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Robert Hall

Researcher at Wageningen University and Research Centre

Publications -  561
Citations -  32813

Robert Hall is an academic researcher from Wageningen University and Research Centre. The author has contributed to research in topics: Provenance & Basement (geology). The author has an hindex of 81, co-authored 525 publications receiving 28159 citations. Previous affiliations of Robert Hall include Rice University & University College London.

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Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations

TL;DR: In this article, a model for the Cenozoic development of the region of SE Asia and the SW Pacific is presented and its implications are discussed, accompanied by computer animations in a variety of formats.
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Enrichment of tomato fruit with health-promoting anthocyanins by expression of select transcription factors.

TL;DR: In this paper, the authors expressed two transcription factors from snapdragon in tomato, and found that the fruit of the plants accumulated anthocyanins at levels substantially higher than previously reported for efforts to engineer Anthocyanin accumulation in tomato and at concentrations comparable to the levels found in blackberries and blueberries.
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Plant molecular stress responses face climate change.

TL;DR: The role which '-omics' research, coupled to systems biology approaches, can play in future research on plants seemingly unable to adapt as well as those which can tolerate climatic change is addressed.
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Untargeted large-scale plant metabolomics using liquid chromatography coupled to mass spectrometry

TL;DR: A detailed protocol for large-scale untargeted metabolomics of plant tissues, based on reversed phase liquid chromatography coupled to high-resolution mass spectrometry (LC-QTOF MS) of aqueous methanol extracts is described.
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Late Jurassic–Cenozoic reconstructions of the Indonesian region and the Indian Ocean

TL;DR: The Sundaland region was assembled by closure of Tethyan oceans and addition of continental fragments in the Cretaceous and Cenozoic as discussed by the authors, and a marked change in deep mantle structure at about 110°E reflects different subduction histories north of India and Australia since 90-Ma.