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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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Environmental influences on regional deep-sea species diversity

TL;DR: A conceptual model of how interdependent environmental factors shape regional-scale variation in local diversity in the deep sea is presented, showing how environmental gradients may form geographic patterns of diversity by influencing local processes such as predation, resource partitioning, competitive exclusion, and facilitation that determine species coexistence.
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A response by benthic Foraminifera to the deposition of phytodetritus in the deep sea

Andrew J. Gooday
- 01 Mar 1988 - 
TL;DR: Evidence is presented that certain small benthic Foraminifera (within the meiofaunal size-range) react dramatically to the presence of phytodetritus, suggesting that some deep-sea bentho-foramina are specialist feeders that bloom opportunistically when the appropriate food becomes available, while others remain unaffected by the organic influx.
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Effects of natural and human-induced hypoxia on coastal benthos

TL;DR: Large areas of low oxygen persist seasonally or continuously beneath upwelling regions, associated with the upper parts of oxygen minimum zones (SE Pacific, W Africa, N Indian Ocean), and support a resident fauna that is adapted to survive and reproduce at oxygen concentrations.
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Exponential Decline of Deep-Sea Ecosystem Functioning Linked to Benthic Biodiversity Loss

TL;DR: This study provides scientific evidence that the conservation of deep-sea biodiversity is a priority for a sustainable functioning of the worlds' oceans and suggests that mutually positive functional interactions can be common in the largest biome of the authors' biosphere.
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Responses by benthic organisms to inputs of organic material to the ocean floor:a review.

TL;DR: In this article, it has been shown that macroaggregates originating from the euphotic zone settle at a rate of approximately 100-150 m d -1 to form a deposit (phytodetritus) on the sediment surface.