Marine snow, organic solute plumes, and optimal chemosensory behavior of bacteria

By T. Kiørboe, G. Jackson. 2001

283 citations recorded by the source corpus.

Subfields: Atmospheric Science, Condensed Matter Physics, Ecology

View Paper: https://www.semanticscholar.org/paper/748959012eeb9bdfb0c5b4d755aba07a7fd43f18

How researchers see this paper

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

In Atmospheric Science

In Condensed Matter Physics

In Ecology

Citations in the corpus

Microbial Surface Colonization and Biofilm Development in Marine Environments (2015, background): “The release of labile DOC from POC degradation by particleassociated microorganisms may not only fuel the microbial loop (198, 273, 274) but also facilitate the priming effect that stimulates the degradation of recalcitrant organic matter (275, 276).”
Mechanisms of Microbial Carbon Sequestration in the Ocean - Future Research Directions (2014, background): “In fact, this plume may account for a significant fraction of the microbial production and remineralization (Kiorboe and Jackson, 2001).”
Microbial ecology of organic aggregates in aquatic ecosystems (2002, background): “…heterogeneities of nutrients in the bulk water, which may affect nutrient recycling and colonization processes by chemotactic microorganisms and remote chemosensoric detection by meso- and macrozooplankton (Kiørboe 2001, Kiørboe & Jackson 2001, Kiørboe & Thygesen 2001, Kiørboe et al. 2001).”
Mesopelagic zone ecology and biogeochemistry - a synthesis (2010, background): “Freeliving bacteria in the deep-ocean may sense the enriched nutrient environment around a particle and actively swim towards it (Jackson, 1989; Blackburn and Fenchel, 1999; Kiørboe and Jackson, 2001), forming a ‘detritosphere’ ecosystem around the particle (Biddanda and Pomeroy, 1988).”
Formation and fate of marine snow: small-scale processes with large- scale implications (2001, methodology): “We have simulated colonization rates of bacteria with chemokinetic behaviour assuming a swimming velocity of 100 µm s-1 and a tumbling frequency of 1 s-1 and optimal chemosensory capabilities (Kiørboe and Jackson, 2001).”
Benthic life in the pelagic: Aggregate encounter and degradation rates by pelagic harpacticoid copepods (2005, methodology): “The size spectrum can, however, be estimated from the volume concentration if one assumes a power function to represent the aggregate size spectrum and assumes the exponent of the size spectrum to be three (Jackson et al. 1997; Kiørboe and Jackson 2001).”
Microbial oceanography of the dark ocean's pelagic realm (2009, background): “Many of these are able to sense nutrient gradients (Jackson 1989; Blackburn and Fenchel 1999; Kiørboe and Jackson 2001) and actively swim towards the aggregates assimilating organic compounds, which are solubilized by the colonizers (Fenchel 2001, 2002; Kiørboe et al. 2002).”
Emerging concepts on microbial processes in the bathypelagic ocean-ecology, biogeochemistry, and genomics (2010, background): “Kiørboe and Jackson (2001) developed a model to explain the formation of a plume of DOM streaming behind sinking particles.”
Turnover of dead jellyfish: stimulation and retardation of microbial activity (2006, background): “Dead jellyfish, and the chemical plumes (cf. Kiørboe & Jackson 2001) around them, constitute habitats and food for both microorganisms and larger invertebrates.”
The multiple fates of sinking particles in the North Atlantic Ocean (2015, background): “The POMsusp and DOM can then provide an immediate metabolic substrate for free-living bacteria in the water column [Kiørboe and Jackson, 2001].”