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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.

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The Global Boundary Stratotype Section and Point (GSSP) for the base of the Pliensbachian Stage (Lower Jurassic), Wine Haven, Yorkshire, UK.

TL;DR: Following votes by the Pliensbachian Working Group, the Jurassic Subcommission and the International Commission on Stratigraphy, IUGS rati.ed the proposed Global Boundary Stratotype Section and Point (GSSP) for the base of the lower Jurassic at the bottom of bed 73b in the Wine Haven section, Robin Hood's Bay, Yorkshire Coast, UK.
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Chemostratigraphy of the Upper Albian to mid‐Turonian Natih Formation (Oman) – how authigenic carbonate changes a global pattern

TL;DR: In this paper, the authors established a biostratigraphy and chemostratigy of the Natih Formation and reconstructed depositional conditions of organic-rich sediments in an intra-platform basin during Cenomanian-Turonian times.
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Orbitally induced cycles in the chalk facies of the United Kingdom

TL;DR: In this paper, the characteristic rhythmic bedding of the Upper Cretaceous pelagic carbonate sequences of the United Kingdom is interpreted as the result of orbital variations, and a 23,000 year and a 41.500 year cycle have been recognized and can be used to confirm the dating of late Cenomanian events.
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Magnitude and profile of organic carbon isotope records from the Paleocene-Eocene Thermal Maximum: Evidence from northern Spain

TL;DR: In this paper, high-resolution organic carbon profiles of six PETM sections in northern Spain are presented that span a transect from continental to marine environments and allow a comparison of the magnitude of the excursion, the shape of the vertical δ13Cδ 13C profile during the PETM episode, and the relative timing of the onset of the associated Carbon Isotope Excursion across a linked sediment routing system.
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Isotopic analysis of coexisting Late Jurassic fish otoliths and molluscs: Implications for upper-ocean water temperature estimates

TL;DR: The negative carbon isotopes of the otoliths may point to a freshwater flow and potentially migratory nature of the marine environment as mentioned in this paper, given the large departures from equilibrium fractionation toward more negative carbon values reported from modern marine fi sh.