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Jim D. Marshall

Researcher at University of Liverpool

Publications -  85
Citations -  6350

Jim D. Marshall is an academic researcher from University of Liverpool. The author has contributed to research in topics: Diagenesis & Carbonate. The author has an hindex of 39, co-authored 84 publications receiving 5836 citations. Previous affiliations of Jim D. Marshall include Spanish National Research Council & University of Reading.

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Palaeoclimate interpretation of stable isotope data from lake sediment archives

TL;DR: A review of the controls on the isotope composition of lacustrine skeletal and non-skeletal deposits and how stable isotope studies contribute to an understanding of changes in temperature, precipitation patterns, evaporation and the carbon cycle can be found in this article.
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Climatic and oceanographic isotopic signals from the carbonate rock record and their preservation

TL;DR: In this paper, the effects of post-depositional diagenetic alteration of marine limestones are identified using a combination of their mineralogical potential and depositional setting, together with subsequent changes in relative sea-level and burial history.
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Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse period

TL;DR: The end Ordovician glaciation is distinct among Phanerozoic glaciations in that CO 2, levels were generally high, yet major continental ice sheets accumulated on the Gondwana supercontinent as mentioned in this paper.
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High-resolution stable isotope stratigraphy of Upper Ordovician sequences: Constraints on the timing of bioevents and environmental changes associated with mass extinction and glaciation

TL;DR: In this article, the authors argue that the distinctive Late Ordovician carbon isotope profile provides a chronostratigraphic "ruler" against which a sequence of environmental and biotic events may be located.
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The Cenomanian-Turonian boundary at Eastbourne (Sussex, UK): a proposed European reference section

TL;DR: The Cenomanian-Turonian boundary (CTB) section at Eastbourne, Sussex, England is the thickest at outcrop in the Anglo-Paris Basin, is rich in macro-, micro- and nanno-fossils, and shows less diagenetic alteration than other sections in NW Europe.