Microbial community structure and standing stocks in the NE Atlantic in June and July of 1996

By Glen A. Tarran, Mikhail Zubkov, M. Sleigh, P. Burkill, M. Yallop. 2001

110 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/0ab2b1ece05e6fbc7805eec9afa6d68667e5768f

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In Ecology

1. Hongyue Dang
2. Farooq Azam
3. C. Robinson
4. H. Jeong
5. K. Seong
6. L. Legendre
7. W. Yih
8. David L. Kirchman

In Oceanography

1. M. Landry
2. A. Poulton
3. C. Daniels
4. R. Sheward
5. A. Charalampopoulou
6. C. Robinson
7. K. Seong
8. Farooq Azam

Citations in the corpus

• Seasonal dynamics of picoplankton in shelf waters of the southern Bay of Biscay (2006, result): “The overall abundance of picoeukaryotes was similar to that found in other studies (Buck et al. 1996, Tarran et al. 2001) and less variable than that of cyanobacteria, in agreement with reports from other zones (Liu et al. 2002).”
• Mechanisms of Microbial Carbon Sequestration in the Ocean - Future Research Directions (2014, background): “Cyclonic eddies enhance nutrient inputs to the surface ocean increasing new production (Falkowski et al., 1991; Harris et al., 1997; Moran et al., 2001) and chlorophyll concentrations (Arístegui et al., 1997; McGillicuddy Jr. et al., 1998; Tarran et al., 2001).”
• Biogeochemical implications of comparative growth rates of Emiliania huxleyi and Coccolithus species (2014, background): “…distributed throughout the oceans, the biogeography of C. pelagicus only covers 65 the Arctic Ocean and the sub-polar northern hemisphere (McIntyre and Bé, 1967; McIntyre et 66 al., 1970), with a particular prevalence in the sub-polar North Atlantic (Milliman, 1980; 67 Tarran et al., 2001).”
• Depth-stratified phytoplankton dynamics in Cyclone Opal, a subtropical mesoscale eddy (2008, background): “Eddies, in particular, are common and often long-lived features of ocean circulation with demonstrable, though highly variable, impacts on phytoplankton production, biomass and community structure (Allen et al., 1996; Froneman and Perissinotto, 1996; Tarran et al., 2001; Bidigare et al., 2003; Vai”
• Coccolithophore dynamics in non‐bloom conditions during late summer in the central Iceland Basin (July‐August 2007) (2010, methodology): “Cell abundances from flow cytometer counts were converted to biomass using literature values (Tarran et al. 2001, 2006).”
• Feeding by red-tide dinoflagellates on the cyanobacterium Synechococcus (2005, background): “These dinoflagellates usually co-occur with Synechococcus and/or the blooms of these dinoflagellates sometimes succeed those of Synechococcus (Taslakian & Hardy 1976, Chavez et al. 1996, Tarran et al. 1999, 2001, Duyl et al. 2002, Murrell & Lores 2004).”