M
Malcolm B. Hart
Researcher at University of Plymouth
Publications - 185
Citations - 4723
Malcolm B. Hart is an academic researcher from University of Plymouth. The author has contributed to research in topics: Foraminifera & Cretaceous. The author has an hindex of 35, co-authored 184 publications receiving 4373 citations. Previous affiliations of Malcolm B. Hart include British Museum & University of Sheffield.
Papers
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Cenomanian palaeogeography of the North Atlantic and possible Mid-Cenomanian eustatic movements and their implications
Malcolm B. Hart,D. H. Tarling +1 more
TL;DR: In this paper, a major micropalaeontological non-sequence in the British Cenomanian correlates with similar features elsewhere in Europe and in North America and probably indicates a major eustatic episode in the mid-Cenomanians.
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New hybodontiform and neoselachian sharks from the Lower Triassic of Oman
Martha B. Koot,Gilles Cuny,Michael J. Orchard,Sylvain Richoz,Malcolm B. Hart,Richard J. Twitchett +5 more
TL;DR: For example, Koot et al. as discussed by the authors reported elasmobranchs from Lower Triassic (Lopingian-Olenekian) deposits in the Hawasina Basin of Oman.
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The Cretaceous/Paleogene boundary: Foraminifera, sea grasses, sea level change and sequence stratigraphy
TL;DR: In this article, the tsunami generated by the Chicxulub impact eroded the uppermost Cretaceous surface of the Gulf Coast region (U.S.A.) forming a distinctive topography that was previously interpreted as a sequence boundary.
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Foraminiferal recovery after the mid-Cretaceous oceanic anoxic events (OAEs) in the Cauvery Basin, southeast India
TL;DR: The Cauvery Basin, SE India, is one of the best exposed late Mesozoic to Tertiary basins in India, and the study of foraminiferal assemblages from the core samples obtained from two 120m deep wells in the basin records the occurrence of two mid-Cretaceous anoxic events as mentioned in this paper.
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Teredolites from the Garudamangalam sandstone formation (Late Turonian‐Coniacian), Cauvery basin, southeast India
TL;DR: Teredolites-infested loggrounds are abundant in the late Turonian-Coniacian Garudamangalam Sandstone Formation in the Cauvery Basin, Southeast India as mentioned in this paper.