A5037993049- Paleontology and Stratigraphy of Fossils
- Hydrocarbon exploration and reservoir analysis
- Geology and Paleoclimatology Research
- Geological Studies and Exploration
- Geological and Geophysical Studies
- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Geological formations and processes
- Evolution and Paleontology Studies
- Paleontology and Evolutionary Biology
- Geological and Geophysical Studies Worldwide
- Archaeological and Geological Studies
- Geological Formations and Processes Exploration
- Geochemistry and Elemental Analysis
- Space Exploration and Technology
- Marine Biology and Ecology Research
- Scientific Research and Discoveries
- Astro and Planetary Science
- Marine and coastal plant biology
- Image Processing and 3D Reconstruction
- Fish biology, ecology, and behavior
- Pleistocene-Era Hominins and Archaeology
- Study of Mite Species
- Fossil Insects in Amber
- Ancient and Medieval Archaeology Studies
University of Pisa
2009-2023
National Museum of Denmark
2023
University of Copenhagen
2023
Cambrian to Lower Ordovician acritarchs and conodont species have been recorded from the Furuhäll Section at Köpingsklint on Öland, Sweden. The are represented by three different microfloras. first is found base of section investigated characterized association Cristallinium cambriense with Eliasum llaniscum, Retisphaeridium dichamerum R. howellii. This microflora has in strata previously referred Paradoxides paradoxissimus trilobite Superzone.
 second includes Timofeevia lancarae, T....
Shanchi Peng, Loren E. Babcock, Jingxun Zuo, Huanling Lin, Xuejian Zhu, Xianfeng Yang, Richard A. Robison, Yuping Qi, Gabriella Bagnoli, Yong'an Chen. Episodes 2009;32:41-55. https://doi.org/10.18814/epiiugs/2009/v32i1/006
Shanchi Peng, Loren E. Babcock, Jingxun Zuo, Xuejian Zhu, Huanling Lin, Xianfeng Yang, Yuping Qi, Gabriella Bagnoli, Longwu Wang. Episodes 2012;35:462-77. https://doi.org/10.18814/epiiugs/2012/v35i4/002
Terfelt, F, Bagnoli, G. & Stouge, S. 2011: Re-evaluation of the conodont Iapetognathus and implications for base Ordovician System GSSP. Lethaia, Vol. 45, pp. 227–237. In 2000, International Union Geological Sciences (IUGS) ratified decision from Working Group on Cambrian–Ordovician Boundary (COBWG) to place Global boundary Stratotype Section Point (GSSP) in Green section, Newfoundland, Canada, at a point coinciding with first appearance fluctivagus. However, restudy successions shows that...
In 2019 the Sub-Commission on Ordovician System approved Xiaoyangqiao section, North China as a new ASSP section for base of System.The sedimentary succession is exposed in natural outcrop near Dayangcha Village at position 42 °3'24''N, 126 °42'21''E.It has well-preserved, abundant and diverse fossil record across boundary with key markers (conodonts graptolites), which provide improved intercontinental correlation Cambrian-Ordovician boundary.The appearance first planktonic graptolites...
Abstract The current study presents new bed‐by‐bed brachiopod δ 13 C and 18 O records from Öland, Sweden, which together with previously published data the East Baltic region, constitutes a high‐resolution paired bulk rock carbon oxygen isotope archive through Lower to Upper Ordovician successions of Baltoscandia. This set refines temporal control on global O‐trend considerably, improving paleoenvironmental reconstructions main phase Great Biodiversification Event (GOBE). Öland display...
The Alum Shale Formation exposed at the Degerhamn quarry road section, southern Öland, Sweden, contains a diversified assemblage of euconodonts, paraconodonts and protoconodonts, majority which have ranges confined to Furongian Series (Cambrian). first occurrence (FO) cosmopolitan euconodont species Proconodontus muelleri is recorded in uppermost part Ctenopyge spectabilis trilobite Zone appearance datum Cordylodus? andresi upper Parabolina lobata Zone. Three new successive paraconodont...
The Cape Cormorant Formation of the Table Head Group exposed on Port au Peninsula, western Newfoundland, is composed dark-brown to black shales with interbeds thin calcareous silty and sandy distal turbidites. Distinctive carbonate conglomerates breccias derived from foundering shelf are occasionally found in formation. sediments accumulated foreland basin formed during early stage Taconic orogeny. faunas upper part include graptolites, conodonts, chitinozoans. graptolites well preserved,...
The Pre-Mesozoic units exposed in the inner Northern Apennines mostly consist of Pennsylvanian-Permian successions unconformably deposited on a continental crust consolidated at end Variscan orogenic cycle (Silurian-Carboniferous). In Apennines, exposures this crust, Cambrian?-Devonian age, have been described Tuscany, Elba Island (Tuscan Archipelago) and, partly, scattered and isolated outcrops southern Tuscany. This paper reappraises most significant succession (i.e., Risanguigno...