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Andrew J. Gooday
Researcher at National Oceanography Centre
Publications - 233
Citations - 16367
Andrew J. Gooday is an academic researcher from National Oceanography Centre. The author has contributed to research in topics: Foraminifera & Benthic zone. The author has an hindex of 59, co-authored 221 publications receiving 14737 citations. Previous affiliations of Andrew J. Gooday include National Oceanography Centre, Southampton & University of Geneva.
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Giant, highly diverse protists in the abyssal Pacific: vulnerability to impacts from seabed mining and potential for recovery.
TL;DR: Xenophyophores, giant deep-sea agglutinated foraminifera, dominate the benthic megafauna in the eastern equatorial Pacific Clarion-Clipperton Zone and could be among the first large immobile organisms to reappear in mining-impacted areas.
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Megafaunal ecology of the western Clarion Clipperton Zone
Jennifer M. Durden,Meagan Putts,Sarah R. D. Bingo,Astrid B. Leitner,Jeffrey C. Drazen,Andrew J. Gooday,Andrew J. Gooday,Daniel O.B. Jones,Andrew K. Sweetman,Travis Washburn,Craig R. Smith +10 more
TL;DR: In this article, a combination of seabed photography and direct sampling was used to assess the environment and megafauna on the soft sediment habitats on the abyssal plain in three Areas of Particular Environmental Interest (APEIs) and seamounts in two of those APEIs.
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Agglutinated foraminifera (superfamily Hormosinacea) across the Indian margin oxygen minimum zone (Arabian Sea)
TL;DR: A semi-quantitative survey of ‘live’ and dead hormosinacean foraminifera at six sites across the Indian margin oxygen minimum zone (OMZ) finds that at least two Reophax species are common to the Indian and Pakistan margin OMZ; one of these may be confined to the core of the Arabian Sea OMZ.
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The organic-walled genera Resigella and Conicotheca (Protista, Foraminifera) at two Arctic deep-sea sites (North Pole and Barents Sea), including the description of a new species of Resigella
TL;DR: A new organic-walled foraminiferan species from the central Arctic Ocean (North Pole; 4,300 m water depth) and the Håkon Mosby Mud Volcano (HMMV) at the south-western Barents Sea continental margin is described based on morphological features.