Biological Responses to Seasonally Varying Fluxes of Organic Matter to the Ocean Floor: A Review

By A. Gooday. 2002

294 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/c230b7875a6f1f5acd85e0bb669a820135cfb94d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

In Global and Planetary Change

In Oceanography

Citations in the corpus

Population structure of the oldest known macroscopic communities from Mistaken Point, Newfoundland (2013, background): “…exploiting new substrate, and more likely represent climax communities with differences in taxonomic composition and relative abundance reflecting local conditions of current energy, nutrient availability, and dissolved oxygen (see also Grazhdankin 2004; Wilby et al. 2011; Gehling and Droser 2013).”
On some hypotheses of diversity of animal life at great depths on the sea floor (2015, background): “As such, the abundance and biomass of benthic organisms is related directly to the amount of food reaching the sediment surface (Gooday 2002; Smith et al. 2008; McClain et al. 2012a,b).”
Biodiversity of macrofaunal assemblages from three Portuguese submarine canyons (NE Atlantic) (2011, background): “In the deep-sea, benthic macrofaunal assemblages are highly dependent on allochthonous organic matter (Rowe, 1981; Billett et al., 1983; Gooday, 2002; Rex et al., 2006; Smith et al., 2008) and their abundance usually declines with increasing water depth and increasing distance from shore (Sanders et”
Environmental and Gut Bacteroidetes: The Food Connection (2011, background): “Coastal and deep-sea environments typically receive seasonal pulses of organic matter after phytoplankton bloom events (Gooday, 2002; Kim et al., 2009).”
Spatial and temporal variations in deep-sea meiofauna assemblages in the Marginal Ice Zone of the Arctic Ocean (2007, background): “This means that in practice it is difficult to distinguish between temporal variability and spatial patchiness (Gooday, 2002).”
Benthic foraminifera as trophic links between phytodetritus and benthic metazoans: carbon and nitrogen isotopic evidence (2008, background): “Unpronounced seasonality of the metazoan meiobenthos in relation to phytodetritus deposition was also shown in the review by Gooday (2002).”
The Role of Biodiversity in the Functioning of Freshwater and Marine Benthic Ecosystems (2004, unknown): “As a result, the dynamics of benthic ecosystems contrast with those of terrestrial ecosystems in that they are largely shaped by the surrounding fluid (water), which induces shear stress at the sediment‐water interface (Kling et al. 2000, Gooday 2002 ).”
The deep-sea floor ecosystem: current status and prospects of anthropogenic change by the year 2025 (2003, background): “…more rapidly reproducing biota, such as microbes and foraminifera, show a rapid population response to episodic food input at the deep-sea floor, whereas larger, more longerlived taxa generally integrate seasonal changes and may only respond to interannual and decadal changes (Gooday 2002).”