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Antonietta Quigg

Researcher at Texas A&M University at Galveston

Publications -  168
Citations -  10454

Antonietta Quigg is an academic researcher from Texas A&M University at Galveston. The author has contributed to research in topics: Phytoplankton & Corexit. The author has an hindex of 37, co-authored 164 publications receiving 8829 citations. Previous affiliations of Antonietta Quigg include Hospital Corporation of America & Texas A&M Health Science Center College of Medicine.

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Environmental behavior and ecotoxicity of engineered nanoparticles to algae, plants, and fungi

TL;DR: The surface properties of ENPs are of essential importance for their aggregation behavior, and thus for their mobility in aquatic and terrestrial systems and for their interactions with algae, plants and, fungi as mentioned in this paper.
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The Evolution of Modern Eukaryotic Phytoplankton

TL;DR: The geological, geochemical, and biological processes that contributed to the rise of the dinoflagellates, coccolithophores, and diatoms all contain plastids derived from an ancestral red alga by secondary symbiosis are examined.
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Phytoplankton in a changing world: cell size and elemental stoichiometry

TL;DR: It is suggested that cell size and elemental stoichiometry are promising ecophysiological traits for modelling and tracking changes in phytoplankton community structure in response to climate change.
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The elemental composition of some marine phytoplankton

TL;DR: A comparison of results with published data suggests that the measured compositions reflect chiefly the intrinsic trace element physiology of the individual species, and provides a basis for examining how phytoplankton influence the relative distributions of the ensemble of major and trace elements in the ocean.
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The evolutionary inheritance of elemental stoichiometry in marine phytoplankton

TL;DR: The compositional differences between the two plastid superfamilies suggest that changes in ocean redox state strongly influenced the evolution and selection of eukaryotic phytoplankton since the Proterozoic era.