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Ireneusz Walaszczyk
University of Warsaw
CretaceousGeologyPaleontologyInoceramusBiostratigraphy
81Publications
21H-index
1,680Citations
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#1Andrew S. Gale (University of Portsmouth)H-Index: 42
#2William James Kennedy (University of Oxford)H-Index: 37
Last. Ireneusz Walaszczyk (University of Warsaw)H-Index: 21
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The lithostratigraphy, biostratigraphy, sequence stratigraphy, ammonite and inoceramid faunas of the Upper Albian, Cenomanian, and Lower Turonian Karai Formation, the highest unit of the Uttatur Group in the Pondicherry Sub-Basin of the Cauvery Basin in Tamil Nadu, south India, are documented. Detailed logs and descriptions of sections between Karai and Kulakkalnattam, Odiyam and Kunnam, and north-west of Garudamangalam are presented. They provide the evidence for an ammonite zonal scheme that c...
2 Citations
The Upper Turonian to Middle Coniacian (Upper Cretaceous) succession of the Babadag Basin (North Dobrogea, Romania) constitutes an apparently continuous fossiliferous carbonate succession. The presence of moderately rich inoceramid, ammonite and foraminiferal assemblages allows for the application of a precise biostratigraphic subdivision. The palaeoenvironmental conditions and evolution of the Babadag Basin during the Late Turonian–Middle Coniacian are inferred using microfacies analysis and fo...
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#1A. Guy Plint (UWO: University of Western Ontario)H-Index: 28
#2Jessica R. Krawetz (UWO: University of Western Ontario)H-Index: 3
Last. Ireneusz Walaszczyk (University of Warsaw)H-Index: 21
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In north-central Alberta and adjacent British Columbia, clastic strata of the middle to late Albian Peace River and Shaftesbury formations were deposited in alluvial to shallow marine environments across the foredeep of the Western Canada Foreland Basin. A high-resolution, log and core-based allostratigraphic framework for the Paddy Member of the Peace River Formation established nine allomembers, PA to PI, bounded by flooding surfaces and apparently equivalent non-marine surfaces. Within the es...
2 CitationsSource
#1Ireneusz Walaszczyk (University of Warsaw)H-Index: 21
#2William James Kennedy (University of Oxford)H-Index: 37
Last. Amruta R. ParanjapeH-Index: 1
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The lower (but not lowermost) part of the Upper Cretaceous Anaipadi Formation of the Trichinopoly Group in the area between Kulatur, Saradamangalam and Anaipadi, in the south-western part of the Cauvery Basin in southeast India yielded rich inoceramid and ammonite faunas. The ammonites: Mesopuzosia gaudama (Forbes, 1846), Damesites sugata (Forbes, 1846), Onitschoceras sp., Kossmaticeras ( Kossmaticeras ) theobaldianum (Stoliczka, 1865), Lewesiceras jimboi (Kossmat, 1898), Placenticeras kaffrariu...
2 Citations
ANDRZEJ M. RADWAŃSKI 24th July 1934 – 7th January 2016 Professor Andrzej Radwanski died peacefully at the age of 81 on January 7, 2016. Active in the science he loved to the end of his life, his death took from us a much loved husband, father, grandfather and colleague. Geology lost one of the masters of the subject, who roamed over close on half a billion years of earth history with consummate ease. He is survived by his wife Ula, son Michal, daughter-in-law Ania, and granddaughters Alicja and ...
#1Dee Ann CooperH-Index: 2
#2Roger W. CooperH-Index: 1
Last. Ireneusz Walaszczyk (University of Warsaw)H-Index: 21
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The upper lower Cenomanian through middle Santonian (Upper Cretaceous) of the Boquillas Formation in the Big Bend Region of Trans-Pecos Texas consists of a marine carbonate succession deposited at the southern end of the Western Interior Seaway. The Boquillas Formation, subdivided into the lower, c. 78 m thick limestone-shale Ernst Member, and the upper, c. 132 m thick limestone/chalk/marl San Vicente Member, was deposited in a shallow shelf open marine environment at the junction between the We...
2 CitationsSource
#1Ireneusz Walaszczyk (University of Warsaw)H-Index: 21
#2Christopher J. Wood (University of Warsaw)H-Index: 1
Abstract The Staffhorst shaft (Lower Saxony, Germany) ranks amongst the critical sections for documentation of the inoceramid record of the Euramerican Coniacian Stage (Upper Cretaceous). In spite of a number of disadvantages (i.e., interval sampling and stratigraphical gaps), this section does provide details of the inoceramid distribution across insufficiently known substage boundary intervals of the Coniacian. The lower–middle Coniacian boundary is marked by the Inoceramus gibbosus Zone, at t...
2 CitationsSource
#1Neil H. LandmanH-Index: 28
#2A. Guy PlintH-Index: 28
Last. Ian JarvisH-Index: 33
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172 pages, 15 folded leaves of plates : illustrations (some color), maps (some color) ; 26 cm. chapter 1. Integrated, high-resolution allostratigraphic, biostratigraphic and carbon-isotope correlation of Coniacian strata (Upper Cretaceous), western Alberta and northern Montana / A. Guy Plint, Elizabeth A. Hooper, Meriem D. Grifi, Ireneusz Walaszczyk, Neil H. Landman, Darren R. Grocke, Joao P. Trabucho Alexandre, and Ian Jarvis -- chapter 2. Inoceramid bivalves from the Coniacian and basal Santon...
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