scispace - formally typeset
D

David M. Moore

Researcher at University of Reading

Publications -  11
Citations -  278

David M. Moore is an academic researcher from University of Reading. The author has contributed to research in topics: Holocene & Sclereid. The author has an hindex of 9, co-authored 11 publications receiving 263 citations.

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Post-glacial vegetation in the South Patagonian territory of the giant ground sloth, Mylodon

TL;DR: In this article, the authors reconstructed the changing postglacial vegetation of the region from macrofossils derived from deposits in the Cueva de Patagonia in southern Chile.
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Morphological and palynological studies in Phlomis L., Eremostachys Bunge and Paraphlomis Prain (Labiatae)

TL;DR: Information from morphology and palynology, together with anatomical, cytological and chemical data, is utilized to examine the status of the genus Phlomis and its close relatives Eremostachys and ParaphLomis, and strongly support the removal of the Chinese species, Ph lomis rolata, to the genus Lamiophlom is.
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Chemotaxonomy, variation and geographical distribution of the Empetraceae

TL;DR: In Empetrum, the flavonoids differ modally in the three species usually accepted, thus confirming data on fruit colour and breeding systems, and suggesting that the genus comprises one species with about three subspecies at diploid and tetraploid levels.
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The taxonomic significance of leaf micromorphology in the genus Eugenia L. (Myrtaceae)

TL;DR: Leaf micromorphological features of both the Old and New World representatives of Eugenia L. axillaris have been studied and the taxonomic significance of these features in identification and elucidation of species from both areas is discussed.
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Late Pleistocene and Holocene landscape evolution and environmental change in the Lake Sulivan area, Falkland Islands, South Atlantic.

TL;DR: In this article, the late Pleistocene and Holocene landscape evolution around Lake Sulivan, Falkland Islands, South Atlantic, is assessed using morphological, stratigraphical, palaeoecological and 14C-dating evidence.