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Jennifer Huggett

Researcher at Natural History Museum

Publications -  51
Citations -  1308

Jennifer Huggett is an academic researcher from Natural History Museum. The author has contributed to research in topics: Illite & Authigenic. The author has an hindex of 18, co-authored 47 publications receiving 1108 citations. Previous affiliations of Jennifer Huggett include University of Greenwich & East Sussex County Council.

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Marine biodiversity through the Late Cenomanian–Early Turonian: palaeoceanographic controls and sequence stratigraphic biases

TL;DR: In this paper, changes in marine macro-and microfauna, sedimentary geochemistry and surface-water palaeoproductivity through the last 500 to 1000 years of the Cenomanian and first 300 to 400 years of Turonian are documented.
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Evolution of the Toarcian (Early Jurassic) carbon-cycle and global climatic controls on local sedimentary processes (Cardigan Bay Basin, UK)

TL;DR: In this paper, the authors present integrated geochemical and physical proxy data (high-resolution carbon-isotope data (δ13C), bulk and molecular organic geochemistry, inorganic petrology, mineral characterisation, and major and trace-element concentrations) from the biostratigraphically complete and expanded entire Toarcian succession in the Llanbedr (Mochras Farm) Borehole, Cardigan Bay Basin, Wales, UK.
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Petrology and palaeoenvironmental significance of glaucony in the Eocene succession at Whitecliff Bay, Hampshire Basin, UK

TL;DR: This article investigated the value of glaucony as a palaeoenvironmental indicator through an investigation of the pellets, and their distribution and reworking in the predominantly brackish to shallow marine Tertiary sediments of the Hampshire basin, together with a reevaluation of the sedimentology.
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Late Jurassic palaeoclimatic change from clay mineralogy and gamma-ray spectrometry of the Kimmeridge Clay, Dorset, UK

TL;DR: In this article, a new clay mineral dataset is presented from a 600 m thick composite core through the Kimmeridge Clay Formation, southern England, which contains mainly illite and kaolinite, with minor randomly interstratified illite-smectite mixed layer clays.
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Low-temperature illitization of smectite in the late eocene and early oligocene of the Isle of Wight (Hampshire basin), U.K.

TL;DR: In this article, the illite-smectite transition has been investigated in the <0.5 μm fraction by XRD analysis (powder and oriented mounts), thermogravimetry (TG), analytical SEM, and chemical analysis of Fe2+.