic, Jurassic and Cretaceous rocks occur, whereas the rest of the island is built up of Pre-Cambrian and Lo­ wer Palaezoic rocks.
    [Show full text]